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利用重力卫星观测资料解算中国大陆水储量变化
  • 期刊名称:大地测量与地球动力学,Vol. 27, No.3,P68-71,2007.
  • 时间:0
  • 分类:P333[天文地球—水文科学;水利工程—水文学及水资源;天文地球—地球物理学]
  • 作者机构:[1]中国科学院测量与地球物理研究所,武汉 430077, [2]中国科学院研究生院,北京 100039
  • 相关基金:国家自然科学基金(40574035);中国科学院资源环境领域野外台站研究基金(40474029).致谢 感谢陈剑利博士提供CPC水文模式数据!
  • 相关项目:利用卫星重力、测高和海洋资料研究海平面对大气压变化的响应
中文摘要:

利用GRACE重力卫星2002年4月~2004年7月共计20个月的时变重力场数据,反演了中国大陆空间大尺度陆地水储量变化,并将该结果与美国气候预测中心(CPC)的全球水文模式结果进行了比较.结果显示:GRACE的结果与水文模式结果在大多数区域符合得相当好:在西藏、西南和华南地区,水储量季节性变化的幅值达到12~14 cm;在华东、华中、西北东部地区,水储量季节性变化的幅度一般在8 cm左右;在新疆地区,水储量季节性变化很小.而在华北、东北地区,GRACE的结果与模式结果存在较大差别.

英文摘要:

The variations of water storage at large space scales in Chinese mainland are in,versed by use of 20- month GRACE gravity field solutions (from April 2002 to July 2004). Chinese mainland is divided into 8 major typical regions, the monthly variations of water storage in each region are calculated respectively, and then the results are compared with that derived from the NOAA' s CPC ( Climate Prediction Center) hydrologic model. The comparison results show good consistencies in most regions: in Tibet, Southwest and South China, the amplitude of annual variations in water storage are about 12 - 14 cm, the maximum and minimum values appear in September and April respectively; and there are variations of about 8cm in East & Central China and the eastern part of Southwest China,in Xinjiang area, the variation is obvious. However, in North & Northeast China, there are obvious differences between the GRACE and CPC modeled results.

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