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://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:ed373b17ab144f008a5836d8e2f1d0eb 2023-05-15T16:41:06+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 2022-07-01 https://doi.org/10.5194/tc-16-2725-2022 https://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb en eng Copernicus Publications doi:10.5194/tc-16-2725-2022 1994-0416 1994-0424 https://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb undefined The Cryosphere, Vol 16, Pp 2725-2743 (2022) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.5194/tc-16-2725-2022 2023-01-22T19:33:34Z 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 Unknown The Cryosphere 16 7 2725 2743 |
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geo envir 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 |
geo envir |
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://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf 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 |
doi:10.5194/tc-16-2725-2022 1994-0416 1994-0424 https://tc.copernicus.org/articles/16/2725/2022/tc-16-2725-2022.pdf https://doaj.org/article/ed373b17ab144f008a5836d8e2f1d0eb |
op_rights |
undefined |
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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1766031547998142464 |