Articles | Volume 25, issue 3
https://doi.org/10.5194/hess-25-1569-2021
https://doi.org/10.5194/hess-25-1569-2021
Research article
 | 
29 Mar 2021
Research article |  | 29 Mar 2021

The benefit of brightness temperature assimilation for the SMAP Level-4 surface and root-zone soil moisture analysis

Jianxiu Qiu, Jianzhi Dong, Wade T. Crow, Xiaohu Zhang, Rolf H. Reichle, and Gabrielle J. M. De Lannoy

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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 (further review by editor and referees) (23 Nov 2020) by Bob Su
AR by Jianxiu Qiu on behalf of the Authors (03 Dec 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (14 Dec 2020) by Bob Su
RR by Anonymous Referee #2 (23 Dec 2020)
RR by Anonymous Referee #1 (30 Dec 2020)
ED: Publish subject to revisions (further review by editor and referees) (19 Jan 2021) by Bob Su
AR by Jianxiu Qiu on behalf of the Authors (29 Jan 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (14 Feb 2021) by Bob Su
AR by Jianxiu Qiu on behalf of the Authors (19 Feb 2021)
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Short summary
The SMAP L4 dataset has been extensively used in hydrological applications. We innovatively use a machine learning method to analyze how the efficiency of the L4 data assimilation (DA) system is determined. It shows that DA efficiency is mainly related to Tb innovation, followed by error in precipitation forcing and microwave soil roughness. Since the L4 system can effectively filter out precipitation error, future development should focus on correctly specifying the SSM–RZSM coupling strength.