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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Published in:The Cryosphere
Main Authors: J. E. Christian, A. A. Robel, G. Catania
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
geo
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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spelling 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
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle 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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