Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison
Accepted manuscript version. Published version available in Quaternary Science Reviews (2016) 147, p.122-135. The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glacial retreat phase, remains largely ambiguous due to the paucity of direct marine- and terre...
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Online Access: | https://hdl.handle.net/10037/12882 https://doi.org/10.1016/j.quascirev.2016.02.011 |
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ftunivtroemsoe:oai:munin.uit.no:10037/12882 2023-05-15T14:26:22+02:00 Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison Auriac, Amandine Whitehouse, P.L. Bentley, M.J. Patton, Henry Lloyd, J.M. Hubbard, Alun Lloyd 2016-09-01 https://hdl.handle.net/10037/12882 https://doi.org/10.1016/j.quascirev.2016.02.011 eng eng Elsevier Quaternary Science Reviews info:eu-repo/grantAgreement/EC/FP7-PEOPLE/317217/EU/Glaciated North Atlantic Margins/GLANAM/ info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ info:eu-repo/grantAgreement/RCN/PETROMAKS2/200672/Norway/Glaciations in the Barents Sea area// FRIDAID 1348282 doi:10.1016/j.quascirev.2016.02.011 0277-3791 1873-457X https://hdl.handle.net/10037/12882 openAccess Glacial isostatic adjustment modelling Ice sheet Barents Sea Relative sea level VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 Journal article Tidsskriftartikkel Peer reviewed 2016 ftunivtroemsoe https://doi.org/10.1016/j.quascirev.2016.02.011 2021-06-25T17:55:30Z Accepted manuscript version. Published version available in Quaternary Science Reviews (2016) 147, p.122-135. The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glacial retreat phase, remains largely ambiguous due to the paucity of direct marine- and terrestrial-based evidence constraining its horizontal and vertical extent and chronology. One way of validating the numerous BSIS reconstructions previously proposed is to collate and apply them under a wide range of Earth models and to compare prognostic (isostatic) output through time with known relative sea-level (RSL) data. Here we compare six contrasting BSIS load scenarios via a spherical Earth system model and derive a best-fit, χ2 parameter using RSL data from the four main terrestrial regions within the domain: Svalbard, Franz Josef Land, Novaya Zemlya and northern Norway. Poor χ2 values allow two load scenarios to be dismissed, leaving four that agree well with RSL observations. The remaining four scenarios optimally fit the RSL data when combined with Earth models that have an upper mantle viscosity of 0.2–2 × 1021 Pa s, while there is less sensitivity to the lithosphere thickness (ranging from 71 to 120 km) and lower mantle viscosity (spanning 1–50 × 1021 Pa s). GPS observations are also compared with predictions of present-day uplift across the Barents Sea. Key locations where relative sea-level and GPS data would prove critical in constraining future ice-sheet modelling efforts are also identified. Article in Journal/Newspaper Arctic Barents Sea Franz Josef Land Ice Sheet Northern Norway Novaya Zemlya Sea ice Svalbard University of Tromsø: Munin Open Research Archive Barents Sea Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Norway Svalbard Quaternary Science Reviews 147 122 135 |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
Glacial isostatic adjustment modelling Ice sheet Barents Sea Relative sea level VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 |
spellingShingle |
Glacial isostatic adjustment modelling Ice sheet Barents Sea Relative sea level VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 Auriac, Amandine Whitehouse, P.L. Bentley, M.J. Patton, Henry Lloyd, J.M. Hubbard, Alun Lloyd Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
topic_facet |
Glacial isostatic adjustment modelling Ice sheet Barents Sea Relative sea level VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 |
description |
Accepted manuscript version. Published version available in Quaternary Science Reviews (2016) 147, p.122-135. The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glacial retreat phase, remains largely ambiguous due to the paucity of direct marine- and terrestrial-based evidence constraining its horizontal and vertical extent and chronology. One way of validating the numerous BSIS reconstructions previously proposed is to collate and apply them under a wide range of Earth models and to compare prognostic (isostatic) output through time with known relative sea-level (RSL) data. Here we compare six contrasting BSIS load scenarios via a spherical Earth system model and derive a best-fit, χ2 parameter using RSL data from the four main terrestrial regions within the domain: Svalbard, Franz Josef Land, Novaya Zemlya and northern Norway. Poor χ2 values allow two load scenarios to be dismissed, leaving four that agree well with RSL observations. The remaining four scenarios optimally fit the RSL data when combined with Earth models that have an upper mantle viscosity of 0.2–2 × 1021 Pa s, while there is less sensitivity to the lithosphere thickness (ranging from 71 to 120 km) and lower mantle viscosity (spanning 1–50 × 1021 Pa s). GPS observations are also compared with predictions of present-day uplift across the Barents Sea. Key locations where relative sea-level and GPS data would prove critical in constraining future ice-sheet modelling efforts are also identified. |
format |
Article in Journal/Newspaper |
author |
Auriac, Amandine Whitehouse, P.L. Bentley, M.J. Patton, Henry Lloyd, J.M. Hubbard, Alun Lloyd |
author_facet |
Auriac, Amandine Whitehouse, P.L. Bentley, M.J. Patton, Henry Lloyd, J.M. Hubbard, Alun Lloyd |
author_sort |
Auriac, Amandine |
title |
Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
title_short |
Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
title_full |
Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
title_fullStr |
Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
title_full_unstemmed |
Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison |
title_sort |
glacial isostatic adjustment associated with the barents sea ice sheet: a modelling inter-comparison |
publisher |
Elsevier |
publishDate |
2016 |
url |
https://hdl.handle.net/10037/12882 https://doi.org/10.1016/j.quascirev.2016.02.011 |
long_lat |
ENVELOPE(55.000,55.000,81.000,81.000) |
geographic |
Barents Sea Franz Josef Land Norway Svalbard |
geographic_facet |
Barents Sea Franz Josef Land Norway Svalbard |
genre |
Arctic Barents Sea Franz Josef Land Ice Sheet Northern Norway Novaya Zemlya Sea ice Svalbard |
genre_facet |
Arctic Barents Sea Franz Josef Land Ice Sheet Northern Norway Novaya Zemlya Sea ice Svalbard |
op_relation |
Quaternary Science Reviews info:eu-repo/grantAgreement/EC/FP7-PEOPLE/317217/EU/Glaciated North Atlantic Margins/GLANAM/ info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ info:eu-repo/grantAgreement/RCN/PETROMAKS2/200672/Norway/Glaciations in the Barents Sea area// FRIDAID 1348282 doi:10.1016/j.quascirev.2016.02.011 0277-3791 1873-457X https://hdl.handle.net/10037/12882 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2016.02.011 |
container_title |
Quaternary Science Reviews |
container_volume |
147 |
container_start_page |
122 |
op_container_end_page |
135 |
_version_ |
1766298891100094464 |