Mass balance loss of Mount Baker, Washington glaciers 1990–2010

Abstract Mount Baker, North Cascades, WA, has a current glacierized area of 38.6 km 2 . From 1984 to 2010, the North Cascade Glacier Climate Project has monitored the annual mass balance (Ba), accumulation area ratio (AAR), terminus behaviour and longitudinal profiles of Mount Baker glaciers. The Ba...

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Published in:Hydrological Processes
Main Authors: Pelto, Mauri, Brown, Courtenay
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.9453
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9453
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spelling crwiley:10.1002/hyp.9453 2024-09-15T17:57:09+00:00 Mass balance loss of Mount Baker, Washington glaciers 1990–2010 Pelto, Mauri Brown, Courtenay 2012 http://dx.doi.org/10.1002/hyp.9453 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9453 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9453 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 26, issue 17, page 2601-2607 ISSN 0885-6087 1099-1085 journal-article 2012 crwiley https://doi.org/10.1002/hyp.9453 2024-07-30T04:21:59Z Abstract Mount Baker, North Cascades, WA, has a current glacierized area of 38.6 km 2 . From 1984 to 2010, the North Cascade Glacier Climate Project has monitored the annual mass balance (Ba), accumulation area ratio (AAR), terminus behaviour and longitudinal profiles of Mount Baker glaciers. The Ba on Rainbow, Easton and Sholes Glaciers from 1990 to 2010 averaged −0.52 m w.e. a −1 (m a −1 ). Terminus observations on nine principal Mount Baker glaciers, 1984–2009, indicate retreat ranging from 240 to 520 m, with a mean of 370 m or 14 m a −1 . AAR observations on Rainbow, Sholes and Easton Glaciers for 1990–2010 indicate a mean AAR of 0.55 and a steady state AAR of 0.65. A comparison of Ba and AAR on these three glaciers yields a relationship that is used in combination with AAR observations made on all Mount Baker glaciers during 7 years to assess Mount Baker glacier mass balance. Utilizing the AAR–Ba relationship for the three glaciers yields a mean Ba of −0.55 m a −1 for the 1990–2010 period, 0.03 m a −1 higher than the measured mean Ba. The mean Ba based on the AAR–Ba relationship for the entire mountain from 1990 to 2010 is −0.57 m a −1 . The product of the mean observed mass balance gradient determined from 11 000 surface mass balance measurements and glacier area in each 100‐m elevation band on Mount Baker yields a Ba of −0.50 m a −1 from 1990–2010 for the entire mountain. The median altitude of the three index glaciers is lower than that of all Mount Baker glaciers. Adjusting the balance gradient for this difference yields a mean Ba of −0.77 m a −1 from 1990 to 2010. All but one estimate converge on a loss of −0.5 m a −1 for Mount Baker from 1990 to 2010. This equates to an 11‐m loss in glacier thickness, 12–20% of the entire 1990 volume of glaciers on Mount Baker. Copyright © 2012 John Wiley & Sons, Ltd. Article in Journal/Newspaper Baker Glacier Wiley Online Library Hydrological Processes 26 17 2601 2607
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Mount Baker, North Cascades, WA, has a current glacierized area of 38.6 km 2 . From 1984 to 2010, the North Cascade Glacier Climate Project has monitored the annual mass balance (Ba), accumulation area ratio (AAR), terminus behaviour and longitudinal profiles of Mount Baker glaciers. The Ba on Rainbow, Easton and Sholes Glaciers from 1990 to 2010 averaged −0.52 m w.e. a −1 (m a −1 ). Terminus observations on nine principal Mount Baker glaciers, 1984–2009, indicate retreat ranging from 240 to 520 m, with a mean of 370 m or 14 m a −1 . AAR observations on Rainbow, Sholes and Easton Glaciers for 1990–2010 indicate a mean AAR of 0.55 and a steady state AAR of 0.65. A comparison of Ba and AAR on these three glaciers yields a relationship that is used in combination with AAR observations made on all Mount Baker glaciers during 7 years to assess Mount Baker glacier mass balance. Utilizing the AAR–Ba relationship for the three glaciers yields a mean Ba of −0.55 m a −1 for the 1990–2010 period, 0.03 m a −1 higher than the measured mean Ba. The mean Ba based on the AAR–Ba relationship for the entire mountain from 1990 to 2010 is −0.57 m a −1 . The product of the mean observed mass balance gradient determined from 11 000 surface mass balance measurements and glacier area in each 100‐m elevation band on Mount Baker yields a Ba of −0.50 m a −1 from 1990–2010 for the entire mountain. The median altitude of the three index glaciers is lower than that of all Mount Baker glaciers. Adjusting the balance gradient for this difference yields a mean Ba of −0.77 m a −1 from 1990 to 2010. All but one estimate converge on a loss of −0.5 m a −1 for Mount Baker from 1990 to 2010. This equates to an 11‐m loss in glacier thickness, 12–20% of the entire 1990 volume of glaciers on Mount Baker. Copyright © 2012 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Pelto, Mauri
Brown, Courtenay
spellingShingle Pelto, Mauri
Brown, Courtenay
Mass balance loss of Mount Baker, Washington glaciers 1990–2010
author_facet Pelto, Mauri
Brown, Courtenay
author_sort Pelto, Mauri
title Mass balance loss of Mount Baker, Washington glaciers 1990–2010
title_short Mass balance loss of Mount Baker, Washington glaciers 1990–2010
title_full Mass balance loss of Mount Baker, Washington glaciers 1990–2010
title_fullStr Mass balance loss of Mount Baker, Washington glaciers 1990–2010
title_full_unstemmed Mass balance loss of Mount Baker, Washington glaciers 1990–2010
title_sort mass balance loss of mount baker, washington glaciers 1990–2010
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1002/hyp.9453
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9453
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9453
genre Baker Glacier
genre_facet Baker Glacier
op_source Hydrological Processes
volume 26, issue 17, page 2601-2607
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.9453
container_title Hydrological Processes
container_volume 26
container_issue 17
container_start_page 2601
op_container_end_page 2607
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