easterlies

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网络  东风带; 东风

双语例句

• In winter, the circum-polar westeries prevail in the eastern hemisphere in low latitudes, while in summer there shows strong easterlies and a quasi-stationary sub-tropical high in the upper troposphere over the Asia-African continent.
  在东半球低纬度冬季为绕极西风，而到夏季为强东风气流，并在亚非高空产生强大的副热带大陆高压。
• It is then possible that "Kelvin cat's eyes" produced by the nonlinear critical layer is a new physical mechanism generating the subtropical high in the vicinity of the interface betWeen zonal easterlies and westerlies.
  因此，非线性临界层产生的Kelvin猫眼有可能是位于纬向东西风交界面附近的副热带高压形成的一种新的物理机制。
• Case study on the impact of the vortex in the easterlies over the tropical upper troposphere on the sub tropical anticyclone over Western Pacific Ocean
  热带对流层上空东风带扰动影响西太平洋副热带高压的个例分析
• The Meiyu cloud band is associated with an anticyclonic wind belt with mid-latitude westerlies to the north and subtropical easterlies to the south.
  中纬度西风与MCS南部的偏东北风构成一个反气旋环流带。
• The correlations between profile characteristics of easterlies and westerlies and the structure of stationary waves of the general circulation equilibrium state, forced by external forcing, are investigated with a simplified two-level model.
  本文采用简化数学模型探讨了东、西风廓线特征与外源强迫下大气环流平衡态定常波结构的相关关系。
• The summer monsoon circulation in India was established somewhat later, accompanying with the Somali low jer and the northern upper Easterlies.
  印度夏季风环流建立时间较晚，它与索马里低空急流，北支高空东风急流相联系。
• Otherwise, local Hadley circulation plays a key role on the interface structure formation of the easterlies and westerlies in Asian regional tropical troposphere.
  另外，局域Hadley环流对亚洲区域热带对流层东西风带界面结构特征的形成起关键作用，该交界面关于赤道准对称。
• Whereas the monsoonal circulation in the tropical South China Sea is related to the cross-equatorial current from Australia and the southern upper Easterlies.
  而南海热带季风环流与源于澳大利亚的跨赤道气流，南支高空东风相联系。
• Further investigation find that the anomaly of AO contributes to the temperature anomalies of the Northeast China through the interaction of the Siberian high, Aleutian low, the polar easterlies in east Asia and the winds anomalies in winter in this area.
  研究表明，AO的异常变化通过西伯利亚高压、阿留申低压、东亚地区极地东风以及东亚冬季风异常，进而影响我国东北地区冬季温度异常，它们之间存在着密切的相关关系。
• The third wind belt develops as cold polar air sinks and moves south, is deflected to the right, and is therefore called the polar easterlies.
  当冷的极地的空气下沉并且移动南方，受科氏力影响偏向右边，因此被称为极地东风带。