阿留申低压

  • 网络Aleutian Low
阿留申低压阿留申低压
  1. 除冬季亚洲大陆高压增强和阿留申低压加深南移可能触发ELNino事件外,全球变暖的线性递增趋势对于ELNino事件的发生也有一定影响。

    The linear trends of global warming seems to play a certain role for El Nino onset except the Asian continent high increasing and Aleutian low decreasing and shifting southeastward .

  2. 风应力异常敏感性试验的结果显示,阿留申低压南面增强的西风可以显著地增强表层的Ekman平流,导致北太平洋中部海温的负异常。

    Numerical experiments reveal that an enhancement of westerly in the south vicinity of Aleutian low significantly increases the Ekman advection consequently cooling the central North Pacific .

  3. 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 .

  4. 近50年阿留申低压地区凝结加热的变化

    Variation of the Condensation Heating in the Region of the Aleutian Low during the Last 50 Years

  5. 北太平洋热含量的年代际变化特征及其与阿留申低压的关系

    Features of Interdecadal Variation of the North Pacific Heat Storage and Their Relation to the Aleutian Low

  6. 该处凝结加热的垂直分布不均匀可引起大气环流热力适应,从而可能有利于阿留申低压的加强;

    The vertical structure of heating in this region will lead to the atmospheric adaptation to diabatic heating , which may be in favor of the intensification of the Aleutian Low ;

  7. 基本态的第一特征向量表现为弱西伯利亚高压、强北大西洋高压的强纬向环流的特征;第二特征向量表现为弱阿留申低压及强北太平洋高压。

    The first eigenvector of the base state displays a weak Siberian high , a robust Atlantic high and intense zonal circulation , while the second reveals a feeble Aleutian low and a vigorous North Pacific high .

  8. 研究表明:冬季阿留申低压地区上空存在较强的凝结加热,它与阿留申低压的强度存在显著的正相关关系;

    The results show that there is strong condensation heating in the region of the Aleutian low only in winter , and there is a significantly positive correlation between this condensation heating and the intensity of the Aleutian low ;

  9. 冷夏前期,大陆冷高压偏弱,冷空气活跃,冰岛低压和阿留申低压发展较深,太平洋副高持续偏弱,这种状态可以持续到夏季,便形成了东北地区的冷夏。

    In pre-cold summer , continual cold high is weaker , cold air is active , Icelandic low and Aleutian low develop more heavier , Pacific sub-high continues weaker , which can sustain to summer , so that this case leads to cold summer in east-north of China .

  10. 生活在阿留申群岛和阿拉斯加州的民族的人。近50年阿留申低压地区凝结加热的变化

    A member of the people inhabiting the Aleutian Islands and W Alaska . Variation of the Condensation Heating in the Region of the Aleutian Low during the Last 50 Years