Aeolian processes: incl. erosion, deposition, transportation Flashcards
what planets could have aeolian activity
all terrestrial planets with dynamic atmospheres- mars, venus, earth
why is aeolian erosion and transport especially effective in deserts
sediment largely loose in sandy deserts and not held by vegetation due to moisture deficit, the carried sand makes the wind more erosive
what is the kármán line
the line approx 100km above the earths surface that delineates the boundary of atmosphere and space
what does it mean to say the atmosphere is in hydrostatic equilibrium
pressure is exerted in all directions, making it relatively stable
layers of the atmosphere
thermosphere, mesosphere, stratosphere, troposphere
describe laminar flow
thin sheets of moving air over one another, little mixing of layers with the surface air being stationary
describe turbulent flow
mixing between layers, gusts and eddies, surface layer is stationary
what causes turbulent wind flow
variations in surface topography or variable surface heating
which type of air flow can entrain sand more easily
turbulent
what is the reynolds number
it distinguishes between laminar and turbulent flow
what wind has the highest velocity in the troposphere
jet stream
what is the boundary layer
the layer roughly 300m in altitude in which all exchanges between surface and atmosphere take place
describe the wind conditions of the boundary layer
turbulent flow, slower due to friction, dust storms will fill up within the boundary layer
what is the roughness layer
2-5cm over grass or 2-5 m in forests, almost still flow
can be determined by plant height and flexibility
what is the roughness length
height where the wind is effectively 0m per second
3 forces that work together to entrain sediment in the wind
gravity- keep grain at surface, drag- moves grain along ground, lift- shear stress
4 methods of aeolian sediment transport
suspension, creep, reptation, saltation
describe creep
grain remains in contact w surface most of the time, coarser grains,
describe reptation
hopping motion, transitional between creep and saltation, hit other grains and cause them to bounce forward
describe saltation
jumping motion, 35 degree angle, parabolic pathway, 2-4cm height, dominant transport method
5 factors influencing sediment entrainment in aeolian systems
sediment size surface vegetation surface crusting surface moisture surface slope
what is fluid threshold velocity
min wind speed to initiate grain movement by wind force alone
what is impact threshold
min wind speed needed to initiate particle movement as a result of reptation
what bacteria can create organic crusts
cyanobacteria
what moisture content is the threshold to inhibit sediment transport
2-5%
what is the effect of fog on entrainment
can reduce ability of wind to cause entrainment
name the 2 sides of a dune
windward slope and slip face
which dune side is steepest
slip face
which slope is easier to erode
downslope- decreased critical threshold
impact of surface veg on entrainment
surface roughness length due to plants slows velocity- plant height and flexibility
what 2 main factors make up sediment movement
erosivity (power of wind) and erodibility (grain characteristics holding particles in place)
what is deflation
aeolian erosion: wind causes the lifting and transport of lighter particles from dry soil
what feature can show the predominant wind direction of the past or present
lunettes: dust plume deposits formed from the wind moving material away from lake hollows
formation of desert pavements
wind picks up finer materials through deflation and leaves behind lag deposit-> stony pavement becomes a protective layer
3 controls on wind erosion
susceptible surfaces, sufficient wind energy, removal from site of eroded material
what is abrasion
erosion by suspended sand particles (transfer of kinetic energy)
what is a ventifact
a rock sculptd by wind-borne particles (worn, faceted, cut or polished by these particles)
what is the facet of a ventifact
a curved or flat surface cut by the wind into a ventifact
what is a keel on a ventifact
sharp edge or ridge between the lee and windward side of a ventifact
what is the difference between flutes and grooves
grooves open through while flutes are closed at each end
when did most abrasion on rocks seen today occur
last glacial maximum with v high winds and lots of dust
what are pedestal rocks
shaped like a mushroom, undercut by wind abrasion/ enhanced chemical weathering at the base
what are yardangs
long ridges of resistant rock jutting out of the landscape due to the erosion of less resistant rock first
micro-yardangs can form on top
meso-yardangs are smaller and more assymmetrical, have a flat steep side and sloping downwind side