Works matching IS 00223670 AND DT 2009 AND VI 39 AND IP 6
Results: 16
Alongshelf Variability of Inner-Shelf Circulation along the Central Oregon Coast during Summer.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1380, doi. 10.1175/2008JPO3760.1
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Seasonal Evolution of Aleutian Low Pressure Systems: Implications for the North Pacific Subpolar Circulation.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1317, doi. 10.1175/2008JPO3891.1
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Distribution and Modification of North Pacific Intermediate Water around the Subarctic Frontal Zone East of 150°E.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1462, doi. 10.1175/2008JPO3919.1
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On the Mechanisms of Episodic Salinity Outflow Events in the Strait of Hormuz.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1340, doi. 10.1175/2008JPO3941.1
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Accelerating Dense-Water Flow down a Slope.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1495, doi. 10.1175/2008JPO3964.1
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Modeling the Dynamics of the North Water Polynya Ice Bridge.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1448, doi. 10.1175/2008JPO3965.1
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Coastal Wind-Driven Circulation in the Vicinity of a Bank. Part I: Modeling Flow over Idealized Symmetric Banks.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1273, doi. 10.1175/2008JPO3966.1
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Coastal Wind-Driven Circulation in the Vicinity of a Bank. Part II: Modeling Flow over the Heceta Bank Complex on the Oregon Coast.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1298, doi. 10.1175/2008JPO3967.1
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A Diagnostic Model for Mixed Layer Depth Estimation with Application to Ocean Station P in the Northeast Pacific.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1399, doi. 10.1175/2008JPO3984.1
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Comments on “Is the Faroe Bank Channel Overflow Hydraulically Controlled?”.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1534, doi. 10.1175/2008JPO4020.1
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A New Climatology of Air–Sea Density Fluxes and Surface Water Mass Transformation Rates Constrained by WOCE.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1432, doi. 10.1175/2008JPO4025.1
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Why Were Sea Surface Temperatures so Different in the Eastern Equatorial Atlantic in June 2005 and 2006?
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1416, doi. 10.1175/2008JPO4030.1
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Nonstationary Westward Translation of Nonlinear Frontal Warm-Core Eddies.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1486, doi. 10.1175/2008JPO4089.1
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Role of Eddy Forcing in the Dynamics of Multiple Zonal Jets in a Model of the North Atlantic.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1361, doi. 10.1175/2008JPO4096.1
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Subinertial Slope-Trapped Waves in the Northeastern Gulf of Mexico.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1475, doi. 10.1175/2009JPO3925.1
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- Article
Anisotropic Response of Surface Currents to the Wind in a Coastal Region.
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- Journal of Physical Oceanography, 2009, v. 39, n. 6, p. 1512, doi. 10.1175/2009JPO4013.1
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