Deserts Flashcards

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1
Q

what is a desert

A

an area/region, lacking in moisture, often exposing expanses of barren rock and/or sediment + hosting climatic condition hostile to life

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2
Q

what are teh 3 main types of deserts

A

Subtropical Deserts

Polar Deserts

Mid-Latitude Deserts
- rainshadow
- continental interior

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3
Q

what are semi-arid regions ( dry but no quite deserts) referred to as?

A

“steepes”

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4
Q

How does atmospheric circulation work?

A

Due to Earth’s rotation, convection cells are a little more complicated

Air flow is deflected due to Coriolis force

The convection pattern is broken up into 3 types of circulation cells

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5
Q

what are hadley cells

A

On either side of equator to 30 latitude (N + S). Equator marks zone of low pressure where air rises

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6
Q

what are polar cells?

A

Centred at poles (90 latitude) where cold air sinks to produce polar high pressure area

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7
Q

what are ferrell cells

A

btwn Hadley + Polar cells (circulation driven mostly by movement from Hadley + Polar cells

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8
Q

where do subtropical deserts occur?

A

In general, subtropical deserts occur under high-pressure belts btwn Hadley + Ferrell cells (where dry air flows downward)

Opposite to conditions in low pressure belts in which moist air rises, moisture condenses into droplets (when cooled) + falls as precipitation (very wet climate)

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9
Q

where do polar deserts occur?

A

Polar deserts occur under high-pressure regions (where dry air flows downward)

Sub-tropical deserts, which are hot

Polar deserts at the poles are very cold

Polar deserts occur both near North Pole and South Pole (Antarctica)

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10
Q

what are rainshadow deserts?

A

Deserts can develop at mid-latitudes due to the “rainshadow” effect of mountain

As moist air from the ocean meets a mountain barrier, it is forced to rise over the mountain

Moisture condenses to form clouds + falls as precipitation on windward side of the mountain

A rain shadow desert is produced on the leeward side of the mountains (as moisture supply has been spent)

Called “rainshadow” deserts bc they occur in “rainshadow” areas of mountain belt

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11
Q

when can large deserts develop in mid-latitudes

A

if there is a very large continent at that latitude

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12
Q

what are physical components of deserts

A

water
Tends to be scarce for much of the time

But when it rains, it really rains (torrential downpours)

Flash floods common, produce ephemeral (short-lived) streams

wind
Can be little wind

But when wind blows, it is often severe

As w/ the case w/ water, the lack of anchoring vegetation means that wind has strong erosive power

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13
Q

how is sediment transported by wind

A

Bedload (at land surface) via rolling, sliding, saltation

Suspended load (suspended in air)

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14
Q

what is the process of deflation in deserts

A

Wind selectively picks up light/small particles + carries them away in suspension (“winnowing”)

The leaves a residue of larger fragments, forming a desert pavement of larger stones

The pavement can protect the underlying material from further erosion

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15
Q

what is the process of a blowout

A

produced by deflation are shallow depressions appropriately called blowouts

Within a blowout, small patches of soil anchored by vegetation can remain as raised humps

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16
Q

what is the process of abrasion

A

Sediment particles carried in suspension can polish solid surfaces of exposed rock outcrops + fragments via abrasion

Rock that have been worn smooth + polished by this sandblasting process are called ventifacts

17
Q

what are aelian deposits

A

accumulations of sediment composed of sediment particles transported + deposited by wind

18
Q

what is loess

A

Windblown silt + clay (associated w/ arid regions + dry conditions associated w/ glaciations) Thick accumulations of loess can be deposited far from their desert or glacial source areas

19
Q

what is sand

A

Sand-sized particles or resistant minerals. Commonly moulded by wind into dunes

20
Q

what are crossbedding in dunes

A

Many dunes have asymmetric profile w/ gently inclined upwind (windward) slope + steep leeward (down-wind slope)

Sand is transported (by wind) up the gentler windward slope by saltation, then avalanches down the steep “slip” face of the down-wind (leeward) slope

As the process continues, the dunes migrate downwind, producing inclined patterns called crossbeds (crossbeds can also produced by ripples in a water current)

Crossbeds always slant in the down-current direction (so are valuable flow direction indicators)

21
Q

what factors do the shapes of dunes depend on?

A

sand supply, wind strength (and speed), presence/absence of vegetation + various other factors

22
Q

what are barchan dunes?

A

crescent-shaped dunes w/ their tips pointing downwind. Develop on level surfaces w/ low sand supply

23
Q

what are transverse dunes?

A

ridge-like, oriented perpendicular to wind direction. Develop where sand supply is very high

24
Q

what are parabolic dunes

A

Crescent-shaped dunes w/ tips pointing upwind. Develop where the land surface is stabilized by vegetation + sand supply is high (depressions btwn the tips are blowouts)