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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;2025年11月25日 (火) 14:37時点における版&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;1行目:&lt;/td&gt;
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/del&gt;an unprecedented &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution &lt;/del&gt;simulation for &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:WilliemaePittman portable cutting shears] &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convection zone. Our calculation reproduces the fast equator and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/del&gt;shear layer (NSSL) of differential rotation and the near-floor poleward meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;move &lt;/del&gt;simultaneously. The NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;positioned &lt;/del&gt;in a complex layer where the spatial and time scales of thermal convection are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considerably &lt;/del&gt;small &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in contrast &lt;/del&gt;with the deep convection zone. While there have been several makes an attempt to reproduce the NSSL in numerical simulation, the results are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;still removed &lt;/del&gt;from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reality&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;On &lt;/del&gt;this &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/del&gt;, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drive &lt;/del&gt;within the NSSL. We emphasize the significance of the magnetic &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field &lt;/del&gt;in the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and the sluggish pole. Omega within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar inside&lt;/del&gt;. Within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convection zone, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;have now &lt;/del&gt;two shear layers, i.e., the tachocline &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;around &lt;/del&gt;the base of the convection zone and the near-surface shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;interplay &lt;/del&gt;between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the layer. T/g,  [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http&lt;/del&gt;://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;service&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;megaworks.ai&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;board&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bbs/board&lt;/del&gt;.php?&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bo_table&lt;/del&gt;=&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;hwang_form&amp;amp;wr_id=3311145 portable cutting shears&lt;/del&gt;] &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the place TT and gg are the temperature and &lt;/del&gt;the gravitational acceleration, respectively. 60 and a pair of Mm, respectively. Thus, the time scales of the convection vary from a month to several hours in these &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;areas&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As a result&lt;/del&gt;, the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the NSSL is just not &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly &lt;/del&gt;affected by the rotation. ′ denote the longitudinal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;common &lt;/del&gt;and the deviation from the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In addition&lt;/del&gt;, Miesch &amp;amp; Hindman (2011) suggest that we need a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pressure &lt;/del&gt;to stability with the latitudinal Coriolis drive to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/del&gt;the NSSL. It's &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;difficult &lt;/del&gt;for numerical simulations to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cover &lt;/del&gt;a broad &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;vary &lt;/del&gt;of spatial and time scales. The numerical &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;approach &lt;/del&gt;for the NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highly &lt;/del&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;improve &lt;/del&gt;the superadiabaticity around the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;top &lt;/del&gt;boundary of their calculation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;focus on &lt;/del&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;particularly &lt;/del&gt;at low and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high &lt;/del&gt;latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulate&lt;/del&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/del&gt;an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;additionally &lt;/del&gt;fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;development &lt;/del&gt;mechanism of the meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement have to &lt;/del&gt;be understood to reproduce the proper NSSL. Of their &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highly &lt;/del&gt;rotationally constrained convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;referred to &lt;/del&gt;as the Busse column, is required to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/del&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;diminished &lt;/del&gt;the photo voltaic luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) increased the rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;price &lt;/del&gt;so as to enhance the rotational &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;influence &lt;/del&gt;on the thermal convection. We word that the lower in luminosity and the rise in rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge &lt;/del&gt;have the identical &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;impact &lt;/del&gt;on the Rossby &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantity&lt;/del&gt;. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even within the close to-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor high &lt;/del&gt;Rossby &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantity &lt;/del&gt;layer. The environment friendly &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;technology &lt;/del&gt;of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/del&gt;-floor circulation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;via &lt;/del&gt;the gyroscopic pumping effectively suppresses the development of the NSSL. When the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;previous &lt;/del&gt;calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;didn't &lt;/del&gt;have any approach to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like DR &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out using &lt;/del&gt;the lowered luminosity, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;larger &lt;/del&gt;rotation charges or enhanced diffusivities (&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convective conundrum). That is, the typical &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;not too long ago &lt;/del&gt;provide a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;possible resolution &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;construct &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/del&gt;-like differential rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out &lt;/del&gt;using &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;particular &lt;/del&gt;therapy proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/ins&gt;an unprecedented &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decision &lt;/ins&gt;simulation for the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convection zone. Our calculation reproduces the fast equator and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/ins&gt;shear layer (NSSL) of differential rotation and the near-floor poleward meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement &lt;/ins&gt;simultaneously. The NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;located &lt;/ins&gt;in a complex layer where the spatial and time scales of thermal convection are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly &lt;/ins&gt;small &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;compared &lt;/ins&gt;with the deep convection zone. While there have been several makes an attempt to reproduce the NSSL in numerical simulation, the results are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;nonetheless far &lt;/ins&gt;from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actuality&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/ins&gt;this &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/ins&gt;, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[https://rentry.co/2565-tips-on-how-to-check-in-case-your-barber-shears-are-sharp-enough-to-chop-hair Wood Ranger Power Shears] &lt;/ins&gt;within the NSSL. We emphasize the significance of the magnetic &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;area &lt;/ins&gt;in the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and the sluggish pole. Omega within the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic interior&lt;/ins&gt;. Within the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convection zone, we&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;'ve &lt;/ins&gt;two shear layers, i.e., the tachocline &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;round &lt;/ins&gt;the base of the convection zone and the near-surface shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;interaction &lt;/ins&gt;between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the layer. T/g, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the place TT and gg are the temperature and &lt;/ins&gt; [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https&lt;/ins&gt;://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;plamosoku&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;com&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enjyo&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;index&lt;/ins&gt;.php?&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;title&lt;/ins&gt;=&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%E5%88%A9%E7%94%A8%E8%80%85:LeticiaG25 Wood Ranger Power Shears&lt;/ins&gt;] the gravitational acceleration, respectively. 