The nonlinear equation of state of sea water and the global water mass distribution

The role of nonlinearities of the equation of state (EOS) of seawater for the distribution of water masses in the global ocean is examined through simulations with an ocean general circulation model with various manipulated versions of the EOS. A simulation with a strongly simplified EOS, which cont...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Nycander, Jonas, Hieronymus, Magnus, Roquet, Fabien
Format: Article in Journal/Newspaper
Language:English
Published: Stockholms universitet, Meteorologiska institutionen (MISU) 2015
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123384
https://doi.org/10.1002/2015GL065525
id ftstockholmuniv:oai:DiVA.org:su-123384
record_format openpolar
spelling ftstockholmuniv:oai:DiVA.org:su-123384 2023-05-15T14:01:56+02:00 The nonlinear equation of state of sea water and the global water mass distribution Nycander, Jonas Hieronymus, Magnus Roquet, Fabien 2015 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123384 https://doi.org/10.1002/2015GL065525 eng eng Stockholms universitet, Meteorologiska institutionen (MISU) Geophysical Research Letters, 0094-8276, 2015, 42:18, s. 7714-7721 orcid:0000-0002-4414-6859 orcid:0000-0003-1124-4564 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123384 doi:10.1002/2015GL065525 ISI:000363412400059 info:eu-repo/semantics/openAccess water mass distribution cabbeling thermobaricity 4532 General circulation 4515 Deep recirculations Oceanography Hydrology and Water Resources Oceanografi hydrologi och vattenresurser Article in journal info:eu-repo/semantics/article text 2015 ftstockholmuniv https://doi.org/10.1002/2015GL065525 2023-02-23T21:41:29Z The role of nonlinearities of the equation of state (EOS) of seawater for the distribution of water masses in the global ocean is examined through simulations with an ocean general circulation model with various manipulated versions of the EOS. A simulation with a strongly simplified EOS, which contains only two nonlinear terms, still produces a realistic water mass distribution, demonstrating that these two nonlinearities are indeed the essential ones. Further simulations show that each of these two nonlinear terms affects a specific aspect of the water mass distribution: the cabbeling term is crucial for the formation of Antarctic Intermediate Water and the thermobaric term for the layering of North Atlantic Deep Water and Antarctic Bottom Water. Article in Journal/Newspaper Antarc* Antarctic North Atlantic Deep Water North Atlantic Stockholm University: Publications (DiVA) Antarctic Geophysical Research Letters 42 18 7714 7721
institution Open Polar
collection Stockholm University: Publications (DiVA)
op_collection_id ftstockholmuniv
language English
topic water mass distribution
cabbeling
thermobaricity
4532 General circulation
4515 Deep recirculations
Oceanography
Hydrology and Water Resources
Oceanografi
hydrologi och vattenresurser
spellingShingle water mass distribution
cabbeling
thermobaricity
4532 General circulation
4515 Deep recirculations
Oceanography
Hydrology and Water Resources
Oceanografi
hydrologi och vattenresurser
Nycander, Jonas
Hieronymus, Magnus
Roquet, Fabien
The nonlinear equation of state of sea water and the global water mass distribution
topic_facet water mass distribution
cabbeling
thermobaricity
4532 General circulation
4515 Deep recirculations
Oceanography
Hydrology and Water Resources
Oceanografi
hydrologi och vattenresurser
description The role of nonlinearities of the equation of state (EOS) of seawater for the distribution of water masses in the global ocean is examined through simulations with an ocean general circulation model with various manipulated versions of the EOS. A simulation with a strongly simplified EOS, which contains only two nonlinear terms, still produces a realistic water mass distribution, demonstrating that these two nonlinearities are indeed the essential ones. Further simulations show that each of these two nonlinear terms affects a specific aspect of the water mass distribution: the cabbeling term is crucial for the formation of Antarctic Intermediate Water and the thermobaric term for the layering of North Atlantic Deep Water and Antarctic Bottom Water.
format Article in Journal/Newspaper
author Nycander, Jonas
Hieronymus, Magnus
Roquet, Fabien
author_facet Nycander, Jonas
Hieronymus, Magnus
Roquet, Fabien
author_sort Nycander, Jonas
title The nonlinear equation of state of sea water and the global water mass distribution
title_short The nonlinear equation of state of sea water and the global water mass distribution
title_full The nonlinear equation of state of sea water and the global water mass distribution
title_fullStr The nonlinear equation of state of sea water and the global water mass distribution
title_full_unstemmed The nonlinear equation of state of sea water and the global water mass distribution
title_sort nonlinear equation of state of sea water and the global water mass distribution
publisher Stockholms universitet, Meteorologiska institutionen (MISU)
publishDate 2015
url http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123384
https://doi.org/10.1002/2015GL065525
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
North Atlantic Deep Water
North Atlantic
genre_facet Antarc*
Antarctic
North Atlantic Deep Water
North Atlantic
op_relation Geophysical Research Letters, 0094-8276, 2015, 42:18, s. 7714-7721
orcid:0000-0002-4414-6859
orcid:0000-0003-1124-4564
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-123384
doi:10.1002/2015GL065525
ISI:000363412400059
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1002/2015GL065525
container_title Geophysical Research Letters
container_volume 42
container_issue 18
container_start_page 7714
op_container_end_page 7721
_version_ 1766272012257329152