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: Jason Amundson, Dustin Carroll
Format: Dataset
Language:unknown
Published: Arctic Data Center 2017
Subjects:
glacier
glaciers
Tidewater
Alaska
Online Access:https://doi.org/10.18739/A21K1Q
id dataone:doi:10.18739/A21K1Q
record_format openpolar
spelling dataone:doi:10.18739/A21K1Q 2024-06-03T18:46:50+00:00 Simulations of subglacial discharge and submarine melting during tidewater glacier retreat Jason Amundson Dustin Carroll Southeast Alaska ENVELOPE(-132.3417,-132.3417,56.85,56.85) BEGINDATE: 2017-01-01T00:00:00Z ENDDATE: 2017-01-01T00:00:00Z 2017-11-14T00:00:00Z https://doi.org/10.18739/A21K1Q unknown Arctic Data Center Dataset 2017 dataone:urn:node:ARCTIC https://doi.org/10.18739/A21K1Q 2024-06-03T18:10:36Z 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 glacier glaciers Tidewater Alaska Arctic Data Center (via DataONE) ENVELOPE(-132.3417,-132.3417,56.85,56.85)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
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 Jason Amundson
Dustin Carroll
spellingShingle Jason Amundson
Dustin Carroll
Simulations of subglacial discharge and submarine melting during tidewater glacier retreat
author_facet Jason Amundson
Dustin Carroll
author_sort Jason Amundson
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 Arctic Data Center
publishDate 2017
url https://doi.org/10.18739/A21K1Q
op_coverage Southeast Alaska
ENVELOPE(-132.3417,-132.3417,56.85,56.85)
BEGINDATE: 2017-01-01T00:00:00Z ENDDATE: 2017-01-01T00:00:00Z
long_lat ENVELOPE(-132.3417,-132.3417,56.85,56.85)
genre glacier
glaciers
Tidewater
Alaska
genre_facet glacier
glaciers
Tidewater
Alaska
op_doi https://doi.org/10.18739/A21K1Q
_version_ 1800871797491499008

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