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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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (17 Sep 2015) by Theresa Blume
AR by Wei Hu on behalf of the Authors (20 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Oct 2015) by Theresa Blume
RR by Anonymous Referee #2 (17 Nov 2015)
RR by Anonymous Referee #1 (22 Nov 2015)
ED: Publish subject to minor revisions (Editor review) (07 Dec 2015) by Theresa Blume
AR by Anne Brekerbohm on behalf of the Authors (18 Dec 2015)  Author's response    Manuscript
ED: Publish subject to technical corrections (17 Jan 2016) by Theresa Blume
AR by Wei Hu on behalf of the Authors (20 Jan 2016)  Author's response    Manuscript
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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.