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Midlatitude Cyclones (Storms) Extratropical cyclone or wave cyclone or frontogenesis or storm Low pressure area with counter-clockwise circulation. Atmosphere.

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Presentation on theme: "Midlatitude Cyclones (Storms) Extratropical cyclone or wave cyclone or frontogenesis or storm Low pressure area with counter-clockwise circulation. Atmosphere."— Presentation transcript:

1 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.

2 Storms Center of intense low pressure with cyclonic circulation and resultant precipitation. Midlatitude Cyclone Hurricane Tornadoes Not thunderstorms, no cyclonic motion.

3 Cyclogenesis in Action: Mid-latitude (extratropical) cyclones

4 Air Masses Definition: volume of air with same temperature and humidity characteristics Source Regions: where air masses come from. Classification: warm or cold, moist or dry

5 Air Masses Affecting North America

6 Frontogenesis

7

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9 Occluded Front : The Death of a Storm

10 Occluded Front

11 Weather Maps

12 Today’s Weather Map

13 Storm Tracks: North America Actual Storm Tracks (1991) Storms (Storm Tracks) generally travel from West to East in North America all year They shift North in summer & South in Winter Average Storm Tracks Moving West To East

14 Midlatitude Cyclone Characteristics Motion: these storms move across the midlatitudes at about 30 m.p.h. from west to east as they rotate once around a low pressure center. Size: roughly 1,000 miles in diameter, the largest of storms Lifespan: 3-6 days to develop, 3-6 to dissipate Pressure: center roughly 990-1000 mb (1-2 % drop)


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