Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica

Supraglacial lakes on Antarctic ice shelves can have far-reaching implications for ice-sheet stability, highlighting the need to understand their dynamics, controls and role in the ice-sheet mass budget. We combine a detailed satellite-based record of seasonal lake evolution in Dronning Maud Land wi...

Full description

Saved in:
Bibliographic Details
Main Authors: Anirudha Mahagaonkar, Geir Moholdt, Quentin Glaude, Thomas Vikhamar Schuler
Format: Article
Language:English
Published: Cambridge University Press 2024-01-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143024000662/type/journal_article
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1841526422249668608
author Anirudha Mahagaonkar
Geir Moholdt
Quentin Glaude
Thomas Vikhamar Schuler
author_facet Anirudha Mahagaonkar
Geir Moholdt
Quentin Glaude
Thomas Vikhamar Schuler
author_sort Anirudha Mahagaonkar
collection DOAJ
description Supraglacial lakes on Antarctic ice shelves can have far-reaching implications for ice-sheet stability, highlighting the need to understand their dynamics, controls and role in the ice-sheet mass budget. We combine a detailed satellite-based record of seasonal lake evolution in Dronning Maud Land with a high-resolution simulation from the regional climate model Modèle Atmosphérique Régional to identify drivers of lake variability between 2014 and 2021. Correlations between summer lake extents and climate parameters reveal complex relationships that vary both in space and time. Shortwave radiation contributes positively to the energy budget during summer melt seasons, but summers with enhanced longwave radiation are more prone to surface melting and ponding, which is further enhanced by advected heat from summer precipitation. In contrast, previous winter precipitation has a negative effect on summer lake extents, presumably by increasing albedo and pore space, delaying the accumulation of meltwater. Downslope katabatic or föhn winds promote ponding around the grounding zones of some ice shelves. At a larger scale, we find that summers during periods of negative southern annular mode are associated with increased ponding in Dronning Maud Land. The high variability in seasonal lake extents indicates that these ice shelves are highly sensitive to future warming or intensified extreme events.
format Article
id doaj-art-622e4aaac3af40e9815b44d41a06e82a
institution Kabale University
issn 0022-1430
1727-5652
language English
publishDate 2024-01-01
publisher Cambridge University Press
record_format Article
series Journal of Glaciology
spelling doaj-art-622e4aaac3af40e9815b44d41a06e82a2025-01-16T21:48:49ZengCambridge University PressJournal of Glaciology0022-14301727-56522024-01-017010.1017/jog.2024.66Supraglacial lake evolution and its drivers in Dronning Maud Land, East AntarcticaAnirudha Mahagaonkar0https://orcid.org/0000-0001-5013-3248Geir Moholdt1Quentin Glaude2Thomas Vikhamar Schuler3https://orcid.org/0000-0003-0972-3929Glaciology and Geology Section, Norwegian Polar Institute, Tromsø, Norway Department of Geosciences, University of Oslo, Oslo, NorwayGlaciology and Geology Section, Norwegian Polar Institute, Tromsø, NorwayLaboratory of Climatology, University of Liège, Liège, Belgium Centre Spatial de Liège, Laboratory of Signal Processing, University of Liège, Liège, BelgiumDepartment of Geosciences, University of Oslo, Oslo, NorwaySupraglacial lakes on Antarctic ice shelves can have far-reaching implications for ice-sheet stability, highlighting the need to understand their dynamics, controls and role in the ice-sheet mass budget. We combine a detailed satellite-based record of seasonal lake evolution in Dronning Maud Land with a high-resolution simulation from the regional climate model Modèle Atmosphérique Régional to identify drivers of lake variability between 2014 and 2021. Correlations between summer lake extents and climate parameters reveal complex relationships that vary both in space and time. Shortwave radiation contributes positively to the energy budget during summer melt seasons, but summers with enhanced longwave radiation are more prone to surface melting and ponding, which is further enhanced by advected heat from summer precipitation. In contrast, previous winter precipitation has a negative effect on summer lake extents, presumably by increasing albedo and pore space, delaying the accumulation of meltwater. Downslope katabatic or föhn winds promote ponding around the grounding zones of some ice shelves. At a larger scale, we find that summers during periods of negative southern annular mode are associated with increased ponding in Dronning Maud Land. The high variability in seasonal lake extents indicates that these ice shelves are highly sensitive to future warming or intensified extreme events.https://www.cambridge.org/core/product/identifier/S0022143024000662/type/journal_articleAntarctic glaciologyice/atmosphere interactionsice shelvesmelt – surfaceremote sensing
spellingShingle Anirudha Mahagaonkar
Geir Moholdt
Quentin Glaude
Thomas Vikhamar Schuler
Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
Journal of Glaciology
Antarctic glaciology
ice/atmosphere interactions
ice shelves
melt – surface
remote sensing
title Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
title_full Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
title_fullStr Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
title_full_unstemmed Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
title_short Supraglacial lake evolution and its drivers in Dronning Maud Land, East Antarctica
title_sort supraglacial lake evolution and its drivers in dronning maud land east antarctica
topic Antarctic glaciology
ice/atmosphere interactions
ice shelves
melt – surface
remote sensing
url https://www.cambridge.org/core/product/identifier/S0022143024000662/type/journal_article
work_keys_str_mv AT anirudhamahagaonkar supraglaciallakeevolutionanditsdriversindronningmaudlandeastantarctica
AT geirmoholdt supraglaciallakeevolutionanditsdriversindronningmaudlandeastantarctica
AT quentinglaude supraglaciallakeevolutionanditsdriversindronningmaudlandeastantarctica
AT thomasvikhamarschuler supraglaciallakeevolutionanditsdriversindronningmaudlandeastantarctica