The coldest layer of the atmosphere is in the Mesosphere. This is because temperatures are decreasing as the Mesosphere extends upward above the Stratosphere. The air is thinner because the air particles are further apart. The next layer, known as the Thermosphere is the hottest layer. The reason why this layer is so hot, is because it contains fewer air molecules then the other layers, making the air very thin and easy to warm. The Thermosphere is closest to the sun and most sensitive to solar energy which is why it gets hot very quickly.
thermosphere
Mesosphere
thermosphere
there are 5 layers of the atmosphere :-troposphere ( our layer)-stratosphere ( the layer which contains the ozone layer)-mesosphere (the coldest layer)-thermosphere (the hottest layer)-exosphere ( the layer that leaves into space)
The middle layer of the atmosphere is called the stratosphere. It is located above the troposphere (the lowest layer) and below the mesosphere (the next layer up). In the stratosphere, the concentration of ozone helps to absorb and block a significant amount of the sun's harmful ultraviolet radiation.
thermosphere
Mesosphere
thermosphere
there are 5 layers of the atmosphere :-troposphere ( our layer)-stratosphere ( the layer which contains the ozone layer)-mesosphere (the coldest layer)-thermosphere (the hottest layer)-exosphere ( the layer that leaves into space)
After the troposphere, the next layer of the atmosphere with the highest temperatures is the stratosphere. In the stratosphere, temperatures increase with altitude due to the absorption of ultraviolet radiation by the ozone layer. This heating effect causes the stratosphere to be warmer at higher altitudes compared to the lower part of the layer.
The layer of atmosphere closest to the earth's surface is troposphere. The next layer is stratosphere which contains the ozone layer. After that comes the mesosphere, Ionosphere n exosphere.
The different layers of atmosphere, starting with the lowest layer in which most clouds appear, is the troposphere. The next layer is the stratosphere, which has the ozone layer at its upper limit about 50 km above sea level. The next layer is called the mesosphere, and above this is the ionosphere which extends to about 1,000 km. Next is the thermosphere and then the outside layer of atmosphere called the exosphere, which reaches a height of about 6,000 km above sea level..
The middle layer of the atmosphere is called the stratosphere. It is located above the troposphere (the lowest layer) and below the mesosphere (the next layer up). In the stratosphere, the concentration of ozone helps to absorb and block a significant amount of the sun's harmful ultraviolet radiation.
That's a very general question. In the broadest sense, Earth's atmosphere allows life to exist on the Earth. It's a mixture of approximately 78% Nitrogen, 21% Oxygen, and the remaining 1% of other gases (primarily argon). Oxygen, of course, is essential for animal life, and the carbon dioxide in the atmosphere allows for plant life. The atmosphere consists of 5 layers. The outermost layer, the Exosphere, is essentially space with some floating air molecules. The next innermost layer is the Thermosphere, and is, surprisingly, quite prone to extreme temperatures (temperatures are often much higher during daylight and colder during nighttime than Earth's surface at the same time). The next innermost layer is the Mesosphere, where the coldest temperatures on Earth may be found. Going inwards again, the next layer is the Stratosphere, which is particularly important because it contains the ozone layer, a layer of molecules (O3) which absorb harmful UV rays. Without the ozone layer, life could not exist in its present form. And finally we arrive at the Troposphere, which lies directly upon the Earth's surface. The air we breath is trapped in this layer, and much of our weather exists in this layer.
That's a very general question. In the broadest sense, Earth's atmosphere allows life to exist on the Earth. It's a mixture of approximately 78% Nitrogen, 21% Oxygen, and the remaining 1% of other gases (primarily argon). Oxygen, of course, is essential for animal life, and the carbon dioxide in the atmosphere allows for plant life. The atmosphere consists of 5 layers. The outermost layer, the Exosphere, is essentially space with some floating air molecules. The next innermost layer is the Thermosphere, and is, surprisingly, quite prone to extreme temperatures (temperatures are often much higher during daylight and colder during nighttime than Earth's surface at the same time). The next innermost layer is the Mesosphere, where the coldest temperatures on Earth may be found. Going inwards again, the next layer is the Stratosphere, which is particularly important because it contains the ozone layer, a layer of molecules (O3) which absorb harmful UV rays. Without the ozone layer, life could not exist in its present form. And finally we arrive at the Troposphere, which lies directly upon the Earth's surface. The air we breath is trapped in this layer, and much of our weather exists in this layer.
Venus is hottest. Next is Mercury.
the first layer is the surface layer it is nice and warm and mixed with the waves. the next layer is the thermocline it is just warm not any thing special. the next is freezing cold i would not want to go there.