Uneven heating of Earth is influenced by heat capacity variations between land and water, sunlight angle changes, and air pressure differences.
Uneven heating of the Earth's surface is caused by several factors, including the difference in heat capacities between land and water, the variations in the angle of incoming sunlight at different locations, and the resulting circulation of air from areas of high pressure to low pressure. This leads to regions receiving varying amounts of solar energy and experiencing different heating rates.
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