Brief communication: Firn data compilation reveals the evolution of the firn air content on the Greenland ice sheet

The firn covering the Greenland ice sheet interior can retain part of the surface melt, buffering the ice sheet’s contribution to sea level, but its characteristics are still little known. Using remote-sensing observations from 2000- 2017, we estimate that firn covers 1,405,500 ±17,250 km 2 of the i...

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Bibliographic Details
Main Authors: Vandecrux, Baptiste Robert Marcel, MacFerrin, Michael, Machguth, Horst, Colgan, William T., van As, Dirk, Heilig, Achim, Stevens, C. Max, Charalampidis, Charalampos, Fausto, Robert S., Morris, Elizabeth M., Mosley-Thompson, Ellen, Koenig, Lora, Montgomery, Lynn N., Miège, Clément, Simonsen, Sebastian Bjerregaard, Ingeman-Nielsen, Thomas, Box, Jason E.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Greenland
Ice Sheet
The Cryosphere
The Cryosphere Discussions
Online Access:https://orbit.dtu.dk/en/publications/a1ce3529-5ddb-4c9e-8bd4-adcd21d520cb
https://doi.org/10.5194/tc-2018-172
https://backend.orbit.dtu.dk/ws/files/166661300/Untitled.pdf
https://backend.orbit.dtu.dk/ws/files/190069462/tc_13_845_2019.pdf
Description
Summary:The firn covering the Greenland ice sheet interior can retain part of the surface melt, buffering the ice sheet’s contribution to sea level, but its characteristics are still little known. Using remote-sensing observations from 2000- 2017, we estimate that firn covers 1,405,500 ±17,250 km 2 of the ice sheet. We present 344 firn-core-derived observations of the top 10 m firn air content (FAC 10 ), indicative of the firn’s meltwater retention capacity. FAC 10 remained stable in the coldest 74% of the firn area during 1953-2017, while FAC 10 decreased in the warmest and driest 12% of the firn area between 1997-2008 and 2011-2017, resulting in a loss of 180 ±78 km 3 (-26 ±11%) of air from the near-surface firn.

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