westerlies

英 [ˈwɛstəliz]

美 [ˈwɛstərliz]

n.  西风
westerly的复数

双语例句

• 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。
• At this time if a trough in the south branch of the westerlies moves eastward over this cold cushion, then there offen appears a trough and frontogenesis in the region surface high.
  在高空平直的西风环流下，沿南支西风急流带，有低压槽在冷空气垫之上东移，地面高气压区域中常有低压槽和锋生出现。
• On the estimation of movement and development of the troughs and wedges in the westerlies
  西风带中槽脊的移动与发展的估计
• Influence of the Stationary Disturbance in the Westerlies on the Blocking Highs over the Northeastern Asia in Summer
  水平扩散对东西风带模拟的改进夏季西风带定常扰动对东北亚阻塞高压的影响
• Amplification of westerlies trough and ridge in Southern Hemisphere mid-high latitude and augmentation of subtropical system meridional circulation in Northern Hemisphere are significant role of the Asian summer monsoon onset.
  南半球中高纬西风带槽脊振幅的增强和北半球副热带系统经向环流的加大是南海夏季风爆发的重要原因。
• 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；
• 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。
• The Abnormal Activity of the Westerlies System and Its Impacts on 2003 Summer Heavy Rainfall over Huaihe Basins
  西风带系统的异常活动对2003年淮河暴雨的作用机制研究
• NAKRI will travel E/ ENE under the influence of the westerlies.
  娜基莉将受西风带的影响向东至东北偏东移动。
• 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。