西风带

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  • westerlies
西风带西风带
  1. 娜基莉将受西风带的影响向东至东北偏东移动。

    NAKRI will travel E / ENE under the influence of the westerlies .

  2. 大尺度热源、热汇和地形对西风带的常定扰动(二)

    The steady state perturbations of the Westerlies by the large-scale heat sources and sinks and earth 's orography (ⅱ)

  3. Q矢量锋生函数计算分析表明,该环流圈形成了暴雨区与东北远距离的西风带系统之间的能量转换机制。

    Q-vector frontogenesis function analysis indicated that such circulation cell generated energy transforming system between torrential rain area and the distant westerly to the northeast .

  4. 在西风带,则得到阻高型Rossby孤立波,与阻高也有同样的演变规律。

    And the blocking high solitary Rossby waves which also resemble actual blocking high 's could be gotten too .

  5. 当WENDY低压北上与西风带系统相接、叠加时,高层辐散、低层辐合的良好环境使WENDY环流内的对流云团进一步加强发展。

    When WENDY connected with westerly system , good environment of higher level divergence and lower level convergence strengthened the development of convective cloud .

  6. 沿着西风带急流,Rossby波能量的向东传播在连接欧洲和东亚区域起到重要作用。

    The eastern spread of Rossby wave energy played an important role in connecting Europe and East Asia along the westerly jet .

  7. 高原季风对500hPa中纬度西风带活动的影响

    The relationships between Plateau Monsoon and 500 hPa Westerly Activities In Mid-latitude

  8. 多(少)雨年,中层500hPa中高纬西风带经向运动加强(减弱),从贝加尔湖以北的高纬地区到日本附近的高度场呈+-+(-+-)的波列分布。

    On middle layer ( 500 hPa ), the meridional movement of westly belt in high-middle latitudes strengrhen ( weakened ), there are + - + wave train distributions from the high latitude region to the north of Baikal to the height field near Japan .

  9. 气温变暖对西北西风带冬季气温的影响分析

    Warming on the Northwest westerly with the impact of winter temperatures

  10. 西风带与季风对中国西北地区的水汽输送

    Atmospheric water vapor transport from westerly and monsoon over the Northwest China

  11. 西风带波扰的移行速度

    On the Propagation Speed of Wave Disturbanes in the Westerlies

  12. 岛屿位于气候恶劣的“咆哮西风带”

    The island sits in the infamous " roaring forties "

  13. 一般来说,盛行西风带的气温比较适中。

    The belts of prevailing westerlies in general have moderate average temperature .

  14. 35°S以南的西风带风力较强。

    The west wind is more stronger in the zone south form 40 ° S.

  15. 西风带在这片大陆上常年循环。

    That westerly wind belt circulates the continent .

  16. 西风带中槽脊的移动与发展的估计

    On the estimation of movement and development of the troughs and wedges in the westerlies

  17. 西风带研究的重要意义

    The important significance of westerly wind study

  18. 西风带形势稳定;

    The westerlies situation is stable .

  19. 西风带研究动态

    The Study of Westerly Belt

  20. 阴影区表示西风带。

    Shaded areas are westerlies .

  21. 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

    Influence of the Stationary Disturbance in the Westerlies on the Blocking Highs over the Northeastern Asia in Summer

  22. 美国的气候相当有力地说明了西风带北缘的复杂性。

    The complexities of the northern belt of westerlies are well illustrated in climates in the United States .

  23. 大气环流持续性异常现象&阻塞系统的活动,是一种在西风带中重要的低频变化过程。

    The persistent anomaly in the atmospheric circulation-blocking activity , is an important low-frequency process in the westerly .

  24. 西风带系统的异常活动对2003年淮河暴雨的作用机制研究

    The Abnormal Activity of the Westerlies System and Its Impacts on 2003 Summer Heavy Rainfall over Huaihe Basins

  25. 模式对西风带大型环流形势的预报能力优于对副热带系统的预报能力。

    The model is better working in forecasting of the westerly belt circulation than in prediction of the subtropical circulation .

  26. 当西风带的弱冷空气与副热带高压西北侧的西南气流交汇时,触发对流产生;

    The convection appeared when the cold air of westerlies met the southwest air flow in the west of subtropical high .

  27. 由扰动方程中可以看出通过西风带中的基本波动,不同波长的扰动有了相互制约的关系。

    The equation for the disturbed motion shows that in such a basic current the disturbances of different wave lengths mutually interact .

  28. 西风带系统云系的闪电分布形态特征和范围与热带系统云系有很大的差异。

    Cloud systems of the westerly zone system are quite different from the tropical system in the lightning distribution character and range .

  29. 对梅期进行的波谱分析指出:在入、出梅前后中纬度西风带确实存在优势波的调整。

    Wave spectrum analysis indicates that around the Meiyu end there is indeed an adjustment of the prevailing wave in the mid-latitude westerly .

  30. 中高纬的纬向西风带先增强后减弱甚至消亡,而低纬的东风带则一直减弱。

    Zonal west wind at high latitude becomes stronger and then weaker , but weaker all along for east wind at low latitude .