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.
The troposphere can vary in thickness from about 8 km at the poles to 16 km at the equator. The mesosphere is typically around 50 km thick.
It Decreases by 6.5 degrees Celsius per KM. Most weather occurs here where we live. Convection Currents. At the surface it extends out 6-8 km at the poles and 17 km at the equator. Even though the temperature decreases by 6.5 degrees celsivus per KM, it stabilizes at 12 km
It is 87 km of altitude.
The troposphere is the layer of the atmosphere that extends to an average altitude of about 12 km. This is where most weather phenomena occur and where temperature generally decreases with increasing altitude.
The troposphere is the lowest layer of Earth's atmosphere where weather events occur. It extends from the Earth's surface up to about 10-15 km (6-9 miles) in altitude, depending on latitude. Within the troposphere, temperature generally decreases with altitude.
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 layer of the atmosphere that reaches the highest altitude is the exosphere. It extends from about 700 km (440 miles) above Earth's surface to 10,000 km (6,200 miles) or more. Within the exosphere, gases are very sparse, and particles can travel long distances without colliding with other particles.
The altitude range of the stratosphere is typically between 10 to 50 kilometers (6 to 31 miles) above the Earth's surface. However, the exact range can vary depending on factors such as latitude and season.
The atmosphere that is 10 km from Earth's surface is the upper part of the troposphere. This region is known as the tropopause, which is the boundary between the troposphere and the stratosphere. At this altitude, the temperature is typically much colder and atmospheric pressure decreases.
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 two lowest layers of the atmosphere are the troposphere and the stratosphere. The troposphere is where weather phenomena occur and contains most of the Earth's gases. The stratosphere is above the troposphere and contains the ozone layer, which helps protect us from the sun's harmful rays.
The lowest layer of the Earth's atmosphere is called the troposphere. This layer is where nearly all weather phenomena occur and it extends from the Earth's surface up to about 10-15 km (6-9 miles) in altitude.
32.8 ft
The thermosphere is the layer of the Earth's atmosphere that reaches the highest altitude. It extends from about 80 km (50 miles) to 550 km (340 miles) above the Earth's surface.