Articles | Volume 13, issue 11
https://doi.org/10.5194/tc-13-2977-2019
https://doi.org/10.5194/tc-13-2977-2019
Research article
 | 
13 Nov 2019
Research article |  | 13 Nov 2019

Recent glacier and lake changes in High Mountain Asia and their relation to precipitation changes

Désirée Treichler, Andreas Kääb, Nadine Salzmann, and Chong-Yu Xu

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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
AR by Désirée Treichler on behalf of the Authors (14 May 2019)  Author's response   Manuscript 
ED: Reconsider after major revisions (31 May 2019) by Bert Wouters
ED: Referee Nomination & Report Request started (06 Jun 2019) by Bert Wouters
RR by Anonymous Referee #2 (28 Jun 2019)
ED: Publish subject to minor revisions (review by editor) (08 Aug 2019) by Bert Wouters
AR by Désirée Treichler on behalf of the Authors (16 Aug 2019)  Author's response   Manuscript 
ED: Publish as is (05 Sep 2019) by Bert Wouters
AR by Désirée Treichler on behalf of the Authors (13 Sep 2019)  Manuscript 
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Short summary
Glacier growth such as that found on the Tibetan Plateau (TP) is counterintuitive in a warming world. Climate models and meteorological data are conflicting about the reasons for this glacier anomaly. We quantify the glacier changes in High Mountain Asia using satellite laser altimetry as well as the growth of over 1300 inland lakes on the TP. Our study suggests that increased summer precipitation is likely the largest contributor to the recently observed increases in glacier and lake masses.