Access the full text.
Sign up today, get DeepDyve free for 14 days.
G. Mellor, Tetsuji Yamada (1982)
Development of a turbulence closure model for geophysical fluid problemsReviews of Geophysics, 20
(1994)
Numerical experiments of internal wave
L. Maas, J. Zimmerman (1989)
Tide-topography interactions in a stratified shelf sea II. Bottom trapped internal tides and baroclinic residual currentsGeophysical and Astrophysical Fluid Dynamics, 45
A. Gill (1982)
Atmosphere-Ocean Dynamics
D. Brickman, J. Loder (1993)
Energetics of the Internal Tide on Northern Georges BankJournal of Physical Oceanography, 23
W. Chuang, Dong-Ping Wang (1981)
Effects of Density Front on the Generation and Propagation of Internal TidesJournal of Physical Oceanography, 11
K. Lamb (1994)
Numerical experiments of internal wave generation by strong tidal flow across a finite amplitude bank edgeJournal of Geophysical Research, 99
J. Huthnance (1989)
Internal tides and waves near the continental shelf edgeGeophysical and Astrophysical Fluid Dynamics, 48
Dong-Ping Wang (1985)
Numerical Study of Gravity Currents in a ChannelJournal of Physical Oceanography, 15
Weather Bureau (1963)
GENERAL CIRCULATION EXPERIMENTS WITH THE PRIMITIVE EQUATIONSMonthly Weather Review, 91
P. Smolarkiewicz (1984)
A Fully Multidimensional Positive Definite Advection Transport Algorithm with Small Implicit DiffusionJournal of Computational Physics, 54
Changsheng Chen, R. Beardsley (1998)
Tidal mixing and cross-frontal particle exchange over a finite amplitude asymmetric bank : a model study with application to Georges Bank, 25
P. Holloway (1984)
On the Semidiurnal Internal Tide at a Shelf-Break Region on the Australian North West ShelfJournal of Physical Oceanography, 14
Dake Chen, Dong-Ping Wang (1990)
Simulating the time-variable coastal upwelling during CODE 2Journal of Marine Research, 48
L. Hodges, W. Reichelderfer, J. Caskey, Smagorinsky (1962)
GENERAL CIRCULATION EXPERIMENTS WITH THE PRIMITIVE EQUATIONS I . THE BASIC EXPERIMENT
P. Holloway (1996)
A Numerical Model of Internal Tides with Application to the Australian North West ShelfJournal of Physical Oceanography, 26
Chia-chiao Lin (1944)
On the Development of Turbulence
(1995)
A numerical study of stratified
Dong-Ping Wang (1982)
Development of a Three-Dimensional, Limited-Area (Island) Shelf Circulation ModelJournal of Physical Oceanography, 12
C. Wunsch (1975)
Internal tides in the oceanReviews of Geophysics, 13
P. Baines (1982)
On internal tide generation models, 29
(1984)
A fully multidimensional positive definite
Changsheng Chen, R. Beardsley (1995)
A Numerical Study of Stratified Tidal Rectification over Finite-Amplitude Banks. Part I: Symmetric BanksJournal of Physical Oceanography, 25
(1993)
Energetics of internal tide on northern
(1984)
On the semidiurnal internal tide at a shelfbreak
Dong-Ping Wang, Dake Chen, T. Sherwin (1990)
Coupling between mixing and advection in a shallow sea front, 10
Hsien-Wang Ou, L. Maas (1988)
Tides near a shelf-slope frontContinental Shelf Research, 8
Internal tides near a midlatitude shelf––slope front are studied using an idealized numerical model, with emphasis on their structure, energetics, and mixing effects. It is found that the properties of internal tides are highly dependent on frontal configuration and tidal frequency. At a winter front, energetic internal tides are generated and arrested in the frontal zone; the cross-shelf flow tends to be surface (bottom) intensified by a large internal circulation cell at the diurnal (semidiurnal) frequency. At a summer front, the diurnal internal tide is still trapped, but a semidiurnal internal tide propagates out of the frontal zone in the offshore direction while arrested at the inshore boundary. The presence of the shelf––slope front enhances the generation of internal tides, and it also causes an amplification of the semidiurnal internal tide by trapping its energy in the frontal zone. This amplification is most prominent at the offshore boundary of the winter front and the inshore boundary of the summer front, where strong tidal refraction takes place. Internal tides can cause significant mixing and dispersion in the frontal zone, with the semidiurnal internal tide being most effective toward the frontal boundaries, and the diurnal internal tide more effective near the site of generation.
Journal of Physical Oceanography – American Meteorological Society
Published: Dec 18, 2001
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.