Weather is confined to the troposphere because : <u>The temperature of the stratosphere prevents tropospheric air from rising into it</u>.
<h3>Why is weather confined to the Troposphere?</h3>
Weather, as most commonly defined, occurs in the troposphere, the lowest region of the atmosphere that extends from the Earth’s surface to 6–8 km (4–5 miles) at the poles and to about 17 km (11 miles) at the Equator.
The troposphere is the layer where most of the world's weather takes place. Since temperature decreases with altitude in the troposphere, warm air near the surface of the Earth can readily rise, being less dense than the colder air above it.
Weather is largely confined to the troposphere since this is where almost all clouds occur and almost all precipitation develops. Phenomena occurring in higher regions of the troposphere and above, such as jet streams and upper-air waves, significantly affect sea-level atmospheric-pressure patterns—the so-called highs and lows—and thereby the weather conditions at the terrestrial surface.
Its Basically, because that is the layer where most of the water vapor exists, as well as it is the layer where the greatest energy imbalance between the surface and the atmosphere exists.
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