hot deserts Flashcards
describe the distribution of hot deserts globally:
hot deserts are mainly distributed on and around the tropics of Cancer and Capricorn, and never on the Equator. they’re situated on the majority of continents, especially in North Africa and the West of South America.
describe the rain-shadow effect:
moist air arrives from a body of water, and encounters a mountain. the air is forced to rise over the mountain, cool, condense, and form rainclouds. rain falls on the windward side of the mountain, creating a rainforest. the air then continues over to the other, leeward side of the mountain, and sinks. this cold, sinking air creates an area of high pressure, creating cloudless skies and little rain. this is the rain shadow region, where a desert forms.
what is the average desert climate throughout the year?
- temperature rises to a peak towards the middle of the year, with lowest average temperatures being 16/17 degrees celsius in december, and highest temperatures being roughly 45 degrees celsius in july.
- rainfall is low all year round, with the highest yearly rainfall occurring in january, at 4.5 mm of rain across the entire month. may and june usually have particularly low rainfall levels, at 0-2 mm of rainfall.
how does the Hadley cell influence where hot deserts occur?
- the sun is overhead at the equator and water evaporates. it heats the air, which rises and carries moisture up. it then cools and condenses to form rain. this forms a tropical rainforest.
- the air continues to the north and south, and the dry air begins to sink at the two tropics, creating clear skies and desert conditions. this is where deserts occur, at about 30 degrees north and south of the equator.
- the air then travels back to the equator, and the cycle starts again.
what are the physical characteristics of the desert ecosystem?
- lack of vegetation
- poor, dry soil
- clear skies (due to high pressure)
- mountains/flat plains
- hot, has little rain
- extreme temperatures: over 45 degrees celsius during the day, drops to 0 degrees celsius at night.
- less than 250mm of rainfall per year.
describe the desert climate:
- a daily diurnal range: hot in the day, cold at night. this is because clear skies during the day mean the sun can heat the surface temperature to over 40 degrees celsius. at night, however, there are no clouds to act like a blanket to keep the heat in, so heat is lost. temperatures drop very low, to even 0 degrees celsius.
- windy with frequent sandstorms as air moves from high to low pressure.
- unreliable rainfall: flash floods can happen as sometimes, the whole year’s rainfall falls in one very heavy storm.
- dry with overall very low rainfall all year: the definition of desert is a place which receives under 250mm of precipitation/per year.
how is water accessed in desert areas?
- the Hoover Dam helps store the water of the Colorado River in Lake Mead behind.
- in many desert areas, water is stored in underground rocks called aquifers. it can then be pumped to the surface for use.
- large canals and aqueducts then distribute water to desert areas in Arizona and California.
> this does mean that water is subject to
evaporation, however, but the process is
relatively easier and less expensive.
describe desert soil:
- can be either rocky/sandy.
- the soil is exposed to extreme temperatures, and is often partially formed because of the lack of water.
- high evaporation rates mean that salts are drawn to the surface, leaving a white crust. this is called SALINISATION.
- the lack of plants means there’s little organic matter in the soil, so it’s not very fertile.
describe some common animal adaptations:
- nocturnal: it’s cooler to hunt at night than during the day.
- live underground: provides shade from the hot midday sun.
- large ears: (e.g. fennec fox). blood flow through the ears will be cooled by the wind through the stretched, taut skin. this blood then re-enters the body and cools the animal internally.
- bushy tails: (e.g. desert ground squirrel). when animals hunt, the tail can act as a parasol, when positioned correctly. this prevents the animal from overheating.
describe the adaptations of a camel:
- stretchy nostrils that open and close to keep out the sand.
- a leathery mouth, allowing camels to eat spiky plants (e.g. cacti).
- long eyelashes with multiple layers to keep sand out of their eyes.
- hump on the back to store fats and minerals, which can be broken down into essential nutrients (e.g. water) during droughts, which are common in the desert. water is stored under the belly to keep it cool.
- padded feet protect the feet from sinking into the ground, and to protect it from the heat of the ground.
describe the adaptations of meerkats:
- dark patches around the eyes help cut down on the sun’s glare.
- long, horizontal pupils give them a wide range of vision to spot predators more easily.
- thin fur and dark stomach skin help to regulate body temperature.
- a special membrane can cover and protect the eye while burrowing, and close-able ears to prevent sand-intake.
describe the adaptations of the desert holly:
- takes salt from the soil and creates a thin white surface coating to reflect the sunlight.
- it’s leaves grow at a 70 degree angle, so that the plant doesn’t receive direct sunlight at midday.
- some have long, shallow roots, which collect water over large areas.
describe the adaptations of the saguaro cactus:
- many long but shallow roots to soak up as must water as possible after rainfall.
- thick, waxy skin reflects some of the sun’s heat and reduces moisture loss through transpiration. it also takes up the job of photosynthesis, because of its chlorophyll presence.
- spikes instead of leaves reduce moisture loss (more efficient in heat) and prevent many animals from eating the plant.
how can a thick, fleshy body aid some plants?
thick, fleshy bodies (called succulents) allow the water to be stored inside the plant and to be used during long periods of no rainfall (droughts).
describe interdependence in a hot desert:
- the growth of plants is limited due to the extremes of temperature and lack of water
- therefore the nutrient cycle is very slow
- due to a lack of organic matter, the soils are coarse, sandy, and low in nutrients
describe biodiversity issues in the desert:
- low levels of precipitation and high temperatures lead to low biodiversity
- therefore where water is available there are higher levels of biodiversity, and this can lead to a ‘desert bloom’, leading to over 200 species of flowers blooming, also attracting insects and lizards.
- human activities also threat biodiversity, such as mining, climate change and fuelwood gathering.