Air does not mix between the troposphere and stratosphere primarily due to the presence of a temperature inversion at the tropopause, which is the boundary between these two atmospheric layers. In the troposphere, temperature decreases with altitude, while in the stratosphere, it increases. This temperature difference creates a stable layer that inhibits vertical mixing, preventing the two layers from intermingling significantly. Additionally, the stability of the stratosphere prevents turbulence that could facilitate mixing.
Air from the troposphere and stratosphere cannot mix freely primarily due to the temperature inversion that characterizes the boundary between these two layers. In the troposphere, temperature decreases with altitude, while in the stratosphere, it increases with altitude. This temperature difference creates a stable layer that inhibits vertical mixing. Additionally, the presence of the tropopause acts as a barrier, preventing the turbulent air of the troposphere from easily entering the more stratified stratosphere.
Water vapor does not rise into the stratosphere primarily due to the temperature inversion that occurs at the boundary between the troposphere and stratosphere. In the troposphere, temperature decreases with altitude, allowing rising air to cool and condense, forming clouds. However, in the stratosphere, temperatures increase with altitude, creating a stable layer that inhibits the vertical movement of air and water vapor. Additionally, most water vapor condenses and precipitates out in the troposphere before it can reach the stratosphere.
The troposphere and stratosphere are the two atmospheric layers that can contain air as warm as 25°C. The troposphere is where most of the Earth's weather occurs and its temperature decreases with altitude. The stratosphere is located above the troposphere and contains the ozone layer, which absorbs and scatters UV radiation.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It is a fast-flowing, narrow air current that moves from west to east at high altitudes.
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.
Air from the troposphere and stratosphere doesn't mix freely because of a layer called the tropopause, which acts as a barrier preventing the two layers from easily intermingling. The tropopause has different temperature and pressure characteristics that act as a boundary between the troposphere and stratosphere. This separation helps maintain the stability and structure of each layer.
Air pressure decreases as you move from the troposphere to the stratosphere. This is because the weight of the air above is less in the stratosphere, leading to lower air pressure at higher altitudes.
Air from the troposphere and stratosphere cannot mix freely primarily due to the temperature inversion that characterizes the boundary between these two layers. In the troposphere, temperature decreases with altitude, while in the stratosphere, it increases with altitude. This temperature difference creates a stable layer that inhibits vertical mixing. Additionally, the presence of the tropopause acts as a barrier, preventing the turbulent air of the troposphere from easily entering the more stratified stratosphere.
The layers are present in stratosphere. These are troposphere, stratosphere, mesosphere, thermosphere.
it is same because there are both in the air.
air pressure decreases
Water vapor does not rise into the stratosphere primarily due to the temperature inversion that occurs at the boundary between the troposphere and stratosphere. In the troposphere, temperature decreases with altitude, allowing rising air to cool and condense, forming clouds. However, in the stratosphere, temperatures increase with altitude, creating a stable layer that inhibits the vertical movement of air and water vapor. Additionally, most water vapor condenses and precipitates out in the troposphere before it can reach the stratosphere.
The troposphere and stratosphere are the two atmospheric layers that can contain air as warm as 25°C. The troposphere is where most of the Earth's weather occurs and its temperature decreases with altitude. The stratosphere is located above the troposphere and contains the ozone layer, which absorbs and scatters UV radiation.
Ozone in the troposphere is considered a pollutant and harmful to human health at ground level, while ozone in the stratosphere is beneficial as it forms the ozone layer that protects the Earth from harmful ultraviolet radiation. The mechanisms for forming and breaking down ozone also differ between the two layers.
The Stratosphere, about 33,ooo Feet or 6.25 Miles up This is genrally (Above the Weather ) regarding commercial craft. Its actually located in the upper troposphere and is a big part of the weather scene. Hope that helped! :)
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It is a fast-flowing, narrow air current that moves from west to east at high altitudes.
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.