A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats
Many marine-terminating outlet glaciers have retreated rapidly in recent decades, but these changes have not been formally attributed to anthropogenic climate change. A key challenge for such an attribution assessment is that if glacier termini are sufficiently perturbed from bathymetric highs, ice-...
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2022
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Online Access: | https://doi.org/10.5194/tc-16-2725-2022 https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb |
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ftdoajarticles:oai:doaj.org/article:ed373b17ab144f008a5836d8e2f1d0eb 2023-05-15T16:41:11+02:00 A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats J. E. Christian A. A. Robel G. Catania 2022-07-01T00:00:00Z https://doi.org/10.5194/tc-16-2725-2022 https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb EN eng Copernicus Publications https://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-2725-2022 1994-0416 1994-0424 https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb The Cryosphere, Vol 16, Pp 2725-2743 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-2725-2022 2022-12-30T22:23:49Z Many marine-terminating outlet glaciers have retreated rapidly in recent decades, but these changes have not been formally attributed to anthropogenic climate change. A key challenge for such an attribution assessment is that if glacier termini are sufficiently perturbed from bathymetric highs, ice-dynamic feedbacks can cause rapid retreat even without further climate forcing. In the presence of internal climate variability, attribution thus depends on understanding whether (or how frequently) these rapid retreats could be triggered by climatic noise alone. Our simulations with idealized glaciers show that in a noisy climate, rapid retreat is a stochastic phenomenon. We therefore propose a probabilistic approach to attribution and present a framework for analysis that uses ensembles of many simulations with independent realizations of random climate variability. Synthetic experiments show that century-scale climate trends substantially increase the likelihood of rapid glacier retreat. This effect depends on the timescales over which ice dynamics integrate forcing. For a population of synthetic glaciers with different topographies, we find that external trends increase the number of large retreats triggered within the population, offering a metric for regional attribution. Our analyses suggest that formal attribution studies are tractable and should be further pursued to clarify the human role in recent ice-sheet change. We emphasize that early-industrial-era constraints on glacier and climate state are likely to be crucial for such studies. Article in Journal/Newspaper Ice Sheet The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 16 7 2725 2743 |
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 J. E. Christian A. A. Robel G. Catania A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
Many marine-terminating outlet glaciers have retreated rapidly in recent decades, but these changes have not been formally attributed to anthropogenic climate change. A key challenge for such an attribution assessment is that if glacier termini are sufficiently perturbed from bathymetric highs, ice-dynamic feedbacks can cause rapid retreat even without further climate forcing. In the presence of internal climate variability, attribution thus depends on understanding whether (or how frequently) these rapid retreats could be triggered by climatic noise alone. Our simulations with idealized glaciers show that in a noisy climate, rapid retreat is a stochastic phenomenon. We therefore propose a probabilistic approach to attribution and present a framework for analysis that uses ensembles of many simulations with independent realizations of random climate variability. Synthetic experiments show that century-scale climate trends substantially increase the likelihood of rapid glacier retreat. This effect depends on the timescales over which ice dynamics integrate forcing. For a population of synthetic glaciers with different topographies, we find that external trends increase the number of large retreats triggered within the population, offering a metric for regional attribution. Our analyses suggest that formal attribution studies are tractable and should be further pursued to clarify the human role in recent ice-sheet change. We emphasize that early-industrial-era constraints on glacier and climate state are likely to be crucial for such studies. |
format |
Article in Journal/Newspaper |
author |
J. E. Christian A. A. Robel G. Catania |
author_facet |
J. E. Christian A. A. Robel G. Catania |
author_sort |
J. E. Christian |
title |
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
title_short |
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
title_full |
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
title_fullStr |
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
title_full_unstemmed |
A probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
title_sort |
probabilistic framework for quantifying the role of anthropogenic climate change in marine-terminating glacier retreats |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/tc-16-2725-2022 https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb |
genre |
Ice Sheet The Cryosphere |
genre_facet |
Ice Sheet The Cryosphere |
op_source |
The Cryosphere, Vol 16, Pp 2725-2743 (2022) |
op_relation |
https://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-2725-2022 1994-0416 1994-0424 https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb |
op_doi |
https://doi.org/10.5194/tc-16-2725-2022 |
container_title |
The Cryosphere |
container_volume |
16 |
container_issue |
7 |
container_start_page |
2725 |
op_container_end_page |
2743 |
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1766031625038069760 |