Simulations of subglacial discharge and submarine melting during tidewater glacier retreat

Please open README.pdf for instructions on how to use this data package. To first order, subglacial discharge depends on climate, which determines precipitation fluxes and glacier mass balance, and the rate of glacier volume change. For tidewater glaciers, large and rapid changes in glacier volume c...

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Bibliographic Details
Main Authors: Amundson, Jason, Carroll, Dustin
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2017
Subjects:
Tidewater
Online Access:https://dx.doi.org/10.18739/a25t3g08s
https://arcticdata.io/catalog/view/doi:10.18739/A25T3G08S
id ftdatacite:10.18739/a25t3g08s
record_format openpolar
spelling ftdatacite:10.18739/a25t3g08s 2023-05-15T18:33:02+02:00 Simulations of subglacial discharge and submarine melting during tidewater glacier retreat Amundson, Jason Carroll, Dustin 2017 text/xml https://dx.doi.org/10.18739/a25t3g08s https://arcticdata.io/catalog/view/doi:10.18739/A25T3G08S en eng NSF Arctic Data Center dataset Dataset 2017 ftdatacite https://doi.org/10.18739/a25t3g08s 2021-11-05T12:55:41Z Please open README.pdf for instructions on how to use this data package. To first order, subglacial discharge depends on climate, which determines precipitation fluxes and glacier mass balance, and the rate of glacier volume change. For tidewater glaciers, large and rapid changes in glacier volume can occur independent of climate change due to strong glacier dynamic feedbacks. Using an idealized tidewater glacier model, we show that these feedbacks produce secular variations in subglacial discharge and submarine melting that are influenced by subglacial topography. Dataset Tidewater DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Please open README.pdf for instructions on how to use this data package. To first order, subglacial discharge depends on climate, which determines precipitation fluxes and glacier mass balance, and the rate of glacier volume change. For tidewater glaciers, large and rapid changes in glacier volume can occur independent of climate change due to strong glacier dynamic feedbacks. Using an idealized tidewater glacier model, we show that these feedbacks produce secular variations in subglacial discharge and submarine melting that are influenced by subglacial topography.
format Dataset
author Amundson, Jason
Carroll, Dustin
spellingShingle Amundson, Jason
Carroll, Dustin
Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
author_facet Amundson, Jason
Carroll, Dustin
author_sort Amundson, Jason
title Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
title_short Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
title_full Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
title_fullStr Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
title_full_unstemmed Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
title_sort simulations of subglacial discharge and submarine melting during tidewater glacier retreat
publisher NSF Arctic Data Center
publishDate 2017
url https://dx.doi.org/10.18739/a25t3g08s
https://arcticdata.io/catalog/view/doi:10.18739/A25T3G08S
genre Tidewater
genre_facet Tidewater
op_doi https://doi.org/10.18739/a25t3g08s
_version_ 1766217287171309568

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