The greater the angle of insolation, or the angle at which sunlight strikes the Earth's surface, means that solar energy is more concentrated over a smaller area, leading to increased temperatures. This typically occurs in regions closer to the equator, where the sun is more directly overhead throughout the year. Conversely, locations at higher latitudes receive sunlight at a lower angle, resulting in less intense insolation and cooler temperatures. Thus, the angle of insolation significantly influences climate and weather patterns in different regions.
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