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the stratosphere is in control of raising the altitude in the temperature. And is the secon layer of gas in the atmosphere.
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∙ 15y ago
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How long did it take to build the Las Vegas stratosphere?
how long did it take to buid the stratospher
A gas in the stratospher that helps to protect earth from ultraviolet radiation?
The gas is a miracle for earth. It is ozone.
Why are ozone layer locate in stratospher?
The ozone layer is in the stratosphere. It is because of the factors that create ozone.
How does the troposphere and stratospher protect us?
They contain the ozone gas. It protects us from the harmful UV rays of the sun.
How is stratospher ozone destroyed?
Stratospheric ozone is being destroyed regularly. It is by various ODS i.e. natural and man made.
What are the layers of the Earth's Atmosphere from the ground up?
The layers of the atmosphere are thetroposhphere where most of the weather occurs and this is the layer we live on. The stratospher is the layer that contains thes ozone and 19% of the gasses. The moseospher is the thirs layer and is the coldest plus meteors burn up in this layer. The thermospher is the 4th layer and the warmest. The exosphere is the outer most layer and is often called outerspace.
What is the same in every layer of the atmosphere?
# Thermosphere:The word thermosphere means "heat sphere," or "warm layer." The temperatur of the thermosphere may reach 2000 degrees C or more. # Mesosphere:The tempereature in the mesosphere drops to about -100 degrees C. # Stratosphere:The stratospher is still cold, but not so cold as the Mesosphere. Temperatures stay around -60 degrees C. # Troposphere:The tropospher is the layer in which we all live.
What happens to temperature as altitude increases in the stratosphere?
The temperature increasesThe 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.The word stratosphere is from the Greek meaning 'stratified layer' and sphaira meaning ball. The stratosphere is layered in temperature because it is heated from above by absorption of ultraviolet radiation from the Sun. Within this layer, temperature increases as altitude increases (see temperature inversion); the top of the stratosphere has a temperature of about 270 K (−3°C or 29.6°F), just slightly below the freezing point of water.[1] This top is called the stratopause, above which temperature again decreases with height. The vertical stratification, with warmer layers above and cooler layers below, makes the stratosphere dynamically stable: there is no regular convection and associated turbulence in this part of the atmosphere. The heating is caused by an ozone layer that absorbs solar ultraviolet radiation, heating the upper layers of the stratosphere. The base of the stratosphere occurs where heating by conduction from above and heating by convection from below (through the troposphere) balance out; hence, the stratosphere begins at lower altitudes near the poles due to the lower ground temperature.The major reason for the temperature increase with altitude is that most of the ozone (O3) is contained in the stratosphere. High energy ultraviolet light interacts with ozone to cause the temperature increase. Commercial airliners typically cruise at altitudes of 9-12 km in temperate latitudes, in the lower reaches of the stratosphere.[2] They do this to optimize jet engine fuel burn, mostly thanks to the low temperatures encountered near the tropopause. It also allows them to stay above any hard weather, and avoid atmospheric turbulence from the convection in the troposphere. Turbulence experienced in the cruise phase of flight is often caused by convective overshoot from the troposphere below. Although a few gliders have achieved great altitudes in the powerful thermals in thunderstorms, this is dangerous. Most high altitude flights by gliders use lee waves from mountain ranges and were used to set the current record of 15,447m (50,671 feet).Source(s):http://en.wikipedia.org/wiki/Stratospher…
