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<br>We carry out an unprecedented excessive-resolution simulation for the photo voltaic convection zone. Our calculation reproduces the fast equator and close to-floor [https://wiki.dulovic.tech/index.php/User:PhilipPratt Wood Ranger Power Shears] shear layer (NSSL) of differential rotation and the close to-surface poleward meridional movement concurrently. The NSSL is located in a posh layer where the spatial and time scales of thermal convection are considerably small compared with the deep convection zone. While there have been a number of attempts to reproduce the NSSL in numerical simulation, the outcomes are nonetheless removed from actuality. On this examine, we reach reproducing an NSSL in our new calculation. 4) the turbulent viscosity and magnetic tension are latitudinally balanced with the Coriolis [http://jicc.kr/bbs/board.php?bo_table=hosung3&wr_id=646519 Wood Ranger Power Shears features] within the NSSL. We emphasize the importance of the magnetic subject 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 in the solar inside. In the solar convection zone, we now have two shear layers, i.e., the tachocline around the base of the convection zone and the close to-floor shear layer (NSSL).<br><br><br><br>The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel & Zahn, 1992; Gough & McIntyre, 1998; Forgács-Dajka & 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 2 Mm, respectively. Thus, the time scales of the convection vary from a month to a number of hours in these regions. As a result, the convection in the NSSL just isn't significantly affected by the rotation. ′ denote the longitudinal common and the deviation from the average. In addition, Miesch & Hindman (2011) recommend that we need a force to balance with the latitudinal Coriolis [https://santo.kr:443/bbs/board.php?bo_table=free&wr_id=254433 Wood Ranger Power Shears] to take care of the NSSL. It is difficult for numerical simulations to cowl a broad range of spatial and time scales. The numerical strategy for the NSSL is extremely restricted.<br><br><br><br>Guerrero et al. (2013) improve the superadiabaticity around the top boundary of their calculation box and talk about the formation mechanism of the NSSL following Foukal & Jokipii (1975). Hotta et al. NSSL-like function, 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) perform an analogous calculation to Hotta et al. 2015) and reproduce the NSSL-like function at high and low latitudes. The authors additionally fail to reproduce the NSSL within the mid-latitude. They conclude that the detailed development mechanism of the meridional stream must be understood to reproduce the correct NSSL. Of their research, highly rotationally constrained convection called the Busse column, is required to reproduce the photo voltaic-like quick equator differential rotation. Hotta et al. (2015) diminished the solar luminosity and Matilsky et al.<br><br><br><br>2019) elevated the rotation charge so as to enhance the rotational influence on the thermal convection. We be aware that the lower in luminosity and the increase in rotation charge 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 within the near-surface high Rossby quantity layer. The efficient technology of the close to-surface circulation by way of 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 manner to maintain the photo voltaic-like DR with out using the lowered luminosity, larger rotation charges or enhanced diffusivities (solar convective conundrum). That's, the everyday "high-resolution" simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta & Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) recently present a possible solution to construct the solar-like differential rotation without utilizing particular therapy proven above.<br>
<br>We carry out an unprecedented high-decision simulation for the solar convection zone. Our calculation reproduces the fast equator and close to-floor shear layer (NSSL) of differential rotation and the near-floor poleward meridional movement simultaneously. The NSSL is located in a complex layer where the spatial and time scales of thermal convection are significantly small compared with the deep convection zone. While there have been several makes an attempt to reproduce the NSSL in numerical simulation, the results are nonetheless far from actuality. In 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 [https://rentry.co/2565-tips-on-how-to-check-in-case-your-barber-shears-are-sharp-enough-to-chop-hair Wood Ranger Power Shears] within the NSSL. We emphasize the significance of the magnetic area in the photo voltaic convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and the sluggish pole. Omega within the photo voltaic interior. Within the photo voltaic convection zone, we've two shear layers, i.e., the tachocline round the base of the convection zone and the near-surface shear layer (NSSL).<br><br><br><br>The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel & Zahn, 1992; Gough & McIntyre, 1998; Forgács-Dajka & 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 [https://plamosoku.com/enjyo/index.php?title=%E5%88%A9%E7%94%A8%E8%80%85:LeticiaG25 Wood Ranger Power Shears] 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 regions. Because of this, the convection within the NSSL is just not considerably affected by the rotation. ′ denote the longitudinal average and the deviation from the common. As well as, Miesch & Hindman (2011) suggest that we need a power to stability with the latitudinal Coriolis drive to take care of the NSSL. It's troublesome for numerical simulations to cowl a broad range of spatial and time scales. The numerical strategy for the NSSL is extremely restricted.<br><br><br><br>Guerrero et al. (2013) enhance the superadiabaticity around the highest boundary of their calculation box and talk about the formation mechanism of the NSSL following Foukal & Jokipii (1975). Hotta et al. NSSL-like feature, especially 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 flow. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) perform an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors also fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed construction mechanism of the meridional flow must be understood to reproduce the proper NSSL. Of their research, extremely rotationally constrained convection known as the Busse column, is required to reproduce the photo voltaic-like fast equator differential rotation. Hotta et al. (2015) decreased the photo voltaic luminosity and Matilsky et al.<br><br><br><br>2019) increased the rotation charge so as to enhance the rotational affect on the thermal convection. We word that the lower in luminosity and the rise in rotation fee have the identical effect on the Rossby number. 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-surface excessive Rossby number layer. The environment friendly generation of the close to-floor circulation by way of the gyroscopic pumping effectively suppresses the development of the NSSL. When the earlier calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we did not have any approach to take care of the solar-like DR without utilizing the lowered luminosity, bigger rotation charges or enhanced diffusivities (solar convective conundrum). That is, the typical "high-resolution" simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta & Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) recently provide a attainable answer to assemble the photo voltaic-like differential rotation without using special therapy proven above.<br>

