'Midlatitude cyclone' diaporamas de présentation

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Midlatitude cyclones

Identify and describe the North American air masses that influence the weather patterns for Lexington Differentiate between frontal types and recognize their map symbols Explain how precipitation patterns may vary between a warm and a cold front Describe the stages of cyclogenesis

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Air Masses and Midlatitude Cyclones

Air Masses and Midlatitude Cyclones. ATS 351 Lab 11 November 16, 2009. Air Masses of North America. Air mass: extremely large body of air whose properties of temperature and humidity are fairly similar in any horizontal direction at any given latitude Named for their region of origin

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OSSEs: Observing Systems Simulation Experiments JCSDA: Joint Center for Satellite Data Assimilation SWA: Simpson We

EGU2008-A-10290. OSSEs: Observing Systems Simulation Experiments JCSDA: Joint Center for Satellite Data Assimilation SWA: Simpson Weather Associates ESRL: Earth System Research Laboratory ( formerly FSL, CDC, ETL). Progress in Joint OSSEs

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Ever heard of a Temperate Cyclone?

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The Midlatitude Cyclone

The Midlatitude Cyclone. Cyclone Development begins with a stationary front. Before Birth. Forecasting where on the Stationary front the development will occur is the tricky part!. Nascent stage of Cyclone Development. Birth and adolescence. Mature stage of Cyclone Development.

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Midlatitude Cyclones (Storms)

Midlatitude Cyclones (Storms). Extratropical cyclone or wave cyclone or frontogenesis or storm Low pressure area with counter-clockwise circulation. Atmosphere collects water as water vapor in evaporation from oceans, lakes. It is returned via precipitation, often caused by storms.

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