Jet streams form where cold polar air meets warm tropical air. This creates a very steep “pressure gradient” in the upper atmosphere. Think of it like a steep hill; the steeper the temperature difference, the faster the air “rolls” down ...
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Jet streams form where cold polar air meets warm tropical air. This creates a very steep “pressure gradient” in the upper atmosphere. Think of it like a steep hill; the steeper the temperature difference, the faster the air “rolls” down ...