Incorporating tides and internal gravity waves within global ocean general circulation models: A review

•We review global ocean models with simultaneous tidal and atmospheric forcing.•Tidal interactions with other earth system components can be studied in such models.•Global internal wave models are used to plan field and satellite missions.•Global internal wave models are used in operational oceanogr...

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Vydáno v:Progress in oceanography Ročník 206; s. 102824
Hlavní autor: Arbic, Brian K.
Médium: Journal Article
Jazyk:angličtina
Vydáno: Elsevier Ltd 01.08.2022
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ISSN:0079-6611, 1873-4472
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Abstract •We review global ocean models with simultaneous tidal and atmospheric forcing.•Tidal interactions with other earth system components can be studied in such models.•Global internal wave models are used to plan field and satellite missions.•Global internal wave models are used in operational oceanography.•Global internal wave models are used to provide boundary forcing for regional models. Until recently, high-resolution global modeling of tides has been done separately from high-resolution global modeling of the atmospherically-forced oceanic general circulation. Here we review the emerging class of high-resolution global models that are simultaneously forced by both atmospheric fields and the astronomical tidal potential. Such models simulate barotropic (surface) tides, internal tides, near-inertial motions, the eddying general oceanic circulation, and a partially resolved internal gravity wave (IGW) continuum spectrum (Garrett-Munk spectrum) simultaneously. We review the technical aspects of such global models and their myriad applications, for example, in satellite oceanography, operational oceanography, boundary forcing of regional models, tidal-cryosphere interactions, and assessment of future coastal flooding hazards in a changing climate with altered tides.
AbstractList Until recently, high-resolution global modeling of tides has been done separately from high-resolution global modeling of the atmospherically-forced oceanic general circulation. Here we review the emerging class of high-resolution global models that are simultaneously forced by both atmospheric fields and the astronomical tidal potential. Such models simulate barotropic (surface) tides, internal tides, near-inertial motions, the eddying general oceanic circulation, and a partially resolved internal gravity wave (IGW) continuum spectrum (Garrett-Munk spectrum) simultaneously. We review the technical aspects of such global models and their myriad applications, for example, in satellite oceanography, operational oceanography, boundary forcing of regional models, tidal-cryosphere interactions, and assessment of future coastal flooding hazards in a changing climate with altered tides.
•We review global ocean models with simultaneous tidal and atmospheric forcing.•Tidal interactions with other earth system components can be studied in such models.•Global internal wave models are used to plan field and satellite missions.•Global internal wave models are used in operational oceanography.•Global internal wave models are used to provide boundary forcing for regional models. Until recently, high-resolution global modeling of tides has been done separately from high-resolution global modeling of the atmospherically-forced oceanic general circulation. Here we review the emerging class of high-resolution global models that are simultaneously forced by both atmospheric fields and the astronomical tidal potential. Such models simulate barotropic (surface) tides, internal tides, near-inertial motions, the eddying general oceanic circulation, and a partially resolved internal gravity wave (IGW) continuum spectrum (Garrett-Munk spectrum) simultaneously. We review the technical aspects of such global models and their myriad applications, for example, in satellite oceanography, operational oceanography, boundary forcing of regional models, tidal-cryosphere interactions, and assessment of future coastal flooding hazards in a changing climate with altered tides.
ArticleNumber 102824
Author Arbic, Brian K.
Author_xml – sequence: 1
  givenname: Brian K.
  orcidid: 0000-0002-7969-2294
  surname: Arbic
  fullname: Arbic, Brian K.
  email: arbic@umich.edu
  organization: Department of Earth and Environmental Sciences, University of Michigan, 2534 North University Building, 1100 North University Avenue, Ann Arbor, MI 48109, USA
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Keywords Internal tides
Ocean modeling
Ocean tides
Ocean mixing
Internal gravity waves
General oceanic circulation
Language English
License This is an open access article under the CC BY license.
LinkModel OpenURL
MergedId FETCHMERGED-LOGICAL-c385t-9d45a6620ca49ed869b7486da254cfb6f950a4bc0d0c887611ceb1c515783dfd3
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content type line 23
ORCID 0000-0002-7969-2294
OpenAccessLink https://dx.doi.org/10.1016/j.pocean.2022.102824
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PQPubID 24069
ParticipantIDs proquest_miscellaneous_2675571671
crossref_primary_10_1016_j_pocean_2022_102824
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PublicationCentury 2000
PublicationDate August 2022
2022-08-00
20220801
PublicationDateYYYYMMDD 2022-08-01
PublicationDate_xml – month: 08
  year: 2022
  text: August 2022
PublicationDecade 2020
PublicationTitle Progress in oceanography
PublicationYear 2022
Publisher Elsevier Ltd
Publisher_xml – name: Elsevier Ltd
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Snippet •We review global ocean models with simultaneous tidal and atmospheric forcing.•Tidal interactions with other earth system components can be studied in such...
Until recently, high-resolution global modeling of tides has been done separately from high-resolution global modeling of the atmospherically-forced oceanic...
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SubjectTerms class
climate
General oceanic circulation
gravity
gravity waves
Internal gravity waves
Internal tides
Ocean mixing
Ocean modeling
Ocean tides
oceanography
oceans
satellites
Title Incorporating tides and internal gravity waves within global ocean general circulation models: A review
URI https://dx.doi.org/10.1016/j.pocean.2022.102824
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