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  1. 系集預報的應用翻轉了對颱風與豪雨定量 降水預報的傳統框架,而使得定量降水預 報技術的發展進入了一個全新的領域。. 52. 路徑預報誤差 • 導致實際降水熱區定 量降水預報的低估 • 非降水熱區有高估的 趨勢. 53. NORTH. Best SOUTH. 852. 884 400~700 ~400. 問題是 ...

  2. Department of Commerce // National Oceanic and Atmospheric Administration // 7 HFSA v0.1A: FV3-based Stand- Alone Regional HAFS coupled with HYCOM, NATL basin HAFS v0.1B: FV3-based Global- nest HAFS, no ocean coupling, NATL basin HAFS v0.1J: FV3-based Stand

  3. 二、次表層海溫 最近30天平均(下圖)及上一個30天平均(上圖)的赤道剖面次表層海溫距平,綠色線為攝氏20度等溫線,約略可代表斜溫層深度。縱軸為深度,單位為公尺,橫軸為經度。最近2年的近赤道上層海洋熱含量與Nino3.4指標(黑色實線)。

  4. PK ‚4²P^Æ2 '' mimetypeapplication/vnd.oasis.opendocument.textPK ‚4²P Configurations2/popupmenu/PK ‚4²P Configurations2/menubar/PK ‚4²P Configurations2 ...

  5. Requirements for Unified Model •Atmospheric Dynamics –Non-Hydrostatic –Scalable, stable and efficient •Physics –Most attractive area for development –Scale-aware/adaptive –Single column vs. 3D –Focus on interactions among various components (including

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