hot deserts and their land scapes : use with notes. Flashcards

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1
Q

what is meant by the term “hot desert”

A

a part of the workd with very high average temperatures and extremely low temperatures. These areas have less 250mm of rainfall/yr

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2
Q

what arethe 3 ways of classifying deserts?

A

hyper arid, arid and semi arid zones.

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3
Q

what is the aridity index of hyper arid zones?

A

<0.03

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4
Q

what are the characteristics of hyper arid zones?

A

AI of 0.03 Dryland w/o vegetation.

Nomadic pastorlasim os practiced here and annual rainfall is v v low.

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5
Q

what is the aridity index of an arid zone?

A

0.03 - 0.2

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6
Q

what is the aridity index od semi arid regions?

A

0.2 - 0.5

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7
Q

what is the aridity index.

A

The differenence b/w precip and pot evapotransp, It give value of water deficit and thus is used to classify deserts in terms of aridity. the LOWER the number the >er aridity.

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8
Q

what is aridity?

A

the state of being v v dry w/o enough rain for plants.

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9
Q

characteristic/ definition of an “arid zone”

A

the climate of an area that reaches <250mm precipitation/yr.

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10
Q

characteristics/definition of a “semi arid” zone?

A

The climate of an area that recieves b/w 250mm and 5000mm precip/yr.

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11
Q

what is potential evapotranspiration?

A

drying power, ie the amount of water that would evaporate/trapnspire if it was present.

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12
Q

EQ: Based on the characteristics of a hot desert in hyper arid, arid what would happen to the water if there was a storm?

A

HIgh temperatures result in soils being baked hard and as result, water would runoff thus low infiltration and high overland flow.
Hot temperatures also means that the water will evaporate vv quickly.
Cactus have v v long roots and thus will absorb any water v v quickly ( and swell up)

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13
Q

Where are hot deserts located Ie the distribution?

A

Hot deserts cover 1/5th of the surface of the earth adn they run in parralel belts that run along the tropics 30N and south of the equator. They occur in hot arid and semi arid mid and low latitudes. They continetianally tend to sit on the Western side of of continents such as those in SOuth AMerica(the Atacama)
They can also be found behind mountain ranges.

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14
Q

what are the major deserts in the N hemisphere?

list by the regions North America, Africa, Asia

A

North America : Mojave, Sonoran
Africa : Sahara
Asia : Thar streching from the red sea to the middle east to pakistan and India), Arabian desert

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15
Q

What are the major deserts in the S hemisphere?

list by continet ie South America, Africa and Australia

A

S America –> Atacam
Africa : Namib , Kalahri and Karoo
Australia : Great Sandy , Great Victoria and the SImpson desert.

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16
Q

which 4 ways can cause aridity?

A

cold ocean currents
relief (ie rainshadow effect)
continentiality
general pattern of atmispheric circulation.

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17
Q

How does the global atmospheric circulation lead to aridity?

A

At the equator, there is a net gain in energy due to large amounts ofsolar insolation from the overhead sun. Air in contact with the earth will rise and cool forming clouds and leading to precipitation, The rising air is replaced by air rushing in from N and S creating an aea of low pressur e(high rainfall) known as the ITCZ. Rising dry air begins to cool + move polwards + at 20/30 degrees it descends, creating an area of high pressure. As it desends it warms and expands resulting in little cloud formation and thus clear skies which result in high heat and aridity in these areas.
In areas of high pressure, winds also blow outwards so no moisture brought in thus low precip –> v v arid + dry.
High pa also means lack of cloud formation thus >er aridity.

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18
Q

how does continentiality result in aridity

A

Central parts of continents are more arid than coastal areas.
Water heats up the water in coastal areas slowly (and to a lower temp than that of the land) due to high SHC. Evaporation occurs from the water and latent heat is also transferred along water droplets to atoms. Cool and condense ==> rain and thus coastal areas recieve high er amounts of precipitation.
Inland, there are no clouds to block insolation and thus temps vv high durign day but also high diurnal range so land cools rapidly at night. When air moves inland, it has low moisture cotntent (after dropping it all by coasst ) –> high aridity

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19
Q

how does relief result in aridity?

