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The troposphere ends at 16 km above the earths surface and ranges from 20 to -60 *C
The International Space Station's altitude varies from 199 miles to 215 miles or 319.6 km to 346.9 km above the Earth's surface.
It is 87 km of altitude.
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.
The troposphere, which is the lowest layer of the atmosphere, extends from the surface of the Earth up to a height that varies between about 9 km (or 30,000 ft) at the poles and 17 km (or 56,000 ft) at the equator.
Troposphere
The troposphere ends at 16 km above the earths surface and ranges from 20 to -60 *C
The stratosphere is between the troposphere and the mesosphere and has an altitude starting around 30 km.
The TROPOSPHERE (up to 10 km altitude, where we live) and the STRATOSPHERE (10 to 50 km altitude, where jet aircraft fly).
The stratosphere is normally considered to extend from about 11 km to 50 km above the earth's surface (7 - 31 miles).
The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at moderate latitudes, while at the poles it starts at about 8 km (5 miles) altitude.--Wikipedia
The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at mid-latitudes, while at the poles it starts at about 8 km (5 miles) altitude.
1. Weather occurs in the troposphere. 2. The depth of the troposphere varies from 16 km to 9 km.
The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at mid-latitudes, while at the poles it starts at about 8 km (5 miles) altitude
It is approximately 5 1/2 miles (29000 ft or 9 km) thick
The layer above the troposphere, and below the mesosphere. Near the equator, this places the stratosphere between 10 and 50 km in altitude. It is lower at the poles.
- The lowest layer (about 15 km from the ground) - Contains normal air composed of N2, O2, water vapour, CO2, etc. - Temperature decreases with altitude