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Coriolis parameter - PowerPoint PPT Presentation

Condensation- Induced Winds a supplemental theorem to the traditional thermal wind model

Deborah E. Ross University of Montana Department of Physics and Astronomy. Condensation- Induced Winds a supplemental theorem to the traditional thermal wind model. Overview. Basic Meteorological Assumptions Traditional Wind Model Condensation Induced Winds Derivation

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458 views • 36 slides

From observations to models:

From observations to models:. More on the western boundary current problem. Stommel-Munk model. Stommel (1948) and Munk (1950) solved the western boundary current problem by including friction in the equations of motion.

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531 views • 18 slides

5.5 Rossby Waves

5.5 Rossby Waves. -Mechanism and Examples in the Real Atmosphere. Coriolis Effect. ?. 2?. ?. z. 2?sin? Planetary vorticity. ?. 2?. z. Coriolis Parameter. f/2?. f always increases northward!. S. N. B. C. A. C. A.

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795 views • 14 slides

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Coriolis parameter - PowerPoint PPT Presentation

Condensation- Induced Winds a supplemental theorem to the traditional thermal wind model

From observations to models:

5.5 Rossby Waves