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夏季青藏高原大气热源低频振荡与南亚高压东西振荡的关系

王黎娟 葛静

王黎娟, 葛静. 夏季青藏高原大气热源低频振荡与南亚高压东西振荡的关系[J]. 大气科学, 2016, 40(4): 853-863. doi: 10.3878/j.issn.1006-9895.1509.15164
引用本文: 王黎娟, 葛静. 夏季青藏高原大气热源低频振荡与南亚高压东西振荡的关系[J]. 大气科学, 2016, 40(4): 853-863. doi: 10.3878/j.issn.1006-9895.1509.15164
WANG Lijuan, GE Jing. Relationship between Low-frequency Oscillations of Atmospheric Heat Source over the Tibetan Plateau and Longitudinal Oscillations of the South Asia High in the Summer[J]. Chinese Journal of Atmospheric Sciences, 2016, 40(4): 853-863. doi: 10.3878/j.issn.1006-9895.1509.15164
Citation: WANG Lijuan, GE Jing. Relationship between Low-frequency Oscillations of Atmospheric Heat Source over the Tibetan Plateau and Longitudinal Oscillations of the South Asia High in the Summer[J]. Chinese Journal of Atmospheric Sciences, 2016, 40(4): 853-863. doi: 10.3878/j.issn.1006-9895.1509.15164

夏季青藏高原大气热源低频振荡与南亚高压东西振荡的关系

doi: 10.3878/j.issn.1006-9895.1509.15164
基金项目: 第三次青藏高原科学实验项目--边界层与对流层观测GYHY201406001,江苏省高校自然科学研究重大项目14KJA170004,江苏省自然科学基金项目BK20131432,江苏省“青蓝工程”项目,江苏省“333”工程项目

Relationship between Low-frequency Oscillations of Atmospheric Heat Source over the Tibetan Plateau and Longitudinal Oscillations of the South Asia High in the Summer

  • 摘要: 利用1983~2012年NCEP/NCAR逐日再分析资料对夏季青藏高原大气热源和南亚高压东西振荡的低频特征以及两者的关系进行了讨论,发现夏季青藏高原东部大气热源与南亚高压纬向运动的主要低频周期都是10~20 d。在高原东部大气热源10~20 d振荡峰值位相,青藏高原上空被低频气旋控制,高原西部被低频反气旋控制,导致南亚高压主要高压中心向西移动呈伊朗高压模态;在大气热源10~20 d振荡谷值位相,低频环流形势完全相反,青藏高原上空被低频反气旋控制,高原西部被低频气旋控制,致使南亚高压主要高压中心向东移动呈青藏高压模态。高原热力场异常导致其上空暖中心变化从而引起的高层风场变化可以解释南亚高压的东西振荡。
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  • 收稿日期:  2015-03-23

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