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westerlies

英 [ˈwɛstəliz]

美 [ˈwɛstərliz]

n.  西风
westerly的复数

双语例句

  • During the negative BWA summer, equatorial westerlies are weaker than the climatological mean since the above physical process is weakened with the equatorial eastward propagating BSISO weaker.
    而在负BWA年,赤道地区西风背景减弱,以上物理过程受削弱使赤道东传BSISO偏弱。
  • The close relation is also represented by the relationship between the utilizable water resource and the synoptic system of westerlies and subtropical belt.
    主要表现在与前年秋季和冬季高度场的相关上,与大气环流中高纬西风带系统和副热带系统强弱也有十分密切关系。
  • It shows that these equatorial westerlies are an important basic current in the low latitudes in Indian Ocean.
    分析表明,赤道西风是印度洋低纬地区的一支重要的基本气流。
  • Strong westerlies, at times, have been observed near the tropopause over Recife, Brasil, approximately9o from the equator.
    强大的西风气流有时曾在离赤道大约9个纬度的巴西Recife上空的对流层顶附近观测到过。
  • The prevailing south-west winds or the Westerlies blow over the country all the year round bringing warm and wet air in winter and keeping the temperatures moderate;
    一年四季盛行的西南风和西风在冬季从大西洋带来温暖、潮湿的空气,使气温适宜;
  • Shaded areas are westerlies.
    阴影区表示西风带。
  • Results show that the variation of the position and the intensity of the western Pacific subtropical high play a crucial role in going northward typhoons. Furthermore, the middle-latitude westerlies systems and the South Asian High actions have an important influence on typhoon ′ s northward movements.
    结果发现,不仅西北太平洋副热带高压位置和强度变化对台风登陆北上起决定性作用,而且西风带系统和南亚高压活动有利于台风登陆后北折和持续北上也有不可忽视的影响。
  • The connection between profile characteristics of the westerlies and seasonal characters of atmospheric circulation pattern are studied used observation data.
    文中采用实际观测资料研究了西风廓线特征与大气环流型季节特征之间的联系。
  • The circulation features in the westerlies, especially, distribution and variation of the upper – level westerlies play an important role in controlling the different tracks.
    西风环流,尤其是中、高纬度高层西风的分布及其变化对于形成不同类型的台风路径亦起了很重要的作用。
  • The relationship between the main characteristics of the Pacific subtropical high and typhoon tracks during the occurrence of the westerly belt long-wave trough over some specific regions in Asia is discussed according to the interaction between the mid-latitude westerlies and the circulation system in the subtropical region.
    本文根据中纬度西风带和副热带地区的环流相互作用,讨论了西风带长波槽出现在亚洲上空几个特定地区时,出现的太平洋副高和台风路径的主要特征。