A

Tall mountains force winds upwards and thus the air rises. As the air cools and condenses, its ability to hold water declines and thus water dropped as relief rainfall over the mntns. As prevailing wind continues to carry the air over the mountain inland, the air holds vv little moisture and thus little rainfall occur on the leeward side of the mntns. AIr descenbds on the leeward side of the mntn , and the sinking air warms up slightly resulting in the ar above being v v clear + dry w/ no rainfall (humidity also drops). This is the rainshadow effect.

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20
Q

how do cold ocean currents result in aridity?

A

prevailing winds that pass over cold oceans is cooled, increasing humidity and eventually the moisture condenses to form a fog offshore. As the land heats up quicker than sea, this may generate onshore breezes, which suck fog + mist inland. However the intense heating from the sun directly overhead burns this away resulting in deserts being dry and arid.
When mositure is released as precip its released over the ocenas before hitting land and thus air that does move in has low moisture content and thus low rainfall.

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21
Q

what are the main characteristics of hot desert?

A

The are hot and have large variations in temp
they have little vegetation
the soils are dry and infertile.
spotty rains

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22
Q

what kind of temperatures do hot deserts experience?

A

Diurnal temperatures.

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23
Q

What is meant by a diurnal temperature range?

A

It is the diff b/w the v v high daytime temp(ie >40 deg) where land is heated due to direct insolation from the sun and the v v cool night temps where temp drops rapidly

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24
Q

How is the rainfall in hot deserts described as and why?

A

“Spotty” –> it is sporadic and often unpredictable.

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25
Q

Hot desert characterisitc : Hot + large variation in temp

A

Mean avg temp is around 2- - 30 deg however there is SOME seasonal variation w/ temp risign to 50 de in summer and below 0 in winter.
The temps also vary daily due to the diurnal temp ranges.
in desert margins the annual temps are lower b/w 10 - 20 degs and thus the temp extremes are less extreme.
The large vatriations in temps is due to the high pa dry desert air that has no clouds thus cant block out sunlight during the day OR insulate/trap heat in the night.

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26
Q

Hot desert characteristic : little vegetation

A

Biomass is v v low in hot deserts fue the lack of water which makes it v v hard to grow. Amount of veg varies(ie sand dunes or plenty of cacti and grasses) .
Plants such as cacti are specialised to survive inthe hot and arid conditions.
however in desert marigns, there is more vegetation incl grasses and shrubs. The no of veg increases as u move away from center of desert due to the increaing availability of water.

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27
Q

hot desert characteristic: Dry and infertile + unproductive soils

A

Soils are infertile in some areas due to the high salt content which arises due to the accumulation of salts as a result of capillary action moving water upwards. Soils are unworkable and sandy/rock and dry due to low rainfall and high temps ans thus as a result its v v hard to sew seeds that will root bc soils are tooo dry.

in desert margins however, the soils are much more fertiel than soils in the desert bc there is more vegation to fall and thus create leaf ltter + huma thus org matter which veg needs to grow.
Soil is less sandy than those in deserts duye to greater weathering in desert margins.

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28
Q

what percentage of the earths surfaces is desert soils ?

A

17%

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29
Q

how much soils as a % is present in AUstralia ?

A

44%

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30
Q

what is the % of desert soils in Africa?

A

37%

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31
Q

what is the % of desert soils in Eurasia ?

A

15%

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32
Q

why migh soils not develop well in arid climates.

A

when soils 1st develope in desert soils they start of as thin alkaline and saline soils w/ v v thin profiles.

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33
Q

what is the reasoning for the slow rate of soil devlopement.

A
  • little vegetation : due to lack of water from lack of rainfall.
  • the little plants that are adapted to the hot desert environment. Plants that are adapted against absicission dont add to hummus layer ie the spines of cacti.
  • heat –> high temperature results in water in soils evaporating.
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34
Q

what are most desert soils characterised by?

A

A thick accumulation of basic mineral salts ie Ca2+ and Na+ compounds.

35
Q

why are desert soils saline (ie the crust of aslt)

A

the high temperatures mean that there are high levels of evaporation>precip resulting in capillary action pulling moisture up from the sand aling w/ dissolved minerals. when the water eveporates, the minerals form a salty crust at the soil surface.

36
Q

apart from creatign a vv dry environment how else does lack of rainfall shape the characteristics of the soils.

