冬季风

  • 网络winter monsoon;EAWM
冬季风冬季风
  1. 异常东亚冬季风激发ENSO的数值模拟研究

    Numerical Simulations of Anomalous Winter Monsoon in East Asia Exciting ENSO

  2. 东亚冬季风异常与全球大气环流变化I.强弱冬季风影响的对比研究

    Eastern Asian Winter Monsoon Anomaly and Variation of Global Circulation Part I : A Comparison Study on Strong and Weak Winter Monsoon

  3. 极地涡旋是冬季风形成的一个风系。

    The polar vortex is a system of wintertime winds .

  4. 东亚冬季风异常与ENSO循环关系的进一步研究

    A Further Research on the Cyclic Relationship between Anomalous East-Asian Winter Monsoon and ENSO

  5. 前期秋季USB模态与东亚冬季风及东亚副热带夏季风之间为负相关关系;

    The USB mode exhibits significant negative correlations with the strength of the East Asian winter monsoon and the East Asian subtropical summer monsoon .

  6. 东亚冬季风年际变化的ENSO信息Ⅰ.观测资料分析

    ENSO Signals in the Interannual Variability of East-Asian Winter Monsoon . Part ⅰ: Observed Data Analyses

  7. 东亚冬季风对秋、冬季SSTA响应的数值试验

    Numerical Experiments on the Responses of East Asian Winter Monsoon to Autumn and Winter SSTA

  8. 当冬季风异常不是由与ELNino或LaNina事件有关的海温异常所引起时,两者之间就缺少显著的联系。

    When the anomalous winter monsoon is not related to the SSTA associated with El Nino or La Nina events , there is no close linkage between them .

  9. 运用相关及滑动相关的计算技术,讨论了近百年东亚冬季风与ENSO循环的相互关系及其年代际异常。

    Based on the method of coherence and moving coherence analysis , the interaction of East Asian monsoon with ENSO cycle and their interdecadal variations in last century are investigated .

  10. 其中11.3~11.0KaBP的冷湿期反映冬季风效应增强,该区可能位于锋面进退的位置,造成较大的有效湿度。

    In the period of 3 ~ 11.0 ka BP , it became cold and wet , with an increased effect of the dry monsoon , and the area was probably situated in a position of the frontal zone . causing considerable effective humidity .

  11. 南海TAV的变化与ENSO事件、东亚冬季风和热带大气环流的变异密切相关。

    The changes of TAV of the ocean are closely related to ENSOevents , the Asian winter monsoon and the tropical atmospheric circulation anomalies .

  12. 因此,数值模拟进一步证实了我们过去从资料诊断和理论分析中得到的结论,即东亚冬季风异常是激发产生ENSO的重要机制。

    Therefore , numerical experiments further prove the conclusion unraveled based on the observed data diagnoses and theoretical analyses in the previous studies & anomalous winter monsoon in East Asia is an important exciting mechanism of ENSO ;

  13. 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。

    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 .

  14. 冬季风的QBO在1920年代前振幅较小,且大约呈现12a的大振幅和6a的小振幅波状的周期变化;

    That the amplitude of QBO in winter monsoon is smaller before 1920s and shows the wavelike changing with greater amplitude of about 12 years and smaller of about 6 years ;

  15. 本文用美国普林斯顿大学海洋模式(POM)的南海版本(SCS-POM)模拟了持续冬季风风应力作用下,南海海流的响应特征。

    The South China Sea version ( SCS-POM ) of the U. S. Princeton University Ocean Model ( POM ) is used in simulations of the responsive properties of oceanic currents in the South China Sea ( SCS ) to the wind stress of winter monsoon .

  16. 利用500hPa北半球格点资料,参照历史平均东亚大槽位置,定义了东亚冬季风强度指数(I500)。

    Based on 500 hPa geopotential height fields and mean position of East Asian trough , a definition of the East Asian winter monsoon index ( I_ ( 500 )) is given .

  17. PDO和SAIB区域的海温变化,尤其是前期(特别是夏季)SAIB区的正海温异常可能对东亚冬季风(蒙古冷高压)的加强活动有指示意义。

    Since the SSTA mode is relatively stationary , the PDO and SST anomaly in the SAIB region could be the factor to predict the Mongolia high activity in winter ( East Asian winter monsoon ) .

  18. 我国的东亚冬季风研究

    A review of studies on East Asia winter monsoon in China

  19. 中国南方地区冬季风降水异常的分析

    An analysis on anomalous precipitation in southern China during winter monsoons

  20. 极涡显著加强(减弱),东亚冬季风减弱(加强)。

    If polar vortex remarkably strengthen , Winter East Asian monsoon weaken .

  21. 冬季风爆发前西伯利亚高压的演变

    The Evolution of Siberian High Prior to the Outbreak of Cold Air

  22. 东亚冬季风指数的定义及其年际年代际异常

    Definition of a East Asian Winter Monsoon Index and Its Variation Characteristics

  23. 早、中更新世东亚冬季风强度的快速变化

    Rapid changes in East Asia winter monsoon in early and Middle Pleistocene

  24. 秋季黑潮海温与东亚冬季风的相关联系

    Relationship between Autumn Kuroshio SST and East Asian Winter Monsoon

  25. 兰州东部地区冬季风场温度场模拟

    The simulations of winter wind and temperature fields of Eastern Lanzhou Area

  26. 东亚冬季风的演变特征

    Climatological Characteristics of evolution of East Asian Winter Monsoon

  27. 夏季风减弱,冬季风增强,年均温下降至*-12OC,降水量降至650nun以下。

    Summer monsoon was weaker and winter monsoon stronger .

  28. 东亚冬季风环流与大气加热场的联系

    The relationship between winter monsoonal circulation and atmospheric heating field of East Asia

  29. 东亚冬季风强度指数及其变化的分析

    East Asian winter monsoon index and its variation analysis

  30. 冬季风期间南海地区冷涌的动力学分析

    Dynamical analysis of cold surge in the South China Sea during winter monsoon