Desert is a biome characterized by low amount of rainfall (>250mm), high temperature (40 - 50 °C in summer), and sparse vegetation.
Characteristics of a hot desert:
near tropics of cancer and capricorn
very little biodiversity
very hot (in summer cand be over 50 degrees)
cold at night (0 degrees)
less than 250 mm of rain
soil is sandy,rocky,thin and has a crusty layer of salt
Plant adaptations in a hot desert:
Small leaves/spikes - less waterlost by transpiration
Taproots - long roots (7-10m) that reach deep underground to access water
Waxy skin - thick,waxy skin to reduce water loss by transpiration
Water storage - some plants store water in stems,leaves,roots because of infrequent rainfall
Desertification prevention:
Planting more trees
Planting drought resistant plants
Bunds
Flat roofs, water can collect on top
Desertification causes:
Population growth
Cutting down trees
Overgrazing (when land cannot sustain the number of animals feeding on it)
Soil erosion
Climate change
Examples of deserts are Sahara desert in Egypt, Africa and Thar desert in Rajasthan, India.
Soil in a desert:
Lack of organicmaterial due to lack of vegetation
Very dry and soaks up waterrapidly
Evaporation draws salts to surface, leaving whitepower on the ground
Not very fertile
Animal adpatations in a desert:
Fennec fox - largeears to hear prey and regulate body temperature
Thorny devil - has thorns that cover body to protect against predators
Camel adpatations :
Longeyelashes - to protect against sand
Thickfur - provide warmth at night
Fat filledhump - supply energy
Longlegs - efficient for travellinglong distances
Widepaddedfeet - easier to walk on sand and rock
Paddedknees - protect when kneeling on hot sand
Thinslits for nostrils - closed during a sandstorm
Desertification - the process of land turning into desert
If vegetation is removed then there will be no roots to bindsoiltogether. So if strongwinds or heavyrainfall occurs, the soil will be washedaway, this is called soilerosion. Overtime this can lead to desertification.