Articles | Volume 24, issue 12
Hydrol. Earth Syst. Sci., 24, 5937–5951, 2020
https://doi.org/10.5194/hess-24-5937-2020

Special issue: Data acquisition and modelling of hydrological, hydrogeological...

Hydrol. Earth Syst. Sci., 24, 5937–5951, 2020
https://doi.org/10.5194/hess-24-5937-2020

Research article 16 Dec 2020

Research article | 16 Dec 2020

Simulation analysis of local land atmosphere coupling in rainy season over a typical underlying surface in the Tibetan Plateau

Genhou Sun et al.

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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 revisions (further review by editor and referees) (27 Sep 2020) by Insa Neuweiler
AR by Genhou SUN on behalf of the Authors (08 Oct 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Oct 2020) by Insa Neuweiler
RR by Anonymous Referee #2 (26 Oct 2020)
RR by Anonymous Referee #1 (05 Nov 2020)
ED: Publish as is (07 Nov 2020) by Insa Neuweiler
AR by Genhou SUN on behalf of the Authors (08 Nov 2020)  Author's response    Manuscript
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Short summary
We investigate the influence of soil conditions on the planetary boundary layer (PBL) thermodynamics and convective cloud formations over a typical underlying surface, based on a series of simulations on a sunny day in the Tibetan Plateau, using the Weather Research and Forecasting (WRF) model. The real-case simulation and sensitivity simulations indicate that the soil moisture could have a strong impact on PBL thermodynamics, which may be favorable for the convective cloud formations.