the atmospheric layers ratified at higher levels give reason
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Troposphere: From the surface to about 10 km aloft is the troposphere. Much of the weather that takes places in the atmosphere occurs in this layer. On average, the temperature decreases with height in this layer because the sun warms the surface and then that heat is distributed upwards. It gets colder in the layer the further above the warmth of the surface. One of the characteristics of the troposphere is how much the air mixes, thus it is sometimes referred to as a mixing layer. Mixing occurs so easily since this layer has warm air under cold air. Convective thermals from the surface mix the air in the layer similar to what you would see in a lava lamp.
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