Zobrazeno 1 - 10
of 51
pro vyhledávání: '"Timothy W. Kao"'
Autor:
Kamal Saffarinia, Timothy W. Kao
Publikováno v:
Dynamics of Atmospheres and Oceans. 23:379-391
The full Navier-Stokes and diffusion equations are applied to study the breaking of an internal soliton on the continuously stratified pycnocline in a two-layer system and its interaction with a slope. First, these equations are solved numerically to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10ac3c2946f37dbb2b241d81bd5514ce
https://doi.org/10.1016/0377-0265(95)00428-9
https://doi.org/10.1016/0377-0265(95)00428-9
Publikováno v:
Journal of Geophysical Research. 97:11219-11236
A three-dimensional hydrodynamic model is developed to study the circulation in the Arabian Gulf. The model contains realistic basin geometries and bathymetries of the Arabian Gulf and a good portion of the Gulf of Oman and is driven by monthly clima
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37e700cbfc1809fbfe8bddd7f1732967
https://doi.org/10.1029/92jc00841
https://doi.org/10.1029/92jc00841
Autor:
Timothy W. Kao, Hsien-Ping Pao
Publikováno v:
Geophysical & Astrophysical Fluid Dynamics. 10:109-114
A new method is introduced to produce a uniform stratified flow over a stationary obstacle in an open channel. The flow is achieved by discharging the flow from the channel through a sink. The details of the sink are unimportant. The flow speed is li
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40cac67d3daab5b4d4bd2a86aa1052ac
https://doi.org/10.1080/03091927808242631
https://doi.org/10.1080/03091927808242631
Autor:
Timothy W. Kao
Publikováno v:
Journal of Physical Oceanography. 11:1215-1223
In Part I of this series, a framework was introduced for the study of oceanic frontal dynamics. The dynamics was studied by posing an initial value problem, starting with a near-surface discharge of buoyant water with a prescribed density deficit int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::540605fa0cc58556001b1cd3b0fa04c0
https://doi.org/10.1175/1520-0485(1981)011<1215:tdoofp>2.0.co
https://doi.org/10.1175/1520-0485(1981)011<1215:tdoofp>2.0.co
Autor:
Timothy W. Kao, Shenn-Yu Chao
Publikováno v:
Journal of Physical Oceanography. 17:792-807
The frontal instability of major baroclinic ocean currents such as the Gulf Stream is numerically studied here, using a three-dimensional, primitive-equation model. The model current is driven by a buoyant discharge near the surface from the light wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d773b844e25f643dd626376dd2efbd93
https://doi.org/10.1175/1520-0485(1987)017<0792:fioboc>2.0.co
https://doi.org/10.1175/1520-0485(1987)017<0792:fioboc>2.0.co
Autor:
Timothy W. Kao
Publikováno v:
Journal of Physical Oceanography. 17:123-133
The structure of the Gulf Stream Current is associated with the quasi-permanent density front in the western North Atlantic. The lighter mass of warmer but saltier water of the Sargasso Sea is separated from the slope water by inclined isopycnals tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3ffab6c8d7c95559e2520168281a21d
https://doi.org/10.1175/1520-0485(1987)017<0123:tgsaif>2.0.co
https://doi.org/10.1175/1520-0485(1987)017<0123:tgsaif>2.0.co
Publikováno v:
Journal of Fluid Mechanics. 65:657-688
An investigation is made of selective withdrawal of a linear stratified fluid from a line sink in a channel of depth d. The flow is characterized by a densimetric Froude number F = Q/Nd2, where Q is the discharge per unit width and N is the Väisäl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a8ac025c37074b60715fd1fc0399feb
https://doi.org/10.1017/s0022112074001595
https://doi.org/10.1017/s0022112074001595
Publikováno v:
Journal of Fluid Mechanics. 65:689-710
Experiments were conducted to examine the development and establishment of the withdrawal current in the selective withdrawal of a stratified fluid from a line sink. The experiments were performed in a Plexiglas channel 30·5 ft long 14 in. wide, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b0a97f632b7fa1e8fa3e1098befae53
https://doi.org/10.1017/s0022112074001601
https://doi.org/10.1017/s0022112074001601
Autor:
Timothy W. Kao
Publikováno v:
Journal of the Hydraulics Division. 102:717-729
A general criterion for the presence or absence of selective withdrawal in a fluid or arbitrary stratification due to a line sink in a channel is presented. Several examples are given. The criterion is based on whether the speed of upstream propagati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf97400bff9f582cba98da64da53e5ab
https://doi.org/10.1061/jyceaj.0004553
https://doi.org/10.1061/jyceaj.0004553
Autor:
Timothy W. Kao
Publikováno v:
Journal of the Hydraulics Division. 103:543-555
The velocity of propagation of a variety of gravity motivated density currents is given. Several stratification configurations of the ambient fluid environment are considered. Applications are given to surface warm discharge in lakes or reservoirs, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e74806d40c110fc3829c7bb04557542b
https://doi.org/10.1061/jyceaj.0004752
https://doi.org/10.1061/jyceaj.0004752