60 and a pair of Mm, respectively. Thus, the time scales of the convection vary from a month to several hours in these &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regions&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Because of this&lt;/ins&gt;, the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the NSSL is just not &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considerably &lt;/ins&gt;affected by the rotation. ′ denote the longitudinal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average &lt;/ins&gt;and the deviation from the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;common&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As well as&lt;/ins&gt;, Miesch &amp;amp; Hindman (2011) suggest that we need a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;power &lt;/ins&gt;to stability with the latitudinal Coriolis drive to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/ins&gt;the NSSL. It's &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;troublesome &lt;/ins&gt;for numerical simulations to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cowl &lt;/ins&gt;a broad &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;range &lt;/ins&gt;of spatial and time scales. The numerical &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;strategy &lt;/ins&gt;for the NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/ins&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/ins&gt;the superadiabaticity around the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highest &lt;/ins&gt;boundary of their calculation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;box &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;talk about &lt;/ins&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;especially &lt;/ins&gt;at low and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive &lt;/ins&gt;latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow&lt;/ins&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/ins&gt;an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;also &lt;/ins&gt;fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;construction &lt;/ins&gt;mechanism of the meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow must &lt;/ins&gt;be understood to reproduce the proper NSSL. Of their &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/ins&gt;rotationally constrained convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;known &lt;/ins&gt;as the Busse column, is required to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/ins&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decreased &lt;/ins&gt;the photo voltaic luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) increased the rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge &lt;/ins&gt;so as to enhance the rotational &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;affect &lt;/ins&gt;on the thermal convection. We word that the lower in luminosity and the rise in rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fee &lt;/ins&gt;have the identical &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;effect &lt;/ins&gt;on the Rossby &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number&lt;/ins&gt;. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even within the close to-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface excessive &lt;/ins&gt;Rossby &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number &lt;/ins&gt;layer. The environment friendly &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;generation &lt;/ins&gt;of the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/ins&gt;-floor circulation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;by way of &lt;/ins&gt;the gyroscopic pumping effectively suppresses the development of the NSSL. When the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;earlier &lt;/ins&gt;calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;did not &lt;/ins&gt;have any approach to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like DR &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without utilizing &lt;/ins&gt;the lowered luminosity, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bigger &lt;/ins&gt;rotation charges or enhanced diffusivities (&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convective conundrum). That is, the typical &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;recently &lt;/ins&gt;provide a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attainable answer &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assemble &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/ins&gt;-like differential rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without &lt;/ins&gt;using &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;special &lt;/ins&gt;therapy proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>152.232.160.64</name></author>
	</entry>
	<entry>
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		<title>2025年11月25日 (火) 08:49に192.111.135.18による</title>
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;2025年11月25日 (火) 08:49時点における版&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;1行目:&lt;/td&gt;
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We perform an unprecedented &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decision &lt;/del&gt;simulation for the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convection zone. Our calculation reproduces the fast equator and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/del&gt;-surface shear layer (NSSL) of differential rotation and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [http://stephankrieger.net/index.php?title=Benutzer:MinnaRedrick Wood Ranger Power Shears] &lt;/del&gt;the near-floor poleward meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow &lt;/del&gt;simultaneously. The NSSL is positioned in a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fancy &lt;/del&gt;layer where the spatial and time scales of thermal convection are considerably small &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;compared &lt;/del&gt;with the deep convection zone. While there have been &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a number of attempts &lt;/del&gt;to reproduce the NSSL in numerical simulation, the results are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;nonetheless &lt;/del&gt;removed from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actuality&lt;/del&gt;. On this &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/del&gt;, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [http://8.137.127.117:3000/angellau586563/wood-ranger-power-shears-reviews2001/wiki/Pruning+%2526+Trimming+Tools+For+Trees%252C+Hedges+%2526+Gardens Wood Ranger brand shears] &lt;/del&gt;magnetic tension are latitudinally balanced with the Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force in &lt;/del&gt;the NSSL. We emphasize the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;importance &lt;/del&gt;of the magnetic &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;area within &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://fromkorea.peoplead.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=12533 Wood Ranger Power Shears reviews] &lt;/del&gt;the sluggish pole. Omega &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the solar inside. Within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convection zone, we have now two shear layers, i.e., the tachocline around the base of the convection zone and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/del&gt;shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interplay between the convection and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [http://wiki.abh.pt/index.php?title=National_Geographic_Magazine_Volume_31_Number_6_The_Conversion_Of_Old_Newspapers_And_Candle_Ends_Into_Fuel Wood Ranger Power Shears sale] &lt;/del&gt;radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;brief &lt;/del&gt;time scales of the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and a pair of Mm, respectively. Thus, the time scales of the convection vary from a month to several hours in these &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regions&lt;/del&gt;. As a result, the convection in the NSSL just &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;isn't considerably &lt;/del&gt;affected by the rotation. ′ denote the longitudinal common and the deviation from the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;typical&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As well as&lt;/del&gt;, Miesch &amp;amp; Hindman (2011) suggest that we&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;'d like &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[https://62.113.42.100/rayfordhunting Wood Ranger Power Shears] &lt;/del&gt;to stability with the latitudinal Coriolis drive to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/del&gt;the NSSL. It's &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;tough &lt;/del&gt;for numerical simulations to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cowl &lt;/del&gt;a broad &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;range &lt;/del&gt;of spatial and time scales. The numerical approach for the NSSL is highly restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/del&gt;the superadiabaticity &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;round &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highest &lt;/del&gt;boundary of their calculation field and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;discuss &lt;/del&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, particularly at low and high latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow&lt;/del&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) carry out an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;also &lt;/del&gt;fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;building &lt;/del&gt;mechanism of the meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulation should &lt;/del&gt;be understood to reproduce the proper NSSL. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/del&gt;their &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;examine&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/del&gt;rotationally constrained convection referred to as the Busse column, is required to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reduced &lt;/del&gt;the photo voltaic luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;elevated &lt;/del&gt;the rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fee in order &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reinforce &lt;/del&gt;the rotational influence on the thermal convection. We &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;be aware &lt;/del&gt;that the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decrease &lt;/del&gt;in luminosity and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;increase &lt;/del&gt;in rotation charge have the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;same &lt;/del&gt;impact on the Rossby quantity. