风偏的英文

• windage yaw

• "风"英文翻译    wind
• "偏"英文翻译    inclined to one side; slanti ...
• "风偏差" 英文翻译 :    windage
• "风偏角" 英文翻译 :    deviation of wind
• "风偏流" 英文翻译 :    wind drift
• "风偏向" 英文翻译 :    deviation of wind
• "风偏转" 英文翻译 :    wind deflection
• "表面流,风偏移" 英文翻译 :    wind drift
• "侧风偏流" 英文翻译 :    cross wind drift
• "向风偏航" 英文翻译 :    ardency
• "向下风偏转" 英文翻译 :    fall to leeward
• "修正风偏差" 英文翻译 :    compensation for wind; compensationforwind
• "飞机随风偏移" 英文翻译 :    drift off
• "向下风偏航性" 英文翻译 :    slackness
• "风篷儿" 英文翻译 :    feng peng er
• "风配图" 英文翻译 :    wind rose
• "风炮" 英文翻译 :    fm-688gl; pneumatic pick; zc-55gl
• "风派人物" 英文翻译 :    opportunist; fence-sitter; timeserver; a weather cock
• "风疟" 英文翻译 :    wind malaria; wind type malaria; wind-malaria; wind-type malaria

• ( 2 ) the anomalous eawm predominantly relates to the winter kuroshio ssta . the winter kuroshio ssta becomes positive ( negative ) when there is a strong ( weak ) eawm . the possible links might be the winter latent and sensible heat release in the west - northern pacific ocean
  ( 2 )东亚冬季风异常对冬季黑潮区域海温异常有密切的联系，当东亚冬季风偏强时，冬季黑潮区域海温偏低；反之，冬季黑潮区域海温偏高。
• ( 3 ) when the heat source over the bay of bengal is abnormally strong ( weak ) , the sourthern asian high extends westward ( eastward ) , and the western pacific subtropical high extends eastward ( westward ) , and the indian summer monsoon is stronger ( weaker ) , and the eastern asian tropical summer monsoon is weaker ( stronger )
  ( 3 )当孟加拉湾热源异常强(弱)时，南亚高压偏西(东) ，西太平洋副热带高压位置偏东(西) ；印度夏季风偏强(弱) ，东亚热带季风偏弱(强) 。
• When the heat source over the bay of bengal was abnormally strong ( weak ) , the southern asian high extended westward ( eastward ) , and the western pacific subtropical high extended eastward ( westward ) , and the indian summer monsoon was stronger ( weaker ) , and the eastern asian tropical summer monsoon was weaker ( stronger )
  当孟加拉湾热源异常强（弱）时，南亚高压偏西（东） ，西太平洋副热带高压位置偏东（西） ；印度夏季风偏强（弱） ，东亚热带季风偏弱（强） 。
• ( 4 ) the correlations are significant between the sth position index and the general circulation . in the westerly ( easterly ) year , equatorial westerly is weaker ( stronger ) , cross - equatorial flow is weaker ( stronger ) , south china sea summer monsoon is weaker ( stronger ) , the yangtze river valley westerly is stronger ( weaker ) , which has the positive ( negative ) effect on the maintenance of rain band over the yangtze river valley , so the rainfall is more ( less ) in this area and it is hit by floods ( droughts ) , vice versa
  ( 4 )本文运用定义的副高指数研究了六月份副高偏东偏西年份的大型环流特征及其对我国东部天气的影响，风矢量场和相关场分析结果表明：副高偏西(东)年，赤道西风减弱(增强) ，越赤道气流偏弱(增强) ，南海夏季风偏弱(强) ，而长江流域西风增强(减弱) ，有(不)利于雨带在江淮流域维持，该地区降水偏多(少)易涝(旱) 。
• O in the century . annual rainfall in hong kong was found to be inversely related to the strength of the monsoon in the preceding winter ( figure 3 ) , e . g . , following the weak monsoon in december 1994 - february 1995 ( preceding winter of 1995 ) , 2754 mm of rainfall were recorded in 1995 , 540 mm more than the normal rainfall of 2214 mm . figure 2
  假若冬季季候风偏弱，随后一年雨量偏多的机会亦会较高（见图三） ，例如1994年12月至1995年2月期间的冬季（即1995年的前期冬季）季候风偏弱， 1995年录得的年雨量达到2754毫米，比气候平均的2214毫米多了540毫米。
• ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ) , and the low of the asian land is stronger ( weaker ) , which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ) , then the southeastern , warm and damp airflow towards the north china is stronger ( weaker ) , and the cold airflow of the high level over the north china is also stronger ( weaker ) , which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ) , while the sst of west wind drift is higher ( lower )
  ( 5 )春季格陵兰海冰面积偏大(小) ：后期夏季日本海高压偏强(弱) ，而大陆上低压也偏强(弱) ，易(不易)形成西低东阻的形势；华北地区的上升运动增强(减弱) ；东亚夏季风偏强(弱) ，向华北地区输送的西南暖湿气流偏强(弱) ，而对应高空华北地区上空冷空气活动偏强(弱) ，利于(不利于)华北上空冷暖空气的交汇；夏季赤道东太平洋海温偏低(高) ，西风漂流区海温偏高(低) 。在以上的环流背景下，华北夏季降水偏多(少) ，易涝(旱) 。
• As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
  结果发现当黑潮海温冷异常时，后期夏季大陆热低压加深，东亚夏季风偏强。中纬度阻塞高压减弱，东亚地区纬向环流发展，在东亚-西太平洋地区激发“ - + - ”的东亚遥相关型，从而西太平洋副高强度偏弱，面积偏小，位置偏东、偏北，东亚梅雨锋也偏弱，季风槽则变强，位置偏北。同时南亚高压偏弱，位置偏北、偏东，易形成东部型。
• In dry ( wet ) year , mongolia high was stronger ( weaker ) , indian low was later ( sooner ) and weaker ( stronger ) , baikal blocking high was stronger ( weaker ) , asian summer monsoon was weaker ( stronger ) , west pacific subtropical high leaned toward north ( south ) , east ( west )
  这些异常表现为：旱(涝)年蒙古高压异常偏强(弱) ，印度热低压建立晚(早)且较弱(强) ，贝加尔湖阻塞高压较强(弱) ，亚洲夏季风偏弱(强) ，西太平洋副热带高压偏南(北) ，偏东(西) 。
• Analysis shows that when summer precipitation in north china is richer ( less ) , tropical east pacific ssta is colder ( warmer ) phase , and slp and 500hpa geo - potential height are negative ( positive ) anomaly over the asia , west pacific sub - high is northerner ( southerner ) , and block high in mid - highs latitude happens less ( more ) than normal , east monsoon is stronger ( weaker )
  分析表明华北夏季多(少)雨期，赤道中东太平洋ssta处于冷(暖)位相，在非洲大陆上slp利500hpa位势高度均为负(正)异常，西北太平洋副高位置偏北(南) ，中纬度阻塞高压发生频率较低(高) ，东亚夏季风偏强(弱) 。