A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.

The speed of Greenland's fastest glacier, Jakobshavn Isbrae, has varied substantially since its speedup in the late 1990s. Here we present observations of surface velocity, mélange rigidity, and surface elevation to examine its behaviour over the last decade. Consistent with earlier results, we...

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Published in:The Cryosphere
Main Authors: Joughin, Ian, Shean, David E, Smith, Benjamin E, Floricioiu, Dana
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-211-2020
https://pubmed.ncbi.nlm.nih.gov/32355554
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7192015/
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author Joughin, Ian
Shean, David E
Smith, Benjamin E
Floricioiu, Dana
author_facet Joughin, Ian
Shean, David E
Smith, Benjamin E
Floricioiu, Dana
author_sort Joughin, Ian
collection Unknown
container_issue 1
container_start_page 211
container_title The Cryosphere
container_volume 14
description The speed of Greenland's fastest glacier, Jakobshavn Isbrae, has varied substantially since its speedup in the late 1990s. Here we present observations of surface velocity, mélange rigidity, and surface elevation to examine its behaviour over the last decade. Consistent with earlier results, we find a pronounced cycle of summer speedup and thinning followed by winter slowdown and thickening. There were extended periods of rigid mélange in the winters of 2016-17 and 2017-18, concurrent with terminus advances ~6 km farther than in the several winters prior. These terminus advances to shallower depths caused slowdowns, leading to substantial thickening, as has been noted elsewhere. The extended periods of rigid mélange coincide well with a period of cooler waters in Disko Bay. Thus, along with the relative timing of the seasonal slowdown, our results suggest that the ocean's dominant influence on Jakobshavn Isbrae is through its effect on winter mélange rigidity, rather than summer submarine melting. The elevation time series also reveals that in summers when the area upstream of the terminus approaches flotation, large surface depressions can form, which eventually become the detachment points for major calving events. It appears that as elevations near flotation, basal crevasses can form, which initiates a necking process that forms the depressions. The elevation data also show that steep cliffs often evolve into short floating extensions, rather than collapsing catastrophically due to brittle failure. Finally, summer 2019 speeds were slightly faster than the prior two summers, leaving it unclear whether the slowdown is ending.
format Article in Journal/Newspaper
genre Disko Bay
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op_doi https://doi.org/10.5194/tc-14-211-2020
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https://pubmed.ncbi.nlm.nih.gov/32355554
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7192015/
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spelling ftpubmed:32355554 2025-06-15T14:25:57+00:00 A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity. Joughin, Ian Shean, David E Smith, Benjamin E Floricioiu, Dana 2020 https://doi.org/10.5194/tc-14-211-2020 https://pubmed.ncbi.nlm.nih.gov/32355554 https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7192015/ eng eng https://doi.org/10.5194/tc-14-211-2020 https://pubmed.ncbi.nlm.nih.gov/32355554 https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7192015/ Cryosphere ISSN:1994-0424 Volume:14 Issue:1 Journal Article 2020 ftpubmed https://doi.org/10.5194/tc-14-211-2020 2025-05-30T16:54:00Z The speed of Greenland's fastest glacier, Jakobshavn Isbrae, has varied substantially since its speedup in the late 1990s. Here we present observations of surface velocity, mélange rigidity, and surface elevation to examine its behaviour over the last decade. Consistent with earlier results, we find a pronounced cycle of summer speedup and thinning followed by winter slowdown and thickening. There were extended periods of rigid mélange in the winters of 2016-17 and 2017-18, concurrent with terminus advances ~6 km farther than in the several winters prior. These terminus advances to shallower depths caused slowdowns, leading to substantial thickening, as has been noted elsewhere. The extended periods of rigid mélange coincide well with a period of cooler waters in Disko Bay. Thus, along with the relative timing of the seasonal slowdown, our results suggest that the ocean's dominant influence on Jakobshavn Isbrae is through its effect on winter mélange rigidity, rather than summer submarine melting. The elevation time series also reveals that in summers when the area upstream of the terminus approaches flotation, large surface depressions can form, which eventually become the detachment points for major calving events. It appears that as elevations near flotation, basal crevasses can form, which initiates a necking process that forms the depressions. The elevation data also show that steep cliffs often evolve into short floating extensions, rather than collapsing catastrophically due to brittle failure. Finally, summer 2019 speeds were slightly faster than the prior two summers, leaving it unclear whether the slowdown is ending. Article in Journal/Newspaper Disko Bay Jakobshavn Unknown The Cryosphere 14 1 211 227
spellingShingle Joughin, Ian
Shean, David E
Smith, Benjamin E
Floricioiu, Dana
A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title_full A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title_fullStr A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title_full_unstemmed A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title_short A Decade of Variability on Jakobshavn Isbrae: Ocean Temperatures Pace Speed Through Influence on Mélange Rigidity.
title_sort decade of variability on jakobshavn isbrae: ocean temperatures pace speed through influence on mélange rigidity.
url https://doi.org/10.5194/tc-14-211-2020
https://pubmed.ncbi.nlm.nih.gov/32355554
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7192015/