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1000 Titel
  • Mapping geodetically inferred Antarctic ice surface height changes into thickness changes: a sensitivity study
1000 Autor/in
  1. Valencic, Natasha |
  2. Pan, Linda |
  3. Latychev, Konstantin |
  4. Gomez, Natalya |
  5. Powell, Evelyn |
  6. Mitrovica, Jerry X. |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-06-26
1000 Erschienen in
1000 Quellenangabe
  • 18(6):2969-2978
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-2969-2024 |
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1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Determining recent Antarctic ice volume changes from satellite altimeter measurements of ice surface height requires a correction for contemporaneous vertical crustal deformation. This correction must consider two main sources of crustal deformation: (1) ongoing glacial isostatic adjustment (GIA), that is, the deformational, gravitational, and rotational response to Late Pleistocene and Holocene ice and ocean mass changes and (2) modern ice mass change. In this study, we seek to quantify the uncertainties associated with each of these corrections. Corrections of ice surface height changes for correction 1 have generally involved the adoption of global models of GIA defined by some preferred combination of ice history and mantle viscoelastic structure. We have computed the GIA correction generated from a coupled ice sheet–sea level model and a realistic Earth model incorporating three-dimensional viscoelastic structure. Integrating the difference between this correction and those from recent GIA analyses widely adopted in the literature yields an uncertainty in total present-day ice volume change equivalent to approximately 10 % of Antarctic ice mass loss inferred for the period 2010–2020. This reinforces earlier work indicating that ice histories characterized by relatively high excess ice volume at the Last Glacial Maximum may be introducing a significant error in estimates of modern melt rates. Regarding correction 2, a spatially invariant scaling has commonly been used to convert GIA-corrected ice surface height changes obtained from satellite altimetry to ice volume estimates. We adopt modeling results based on a projection of Antarctic ice mass change over the period 2015–2055 to demonstrate a spatial variability in the scaling of up to 10 % across the ice sheet. Furthermore, using these calculations, we find a systematic error of ∼ 3 % in the projected net ice volume change, with most of the difference arising in areas of West Antarctica above mantle zones of low viscosity. </jats:p>
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0009-0002-2902-261X|https://orcid.org/0000-0003-0247-4309|https://frl.publisso.de/adhoc/uri/TGF0eWNoZXYsIEtvbnN0YW50aW4=|https://orcid.org/0000-0002-2463-7917|https://frl.publisso.de/adhoc/uri/UG93ZWxsLCBFdmVseW4=|https://frl.publisso.de/adhoc/uri/TWl0cm92aWNhLCBKZXJyeSBYLg==
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  • DeepGreen-ID: 60a273740d864aedaf40422a2f166356 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
1000 Label
1000 Förderer
  1. Harvard University |
  2. National Science Foundation |
  3. Fonds de recherche du Québec – Nature et technologies |
  4. Natural Sciences and Engineering Research Council of Canada |
  5. Canada Excellence Research Chairs, Government of Canada |
  6. National Aeronautics and Space Administration |
  7. John D. and Catherine T. MacArthur Foundation |
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    1000 Förderer Harvard University |
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    1000 Förderer National Science Foundation |
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    1000 Förderer Fonds de recherche du Québec – Nature et technologies |
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    1000 Förderer Natural Sciences and Engineering Research Council of Canada |
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    1000 Förderer Canada Excellence Research Chairs, Government of Canada |
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    1000 Förderer National Aeronautics and Space Administration |
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    1000 Förderer John D. and Catherine T. MacArthur Foundation |
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