Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes

The mass balance of glaciers and ice caps is sensitive to changing climate conditions. The mass changes derived in this study are determined from elevation changes derived measured by the Ice, Cloud, and land Elevation Satellite (ICESat) for the time period 2003–2009. Four methods, based on interpol...

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Published in:The Cryosphere
Main Authors: Nilsson, J., Sandberg Sørensen, L., Barletta, V. R., Forsberg, R.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-9-139-2015
https://tc.copernicus.org/articles/9/139/2015/
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spelling ftcopernicus:oai:publications.copernicus.org:tc22658 2023-05-15T14:58:41+02:00 Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes Nilsson, J. Sandberg Sørensen, L. Barletta, V. R. Forsberg, R. 2018-09-27 application/pdf https://doi.org/10.5194/tc-9-139-2015 https://tc.copernicus.org/articles/9/139/2015/ eng eng doi:10.5194/tc-9-139-2015 https://tc.copernicus.org/articles/9/139/2015/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-9-139-2015 2020-07-20T16:24:47Z The mass balance of glaciers and ice caps is sensitive to changing climate conditions. The mass changes derived in this study are determined from elevation changes derived measured by the Ice, Cloud, and land Elevation Satellite (ICESat) for the time period 2003–2009. Four methods, based on interpolation and extrapolation, are used to regionalize these elevation changes to areas without satellite coverage. A constant density assumption is then applied to estimate the mass change by integrating over the entire glaciated region. The main purpose of this study is to investigate the sensitivity of the regional mass balance of Arctic ice caps and glaciers to different regionalization schemes. The sensitivity analysis is based on studying the spread of mass changes and their associated errors, and the suitability of the different regionalization techniques is assessed through cross-validation. The cross-validation results shows comparable accuracies for all regionalization methods, but the inferred mass change in individual regions, such as Svalbard and Iceland, can vary up to 4 Gt a −1 , which exceeds the estimated errors by roughly 50% for these regions. This study further finds that this spread in mass balance is connected to the magnitude of the elevation change variability. This indicates that care should be taken when choosing a regionalization method, especially for areas which exhibit large variability in elevation change. Text Arctic Iceland Svalbard Copernicus Publications: E-Journals Arctic Svalbard The Cryosphere 9 1 139 150
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The mass balance of glaciers and ice caps is sensitive to changing climate conditions. The mass changes derived in this study are determined from elevation changes derived measured by the Ice, Cloud, and land Elevation Satellite (ICESat) for the time period 2003–2009. Four methods, based on interpolation and extrapolation, are used to regionalize these elevation changes to areas without satellite coverage. A constant density assumption is then applied to estimate the mass change by integrating over the entire glaciated region. The main purpose of this study is to investigate the sensitivity of the regional mass balance of Arctic ice caps and glaciers to different regionalization schemes. The sensitivity analysis is based on studying the spread of mass changes and their associated errors, and the suitability of the different regionalization techniques is assessed through cross-validation. The cross-validation results shows comparable accuracies for all regionalization methods, but the inferred mass change in individual regions, such as Svalbard and Iceland, can vary up to 4 Gt a −1 , which exceeds the estimated errors by roughly 50% for these regions. This study further finds that this spread in mass balance is connected to the magnitude of the elevation change variability. This indicates that care should be taken when choosing a regionalization method, especially for areas which exhibit large variability in elevation change.
format Text
author Nilsson, J.
Sandberg Sørensen, L.
Barletta, V. R.
Forsberg, R.
spellingShingle Nilsson, J.
Sandberg Sørensen, L.
Barletta, V. R.
Forsberg, R.
Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
author_facet Nilsson, J.
Sandberg Sørensen, L.
Barletta, V. R.
Forsberg, R.
author_sort Nilsson, J.
title Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
title_short Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
title_full Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
title_fullStr Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
title_full_unstemmed Mass changes in Arctic ice caps and glaciers: implications of regionalizing elevation changes
title_sort mass changes in arctic ice caps and glaciers: implications of regionalizing elevation changes
publishDate 2018
url https://doi.org/10.5194/tc-9-139-2015
https://tc.copernicus.org/articles/9/139/2015/
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Iceland
Svalbard
genre_facet Arctic
Iceland
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-9-139-2015
https://tc.copernicus.org/articles/9/139/2015/
op_doi https://doi.org/10.5194/tc-9-139-2015
container_title The Cryosphere
container_volume 9
container_issue 1
container_start_page 139
op_container_end_page 150
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