Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling

The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above present day level, due in part to the partial collapse of the Greenland and West Antarctic Ice Sheets. Assessing the pattern of sea level change for this period is complicated due to the uncertainties i...

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Main Authors: Gowan, Evan, Rovere, Alessio, Lohmann, Gerrit
Format: Conference Object
Language:unknown
Published: 2018
Subjects:
Online Access:https://epic.awi.de/id/eprint/48801/
https://epic.awi.de/id/eprint/48801/1/palsea_poster.pdf
https://hdl.handle.net/10013/epic.11b6b873-d77a-4f1b-9657-9011f4e569b1
id ftawi:oai:epic.awi.de:48801
record_format openpolar
spelling ftawi:oai:epic.awi.de:48801 2024-09-15T17:45:26+00:00 Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling Gowan, Evan Rovere, Alessio Lohmann, Gerrit 2018 application/pdf https://epic.awi.de/id/eprint/48801/ https://epic.awi.de/id/eprint/48801/1/palsea_poster.pdf https://hdl.handle.net/10013/epic.11b6b873-d77a-4f1b-9657-9011f4e569b1 unknown https://epic.awi.de/id/eprint/48801/1/palsea_poster.pdf Gowan, E. orcid:0000-0002-0119-9440 , Rovere, A. and Lohmann, G. orcid:0000-0003-2089-733X (2018) Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling , PALSEA-QUIGS workshop, Galloway, New Jersey, USA, 24 September 2018 - 27 September 2018 . hdl:10013/epic.11b6b873-d77a-4f1b-9657-9011f4e569b1 EPIC3PALSEA-QUIGS workshop, Galloway, New Jersey, USA, 2018-09-24-2018-09-27 Conference notRev 2018 ftawi 2024-06-24T04:21:00Z The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above present day level, due in part to the partial collapse of the Greenland and West Antarctic Ice Sheets. Assessing the pattern of sea level change for this period is complicated due to the uncertainties in the relative contributions of these two ice sheets. In addition, past sea level is the integrated history of water load changes and associated glacial isostatic adjustment before and after the period of interest. We present a the initial results of a global ice sheet reconstruction that seeks to untangle the last interglacial ice sheet configuration. The ice sheets are reconstructed by using the program ICESHEET, which uses ice sheet margin reconstructions and estimates of basal shear stress to produce realistic ice sheet configurations. We calibrate this model by modelling glacial-isostatic adjustment with relative sea level indicators. We also investigate the role of different Earth rheology models on the global pattern of sea level change during this period. We make an assessment of how much uncertainty in the last interglacial sea level is due to the ice sheet configuration during the last glacial cycle. Conference Object Antarc* Antarctic Greenland Ice Sheet Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above present day level, due in part to the partial collapse of the Greenland and West Antarctic Ice Sheets. Assessing the pattern of sea level change for this period is complicated due to the uncertainties in the relative contributions of these two ice sheets. In addition, past sea level is the integrated history of water load changes and associated glacial isostatic adjustment before and after the period of interest. We present a the initial results of a global ice sheet reconstruction that seeks to untangle the last interglacial ice sheet configuration. The ice sheets are reconstructed by using the program ICESHEET, which uses ice sheet margin reconstructions and estimates of basal shear stress to produce realistic ice sheet configurations. We calibrate this model by modelling glacial-isostatic adjustment with relative sea level indicators. We also investigate the role of different Earth rheology models on the global pattern of sea level change during this period. We make an assessment of how much uncertainty in the last interglacial sea level is due to the ice sheet configuration during the last glacial cycle.
format Conference Object
author Gowan, Evan
Rovere, Alessio
Lohmann, Gerrit
spellingShingle Gowan, Evan
Rovere, Alessio
Lohmann, Gerrit
Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
author_facet Gowan, Evan
Rovere, Alessio
Lohmann, Gerrit
author_sort Gowan, Evan
title Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
title_short Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
title_full Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
title_fullStr Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
title_full_unstemmed Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
title_sort determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling
publishDate 2018
url https://epic.awi.de/id/eprint/48801/
https://epic.awi.de/id/eprint/48801/1/palsea_poster.pdf
https://hdl.handle.net/10013/epic.11b6b873-d77a-4f1b-9657-9011f4e569b1
genre Antarc*
Antarctic
Greenland
Ice Sheet
genre_facet Antarc*
Antarctic
Greenland
Ice Sheet
op_source EPIC3PALSEA-QUIGS workshop, Galloway, New Jersey, USA, 2018-09-24-2018-09-27
op_relation https://epic.awi.de/id/eprint/48801/1/palsea_poster.pdf
Gowan, E. orcid:0000-0002-0119-9440 , Rovere, A. and Lohmann, G. orcid:0000-0003-2089-733X (2018) Determining last interglacial ice sheet configuration using glacial isostatic adjustment modelling , PALSEA-QUIGS workshop, Galloway, New Jersey, USA, 24 September 2018 - 27 September 2018 . hdl:10013/epic.11b6b873-d77a-4f1b-9657-9011f4e569b1
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