迎风坡的英文

• wind sweep
• windward slope

• "迎风"英文翻译    facing the wind; against the ...
• "坡"英文翻译    slope
• "迎风" 英文翻译 :    1.(对着风) facing the wind; against the wind; windward 迎风航行 sail close to [near] the wind; headwind sailing (帆船运动); pointing; 迎风前进 haul upon the wind2.(随风)down the wind; with the wind3.[航海学] aweather 迎风使舵! helm aweather
• "背风坡" 英文翻译 :    downwind slope; lee slope; lee-slope; leeward slope; leewardslope
• "向风坡" 英文翻译 :    windward slope; windwardslope
• "背风坡低压" 英文翻译 :    lee depression
• "逆风,迎风" 英文翻译 :    hurl to the winds; throw to the winds
• "迎风岸" 英文翻译 :    weather shore; wind-ward bank
• "迎风边" 英文翻译 :    windward side
• "迎风波" 英文翻译 :    windward slope
• "迎风潮" 英文翻译 :    weather tide; windward flood
• "迎风的" 英文翻译 :    into wind; intowind; weather; windward
• "迎风飞" 英文翻译 :    wind blows
• "迎风阁" 英文翻译 :    yfg
• "迎风航" 英文翻译 :    sail to windward
• "迎风礁" 英文翻译 :    windward reef
• "迎风流" 英文翻译 :    windward set
• "迎风面" 英文翻译 :    weather side; windward side; windward surface
• "迎风桥" 英文翻译 :    yingfengqiao
• "迎风舷" 英文翻译 :    weather side
• "迎风弦" 英文翻译 :    weather-board
• "迎风向" 英文翻译 :    windward
• "迎风航驶迎风航驶" 英文翻译 :    on a wind; on the wind
• "帆的迎风缘" 英文翻译 :    luff of sail
• "风区迎风端" 英文翻译 :    windward end of fetch

• Besides , the upward motion on the aweather slope of main mountains of zhoushan archipelago can induce more precipitation and orographic highs
  另外，气流爬越岛屿的主要山脉时的上升运动，会导致迎风坡的降水增多，并诱生中小尺度的地形高压。
• 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
  暖区有明显的强降水中心，雨强极大值出现在山区迎风坡，降水雨滴谱谱宽较大，有时滴谱呈双峰型分布；冷区降水区常呈带状分布，雨区范围大，雨滴谱较窄，雨滴谱为单峰型。
• 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
  纵向岭谷区多年平均夏季降水空间分布主要由纵向岭谷的“阻隔”效应，以及夏季从孟加拉湾来的气流和从南海来的气流在相应迎风坡面辐合，形成两支较强的上升气流所致；而纵向剖面大气环流的变化则较为均匀，显示了纵向岭谷的“通道”效应。