雲粒の落下・雲粒の荷重効果を考慮し, 水平 50 km, 鉛直 20 km の領域で計算を行なった.
高度 15 km より上にスポンジ層(緩和時間 3000 sec)を導入し, 最下層で拡散型の熱フラックスを与えた.
計算コストを下げる為, 雲粒落下速度において, 粘性係数・平均自由行程は基本場の量で評価した.
放射冷却は乾燥断熱減率に従う層(高度 5 km より下)で与えた.
この数値実験において, 等温層での内部重力波の鉛直方向の位相速度は
0.6 -- 1.0 m/s である.
また水平波長は 3 -- 4 km, 鉛直波長は 15 -- 30 km である.
数値実験で実現される波長を用いて, 上記文書 (35) 式より鉛直方向の
位相速度を見積もってみると,
となり, 数値実験で実現される位相速度とおおよそ一致する.
即ち, 本実験で現れる波は重力波の分散関係式をおおよそ満たしている.
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_VelZ_00226800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_VelZ_00237600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_VelZ_00248400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_VelZ_00259200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00000000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00010800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00021600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00032400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00043200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00054000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00064800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00075600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00086400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00097200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00108000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00118800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00129600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00140400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00151200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00162000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00172800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00183600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00194400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00205200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00216000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00226800.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00237600.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00248400.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Km_00259200.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_MassTotal.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_CloudMassTotal.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_KineticEnergyTotal.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00172800-00259200_x15000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00216000-00259200_z18000-25000_x15000.png
高度 18 - 25 km における温位偏差の t-z 図.
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_overplot10.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00256800_overplot150.png
t=256800 sec における様々な水平座標での温位偏差の鉛直分布. スポンジ層(高度 18 km 以上)において, 鉛直上向きに伝播する内部重力波の振幅は約 0.25 倍となっている.
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00258000_overplot150.png
t=258000 sec における様々な水平座標での温位偏差の鉛直分布. スポンジ層(高度 18 km 以上)において, 鉛直上向きに伝播する内部重力波の振幅は約 0.25 倍となっている.
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_overplot150.png
t=259200 sec における様々な水平座標での温位偏差の鉛直分布. スポンジ層(高度 18 km 以上)において, 鉛直上向きに伝播する内部重力波の振幅は約 0.25 倍となっている.
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_x05000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_x10000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_x15000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_x20000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_PotTdempDev_t00259200_x25000.png
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CS1_30kmx25km-thetafix-fall-loading-cooling-from-1km-to-5km-Newton3000_Temp_TZ.png
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