Generally, the air pressure and density decreases with the increase in the height of the atmosphere. But, there are more complex equations at elevation with temperature and in some areas the temperature can be relatively stable or even increased, with increasing height. The general pattern of temperature and height is known by the constant and balloon sounding. This behavior of temperature distinguishes between the atmospheric layer Yayaei way to a second, five major stages of Earth's atmosphere (atmospheric stratification, it is called) is shared between the lowest levels yayasarbocca follows:
XMondal> 700 kilometers (> 440 miles)
Thoracic: 80 to 700 kilometers (50 to 440 miles) [7]
Mesomandal: 50 to 80 kilometers (31 to 50 miles)
Stratosphere: 12/15 to 50 kilometers (7/9 to 31 miles)
Troposphere: 0 to 12/15 kilometers (0 to 7/9 miles)
The exosphere is the most distant layer of Earth's atmosphere, starting from Exesbase, expanding over 700 kilometers, and about half the distance of the Moon distance from the sea level. It is mainly composed of hydrogen, helium and some heavy observations such as nitrogen, oxygen and carbon dioxide. These molecules and atoms It is so distant that it does not clash with each other as a result The gas behaves as Zone These particles thrown open whenever trajectories to follow the path of the object in the air Its so light These levels.
The thermal expansion increases with elevation of elevation of elevation of this level to about 80 kilometers (50 miles; 260,000 feet) and from the Mesobarite to the thermodynamics, which increases altitude with elevation of the level which enters the spine. Since the thermodynamic ecosystem is located below it is also known as exosbase. Its average height is about 700 kilometers from the Earth, but in reality the solar function The change varies from 500 to 1000 (310-620 mi; 1600000-3300000 ft) kilometers. This level of temperature is up to 1,500 ° C (2,700 ° F). International space station's orbit lies between 320 to 380 kilometers (200 and 240 miles) from this level. Polarity, which is known as the Aurora borealis in the northern hemisphere, and the Arora Australis (aurora australis) in the southern hemisphere, is sometimes seen in the thoracic and exosphere sections below.
The Mesomandal is spread from the stratovirus at 50 kilometers (160,000 feet 31 miles) above sea level, ranging from 80 to 85 (50-53 miles; 2,60000-280000 feet) kilometers from the stratosphere to the Mesopotamia. Lokpind generally ranges from 76 km to 100 km Mesomalas can be seen. The temperature decreases with the increase in height in the Mesomandum. The levels are so low that it is the coldest place in the world and the average temperature of the place is about -85 ° C (120 ° F, 190 K.), The temperature can be as high as -100 ° C (-150 ° F; 170 K) May be reduced. [10] Due to the cold temperature of this layer, the water vapor can be tied to the concrete bund.
Stratosphere zones begin to trumpet above 12/15 kilometers (7.5 / 9.3 miles, 39,000 / 49,104 feet) from Earth, from 50 to 55 (31-34 miles) 160,000-180,000 Feet). The atmospheric pressure at the top of the stratosphere is one in 1000 parts of the sea surface. This level of temperature with height due to increased ultraviolet radiation absorption by the ozone layer Transpiration temperature can be -60 ° C (-76 ° F; 210 Kelvin), much warmer than the stratosphere.
The troposphere starts from the surface and extends upto troporphism at about 12/15 kilometers, although this height varies due to the weather, which is approximately 9 kilometers (30,000 feet) in the pole and about 17 kilometers (56,000 feet) in the equator. The troposphere The most overheated is by the heat radiated by the surface of the earth, so the lowest part of the troposphere is warm and height enhancement Payamulata reducing the temperature of the cloud, including all weather conditions, such as trapomandala upadana contains about 80% of the atmosphere's mass. For trapobirati the border between the trapomandala and stratomandalera.
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