Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+)
We present the result of the third Marine Ice Sheet Model Intercomparison Project, MISMIP+. MISMIP+ is intended to be a benchmark for ice-flow models which include fast sliding marine ice streams and floating ice shelves and in particular a treatment of viscous stress that is sufficient to model but...
Published in: | The Cryosphere |
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Language: | English |
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Online Access: | https://doi.org/10.5194/tc-14-2283-2020 |
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ftncar:oai:drupal-site.org:articles_23533 2024-04-28T08:24:49+00:00 Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) Cornford, Stephen L. (author) Seroussi, Helene (author) Asay-Davis, Xylar S. (author) Gudmundsson, G. Hilmar (author) Arthern, Rob (author) Borstad, Chris (author) Christmann, Julia (author) Dias dos Santos, Thiago (author) Feldmann, Johannes (author) Goldberg, Daniel (author) Hoffman, Matthew J. (author) Humbert, Angelika (author) Kleiner, Thomas (author) Leguy, Gunter (author) Lipscomb, William H. (author) Merino, Nacho (author) Durand, Gaël (author) Morlighem, Mathieu (author) Pollard, David (author) Rückamp, Martin (author) Williams, C. Rosie (author) Yu, Hongju (author) 2020-07-21 https://doi.org/10.5194/tc-14-2283-2020 en eng The Cryosphere--The Cryosphere--1994-0424 articles:23533 ark:/85065/d7m61ph5 doi:10.5194/tc-14-2283-2020 Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2020 ftncar https://doi.org/10.5194/tc-14-2283-2020 2024-04-04T17:34:52Z We present the result of the third Marine Ice Sheet Model Intercomparison Project, MISMIP+. MISMIP+ is intended to be a benchmark for ice-flow models which include fast sliding marine ice streams and floating ice shelves and in particular a treatment of viscous stress that is sufficient to model buttressing, where upstream ice flow is restrained by a downstream ice shelf. A set of idealized experiments first tests that models are able to maintain a steady state with the grounding line located on a retrograde slope due to buttressing and then explore scenarios where a reduction in that buttressing causes ice stream acceleration, thinning, and grounding line retreat. The majority of participating models passed the first test and then produced similar responses to the loss of buttressing. We find that the most important distinction between models in this particular type of simulation is in the treatment of sliding at the bed, with other distinctions - notably the difference between the simpler and more complete treatments of englacial stress but also the differences between numerical methods - taking a secondary role. 1852977 Article in Journal/Newspaper Ice Sheet Ice Shelf Ice Shelves The Cryosphere OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) The Cryosphere 14 7 2283 2301 |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
We present the result of the third Marine Ice Sheet Model Intercomparison Project, MISMIP+. MISMIP+ is intended to be a benchmark for ice-flow models which include fast sliding marine ice streams and floating ice shelves and in particular a treatment of viscous stress that is sufficient to model buttressing, where upstream ice flow is restrained by a downstream ice shelf. A set of idealized experiments first tests that models are able to maintain a steady state with the grounding line located on a retrograde slope due to buttressing and then explore scenarios where a reduction in that buttressing causes ice stream acceleration, thinning, and grounding line retreat. The majority of participating models passed the first test and then produced similar responses to the loss of buttressing. We find that the most important distinction between models in this particular type of simulation is in the treatment of sliding at the bed, with other distinctions - notably the difference between the simpler and more complete treatments of englacial stress but also the differences between numerical methods - taking a secondary role. 1852977 |
author2 |
Cornford, Stephen L. (author) Seroussi, Helene (author) Asay-Davis, Xylar S. (author) Gudmundsson, G. Hilmar (author) Arthern, Rob (author) Borstad, Chris (author) Christmann, Julia (author) Dias dos Santos, Thiago (author) Feldmann, Johannes (author) Goldberg, Daniel (author) Hoffman, Matthew J. (author) Humbert, Angelika (author) Kleiner, Thomas (author) Leguy, Gunter (author) Lipscomb, William H. (author) Merino, Nacho (author) Durand, Gaël (author) Morlighem, Mathieu (author) Pollard, David (author) Rückamp, Martin (author) Williams, C. Rosie (author) Yu, Hongju (author) |
format |
Article in Journal/Newspaper |
title |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
spellingShingle |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
title_short |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
title_full |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
title_fullStr |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
title_full_unstemmed |
Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+) |
title_sort |
results of the third marine ice sheet model intercomparison project (mismip+) |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-14-2283-2020 |
genre |
Ice Sheet Ice Shelf Ice Shelves The Cryosphere |
genre_facet |
Ice Sheet Ice Shelf Ice Shelves The Cryosphere |
op_relation |
The Cryosphere--The Cryosphere--1994-0424 articles:23533 ark:/85065/d7m61ph5 doi:10.5194/tc-14-2283-2020 |
op_rights |
Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. |
op_doi |
https://doi.org/10.5194/tc-14-2283-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
7 |
container_start_page |
2283 |
op_container_end_page |
2301 |
_version_ |
1797584858943324160 |