Works matching IS 00223670 AND DT 2004 AND VI 34 AND IP 8
Results: 10
Structure of the Circulation Induced by a Shoaling Topographic Wave.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1793, doi. 10.1175/1520-0485(2004)034<1793:SOTCIB>2.0.CO;2
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Global Ocean Circulation Modes Derived from a Multiple Box Model.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1811, doi. 10.1175/1520-0485(2004)034<1811:GOCMDF>2.0.CO;2
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Internal Tides Generated on a Corrugated Continental Slope. Part II: Along-Slope Barotropic Forcing.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1824, doi. 10.1175/1520-0485(2004)034<1824:ITGOAC>2.0.CO;2
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Driving Mechanism of Band Structure of Mean Current over the Continental Shelf.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1839, doi. 10.1175/1520-0485(2004)034<1839:DMOBSO>2.0.CO;2
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Reducing Errors in Temperature and Salinity in an Ocean Model Forced by Restoring Boundary Conditions.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1856, doi. 10.1175/1520-0485(2004)034<1856:REITAS>2.0.CO;2
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Absolute Transports of Mass and Temperature for the North Atlantic Current– Subpolar Front System.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1870, doi. 10.1175/1520-0485(2004)034<1870:ATOMAT>2.0.CO;2
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Oceanic Turbulence and Stochastic Models from Subsurface Lagrangian Data for the Northwest Atlantic Ocean.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1884, doi. 10.1175/1520-0485(2004)034<1884:OTASMF>2.0.CO;2
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Latitudinal and Frequency Characteristics of the Westward Propagation of Large-Scale Oceanic Variability.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1907, doi. 10.1175/1520-0485(2004)034<1907:LAFCOT>2.0.CO;2
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The Global S<sub>1</sub> Tide.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1922, doi. 10.1175/1520-0485(2004)034<1922:TGST>2.0.CO;2
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Temperature Advection: Internal versus External Processes.
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- Journal of Physical Oceanography, 2004, v. 34, n. 8, p. 1936, doi. 10.1175/1520-0485(2004)034<1936:TAIVEP>2.0.CO;2
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