Articles | Volume 16, issue 2
https://doi.org/10.5194/nhess-16-469-2016
https://doi.org/10.5194/nhess-16-469-2016
Research article
 | 
17 Feb 2016
Research article |  | 17 Feb 2016

Variations in water storage in China over recent decades from GRACE observations and GLDAS

X. Mo, J. J. Wu, Q. Wang, and H. Zhou

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Cited articles

Andersen, O. B., Seneviratne, S. I., Hinderer, J., and Viterbo, P.: GRACE-derived terrestrial water storage depletion associated with the 2003 European heat wave, Geophys. Res. Lett., 32, L18405, https://doi.org/10.1029/2005GL023574, 2005.
Betts, A. K., Chen, F., Mitchell, K., and Janjic, Z. I.: Assessment of the land surface and boundary layer models in two operational versions of the NCEP Eta model using FIFE data, Mon. Weather Rev., 125, 2896–2916, 1997.
Bonan, G. B., Oleson, K. W., Vertenstein, M., Levis, S., Zeng, X. B., Dai, Y. J., Dickinson, R. E., and Yang, Z. L.: The land surface climatology of the NCAR Land Surface Model coupled to the NCAR Community Climate Model, J. Climate, 11, 1307–1326, 1998.
Chen, F., Mitchell, K., Schaake, J., Xue, Y. K., Pan, H. L., Koren, V., Duan, Q. Y., Ek, M., and Betts, A.: Modeling of land-surface evaporation by four schemes and comparison with FIFE observations, J. Geophys. Res., 101, 7251–7268, 1996.
Chen, J. L., Wilson, C. R., Famiglietti, J. S., and Rodell, M.: Attenuation effect on seasonal basin-scale water storage changes from GRACE time-variable gravity, J. Geodesy., 81, 237–245, 2007.
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Short summary
GRACE provided a new perspective on the anomaly monitoring of water resources. In 2003–2013, TWS in China generally followed variations in annual precipitation; it decreased in northern basins and increased in the south. In the North China Plain, human activities might have interfered with TWS's response to climate; it kept decreasing until 2012. With grid-scaled TWS, small regions with significant increasing trends were also identified in Hoh Xil and the headstream region of the Yellow River.
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