Articles | Volume 22, issue 3
https://doi.org/10.5194/hess-22-1811-2018
https://doi.org/10.5194/hess-22-1811-2018
Research article
 | 
13 Mar 2018
Research article |  | 13 Mar 2018

On the use of the GRACE normal equation of inter-satellite tracking data for estimation of soil moisture and groundwater in Australia

Natthachet Tangdamrongsub, Shin-Chan Han, Mark Decker, In-Young Yeo, and Hyungjun Kim

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 (further review by Editor and Referees) (10 Sep 2017) by Louise Slater
AR by Natthachet Tangdamrongsub on behalf of the Authors (17 Oct 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (20 Oct 2017) by Louise Slater
RR by Anonymous Referee #2 (16 Nov 2017)
RR by Anonymous Referee #3 (08 Dec 2017)
RR by Anonymous Referee #1 (11 Dec 2017)
ED: Reconsider after major revisions (further review by editor and referees) (17 Dec 2017) by Louise Slater
AR by Anna Mirena Feist-Polner on behalf of the Authors (19 Jan 2018)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (31 Jan 2018) by Louise Slater
AR by Natthachet Tangdamrongsub on behalf of the Authors (01 Feb 2018)  Author's response    Manuscript
ED: Publish as is (02 Feb 2018) by Louise Slater
Download
Short summary
We present a new approach to improve the water storage estimate. Our approach combines GRACE's raw data (least-squares normal equation) with the results from the Community Atmosphere Land Exchange (CABLE) model. No post-processing filter is applied to GRACE data, and the full GRACE signal and error information are exploited. The approach is applied over 10 Australian river basins, and the evident improvement of the water storage estimate, particularly groundwater component, is clearly observed.