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Table 1:

Basic parameters of the RHD models (mostly 2D and only one 3D).

Model 		p $n_x \times n_z$ $x \times z$ t0 - t1 $C_{\rm Cour}$ $s_{\rm in}$ $T_{\rm eff,sta}$ $T_{\rm eff}$ $T_{\rm opa}$
      km $\times$ km 103 s   erg K-1 g-1 K K K

mt09g50mm00n10 		d 400 $\times$ 430 220 $\times$ 94 90-130 0.30 0.671 $\times$ 109 900 897 1000
mt09g50mm00n11 d 400 $\times$ 410 220 $\times$ 90 240-275 0.30 0.671 $\times$ 109 900 897 1000
mt10g50mm00n03 d 400 $\times$ 400 240 $\times$ 96 140-195 0.27 0.683 $\times$ 109 1000 1030 1000
mt11g50mm00n05 d 400 $\times$ 356 260 $\times$ 92 245-285 0.30 0.690 $\times$ 109 1100 1114 1800
mt12g50mm00n01 s 400 $\times$ 336 280 $\times$ 94 110-190 0.40 0.701 $\times$ 109 1200 1226 1800
mt12g50mm00n07 s 400 $\times$ 380 280 $\times$ 106 80-150 0.40 0.701 $\times$ 109 1200 1228 1800
mt12g50mm00n10 s 400 $\times$ 336 280 $\times$ 94 270-370 0.37 0.701 $\times$ 109 1200 1224 1800
mt13g50mm00n01 s 400 $\times$ 270 300 $\times$ 100 80-190 0.40 0.711 $\times$ 109 1300 1335 1800
mt13g50mm00n02 d 400 $\times$ 270 300 $\times$ 100 130-200 0.40 0.711 $\times$ 109 1300 1336 1800
mt13g50mm00n03 s 400 $\times$ 270 300 $\times$ 100 250-390 0.35 0.711 $\times$ 109 1300 1333 1800
mt14g50mm00n01 s 400 $\times$ 270 320 $\times$ 106 40-140 0.40 0.719 $\times$ 109 1400 1436 1800
mt14g50mm00n02 s 400 $\times$ 270 320 $\times$ 106 140-280 0.40 0.719 $\times$ 109 1400 1437 1800
mt15g50mm00n01 s 400 $\times$ 270 340 $\times$ 113 50-140 0.40 0.728 $\times$ 109 1500 1533 1800
mt15g50mm00n02 s 400 $\times$ 270 340 $\times$ 113 150-190 0.40 0.728 $\times$ 109 1500 1533 1800
mt15g50mm00n03 s 400 $\times$ 270 340 $\times$ 113 260-380 0.30 0.728 $\times$ 109 1500 1533 1800
mt15g50mm00n04 s 300 $\times$ 270 340 $\times$ 113 40-150 0.30 0.728 $\times$ 109 1500 1532 1800
mt15g50mm00n06 s 3002 $\times$ 270 3402 $\times$ 113 10-15 0.30 0.728 $\times$ 109 1500 1532 1800
mt15g50mm00n07 s 400 $\times$ 300 340 $\times$ 127 70-150 0.30 0.728 $\times$ 109 1500 1533 1800
mt16g50mm00n06 s 400 $\times$ 366 352 $\times$ 128 20-190 0.40 0.737 $\times$ 109 1600 1648 1800
mt17g50mm00n02 s 400 $\times$ 352 380 $\times$ 133 40-190 0.40 0.747 $\times$ 109 1700 1757 1800
mt18g50mm00n07 s 400 $\times$ 343 400 $\times$ 137 40-190 0.40 0.756 $\times$ 109 1800 1858 1800
mt19g50mm00n02 s 400 $\times$ 334 420 $\times$ 140 40-80 0.40 0.765 $\times$ 109 1900 1953 1800
mt19g50mm00n03 s 400 $\times$ 334 420 $\times$ 140 120-290 0.30 0.765 $\times$ 109 1900 1953 1800
mt20g50mm00n05 s 400 $\times$ 362 380 $\times$ 137 40-210 0.20 0.775 $\times$ 109 2000 2052 1800
mt22g50mm00n05 s 400 $\times$ 351 400 $\times$ 140 70-150 0.20 0.798 $\times$ 109 2200 2247 1800
mt24g50mm00n01 s 400 $\times$ 344 420 $\times$ 144 70-190 0.20 0.825 $\times$ 109 2400 2426 1800
mt26g50mm00n01 s 400 $\times$ 353 420 $\times$ 148 70-140 0.20 0.859 $\times$ 109 2600 2597 1800
mt26g50mm00n02 s 400 $\times$ 353 420 $\times$ 148 70-140 0.20 0.859 $\times$ 109 2600 2611 2800
mt28g50mm00n01 s 400 $\times$ 357 440 $\times$ 157 70-140 0.20 0.905 $\times$ 109 2800 2801 2800
mt28g50mm00n02 s 400 $\times$ 380 440 $\times$ 167 40-100 0.20 0.905 $\times$ 109 2800 2801 2800

Notes. The columns show model name, numerical precision (single or double), horizontal $\times$ vertical resolution, horizontal $\times$ vertical size [km $\times$ km], time span used for averaging [103 s], Courant number, entropy of the material in the deeper layers [erg K-1 g-1], effective temperature of the PHOENIX model used for the start file [K], effective temperature of the RHD model versus the average time span [K], and effective temperature of the reference atmosphere used for the opacity table [K].


Source LaTeX | All tables | In the text

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