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Heat in the atmosphere is distributed in vertical mixing process by means of convection. It is also known as the process of vertical distribution.

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Why the atmosphere is thinner in the poles?

The atmosphere is thinner at the poles primarily due to the Earth's curvature and the angle of sunlight. At the poles, the sun's rays strike the surface at a more oblique angle, spreading energy over a larger area and resulting in lower temperatures. This leads to a denser air mass at lower latitudes, while the colder, denser air at the poles contributes to a more compact atmosphere. Additionally, the polar regions experience less convection and vertical mixing, further contributing to the thinner atmosphere.


What part of the atmosphere has no weather disturbance?

The stratosphere is the part of the atmosphere that typically experiences little to no weather disturbance. Unlike the troposphere, where most weather occurs due to convection and other atmospheric processes, the stratosphere is characterized by stable air and a lack of vertical mixing. This stability is largely due to the presence of the ozone layer, which absorbs ultraviolet radiation and causes temperature to increase with altitude.


How does oxygen move through the atmosphere?

Oxygen moves through the atmosphere primarily through two processes: diffusion and convection. Diffusion allows oxygen molecules to spread from areas of higher concentration to areas of lower concentration, ensuring even distribution. Convection, driven by temperature differences, facilitates the vertical movement of air, mixing oxygen throughout different layers of the atmosphere. Additionally, photosynthesis by plants continuously replenishes atmospheric oxygen, contributing to its movement and concentration in the air.


How does CO2 get into the upper atmosphere?

CO2 in the atmosphere exists throughout different layers, but it is mainly transported to the upper atmosphere through atmospheric circulation and mixing processes. Some CO2 molecules can also be carried to the upper atmosphere by volcanic eruptions or in the form of methane, which can be oxidized into CO2 at higher altitudes.


What are 3 characteristics of the stratosphere in the atmosphere?

The stratosphere is characterized by a relatively stable temperature that increases with altitude, primarily due to the absorption of ultraviolet radiation by the ozone layer. It extends from about 10 to 50 kilometers above Earth's surface and contains the ozone layer, which protects life by filtering harmful UV radiation. Additionally, the stratosphere has minimal vertical mixing, leading to less weather activity compared to the troposphere below it.

Related Questions

Heat in the atmosphere is distributed through a vertical mixing process called?

convection. Warm air rises from the surface, carrying heat energy upward and distributing it vertically through the atmosphere. This convection process helps regulate temperatures and circulate heat around the globe.


Which layer of the atmosphere is weather found in?

Weather is primarily found in the troposphere, which is the lowest layer of Earth's atmosphere. The troposphere is where most weather events, such as clouds, rain, snow, and storms, occur due to vertical mixing of air and moisture.


What does homoginise mean?

Homogenize means to make a substance uniform or consistent by mixing or blending it thoroughly. This process ensures that the components are evenly distributed throughout the mixture.


What is the purpose of the tropopause?

The tropopause acts as a boundary between the troposphere and the stratosphere. Its primary purpose is to inhibit the vertical mixing of air masses between these two atmospheric layers, which helps maintain stability in the Earth's atmosphere.


What is the processes involved in making buttermilk?

Cooking process mixing process baking process storing process mixing ingredient process etc..........


The Arctic Ocean is stratified and has limited vertical mixing of water because?

The Arctic Ocean is stratified and has limited vertical mixing of water because of its cold temperatures and the presence of a halocline, which is a layer with a sharp decrease in salinity. This halocline acts as a barrier to vertical mixing by preventing the movement of water between different layers.


What get inverted in a thermal inversion?

In a thermal inversion, the normal decrease in temperature with altitude is reversed, leading to warmer air above cooler air. This can trap pollutants and lead to poor air quality, as the inversion prevents vertical mixing of the atmosphere.


Is mixing salt and water?

Yes, mixing salt and water results in the salt dissolving in the water. This forms a homogeneous solution where the salt particles are evenly distributed throughout the water.


Is mixing iron and sulphur chemical or physical change?

A simple mixing is a physical process.


Is mixing iron and sulphur a chemical or physical change?

A simple mixing is a physical process.


What is the process of mixing colors called?

The process of mixing colors is called color blending or color mixing. This involves combining different hues to create new colors by mixing varying amounts of each pigment. This process is fundamental in art and design to achieve desired color tones and shades.


What has the author William Seth Spitzer written?

William Seth Spitzer has written: 'Rates of vertical mixing, gas exchange, and new production' -- subject(s): Oceanic mixing