A

the lack of rainfall means that htere is limited weathering of rock, which when it does occur is vv v slow and thus soils are vv thin.

37
Q

Outline the 4 main fetures of soils in hot desert environments (4m)

A
  • soil is a micture of organic and inorganic material
  • deserts have very poorly developed and thin soils due to the lack of organic matter forming humus. Even when the scarce highly adapted vegetation dies, the lack of water stops it decomposing and producing a humus to enrihc a developing soil
  • desert soils are v v sandy porous and permeable and thus have a poor moisture retention.
  • however, wilst the soils have a poor quality , the lack of rainfall means that leaching is minimal and thus there are some plant nutrients that are avalable and w/ the right irrigation + soil mnagemnent crops an be grown successfully in desert regions ie Almeria , Spain,
38
Q

what is the main soil type in deserts?

A

Aridisols

39
Q

what are aridisols?

A

they are a soil characterised by the accumulation of mineral salts near the surface.

40
Q

describe the soil profile for aridisols?

A

they range from a redding yellow to a grey brown depending on the nature of the parent material.
they are generally v v thin (<100cm).

41
Q

describe some characteristics of aridisols

A

alkaline,
saline,
infertile
climate drives the vegetation here
low organic content in soils ( due to the lack of decomposition of organic matter as it is v v slow + low)
these soils also have v v sparse vegetation due to the low amounts of rain

42
Q

are deserts just areas of sand?

A

no, the sand layer has soils beneath them

43
Q

why are desert soils not vv fertile:?

A

they dont contain much organic matter (due to the lack of vegetation growing here)

44
Q

why are desert soils vv dry

A

evap>precip
low rainfall
high temperatures.

45
Q

what are the 2 main types of aridisols?

A

sierozems and raw mineral soils.

46
Q

are siernozems semi arid or arid regions

A

semi arid

47
Q

are raw mineral soils semi arid or arid regions

A

arid

48
Q

what kind of texture do raw mineral soils have and why?

A

coarse textre due to the physical weathering.

chemical weathering also does occur and thius results in capillary action resulting in the accumulation of Ca2+ and Na+

49
Q

why are the soils v v similar b.w the horizons in raw mineral soils

A

thre is a lack of moisture so there is limited leaching

50
Q

why are the raw mineral soils deemed more unproductive than infertile

A

they do have some minerals and salts available but the lack or rainfall and the extreme temperatres limit the veg.
the lack of abscission als omeans there is no leaf litter and thus no humus or organic matter.

51
Q

what can form on the surfce of raw mineral soils and why?

A

hard salt crusts.

52
Q

what are siernozems?

A

these are grey desert soils

53
Q

where do siernozems occur?

A

in arid regions where the rainfall recieved is less than 250mm

54
Q

what do siernozems look like? why?

A

they are darker in colour, due to the presence of some organcic moisture + matter as they often develope beneath desert shrun

55
Q

what are siernozems often used for?

A

cultivation and with continued irrigation, they form calcium rich horizons

56
Q

what is meant by the term humus?

A

amouros dark coloured colloidal matter in the soil. Its a complex of of the fractions of organic matter of plant, animal and microbial organisms that are most resistant to decomposition.

57
Q

what ar ethe 3 main factors that make it difficult for vegetation to survive in hot deserts?

A

lack of rainfall
soil
heat

58
Q

why does the lack of rainfall make it challenging for vegetation to survive inhot deserts?

A

the rainfall is often spotty and comes in short sharp bursts. The lack of rainfall makes it difficult for plants to grow

59
Q

why does the soil in hot deserts make it hard for vegetation to survive

A

the soil sare often v v salty and poor quality. they lack nutrients and are victim of slow decomposition

60
Q

why does the heat make it hard for vegetation to survive.

A

the temperatures are extreme and the effect of diurnal temperatures also makes it v v hard.

61
Q

how do plants in desert survive then?

A

they have special adaptations.

62
Q

what types or of plants usually grow in deserts?

A

short woody trees, ground hugging shrubs.

63
Q

why do plants have waxy cuticles?

A

thick waxy cuticles to reduce water loss but to help reflect suns heat

64
Q

what are the 4 main typees of plant adapted to the desert environment.

A

xerophytes,
phreotophytes,
ephemrals,
halophytes

65
Q

what are xerophytes and how are they adapted to desert climates?

