Articles | Volume 20, issue 1
https://doi.org/10.5194/hess-20-571-2016
https://doi.org/10.5194/hess-20-571-2016
Research article
 | 
02 Feb 2016
Research article |  | 02 Feb 2016

Estimating spatially distributed soil water content at small watershed scales based on decomposition of temporal anomaly and time stability analysis

W. Hu and B. C. Si

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Short summary
Spatiotemporal SWC was decomposed into into three terms (spatial forcing, temporal forcing, and interactions between spatial and temporal forcing) for near surface and root zone; Empirical orthogonal function indicated that underlying patterns exist in the interaction term at small watershed scales; Estimation of spatially distributed SWC benefits from decomposition of the interaction term; The suggested decomposition of SWC with time stability analysis has potential in SWC downscaling.