Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015

Despite much progress with remote sensing, on-site measurements of glacier mass balance (with stakes and snow pits) still have advantages for resolution of interannual and seasonal changes of mass balance. Understanding these changes may help to identify the types of glaciers most sensitive to clima...

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Published in:Frontiers in Earth Science
Main Authors: Roger J. Braithwaite, Philip D. Hughes
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2020
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2020.00302
https://doaj.org/article/2f704eb907e74613928a81f9a45173b1
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spelling ftdoajarticles:oai:doaj.org/article:2f704eb907e74613928a81f9a45173b1 2023-05-15T15:08:48+02:00 Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015 Roger J. Braithwaite Philip D. Hughes 2020-08-01T00:00:00Z https://doi.org/10.3389/feart.2020.00302 https://doaj.org/article/2f704eb907e74613928a81f9a45173b1 EN eng Frontiers Media S.A. https://www.frontiersin.org/article/10.3389/feart.2020.00302/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2020.00302 https://doaj.org/article/2f704eb907e74613928a81f9a45173b1 Frontiers in Earth Science, Vol 8 (2020) glacier mass balance balance amplitude climate at equilibrium line altitude Randolph Glacier Inventory Climatic Research Unit/University of East Anglia gridded climatology Science Q article 2020 ftdoajarticles https://doi.org/10.3389/feart.2020.00302 2022-12-31T14:21:08Z Despite much progress with remote sensing, on-site measurements of glacier mass balance (with stakes and snow pits) still have advantages for resolution of interannual and seasonal changes of mass balance. Understanding these changes may help to identify the types of glaciers most sensitive to climate change. The standard deviation of mass balance data series for a few years describes the interannual variability, and balance amplitude, defined as half the difference between winter and summer balances, describes the seasonal variability. Interannual variability increases with seasonal variability, and seasonal variability increases with annual precipitation and summer temperature available from a half-degree gridded climatology. Measured glaciers have higher mean and median precipitation than average for all glaciers in the Randolph Glacier Inventory (version 6). High balance amplitudes are associated with warm/wet (maritime) environments and low amplitudes with cold/dry (continental) environments, as shown in previous studies of climate at the equilibrium line altitude. Balance amplitude can be modelled for half-degree grid squares in the glacier inventory using multiple regression of measured balance amplitude on the climate data. The resulting modelled balance amplitude is relatively low for Arctic Islands and Central Asia, but high for Western North America, Iceland, Scandinavia, Alps, and Caucasus. Article in Journal/Newspaper Arctic Climate change glacier Iceland Directory of Open Access Journals: DOAJ Articles Arctic Frontiers in Earth Science 8
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic glacier mass balance
balance amplitude
climate at equilibrium line altitude
Randolph Glacier Inventory
Climatic Research Unit/University of East Anglia gridded climatology
Science
Q
spellingShingle glacier mass balance
balance amplitude
climate at equilibrium line altitude
Randolph Glacier Inventory
Climatic Research Unit/University of East Anglia gridded climatology
Science
Q
Roger J. Braithwaite
Philip D. Hughes
Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
topic_facet glacier mass balance
balance amplitude
climate at equilibrium line altitude
Randolph Glacier Inventory
Climatic Research Unit/University of East Anglia gridded climatology
Science
Q
description Despite much progress with remote sensing, on-site measurements of glacier mass balance (with stakes and snow pits) still have advantages for resolution of interannual and seasonal changes of mass balance. Understanding these changes may help to identify the types of glaciers most sensitive to climate change. The standard deviation of mass balance data series for a few years describes the interannual variability, and balance amplitude, defined as half the difference between winter and summer balances, describes the seasonal variability. Interannual variability increases with seasonal variability, and seasonal variability increases with annual precipitation and summer temperature available from a half-degree gridded climatology. Measured glaciers have higher mean and median precipitation than average for all glaciers in the Randolph Glacier Inventory (version 6). High balance amplitudes are associated with warm/wet (maritime) environments and low amplitudes with cold/dry (continental) environments, as shown in previous studies of climate at the equilibrium line altitude. Balance amplitude can be modelled for half-degree grid squares in the glacier inventory using multiple regression of measured balance amplitude on the climate data. The resulting modelled balance amplitude is relatively low for Arctic Islands and Central Asia, but high for Western North America, Iceland, Scandinavia, Alps, and Caucasus.
format Article in Journal/Newspaper
author Roger J. Braithwaite
Philip D. Hughes
author_facet Roger J. Braithwaite
Philip D. Hughes
author_sort Roger J. Braithwaite
title Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
title_short Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
title_full Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
title_fullStr Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
title_full_unstemmed Regional Geography of Glacier Mass Balance Variability Over Seven Decades 1946–2015
title_sort regional geography of glacier mass balance variability over seven decades 1946–2015
publisher Frontiers Media S.A.
publishDate 2020
url https://doi.org/10.3389/feart.2020.00302
https://doaj.org/article/2f704eb907e74613928a81f9a45173b1
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
glacier
Iceland
genre_facet Arctic
Climate change
glacier
Iceland
op_source Frontiers in Earth Science, Vol 8 (2020)
op_relation https://www.frontiersin.org/article/10.3389/feart.2020.00302/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2020.00302
https://doaj.org/article/2f704eb907e74613928a81f9a45173b1
op_doi https://doi.org/10.3389/feart.2020.00302
container_title Frontiers in Earth Science
container_volume 8
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