Closing Greenland's Mass Balance:Frontal Ablation of Every Greenlandic Glacier From 2000 to 2020

In Greenland, 87% of the glacierized area terminates in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified. Using measurements and models we calculate frontal ablation of Greenland's 213 outlet and 537 peripheral glaciers and find a total...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Kochtitzky, William, Copland, Luke, King, Michalea, Hugonnet, Romain, Jiskoot, Hester, Morlighem, Mathieu, Millan, Romain, Khan, Shfaqat Abbas, Noël, Brice
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/a6a5f12b-ba59-46ed-b023-e33643dea287
https://doi.org/10.1029/2023GL104095
https://backend.orbit.dtu.dk/ws/files/336026495/Geophysical_Research_Letters_-_2023_-_Kochtitzky.pdf
Description
Summary:In Greenland, 87% of the glacierized area terminates in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified. Using measurements and models we calculate frontal ablation of Greenland's 213 outlet and 537 peripheral glaciers and find a total frontal ablation of 481.8 ± 24.0 for 2000–2010 and 510.2 ± 18.6 Gt a −1 for 2010–2020. Ice discharge accounted for ∼90% of frontal ablation during both periods, while mass loss due to terminus retreat comprised the remainder. Only 16 glaciers were responsible for the majority (>50%) of frontal ablation from 2010 to 2020. These estimates, along with the climatic-basal balance, allow for a more complete accounting of Greenland Ice Sheet and peripheral glacier mass balance. In total, Greenland accounted for ∼90% of Northern Hemisphere frontal ablation for 2000–2010 and 2010–2020.