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troposphere:- The troposphere contains particles of dust which serve as nuclear centers for the formation of clouds. There is decrease of temperature with a mean rate of about 6.40C per km. it is from 0 to 15 kilometers. it has more air and has many clouds. Stratosphere No visible weather phenomena take place in this layer In this layer the temperature does not change with altitude.er stratosphere it is from 15 km to 50 km. there is very little air and jet aeroplanes fly in this layer.
The height of the Tropopause depends mainly on the Latitude. At the Poles, it is about 30,000' and at the equator it is about 60,000. This number varies with a change in temperature/season. It is higher at the equator due to a naturally higher temperature at sea level, this means the parcel of air has a lower density. Because of the lower density the parcel of air will be more 'stretched out' than the air at the poles (the colder parcel of air with a higher density).
The stratosphere is very dry; air there contains little water vapor. Because of this, few clouds are found in this layer; almost all clouds occur in the lower, more humid troposphere. Polar stratospheric clouds (PSCs) are the exception. PSCs appear in the lower stratosphere near the poles in winter. They are only found in certain latitudes and temperatures.
Troposphere
The thermosphere and the stratosphere are two atmospheric layers that can have warm air.
The layers are present in stratosphere. These are troposphere, stratosphere, mesosphere, thermosphere.
it is same because there are both in the air.
Layers of atmousphere/Air: Troposphere, Stratosphere, Mesosphere and Theremosphere
air pressure decreases
air pressure decreases
In the troposphere, plants and animals can be harmed, but in the stratosphere, there is no life because in the troposphere is closest to earth n the air u breath is part of the troposphere. and in the stratosphere the air can affect your lungs
troposphere:- The troposphere contains particles of dust which serve as nuclear centers for the formation of clouds. There is decrease of temperature with a mean rate of about 6.40C per km. it is from 0 to 15 kilometers. it has more air and has many clouds. Stratosphere No visible weather phenomena take place in this layer In this layer the temperature does not change with altitude.er stratosphere it is from 15 km to 50 km. there is very little air and jet aeroplanes fly in this layer.
The height of the Tropopause depends mainly on the Latitude. At the Poles, it is about 30,000' and at the equator it is about 60,000. This number varies with a change in temperature/season. It is higher at the equator due to a naturally higher temperature at sea level, this means the parcel of air has a lower density. Because of the lower density the parcel of air will be more 'stretched out' than the air at the poles (the colder parcel of air with a higher density).
Because of the temperature in the troposphere that decreases as the altitude also lowers, convection only happens on it and not in the stratosphere. Also, because of the warm air from the land that is rising to the troposphere it becomes denser than the air above it that makes convection only happen in the said layer.
The stratosphere is the second layer in the atmosphere, right above the troposphere. The air is warmer the higher you go up and cooler farther down. Commercial aircraft flies in the lower layer of the stratosphere.
the sun's radiation warms it up.
This is the troposphere. It is the layer of air where all weather occurs. Above the troposphere is the stratosphere, home of the ozone layer.