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arid aeolian wind erosion
deflation: entrainment of lose material and sediment, attrition: sediment collides with each other and wears away, abrasion: windblown particles impact surfaces removing partciles
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arid aeolian wind tranporation
suspension: fine sediment carried in air, saltation: sand grains move in hops along ground, surface creep: sediment pushed or rolled along
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arid aeolian wind deposition
inputs exceed out puts, obstacle, wind speed changes, load deposited forming dunes, move in the direction of the prevailing wind: barchan longitudinal transverse star parabolic
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arid characteristics
little ppt, sparse veg, few clouds, high evap rates, high temp ranges, hyper >100mm, arid 100-300mm, semi 300-600mm
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arid causes
atmospheric circulation, prevailing winds, relief rainfall, ocean currents, continentality
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arid weathering physical
insolation: moisture high temp ranges outer layers expand more, eventually break off exfoliation, salt crystallisation: salt crystallises out of solution grows in size forcing rocks apart, freeze thaw: water freezes expand 9% many cycles breaks apart
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Other cards in this set

Card 2

Front

suspension: fine sediment carried in air, saltation: sand grains move in hops along ground, surface creep: sediment pushed or rolled along

Back

arid aeolian wind tranporation

Card 3

Front

inputs exceed out puts, obstacle, wind speed changes, load deposited forming dunes, move in the direction of the prevailing wind: barchan longitudinal transverse star parabolic

Back

Preview of the back of card 3

Card 4

Front

little ppt, sparse veg, few clouds, high evap rates, high temp ranges, hyper >100mm, arid 100-300mm, semi 300-600mm

Back

Preview of the back of card 4

Card 5

Front

atmospheric circulation, prevailing winds, relief rainfall, ocean currents, continentality

Back

Preview of the back of card 5
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