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The depth of the trophosphere, or the layer of the atmosphere where most weather phenomena occur, typically varies from the surface up to about 8 to 15 kilometers (5 to 9 miles) above sea level, depending on geographic location and atmospheric conditions. It is generally deeper in tropical regions due to warmer temperatures, which increase buoyancy and convection, while it tends to be shallower in polar areas. Additionally, factors such as seasonal changes and weather systems can also influence the depth of the trophosphere.

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3w ago

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