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/del&gt;-floor &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive &lt;/del&gt;Rossby &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number &lt;/del&gt;layer. The &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;efficient era &lt;/del&gt;of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/del&gt;-floor circulation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through &lt;/del&gt;the gyroscopic pumping effectively suppresses the development of the NSSL. When the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;earlier &lt;/del&gt;calculation (Hotta et al., &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:Lea618508996 Wood Ranger Power Shears] &lt;/del&gt;2015; Matilsky et al., &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://prirechensk.ru/2018/06/22/%d0%bf%d0%be%d1%81%d1%82%d0%b0%d0%bd%d0%be%d0%b2%d0%bb%d0%b5%d0%bd%d0%b8%d0%b5-%e2%84%96-90-%d0%be%d1%82-02-10-2013/ buy Wood Ranger Power Shears] &lt;/del&gt;2019) was carried out, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;did not &lt;/del&gt;have any &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;means &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/del&gt;-like DR &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without &lt;/del&gt;using the lowered luminosity, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bigger &lt;/del&gt;rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rates &lt;/del&gt;or enhanced diffusivities (photo voltaic convective conundrum). That&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;'s&lt;/del&gt;, the typical &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;just lately present &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attainable solution &lt;/del&gt;to construct the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like differential rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without &lt;/del&gt;using &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;special treatment &lt;/del&gt;proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We perform an unprecedented &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution &lt;/ins&gt;simulation for &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:WilliemaePittman portable cutting shears] &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convection zone. Our calculation reproduces the fast equator and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/ins&gt;-surface shear layer (NSSL) of differential rotation and the near-floor poleward meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;move &lt;/ins&gt;simultaneously. The NSSL is positioned in a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;complex &lt;/ins&gt;layer where the spatial and time scales of thermal convection are considerably small &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in contrast &lt;/ins&gt;with the deep convection zone. While there have been &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;several makes an attempt &lt;/ins&gt;to reproduce the NSSL in numerical simulation, the results are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;still &lt;/ins&gt;removed from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reality&lt;/ins&gt;. On this &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/ins&gt;, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drive within &lt;/ins&gt;the NSSL. We emphasize the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significance &lt;/ins&gt;of the magnetic &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field in &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and the sluggish pole. Omega &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the solar inside. Within the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convection zone, we have now two shear layers, i.e., the tachocline around the base of the convection zone and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/ins&gt;shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interplay between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/ins&gt;time scales of the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the layer. T/g, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [http://service.megaworks.ai/board/bbs/board.php?bo_table=hwang_form&amp;amp;wr_id=3311145 portable cutting shears] &lt;/ins&gt;the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and a pair of Mm, respectively. Thus, the time scales of the convection vary from a month to several hours in these &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;areas&lt;/ins&gt;. As a result, the convection in the NSSL &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/ins&gt;just &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;not significantly &lt;/ins&gt;affected by the rotation. ′ denote the longitudinal common and the deviation from the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In addition&lt;/ins&gt;, Miesch &amp;amp; Hindman (2011) suggest that we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;need &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pressure &lt;/ins&gt;to stability with the latitudinal Coriolis drive to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/ins&gt;the NSSL. It's &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;difficult &lt;/ins&gt;for numerical simulations to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cover &lt;/ins&gt;a broad &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;vary &lt;/ins&gt;of spatial and time scales. The numerical approach for the NSSL is highly restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;improve &lt;/ins&gt;the superadiabaticity &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;around &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;top &lt;/ins&gt;boundary of their calculation field and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;focus on &lt;/ins&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, particularly at low and high latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulate&lt;/ins&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) carry out an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;additionally &lt;/ins&gt;fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;development &lt;/ins&gt;mechanism of the meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement have to &lt;/ins&gt;be understood to reproduce the proper NSSL. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Of &lt;/ins&gt;their &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highly &lt;/ins&gt;rotationally constrained convection referred to as the Busse column, is required to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;diminished &lt;/ins&gt;the photo voltaic luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;increased &lt;/ins&gt;the rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;price so as &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/ins&gt;the rotational influence on the thermal convection. We &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;word &lt;/ins&gt;that the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lower &lt;/ins&gt;in luminosity and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rise &lt;/ins&gt;in rotation charge have the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identical &lt;/ins&gt;impact on the Rossby quantity. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/ins&gt;-floor &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high &lt;/ins&gt;Rossby &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantity &lt;/ins&gt;layer. The &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environment friendly technology &lt;/ins&gt;of the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/ins&gt;-floor circulation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;via &lt;/ins&gt;the gyroscopic pumping effectively suppresses the development of the NSSL. When the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;previous &lt;/ins&gt;calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;didn't &lt;/ins&gt;have any &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;approach &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/ins&gt;-like DR &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out &lt;/ins&gt;using the lowered luminosity, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;larger &lt;/ins&gt;rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charges &lt;/ins&gt;or enhanced diffusivities (photo voltaic convective conundrum). That &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is&lt;/ins&gt;, the typical &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;not too long ago provide &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;possible resolution &lt;/ins&gt;to construct the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like differential rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out &lt;/ins&gt;using &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;particular therapy &lt;/ins&gt;proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>192.111.135.18</name></author>
	</entry>
	<entry>
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		<title>2025年11月8日 (土) 23:24にLea618508996による</title>
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/del&gt;an unprecedented high-decision simulation for the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convection zone. Our calculation reproduces the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/del&gt;equator  [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https&lt;/del&gt;://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;www&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;caselvaticanuoto&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;it/2022/01/05/special-post-christmas-gym/ &lt;/del&gt;Wood Ranger &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;brand shears&lt;/del&gt;] &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and &lt;/del&gt;near-floor &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;shear layer (NSSL) of differential rotation and the close to-surface &lt;/del&gt;poleward meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulate concurrently&lt;/del&gt;. The NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;situated &lt;/del&gt;in a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;posh &lt;/del&gt;layer &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the place &lt;/del&gt;the spatial and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; garden [https://oerdigamers.info/index.php/Pruning_Trimming_Tools_For_Trees_Hedges_Gardens power shears] &lt;/del&gt;time scales of thermal convection are considerably small compared with the deep convection zone. While there have been a number of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;makes an attempt &lt;/del&gt;to reproduce the NSSL in numerical simulation, the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;outcomes &lt;/del&gt;are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;still &lt;/del&gt;removed from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reality&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/del&gt;this research, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drive &lt;/del&gt;in the NSSL. We emphasize the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significance &lt;/del&gt;of the magnetic &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;subject &lt;/del&gt;within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/del&gt;equator and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;gradual &lt;/del&gt;pole. Omega &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic interior&lt;/del&gt;. Within the photo voltaic convection zone, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;now &lt;/del&gt;we have two shear layers, i.e., the tachocline around the base of the convection zone and the close to-floor shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;interaction &lt;/del&gt;between the convection and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;radiation zones (Spiegel &amp;amp; Zahn, &lt;/del&gt; [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https&lt;/del&gt;://wiki.