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Enthalpy balance theory unifies diverse glacier surge behaviour
Annals of Glaciology, Pages: 1 - 7
Swansea University Author:
Adrian Luckman
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DOI (Published version): 10.1017/aog.2023.23
Abstract
It is commonly asserted that there are two distinct classes of glacier surges: slow, long-duration ‘Svalbard-type’ surges, triggered by a transition from cold- to warm-based conditions (thermal switching), and fast, shorter-duration ‘Alaska-type’ surges triggered by a reorganisation of the basal dra...
Published in: | Annals of Glaciology |
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ISSN: | 0260-3055 1727-5644 |
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Cambridge University Press (CUP)
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URI: | https://cronfa.swan.ac.uk/Record/cronfa63226 |
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v2 63226 2023-04-21 Enthalpy balance theory unifies diverse glacier surge behaviour 008cb668b2671b653a88677f075799a9 0000-0002-9618-5905 Adrian Luckman Adrian Luckman true false 2023-04-21 SGE It is commonly asserted that there are two distinct classes of glacier surges: slow, long-duration ‘Svalbard-type’ surges, triggered by a transition from cold- to warm-based conditions (thermal switching), and fast, shorter-duration ‘Alaska-type’ surges triggered by a reorganisation of the basal drainage system (hydraulic switching). This classification, however, reflects neither the diversity of surges in Svalbard and Alaska (and other regions), nor the fundamental dynamic processes underlying all surges. We argue that enthalpy balance theory offers a framework for understanding the spectrum of glacier surging behaviours while emphasising their essential dynamic unity. In this paper, we summarise enthalpy balance theory, illustrate its potential to explain so-called ‘Svalbard-type’ and ‘Alaska-type’ surges using a single set of principles, and show examples of a much wider range of glacier surge behaviour than previously observed. We then identify some future directions for research, including strategies for testing predictions of the theory against field and remote sensing data, and priorities for numerical model development. Journal Article Annals of Glaciology 1 7 Cambridge University Press (CUP) 0260-3055 1727-5644 Glacier modelling, glacier surges, subglacial processes 0 0 0 0001-01-01 10.1017/aog.2023.23 http://dx.doi.org/10.1017/aog.2023.23 COLLEGE NANME Geography COLLEGE CODE SGE Swansea University Another institution paid the OA fee 2023-05-31T11:25:54.7195199 2023-04-21T16:05:14.8391053 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Douglas I. Benn 1 Ian J. Hewitt 2 Adrian Luckman 0000-0002-9618-5905 3 63226__27591__9da24e57a6854d5da42477b829f242e4.pdf 63226.pdf 2023-05-24T11:42:52.8956044 Output 2770070 application/pdf Version of Record true This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited. true eng http://creativecommons.org/licenses/by/4.0/ |
title |
Enthalpy balance theory unifies diverse glacier surge behaviour |
spellingShingle |
Enthalpy balance theory unifies diverse glacier surge behaviour Adrian Luckman |
title_short |
Enthalpy balance theory unifies diverse glacier surge behaviour |
title_full |
Enthalpy balance theory unifies diverse glacier surge behaviour |
title_fullStr |
Enthalpy balance theory unifies diverse glacier surge behaviour |
title_full_unstemmed |
Enthalpy balance theory unifies diverse glacier surge behaviour |
title_sort |
Enthalpy balance theory unifies diverse glacier surge behaviour |
author_id_str_mv |
008cb668b2671b653a88677f075799a9 |
author_id_fullname_str_mv |
008cb668b2671b653a88677f075799a9_***_Adrian Luckman |
author |
Adrian Luckman |
author2 |
Douglas I. Benn Ian J. Hewitt Adrian Luckman |
format |
Journal article |
container_title |
Annals of Glaciology |
container_start_page |
1 |
institution |
Swansea University |
issn |
0260-3055 1727-5644 |
doi_str_mv |
10.1017/aog.2023.23 |
publisher |
Cambridge University Press (CUP) |
college_str |
Faculty of Science and Engineering |
hierarchytype |
|
hierarchy_top_id |
facultyofscienceandengineering |
hierarchy_top_title |
Faculty of Science and Engineering |
hierarchy_parent_id |
facultyofscienceandengineering |
hierarchy_parent_title |
Faculty of Science and Engineering |
department_str |
School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography |
url |
http://dx.doi.org/10.1017/aog.2023.23 |
document_store_str |
1 |
active_str |
0 |
description |
It is commonly asserted that there are two distinct classes of glacier surges: slow, long-duration ‘Svalbard-type’ surges, triggered by a transition from cold- to warm-based conditions (thermal switching), and fast, shorter-duration ‘Alaska-type’ surges triggered by a reorganisation of the basal drainage system (hydraulic switching). This classification, however, reflects neither the diversity of surges in Svalbard and Alaska (and other regions), nor the fundamental dynamic processes underlying all surges. We argue that enthalpy balance theory offers a framework for understanding the spectrum of glacier surging behaviours while emphasising their essential dynamic unity. In this paper, we summarise enthalpy balance theory, illustrate its potential to explain so-called ‘Svalbard-type’ and ‘Alaska-type’ surges using a single set of principles, and show examples of a much wider range of glacier surge behaviour than previously observed. We then identify some future directions for research, including strategies for testing predictions of the theory against field and remote sensing data, and priorities for numerical model development. |
published_date |
0001-01-01T11:25:54Z |
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1767404998827704320 |
score |
10.970258 |