The Equator shows two peaks in daily insolation over the course of a year.

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The Equator receives two peaks in daily insolation over the course of a year, as it is the region where the sun's rays directly hit the Earth's surface for the most extended amount of time. This phenomenon occurs during both the equinoxes, when the tilt of the Earth is aligned with the sun, resulting in equal amounts of daylight and darkness. Throughout the year, the length of the day and the amount of sunlight received varies between the Equator and the poles, leading to different patterns of insolation.

The Equator Shows Two Peaks in Daily Insolation Over the Course