Arid - KQ1 (processes and factors giving arid environment their distinctive characteristics) Flashcards

1
Q

What are lines of latitude?

A

Imaginary lines around the Earth running parallel to the equator
- Measured in degrees N or S of the equator

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2
Q

What is altitude?

A

A measure of an area’s height above sea level

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3
Q

What is aridity?

A

When an area receives less than 250mm of rainfall a year

- Measured in aridity index = p (annual average precipitation) / PET (annual potential evapotranspiration)

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4
Q

What are the characteristics of hyper-arid environments?

A
  • Aridity index = less than 0.3
  • Mean annual precipitation = less than 100mm
  • 7.5% of world’s surface
  • Extremely dry = no rain for several years
  • Very few shrubs
  • Nomadic pastoralism only = move herds of sheep from place to place
  • EXAMPLE = Sahara Desert, Morocco
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5
Q

What are the characteristics of arid environments?

A
  • Aridity index = 0.03 - 0.2
  • Mean annual precipitation = 100-250mm
  • 12.1% of World’s surface
  • Infrequent and unreliable rainfall
  • Some grasses, shrubs and trees
  • Pastoral farming possible where perennial streams (flow all year round)
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6
Q

What are the characteristics of semi-arid environments?

A
  • Aridity index = 1.2-1.5
  • Mean annual precipitation = 250-500mm
  • 17.7% of world’s surface
  • High and more reliable rainfall
  • Usually a seasonal pattern of rainfall
  • More continuous vegetation
  • Arable farming possible
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7
Q

What causes aridity?

A
  • High pressure/latitude
  • Continentality
  • Rain shadow/relief
  • Ocean currents/offshore winds
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8
Q

How does high pressure/latitude cause aridity?

A
  • Often subtropical high pressure cells (30N/S of equator)
  • Intense solar insolation and converging air streams at ground level at equator = ascending air stream = Hadley Cell
  • Air continues to rise until trop tropopause = cannot rise anymore = deflected polewards = cools and sinks
  • Air in these cells = converges, sinks and subsidises, compresses, warms
  • Subsidence prevents air from rising from ground surface = from cooling, condensing and forming cloud/rain
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9
Q

Why does sinking air provide ideal arid conditions?

A
  • Dry air = lost most moisture as dropped in convectional rainstorms in equatorial regions
  • Cloudless and warm = can hold more moisture than cold air = no clouds form
  • Persistent = warm air can hold more moisture than cold air = lower air nearer surface = warm and dry
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10
Q

How does continentality cause aridity?

A
  • The tendency for the middle of large continents to experience extremes of temperature and less rain
  • Areas in centre of land masses (eg Simpson Desert in Central Australia) = dry because they are far from rain bearing winds which collect moisture from sea
  • Moisture is precipitated near coast = little moisture for continent centre
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11
Q

How does a rain shadow/relief cause aridity?

A
  • High mountain ranges block passage of rain bearing winds which increases aridity on leeward (sheltered side)
  • Moist air is forced to rise on mountain’s leeward side = air expands, cools and condenses to produce rain and cloud
  • Rains = any air on leeward side = already lost moisture = dryer and warmer on leeward
  • EXAMPLE = winds from SE reaching Andes and Rockies = moisture won’t reach west-facing slopes such as the Atacama Desert
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12
Q

How are arid areas distributed?

A
  • Hyper-arid mainly in Africa
  • Deserts further N and S of equator
  • Concentrated on west side of continents
  • Hyper-arid surrounded by arid surrounded by semi-arid
  • EXAMPLE = Arabian, Thar, Irania, Gobi, Sonoran, Great Bason, Sahara
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13
Q

What is mechanical weathering?

A

Occurs as a result of sudden temperature changes between hot days and freezing nights

  • Granular disintegration
  • Block separation
  • Shattering
  • Exfoliation
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14
Q

What is granular disintegration?

A

Mechanical weathering
- Grain rocks (eg granite) break down into grains of sand quickly as contains black and white crystals which heat up and cool down at different rates

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15
Q

What is block separation?

A

Mechanical weathering
- Well jointed sedimentary rocks (eg limestone) start to break down along their joints and bedding planes which are their main lines of weakness

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16
Q

What is shattering?

A

Mechanical weathering

  • Rocks which have neither coarse grains nor blocky structure shatter into irregular fragments with sharp edges
  • Basalt is black and metallic so absorbs heat and expands rapidly
17
Q

What is exfoliation?

A

Mechanical weathering

  • Expansion and contraction causes the surface layer to flake off = more exposed to temperature
  • Peeling process = onion skin weathering
18
Q

What is chemical weathering?

A

The erosion or disintegration of rocks, building materials, etc, caused by chemical reactions

  • Hydrolysis
  • Oxidation
  • Crystal growth
19
Q

What is hydrolysis?

