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Published byAnabel Cole Modified over 9 years ago
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Midterm 2 Test on Friday, Feb. 25 th Multiple choice just like the last exam Study chapters 3-8 (up to p 227 in Ch 8) Bring a pink PARSCORE Scantron sheet Make up midterm tomorrow cancelled. New test time TBD. Evening review session tonight from 8:00 – 9:30 in Engineering I Room 1104
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Wildlands Program
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Today, we will... Review air masses Review atmospheric lifting mechanisms Understand upper atmosphere dynamics of the jet stream and Rossby waves Learn about the formation of mid-latitude cyclones
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recall the Aleutian and Icelandic low pressure systems
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Key low pressure systems Aleutian LowIcelandic Low
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Maritime Tropical (mT) Air Mass Influence on Southeast Precipitation unstable air on the west side of anticyclones combined with warm water of the Gulf stream
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Location of Deserts
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Atmospheric Lifting Occurs at a Range of Scales
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Convergent Lifting think of the ITCZ - air converges from all points to low pressure zones and the displaced air is lofted
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Convectional Lifting unequal surface heating produces hotspots where ‘bubbles’ of air will rise - this is convection
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Orographic Lifting air cools as it ascends dry air warms as it descends
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the moisture in the cloud gets wrung out by condensation
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Hawaii
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Cherrapunji, India Average annual precipitation: 11430 mm (37.5 ft) Record annual precipitation: 26470 mm (86.8 ft)
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