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12~14cm;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8cm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。
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.
出处
《大地测量与地球动力学》
CSCD
北大核心
2007年第3期68-71,共4页
Journal of Geodesy and Geodynamics
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)
关键词
GRACE
时变重力场
陆地水储量
水文模式
大地水准面
GRACE( Gravity Recovery and Climate Experiment), temporal gravity, land water storage, hydrology model, geoid