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;novaverseonline&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;com&lt;/del&gt;/index.php&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;/User:TawannaBuckner2 buy &lt;/del&gt;Wood Ranger Power Shears] 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/del&gt;time scales of the convection in the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:AngelicaHarkness Wood Ranger Power Shears] &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;couple &lt;/del&gt;of Mm, respectively. Thus, the time scales of the convection vary from a month to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a number of &lt;/del&gt;hours in these regions. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Consequently&lt;/del&gt;, the convection in the NSSL just isn't considerably affected by the rotation. ′ denote the longitudinal common and the deviation from the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average&lt;/del&gt;. As well as, Miesch &amp;amp; Hindman (2011) suggest that we'd like a [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http&lt;/del&gt;://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;123&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;57&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;51&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;87:40003/alisonhinchcli/alison2009&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;wiki/Nibbler+%2526+Shears+Parts &lt;/del&gt;Wood Ranger Power Shears] to stability with the latitudinal Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;keep up &lt;/del&gt;the NSSL. It's tough &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[http://ww.enhasusg.co.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=1904657 Wood Ranger Power Shears &lt;/del&gt;for &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sale] &lt;/del&gt;numerical simulations to cowl a broad range of spatial and time scales. The numerical &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;strategy &lt;/del&gt;for the NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;very &lt;/del&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) enhance the superadiabaticity round the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;top &lt;/del&gt;boundary of their calculation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;box &lt;/del&gt;and discuss the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, particularly at low and high latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;move&lt;/del&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/del&gt;an &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;analogous &lt;/del&gt;calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;additionally &lt;/del&gt;fail to reproduce the NSSL &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the mid-latitude. They conclude that the detailed building mechanism of the meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement &lt;/del&gt;should be understood to reproduce the proper NSSL. In their &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/del&gt;, extremely rotationally constrained convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;known &lt;/del&gt;as the Busse column, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://fakenews.win/wiki/User:BurtonMcGowan31 Wood Ranger Power Shears official site] &lt;/del&gt;is required to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/del&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lowered &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) elevated the rotation fee in order to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/del&gt;the rotational &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;affect &lt;/del&gt;on the thermal convection. We be aware that the decrease in luminosity and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rise &lt;/del&gt;in rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;price &lt;/del&gt;have the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identical effect &lt;/del&gt;on the Rossby quantity. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the near-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/del&gt;excessive Rossby &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantity &lt;/del&gt;layer. The &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environment friendly technology &lt;/del&gt;of the close to-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/del&gt;circulation through the gyroscopic pumping effectively suppresses the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;construction &lt;/del&gt;of the NSSL. When the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;previous &lt;/del&gt;calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;didn't &lt;/del&gt;have any means to take care of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like DR without &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;utilizing &lt;/del&gt;the lowered luminosity, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;larger &lt;/del&gt;rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charges &lt;/del&gt;or enhanced diffusivities (&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convective conundrum). That's, the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;everyday &lt;/del&gt;&amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;recently provide &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;doable answer &lt;/del&gt;to construct the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/del&gt;-like differential rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out &lt;/del&gt;using &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;particular &lt;/del&gt;treatment &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;shown &lt;/del&gt;above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/ins&gt;an unprecedented high-decision simulation for the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convection zone. Our calculation reproduces the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/ins&gt;equator &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and close to-surface shear layer (NSSL) of differential rotation and &lt;/ins&gt; [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http&lt;/ins&gt;://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;stephankrieger&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;net/index&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;php?title=Benutzer:MinnaRedrick &lt;/ins&gt;Wood Ranger &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Power Shears&lt;/ins&gt;] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the &lt;/ins&gt;near-floor poleward meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow simultaneously&lt;/ins&gt;. The NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;positioned &lt;/ins&gt;in a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fancy &lt;/ins&gt;layer &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;where &lt;/ins&gt;the spatial and time scales of thermal convection are considerably small compared with the deep convection zone. While there have been a number of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attempts &lt;/ins&gt;to reproduce the NSSL in numerical simulation, the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;results &lt;/ins&gt;are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;nonetheless &lt;/ins&gt;removed from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actuality&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;On &lt;/ins&gt;this research, we succeed in reproducing an NSSL in our new calculation. 4) the turbulent viscosity and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [http://8.137.127.117:3000/angellau586563/wood-ranger-power-shears-reviews2001/wiki/Pruning+%2526+Trimming+Tools+For+Trees%252C+Hedges+%2526+Gardens Wood Ranger brand shears] &lt;/ins&gt;magnetic tension are latitudinally balanced with the Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force &lt;/ins&gt;in the NSSL. We emphasize the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;importance &lt;/ins&gt;of the magnetic &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;area &lt;/ins&gt;within the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/ins&gt;equator and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://fromkorea.peoplead.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=12533 Wood Ranger Power Shears reviews] &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sluggish &lt;/ins&gt;pole. Omega &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar inside&lt;/ins&gt;. Within the photo voltaic convection zone, we have &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;now &lt;/ins&gt;two shear layers, i.e., the tachocline around the base of the convection zone and the close to-floor shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;interplay &lt;/ins&gt;between the convection and  [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http&lt;/ins&gt;://wiki.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;abh&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pt&lt;/ins&gt;/index.php&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;?title=National_Geographic_Magazine_Volume_31_Number_6_The_Conversion_Of_Old_Newspapers_And_Candle_Ends_Into_Fuel &lt;/ins&gt;Wood Ranger Power Shears &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sale&lt;/ins&gt;] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;radiation zones (Spiegel &amp;amp; Zahn, &lt;/ins&gt;1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;brief &lt;/ins&gt;time scales of the convection in the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;pair &lt;/ins&gt;of Mm, respectively. Thus, the time scales of the convection vary from a month to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;several &lt;/ins&gt;hours in these regions. