Variation in the intensity of sunlight affects temperature differences on Earth's surface primarily due to the angle at which sunlight strikes the ground. Areas receiving direct sunlight, such as the equator, experience higher temperatures because the sun's rays are concentrated over a smaller surface area. In contrast, regions at higher latitudes receive sunlight at a slanted angle, dispersing the solar energy over a larger area, thus resulting in cooler temperatures. Seasonal changes and atmospheric conditions can also influence how sunlight is distributed, further contributing to temperature variations.
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