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Ice age cycles explain why the Earth cools, warms, and whether another freeze is coming
While the Milankovitch Cycles operate on timescales far longer than human lifespans, their effects are always at play.
Around 20,000 years ago, Earth was very, very cold. Global temperatures were 10 degrees Fahrenheit colder than they are today and most of North America was covered in ice. That ice was almost half a ...
Scientists have uncovered a missing feedback in Earth’s carbon cycle that could cause global warming to overshoot into an ice age. As the planet warms, nutrient-rich runoff fuels plankton blooms that ...
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