Final answer:
Deserts are found between 15 and 30 degrees latitude north and south of the equator primarily because of the Hadley Cells, where descending dry air creates arid high-pressure areas, as well as the rain shadow effect from mountain ranges.
Step-by-step explanation:
Deserts generally exist between 15 and 30 degrees north or south of the equator due to the global wind and climate patterns known as the Hadley Cells. These cells create a cycle where warm moist air rises at the equator and cool, dry air sinks approximately 15-30 degrees latitude away from the equator. The descending dry air results in high-pressure, arid conditions, producing deserts.
Moreover, these areas are often on the leeward side of mountain ranges, leading to a rain shadow effect, where moist air releases its precipitation on the windward side, leaving the leeward side dry. Examples of this include the Mohave and Sonoran deserts. With evaporation typically exceeding precipitation, subtropical deserts can have extremely high daytime temperatures and very low annual rainfalls, such as those found in central Australia and northern Africa.