Sentinel-1 detection of perennial firn aquifers in the Antarctic Peninsula

In recent years, the existence of perennial firn aquifers in the Antarctic Peninsula (AP) has been confirmed by in situ observations. Previous studies have suggested that these subsurface aquifers, together with meltwater ponds at the surface, provide a reservoir of liquid water to feed propagating...

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Bibliographic Details
Main Authors: Buth, Lena G., Di Biase, Valeria, Kuipers Munneke, Peter, Lhermitte, Stef, Veldhuijsen, Sanne B. M., de Roda Husman, Sophie, van den Broeke, Michiel R., Wouters, Bert
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
article
Verlagsveröffentlichung
Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
Ice Shelves
Online Access:https://doi.org/10.5194/egusphere-2023-2000
https://noa.gwlb.de/receive/cop_mods_00069075
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067477/egusphere-2023-2000.pdf
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-2000/egusphere-2023-2000.pdf
Description
Summary:In recent years, the existence of perennial firn aquifers in the Antarctic Peninsula (AP) has been confirmed by in situ observations. Previous studies have suggested that these subsurface aquifers, together with meltwater ponds at the surface, provide a reservoir of liquid water to feed propagating fractures, promoting hydrofracture-driven ice-shelf disintegration. This study maps perennial firn aquifers in the AP from space using C-band Synthetic Aperture Radar imagery from ESA's Sentinel-1 (S1) mission. With these observations, we detect firn aquifers at 1 km × 1 km resolution, for the period 2017 to 2020. Existing methods, that use S1 data and rely on a backscatter intensity difference threshold approach, are prone to misclassify late-melt events as aquifers, when applied to the AP. Therefore, we have developed and evaluated a new approach that is better suited to the Antarctic environment. The new method exploits the characteristic, gradual backscatter increase during the (partial) refreezing of the liquid water in the firn layer after the peak of the melt season. Most firn aquifers are detected in the north and northwest of the AP, as well as on the Wilkins and George VI ice shelves. Aquifer locations detected with the present methodology agree with in situ observations and with model simulations of firn water content.

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