Summary
Sun warms the surface by day; at night the surface loses heat by radiating it into space. Clouds, humidity, and wind change this ‘heat escape,’ making some nights biting and others mild.
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Summary
Sun warms the surface by day; at night the surface loses heat by radiating it into space. Clouds, humidity, and wind change this ‘heat escape,’ making some nights biting and others mild.
On a historical timescale, the Sahara was green and wetter “yesterday.” As rainfall patterns shifted, lakes shrank—leaving not just sand, but a massive climate story.
We picture sand, but deserts are defined by rainfall. Antarctica gets so little precipitation it’s technically a vast desert—its snow cover simply hides the fact.
As cities expand, they often build on top of older layers—streets rise and history stacks. Underground, old houses, shops, and roads can remain like frozen time.
While a mountain’s windward side gets soaked, the other side can dry out. Air rises, drops rain, then descends, warms, and loses moisture—creating a rain shadow.
In some coasts there’s water but almost no usable oxygen, forcing life to flee. Excess nutrients trigger algal blooms, then decay consumes oxygen and the area goes quiet.
The rocks at the bottom of the Grand Canyon are about half as old as Earth.
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