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The layers are to scale. From the Earth's surface to the top of the stratosphere (50km) is just under 1% of Earth's radius. The exosphere is a thin, atmosphere-like volume surrounding a planet or natural satellite where molecules are gravitationally bound to that body, but where the density is so low that the molecules are essentially collision ...
As a lower boundary for the exosphere this boundary is also called the exobase. [1] The exact altitude varies by the energy inputs of location, time of day, solar flux, season, etc. and can be between 500 and 1,000 kilometres (310 and 620 mi) high at a given place and time because of these. A portion of the magnetosphere dips below this layer ...
The layers of Earth's atmosphere with the Kármán line indicated (not to scale) [9] The FAI uses the term Kármán line to define the boundary between aeronautics and astronautics: [6] Aeronautics: For FAI purposes, aerial activity, including all air sports, within 100 km of Earth's surface.
The exosphere is the outermost layer of Earth's atmosphere (though it is so tenuous that some scientists consider it to be part of interplanetary space rather than part of the atmosphere). It extends from the thermopause (also known as the "exobase") at the top of the thermosphere to a poorly defined boundary with the solar wind and ...
Five distinct layers have been identified, the troposphere, stratosphere, mesosphere, thermosphere and exosphere. With solid data, scientists can better understand the extremely complex systems ...
In the exosphere, beginning at about 600 km (375 mi) above sea level, the atmosphere turns into space, although, by the judging criteria set for the definition of the Kármán line (100 km), most of the thermosphere is part of space. The border between the thermosphere and exosphere is known as the thermopause.
Exosphere – The outermost layer of an atmosphere; Exobase – The lower boundary of the exosphere; Thermopause – The upper boundary of the thermosphere; Thermosphere – The layer of the atmosphere above the mesosphere and below the exosphere; Mesopause – The temperature minimum at the boundary between the mesosphere and the thermosphere
As such, because the tropopause is an inversion layer in which air-temperature increases with altitude, the temperature of the tropopause remains constant. [2] The layer has the largest concentration of nitrogen. The atmosphere of the Earth is in five layers: (i) the exosphere at 600+ km; (ii) the thermosphere at 600 km;