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Odaka et al. (1998) の計算(dx = 100 m)

概要

arare (arare3m) を用いて Odaka et al. (1998) の再計算を行った.

計算設定

$B%=!<%9%W%m%0%i%`(B arare3m-20050716
$B4pK>l$N29EY(B $B9bEY(B 5 km $B0J2<$O290L(B 245 K, $B9bEY(B 5 km $B0J>e$G$O29EY(B 220 K
$B4pK>l$N05NO(B $B@E?e05J?9U(B ($BCOI=LL$G(B 700 Pa)
$B29EY$N=i4|>qMp(B $B:G2qMp$rM?$($k(B
$B05NO$N=i4|>qMp(B $B$J$7(B
$BIwB.$N=i4|CM(B u = 0 m/s , w = 0 m/s
$BJ| $B9bEY(B 5 km $B0J2<$G(B -50 K /day $B$N0lMMNd5Q(B
$BCOI=LL%U%i%C%/%9(B $B%P%k%/K!(B($B%P%k%/78?t$OG.(B, $B1?F0NL$H$b$K(B 0.01 $B$G0lDj(B, $BCOI=LL29EY(B 270 K $B$G8GDj(B)
$B=ENO2CB.EY(B 3.72 m/s2
$BDj05HfG.(B 32.3 J/K mol (734 J/K kg)
$BJ?6QJ,;RNL(B 44 x 10-3 kg/mol
$BG4@-(B Klemp and Wilhelmson (1978), $B78?t(B 0.2
$B2;GH$N8:?j(B $B$"$j(B ($B78?t$O(B 5.0 x 10-7)
$B;~4V%U%#%k%?(B $B$"$j(B ($B78?t$O(B 0.1)
$B?tCMG4@-(B $B$"$j(B (5.0 x 10-4)
$B7W;;NN0h(B $B?eJ?(B 51.2 km x $B1tD>(B 10 km
$B3J;RE@4V3V(B $B?eJ?(B 100 m x $B1tD>(B 100 m
$B@QJ,;~4V(B 12 $B;~4V(B
$B;~4V%9%F%C%W(B $BD9$$(B: 3 $BIC(B, $BC;$$(B: 0.15 $BIC(B
$B6-3&>r7o(B $B?eJ?(B: $B<~4|(B, $B1tD>(B: rigid-rid($B2<(B), free-slip($B>e(B)
$B?tCM2rK!(B $B?eJ?(B: $BM[2rK!(B, $B1tD>(B: $B1"2rK!(B


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$B
$B PC (Intel Pentium 3 CPU 1 GHz x 2)
$B 48 $B;~4V(B 12 $BJ,(B

$B7W;;7k2L(B


arare-mars-dx100-PotTemp-t43200.png
温位擾乱 (t = 12 hour)

arare-mars-dx100-PotTemp-znarrow-t43200.png
下層の温位擾乱 (t = 12 hour)

arare-mars-dx100-PotTemp-xm-t43200.png
水平平均した値を引いた温位擾乱 (t = 12 hour)

arare-mars-dx100-VelX-t43200.png
水平風速 (t = 12 hour)

arare-mars-dx100-VelZ-t43200.png
鉛直風速 (t = 12 hour)
   
This page is generated by thum/mars_dx100.rb and thum/mars_dx100.txt (2005/12/07 14:57:35 kitamo)
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