Journal cover Journal topic
Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 4.936 IF 4.936
  • IF 5-year value: 5.615 IF 5-year
    5.615
  • CiteScore value: 4.94 CiteScore
    4.94
  • SNIP value: 1.612 SNIP 1.612
  • IPP value: 4.70 IPP 4.70
  • SJR value: 2.134 SJR 2.134
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 107 Scimago H
    index 107
  • h5-index value: 63 h5-index 63
Volume 20, issue 1
Hydrol. Earth Syst. Sci., 20, 571–587, 2016
https://doi.org/10.5194/hess-20-571-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 20, 571–587, 2016
https://doi.org/10.5194/hess-20-571-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

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

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

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
Publications Copernicus
Download
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.
Spatiotemporal SWC was decomposed into into three terms (spatial forcing, temporal forcing, and...
Citation