commit 7d2a1eff603b0f79d76c1d6feedcaa5fdb919557 Author: dalenetracy662 Date: Mon Aug 18 04:51:23 2025 +0800 Add What else is Happening? diff --git a/What-else-is-Happening%3F.md b/What-else-is-Happening%3F.md new file mode 100644 index 0000000..0dab03c --- /dev/null +++ b/What-else-is-Happening%3F.md @@ -0,0 +1,7 @@ +
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The gases that make up Earth's atmosphere are topic to the planet's gravity. In truth, the ambiance weighs in at a mixed 5.5 quadrillion tons (4.99 quadrillion metric tons). The fuel molecules at the bottom, or these closest to the Earth's surface where we all live, are compressed by the load of the air above them. The air closest to us can be the warmest, because the atmosphere is mostly heated by the land and the sea, not by the solar. To grasp this precept, consider an individual frying an egg on the sidewalk on a hot, sunny day. The heat absorbed by the pavement actually fries the egg, not the heat coming down from the solar. When air heats up, its molecules transfer farther apart, making it less dense. This air then rises to larger altitudes where air molecules are less compressed by gravity. When heat, low-pressure air rises, cool, high-strain air seizes the chance to move in underneath it.
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