Rapid submarine ice melting in the grounding zones of ice shelves in West Antarctica
Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE’s major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne...
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| Veröffentlicht in: | Nature communications Jg. 7; H. 1; S. 13243 - 8 |
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| Abstract | Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE’s major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300–490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica.
Ice-shelf bottom melting is thought to cause mass loss in West Antarctica. Here, the authors analyse radar observations of the Dotson and Crosson ice shelves to directly quantify grounding zone unbalanced melting of up to 70 m per year, and illustrate its relation with bed topography and grounding line retreat. |
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| AbstractList | Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300–490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica. Ice-shelf bottom melting is thought to cause mass loss in West Antarctica. Here, the authors analyse radar observations of the Dotson and Crosson ice shelves to directly quantify grounding zone unbalanced melting of up to 70 m per year, and illustrate its relation with bed topography and grounding line retreat. Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300-490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica.Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300-490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica. Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300-490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica. Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE’s major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope and Kohler glaciers. Melting in the grounding zones is found to be much higher than steady-state levels, removing 300–490 m of solid ice between 2002 and 2009 beneath the retreating Smith Glacier. The vigorous, unbalanced melting supports the hypothesis that a significant increase in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s. The synchronous but diverse evolutions of these glaciers illustrate how combinations of oceanography and topography modulate rapid submarine melting to hasten mass loss and glacier retreat from West Antarctica. Ice-shelf bottom melting is thought to cause mass loss in West Antarctica. Here, the authors analyse radar observations of the Dotson and Crosson ice shelves to directly quantify grounding zone unbalanced melting of up to 70 m per year, and illustrate its relation with bed topography and grounding line retreat. Ice-shelf bottom melting is thought to cause mass loss in West Antarctica. Here, the authors analyse radar observations of the Dotson and Crosson ice shelves to directly quantify grounding zone unbalanced melting of up to 70 m per year, and illustrate its relation with bed topography and grounding line retreat. |
| ArticleNumber | 13243 |
| Author | Seroussi, Helene Scheuchl, Bernd Khazendar, Ala Schroeder, Dustin M. Velicogna, Isabella Rignot, Eric Mouginot, Jeremie Sutterley, Tyler C. Schodlok, Michael P. |
| Author_xml | – sequence: 1 givenname: Ala surname: Khazendar fullname: Khazendar, Ala email: ala@jpl.nasa.gov organization: Jet Propulsion Laboratory, California Institute of Technology – sequence: 2 givenname: Eric orcidid: 0000-0002-3366-0481 surname: Rignot fullname: Rignot, Eric organization: Jet Propulsion Laboratory, California Institute of Technology, Department of Earth System Science, University of California – sequence: 3 givenname: Dustin M. surname: Schroeder fullname: Schroeder, Dustin M. organization: Jet Propulsion Laboratory, California Institute of Technology – sequence: 4 givenname: Helene orcidid: 0000-0001-9201-1644 surname: Seroussi fullname: Seroussi, Helene organization: Jet Propulsion Laboratory, California Institute of Technology – sequence: 5 givenname: Michael P. surname: Schodlok fullname: Schodlok, Michael P. organization: Jet Propulsion Laboratory, California Institute of Technology – sequence: 6 givenname: Bernd surname: Scheuchl fullname: Scheuchl, Bernd organization: Department of Earth System Science, University of California – sequence: 7 givenname: Jeremie surname: Mouginot fullname: Mouginot, Jeremie organization: Department of Earth System Science, University of California – sequence: 8 givenname: Tyler C. surname: Sutterley fullname: Sutterley, Tyler C. organization: Department of Earth System Science, University of California – sequence: 9 givenname: Isabella surname: Velicogna fullname: Velicogna, Isabella organization: Jet Propulsion Laboratory, California Institute of Technology, Department of Earth System Science, University of California |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/27780191$$D View this record in MEDLINE/PubMed |
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| Snippet | Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in... Ice-shelf bottom melting is thought to cause mass loss in West Antarctica. Here, the authors analyse radar observations of the Dotson and Crosson ice shelves... |
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| StartPage | 13243 |
| SubjectTerms | 704/106/125 704/829/2737 Airborne radar Anchor ice Equilibrium Glaciers Humanities and Social Sciences Hypotheses Ice Ice shelves Melting multidisciplinary Oceanography Science Science (multidisciplinary) Topography |
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| Title | Rapid submarine ice melting in the grounding zones of ice shelves in West Antarctica |
| URI | https://link.springer.com/article/10.1038/ncomms13243 https://www.ncbi.nlm.nih.gov/pubmed/27780191 https://www.proquest.com/docview/1831879648 https://www.proquest.com/docview/1835676504 https://pubmed.ncbi.nlm.nih.gov/PMC5093338 https://doaj.org/article/ec59c5a6e1684f98b414ff5ee6013c3b |
| Volume | 7 |
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