Low-frequency variability of terrestrial water budget in China using GRACE satellite measurements from 2003 to 2010

Mass variations in terrestrial water storage (TWS) obtained from eight years of satellite data from the Gravity Recovery and Climate Experiment (GRACE) are used to describe low frequency TWS through Empirical Orthogonal Function (EOF) analysis. Results of the second seasonal EOF mode show the influe...

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Bibliographic Details
Published in:Geodesy and Geodynamics
Main Authors: Kaixuan Kang, Hui Li, Peng Peng, Zhengbo Zou
Format: Article in Journal/Newspaper
Language:English
Published: KeAi Communications Co., Ltd. 2015
Subjects:
Online Access:https://doi.org/10.1016/j.geog.2015.12.001
https://doaj.org/article/c733247302d04bc49af56bc3f2e97d29
Description
Summary:Mass variations in terrestrial water storage (TWS) obtained from eight years of satellite data from the Gravity Recovery and Climate Experiment (GRACE) are used to describe low frequency TWS through Empirical Orthogonal Function (EOF) analysis. Results of the second seasonal EOF mode show the influence of the Meiyu season. Annual variability is clearly shown in the precipitation distribution over China, and two new patterns of interannual variability are presented for the first time from observations, where two periods of abrupt acceleration are seen in 2004 and 2008. GRACE successfully measures drought events in southern China, and in this respect, an association with the Arctic Oscillation and El Nino-Southern Oscillation is discussed. This study demonstrates the unique potential of satellite gravity measurements in monitoring TWS variations and large-scale severe drought in China.