2025年11月25日 (火) 23:37時点における最新版


We carry out an unprecedented high-decision simulation for the solar convection zone. Our calculation reproduces the fast equator and close to-floor shear layer (NSSL) of differential rotation and the near-floor poleward meridional movement simultaneously. The NSSL is located in a complex layer where the spatial and time scales of thermal convection are significantly small compared with the deep convection zone. While there have been several makes an attempt to reproduce the NSSL in numerical simulation, the results are nonetheless far from actuality. In 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 Wood Ranger Power Shears within the NSSL. We emphasize the significance of the magnetic area in the photo voltaic convection zone. ††software: R2D2 Hotta et al. The Sun is rotating differentially with the quick equator and the sluggish pole. Omega within the photo voltaic interior. Within the photo voltaic convection zone, we've two shear layers, i.e., the tachocline round the base of the convection zone and the near-surface shear layer (NSSL).



The tachocline is thought to be maintained by the interaction between the convection and radiation zones (Spiegel & Zahn, 1992; Gough & McIntyre, 1998; Forgács-Dajka & 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 Wood Ranger Power Shears 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 regions. Because of this, the convection within the NSSL is just not considerably affected by the rotation. ′ denote the longitudinal average and the deviation from the common. As well as, Miesch & Hindman (2011) suggest that we need a power to stability with the latitudinal Coriolis drive to take care of the NSSL. It's troublesome for numerical simulations to cowl a broad range of spatial and time scales. The numerical strategy for the NSSL is extremely restricted.



Guerrero et al. (2013) enhance the superadiabaticity around the highest boundary of their calculation box and talk about the formation mechanism of the NSSL following Foukal & Jokipii (1975). Hotta et al. NSSL-like feature, especially 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 flow. Hotta et al. (2015) fail to reproduce the NSSL in mid-latitude. Matilsky et al. (2019) perform an identical calculation to Hotta et al. 2015) and reproduce the NSSL-like characteristic at excessive and low latitudes. The authors also fail to reproduce the NSSL in the mid-latitude. They conclude that the detailed construction mechanism of the meridional flow must be understood to reproduce the proper NSSL. Of their research, extremely rotationally constrained convection known as the Busse column, is required to reproduce the photo voltaic-like fast equator differential rotation. Hotta et al. (2015) decreased the photo voltaic luminosity and Matilsky et al.



2019) increased the rotation charge so as to enhance the rotational affect on the thermal convection. We word that the lower in luminosity and the rise in rotation fee have the identical effect on the Rossby number. 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-surface excessive Rossby number layer. The environment friendly generation of the close to-floor circulation by way of the gyroscopic pumping effectively suppresses the development of the NSSL. When the earlier calculation (Hotta et al., 2015; Matilsky et al., 2019) was carried out, we did not have any approach to take care of the solar-like DR without utilizing the lowered luminosity, bigger rotation charges or enhanced diffusivities (solar convective conundrum). That is, the typical "high-resolution" simulations fall into anti-photo voltaic differential rotation. O’Mara et al., 2016; Hotta et al., 2023). Hotta & Kusano (2021)(hereafter HK21) and Hotta et al. 2022)(hereafter HKS22) recently provide a attainable answer to assemble the photo voltaic-like differential rotation without using special therapy proven above.