WIND AND DESERTS
- Deserts
- characterized by a lack of precipitation and high
evaporation rates
- rainfall is unpredictable
- when rain does fall, it is intense and of short
duration
- type of weathering (physical or chemical)
- importance of running water and wind
- location is determined by patterns of
atmospheric circulation
- Coriolis Force
- trade winds
- horse latitudes
- westerlies
- easterlies
- types of deserts
- Subtropical (10- 30N & S latitude)
- Continental Interior
- Rainshadow deserts
- How Does Wind Carries it Load?
- Wind Erosion
- Deflation - removal of loose material by wind
- deflation basin-blowout
- lag deposits
- Abrasion - near surface effect caused by impact
of saltating sand grains
- ventifact (sand blasting)
- Deposition of Material by Wind
- sand dunes
- types
- barchan
- crescent shaped
- tips point downwind
- in areas that are flat and dry
- little vegetation
- limited supply of sand
- constant wind direction
- parabolic
- crescent shaped
- tips point upwind
- commonly in coastal areas with
strong onshore winds
- abundant sand
- partial cover of vegetation
- longitudinal (seif dunes)
- long, parallel ridges
- aligned parallel to the wind
direction
- winds generally converge from
slightly different directions
- 30 - 100 m high; 100 km long
- transverse
- long ridges
- perpendicular to the wind direction
- sand seas
- 200 m high; 3 km wide
- Loess - wind deposited silt and clay