About 10 of a non polar desert is
About 10% of a non -polar desert is dune covered Arid and Semi-Arid Landscapes 1. Arid (Desert) has Precipitation (mm) < 10 x Temperature in o. C 25 o C Desert < 25 cm = 250 mm rain 2. UNESCO index Desert Precipitation/Potential Evaporation < 0. 25 Aridity Index = Potential Evaporation/ Precipitation > 4. 0 Skip Lawson's Theory pp. 283 -284
World's Deserts about 1/5 th of land Types: subtropical, rain-shadow, coastal, interior, polar
Semi-Arid Semi-arid (Steppe, Savannah, dry grassland) has Precipitation (mm) > 10 x Temperature in o. C but < than 20 x (c) 2004 -2013 Charles L. Smart. All rights reserved
Flash Floods Role of Desert Varnish, lack of plant cover Stream Flood (c) 2004 -2013 Charles L. Smart. All rights reserved
Desert Landforms Produced By ba Water ja da alluvial fan Insel berg o arroy pla ya pedim ent pla ya
Arroyo - Water-Carved Canyon Usually dry
Playa, Salar, Sabkha A Playa in Death Valley, California Evaporite Pan of dried-up Playa
Inselberg, Monadnock, Kopje Uluru (Ayers Rock) Pediment
Eolian Processes The physics of wind generated landforms is studied using sand grains in wind tunnels Wind storm, Lothagam Hill dunes
Physics of Wind Transport Sandstorm • Air has low density, so wind is a relatively minor agent of geomorphic change • Rock density 2000 times density same volume of air so rock fragments are difficult to lift with air. • A one meter per second (1 m/sec) flow of water lifts the same particle as about 30 m/sec flow of air
Toadstools • "Undercut, mushroom shaped pedestal rocks in desert areas are commonly attributed to wind erosion" • Ignore Bloom's comments p 291 right 1 following the line above. • This area is frequently hit with high sandstorms. These remove the paint from our trucks. Water and wind formed erosional features such as this toadstool
Wind-Borne Sediment causes deflation and abrasion Sahara to Caribbean Effect on Hurricanes Surface creep
Desert Pavements or Reg Note desert varnish, lack of sand, Iron and Manganese oxides over everything Infiltration is slow – Flash Floods, and most water leaves the area
Desert Pavements (cont'd) – Hammada (Hamada) = barren rock Makes a great runway for supply aircraft Just clear away a few big rocks We tow makeshift rakes behind our Land Rovers Desert Pavement Source: Martin Miller
Erosional Landform - Deflation Hollow Anecdote – How fast does this occur?
Abrasion Origin of Ventifacts
Erosional Landforms - Ventifacts Wind eroded (sand blasted) surfaces
Erosional Landform - Yardangs Sphinx? White Desert, Egypt
Deposition Landforms of Eolian Sands • Reduced wind velocity results in sediments deposition • Dunes are hills of loose wind-born sand • Size, shape, and orientation of dunes are determined by available sand, vegetation, and wind Only 10% of desert surface Sand drift in Lee Of Mountains
Dunes form in a lee High velocity zone Dunes are accumulations in the lee of local obstructions, possibly an upwind dune
Dune Migration Windward slope erosion and transport Just like ripples in a stream Slip face (deposition)
Star Dunes
Star Dunes Variable Wind Direction Copyright © Frank Eckardt 2002
Longitudinal Dunes Constant wind direction, no vegetation
Longitudinal Dunes Constant wind direction, no vegetation
Transverse Dunes Massive volumes of sand, slow but consistent winds
Transverse Dunes Massive volumes of sand, low consistent winds
Barchan Dunes Isolated Dunes, low sand supply, migrating across rock
Barchan Dunes • Isolated – low sand supply; migrating across rock
Parabolic Dunes Horns pinned by plants Typical of coasts
Parabolic Dunes • Stabilized “horns" point upwind
Dunes in Victoria Crater Mars
Suspended Load Transport and Deposition • In dry areas very high winds can suspend fine sand particles
Suspended Load Dust
Loess from the Columbia River Basin • Loess deposits are (usually) of glacial outwash silt. These thin downwind.
Global loess • Origins – Desert – Glacial Layers of dust from Patagonia appear in Vostok cores just prior to interglacials
End Arid and semi-arid What type of dune? Wind
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