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Chapter 7 Circulation of the Atmosphere The Atmosphere 9e Lutgens & Tarbuck Power Point by Michael C. LoPresto. Microscale. Atmospheric Circulation Scales. Mesoscale Sea Breeze (occurs in afternoon). Mesoscale Land Breeze (occurs in early morning). Valley Breeze (afternoon).
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Chapter 7Circulation of the AtmosphereThe Atmosphere 9eLutgens & TarbuckPower Point by Michael C. LoPresto
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)
Macroscale: Global Circulation Over-simplified global model (why is it wrong?)
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)
L Summer Monsoon Circulation
North American Monsoon L
ENSO El Nino Winter Surface Air Pressure Anomaly low high high low La Nina Winter Surface Air Pressure Anomaly
1997 ENSO Movie http://www.noaanews.noaa.gov/stories/s997.htm http://www.cdc.noaa.gov/ENSO/ http://www.cdc.noaa.gov/map/clim/sst_olr/el_nino_anim.shtml http://www.cdc.noaa.gov/map/clim/sst_olr/old_sst/sst_9798_anim.shtml http://www.cdc.noaa.gov/ENSO/Compare/
ENSO Rainfall in North America El Nino Winter Precipitation Rate Anomaly La Nina Winter Precipitation Rate Anomaly
Current ENSO conditions: Equatorial Pacific sea surface temperatures (top) and temperature anomalies (bottom)
Worldwide ENSO Effects Drought Flooding, erosion Drought Drought Tropical Storms Drought Utah: On average, ENSO years are normal, but some ENSO years have brought severe flooding Page 222