Articles | Volume 24, issue 8
https://doi.org/10.5194/hess-24-3881-2020
https://doi.org/10.5194/hess-24-3881-2020
Research article
 | 
04 Aug 2020
Research article |  | 04 Aug 2020

Do surface lateral flows matter for data assimilation of soil moisture observations into hyperresolution land models?

Yohei Sawada

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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: Publish subject to minor revisions (further review by editor) (21 Jun 2020) by Alberto Guadagnini
AR by Yohei Sawada on behalf of the Authors (29 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (04 Jul 2020) by Alberto Guadagnini
AR by Yohei Sawada on behalf of the Authors (06 Jul 2020)  Manuscript 
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Short summary
Hydrologic data assimmilation is the area in which methods to integrate hydrological models and observations are investigated. Recently, hydrological or land models have been increasing their complexity, with very high spatial resolution. However, it is unclear that the current data assimilation method can directly be applied to those hyperresolution models, so that I investigated the applicability and limitation of the existing method by minimalistic numerical experiments.