A question about atmosphere layers

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These are known as "pauses" and act as separators between the layers of the atmosphere. They mark the areas where different processes take place and act as a transition from one layer to another. Therefore, they are not considered as distinct and additional layers in the classification system.
  • #1
termina
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Hello there!
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Layers of our atmosphere are said to be counted according to their temperature,
then why don't scientists include the places where temperature is stable with altitude (as shown in the picture) as distinct and additionnal atmospheric layers?Thank you
 
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  • #2
Those altitudes in the picture are only guidelines. It varies from the poles to the equator.

Have you not considered that those stable areas are actually the boundary markers, distinguishing between the levels?
 
  • #3
termina said:
Hello there!

Layers of our atmosphere are said to be counted according to their temperature,
then why don't scientists include the places where temperature is stable with altitude (as shown in the picture) as distinct and additionnal atmospheric layers?

Thank you

I believe that they do.
There called tropopause, stratopause and mesopause.
Although these are more separators between the layers.

I would assume this is because in the different layers different processes take place and the "pauses" only mark the area where one process shifts into another process, which looks like a stable area, but basically is only a transition from one layer to another.
 
  • #4
I like Serena said:
I believe that they do.
There called tropopause, stratopause and mesopause.

Correct.
 
  • #5
for your question. The layers of our atmosphere are indeed primarily classified based on temperature, as this is a major factor that affects the behavior and characteristics of each layer. However, it is important to note that there are other factors that also contribute to the formation and classification of atmospheric layers, such as air pressure, density, and composition.

The stable temperature zones shown in the picture may not be considered distinct atmospheric layers because they do not have significant differences in these other factors compared to the surrounding layers. They are often referred to as transition zones or boundary regions, where the characteristics of two adjacent layers overlap.

Additionally, the boundaries between atmospheric layers are not always clearly defined and can vary depending on location, time of day, and weather conditions. Therefore, while the temperature may be stable in these transition zones, other factors may still be changing and influencing the behavior of the atmosphere.

I hope this helps to clarify the classification of atmospheric layers and the role of stable temperature zones within them. Thank you for your interest in the science of our atmosphere.
 

FAQ: A question about atmosphere layers

What are the different layers of Earth's atmosphere?

There are five main layers of Earth's atmosphere: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.

What is the difference between each layer of the atmosphere?

The main differences between each layer of the atmosphere are their temperature, pressure, and composition. The temperature generally decreases with height in the troposphere, but increases with height in the stratosphere and thermosphere. The pressure also decreases with height, while the composition of gases varies in each layer.

How does the atmosphere protect us from harmful radiation?

The Earth's atmosphere contains ozone in the stratosphere, which absorbs harmful ultraviolet radiation from the sun. It also contains other gases that absorb or reflect harmful radiation, providing a protective layer for life on Earth.

What is the role of the mesosphere in the atmosphere?

The mesosphere is the third layer of the atmosphere and is responsible for burning up most of the meteors entering Earth's atmosphere. It also helps to regulate the temperature of the thermosphere above it.

How does the atmosphere affect weather and climate?

The atmosphere plays a crucial role in weather and climate by regulating the amount of heat and energy that is absorbed and reflected by the Earth. It also helps to distribute heat and moisture around the globe, influencing weather patterns and climate zones.

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