Topography, climate and ice masses: a review
Topography acts as a filter between regional climate and the consequent response of a glacier or ice sheet. It influences the mass and energy inputs and modifies the ice dynamics. The evolution of the ice sheet surface and, over longer time scales, of the bed topography modulates the climatic forcin...
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crwiley:10.1111/j.1365-3121.1993.tb00266.x 2024-06-23T07:53:45+00:00 Topography, climate and ice masses: a review Kerr, Andrew 1993 http://dx.doi.org/10.1111/j.1365-3121.1993.tb00266.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3121.1993.tb00266.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3121.1993.tb00266.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Terra Nova volume 5, issue 4, page 332-342 ISSN 0954-4879 1365-3121 journal-article 1993 crwiley https://doi.org/10.1111/j.1365-3121.1993.tb00266.x 2024-05-31T08:12:55Z Topography acts as a filter between regional climate and the consequent response of a glacier or ice sheet. It influences the mass and energy inputs and modifies the ice dynamics. The evolution of the ice sheet surface and, over longer time scales, of the bed topography modulates the climatic forcing. Until we have a better understanding of these topographic linkages, the use of geophysical signals from former ice masses to determine palaeoclimates must be regarded as fundamentally flawed. Article in Journal/Newspaper Ice Sheet Wiley Online Library Terra Nova 5 4 332 342 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Topography acts as a filter between regional climate and the consequent response of a glacier or ice sheet. It influences the mass and energy inputs and modifies the ice dynamics. The evolution of the ice sheet surface and, over longer time scales, of the bed topography modulates the climatic forcing. Until we have a better understanding of these topographic linkages, the use of geophysical signals from former ice masses to determine palaeoclimates must be regarded as fundamentally flawed. |
format |
Article in Journal/Newspaper |
author |
Kerr, Andrew |
spellingShingle |
Kerr, Andrew Topography, climate and ice masses: a review |
author_facet |
Kerr, Andrew |
author_sort |
Kerr, Andrew |
title |
Topography, climate and ice masses: a review |
title_short |
Topography, climate and ice masses: a review |
title_full |
Topography, climate and ice masses: a review |
title_fullStr |
Topography, climate and ice masses: a review |
title_full_unstemmed |
Topography, climate and ice masses: a review |
title_sort |
topography, climate and ice masses: a review |
publisher |
Wiley |
publishDate |
1993 |
url |
http://dx.doi.org/10.1111/j.1365-3121.1993.tb00266.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3121.1993.tb00266.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3121.1993.tb00266.x |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Terra Nova volume 5, issue 4, page 332-342 ISSN 0954-4879 1365-3121 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1365-3121.1993.tb00266.x |
container_title |
Terra Nova |
container_volume |
5 |
container_issue |
4 |
container_start_page |
332 |
op_container_end_page |
342 |
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1802645568385712128 |