in homosphere the concentration of gases remain same and gases are mixed while in heterosphere conc. of gases is different and gases are in the form of layers.Read more: What_is_the_difference_between_homosphere_and_the_heterosphere
The homosphere is the lower part of the Earth's atmosphere where the composition of gases is relatively constant and well-mixed, extending up to about 80 km altitude. In contrast, the heterosphere is the upper part of the atmosphere where gases separate based on their molecular weight, with lighter gases like hydrogen and helium being found higher up.
The homosphere is the lower atmosphere, from the Earth's surface up to about 60 kilometers, where the composition of gases is relatively uniform and well mixed. This region includes the troposphere and the lower part of the stratosphere.
The region of the atmosphere that is evenly mixed and behaves as if it were a single gas is the homosphere. This layer extends from the Earth's surface up to about 80 kilometers in altitude and includes the troposphere and most of the stratosphere. In the homosphere, gases are well-mixed due to turbulence and convection processes.
In the troposphere and stratosphere, gases maintain an approximately uniform composition due to mixing processes like convection in the troposphere and slow diffusion in the stratosphere. The concentration of gases starts to vary noticeably in the mesosphere and thermosphere due to decreasing density and interactions with solar radiation.
in homosphere the concentration of gases remain same and gases are mixed while in heterosphere conc. of gases is different and gases are in the form of layers.Read more: What_is_the_difference_between_homosphere_and_the_heterosphere
The troposphere, stratosphere, and mesosphere are the three regions in the homosphere. The homosphere is the lower part of Earth's atmosphere where gases are well mixed.
The homosphere is the lower part of the Earth's atmosphere where the composition of gases is relatively constant and well-mixed, extending up to about 80 km altitude. In contrast, the heterosphere is the upper part of the atmosphere where gases separate based on their molecular weight, with lighter gases like hydrogen and helium being found higher up.
The homosphere includes the troposphere, stratosphere, and mesosphere. These layers are where most weather events and atmospheric processes occur, and they are relatively well-mixed in terms of chemical composition.
The homosphere is the lower atmosphere where gases are well-mixed by turbulence and diffusion. It extends from the Earth's surface up to about 80-100 km in altitude, where the composition of gases like nitrogen, oxygen, and argon remains relatively uniform. This region also includes the troposphere and stratosphere.
The atmosphere above 80km (50 mi) and the homosphere where gases are stratified, with concentrations of the heavier gases decreasing more rapidly with altitude than concentrations of the lighter gases
The homosphere is the lower atmosphere, from the Earth's surface up to about 60 kilometers, where the composition of gases is relatively uniform and well mixed. This region includes the troposphere and the lower part of the stratosphere.
The region of the atmosphere that is evenly mixed and behaves as if it were a single gas is the homosphere. This layer extends from the Earth's surface up to about 80 kilometers in altitude and includes the troposphere and most of the stratosphere. In the homosphere, gases are well-mixed due to turbulence and convection processes.
Magnetosphere Ionoshpere Exosphere (upper and lower) Thermosphere Homosphere - Mesosphere - Stratosphere - Troposphere (high, low, medium, planetary boundary)
The lower 80 kilometers of the atmosphere where gases are found in uniform proportions is known as the homosphere. This region extends from the Earth's surface up to approximately 80 kilometers in altitude and includes the troposphere and the lower portion of the stratosphere. In the homosphere, gases such as nitrogen, oxygen, and other trace gases are well mixed due to the action of atmospheric circulation.
Nitrogen makes up about 78% of the Earth's atmosphere in the homosphere (the lower atmosphere where gases are well-mixed). This high concentration remains fairly constant throughout the homosphere.
In the troposphere and stratosphere, gases maintain an approximately uniform composition due to mixing processes like convection in the troposphere and slow diffusion in the stratosphere. The concentration of gases starts to vary noticeably in the mesosphere and thermosphere due to decreasing density and interactions with solar radiation.