An assessment of global and regional sea level for years 1993–2007 in a suite of interannual CORE-II simulations

•Global mean sea level simulated in interannual CORE simulations.•Regional sea level patterns simulated in interannual CORE simulations.•Theoretical foundation for analysis of global mean sea level and regional patterns. We provide an assessment of sea level simulated in a suite of global ocean-sea...

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Published inOcean modelling (Oxford) Vol. 78; pp. 35 - 89
Main Authors Griffies, Stephen M., Yin, Jianjun, Durack, Paul J., Goddard, Paul, Bates, Susan C., Behrens, Erik, Bentsen, Mats, Bi, Daohua, Biastoch, Arne, Böning, Claus W., Bozec, Alexandra, Chassignet, Eric, Danabasoglu, Gokhan, Danilov, Sergey, Domingues, Catia M., Drange, Helge, Farneti, Riccardo, Fernandez, Elodie, Greatbatch, Richard J., Holland, David M., Ilicak, Mehmet, Large, William G., Lorbacher, Katja, Lu, Jianhua, Marsland, Simon J., Mishra, Akhilesh, George Nurser, A.J., Salas y Mélia, David, Palter, Jaime B., Samuels, Bonita L., Schröter, Jens, Schwarzkopf, Franziska U., Sidorenko, Dmitry, Treguier, Anne Marie, Tseng, Yu-heng, Tsujino, Hiroyuki, Uotila, Petteri, Valcke, Sophie, Voldoire, Aurore, Wang, Qiang, Winton, Michael, Zhang, Xuebin
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.06.2014
Elsevier
Subjects
Online AccessGet full text
ISSN1463-5003
1463-5011
DOI10.1016/j.ocemod.2014.03.004

