Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS
In this thesis, we consider surface loading effects associated with our dynamic cryosphere. Glacial Isostatic Adjustment (GIA) models have been used to constrain the extent of past ice sheets and viscoelastic Earth structure, and to correct geodetic and geological observations for ice age effects. T...
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ftharvardudash:oai:dash.harvard.edu:1/37370254 2023-05-15T14:02:08+02:00 Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS Powell, Evelyn Mitrovica, Jerry X Denolle, Marine Huybers, Peter McColl, Kaighin 2021 application/pdf https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37370254 en eng Powell, Evelyn. 2021. Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS. Doctoral dissertation, Harvard University Graduate School of Arts and Sciences. 28769801 https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37370254 orcid:0000-0001-7661-5878 Geophysics Thesis or Dissertation text 2021 ftharvardudash 2022-04-05T18:53:05Z In this thesis, we consider surface loading effects associated with our dynamic cryosphere. Glacial Isostatic Adjustment (GIA) models have been used to constrain the extent of past ice sheets and viscoelastic Earth structure, and to correct geodetic and geological observations for ice age effects. These models, however, often only consider depth-dependent variations in Earth viscosity and lithospheric structure. Seismic, geological, and geodetic evidence indicates the Antarctic Ice Sheet is underlain by complex, high amplitude variability in 3-D viscoelastic structure. In contrast with West Antarctica’s low viscosity mantle, Canada, the location of the former Laurentide Ice Sheet, is underlain by a thick craton and mantle viscosities higher than the global average. GIA modeling with 3-D mantle structure requires greater model specificity and fidelity, but will also provide a deeper understanding of the past and future evolution of the cryosphere. Our investigation is motivated by two questions: How does 3-D Earth structure impact observations of GIA-induced deformation, and how will 3-D Earth structure affect predictions of sea-level change? We compute gravitationally self-consistent uplift, gravity, and sea-level changes and show that 3-D Earth structure will have significant effects on sea-level changes associated with West Antarctic Ice Sheet melt during interglacial periods. Further, we show that Antarctica’s viscoelastic structure will impact geodetic observables even for timescales when the Earth is commonly treated as a purely elastic body. We demonstrate how the bias in crustal deformation induced by this 3-D structure will impact standard methods to use GPS observations to infer viscoelastic structure in West Antarctica. Finally, we use sea-level modeling to estimate the emergence of an island from Canada’s waters in order to corroborate an Indigenous people’s land claim. Thesis Antarc* Antarctic Antarctica Ice Sheet West Antarctica Harvard University: DASH - Digital Access to Scholarship at Harvard Antarctic The Antarctic West Antarctica West Antarctic Ice Sheet Canada |
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Harvard University: DASH - Digital Access to Scholarship at Harvard |
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ftharvardudash |
language |
English |
topic |
Geophysics |
spellingShingle |
Geophysics Powell, Evelyn Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
topic_facet |
Geophysics |
description |
In this thesis, we consider surface loading effects associated with our dynamic cryosphere. Glacial Isostatic Adjustment (GIA) models have been used to constrain the extent of past ice sheets and viscoelastic Earth structure, and to correct geodetic and geological observations for ice age effects. These models, however, often only consider depth-dependent variations in Earth viscosity and lithospheric structure. Seismic, geological, and geodetic evidence indicates the Antarctic Ice Sheet is underlain by complex, high amplitude variability in 3-D viscoelastic structure. In contrast with West Antarctica’s low viscosity mantle, Canada, the location of the former Laurentide Ice Sheet, is underlain by a thick craton and mantle viscosities higher than the global average. GIA modeling with 3-D mantle structure requires greater model specificity and fidelity, but will also provide a deeper understanding of the past and future evolution of the cryosphere. Our investigation is motivated by two questions: How does 3-D Earth structure impact observations of GIA-induced deformation, and how will 3-D Earth structure affect predictions of sea-level change? We compute gravitationally self-consistent uplift, gravity, and sea-level changes and show that 3-D Earth structure will have significant effects on sea-level changes associated with West Antarctic Ice Sheet melt during interglacial periods. Further, we show that Antarctica’s viscoelastic structure will impact geodetic observables even for timescales when the Earth is commonly treated as a purely elastic body. We demonstrate how the bias in crustal deformation induced by this 3-D structure will impact standard methods to use GPS observations to infer viscoelastic structure in West Antarctica. Finally, we use sea-level modeling to estimate the emergence of an island from Canada’s waters in order to corroborate an Indigenous people’s land claim. |
author2 |
Mitrovica, Jerry X Denolle, Marine Huybers, Peter McColl, Kaighin |
format |
Thesis |
author |
Powell, Evelyn |
author_facet |
Powell, Evelyn |
author_sort |
Powell, Evelyn |
title |
Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
title_short |
Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
title_full |
Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
title_fullStr |
Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
title_full_unstemmed |
Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS |
title_sort |
glacial isostatic adjustment in a region of complex earth structure: the case of wais |
publishDate |
2021 |
url |
https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37370254 |
geographic |
Antarctic The Antarctic West Antarctica West Antarctic Ice Sheet Canada |
geographic_facet |
Antarctic The Antarctic West Antarctica West Antarctic Ice Sheet Canada |
genre |
Antarc* Antarctic Antarctica Ice Sheet West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet West Antarctica |
op_relation |
Powell, Evelyn. 2021. Glacial Isostatic Adjustment in a region of complex Earth structure: The case of WAIS. Doctoral dissertation, Harvard University Graduate School of Arts and Sciences. 28769801 https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37370254 orcid:0000-0001-7661-5878 |
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1766272221545758720 |