Structure of different layers of atmosphere with proper temperature radiant
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1️⃣Troposphere:
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.
2️⃣Stratosphere:
Above the troposphere from about 10 to 50 km above the surface is the stratosphere. The ozone layer is within the stratosphere .
3️⃣Mesosphere:
Above the stratosphere from about 50 to 80 km above the surface is the mesosphere. In this layer the air density is very low and the temperatures get extremely cold with height.
4️⃣Thermosphere:
The thermosphere extends from about 80 km above the surface and gradually merges into outer space. In this layer the air density is so low that measuring temperature begins to have little meaning.
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.
2️⃣Stratosphere:
Above the troposphere from about 10 to 50 km above the surface is the stratosphere. The ozone layer is within the stratosphere .
3️⃣Mesosphere:
Above the stratosphere from about 50 to 80 km above the surface is the mesosphere. In this layer the air density is very low and the temperatures get extremely cold with height.
4️⃣Thermosphere:
The thermosphere extends from about 80 km above the surface and gradually merges into outer space. In this layer the air density is so low that measuring temperature begins to have little meaning.
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