Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic

Analyses of glacial isostatic adjustment (GIA) and deglacial relative sea-level (RSL) change in the Russian Arctic deliver important insights into the Earth's viscosity structure and the deglaciation history of the Eurasian ice sheet complex. Here, we validate the 1D GIA models ICE-6G_C (VM5a)...

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Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Li, Tanghua, Khan, Nicole S., Baranskaya, Alisa V., Shaw, Timothy Adam, Peltier, W. Richard, Stuhne, Gordan R., Wu, Patrick, Horton, Benjamin Peter
Other Authors: Asian School of the Environment, Earth Observatory of Singapore
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Moe
Online Access:https://hdl.handle.net/10356/157193
https://doi.org/10.1029/2021JB023631
id ftnanyangtu:oai:dr.ntu.edu.sg:10356/157193
record_format openpolar
spelling ftnanyangtu:oai:dr.ntu.edu.sg:10356/157193 2023-05-15T14:27:35+02:00 Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic Li, Tanghua Khan, Nicole S. Baranskaya, Alisa V. Shaw, Timothy Adam Peltier, W. Richard Stuhne, Gordan R. Wu, Patrick Horton, Benjamin Peter Asian School of the Environment Earth Observatory of Singapore 2022 application/pdf https://hdl.handle.net/10356/157193 https://doi.org/10.1029/2021JB023631 en eng MOE2019 -T3-1-004 MOE2018-T2-1-030 MOE-T2EP50120-0007 Journal of Geophysical Research: Solid Earth Li, T., Khan, N. S., Baranskaya, A. V., Shaw, T. A., Peltier, W. R., Stuhne, G. R., Wu, P. & Horton, B. P. (2022). Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic. Journal of Geophysical Research: Solid Earth, 127(3), e2021JB023631-. https://dx.doi.org/10.1029/2021JB023631 2169-9356 https://hdl.handle.net/10356/157193 doi:10.1029/2021JB023631 2-s2.0-85127448416 3 127 e2021JB023631 © 2022 The Authors.This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes CC-BY-NC Science::Geology Sea-Level Change Glacial Isostatic Adjustment Lateral Heterogeneity Rheology Russian Arctic Journal Article 2022 ftnanyangtu https://doi.org/10.1029/2021JB023631 2022-05-20T00:14:29Z Analyses of glacial isostatic adjustment (GIA) and deglacial relative sea-level (RSL) change in the Russian Arctic deliver important insights into the Earth's viscosity structure and the deglaciation history of the Eurasian ice sheet complex. Here, we validate the 1D GIA models ICE-6G_C (VM5a) and ICE-7G_NA (VM7) and select new 3D GIA models in the Russian Arctic against a quality-controlled deglacial RSL database of >500 sea-level data points from 24 regions. Both 1D models correspond to the RSL data along the southern coast of the Barents Sea and Franz Josef Land from ∼11 ka BP to present but show notable misfits (>50 m at 10 ka BP) with the White Sea data. We find 3D model predictions of deglacial RSL resolve most of the misfits with the observed data for the White Sea while retaining comparable fits in other regions of the Russian Arctic. Our results further reveal: (a) RSL in the western Russian Arctic is sensitive to elastic lithosphere with lateral thickness variation and 3D viscosity structure in the upper mantle; and (b) RSL in the whole Russian Arctic is less sensitive to 3D viscosity structure in the lower mantle compared to the upper mantle. The 3D models reveal a compromise in the upper mantle between the background viscosity and scaling factor to best fit the RSL data, which needs to be considered in future 3D GIA studies. Ministry of Education (MOE) National Research Foundation (NRF) Published version Tanghua Li, Timothy A. Shaw, and Benjamin P. Horton are supported by the Singapore Ministry of Education Academic Research Fund MOE2019 -T3-1-004, MOE2018-T2-1-030 and MOE-T2EP50120-0007, the National Research Foundation Singapore, and the Singapore Ministry of Education, under the Research Centers of Excellence initia- tive. The research of W. Richard Peltier at Toronto is supported by NSERC discov- ery Grant A9627. The work of Alisa Baranskaya was supported by the Russian Science Foundation Grant 22-77-10,031; she used equipment and facilities obtained within the State Budget Theme ... Article in Journal/Newspaper Arctic Arctic Barents Sea Franz Josef Land Ice Sheet White Sea DR-NTU (Digital Repository at Nanyang Technological University, Singapore) Arctic Barents Sea Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Moe ENVELOPE(-45.683,-45.683,-60.733,-60.733) Peltier ENVELOPE(-63.495,-63.495,-64.854,-64.854) Tive ENVELOPE(12.480,12.480,65.107,65.107) White Sea Journal of Geophysical Research: Solid Earth 127 3
institution Open Polar
collection DR-NTU (Digital Repository at Nanyang Technological University, Singapore)
op_collection_id ftnanyangtu
language English
topic Science::Geology
Sea-Level Change
Glacial Isostatic Adjustment
Lateral Heterogeneity
Rheology
Russian Arctic
spellingShingle Science::Geology
Sea-Level Change
Glacial Isostatic Adjustment
Lateral Heterogeneity
Rheology
Russian Arctic
Li, Tanghua
Khan, Nicole S.
