Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Robert O. Reid"'
Autor:
Robert O. Reid
Publikováno v:
Journal of Marine Research. 78:229-261
Essentially two classes of free edge waves can exist on a sloping continental shelf in the presence of Coriolis force. For small longshore wave length, fundamental waves of the first class behave like Stokes edge waves. However, for great wave length
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::336c10c455e168ae3a29182718509638
https://doi.org/10.1357/002224020834442355
https://doi.org/10.1357/002224020834442355
Autor:
Ou Wang, Robert O. Reid
Publikováno v:
Journal of Physical Oceanography. 34:961-967
The well-known Rhines theory of bottom-trapped topographic Rossby waves (TRW) in a uniformly stratified ocean over a sloping seabed, and its dispersion relation between wave frequency and wavenumber components, have served a very useful purpose in pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0a4afc243af1d40e7b16b9f3ec22ad0
https://doi.org/10.1175/1520-0485(2004)034<0961:brwiae>2.0.co
https://doi.org/10.1175/1520-0485(2004)034<0961:brwiae>2.0.co
Publikováno v:
Geophysical Research Letters. 27:1017-1020
We describe observations of large amplitude wind-driven current oscillations of 24-hr period occurring in the near-surface layer of waters of the Texas-Louisiana continental shelf. The near-surface anti-cyclonic current amplitudes can reach 60 cm s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46ff1965eea907f59009e274d99f3c0f
https://doi.org/10.1029/1999gl010491
https://doi.org/10.1029/1999gl010491
Publikováno v:
Monthly Weather Review. 126:2864-2883
The primary objective of this work is to formulate surface meteorological fields over the northwestern Gulf of Mexico for the period from April 1992 through November 1994 useful for the study of mesoscale processes and for model forcing of the near-c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad64edb9e0081351a40c8892a96827b9
https://doi.org/10.1175/1520-0493(1998)126<2864:asmfot>2.0.co
https://doi.org/10.1175/1520-0493(1998)126<2864:asmfot>2.0.co
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 15:1204-1214
Hourly wind fields for the northwestern Gulf of Mexico (here called LATEX winds) were constructed from in situ measurements for the period April 1992 through November 1994 using statistical (optimal) interpolation. Here the LATEX winds are compared w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6534ab9602fc599020f726d3cff3576
https://doi.org/10.1175/1520-0426(1998)015<1204:acalna>2.0.co
https://doi.org/10.1175/1520-0426(1998)015<1204:acalna>2.0.co
Publikováno v:
Journal of Geophysical Research: Oceans. 103:10377-10390
On the basis of current measurements observed at 31 moorings during April 1992 through November 1994, as part of the Texas-Louisiana Shelf Circulation and Transport Processes Study, we describe the horizontally nondivergent part of the near-surface,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27221a079e7173861c5acfa9e0f1855a
https://doi.org/10.1029/98jc00099
https://doi.org/10.1029/98jc00099
Autor:
Robert O. Reid, Steven F. DiMarco
Publikováno v:
Journal of Geophysical Research: Oceans. 103:3093-3109
We analyzed 81 current meter records of varying lengths (3 to 30 months) to describe the principal diurnal (O1, K1, P1, and Q1) and semidiurnal (S2, M2, K2, and N2) tidal current constituents on the Texas-Louisiana continental shelf. The Louisiana-Te
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0bb5279de65d55493f3d20a3c459a54f
https://doi.org/10.1029/97jc03289
https://doi.org/10.1029/97jc03289
Publikováno v:
Circulation in the Gulf of Mexico: Observations and Models
Low-frequency circulation over the Texas-Louisiana continental shelf is examined. Currents over the inner shelf are upcoast (Rio Grande to Mississippi River) in summer and downcoast in nonsummer and are driven by an annual cycle of winds. This result
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67995bb8d190305a4cc5cb0f3ce72cdf
https://doi.org/10.1029/161gm17
https://doi.org/10.1029/161gm17
Publikováno v:
Circulation in the Gulf of Mexico: Observations and Models
We address four independent sources of observational evidence pertaining to circulation in the Bay of Campeche (BOC), located south of 23°N in the western Gulf of Mexico, with the objective of characterizing its mean circulation, its variability, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c5736ae0305d9a6c39743820366e8b0
https://doi.org/10.1029/161gm20
https://doi.org/10.1029/161gm20
Publikováno v:
Circulation in the Gulf of Mexico: Observations and Models
We analyzed 1397 drifter records collected in the Gulf of Mexico and northwestern Cayman Basin between the years 1989 and 1999 to describe the general features of the upper ocean circulation. These drifters were generally drogued at 50 m below the su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5366590c5ff11154c6fbc3e396aa3f4d
https://doi.org/10.1029/161gm08
https://doi.org/10.1029/161gm08