A

Chemical weathering

- Breakdown of rocks by acidic water to produce clay and soluble salts

20
Q

What is oxidation?

A

Chemical weathering

- Breakdown of rock by oxygen and water = often giving iron rich rocks a rusty coloured weathered surface

21
Q

What us crystal growth?

A

Chemical weathering

  • Salt crystals grow between pores and joints when high temperatures draw saline groundwater to the surface and the water evaporates
  • Lead to granular and block disintegration
22
Q

What is wetting and drying?

A

Repeated expansion on wetting and contraction on drying causes rock to disintegrate
- Type of weathering

23
Q

What is hydration?

A

Minerals (eg anhydrate) absorb water and expand which causes stress and granular disintegration
- Water and anhydrite = gypsum – susceptible to other weathering processes such as carbonation

24
Q

Why is wind erosion effective?

A
  • Extreme pressure differences
  • Little vegetation to slow wind/hold soil together
  • Lots of fine debris from mechanical weathering
25
Q

What are the wind processes?

A
  • Deflation = entrainment and removal by wind of unconsolidated material (Deflation hollows = large enclosed depressions partly created by deflation)
  • Abrasion = when wind-blown sand abrades rock surfaces- Attrition = the action of sand grains colliding with each other and in doing so becoming smaller
26
Q

How does the wind transport?

A
  • Suspension = fine sediment carried within the air
  • Saltation =usually sand grains hopping along the surface
  • Surface creep = rolling along the ground
27
Q

What are landforms by wind erosion?

A
  • Yardangs
  • Rock pedestals
  • Desert pavements
  • Ventifact
28
Q

What are yardangs?

A

Landforms by wind erosion

  • Steep-crested linear ridges of rock orientated parallel to prevailing winds
  • Occur in groups
  • Can vary in height from few cms to over 100m and can be several kms in length
  • EXAMPLE = Kharga yardang field in Egypt
29
Q

What are rock pedestals?

A
  • Top is case hardened by rising fround water that contains salts
  • Case hardened = formation of mineral coating on surface of porous rock by evaporation of mineral-bearing solution
  • Salts crystallise in upper part = harder to erode
  • Bottom stem is thin due to process of wind abrasion = saltating grains abrade bottom of rock between 0-60cm = more effective as case not hardened
  • EXAMPLE = Ameib Ranch, Namib Desert
30
Q

What is a desert pavement?

A

Surface of stones resting on a finer material such as salt, silt or clay
- Form when wind/water removes finer material to leave behind larger stones

31
Q

What are ventifacts?

A

Wind-polished stones which look like brazil nuts and are few cms in size

32
Q

What are landforms by wind deposition?

A

Sand dunes

  • Mound of sand built by Aeolian processes
  • Types = transverse, linear and star dunes
  • Formed depending on wind direction
  • Sand is transported by suspension, saltation or surface creep = sand deposited as dunes by wind can be divided into two main types
  • EXAMPLE = Namib Sand seas
33
Q

What are types of water erosion?

A
  • Flash floods = rare thunderstorms but ground is baked so runoff rapid
  • Exogenous rivers (permanent river deriving its flow from beyond desert margin) = flow from wetter areas
  • Historic water = at end of last ice ages = wetter climates
  • Underground water = groundwater
  • Fog may bring moisture to these arid areas
34
Q

What are the landforms by water?

A
  • Alluvial fans
  • Playa lakes
  • Canyons
  • Wadis
35
Q

What are alluvial fans?

A

Landform by water

  • Fan shaped deposit made up of sediment overtime = often found at base of mountain ranges where intermittent streams flow out
  • Sediment drops out of stream flow as energy decreases due to widening of channel
  • Sediments build up overtime in channels at base of mountains and forces stream to carve another channel
  • EXAMPLE = Death Valley, California
36
Q

What are playas?

A

Landform by water

  • Formed where rock pools evaporate
  • Large and flat areas of land that were once lake beds
  • Covered with salt and other minerals (often white due to salt presence)
  • EXAMPLE = Bonneville Salt Flats, Utah
37
Q

What are canyons?

A

Landform by water

  • Gorge with a deep, narrow channel bounded by resistant rocks
  • Result from vertical erosion by rivers = carry coarse loads at times of high flow = abrades river bed = deeper
  • Valley floor often occupied by exogenous river
  • EXAMPLE = Grand Canyon, USA
38
Q

What are wadis?

A

Landform by water

  • Dry river bed with steep sides and wide flood covered with channel deposits
  • Form when flash floods/seasonal rain creates and ephemeral river (temporary river flowing seasonally/intermittently)
  • High discharge with availability of loose, dry sediment in channel bed = encourages transport of large amounts of sediment
  • Boulders are abraded and underlying bed rock is sourced
  • Vary in size from a single channel a few metres long to dense networks many kms in length
  • EXAMPLE = Wadi Rum, Jordan