迎風坡 的英文怎麼說

中文拼音 [yíngfēngpō]
迎風坡 英文
wind sweep
  • 迎 : 動詞1. （迎接） go to meet; greet; welcome; receive 2. （對著;沖著） move towards; meet face to face
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 坡 : Ⅰ名詞（地面傾斜的地方） slope Ⅱ形容詞（傾斜） sloping; slanting
  • 迎風 : 1 （對著風） facing the wind; against the wind; windward 2 （隨風）down the wind; with the wind3 ...
  1. Besides, the upward motion on the aweather slope of main mountains of zhoushan archipelago can induce more precipitation and orographic highs

    另外，氣流爬越島嶼的主要山脈時的上升運動，會導致迎風坡的降水增多，並誘生中小尺度的地形高壓。
  2. Heavy rainfall occurred in the warm area, and maximum rainfall lay in the windward slope where the width of raindrop size distribution was b roadened and sometimes it was bimodal spectrum. the shape of rain band in cold area was zonal, and the area of rain band was small

    暖區有明顯的強降水中心，雨強極大值出現在山區迎風坡，降水雨滴譜譜寬較大，有時滴譜呈雙峰型分佈；冷區降水區常呈帶狀分佈，雨區范圍大，雨滴譜較窄，雨滴譜為單峰型。
  3. When air travels up the windward slope of a mountain, it condenses to form clouds if it is sufficiently moist and the surrounding is sufficiently cool

    當空氣向山坡的迎風面上升時，若果水份充足及環境溫度夠低，空氣中的水份便會凝結成雲。
  4. The distribution of lrgr summer mean rainfall was determined by the obstructing effect and two stronger ascending airflow that come from bengal bay and south sea and converge around corresponding windward slopes ; the general circulation distribution in meridional section is equal, which showed the passing - effect of lrgr

    縱向嶺谷區多年平均夏季降水空間分佈主要由縱向嶺谷的「阻隔」效應，以及夏季從孟加拉灣來的氣流和從南海來的氣流在相應迎風坡面輻合，形成兩支較強的上升氣流所致；而縱向剖面大氣環流的變化則較為均勻，顯示了縱向嶺谷的「通道」效應。
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