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As a result&lt;/ins&gt;, the convection in the NSSL just isn't considerably affected by the rotation. ′ denote the longitudinal common and the deviation from the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;typical&lt;/ins&gt;. As well as, Miesch &amp;amp; Hindman (2011) suggest that we'd like a [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https&lt;/ins&gt;://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;62&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;113&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;42&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;100&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rayfordhunting &lt;/ins&gt;Wood Ranger Power Shears] to stability with the latitudinal Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drive &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/ins&gt;the NSSL. It's tough for numerical simulations to cowl a broad range of spatial and time scales. The numerical &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;approach &lt;/ins&gt;for the NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highly &lt;/ins&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) enhance the superadiabaticity round the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highest &lt;/ins&gt;boundary of their calculation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field &lt;/ins&gt;and discuss the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, particularly at low and high latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow&lt;/ins&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/ins&gt;an &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identical &lt;/ins&gt;calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;also &lt;/ins&gt;fail to reproduce the NSSL &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the mid-latitude. They conclude that the detailed building mechanism of the meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulation &lt;/ins&gt;should be understood to reproduce the proper NSSL. In their &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;examine&lt;/ins&gt;, extremely rotationally constrained convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;referred to &lt;/ins&gt;as the Busse column, is required to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/ins&gt;-like fast equator differential rotation. Hotta et al. (2015) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reduced &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) elevated the rotation fee in order to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reinforce &lt;/ins&gt;the rotational &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;influence &lt;/ins&gt;on the thermal convection. We be aware that the decrease in luminosity and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;increase &lt;/ins&gt;in rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge &lt;/ins&gt;have the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;same impact &lt;/ins&gt;on the Rossby quantity. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists within the deep layer, upflows are rotationally constrained even &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the near-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/ins&gt;excessive Rossby &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number &lt;/ins&gt;layer. The &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;efficient era &lt;/ins&gt;of the close to-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/ins&gt;circulation through the gyroscopic pumping effectively suppresses the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;development &lt;/ins&gt;of the NSSL. When the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;earlier &lt;/ins&gt;calculation (Hotta et al., &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:Lea618508996 Wood Ranger Power Shears] &lt;/ins&gt;2015; Matilsky et al., &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://prirechensk.ru/2018/06/22/%d0%bf%d0%be%d1%81%d1%82%d0%b0%d0%bd%d0%be%d0%b2%d0%bb%d0%b5%d0%bd%d0%b8%d0%b5-%e2%84%96-90-%d0%be%d1%82-02-10-2013/ buy Wood Ranger Power Shears] &lt;/ins&gt;2019) was carried out, we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;did not &lt;/ins&gt;have any means to take care of the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like DR without &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;using &lt;/ins&gt;the lowered luminosity, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bigger &lt;/ins&gt;rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rates &lt;/ins&gt;or enhanced diffusivities (&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convective conundrum). That's, the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;typical &lt;/ins&gt;&amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;just lately present &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attainable solution &lt;/ins&gt;to construct the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/ins&gt;-like differential rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without &lt;/ins&gt;using &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;special &lt;/ins&gt;treatment &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;proven &lt;/ins&gt;above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Lea618508996</name></author>
	</entry>
	<entry>
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		<title>2025年11月7日 (金) 22:53にAngelicaHarknessによる</title>
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;2025年11月7日 (金) 22:53時点における版&lt;/td&gt;
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We carry out an unprecedented &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution &lt;/del&gt;simulation for the photo voltaic convection zone. Our calculation reproduces the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/del&gt;equator &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and close to-floor &lt;/del&gt; [https://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;wiki&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;dulovic&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;tech&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;index.php&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;User:PhilipPratt &lt;/del&gt;Wood Ranger &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Power Shears&lt;/del&gt;] shear layer (NSSL) of differential rotation and the close to-surface poleward meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement &lt;/del&gt;concurrently. The NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;located &lt;/del&gt;in a posh layer &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;where &lt;/del&gt;the spatial and time scales of thermal convection are considerably small compared with the deep convection zone. While there have been a number of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attempts &lt;/del&gt;to reproduce the NSSL in numerical simulation, the outcomes are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;nonetheless &lt;/del&gt;removed from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actuality&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;On &lt;/del&gt;this &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;examine&lt;/del&gt;, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reach &lt;/del&gt;reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[http://jicc.kr/bbs/board.php?bo_table=hosung3&amp;amp;wr_id=646519 Wood Ranger Power Shears features] within &lt;/del&gt;the NSSL. We emphasize the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;importance &lt;/del&gt;of the magnetic subject within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the fast equator and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sluggish &lt;/del&gt;pole. Omega &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar inside&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/del&gt;convection zone, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;now &lt;/del&gt;have two shear layers, i.e., the tachocline around the base of the convection zone and the close to-floor shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection in the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2 &lt;/del&gt;Mm, respectively. Thus, the time scales of the convection vary from a month to a number of hours in these regions. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As a result&lt;/del&gt;, the convection in the NSSL just isn't &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly &lt;/del&gt;affected by the rotation. ′ denote the longitudinal common and the deviation from the average. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In addition&lt;/del&gt;, Miesch &amp;amp; Hindman (2011) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;recommend &lt;/del&gt;that we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;need &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;balance &lt;/del&gt;with the latitudinal Coriolis [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;https&lt;/del&gt;://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;santo&lt;/del&gt;.kr&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;:443&lt;/del&gt;/bbs/board.php?bo_table=free&amp;amp;wr_id=&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;254433 &lt;/del&gt;Wood Ranger Power Shears] &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;to take care of the NSSL. It is difficult for &lt;/del&gt;numerical simulations to cowl a broad range of spatial and time scales. The numerical strategy for the NSSL is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/del&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;improve &lt;/del&gt;the superadiabaticity &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;around &lt;/del&gt;the top boundary of their calculation box and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;talk about &lt;/del&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;function&lt;/del&gt;, particularly at low and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive &lt;/del&gt;latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulation&lt;/del&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) perform an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;function &lt;/del&gt;at &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high &lt;/del&gt;and low latitudes. The authors additionally fail to reproduce the NSSL within the mid-latitude. They conclude that the detailed &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;development &lt;/del&gt;mechanism of the meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;stream must &lt;/del&gt;be understood to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;correct &lt;/del&gt;NSSL. