Greenland decadal frontal ablation 2000 to 2020 ...

In Greenland, 87% of the glacierized area ends in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified for every glacier. We estimate frontal ablation of the 213 outlet and 537 peripheral glaciers of Greenland and find a total frontal ablation o...

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Main Authors: Kochtitzky, William, Copland, Luke, Hugonnet, Romain, Jiskoot, Hester, Khan, Abbas, King, Michalea, Millan, Romain, Morlighem, Mathieu, Noël, Brice
Format: Dataset
Language:unknown
Published: Canadian Cryospheric Information Network 2022
Subjects:
Online Access:https://dx.doi.org/10.21963/13272
https://www.polardata.ca/pdcsearch?doi_id=13272
id ftdatacite:10.21963/13272
record_format openpolar
spelling ftdatacite:10.21963/13272 2024-09-15T18:07:37+00:00 Greenland decadal frontal ablation 2000 to 2020 ... Kochtitzky, William Copland, Luke Hugonnet, Romain Jiskoot, Hester Khan, Abbas King, Michalea Millan, Romain Morlighem, Mathieu Noël, Brice 2022 https://dx.doi.org/10.21963/13272 https://www.polardata.ca/pdcsearch?doi_id=13272 unknown Canadian Cryospheric Information Network Dataset dataset 2022 ftdatacite https://doi.org/10.21963/13272 2024-07-03T10:33:55Z In Greenland, 87% of the glacierized area ends in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified for every glacier. We estimate frontal ablation of the 213 outlet and 537 peripheral glaciers of Greenland and find a total frontal ablation of 438.5 ± 7.2 Gt a-1 for 2000-2010 and 466.1 ± 6.2 Gt a-1 for 2010-2020. Ice discharge accounted for 90% and 92% of frontal ablation during these periods, respectively, while volume loss due to terminus retreat comprised the remainder. Only 15 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 89.5% and 91.1% of northern hemisphere frontal ablation for 2000-2010, and 2010-2020, respectively. Here, we provide the fluxgates, attributes (velocity and thickness) at points along the fluxgates, ... : The main goal of this dataset is to quantify the frontal ablation (mass loss due to iceberg calving, submarine frontal melting, and subaerial frontal melting and sublimation) of all marine-terminating glaciers in Greenland. This dataset was developed by combining velocity, thickness, and area change observations to compute the solid form of glacier mass loss for the first time. These data will help to close the glacier mass budgets in Greenland and are available for use in other studies. ... Dataset glacier Greenland Ice Sheet DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
description In Greenland, 87% of the glacierized area ends in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified for every glacier. We estimate frontal ablation of the 213 outlet and 537 peripheral glaciers of Greenland and find a total frontal ablation of 438.5 ± 7.2 Gt a-1 for 2000-2010 and 466.1 ± 6.2 Gt a-1 for 2010-2020. Ice discharge accounted for 90% and 92% of frontal ablation during these periods, respectively, while volume loss due to terminus retreat comprised the remainder. Only 15 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 89.5% and 91.1% of northern hemisphere frontal ablation for 2000-2010, and 2010-2020, respectively. Here, we provide the fluxgates, attributes (velocity and thickness) at points along the fluxgates, ... : The main goal of this dataset is to quantify the frontal ablation (mass loss due to iceberg calving, submarine frontal melting, and subaerial frontal melting and sublimation) of all marine-terminating glaciers in Greenland. This dataset was developed by combining velocity, thickness, and area change observations to compute the solid form of glacier mass loss for the first time. These data will help to close the glacier mass budgets in Greenland and are available for use in other studies. ...
format Dataset
author Kochtitzky, William
Copland, Luke
Hugonnet, Romain
Jiskoot, Hester
Khan, Abbas
King, Michalea
Millan, Romain
Morlighem, Mathieu
Noël, Brice
spellingShingle Kochtitzky, William
Copland, Luke
Hugonnet, Romain
Jiskoot, Hester
Khan, Abbas
King, Michalea
Millan, Romain
Morlighem, Mathieu
Noël, Brice
Greenland decadal frontal ablation 2000 to 2020 ...
author_facet Kochtitzky, William
Copland, Luke
Hugonnet, Romain
Jiskoot, Hester
Khan, Abbas
King, Michalea
Millan, Romain
Morlighem, Mathieu
Noël, Brice
author_sort Kochtitzky, William
title Greenland decadal frontal ablation 2000 to 2020 ...
title_short Greenland decadal frontal ablation 2000 to 2020 ...
title_full Greenland decadal frontal ablation 2000 to 2020 ...
title_fullStr Greenland decadal frontal ablation 2000 to 2020 ...
title_full_unstemmed Greenland decadal frontal ablation 2000 to 2020 ...
title_sort greenland decadal frontal ablation 2000 to 2020 ...
publisher Canadian Cryospheric Information Network
publishDate 2022
url https://dx.doi.org/10.21963/13272
https://www.polardata.ca/pdcsearch?doi_id=13272
genre glacier
Greenland
Ice Sheet
genre_facet glacier
Greenland
Ice Sheet
op_doi https://doi.org/10.21963/13272
_version_ 1810444999029948416