'Rossby waves' diaporamas de présentation

AOSS 401, Fall 2007 Lecture 27 November 28 , 2007

AOSS 401, Fall 2007 Lecture 27 November 28 , 2007. Richard B. Rood (Room 2525, SRB) rbrood@umich.edu 734-647-3530 Derek Posselt (Room 2517D, SRB) dposselt@umich.edu 734-936-0502. Class News November 28 , 2007. Homework 7 (Posted tomorrow, Thursday) Due Next Friday Important Dates:

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Process Solutions

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Atmospheric Dynamics on Solid-Surface Bodies

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Measuring the Properties of Rossby Waves from Space

Measuring the Properties of Rossby Waves from Space. Peter Challenor, Paolo Cipollini & the Laboratory for Satellite Oceanography Southampton Oceanography Centre, U.K. Outline. Observations of planetary waves with satellite altimetry Speed estimation techniques

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Rossby and Kelvin Waves, Upwelling, and Equatorial circulation

Rossby and Kelvin Waves, Upwelling, and Equatorial circulation. October 15. Rossby Waves. L: measure of length over which U changes; also a measure of how far parcel travels before acted on by Coriolis. If R 0 <<1, ocean responds by wave propagation. f 3. f 2. f 1. C.

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Diagnostics II

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Ideas from the year-long Warwick Turbulence Symposium Sergey Nazarenko, Warwick, UK

Ideas from the year-long Warwick Turbulence Symposium Sergey Nazarenko, Warwick, UK. Plan. Pick ideas relevant to our discussion.

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ENSO Coupled Ocean-Atmosphere Dynamics and its Representation in Coupled Climate Models

ENSO Coupled Ocean-Atmosphere Dynamics and its Representation in Coupled Climate Models. Antonietta Capotondi NOAA/ Physical Science Division University of Colorado/Cires/CDC. Outline. Review coupled ocean-atmosphere interactions associated with ENSO events

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The dynamics of planetary atmospheres

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Physical Geography

Physical Geography. Weather and Climate Lecture 4 Winds and Global Circulation II. Winds in the Upper Atmosphere. - concept of the geostrophic wind - blows parallel to the isobars due to lack of friction in the upper atmosphere - the formation of jet streams :

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Hiromu Nakagawa 2 Naoya Hoshino 2 M anuela Sornig 1 Guido Sonnabend 3 Dusan Stupar 3

Venus Upper Atmosphere:. Doppler Wind Variations and Comparison with Wave Modeling. Hiromu Nakagawa 2 Naoya Hoshino 2 M anuela Sornig 1 Guido Sonnabend 3 Dusan Stupar 3. RIU, Department for Planetary Science, University of Cologne, Germany

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Why is the highest annual mean insolation NOT along the equator?

Why is the highest annual mean insolation NOT along the equator?. Atmospheric Circulation. L.O.s: To describe and explain atmospheric circulation. To know the impact of the Coriolis Force on the direction of wind.

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Part II: Waves in the Tropics- Theory and Observations

Part II: Waves in the Tropics- Theory and Observations. Derivation of Rossby waves; mixed Rossby gravity waves and vertical propagation. Rossby Waves. Rossby waves result from the conservation of potential vorticity.

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Impacts of El Nino

Impacts of El Nino. Observations Mechanisms for remote impacts. Observations. Growth and Decay of El Nino. A closer look at impacts. http://iri.columbia.edu/climate/ENSO ENSO and CLIMATE Temperature and Precipitation Tropical Cyclones ENSO and SOCIETY Regional impacts

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The Jet Stream and Rossby Waves

The Jet Stream and Rossby Waves. Earth-Sun Relations. Earth-Sun Relations. Seasonal Pressure and Precipitation Patterns. Cold Fronts and Warm Fronts.

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The Jet Stream and Rossby Waves

The Jet Stream and Rossby Waves.

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