Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling

Abstract An unconstrained global ocean simulation for 2020 supports past observations of diurnal internal tides by acoustic tomography during the 1991–1992 Acoustic Mid‐Ocean Dynamics Experiment in the Western North Atlantic. Explicitly representing the tides, the simulation reproduces the functiona...

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Published in:Geophysical Research Letters
Main Authors: B. D. Dushaw, D. Menemenlis
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL101193
https://doaj.org/article/560ee3b2459b4d278e4a36972048c58b
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spelling ftdoajarticles:oai:doaj.org/article:560ee3b2459b4d278e4a36972048c58b 2024-09-15T18:21:55+00:00 Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling B. D. Dushaw D. Menemenlis 2023-02-01T00:00:00Z https://doi.org/10.1029/2022GL101193 https://doaj.org/article/560ee3b2459b4d278e4a36972048c58b EN eng Wiley https://doi.org/10.1029/2022GL101193 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL101193 https://doaj.org/article/560ee3b2459b4d278e4a36972048c58b Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023) internal tides barotropic tides ocean acoustic tomography global ocean model model testing baroclinic tide dissipation Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL101193 2024-08-05T17:49:23Z Abstract An unconstrained global ocean simulation for 2020 supports past observations of diurnal internal tides by acoustic tomography during the 1991–1992 Acoustic Mid‐Ocean Dynamics Experiment in the Western North Atlantic. Explicitly representing the tides, the simulation reproduces the functional form and resonant state of K1 and O1 internal‐tide standing waves, while providing a more realistic physical picture of them. The tomographic data were used to predict the tides in 2020. Not surprisingly, the characteristics of the barotropic and internal tides of the unconstrained simulation deviate from observations. The simulated barotropic tidal currents have excessive, irregular amplitude and lead the acoustic tidal predictions by about 2 hr. While internal‐tide phase coherence is apparent, the simulated internal‐tide variations were irregular in amplitude and phase, unlike the observations. The tomographic tidal measurements therefore provide a quantitative benchmark for improved model representation of tides, internal tides, and dissipation. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 3
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic internal tides
barotropic tides
ocean acoustic tomography
global ocean model
model testing
baroclinic tide dissipation
Geophysics. Cosmic physics
QC801-809
spellingShingle internal tides
barotropic tides
ocean acoustic tomography
global ocean model
model testing
baroclinic tide dissipation
Geophysics. Cosmic physics
QC801-809
B. D. Dushaw
D. Menemenlis
Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
topic_facet internal tides
barotropic tides
ocean acoustic tomography
global ocean model
model testing
baroclinic tide dissipation
Geophysics. Cosmic physics
QC801-809
description Abstract An unconstrained global ocean simulation for 2020 supports past observations of diurnal internal tides by acoustic tomography during the 1991–1992 Acoustic Mid‐Ocean Dynamics Experiment in the Western North Atlantic. Explicitly representing the tides, the simulation reproduces the functional form and resonant state of K1 and O1 internal‐tide standing waves, while providing a more realistic physical picture of them. The tomographic data were used to predict the tides in 2020. Not surprisingly, the characteristics of the barotropic and internal tides of the unconstrained simulation deviate from observations. The simulated barotropic tidal currents have excessive, irregular amplitude and lead the acoustic tidal predictions by about 2 hr. While internal‐tide phase coherence is apparent, the simulated internal‐tide variations were irregular in amplitude and phase, unlike the observations. The tomographic tidal measurements therefore provide a quantitative benchmark for improved model representation of tides, internal tides, and dissipation.
format Article in Journal/Newspaper
author B. D. Dushaw
D. Menemenlis
author_facet B. D. Dushaw
D. Menemenlis
author_sort B. D. Dushaw
title Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
title_short Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
title_full Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
title_fullStr Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
title_full_unstemmed Resonant Diurnal Internal Tides in the North Atlantic: 2. Modeling
title_sort resonant diurnal internal tides in the north atlantic: 2. modeling
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL101193
https://doaj.org/article/560ee3b2459b4d278e4a36972048c58b
genre North Atlantic
genre_facet North Atlantic
op_source Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL101193
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL101193
https://doaj.org/article/560ee3b2459b4d278e4a36972048c58b
op_doi https://doi.org/10.1029/2022GL101193
container_title Geophysical Research Letters
container_volume 50
container_issue 3
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