The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models

The extensive dataset of Variegated Glacier's 1982/83 surge and antecedent quiescent phase is fragmentary and predominantly of flow line nature. Applying the raw centre line data in a flow line model to conduct research into the mechanism behind Variegated Glacier's surge behaviour inevita...

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Published in:Journal of Glaciology
Main Authors: SHARON VAN GEFFEN, JOHANNES OERLEMANS
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/jog.2017.43
https://doaj.org/article/8e6a1deeba204ea98f0f2d192433c376
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spelling ftdoajarticles:oai:doaj.org/article:8e6a1deeba204ea98f0f2d192433c376 2023-05-15T16:57:36+02:00 The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models SHARON VAN GEFFEN JOHANNES OERLEMANS 2017-10-01T00:00:00Z https://doi.org/10.1017/jog.2017.43 https://doaj.org/article/8e6a1deeba204ea98f0f2d192433c376 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143017000430/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.43 0022-1430 1727-5652 https://doaj.org/article/8e6a1deeba204ea98f0f2d192433c376 Journal of Glaciology, Vol 63, Pp 772-782 (2017) glacier flow glacier mass balance glacier modelling glacier surges glacier volume Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2017.43 2023-03-12T01:30:59Z The extensive dataset of Variegated Glacier's 1982/83 surge and antecedent quiescent phase is fragmentary and predominantly of flow line nature. Applying the raw centre line data in a flow line model to conduct research into the mechanism behind Variegated Glacier's surge behaviour inevitably entails problems. In this study, the incomplete dataset is extrapolated into the upper and lower parts of the glacier. Furthermore, the centre line data are adapted to account for differences between width-averaged and centre line surface mass balance and ice thickness change, inflow from tributaries, and changes in surface width over time. The modifications to the dataset are backed-up by observations and clear, plausible physical explanations. Moreover, the revised dataset meets the imposed constraints regarding ice volume flux, specific mass balance and net volume change. Hence, the final dataset is considered a satisfying revision that makes the dataset more valuable for future research. Subsequent application of the revised dataset corroborates the idea that glacier evolution during quiescence is basically the growth back towards steady state after the glacier was brought out of balance by the preceding surge. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 63 241 772 782
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic glacier flow
glacier mass balance
glacier modelling
glacier surges
glacier volume
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle glacier flow
glacier mass balance
glacier modelling
glacier surges
glacier volume
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
SHARON VAN GEFFEN
JOHANNES OERLEMANS
The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
topic_facet glacier flow
glacier mass balance
glacier modelling
glacier surges
glacier volume
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description The extensive dataset of Variegated Glacier's 1982/83 surge and antecedent quiescent phase is fragmentary and predominantly of flow line nature. Applying the raw centre line data in a flow line model to conduct research into the mechanism behind Variegated Glacier's surge behaviour inevitably entails problems. In this study, the incomplete dataset is extrapolated into the upper and lower parts of the glacier. Furthermore, the centre line data are adapted to account for differences between width-averaged and centre line surface mass balance and ice thickness change, inflow from tributaries, and changes in surface width over time. The modifications to the dataset are backed-up by observations and clear, plausible physical explanations. Moreover, the revised dataset meets the imposed constraints regarding ice volume flux, specific mass balance and net volume change. Hence, the final dataset is considered a satisfying revision that makes the dataset more valuable for future research. Subsequent application of the revised dataset corroborates the idea that glacier evolution during quiescence is basically the growth back towards steady state after the glacier was brought out of balance by the preceding surge.
format Article in Journal/Newspaper
author SHARON VAN GEFFEN
JOHANNES OERLEMANS
author_facet SHARON VAN GEFFEN
JOHANNES OERLEMANS
author_sort SHARON VAN GEFFEN
title The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
title_short The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
title_full The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
title_fullStr The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
title_full_unstemmed The 1982/83 surge and antecedent quiescent phase of Variegated Glacier: revising the original dataset for application in flow line models
title_sort 1982/83 surge and antecedent quiescent phase of variegated glacier: revising the original dataset for application in flow line models
publisher Cambridge University Press
publishDate 2017
url https://doi.org/10.1017/jog.2017.43
https://doaj.org/article/8e6a1deeba204ea98f0f2d192433c376
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 63, Pp 772-782 (2017)
op_relation https://www.cambridge.org/core/product/identifier/S0022143017000430/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2017.43
0022-1430
1727-5652
https://doaj.org/article/8e6a1deeba204ea98f0f2d192433c376
op_doi https://doi.org/10.1017/jog.2017.43
container_title Journal of Glaciology
container_volume 63
container_issue 241
container_start_page 772
op_container_end_page 782
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