100+ Sverdrup PowerPoint (PPT) Presentations, Sverdrup PPTs

Sverdrup - PowerPoint PPT Presentation

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. Consider the balance on an f-plane. If f is not constant, then.

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766 views • 39 slides

Ocean Surface Circulation

Ocean Surface Circulation. Motion in the Ocean, Part I, or Why does the ocean have currents, and why do they move in circles?. Two types of Ocean Circulation:. Surface Circulation -- Wind-driven Deep Circulation -- Density (T,S) driven. Atmospheric Circulation. Temperature and Pressure.

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560 views • 32 slides

Abandoning Sverdrup

Abandoning Sverdrup. 80. 70. 60. 50. 40. 30. 20. 10. 0. 70. 70. 60. 60. 50. 50. 40. 40. 30. 30. 0.01. 0.1. 1.0. 10. June Chlorophyll 1998 - 2006 (mg m -3 ). 1953. Google citation count: 561. Net phytoplankton growth occurs when area acd > abdf.

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352 views • 29 slides

Field Trial of a Pulsed Limestone Diversion Well

Field Trial of a Pulsed Limestone Diversion Well. P. L. Sibrell USGS Leetown Science Center, Kearneysville, WV 25430 C. F. Denholm , M. H. Dunn Stream Restoration Inc., Mars, PA. U.S. Department of the Interior U.S. Geological Survey. AMD at Jennings. Vertical Flow Pond. Quonset Hut.

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295 views • 20 slides

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Sverdrup - PowerPoint PPT Presentation

Wind Driven Circulation III

Ocean Surface Circulation

Abandoning Sverdrup

Field Trial of a Pulsed Limestone Diversion Well