Deserts are typically defined by their unique characteristics:
Low Precipitation: Deserts receive less than 250 millimeters (10 inches) of precipitation annually, resulting in water scarcity.
High Temperatures: During the day, desert temperatures can soar to extreme highs, while at night, they can plummet to very low levels due to the lack of humidity.
Hot Deserts: Characterized by extremely high temperatures, examples include the Sahara Desert in Africa and the Arabian Desert in the Middle East.
Cold Deserts: Found at higher latitudes and elevations, with lower temperatures and sparse vegetation, examples include the Gobi Desert in Asia and the Great Basin Desert in North America.
Coastal Deserts: Located near coastal regions, with moderate temperatures and low precipitation, examples include the Atacama Desert in South America and the Namib Desert in Africa.
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