Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model

A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B...

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Published in:Earth and Planetary Science Letters
Main Authors: Gladstone, RM, Lee, V, Rougier, JC, Payne, AJ, Hellmer, H, Le Brocq, A, Shepherd, A, Edwards, TL, Gregory, J, Cornford, S L
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://hdl.handle.net/1983/bbf3bf65-09b2-4c52-a40a-c2be9a181433
https://research-information.bris.ac.uk/en/publications/bbf3bf65-09b2-4c52-a40a-c2be9a181433
https://doi.org/10.1016/j.epsl.2012.04.022
http://www.sciencedirect.com/science/article/pii/S0012821X12001896
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spelling ftubristolcris:oai:research-information.bris.ac.uk:publications/bbf3bf65-09b2-4c52-a40a-c2be9a181433 2024-01-28T10:06:30+01:00 Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model Gladstone, RM Lee, V Rougier, JC Payne, AJ Hellmer, H Le Brocq, A Shepherd, A Edwards, TL Gregory, J Cornford, S L 2012-04 https://hdl.handle.net/1983/bbf3bf65-09b2-4c52-a40a-c2be9a181433 https://research-information.bris.ac.uk/en/publications/bbf3bf65-09b2-4c52-a40a-c2be9a181433 https://doi.org/10.1016/j.epsl.2012.04.022 http://www.sciencedirect.com/science/article/pii/S0012821X12001896 eng eng info:eu-repo/semantics/restrictedAccess Gladstone , RM , Lee , V , Rougier , JC , Payne , AJ , Hellmer , H , Le Brocq , A , Shepherd , A , Edwards , TL , Gregory , J & Cornford , S L 2012 , ' Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model ' , Earth and Planetary Science Letters , vol. 333-334 , pp. 191 - 199 . https://doi.org/10.1016/j.epsl.2012.04.022 article 2012 ftubristolcris https://doi.org/10.1016/j.epsl.2012.04.022 2024-01-04T23:36:41Z A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B ‘business as usual’ emissions scenario. Comparison is made against recent observations to provide a calibrated prediction in the form of a 95% confidence set. Predictions are for monotonic (apart from some small scale fluctuations in a minority of cases) retreat of the grounding line over the next 200 yr with huge uncertainty in the rate of retreat. Full collapse of the main trunk of the PIG during the 22nd century remains a possibility. A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B ‘business as usual’ emissions scenario. Comparison is made against recent observations to provide a calibrated prediction in the form of a 95% confidence set. Predictions are for monotonic (apart from some small scale fluctuations in a minority of cases) retreat of the grounding line over the next 200 yr with huge uncertainty in the rate of retreat. Full collapse of the main trunk of the PIG during the 22nd century remains a possibility. Article in Journal/Newspaper Ice Sheet Pine Island Glacier University of Bristol: Bristol Research Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Earth and Planetary Science Letters 333-334 191 199
institution Open Polar
collection University of Bristol: Bristol Research
op_collection_id ftubristolcris
language English
description A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B ‘business as usual’ emissions scenario. Comparison is made against recent observations to provide a calibrated prediction in the form of a 95% confidence set. Predictions are for monotonic (apart from some small scale fluctuations in a minority of cases) retreat of the grounding line over the next 200 yr with huge uncertainty in the rate of retreat. Full collapse of the main trunk of the PIG during the 22nd century remains a possibility. A flowline ice sheet model is coupled to a box model for cavity circulation and configured for the Pine Island Glacier. An ensemble of 5000 simulations are carried out from 1900 to 2200 with varying inputs and parameters, forced by ocean temperatures predicted by a regional ocean model under the A1B ‘business as usual’ emissions scenario. Comparison is made against recent observations to provide a calibrated prediction in the form of a 95% confidence set. Predictions are for monotonic (apart from some small scale fluctuations in a minority of cases) retreat of the grounding line over the next 200 yr with huge uncertainty in the rate of retreat. Full collapse of the main trunk of the PIG during the 22nd century remains a possibility.
format Article in Journal/Newspaper
author Gladstone, RM
Lee, V
Rougier, JC
Payne, AJ
Hellmer, H
Le Brocq, A
Shepherd, A
Edwards, TL
Gregory, J
Cornford, S L
spellingShingle Gladstone, RM
Lee, V
Rougier, JC
Payne, AJ
Hellmer, H
Le Brocq, A
Shepherd, A
Edwards, TL
Gregory, J
Cornford, S L
Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
author_facet Gladstone, RM
Lee, V
Rougier, JC
Payne, AJ
Hellmer, H
Le Brocq, A
Shepherd, A
Edwards, TL
Gregory, J
Cornford, S L
author_sort Gladstone, RM
title Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
title_short Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
title_full Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
title_fullStr Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
title_full_unstemmed Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model
title_sort calibrated prediction of pine island glacier retreat during the 21st and 22nd centuries with a coupled flowline model
publishDate 2012
url https://hdl.handle.net/1983/bbf3bf65-09b2-4c52-a40a-c2be9a181433
https://research-information.bris.ac.uk/en/publications/bbf3bf65-09b2-4c52-a40a-c2be9a181433
https://doi.org/10.1016/j.epsl.2012.04.022
http://www.sciencedirect.com/science/article/pii/S0012821X12001896
long_lat ENVELOPE(-101.000,-101.000,-75.000,-75.000)
geographic Pine Island Glacier
geographic_facet Pine Island Glacier
genre Ice Sheet
Pine Island Glacier
genre_facet Ice Sheet
Pine Island Glacier
op_source Gladstone , RM , Lee , V , Rougier , JC , Payne , AJ , Hellmer , H , Le Brocq , A , Shepherd , A , Edwards , TL , Gregory , J & Cornford , S L 2012 , ' Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline model ' , Earth and Planetary Science Letters , vol. 333-334 , pp. 191 - 199 . https://doi.org/10.1016/j.epsl.2012.04.022
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/j.epsl.2012.04.022
container_title Earth and Planetary Science Letters
container_volume 333-334
container_start_page 191
op_container_end_page 199
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