Firn air content changes on Antarctic ice shelves under three future warming scenarios

The Antarctic firn layer provides pore space in which an estimated 94 % to 96 % of the surface melt refreezes or is retained as liquid water. Future depletion of firn pore space by increased surface melt, densification and formation of low-permeability ice slabs can potentially lead to meltwater pon...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Veldhuijsen, Sanne B. M., Berg, Willem Jan, Kuipers Munneke, Peter, Broeke, Michiel R.
Format: Text
Language:English
Published: 2024
Subjects:
Antarctic
Antarctic Peninsula
Dronning Maud Land
Roi Baudouin
The Antarctic
Antarc*
Ice Shelf
Ice Shelves
Online Access:https://doi.org/10.5194/tc-18-1983-2024
https://tc.copernicus.org/articles/18/1983/2024/
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Summary:The Antarctic firn layer provides pore space in which an estimated 94 % to 96 % of the surface melt refreezes or is retained as liquid water. Future depletion of firn pore space by increased surface melt, densification and formation of low-permeability ice slabs can potentially lead to meltwater ponding, hydrofracturing and ice-shelf disintegration. Here, we investigate the 21st-century evolution of total firn air content (FAC) and accessible FAC (i.e. the pore space that meltwater can reach) across Antarctic ice shelves. We use the semi-empirical IMAU Firn Densification Model (IMAU-FDM) with an updated dynamical densification expression to cope with changing climate forcing. The firn model is forced by general circulation model output of the Community Earth System Model version 2 (CESM2) for three climate emission scenarios (SSP1-2.6, SSP2-4.5 and SSP5-8.5), dynamically downscaled to a 27 km horizontal resolution by the Regional Atmospheric Climate Model version 2.3p2 (RACMO2.3p2). To estimate accessible FAC, we prescribe a relationship between ice-slab thickness and permeability. In our simulations, ice shelves on the Antarctic Peninsula and the Roi Baudouin Ice Shelf in Dronning Maud Land are particularly vulnerable to total FAC depletion ( &gt; 50 % decrease by 2100), even for low-emission (SSP1-2.6) and intermediate-emission (SSP2-4.5) scenarios. In the high-emission (SSP5-8.5) scenario in particular, the formation of ice slabs further reduces accessible FAC on ice shelves with low accumulation rates (current rates of &lt; 500 mm w . e . yr - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="61pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="b4c8699b596706f7bf9110e998ba2dca"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-18-1983-2024-ie00001.svg" width="61pt" height="15pt" src="tc-18-1983-2024-ie00001.png"/> </svg:svg> ), including many East Antarctic ice shelves and the Filchner–Ronne, Ross, Pine Island and Larsen C ice shelves. These ...

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