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.
Use mathematical representations to support and revise explanations based on evidence about factors affecting biodiversity and populations in ecosystems of different scales.