[地球流体電脳倶楽部] [dcmodel | dcmodel-tools] [dcmodel-thum.rb]

deepconv/arare4 : 主成分凝結を考慮した湿潤対流実験(中層一様冷却・下層拡散型熱フラックス, 臨界飽和比 1.35, 地表面温度 165 K の場合)

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.

計算設定

• 計算領域
  • 水平 30 km
  • 鉛直 25 km
• 基本場の設定
  • 最下層気温 165 K, 地表圧力 7 hPa
  • 地表から高度 3 km 付近まで等温位, 高度 3 km 付近から高度 15 km 付近まで湿潤断熱, 高度 15 km 付近から等温(135 K).
• 空間/時間格子間隔, 境界条件
  • 空間格子間隔
    • 水平 200 m, 鉛直 200 m
    • 格子点数は 150 x 125
  • 時間格子間隔
    • 長い時間ステップ 1.0 sec, 短い時間ステップ 0.125 sec
  • 境界条件
    • 水平境界: 周期境界条件
    • 上下境界: 応力なし, w=0
    • 熱フラックス: 最下層で拡散的に与える
      • F = Kπ(θ_1 - θ_boundary)/ 0.5 Δz (とりあえず木星計算同様に, K = 800 m^2/sec としている)
  • 放射強制
    • 高度 1-5 km: 5 K/day で一様冷却
  • スポンジ層
    • 高度 15 km より上にレイリー摩擦(時定数 3000 s で初期値に戻す)
• 初期条件
  • 最下層で振幅 1.0 K の温位擾乱を与える.
• 積分時間
  • 432000 sec (0 -- 5 日)

結果一覧

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