Spatio-temporal variability of processes across Antarctic ice-bed–ocean interfaces

Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge...

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Vydáno v:Nature communications Ročník 9; číslo 1; s. 2289 - 14
Hlavní autoři: Colleoni, Florence, De Santis, Laura, Siddoway, Christine S., Bergamasco, Andrea, Golledge, Nicholas R., Lohmann, Gerrit, Passchier, Sandra, Siegert, Martin J.
Médium: Journal Article
Jazyk:angličtina
Vydáno: London Nature Publishing Group UK 18.06.2018
Nature Publishing Group
Nature Portfolio
Témata:
704/106/125
704/106/2738
704/106/413
704/2151/210
Aquifers
Climate change
Deformation
Global warming
Humanities and Social Sciences
Hydrologic models
Hydrology
Ice sheets
Ice shelves
Interfaces
Mathematical models
Morphology
multidisciplinary
Review
Review Article
Science
Science (multidisciplinary)
Sediments
Topography
ISSN:2041-1723, 2041-1723
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Abstract Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic’s system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research. Understudied in the Antarctic system are the subsurface interfaces between ice-sheet, ocean and geological substrate. Here, the authors review our understanding of these components and propose new avenues of holistic dynamic modeling to achieve a unified understanding of past, present and future polar climate.
AbstractList Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic's system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research.
Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic’s system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research. Understudied in the Antarctic system are the subsurface interfaces between ice-sheet, ocean and geological substrate. Here, the authors review our understanding of these components and propose new avenues of holistic dynamic modeling to achieve a unified understanding of past, present and future polar climate.
Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic’s system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research. Understudied in the Antarctic system are the subsurface interfaces between ice-sheet, ocean and geological substrate. Here, the authors review our understanding of these components and propose new avenues of holistic dynamic modeling to achieve a unified understanding of past, present and future polar climate.
Understudied in the Antarctic system are the subsurface interfaces between ice-sheet, ocean and geological substrate. Here, the authors review our understanding of these components and propose new avenues of holistic dynamic modeling to achieve a unified understanding of past, present and future polar climate.
Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic's system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research.Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic's system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research.
Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic’s system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research.
ArticleNumber 2289
Author Lohmann, Gerrit
Colleoni, Florence
Golledge, Nicholas R.
De Santis, Laura
Passchier, Sandra
Siddoway, Christine S.
Siegert, Martin J.
Bergamasco, Andrea
Author_xml – sequence: 1
  givenname: Florence
  surname: Colleoni
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– sequence: 2
  givenname: Laura
  surname: De Santis
  fullname: De Santis, Laura
  organization: Istituto Nazionale di Oceanografia Sperimentale
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  givenname: Christine S.
  orcidid: 0000-0003-0478-6138
  surname: Siddoway
  fullname: Siddoway, Christine S.
  organization: Department of Geology, Colorado College
– sequence: 4
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  surname: Bergamasco
  fullname: Bergamasco, Andrea
  organization: Centro Nazionale delle Ricerche - Istituto di Scienze Marine
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  givenname: Nicholas R.
  orcidid: 0000-0001-7676-8970
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  organization: Antarctic Research Centre, Victoria University of Wellington, GNS Science, Avalon
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  organization: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, University of Bremen
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  surname: Passchier
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  organization: Department of Earth and Environmental Studies, Center for Environmental and Life Sciences, Montclair State University
– sequence: 8
  givenname: Martin J.
  orcidid: 0000-0002-0090-4806
  surname: Siegert
  fullname: Siegert, Martin J.
  organization: Grantham Institute and Department of Earth Science and Engineering, Imperial College of London
BackLink https://www.ncbi.nlm.nih.gov/pubmed/29915266$$D View this record in MEDLINE/PubMed
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PublicationTitleAbbrev Nat Commun
PublicationTitleAlternate Nat Commun
PublicationYear 2018
Publisher Nature Publishing Group UK
Nature Publishing Group
Nature Portfolio
Publisher_xml – name: Nature Publishing Group UK
– name: Nature Publishing Group
– name: Nature Portfolio
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Snippet Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models,...
Understudied in the Antarctic system are the subsurface interfaces between ice-sheet, ocean and geological substrate. Here, the authors review our...
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704/106/2738
704/106/413
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Climate change
Deformation
Global warming
Humanities and Social Sciences
Hydrologic models
Hydrology
Ice sheets
Ice shelves
Interfaces
Mathematical models
Morphology
multidisciplinary
Review
Review Article
Science
Science (multidisciplinary)
Sediments
Topography
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Title Spatio-temporal variability of processes across Antarctic ice-bed–ocean interfaces
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