Baranskaya, Alisa V.
Shaw, Timothy Adam
Peltier, W. Richard
Stuhne, Gordan R.
Wu, Patrick
Horton, Benjamin Peter
Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
topic_facet Science::Geology
Sea-Level Change
Glacial Isostatic Adjustment
Lateral Heterogeneity
Rheology
Russian Arctic
description Analyses of glacial isostatic adjustment (GIA) and deglacial relative sea-level (RSL) change in the Russian Arctic deliver important insights into the Earth's viscosity structure and the deglaciation history of the Eurasian ice sheet complex. Here, we validate the 1D GIA models ICE-6G_C (VM5a) and ICE-7G_NA (VM7) and select new 3D GIA models in the Russian Arctic against a quality-controlled deglacial RSL database of >500 sea-level data points from 24 regions. Both 1D models correspond to the RSL data along the southern coast of the Barents Sea and Franz Josef Land from ∼11 ka BP to present but show notable misfits (>50 m at 10 ka BP) with the White Sea data. We find 3D model predictions of deglacial RSL resolve most of the misfits with the observed data for the White Sea while retaining comparable fits in other regions of the Russian Arctic. Our results further reveal: (a) RSL in the western Russian Arctic is sensitive to elastic lithosphere with lateral thickness variation and 3D viscosity structure in the upper mantle; and (b) RSL in the whole Russian Arctic is less sensitive to 3D viscosity structure in the lower mantle compared to the upper mantle. The 3D models reveal a compromise in the upper mantle between the background viscosity and scaling factor to best fit the RSL data, which needs to be considered in future 3D GIA studies. Ministry of Education (MOE) National Research Foundation (NRF) Published version Tanghua Li, Timothy A. Shaw, and Benjamin P. Horton are supported by the Singapore Ministry of Education Academic Research Fund MOE2019 -T3-1-004, MOE2018-T2-1-030 and MOE-T2EP50120-0007, the National Research Foundation Singapore, and the Singapore Ministry of Education, under the Research Centers of Excellence initia- tive. The research of W. Richard Peltier at Toronto is supported by NSERC discov- ery Grant A9627. The work of Alisa Baranskaya was supported by the Russian Science Foundation Grant 22-77-10,031; she used equipment and facilities obtained within the State Budget Theme ...
author2 Asian School of the Environment
Earth Observatory of Singapore
format Article in Journal/Newspaper
author Li, Tanghua
Khan, Nicole S.
Baranskaya, Alisa V.
Shaw, Timothy Adam
Peltier, W. Richard
Stuhne, Gordan R.
Wu, Patrick
Horton, Benjamin Peter
author_facet Li, Tanghua
Khan, Nicole S.
Baranskaya, Alisa V.
Shaw, Timothy Adam
Peltier, W. Richard
Stuhne, Gordan R.
Wu, Patrick
Horton, Benjamin Peter
author_sort Li, Tanghua
title Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
title_short Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
title_full Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
title_fullStr Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
title_full_unstemmed Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic
title_sort influence of 3d earth structure on glacial isostatic adjustment in the russian arctic
publishDate 2022
url https://hdl.handle.net/10356/157193
https://doi.org/10.1029/2021JB023631
long_lat ENVELOPE(55.000,55.000,81.000,81.000)
ENVELOPE(-45.683,-45.683,-60.733,-60.733)
ENVELOPE(-63.495,-63.495,-64.854,-64.854)
ENVELOPE(12.480,12.480,65.107,65.107)
geographic Arctic
Barents Sea
Franz Josef Land
Moe
Peltier
Tive
White Sea
geographic_facet Arctic
Barents Sea
Franz Josef Land
Moe
Peltier
Tive
White Sea
genre Arctic
Arctic
Barents Sea
Franz Josef Land
Ice Sheet
White Sea
genre_facet Arctic
Arctic
Barents Sea
Franz Josef Land
Ice Sheet
White Sea
op_relation MOE2019 -T3-1-004
MOE2018-T2-1-030
MOE-T2EP50120-0007
Journal of Geophysical Research: Solid Earth
Li, T., Khan, N. S., Baranskaya, A. V., Shaw, T. A., Peltier, W. R., Stuhne, G. R., Wu, P. & Horton, B. P. (2022). Influence of 3D earth structure on glacial isostatic adjustment in the Russian Arctic. Journal of Geophysical Research: Solid Earth, 127(3), e2021JB023631-. https://dx.doi.org/10.1029/2021JB023631
2169-9356
https://hdl.handle.net/10356/157193
doi:10.1029/2021JB023631
2-s2.0-85127448416
3
127
e2021JB023631
op_rights © 2022 The Authors.This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes
op_rightsnorm CC-BY-NC
op_doi https://doi.org/10.1029/2021JB023631
container_title Journal of Geophysical Research: Solid Earth
container_volume 127
container_issue 3
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