夏季青藏高原低压的年际和年代际变化及其与我国降水的关系

谢清霞-;范广洲*;周定文;朱丽华;王轶;张永莉

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高原气象 ›› 2012, Vol. 31 ›› Issue (6) : 1503-1510.
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夏季青藏高原低压的年际和年代际变化及其与我国降水的关系

  • 谢清霞-;范广洲*;周定文;朱丽华;王轶;张永莉
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Interannual and Interdecadel Changes of Summer Low over the Qinghai- Xizang Plateau and Its Relationship to Precipitation in China

  • XIE Qing-xia-;FAN Guang-zhou;ZHOU Ding-wen;ZHU Li-hua
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摘要

利用NCEP/NCAR再分析月平均资料, 分析了1948-2009年夏季青藏高原(下称高原)600 hPa位势高度场的变化趋势, 发现整个高原位势高度场都出现大范围的升高, 低压中心主要位于27.5°-40°N、 80°-102.5°E范围内, 定义该范围内位势高度场的平均值为高原夏季低压指数。采用经验正交函数分解(EOF)和小波分析等方法对近62年夏季高原低压的年际和年代际变化特征进行了分析。结果表明, 近62年夏季高原低压总体呈减弱趋势, 在20世纪80年代之前, 夏季高原低压指数均处于低值范围, 并在1962年出现最小值, 在1979年左右出现最大值, 之后在高值范围内上下振荡; 空间分布表现为低压在高原大部分区域均为由南向北递增, 呈明显的纬向分布;  低压在1976年发生了一次较明显的减弱突变\.小波分析表明, 低压具有1~2年和13年周期。利用中国596个测站的月降水资料, 采用相关分析和合成分析等方法分析了高原低压与我国夏季降水的关系, 分析表明, 高原低压增强时长江流域和新疆地区的降水偏多, 而东北、 华北和华南地区的降水则偏少。

Abstract

The tendency variation of 600 hPa geopotential height fields over the Qinghai-Xizang Plateau(QXP) in the summer months (JJA) during1948-2009 were calculated based on the NCEP/NCAR data. The geopotential height field shows a increasing trend since 1948. The center was located on the low area over 27.5°-40°N, 80°-102.5°E on 600 hPa, it is defined regional average as summer  low index over the QXP. Using the Empirical Orthogonal Function (EOF) and wavelet analysis, the interannual and interdecadal changes of the summer low index over the QXP are examined. The results of temporal-spatial structures reveal that: In general, the  summer low over the QXP shows a decreasing trend since 1948. The low index has been in a low phase before  1980s, and it is the lowest in 1962 and the highest in 1979. From the 1980s to the early 21st century the low index has been in a high phase. The spatial distribution of the low index  reveals that most of the low indexes over the QXP region  increase from south to north, appears obvious zonal distribution, and its expansion coefficient shows the long-term positive trend. The analysis of the expansion coefficient shows that there is a obvious weakening change of the low in 1976. Wavelet analysis of expansion coefficients indicates that there are the periods of 1~2  and 13 years. At last, using the precipitation data from 596 stations in China, the relationship between interannual and interdecadal changes of the summer low  over the QXP and the precipitation in China is explored: When the plateau low increasing, the precipitation  in the Yangtze River and Xinjiang is more,  precipitation  in the Northeast China, North  China and South China is less.

关键词

青藏高原 / 热低压 / 降水

Key words

Qinghai-Xizang Plate / Heat low / Precipitation

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谢清霞-;范广洲*;周定文;朱丽华;王轶;张永莉. 夏季青藏高原低压的年际和年代际变化及其与我国降水的关系. 高原气象. 2012, 31(6): 1503-1510
谢清霞-;范广洲*;周定文;朱丽华;王轶;张永莉. Interannual and Interdecadel Changes of Summer Low over the Qinghai- Xizang Plateau and Its Relationship to Precipitation in China. Plateau Meteorology. 2012, 31(6): 1503-1510

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