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南亚高压上下高原时间及其与高原季风建立早晚的关系

张菁 范广洲 赖欣 张永莉 王炳赟

气象科学2017,Vol.37Issue(1):30-40,11.
气象科学2017,Vol.37Issue(1):30-40,11.DOI:10.3969/2016jms.0025

南亚高压上下高原时间及其与高原季风建立早晚的关系

Establishment or retreatment average date of South Asian High over the Tibetan Plateau and its relation with the Tibetan Plateau monsoon onset

张菁 1范广洲 1赖欣 2张永莉 1王炳赟1

作者信息

  • 1. 成都信息工程大学大气科学学院/高原大气与环境四川省重点实验室,成都610225
  • 2. 南京信息工程大学气象灾害预报预警与评估协同创新中心,南京210044
  • 折叠

摘要

Abstract

By using the NCEP/NCAR daily reanalysis data from 1948 to 2013,the establishment or retreatment average date of South Asian High (SAH) over the Tibetan Plateau and its relation with the Tibetan Plateau summer monsoon onset was analyzed.Results show that the SAH moved northward at the beginning of April,jumpped northward abruptly in May,reached to the most northern position of 55 °N in August,and then withdrew southward in September.SAH moved westerly stablely from May to October,and swang drastically from November to the next April.It is concluded that the first establishment average date of SAH over the Tibetan Plateau is on the 33rd pentad of June,and the climate-mean SAH moving out over the Tibetan Plateau is on the 58th pentad of October.The moving date of SAH on the Tibetan Plateau is 73 days later than that of the Plateau summer monsoon onset,and the retreatment date over the Tibetan Plateau is 5 days earlier than that of the plateau winter monsoon onset.The relation between establishment of SAH over the Tibetan Plateau and Tibetan Plateau summer monsoon onset can be explained the thermal effects of the Tibetan Plateau at different stages,which depend on different heights.

关键词

南亚高压/季节变化/青藏高原/高原季风

Key words

SAH/Seasonal variation/The Tibetan Plateau/Tibetan Plateau monsoon

分类

天文与地球科学

引用本文复制引用

张菁,范广洲,赖欣,张永莉,王炳赟..南亚高压上下高原时间及其与高原季风建立早晚的关系[J].气象科学,2017,37(1):30-40,11.

基金项目

国家自然科学基金资助项目(91537214,41275079,41405069,41305077,41505078) (91537214,41275079,41405069,41305077,41505078)

公益性行业(气象)科研专项(GYHY201506001) (气象)

四川省教育厅科研项目(16ZA0203) (16ZA0203)

成都信息工程大学科研项目(J201516,J201518,KYTZ201517) (J201516,J201518,KYTZ201517)

气象科学

OA北大核心CSTPCD

1009-0827

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