风偏 meaning in Chinese
windage yaw
Examples
- ( 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。