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There are five layers in the atomosphere. The troposhere, the stratoshere, the mesoshere, the thermoshere and the exosphere. There is also the ionosphere which is within the thermosphere and is noted for its chemistry.
Just a guess but maybe the exosphere!! But also it could be the Thermosphere, which is the Ionosphere and Exosphere combined.
the ionosphere extends from around 50 km altitude to about 1000 km, Within this range are the the various regions that make it up; D, E, F1, F2 and the topside, with the D region closest to us and the topside farthest from us, and in that order. the topside can also extend to about 2000km in some part of the earth.
No. Earth's core temperature is determined by processes within the Earth.
Temperature change within the months
There are five layers in the atomosphere. The troposhere, the stratoshere, the mesoshere, the thermoshere and the exosphere. There is also the ionosphere which is within the thermosphere and is noted for its chemistry.
ionosphere
Stratification means there are multiple distinct layers within the same region. The stratosphere is stratified by temperature, so there are layers within the stratosphere of distinctly difference temperature.
The Ionosphere!
The Ionosphere!
the layers of the atmosphere in order are troposphere, stratosphere, mesosphere, thermosphere, and exosphere
The thremosphere is the layer of the atmosphere that has two layers within it. The Thermosphere is the layer farthest from Earth's surface. The first layer of the thermosphere is the Ionosphere, and the second layer of the thermosphere is the exosphere
From the Earth outward the layers of the atmosphere are; Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere. These layers are divided by whether the temperature increases or deceases with an increase in altitude within the layer.
In a fusion reactor the hot gases or plasma are contained within a magnetic field.
Chromatin material is contained within the nucleus.
It has DNA that is not contained within the nucleus.
The characteristic is temperature. While pressure diminishes with increasing altitude, it is dependent on the underlying air masses. Temperature changes vary consistently within each of the major layers (troposphere, stratosphere, mesosphere, thermosphere, exosphere).