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Geology 3: Planet Earth

Geology 3: Planet Earth

Geology 3: Planet Earth. Section 1: 0900-1015; DH 306 Section 2: 1330-1445; DH 208. Contact information:. Instructor: Paula Jefferis Office: DH 419 Telephone: 408-924-5016 Email: paula.jefferis-nilsen@sjsu.edu. Welcome to the spring 2011 semester!.

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428 views • 29 slides
Ekman layer at bottom

Ekman layer at bottom

A more general form of the Sverdrup relation. Ekman layer at bottom Spatially changing sea surface height ? and bottom topography z B and pressure p B . Assume atmospheric pressure p ? ?0. Let. , . Integrating. over the vertical column, we have. Similarly. Define.

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200 views • 16 slides
Wind Driven Circulation III

Wind Driven Circulation III

Wind Driven Circulation III. Closed Gyre Circulation Quasi-Geostrophic Vorticity Equation Westward intensification Stommel Model Munk Model Inertia boundary layer Numerical results Observations. Vorticity Equation.

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161 views • 14 slides
Wind Driven Circulation III

Wind Driven Circulation III

Wind Driven Circulation III. Closed Gyre Circulation Quasi-Geostrophic Vorticity Equation Westward intensification Stommel Model Munk Model Inertia boundary layer Numerical results Observations. Vorticity Equation.

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150 views • 14 slides
Ocean Sciences Meeting Orlando, FL 3-7 Mar 2008

Ocean Sciences Meeting Orlando, FL 3-7 Mar 2008

Abyssal Current Steering of Upper Ocean Current Pathways in an Ocean Model with High Vertical Resolution. by. 1 Harley E. Hurlburt, 1 E. Joseph Metzger, 1 Patrick J. Hogan, 2 Charles E. Tilburg and 1 Jay F. Shriver 1 Naval Research Laboratory Oceanography Division

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219 views • 11 slides

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