Sea level change in response to melting of ice sheets
Relative sea level change is estimated with a combination of methods. First a melting scenario with reasonable fresh water input from Greenland ice sheet, glaciers in Alaska or West-Antarctica between 50 and 200 Gt per year are assumed and used as sources in a global Finite Element Sea-Ice Ocean Mod...
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ftawi:oai:epic.awi.de:33782 2024-09-15T17:43:39+00:00 Sea level change in response to melting of ice sheets Brunnabend, Sandra-Esther Schröter, Jens Ivchenko, Vladimir Kusche, Jürgen Rietbroek, Roelof 2013 https://epic.awi.de/id/eprint/33782/ https://hdl.handle.net/10013/epic.42187 unknown Brunnabend, S. E. , Schröter, J. orcid:0000-0002-9240-5798 , Ivchenko, V. , Kusche, J. and Rietbroek, R. (2013) Sea level change in response to melting of ice sheets , IAHS - IAPSO - IASPEI Joint Assembly, Göteborg, July 2013 - unspecified . hdl:10013/epic.42187 EPIC3IAHS - IAPSO - IASPEI Joint Assembly, Göteborg, 2013-07 Conference notRev 2013 ftawi 2024-06-24T04:07:26Z Relative sea level change is estimated with a combination of methods. First a melting scenario with reasonable fresh water input from Greenland ice sheet, glaciers in Alaska or West-Antarctica between 50 and 200 Gt per year are assumed and used as sources in a global Finite Element Sea-Ice Ocean Model (FESOM). The model calculates the evolution of ocean volume and mass using a non linear free sea surface. Other driving forces are atmospheric surface fluxes from NCEP reanalysis and river runoff from hydrologic modelling. The resulting sea level change due to inflow of mass, steric expansion and redistribution as a consequence of ocean dynamic reactions are calculated relative to the geoid. Geoid changes as a response to the changed mass distribution and the associated uplift are calculated in a second step and are augmented by rotational feedback. Finally glacio-isostatic adjustment is used to correct for ongoing vertical movements. A significant fraction of the sea level variations at the North Atlantic coasts can already be explained by our reference experiment (no extra melting prescribed). Including ice sheet melting substantially improves the comparison between modelled sea level and PSMSL tide gauge records. Conference Object Antarc* Antarctica glaciers Greenland Ice Sheet North Atlantic Sea ice West Antarctica Alaska Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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description |
Relative sea level change is estimated with a combination of methods. First a melting scenario with reasonable fresh water input from Greenland ice sheet, glaciers in Alaska or West-Antarctica between 50 and 200 Gt per year are assumed and used as sources in a global Finite Element Sea-Ice Ocean Model (FESOM). The model calculates the evolution of ocean volume and mass using a non linear free sea surface. Other driving forces are atmospheric surface fluxes from NCEP reanalysis and river runoff from hydrologic modelling. The resulting sea level change due to inflow of mass, steric expansion and redistribution as a consequence of ocean dynamic reactions are calculated relative to the geoid. Geoid changes as a response to the changed mass distribution and the associated uplift are calculated in a second step and are augmented by rotational feedback. Finally glacio-isostatic adjustment is used to correct for ongoing vertical movements. A significant fraction of the sea level variations at the North Atlantic coasts can already be explained by our reference experiment (no extra melting prescribed). Including ice sheet melting substantially improves the comparison between modelled sea level and PSMSL tide gauge records. |
format |
Conference Object |
author |
Brunnabend, Sandra-Esther Schröter, Jens Ivchenko, Vladimir Kusche, Jürgen Rietbroek, Roelof |
spellingShingle |
Brunnabend, Sandra-Esther Schröter, Jens Ivchenko, Vladimir Kusche, Jürgen Rietbroek, Roelof Sea level change in response to melting of ice sheets |
author_facet |
Brunnabend, Sandra-Esther Schröter, Jens Ivchenko, Vladimir Kusche, Jürgen Rietbroek, Roelof |
author_sort |
Brunnabend, Sandra-Esther |
title |
Sea level change in response to melting of ice sheets |
title_short |
Sea level change in response to melting of ice sheets |
title_full |
Sea level change in response to melting of ice sheets |
title_fullStr |
Sea level change in response to melting of ice sheets |
title_full_unstemmed |
Sea level change in response to melting of ice sheets |
title_sort |
sea level change in response to melting of ice sheets |
publishDate |
2013 |
url |
https://epic.awi.de/id/eprint/33782/ https://hdl.handle.net/10013/epic.42187 |
genre |
Antarc* Antarctica glaciers Greenland Ice Sheet North Atlantic Sea ice West Antarctica Alaska |
genre_facet |
Antarc* Antarctica glaciers Greenland Ice Sheet North Atlantic Sea ice West Antarctica Alaska |
op_source |
EPIC3IAHS - IAPSO - IASPEI Joint Assembly, Göteborg, 2013-07 |
op_relation |
Brunnabend, S. E. , Schröter, J. orcid:0000-0002-9240-5798 , Ivchenko, V. , Kusche, J. and Rietbroek, R. (2013) Sea level change in response to melting of ice sheets , IAHS - IAPSO - IASPEI Joint Assembly, Göteborg, July 2013 - unspecified . hdl:10013/epic.42187 |
_version_ |
1810490745297043456 |