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SEVERE WEATHER

SEVERE WEATHER

SEVERE WEATHER. Lecture 9. Definition of a Severe Thunderstorm. The National Weather Service defines a severe thunderstorm as a thunderstorm that produces Hail of 1 inch diameter or larger And/or Wind gusts 58 mph or greater A tornado Note: this does not include lightning or heavy rain!.

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Textbook chapter 2, p. 33-36 chapter 3, p. 74-79 chapter 4, p. 122-123

Textbook chapter 2, p. 33-36 chapter 3, p. 74-79 chapter 4, p. 122-123

Textbook chapter 2, p. 33-36 chapter 3, p. 74-79 chapter 4, p. 122-123. Stability and Cloud Development. The Development of Clouds. Why does the atmosphere sometimes produce stratus clouds while at other times cumulus , and/or cumulonimbus clouds form?.

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Yang, M.-J ., D.-L. Zhang, X.-D. Tang, and Y. Zhang, J. Geophys . Res.

Yang, M.-J ., D.-L. Zhang, X.-D. Tang, and Y. Zhang, J. Geophys . Res.

A modeling study of Typhoon Nari (2001) at landfall. Part II: Structural changes and terrain-induced asymmetries. Yang, M.-J ., D.-L. Zhang, X.-D. Tang, and Y. Zhang, J. Geophys . Res. Part I

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EVAPORATIVE WATER LOSS Effective channel - heat loss

EVAPORATIVE WATER LOSS Effective channel - heat loss

EVAPORATIVE WATER LOSS Effective channel - heat loss Ta 25 C - latent heat of vaporization = 582 cal/gm 100 kg animal - with 140,000 cal/h metabolic rate Can maintain thermal equilibrium with evaporation of 240 g H2O per hour. Respiratory Evaporation

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Maintenance of convection above a cold undercurrent in a mesoscale convective system

Maintenance of convection above a cold undercurrent in a mesoscale convective system

School of Earth and Environment INSTITUTE FOR CLIMATE AND ATMOSPHERIC SCIENCE. Maintenance of convection above a cold undercurrent in a mesoscale convective system.

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Adiabatic processes on a thermodynamic chart.

Adiabatic processes on a thermodynamic chart.

Adiabatic processes on a thermodynamic chart. Atms Sc 4310 / 7310 Lab 2 Anthony R. Lupo. Adiabatic processes on a thermodynamic chart. 1st law of thermodynamics in the form (imperfect form) is a statement of the Conservation of energy (heat in = heat out)!.

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ATOC 4720 class36

ATOC 4720 class36

ATOC 4720 class36. The continuity equation The vertically averaged divergence 3. The primitive equations. Equations we have learnt up to now:. (. ). Where,. Leading term, . Change T field. Even when . , which is very small, Pronounced T change with time.

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280 views • 13 slides
Keystone Species - Leaching

Keystone Species - Leaching

Keystone Species - Leaching. Crystal Suggs Dr. Simpson APES 17 April 2012. Keystone Species. A species that is far more important in its community than its relative abundance might suggest APPLICATION A sea otter is a keystone species. Kinetic Energy. The energy of motion APPLICATION

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295 views • 11 slides

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