Ice sheet-albedo feedback estimated from most recent deglaciation
Ice sheet feedbacks are underrepresented in model assessments of climate sensitivity and their magnitudes are still poorly constrained. We combine a recently published record of Earth's Energy Imbalance (EEI) with existing reconstructions of temperature, atmospheric composition, and sea level t...
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ftsouthampton:oai:eprints.soton.ac.uk:493550 2024-10-06T13:49:31+00:00 Ice sheet-albedo feedback estimated from most recent deglaciation Booth, Alice Goodwin, Philip Cael, B.B. 2024-08-06 text https://eprints.soton.ac.uk/493550/ https://eprints.soton.ac.uk/493550/1/Geophysical_Research_Letters_-_2024_-_Booth_-_Ice_Sheet_Albedo_Feedback_Estimated_From_Most_Recent_Deglaciation.pdf en English eng https://eprints.soton.ac.uk/493550/1/Geophysical_Research_Letters_-_2024_-_Booth_-_Ice_Sheet_Albedo_Feedback_Estimated_From_Most_Recent_Deglaciation.pdf Booth, Alice, Goodwin, Philip and Cael, B.B. (2024) Ice sheet-albedo feedback estimated from most recent deglaciation. Geophysical Research Letters, 51 (15), [e2024GL109953]. (doi:10.1029/2024GL109953 <http://dx.doi.org/10.1029/2024GL109953>). cc_by_4 Article PeerReviewed 2024 ftsouthampton https://doi.org/10.1029/2024GL109953 2024-09-11T14:18:14Z Ice sheet feedbacks are underrepresented in model assessments of climate sensitivity and their magnitudes are still poorly constrained. We combine a recently published record of Earth's Energy Imbalance (EEI) with existing reconstructions of temperature, atmospheric composition, and sea level to estimate both the magnitude and timescale of the ice sheet-albedo feedback since the Last Glacial Maximum. This facilitates the first opportunity to quantify this feedback over the most recent deglaciation using a proxy data-driven approach. We find the ice sheet-albedo feedback to be amplifying, increasing the total climate feedback parameter by 42% and reaching an equilibrium magnitude of 0.55 Wm −2 K −1 , with a 66% confidence interval of 0.45–0.63 Wm −2 K −1 . The timescale to equilibrium is estimated as 3.6 ka (66% confidence: 1.9–5.5 ka). These results provide new evidence for the timescale and magnitude of the amplifying ice sheet-albedo feedback that will drive anthropogenic warming for millennia to come. Article in Journal/Newspaper Ice Sheet University of Southampton: e-Prints Soton Geophysical Research Letters 51 15 |
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Open Polar |
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University of Southampton: e-Prints Soton |
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ftsouthampton |
language |
English |
description |
Ice sheet feedbacks are underrepresented in model assessments of climate sensitivity and their magnitudes are still poorly constrained. We combine a recently published record of Earth's Energy Imbalance (EEI) with existing reconstructions of temperature, atmospheric composition, and sea level to estimate both the magnitude and timescale of the ice sheet-albedo feedback since the Last Glacial Maximum. This facilitates the first opportunity to quantify this feedback over the most recent deglaciation using a proxy data-driven approach. We find the ice sheet-albedo feedback to be amplifying, increasing the total climate feedback parameter by 42% and reaching an equilibrium magnitude of 0.55 Wm −2 K −1 , with a 66% confidence interval of 0.45–0.63 Wm −2 K −1 . The timescale to equilibrium is estimated as 3.6 ka (66% confidence: 1.9–5.5 ka). These results provide new evidence for the timescale and magnitude of the amplifying ice sheet-albedo feedback that will drive anthropogenic warming for millennia to come. |
format |
Article in Journal/Newspaper |
author |
Booth, Alice Goodwin, Philip Cael, B.B. |
spellingShingle |
Booth, Alice Goodwin, Philip Cael, B.B. Ice sheet-albedo feedback estimated from most recent deglaciation |
author_facet |
Booth, Alice Goodwin, Philip Cael, B.B. |
author_sort |
Booth, Alice |
title |
Ice sheet-albedo feedback estimated from most recent deglaciation |
title_short |
Ice sheet-albedo feedback estimated from most recent deglaciation |
title_full |
Ice sheet-albedo feedback estimated from most recent deglaciation |
title_fullStr |
Ice sheet-albedo feedback estimated from most recent deglaciation |
title_full_unstemmed |
Ice sheet-albedo feedback estimated from most recent deglaciation |
title_sort |
ice sheet-albedo feedback estimated from most recent deglaciation |
publishDate |
2024 |
url |
https://eprints.soton.ac.uk/493550/ https://eprints.soton.ac.uk/493550/1/Geophysical_Research_Letters_-_2024_-_Booth_-_Ice_Sheet_Albedo_Feedback_Estimated_From_Most_Recent_Deglaciation.pdf |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://eprints.soton.ac.uk/493550/1/Geophysical_Research_Letters_-_2024_-_Booth_-_Ice_Sheet_Albedo_Feedback_Estimated_From_Most_Recent_Deglaciation.pdf Booth, Alice, Goodwin, Philip and Cael, B.B. (2024) Ice sheet-albedo feedback estimated from most recent deglaciation. Geophysical Research Letters, 51 (15), [e2024GL109953]. (doi:10.1029/2024GL109953 <http://dx.doi.org/10.1029/2024GL109953>). |
op_rights |
cc_by_4 |
op_doi |
https://doi.org/10.1029/2024GL109953 |
container_title |
Geophysical Research Letters |
container_volume |
51 |
container_issue |
15 |
_version_ |
1812177590866149376 |