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Answer»

Answer:

The jet stream RESULTS from horizontal differences in temperature that EXIST over a considerable vertical distance through the troposphere. These temperature differences produce a horizontal pressure gradient that DRIVES geostrophic and gradient winds. The GREATER the horizontal temperature DIFFERENCE, the stronger the jet stream.

Explanation:

The jet stream results from horizontal differences in temperature that exist over a considerable vertical distance through the troposphere. These temperature differences produce a horizontal pressure gradient that drives geostrophic and gradient winds. The greater the horizontal temperature difference, the stronger the jet stream.



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