Precession is related to the Ice Age in the sense that it helps propagate and is line with the Ice Age's theory about astronomy, especially pertaining to the earth's orbital forces and the rotation of the earth's axis.
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Precession is one of the factors that influences the Earth's climate over long periods of time, including during ice ages. It refers to the slow wobble in the Earth's axis of rotation, which changes the distribution of sunlight reaching different parts of the planet. This can affect how much solar energy is received in certain regions, potentially contributing to the onset or termination of ice ages.
Precession refers to the slight wobble in Earth's axis as it spins, which affects how sunlight is distributed on the planet's surface. This wobble can influence the timing and intensity of seasons, potentially playing a role in the onset and duration of ice ages. The combination of precession, axial tilt, and orbital eccentricity can lead to changes in the Earth's climate over long periods of time, impacting glaciation patterns.
Earth's precession is believed to be one of the contributing factors to the ice ages, but it is not the sole cause. The most recent ice age, known as the Quaternary glaciation, began around 2.6 million years ago and ended approximately 11,700 years ago. This glacial-interglacial cycle was influenced by a combination of factors, including variations in Earth's orbit, tilt, and precession, as well as changes in atmospheric composition.
Earth's precession
10,000 years ago APEX
During the Ice Age, approximately 30 of the Earth's surface was covered in ice.