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中国西南干旱对气候变暖的响应特征

姚玉璧 张强 王劲松 尚军林 王莺 石界 韩兰英

生态环境学报Issue(9):1409-1417,9.
生态环境学报Issue(9):1409-1417,9.

中国西南干旱对气候变暖的响应特征

The response of drought to climate warming in southwest in China

姚玉璧 1张强 2王劲松 1尚军林 1王莺 3石界 1韩兰英3

作者信息

  • 1. 中国气象局兰州干旱气象研究所 甘肃省干旱气候变化与减灾重点实验室 中国气象局干旱气候变化与减灾重点开放实验室,甘肃 兰州730020
  • 2. 甘肃省定西市气象局,甘肃 定西743000
  • 3. 甘肃省定西市气象局,甘肃 定西743000
  • 折叠

摘要

Abstract

Temporal variation, spatial distribution and sub-regional evolution characteristic of drought on southwestern China and their response characteristic to global climate warming were studied, used drought index analytical method which was based on relative moisture index, according to meteorological data between 1958 and 2012. It provide the scientific basis for coping climate change. Inverse distance weighting (IDW) method of ArcGIS system was used for analytical drawing of spatial data interpolation. The results showed that, annual drought of southwest China mainly distributed in northern Yunnan plateau, western Sichuan plateau and mountainous region of southwestern Sichuan. Drought region covered around 30%of the total region;among which, moderate drought region located in partly of the northern of Yunnan plateau and the western Sichuan plateau, covered around 11%of the total studied region;severe drought region located in northern Yunnan plateau and local area of western Sichuan plateau, covered around 5%; the drought share of 31.7% over the years on the station average. The main drought are winter and spring drought in the studying region, in which the average emergence of winter drought reached76.1%and spring drought reached 46.2%respectially. From 1958 to 2012, the negative absolute value of the relative moisture index increase in middle of Sichuan basin and mostly of Yunnan-Guizhou plateau, indicating the increase of drought level as well as drought intensity. Among which, the Negative absolute value of relative moisture had an increase tendency in most regions of the Yunnan-Guizhou plateau in Summer, autumn and winter, drought significantly enhanced; drought also increase in western Sichuan plateau and mountainous area of southwestern Sichuan in winter;Sichuan basin and north of Sichuan had an increase tendency of drought in autumn;the eastern part of Sichuan basin and Guizhou plateau also had an increase tendency in spring. The time series of index of annual drought has an obvious periodical oscillation of 3~4 a and 7~8 a;2009 is a mutation year of drought obviously strengthened. It is expected that the drought area will still expanding and the drought intensity will enhancing in the next few years in southwest China under the background global climate warming.

关键词

相对湿润度/干旱/气候变化/中国西南

Key words

relative moisture index/drought/climate change/southwest in China

分类

天文与地球科学

引用本文复制引用

姚玉璧,张强,王劲松,尚军林,王莺,石界,韩兰英..中国西南干旱对气候变暖的响应特征[J].生态环境学报,2014,(9):1409-1417,9.

基金项目

国家重点基础研究发展计划(973计划)项目(2013CB430200;2013CB430206);公益性行业(气象)科研专项(GYHY201106029;GYHY201006023);国家自然科学基金(41175081;41275118) (41175081;41275118)

生态环境学报

OA北大核心CSCDCSTPCD

1674-5906

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