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Published byClaude Mosley Modified over 9 years ago
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Chapter 7 Circulation of the Atmosphere The Atmosphere 9e Lutgens & Tarbuck Power Point by Michael C. LoPresto
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Microscale
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Atmospheric Circulation Scales
Distance Time scale Examples Macroscale Planetary Synoptic 1000 – 40,000 km 100 – 500 km Weeks or more Days to weeks Westerlies Hurricanes Mesoscale 1 – 100 km Minutes to hours Thunderstorms, Land-sea breeze Microscale < 1km Seconds to minutes Gusts, dust devils
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Mesoscale Sea Breeze (occurs in afternoon)
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Mesoscale Land Breeze (occurs in early morning)
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Valley Breeze (afternoon)
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Mountain Breeze (early morning)
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Other Common, Named Mesoscale Winds
Chinook – warm winter wind that descends off mountains (Foehn in Alps; Santa Ana in So. Cal.) Katabatic – cold, powerful winter wind that descends off glaciers (mistral in Alps)
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Over-simplified global model (why is it wrong?)
Macroscale: Global Circulation Over-simplified global model (why is it wrong?)
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Best Model for Global Circulation
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Idealized & Actual Prevailing Global Winds
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Seasonal Pressure and Wind Patterns
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January Average Global Pressure and Winds
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July Average Global Pressure and Winds
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Monsoons Seasonal wind (and precipitation) events on large continents
Cooling of land during winter creates high pressure, pushes air offshore (cold dry winds) Heating of land during summer creates low pressure, sucks air inland (warm wet winds)
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Winter Monsoon Circulation
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Summer Monsoon Circulation
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North American Monsoon L
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The Westerlies and the Jet Stream
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Jet Stream
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Jet Stream
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300 mb Equal-Pressure Surface 4.15.05
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300 mb Equal-Pressure Surface 4.15.05
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Rossby Waves
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Meridional and Zonal Flow
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Ocean Currents
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El Nino/Southern Oscillation
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Effects of El Nino
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ENSO El Nino Winter Surface Air Pressure Anomaly low high high low
La Nina Winter Surface Air Pressure Anomaly
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1997 ENSO Movie http://www.noaanews.noaa.gov/stories/s997.htm
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ENSO Movie
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Average Tropical Pacific Sea Surface Temperature
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Sea Surface Temperature March 2002
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ENSO Rainfall in North America
El Nino Winter Precipitation Rate Anomaly La Nina Winter Precipitation Rate Anomaly
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Current ENSO conditions: Equatorial Pacific sea surface temperatures (top) and temperature anomalies (bottom)
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Worldwide ENSO Effects
Drought Flooding, erosion Tropical Storms Drought Drought Drought Utah: On average, ENSO years are normal, but some ENSO years have brought severe flooding Worldwide ENSO Effects Page 222
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