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...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Booth, Alice, Goodwin, Philip, Cael, B.B.
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access: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
id ftsouthampton:oai:eprints.soton.ac.uk:493550
record_format openpolar
spelling 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
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id 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