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Abstract •Global mean sea level simulated in interannual CORE simulations.•Regional sea level patterns simulated in interannual CORE simulations.•Theoretical foundation for analysis of global mean sea level and regional patterns. We provide an assessment of sea level simulated in a suite of global ocean-sea ice models using the interannual CORE atmospheric state to determine surface ocean boundary buoyancy and momentum fluxes. These CORE-II simulations are compared amongst themselves as well as to observation-based estimates. We focus on the final 15years of the simulations (1993–2007), as this is a period where the CORE-II atmospheric state is well sampled, and it allows us to compare sea level related fields to both satellite and in situ analyses. The ensemble mean of the CORE-II simulations broadly agree with various global and regional observation-based analyses during this period, though with the global mean thermosteric sea level rise biased low relative to observation-based analyses. The simulations reveal a positive trend in dynamic sea level in the west Pacific and negative trend in the east, with this trend arising from wind shifts and regional changes in upper 700m ocean heat content. The models also exhibit a thermosteric sea level rise in the subpolar North Atlantic associated with a transition around 1995/1996 of the North Atlantic Oscillation to its negative phase, and the advection of warm subtropical waters into the subpolar gyre. Sea level trends are predominantly associated with steric trends, with thermosteric effects generally far larger than halosteric effects, except in the Arctic and North Atlantic. There is a general anti-correlation between thermosteric and halosteric effects for much of the World Ocean, associated with density compensated changes.
AbstractList We provide an assessment of sea level simulated in a suite of global ocean-sea ice models using the interannual CORE atmospheric state to determine surface ocean boundary buoyancy and momentum fluxes. These CORE-II simulations are compared amongst themselves as well as to observation-based estimates. We focus on the final 15years of the simulations (1993-2007), as this is a period where the CORE-II atmospheric state is well sampled, and it allows us to compare sea level related fields to both satellite and in situ analyses. The ensemble mean of the CORE-II simulations broadly agree with various global and regional observation-based analyses during this period, though with the global mean thermosteric sea level rise biased low relative to observation-based analyses. The simulations reveal a positive trend in dynamic sea level in the west Pacific and negative trend in the east, with this trend arising from wind shifts and regional changes in upper 700m ocean heat content. The models also exhibit a thermosteric sea level rise in the subpolar North Atlantic associated with a transition around 1995/1996 of the North Atlantic Oscillation to its negative phase, and the advection of warm subtropical waters into the subpolar gyre. Sea level trends are predominantly associated with steric trends, with thermosteric effects generally far larger than halosteric effects, except in the Arctic and North Atlantic. There is a general anti-correlation between thermosteric and halosteric effects for much of the World Ocean, associated with density compensated changes.
•Global mean sea level simulated in interannual CORE simulations.•Regional sea level patterns simulated in interannual CORE simulations.•Theoretical foundation for analysis of global mean sea level and regional patterns. We provide an assessment of sea level simulated in a suite of global ocean-sea ice models using the interannual CORE atmospheric state to determine surface ocean boundary buoyancy and momentum fluxes. These CORE-II simulations are compared amongst themselves as well as to observation-based estimates. We focus on the final 15years of the simulations (1993–2007), as this is a period where the CORE-II atmospheric state is well sampled, and it allows us to compare sea level related fields to both satellite and in situ analyses. The ensemble mean of the CORE-II simulations broadly agree with various global and regional observation-based analyses during this period, though with the global mean thermosteric sea level rise biased low relative to observation-based analyses. The simulations reveal a positive trend in dynamic sea level in the west Pacific and negative trend in the east, with this trend arising from wind shifts and regional changes in upper 700m ocean heat content. The models also exhibit a thermosteric sea level rise in the subpolar North Atlantic associated with a transition around 1995/1996 of the North Atlantic Oscillation to its negative phase, and the advection of warm subtropical waters into the subpolar gyre. Sea level trends are predominantly associated with steric trends, with thermosteric effects generally far larger than halosteric effects, except in the Arctic and North Atlantic. There is a general anti-correlation between thermosteric and halosteric effects for much of the World Ocean, associated with density compensated changes.
We provide an assessment of sea level simulated in a suite of global ocean-sea ice models using the interannual CORE atmospheric state to determine surface ocean boundary buoyancy and momentum fluxes. These CORE-II simulations are compared amongst themselves as well as to observation-based estimates. We focus on the final 15 years of the simulations (1993–2007), as this is a period where the CORE-II atmospheric state is well sampled, and it allows us to compare sea level related fields to both satellite and in situ analyses. The ensemble mean of the CORE-II simulations broadly agree with various global and regional observation-based analyses during this period, though with the global mean thermosteric sea level rise biased low relative to observation-based analyses. The simulations reveal a positive trend in dynamic sea level in the west Pacific and negative trend in the east, with this trend arising from wind shifts and regional changes in upper 700 m ocean heat content. The models also exhibit a thermosteric sea level rise in the subpolar North Atlantic associated with a transition around 1995/1996 of the North Atlantic Oscillation to its negative phase, and the advection of warm subtropical waters into the subpolar gyre. Sea level trends are predominantly associated with steric trends, with thermosteric effects generally far larger than halosteric effects, except in the Arctic and North Atlantic. There is a general anti-correlation between thermosteric and halosteric effects for much of the World Ocean, associated with density compensated changes.
Author Danabasoglu, Gokhan
Ilicak, Mehmet
Lu, Jianhua
Mishra, Akhilesh
Valcke, Sophie
Wang, Qiang
Biastoch, Arne
Domingues, Catia M.
Schwarzkopf, Franziska U.
Bi, Daohua
Samuels, Bonita L.
Yin, Jianjun
Farneti, Riccardo
Palter, Jaime B.
Bentsen, Mats
Drange, Helge
Greatbatch, Richard J.
Holland, David M.
Uotila, Petteri
Griffies, Stephen M.
Marsland, Simon J.
Durack, Paul J.
Treguier, Anne Marie
Chassignet, Eric
Winton, Michael
Bates, Susan C.
Zhang, Xuebin
Behrens, Erik
Voldoire, Aurore
Böning, Claus W.
Large, William G.
Sidorenko, Dmitry
Goddard, Paul
Salas y Mélia, David
Tsujino, Hiroyuki
Danilov, Sergey
Lorbacher, Katja
Fernandez, Elodie
Tseng, Yu-heng
George Nurser, A.J.
Schröter, Jens
Bozec, Alexandra
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  organization: Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Australia
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  organization: University of Bergen, Bergen, Norway
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  organization: International Centre for Theoretical Physics (ICTP), Trieste, Italy
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  surname: Fernandez
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Steric sea level
Global sea level
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Sea level
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Snippet •Global mean sea level simulated in interannual CORE simulations.•Regional sea level patterns simulated in interannual CORE simulations.•Theoretical foundation...
We provide an assessment of sea level simulated in a suite of global ocean-sea ice models using the interannual CORE atmospheric state to determine surface...
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SubjectTerms Assessments
Atmospherics
Computer simulation
CORE global ocean-ice simulations
Earth Sciences
Global sea level
North Atlantic oscillation
Ocean heat content
Oceanography
Oceans
Regional
Sciences of the Universe
Sea level
Steric sea level
Trends
Title An assessment of global and regional sea level for years 1993–2007 in a suite of interannual CORE-II simulations
URI https://dx.doi.org/10.1016/j.ocemod.2014.03.004
https://www.proquest.com/docview/1627975742
https://www.proquest.com/docview/1642261222
https://hal.science/hal-01132137
Volume 78
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