An estimate of global glacier volume

I assess the feasibility of using multivariate scaling relationships to estimate glacier volume from glacier inventory data. Scaling laws are calibrated against volume observations optimized for the specific purpose of estimating total global glacier ice volume. I find that adjustments for continent...

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Published in:The Cryosphere
Main Author: Grinsted, A.
Format: Other/Unknown Material
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-7-141-2013
https://tc.copernicus.org/articles/7/141/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:tc16552 2023-05-15T16:40:45+02:00 An estimate of global glacier volume Grinsted, A. 2018-09-27 info:eu-repo/semantics/application/pdf https://doi.org/10.5194/tc-7-141-2013 https://tc.copernicus.org/articles/7/141/2013/ eng eng info:eu-repo/grantAgreement/EC/FP7/246815 doi:10.5194/tc-7-141-2013 https://tc.copernicus.org/articles/7/141/2013/ info:eu-repo/semantics/openAccess eISSN: 1994-0424 info:eu-repo/semantics/Text 2018 ftcopernicus https://doi.org/10.5194/tc-7-141-2013 2020-07-20T16:25:35Z I assess the feasibility of using multivariate scaling relationships to estimate glacier volume from glacier inventory data. Scaling laws are calibrated against volume observations optimized for the specific purpose of estimating total global glacier ice volume. I find that adjustments for continentality and elevation range improve skill of area–volume scaling. These scaling relationships are applied to each record in the Randolph Glacier Inventory, which is the first globally complete inventory of glaciers and ice caps. I estimate that the total volume of all glaciers in the world is 0.35 ± 0.07 m sea level equivalent, including ice sheet peripheral glaciers. This is substantially less than a recent state-of-the-art estimate. Area–volume scaling bias issues for large ice masses, and incomplete inventory data are offered as explanations for the difference. Other/Unknown Material Ice Sheet Copernicus Publications: E-Journals The Cryosphere 7 1 141 151
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description I assess the feasibility of using multivariate scaling relationships to estimate glacier volume from glacier inventory data. Scaling laws are calibrated against volume observations optimized for the specific purpose of estimating total global glacier ice volume. I find that adjustments for continentality and elevation range improve skill of area–volume scaling. These scaling relationships are applied to each record in the Randolph Glacier Inventory, which is the first globally complete inventory of glaciers and ice caps. I estimate that the total volume of all glaciers in the world is 0.35 ± 0.07 m sea level equivalent, including ice sheet peripheral glaciers. This is substantially less than a recent state-of-the-art estimate. Area–volume scaling bias issues for large ice masses, and incomplete inventory data are offered as explanations for the difference.
format Other/Unknown Material
author Grinsted, A.
spellingShingle Grinsted, A.
An estimate of global glacier volume
author_facet Grinsted, A.
author_sort Grinsted, A.
title An estimate of global glacier volume
title_short An estimate of global glacier volume
title_full An estimate of global glacier volume
title_fullStr An estimate of global glacier volume
title_full_unstemmed An estimate of global glacier volume
title_sort estimate of global glacier volume
publishDate 2018
url https://doi.org/10.5194/tc-7-141-2013
https://tc.copernicus.org/articles/7/141/2013/
genre Ice Sheet
genre_facet Ice Sheet
op_source eISSN: 1994-0424
op_relation info:eu-repo/grantAgreement/EC/FP7/246815
doi:10.5194/tc-7-141-2013
https://tc.copernicus.org/articles/7/141/2013/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-7-141-2013
container_title The Cryosphere
container_volume 7
container_issue 1
container_start_page 141
op_container_end_page 151
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