Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry

Pope, Smith, and Kohler glaciers, in the Amundsen Sea Embayment of West Antarctica, have experienced enhanced ocean-induced ice-shelf melt, glacier acceleration, ice thinning, and grounding line retreat in the past thirty years, in a glaciological setting with retrograde bedrock slopes conducive to...

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Main Authors: Milillo, Pietro, Rignot, Eric, Rizzoli, Paola, Scheuchl, Bernd, Mouginot, Jeremie, Bueso Bello, Jose Luis, Prats Iraola, Pau, Dini, Luigi
Format: Dataset
Language:unknown
Published: 2021
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Online Access:https://zenodo.org/record/5637468
https://doi.org/10.7280/D1B114
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:5637468 2023-05-15T13:23:59+02:00 Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry Milillo, Pietro Rignot, Eric Rizzoli, Paola Scheuchl, Bernd Mouginot, Jeremie Bueso Bello, Jose Luis Prats Iraola, Pau Dini, Luigi 2021-11-01 https://zenodo.org/record/5637468 https://doi.org/10.7280/D1B114 unknown https://zenodo.org/communities/dryad https://zenodo.org/record/5637468 https://doi.org/10.7280/D1B114 oai:zenodo.org:5637468 info:eu-repo/semantics/openAccess https://creativecommons.org/publicdomain/zero/1.0/legalcode info:eu-repo/semantics/other dataset 2021 ftzenodo https://doi.org/10.7280/D1B114 2023-03-10T18:55:46Z Pope, Smith, and Kohler glaciers, in the Amundsen Sea Embayment of West Antarctica, have experienced enhanced ocean-induced ice-shelf melt, glacier acceleration, ice thinning, and grounding line retreat in the past thirty years, in a glaciological setting with retrograde bedrock slopes conducive to marine ice sheet instability. Here we present observations of the grounding line retreat of these glaciers since 2014 using a constellation of interferometric radar satellites with a short revisit cycle combined with precision surface elevation data. We find that the glacier grounding lines develop spatially-variable, km-sized, tidally-induced migration zones. After correction for tidal effects, we detect a sustained pattern of retreat coincident with high melt rates of un-grounded ice, marked by episodes of more rapid retreat. In 2017, Pope Glacier retreated 3.5 km in 3.6 months, or 11.7 km/yr. In 2016-2018, Smith West retreated at 2 km/yr and Kohler at 1.3 km/yr. While the retreat slowed down in 2018-2020, these retreat rates are faster than anticipated by numerical models on yearly time scales. We hypothesize that the rapid retreat is caused by un-represented, vigorous ice-ocean interactions acting within newly-formed cavities at the ice-ocean boundary. This Dataset contains InSAR double difference interferograms over Pope, Smith and Kohler glaciers in the Amundsen Sea Embayment, West Antarctica. Data have been acquired by the COSMO-SkyMed constellation and cover the period 2016-2020. A shapefile with the mapped grounding lines is also included in this dataset. Additional dataset: Ice Thickness and height above flotation derived from Bed Machine Antarctica version 2020_06_18. Velocity map derived from Sentinel-1A/B Pixel Offsets for the year 2018-2019 Funding provided by: National Aeronautics and Space AdministrationCrossref Funder Registry ID: http://dx.doi.org/10.13039/100000104Award Number: 17-CRYO17-0025Funding provided by: National Aeronautics and Space AdministrationCrossref Funder Registry ID: ... Dataset Amundsen Sea Antarc* Antarctica Ice Sheet Ice Shelf West Antarctica Zenodo West Antarctica Amundsen Sea Pope Glacier ENVELOPE(-111.500,-111.500,-75.250,-75.250)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Pope, Smith, and Kohler glaciers, in the Amundsen Sea Embayment of West Antarctica, have experienced enhanced ocean-induced ice-shelf melt, glacier acceleration, ice thinning, and grounding line retreat in the past thirty years, in a glaciological setting with retrograde bedrock slopes conducive to marine ice sheet instability. Here we present observations of the grounding line retreat of these glaciers since 2014 using a constellation of interferometric radar satellites with a short revisit cycle combined with precision surface elevation data. We find that the glacier grounding lines develop spatially-variable, km-sized, tidally-induced migration zones. After correction for tidal effects, we detect a sustained pattern of retreat coincident with high melt rates of un-grounded ice, marked by episodes of more rapid retreat. In 2017, Pope Glacier retreated 3.5 km in 3.6 months, or 11.7 km/yr. In 2016-2018, Smith West retreated at 2 km/yr and Kohler at 1.3 km/yr. While the retreat slowed down in 2018-2020, these retreat rates are faster than anticipated by numerical models on yearly time scales. We hypothesize that the rapid retreat is caused by un-represented, vigorous ice-ocean interactions acting within newly-formed cavities at the ice-ocean boundary. This Dataset contains InSAR double difference interferograms over Pope, Smith and Kohler glaciers in the Amundsen Sea Embayment, West Antarctica. Data have been acquired by the COSMO-SkyMed constellation and cover the period 2016-2020. A shapefile with the mapped grounding lines is also included in this dataset. Additional dataset: Ice Thickness and height above flotation derived from Bed Machine Antarctica version 2020_06_18. Velocity map derived from Sentinel-1A/B Pixel Offsets for the year 2018-2019 Funding provided by: National Aeronautics and Space AdministrationCrossref Funder Registry ID: http://dx.doi.org/10.13039/100000104Award Number: 17-CRYO17-0025Funding provided by: National Aeronautics and Space AdministrationCrossref Funder Registry ID: ...
format Dataset
author Milillo, Pietro
Rignot, Eric
Rizzoli, Paola
Scheuchl, Bernd
Mouginot, Jeremie
Bueso Bello, Jose Luis
Prats Iraola, Pau
Dini, Luigi
spellingShingle Milillo, Pietro
Rignot, Eric
Rizzoli, Paola
Scheuchl, Bernd
Mouginot, Jeremie
Bueso Bello, Jose Luis
Prats Iraola, Pau
Dini, Luigi
Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
author_facet Milillo, Pietro
Rignot, Eric
Rizzoli, Paola
Scheuchl, Bernd
Mouginot, Jeremie
Bueso Bello, Jose Luis
Prats Iraola, Pau
Dini, Luigi
author_sort Milillo, Pietro
title Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
title_short Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
title_full Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
title_fullStr Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
title_full_unstemmed Dataset for: Fast retreat of Pope, Smith, and Kohler glaciers in West Antarctica observed by satellite interferometry
title_sort dataset for: fast retreat of pope, smith, and kohler glaciers in west antarctica observed by satellite interferometry
publishDate 2021
url https://zenodo.org/record/5637468
https://doi.org/10.7280/D1B114
long_lat ENVELOPE(-111.500,-111.500,-75.250,-75.250)
geographic West Antarctica
Amundsen Sea
Pope Glacier
geographic_facet West Antarctica
Amundsen Sea
Pope Glacier
genre Amundsen Sea
Antarc*
Antarctica
Ice Sheet
Ice Shelf
West Antarctica
genre_facet Amundsen Sea
Antarc*
Antarctica
Ice Sheet
Ice Shelf
West Antarctica
op_relation https://zenodo.org/communities/dryad
https://zenodo.org/record/5637468
https://doi.org/10.7280/D1B114
oai:zenodo.org:5637468
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.7280/D1B114
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