Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions
Little is known about the distribution of ice in the Antarctic Ice Sheet (AIS) during the Last Glacial Maximum (LGM). Whereas marine and terrestrial geological data indicate that the grounded ice advanced to a position close to the continental-shelf break, the total ice volume is unclear. Glacial bo...
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fttibhannoverren:oai:oa.tib.eu:123456789/10582 2023-05-15T13:53:55+02:00 Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions Blasco, Javier Alvarez-Solas, Jorge Robinson, Alexander Montoya, Marisa 2021-1-18 application/pdf https://oa.tib.eu/renate/handle/123456789/10582 https://doi.org/10.34657/9618 eng eng Katlenburg-Lindau : Copernicus ESSN:1994-0424 DOI:https://doi.org/10.5194/tc-15-215-2021 https://oa.tib.eu/renate/handle/123456789/10582 http://dx.doi.org/10.34657/9618 CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ frei zugänglich CC-BY The Cryosphere : TC 15 (2021), Nr. 1 ddc:910 status-type:publishedVersion doc-type:article doc-type:Text 2021 fttibhannoverren https://doi.org/10.34657/9618 https://doi.org/10.5194/tc-15-215-2021 2022-12-19T17:17:55Z Little is known about the distribution of ice in the Antarctic Ice Sheet (AIS) during the Last Glacial Maximum (LGM). Whereas marine and terrestrial geological data indicate that the grounded ice advanced to a position close to the continental-shelf break, the total ice volume is unclear. Glacial boundary conditions are potentially important sources of uncertainty, in particular basal friction and climatic boundary conditions. Basal friction exerts a strong control on the large-scale dynamics of the ice sheet and thus affects its size and is not well constrained. Glacial climatic boundary conditions determine the net accumulation and ice temperature and are also poorly known. Here we explore the effect of the uncertainty in both features on the total simulated ice storage of the AIS at the LGM. For this purpose we use a hybrid ice sheet shelf model that is forced with different basal drag choices and glacial background climatic conditions obtained from the LGM ensemble climate simulations of the third phase of the Paleoclimate Modelling Intercomparison Project (PMIP3). Overall, we find that the spread in the simulated ice volume for the tested basal drag parameterizations is about the same range as for the different general circulation model (GCM) forcings (4 to 6 m sea level equivalent). For a wide range of plausible basal friction configurations, the simulated ice dynamics vary widely but all simulations produce fully extended ice sheets towards the continental-shelf break. More dynamically active ice sheets correspond to lower ice volumes, while they remain consistent with the available constraints on ice extent. Thus, this work points to the possibility of an AIS with very active ice streams during the LGM. In addition, we find that the surface boundary temperature field plays a crucial role in determining the ice extent through its effect on viscosity. For ice sheets of a similar extent and comparable dynamics, we find that the precipitation field determines the total AIS volume. However, precipitation is ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet The Cryosphere Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) Antarctic The Antarctic |
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Open Polar |
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Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) |
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fttibhannoverren |
language |
English |
topic |
ddc:910 |
spellingShingle |
ddc:910 Blasco, Javier Alvarez-Solas, Jorge Robinson, Alexander Montoya, Marisa Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
topic_facet |
ddc:910 |
description |
Little is known about the distribution of ice in the Antarctic Ice Sheet (AIS) during the Last Glacial Maximum (LGM). Whereas marine and terrestrial geological data indicate that the grounded ice advanced to a position close to the continental-shelf break, the total ice volume is unclear. Glacial boundary conditions are potentially important sources of uncertainty, in particular basal friction and climatic boundary conditions. Basal friction exerts a strong control on the large-scale dynamics of the ice sheet and thus affects its size and is not well constrained. Glacial climatic boundary conditions determine the net accumulation and ice temperature and are also poorly known. Here we explore the effect of the uncertainty in both features on the total simulated ice storage of the AIS at the LGM. For this purpose we use a hybrid ice sheet shelf model that is forced with different basal drag choices and glacial background climatic conditions obtained from the LGM ensemble climate simulations of the third phase of the Paleoclimate Modelling Intercomparison Project (PMIP3). Overall, we find that the spread in the simulated ice volume for the tested basal drag parameterizations is about the same range as for the different general circulation model (GCM) forcings (4 to 6 m sea level equivalent). For a wide range of plausible basal friction configurations, the simulated ice dynamics vary widely but all simulations produce fully extended ice sheets towards the continental-shelf break. More dynamically active ice sheets correspond to lower ice volumes, while they remain consistent with the available constraints on ice extent. Thus, this work points to the possibility of an AIS with very active ice streams during the LGM. In addition, we find that the surface boundary temperature field plays a crucial role in determining the ice extent through its effect on viscosity. For ice sheets of a similar extent and comparable dynamics, we find that the precipitation field determines the total AIS volume. However, precipitation is ... |
format |
Article in Journal/Newspaper |
author |
Blasco, Javier Alvarez-Solas, Jorge Robinson, Alexander Montoya, Marisa |
author_facet |
Blasco, Javier Alvarez-Solas, Jorge Robinson, Alexander Montoya, Marisa |
author_sort |
Blasco, Javier |
title |
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
title_short |
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
title_full |
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
title_fullStr |
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
title_full_unstemmed |
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions |
title_sort |
exploring the impact of atmospheric forcing and basal drag on the antarctic ice sheet under last glacial maximum conditions |
publisher |
Katlenburg-Lindau : Copernicus |
publishDate |
2021 |
url |
https://oa.tib.eu/renate/handle/123456789/10582 https://doi.org/10.34657/9618 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Ice Sheet The Cryosphere |
genre_facet |
Antarc* Antarctic Ice Sheet The Cryosphere |
op_source |
The Cryosphere : TC 15 (2021), Nr. 1 |
op_relation |
ESSN:1994-0424 DOI:https://doi.org/10.5194/tc-15-215-2021 https://oa.tib.eu/renate/handle/123456789/10582 http://dx.doi.org/10.34657/9618 |
op_rights |
CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ frei zugänglich |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/9618 https://doi.org/10.5194/tc-15-215-2021 |
_version_ |
1766259390647631872 |