A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity

The speed of Greenland's fastest glacier, Jakobshavn Isbræ, has varied substantially since its speed-up 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: I. Joughin, D. E. Shean, B. E. Smith, D. Floricioiu
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-211-2020
https://doaj.org/article/989da0e3ff8a4d1ea87112195bf82461
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spelling ftdoajarticles:oai:doaj.org/article:989da0e3ff8a4d1ea87112195bf82461 2023-05-15T16:01:04+02:00 A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity I. Joughin D. E. Shean B. E. Smith D. Floricioiu 2020-01-01T00:00:00Z https://doi.org/10.5194/tc-14-211-2020 https://doaj.org/article/989da0e3ff8a4d1ea87112195bf82461 EN eng Copernicus Publications https://www.the-cryosphere.net/14/211/2020/tc-14-211-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-211-2020 1994-0416 1994-0424 https://doaj.org/article/989da0e3ff8a4d1ea87112195bf82461 The Cryosphere, Vol 14, Pp 211-227 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-211-2020 2022-12-31T08:49:43Z The speed of Greenland's fastest glacier, Jakobshavn Isbræ, has varied substantially since its speed-up 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 speed-up and thinning followed by winter slowdown and thickening. There were extended periods of rigid mélange in the winters of 2016–2017 and 2017–2018, 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 Isbræ 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 approach 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 Jakobshavn isbræ The Cryosphere Directory of Open Access Journals: DOAJ Articles Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) The Cryosphere 14 1 211 227
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
I. Joughin
D. E. Shean
B. E. Smith
D. Floricioiu
A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The speed of Greenland's fastest glacier, Jakobshavn Isbræ, has varied substantially since its speed-up 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 speed-up and thinning followed by winter slowdown and thickening. There were extended periods of rigid mélange in the winters of 2016–2017 and 2017–2018, 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 Isbræ 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 approach 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
author I. Joughin
D. E. Shean
B. E. Smith
D. Floricioiu
author_facet I. Joughin
D. E. Shean
B. E. Smith
D. Floricioiu
author_sort I. Joughin
title A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
title_short A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
title_full A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
title_fullStr A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
title_full_unstemmed A decade of variability on Jakobshavn Isbræ: ocean temperatures pace speed through influence on mélange rigidity
title_sort decade of variability on jakobshavn isbræ: ocean temperatures pace speed through influence on mélange rigidity
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-211-2020
https://doaj.org/article/989da0e3ff8a4d1ea87112195bf82461
long_lat ENVELOPE(-49.917,-49.917,69.167,69.167)
geographic Jakobshavn Isbræ
geographic_facet Jakobshavn Isbræ
genre Disko Bay
Jakobshavn
Jakobshavn isbræ
The Cryosphere
genre_facet Disko Bay
Jakobshavn
Jakobshavn isbræ
The Cryosphere
op_source The Cryosphere, Vol 14, Pp 211-227 (2020)
op_relation https://www.the-cryosphere.net/14/211/2020/tc-14-211-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-211-2020
1994-0416
1994-0424
https://doaj.org/article/989da0e3ff8a4d1ea87112195bf82461
op_doi https://doi.org/10.5194/tc-14-211-2020
container_title The Cryosphere
container_volume 14
container_issue 1
container_start_page 211
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