Articles | Volume 14, issue 11
The Cryosphere, 14, 3811–3827, 2020
https://doi.org/10.5194/tc-14-3811-2020
The Cryosphere, 14, 3811–3827, 2020
https://doi.org/10.5194/tc-14-3811-2020

Research article 09 Nov 2020

Research article | 09 Nov 2020

Recent changes in pan-Antarctic region surface snowmelt detected by AMSR-E and AMSR2

Lei Zheng 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: Reconsider after major revisions (further review by editor and referees) (16 Sep 2019) by Stef Lhermitte
AR by Lei Zheng on behalf of the Authors (19 Sep 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Sep 2019) by Stef Lhermitte
ED: Reconsider after major revisions (further review by editor and referees) (27 Jan 2020) by Stef Lhermitte
AR by Lei Zheng on behalf of the Authors (25 May 2020)  Author's response    Manuscript
ED: Reconsider after major revisions (further review by editor and referees) (16 Jul 2020) by Stef Lhermitte
AR by Lei Zheng on behalf of the Authors (18 Aug 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (24 Sep 2020) by Stef Lhermitte
AR by Lei Zheng on behalf of the Authors (26 Sep 2020)  Author's response    Manuscript
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Short summary
Snowmelt plays a key role in mass and energy balance in polar regions. In this study, we report on the spatial and temporal variations in the surface snowmelt over the Antarctic sea ice and ice sheet (pan-Antarctic region) based on AMSR-E and AMSR2. Melt detection on sea ice is improved by excluding the effect of open water. The decline in surface snowmelt on the Antarctic ice sheet was very likely linked with the enhanced summer Southern Annular Mode.