Articles | Volume 15, issue 5
https://doi.org/10.5194/tc-15-2273-2021
https://doi.org/10.5194/tc-15-2273-2021
Research article
 | 
18 May 2021
Research article |  | 18 May 2021

The surface energy balance in a cold and arid permafrost environment, Ladakh, Himalayas, India

John Mohd Wani, Renoj J. Thayyen, Chandra Shekhar Prasad Ojha, and Stephan Gruber

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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) (26 Oct 2020) by Christian Hauck
AR by Renoj Thayyen (deceased) on behalf of the Authors (21 Dec 2020)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (31 Dec 2020) by Christian Hauck
RR by Giacomo Bertoldi (13 Jan 2021)
ED: Publish subject to minor revisions (review by editor) (17 Mar 2021) by Christian Hauck
AR by Renoj Thayyen (deceased) on behalf of the Authors (22 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (02 Apr 2021) by Christian Hauck
AR by Renoj Thayyen (deceased) on behalf of the Authors (05 Apr 2021)
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Short summary
We study the surface energy balance from a cold-arid permafrost environment in the Indian Himalayan region. The GEOtop model was used for the modelling of surface energy balance. Our results show that the variability in the turbulent heat fluxes is similar to that reported from the seasonally frozen ground and permafrost regions of the Tibetan Plateau. Further, the low relative humidity could be playing a critical role in the surface energy balance and the permafrost processes.