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Of &lt;/del&gt;their &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;highly &lt;/del&gt;rotationally constrained convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;called &lt;/del&gt;the Busse column, is required to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/del&gt;equator differential rotation. Hotta et al. (2015) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;diminished &lt;/del&gt;the solar luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) elevated the rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge so as &lt;/del&gt;to enhance the rotational &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;influence &lt;/del&gt;on the thermal convection. We be aware that the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lower &lt;/del&gt;in luminosity and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;increase &lt;/del&gt;in rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge &lt;/del&gt;have the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;same &lt;/del&gt;effect on the Rossby &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;number&lt;/del&gt;. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the deep layer, upflows are rotationally constrained even within the near-surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high &lt;/del&gt;Rossby quantity layer. The &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;efficient &lt;/del&gt;technology of the close to-surface circulation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;by way of &lt;/del&gt;the gyroscopic pumping effectively suppresses the construction of the NSSL. When the previous calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we didn't have any &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;manner &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/del&gt;the photo voltaic-like DR &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out using &lt;/del&gt;the lowered luminosity, larger rotation charges or enhanced diffusivities (solar convective conundrum). That's, the everyday &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) recently &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;present &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;possible solution &lt;/del&gt;to construct the solar-like differential rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without utilizing &lt;/del&gt;particular &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;therapy proven &lt;/del&gt;above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We carry out an unprecedented &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decision &lt;/ins&gt;simulation for the photo voltaic convection zone. Our calculation reproduces the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/ins&gt;equator  [https://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;www&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;caselvaticanuoto&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;it/2022/01/05&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;special-post-christmas-gym&lt;/ins&gt;/ Wood Ranger &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;brand shears&lt;/ins&gt;] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and near-floor &lt;/ins&gt;shear layer (NSSL) of differential rotation and the close to-surface poleward meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulate &lt;/ins&gt;concurrently. The NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;situated &lt;/ins&gt;in a posh layer &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the place &lt;/ins&gt;the spatial and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; garden [https://oerdigamers.info/index.php/Pruning_Trimming_Tools_For_Trees_Hedges_Gardens power shears] &lt;/ins&gt;time scales of thermal convection are considerably small compared with the deep convection zone. While there have been a number of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;makes an attempt &lt;/ins&gt;to reproduce the NSSL in numerical simulation, the outcomes are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;still &lt;/ins&gt;removed from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reality&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/ins&gt;this &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/ins&gt;, we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;succeed in &lt;/ins&gt;reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;drive in &lt;/ins&gt;the NSSL. We emphasize the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significance &lt;/ins&gt;of the magnetic subject within the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the fast equator and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;gradual &lt;/ins&gt;pole. Omega &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic interior&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Within &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/ins&gt;convection zone, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;now &lt;/ins&gt;we have two shear layers, i.e., the tachocline around the base of the convection zone and the close to-floor shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel &amp;amp; Zahn, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://wiki.novaverseonline.com/index.php/User:TawannaBuckner2 buy Wood Ranger Power Shears] &lt;/ins&gt;1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection in the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:AngelicaHarkness Wood Ranger Power Shears] a couple of &lt;/ins&gt;Mm, respectively. Thus, the time scales of the convection vary from a month to a number of hours in these regions. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Consequently&lt;/ins&gt;, the convection in the NSSL just isn't &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considerably &lt;/ins&gt;affected by the rotation. ′ denote the longitudinal common and the deviation from the average. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As well as&lt;/ins&gt;, Miesch &amp;amp; Hindman (2011) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;suggest &lt;/ins&gt;that we&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;'d like &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[http://123.57.51.87:40003/alisonhinchcli/alison2009/wiki/Nibbler+%2526+Shears+Parts Wood Ranger Power Shears] &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;stability &lt;/ins&gt;with the latitudinal Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force to keep up the NSSL. It's tough &lt;/ins&gt;[&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http&lt;/ins&gt;://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ww.enhasusg.co&lt;/ins&gt;.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;1904657 &lt;/ins&gt;Wood Ranger Power Shears &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;for sale&lt;/ins&gt;] numerical simulations to cowl a broad range of spatial and time scales. The numerical strategy for the NSSL is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;very &lt;/ins&gt;restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/ins&gt;the superadiabaticity &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;round &lt;/ins&gt;the top boundary of their calculation box and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;discuss &lt;/ins&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;feature&lt;/ins&gt;, particularly at low and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high &lt;/ins&gt;latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;move&lt;/ins&gt;. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) perform an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;characteristic &lt;/ins&gt;at &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive &lt;/ins&gt;and low latitudes. The authors additionally fail to reproduce the NSSL within the mid-latitude. They conclude that the detailed &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;building &lt;/ins&gt;mechanism of the meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement should &lt;/ins&gt;be understood to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;proper &lt;/ins&gt;NSSL. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/ins&gt;their &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;study&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extremely &lt;/ins&gt;rotationally constrained convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;known as &lt;/ins&gt;the Busse column, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://fakenews.win/wiki/User:BurtonMcGowan31 Wood Ranger Power Shears official site] &lt;/ins&gt;is required to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/ins&gt;equator differential rotation. Hotta et al. (2015) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lowered &lt;/ins&gt;the solar luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) elevated the rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fee in order &lt;/ins&gt;to enhance the rotational &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;affect &lt;/ins&gt;on the thermal convection. We be aware that the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decrease &lt;/ins&gt;in luminosity and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;rise &lt;/ins&gt;in rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;price &lt;/ins&gt;have the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identical &lt;/ins&gt;effect on the Rossby &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantity&lt;/ins&gt;. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the deep layer, upflows are rotationally constrained even within the near-surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive &lt;/ins&gt;Rossby quantity layer. The &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environment friendly &lt;/ins&gt;technology of the close to-surface circulation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through &lt;/ins&gt;the gyroscopic pumping effectively suppresses the construction of the NSSL. When the previous calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we didn't have any &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;means &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/ins&gt;the photo voltaic-like DR &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without utilizing &lt;/ins&gt;the lowered luminosity, larger rotation charges or enhanced diffusivities (solar convective conundrum). That's, the everyday &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) recently &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provide &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;doable answer &lt;/ins&gt;to construct the solar-like differential rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out using &lt;/ins&gt;particular &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;treatment shown &lt;/ins&gt;above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>AngelicaHarkness</name></author>
	</entry>
	<entry>
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				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;1行目:&lt;/td&gt;
