干旱区研究

干旱区研究 ›› 2013, Vol. 30 ›› Issue (3): 404-411.

• 水土资源 • 上一篇    下一篇

利用GRACE重力卫星监测新疆天山山区水储量时空变化

许民1,2, 叶柏生1,2, 赵求东2, 王建2   

  1. 1. 冰冻圈科学国家重点实验室，甘肃 兰州 730000； 2. 中国科学院寒区旱区环境与工程研究所，甘肃 兰州 730000
  • 收稿日期:2012-05-07 修回日期:2012-06-27 出版日期:2013-05-15 发布日期:2013-05-16
  • 作者简介:许民（1984-），男，博士研究生，主要从事3S技术与寒区旱区水文水资源研究. E-mail： xumin@126.com
  • 基金资助:

    国家自然科学基金重点项目(41130638，41030527，41130641）；国家自然科学青年基金（41001039,41201025）；中国科学院寒区旱区环境与工程研究所青年人才基金项目（51Y251A61）共同资助

Spatiotemporal Change of Water Reserves in the Tianshan Mountains, Xinjiang Based on GRACE

 XU  Min1,2, YE  Bai-Sheng1,2, ZHAO  Qiu-Dong2, WANG  Jian2   

  1. 1. State Key Laboratory of Cryophereic Science, Cold and Arid Regions Environmental and Engineering Research Institute, 
    Chinese Academy of Sciences, Lanzhou 730000,China;  2. Cold and Arid Regions Environmental and 
    Enginee3ring Research Institute, Chinese Academy of Sciences,  Lanzhou 730000, China
  • Received:2012-05-07 Revised:2012-06-27 Online:2013-05-15 Published:2013-05-16

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摘要： 利用经过高斯平滑滤波处理的2003年1月至2010年12月逐月的GRACE卫星时变重力场数据，反演得到新疆天山山区水储量变化,其空间分辨率为1°×1°，结合同时间段该区域31个国家气象台站逐月降水资料，采用趋势分析方法，研究天山山区近8 a来的水储量时空变化特征。结果表明：天山山区水储量变化具有明显的空间差异性，总体表现为东、西部多，中部少的空间分布格局。在时间上，水储量变化与降水具有明显的季节性变化规律，两者变化过程基本一致。天山山区平均水储量变化趋势的年内分布总体上1—12月呈递增变化；1—3月为负增长，最大负增长为21.7 mm•a-1,出现在2月；4—12月呈正增长，最大月份出现在11月，增长趋势达到29.9 mm•a-1。水储量变化增加的主要原因是天山山区近几年夏季降水有所增加造成的。2003—2010年天山山区水储量变化总体上呈逐年下降趋势，平均每月下降速度为4.8 mm，8 a间水储量变化减少约13×108 m3，其主要原因是由于气候转暖、冰川消融加速、山前绿洲灌溉及生活用水量增加，导致山区水储量变化减少。

关键词: GRACE卫星, 水储量变化, 降水, 时空分布, 天山山区, 新疆

Abstract: Change of the volume of water reserves in the Tianshan Mountains was analyzed using the monthly gravity field data derived from GRACE satellite with Gaussian filter during the period from 2003 to 2010, and the spatial resolution was 1°×1°. Trend analysis was used to analyze the spatiotemporal variation trend of water reserves in the Tianshan Mountains in recent 8 years based on the monthly precipitation data observed by 31 state meteorological stations. Results showed that there was a significant spatial variation of water reserves in the Tianshan Mountains, the volume of water reserves in the eastern and western parts of the mountains was higher than that in the central part. Temporally, there was an obvious seasonal variation of water reserves and precipitation, and their change trends were similar. The growth of water reserves in the mountains was negative during the period from January to March, its minimum value, -21.7 mm•a-1, occurred in February. The growth of water reserves was positive during the period from April to December, and its maximum value, 29.9 mm•a-1, occurred in November. However, the volume of water reserves in the Tianshan Mountains was holistically in a decrease trend during the period from 2003 to 2010, it was decreased by 13×108 m3 in recent 8 years, and its average monthly decrease was 4.8 mm. Reduction of water reserves in the Tianshan Mountains was mainly caused by climate warming, aggravation of glacier melt and increase of the volume of irrigation water and domestic water in the piedmont oases.

Key words: GRACE satellite, water reserves, precipitation, spatiotemporal distribution, Tianshan Mountains, Xinjiang