A

succulent plants that contain certain compunds in flesgy leaves/stems that allow them to store ALOT of water.

66
Q

why is it difficult for plants to obtain water after a rainspell in the desert and how are xerophytes adapted to this?

A

the water doesnt penetrate deep in the soils and the soils dont remain moist for long periods of time. As a result succulents have the ability to rapidly absorb huge amounts of water.

67
Q

what are the adaptaptations that xerophytes have to conserve water?

A

thicj waxy cuticles
closed stomata –> both of these make the surface water proof
smally spiky or even no leaves to reduce the SA to limit transpration go

68
Q

give an example of a xerophyte and how its adapted to live in the desert

A

saguaro cactus
- can live for 200yrs and cab abdorb upto 800l of water in arms and stems.
have water in the roots and bulbs on the root systems and they survive on yrs of drought relying on the water recived on a single rain

69
Q

what are phreatophytes?

A

plants with long root systems that lie just beneath the surface.

70
Q

why are the

roots v v long in phreatophytes?

A

the water after rainfall doesnt penetrate v v far and thus roots are long to absorb the water near the surface laterally.
,

71
Q

give an example of a phreatophyte and how its adapted to hot deserts?

A

creosote bush.
has a root system that reaches v v deep ground water as well as being v v radial.
it has a bitter taste + smell to deter animals from eating it.
It also has small leaves and little stomata that close during the day to prevent water loss.
The long roots are also vv tough and hardy and thus anchor them into the sand and allow them to survive in constant;y shifting sand dunes.

72
Q

what are halophytes?

A

plants that are adapted to the salty poor quality soils in hot deserts.

73
Q

how is the saltbrush adapted to jot deserts

A

excrete salt from glands when the conditions are too salty

74
Q

how is the pickle weed adapted to the high salinity pf hot desert soils

A

they have a high water uptake to compensate for the high salt content

75
Q

how else do halophytes adapt to saline conditions

A
  • some develope succulence which dilutes the level of salt in the plant and stores water for use during the dry periods.
    some seeds are kept dormant due to the high salinity but germinate when the rains come and reduce the salinit
76
Q

what are ephemerals?

A

plants that avoid drought altogether by having v v short life cycles
they blom v v rapidly after a rain , channellign their energy into producing seeds that lay dprmant until future rains.

77
Q

give an example of a ephemeral plant?

A

desert lily in the Mojave + sonoran
this plant stores energy in the root and bulds which form deep underground. the energy stored in spring allows the plant to survive almost a yr round dormancy.

78
Q

give an example of a perrenial ephemeral plant?

A

desert paint brush.
thus grows rapidly after the winter rains and flowers + produces seeds. the seed are v v hardy and drought resistant and v v resistant to high temperatures.

79
Q

what are some other ways that plants are adapted to protect themsleves against thirsty desert animals?

A

spikes + spines
bitter taste or toxicity
living in inaccessible locations
creosote bush gives off toxic chemicals that prevent other plants growing near it and competing for the same local water supply

80
Q

what is allelopathy

A

Allelopathy is a common biological phenomenon by which one organism produces biochemicals that influence the growth, survival, development, and reproduction of other organisms
it is responsible for plants growing in unifromed spaces in desers.

81
Q

what is a desert hycinth

A

a parasitic plant that takes nutrients form a halophyte.

It is parasitic bc it cant directly synthesis chlorophyll and thus cant photosynthesise.

82
Q

what are the 3 mechanisms of seed dispersal for desert plants?

A
wind dispersal (ie tumble weeds) 
water dispersal ( blue palo verde tree) 
animal dipersal (Cholla or the jumiping cactus.
83
Q

how can plants reduce transipration to survive in hot deserts?

A
  • may hav eless seeds, throns and spikes which all have small surface areas and small leaves to reduce moisture loss.
    some lose leaves completely in the summer months BUT still have green stems to allow for photosynthesis .
    Some OPEN stomata duringthe DAY and close them at night to absorb co2 in day for p.synth ad to release h20 via evap. closing stomata during hte day would reduce water loss BUT also limit photosynthesis.
    the stomata w/inthe grooves of the leaf vreate microclimates which are humid + have low water vapour potential gradient and thus reduce water loss via transpiration.