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&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/del&gt;an unprecedented &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high&lt;/del&gt;-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface shear layer (NSSL) of differential rotation and &lt;/del&gt; [https://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;kcosep&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;com&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2025/bbs/board&lt;/del&gt;.php&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;?bo_table=free&amp;amp;wr_id=2975788&amp;amp;wv_checked_wr_id= &lt;/del&gt;Wood Ranger Power Shears &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;official site&lt;/del&gt;] the close to-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/del&gt;poleward meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;circulate simultaneously&lt;/del&gt;. The NSSL is located in a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;complex &lt;/del&gt;layer where the spatial and time scales of thermal convection are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly &lt;/del&gt;small &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in contrast &lt;/del&gt;with the deep convection zone. While there have been a number of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;makes an attempt &lt;/del&gt;to reproduce the NSSL in numerical simulation, the outcomes are &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;still &lt;/del&gt;removed from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reality&lt;/del&gt;. On this examine, we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;achieve &lt;/del&gt;reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force &lt;/del&gt;within the NSSL. We emphasize the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significance &lt;/del&gt;of the magnetic &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field &lt;/del&gt;within the photo voltaic convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the fast equator and the sluggish pole. Omega &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the solar inside. In the solar convection zone, we now have two shear layers, i.e., the tachocline around the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;bottom &lt;/del&gt;of the convection zone and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/del&gt;shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a couple of &lt;/del&gt;Mm, respectively. Thus, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://wikirefuge.lpo.fr/index.php?title=Tidying_Up_Big_Time Wood Ranger official] &lt;/del&gt;the time scales of the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;range &lt;/del&gt;from a month to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;several &lt;/del&gt;hours in these &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;areas&lt;/del&gt;. As a result, the convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/del&gt;the NSSL isn't &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considerably &lt;/del&gt;affected by the rotation. ′ denote the longitudinal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average &lt;/del&gt;and the deviation from the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;common&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;As well as&lt;/del&gt;, Miesch &amp;amp; Hindman (2011) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;counsel &lt;/del&gt;that we &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;want &lt;/del&gt;a [https://&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;omnideck&lt;/del&gt;.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;org&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;index&lt;/del&gt;.php&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;/Lawn_Garden_Hand_Tools &lt;/del&gt;Wood Ranger Power Shears &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;official site&lt;/del&gt;] to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;balance with the latitudinal Coriolis pressure to maintain &lt;/del&gt;the NSSL. It&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;'s troublesome &lt;/del&gt;for numerical simulations to cowl a broad &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;vary &lt;/del&gt;of spatial and time scales. The numerical &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;approach &lt;/del&gt;for the NSSL is extremely restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) improve the superadiabaticity &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;round &lt;/del&gt;the top boundary of their calculation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;field &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;focus on &lt;/del&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;feature&lt;/del&gt;, particularly at low and excessive latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional circulation. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/del&gt;an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;characteristic &lt;/del&gt;at high and low latitudes. The authors additionally fail to reproduce the NSSL &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the mid-latitude. They conclude that the detailed &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;construction &lt;/del&gt;mechanism of the meridional &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;flow should &lt;/del&gt;be understood to reproduce the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;proper &lt;/del&gt;NSSL. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In &lt;/del&gt;their &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;examine&lt;/del&gt;, highly rotationally constrained convection &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;referred to as &lt;/del&gt;the Busse column, is required to reproduce the photo voltaic-like &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fast &lt;/del&gt;equator differential rotation. Hotta et al. (2015) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reduced &lt;/del&gt;the solar luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;increased &lt;/del&gt;the rotation charge &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in order &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;boost &lt;/del&gt;the rotational influence on the thermal convection. We &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;notice &lt;/del&gt;that the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;decrease &lt;/del&gt;in luminosity and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:RomaineAldrich5 Wood Ranger Power Shears official site] &lt;/del&gt;the increase in rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fee &lt;/del&gt;have the same effect on the Rossby number. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists in the deep layer, upflows are rotationally constrained even &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/del&gt;the near-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor  [https://hitommy.net/xe1/my_thoughts/1941534 Wood Ranger official] &lt;/del&gt;high Rossby quantity layer. The efficient technology of the close to-surface circulation by way of the gyroscopic pumping &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;successfully &lt;/del&gt;suppresses the construction of the NSSL. When the previous calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we didn't have any manner to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;keep up &lt;/del&gt;the photo voltaic-like DR with out &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;utilizing &lt;/del&gt;the lowered luminosity, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt; electric [https://rijocampers.is/what-do-you-need-to-know-before-traveling-to-iceland/ cordless power shears] [http://classicalmusicmp3freedownload.com/ja/index.php?title=Buttery_Pie_Dough Wood Ranger Power Shears for sale] &lt;/del&gt;larger rotation charges or enhanced diffusivities (&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic &lt;/del&gt;convective conundrum). That's, the everyday &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;just lately &lt;/del&gt;present a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attainable resolution &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assemble &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;photo voltaic&lt;/del&gt;-like differential rotation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with out using &lt;/del&gt;particular &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;treatment &lt;/del&gt;proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;We &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;carry out &lt;/ins&gt;an unprecedented &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excessive&lt;/ins&gt;-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/ins&gt; [https://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;wiki&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;dulovic.tech&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;index&lt;/ins&gt;.php&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;/User:PhilipPratt &lt;/ins&gt;Wood Ranger Power Shears] &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;shear layer (NSSL) of differential rotation and &lt;/ins&gt;the close to-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/ins&gt;poleward meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;movement concurrently&lt;/ins&gt;. The NSSL is located in a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;posh &lt;/ins&gt;layer where the spatial and time scales of thermal convection are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considerably &lt;/ins&gt;small &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;compared &lt;/ins&gt;with the deep convection zone. While there have been a number of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;attempts &lt;/ins&gt;to reproduce the NSSL in numerical simulation, the outcomes are &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;nonetheless &lt;/ins&gt;removed from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actuality&lt;/ins&gt;. On this examine, we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reach &lt;/ins&gt;reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[http://jicc.kr/bbs/board.php?bo_table=hosung3&amp;amp;wr_id=646519 Wood Ranger Power Shears features] &lt;/ins&gt;within the NSSL. We emphasize the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;importance &lt;/ins&gt;of the magnetic &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;subject &lt;/ins&gt;within the photo voltaic convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the fast equator and the sluggish pole. Omega &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the solar inside. In the solar convection zone, we now have two shear layers, i.e., the tachocline around the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;base &lt;/ins&gt;of the convection zone and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;close to&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;floor &lt;/ins&gt;shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2 &lt;/ins&gt;Mm, respectively. Thus, the time scales of the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;vary &lt;/ins&gt;from a month to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a number of &lt;/ins&gt;hours in these &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regions&lt;/ins&gt;. As a result, the convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in &lt;/ins&gt;the NSSL &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;just &lt;/ins&gt;isn't &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;significantly &lt;/ins&gt;affected by the rotation. ′ denote the longitudinal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;common &lt;/ins&gt;and the deviation from the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;In addition&lt;/ins&gt;, Miesch &amp;amp; Hindman (2011) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;recommend &lt;/ins&gt;that we &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;need &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;force to balance with the latitudinal Coriolis &lt;/ins&gt;[https://&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;santo&lt;/ins&gt;.