Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"

The potential contribution of glaciers and ice caps to sea level rise is usually calculated by comparing the estimated total ice volume with the surface area of the ocean. Part of this total ice volume, however, does not contribute to sea level rise because it is below the surface of the ocean or be...

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Main Authors: W. Haeberli, A. Linsbauer
Format: Article
Language:English
Published: Copernicus Publications 2013-05-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/7/817/2013/tc-7-817-2013.pdf
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spelling doaj-f5ecabbbe3a74f66842b534b5d0bdb232020-11-24T23:32:02ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242013-05-017381782110.5194/tc-7-817-2013Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"W. HaeberliA. LinsbauerThe potential contribution of glaciers and ice caps to sea level rise is usually calculated by comparing the estimated total ice volume with the surface area of the ocean. Part of this total ice volume, however, does not contribute to sea level rise because it is below the surface of the ocean or below the levels of future lakes on land. The present communication points to this so far overlooked phenomenon and provides a first order-of-magnitude estimate. It is shown that the effect is small (most likely about 1 to 6 cm sea level equivalent) but systematic, could primarily affect earlier stages of global glacier vanishing, and should therefore be adequately considered. Now-available techniques of slope-related high-resolution glacier bed modelling have the potential to provide more detailed assessments in the future.http://www.the-cryosphere.net/7/817/2013/tc-7-817-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author W. Haeberli
A. Linsbauer
spellingShingle W. Haeberli
A. Linsbauer
Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
The Cryosphere
author_facet W. Haeberli
A. Linsbauer
author_sort W. Haeberli
title Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
title_short Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
title_full Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
title_fullStr Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
title_full_unstemmed Brief communication "Global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
title_sort brief communication "global glacier volumes and sea level – small but systematic effects of ice below the surface of the ocean and of new local lakes on land"
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2013-05-01
description The potential contribution of glaciers and ice caps to sea level rise is usually calculated by comparing the estimated total ice volume with the surface area of the ocean. Part of this total ice volume, however, does not contribute to sea level rise because it is below the surface of the ocean or below the levels of future lakes on land. The present communication points to this so far overlooked phenomenon and provides a first order-of-magnitude estimate. It is shown that the effect is small (most likely about 1 to 6 cm sea level equivalent) but systematic, could primarily affect earlier stages of global glacier vanishing, and should therefore be adequately considered. Now-available techniques of slope-related high-resolution glacier bed modelling have the potential to provide more detailed assessments in the future.
url http://www.the-cryosphere.net/7/817/2013/tc-7-817-2013.pdf
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AT alinsbauer briefcommunicationglobalglaciervolumesandsealevelndashsmallbutsystematiceffectsoficebelowthesurfaceoftheoceanandofnewlocallakesonland
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