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;kr:443/bbs&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;board&lt;/ins&gt;.php&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;?bo_table=free&amp;amp;wr_id=254433 &lt;/ins&gt;Wood Ranger Power Shears] to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;take care of &lt;/ins&gt;the NSSL. It &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is difficult &lt;/ins&gt;for numerical simulations to cowl a broad &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;range &lt;/ins&gt;of spatial and time scales. The numerical &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;strategy &lt;/ins&gt;for the NSSL is extremely restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) improve the superadiabaticity &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;around &lt;/ins&gt;the top boundary of their calculation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;box &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;talk about &lt;/ins&gt;the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;function&lt;/ins&gt;, particularly at low and excessive latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional circulation. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;perform &lt;/ins&gt;an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;function &lt;/ins&gt;at high and low latitudes. The authors additionally fail to reproduce the NSSL &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the mid-latitude. They conclude that the detailed &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;development &lt;/ins&gt;mechanism of the meridional &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;stream must &lt;/ins&gt;be understood to reproduce the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;correct &lt;/ins&gt;NSSL. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Of &lt;/ins&gt;their &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/ins&gt;, highly rotationally constrained convection &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;called &lt;/ins&gt;the Busse column, is required to reproduce the photo voltaic-like &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quick &lt;/ins&gt;equator differential rotation. Hotta et al. (2015) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;diminished &lt;/ins&gt;the solar luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;elevated &lt;/ins&gt;the rotation charge &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;so as &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance &lt;/ins&gt;the rotational influence on the thermal convection. We &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;be aware &lt;/ins&gt;that the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;lower &lt;/ins&gt;in luminosity and the increase in rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;charge &lt;/ins&gt;have the same effect on the Rossby number. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists in the deep layer, upflows are rotationally constrained even &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the near-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface &lt;/ins&gt;high Rossby quantity layer. The efficient technology of the close to-surface circulation by way of the gyroscopic pumping &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;effectively &lt;/ins&gt;suppresses the construction of the NSSL. When the previous calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we didn't have any manner to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintain &lt;/ins&gt;the photo voltaic-like DR with out &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;using &lt;/ins&gt;the lowered luminosity, larger rotation charges or enhanced diffusivities (&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar &lt;/ins&gt;convective conundrum). That's, the everyday &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;recently &lt;/ins&gt;present a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;possible solution &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;construct &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar&lt;/ins&gt;-like differential rotation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;without utilizing &lt;/ins&gt;particular &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;therapy &lt;/ins&gt;proven above.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>FranklinEspino</name></author>
	</entry>
	<entry>
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		<title>192.126.234.26: ページの作成:「&lt;br&gt;We perform an unprecedented high-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and near-surface shear layer…」</title>
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		<updated>2025-09-11T09:33:02Z</updated>

		<summary type="html">&lt;p&gt;ページの作成:「&amp;lt;br&amp;gt;We perform an unprecedented high-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and near-surface shear layer…」&lt;/p&gt;
&lt;p&gt;&lt;b&gt;新規ページ&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;br&amp;gt;We perform an unprecedented high-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and near-surface shear layer (NSSL) of differential rotation and  [https://kcosep.com/2025/bbs/board.php?bo_table=free&amp;amp;wr_id=2975788&amp;amp;wv_checked_wr_id= Wood Ranger Power Shears official site] the close to-floor poleward meridional circulate simultaneously. The NSSL is located in a complex layer where the spatial and time scales of thermal convection are significantly small in contrast with the deep convection zone. While there have been a number of makes an attempt to reproduce the NSSL in numerical simulation, the outcomes are still removed from reality. On this examine, we achieve reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis force within the NSSL. We emphasize the significance of the magnetic field within the photo voltaic convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the fast equator and the sluggish pole. Omega within the solar inside. In the solar convection zone, we now have two shear layers, i.e., the tachocline around the bottom of the convection zone and the near-surface shear layer (NSSL).&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel &amp;amp; Zahn, 1992; Gough &amp;amp; McIntyre, 1998; Forgács-Dajka &amp;amp; Petrovay, 2001; Rempel, 2005; Brun et al., 2011; Matilsky et al., 2022). The NSSL is thought to be maintained by the small-spatial and quick time scales of the convection within the layer. T/g, the place TT and gg are the temperature and the gravitational acceleration, respectively. 60 and a couple of Mm, respectively. Thus,  [https://wikirefuge.lpo.fr/index.php?title=Tidying_Up_Big_Time Wood Ranger official] the time scales of the convection range from a month to several hours in these areas. As a result, the convection within the NSSL isn't considerably affected by the rotation. ′ denote the longitudinal average and the deviation from the common. As well as, Miesch &amp;amp; Hindman (2011) counsel that we want a [https://omnideck.org/index.php/Lawn_Garden_Hand_Tools Wood Ranger Power Shears official site] to balance with the latitudinal Coriolis pressure to maintain the NSSL. It's troublesome for numerical simulations to cowl a broad vary of spatial and time scales. The numerical approach for the NSSL is extremely restricted.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Guerrero et al. (2013) improve the superadiabaticity round the top boundary of their calculation field and focus on the formation mechanism of the NSSL following Foukal &amp;amp; Jokipii (1975). Hotta et al. NSSL-like feature, particularly at low and excessive latitudes. We argue there that the NSSL is maintained by the radially inward angular momentum transport and the turbulent viscosity on the sheared meridional circulation. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) carry out an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at high and low latitudes. The authors additionally fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed construction mechanism of the meridional flow should be understood to reproduce the proper NSSL. In their examine, highly rotationally constrained convection referred to as the Busse column, is required to reproduce the photo voltaic-like fast equator differential rotation. Hotta et al. (2015) reduced the solar luminosity and Matilsky et al.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;2019) increased the rotation charge in order to boost the rotational influence on the thermal convection. We notice that the decrease in luminosity and  [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:RomaineAldrich5 Wood Ranger Power Shears official site] the increase in rotation fee have the same effect on the Rossby number. Matilsky et al. (2019) argue that when the rotationally constrained Busse column exists in the deep layer, upflows are rotationally constrained even in the near-floor  [https://hitommy.net/xe1/my_thoughts/1941534 Wood Ranger official] high Rossby quantity layer. The efficient technology of the close to-surface circulation by way of the gyroscopic pumping successfully suppresses the construction of the NSSL. When the previous calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we didn't have any manner to keep up the photo voltaic-like DR with out utilizing the lowered luminosity,  electric [https://rijocampers.is/what-do-you-need-to-know-before-traveling-to-iceland/ cordless power shears] [http://classicalmusicmp3freedownload.com/ja/index.php?title=Buttery_Pie_Dough Wood Ranger Power Shears for sale] larger rotation charges or enhanced diffusivities (photo voltaic convective conundrum). That's, the everyday &amp;quot;high-resolution&amp;quot; simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta &amp;amp; Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) just lately present a attainable resolution to assemble the photo voltaic-like differential rotation with out using particular treatment proven above.&amp;lt;br&amp;gt;&lt;/div&gt;</summary>
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