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Surfing On A Rocket (Edit), Surfing On A Rocket (Remixed By Zongamin), Surfing On A Rocket (Courtesy Dfa Records By Juan, Surfing On A Rocket (Tel Aviv Rocket Surfing Remak, Surfing On A Rocket (To The Smiling Sun Remix By J... ( 5 tracks)
Bird (Bird), La Puttana Di Closingtown (Prologo Per La Puttana, La Puttana Di Closingtown (Se Vuoi Capire La Loro, La Puttana Di Closingtown (Pat Cobhan Ride), La Puttana Di Closingtown (Fanny Scivola Con Le La... ( 19 tracks)
Don't Be Light - Edit, Don't Be Light - Mr Oizo Remix, How Does It Make You Feel? - Adrian Sherwood Versi, Don't Be Light - Neptunes Remix, People In The City - Modjo Version... ( 10 tracks)
Playground Love (Sung By Gordon Tracks), Bathroom Girl (Demo Version), Playground Love (Vibraphone Version), Playground Love (Nosferatu Remix By Flower Pistols, Highschool Prom (Playground Love - Rob Remix)... ( 5 tracks)
The temperature of the Earth's atmosphere varies with altitude; the mathematical relationship between temperature and altitude varies between the different atmospheric layers:
Pressure
Barometric Formula: (used for airplane flight) barometric formula
Main article: Atmospheric pressure
One mathematical model: NRLMSISE-00
Atmospheric pressure is a direct result of the weight of the air. This means that air pressure varies with location and time, because the amount (and weight) of air above the earth varies with location and time. Atmospheric pressure drops by ~50% at an altitude of about 5 km (equivalently, about 50% of the total atmospheric mass is within the lowest 5 km). The average atmospheric pressure, at sea level, is about 101.3 kilopascals (about 14.7 pounds per square inch).
Thickness of the atmosphere
Even at heights of 1000 km and above, the atmosphere is still present (as can be seen for example by the effects of atmospheric drag on satellites).
Composition
Heterosphere
Below the turbopause at an altitude of about 100 km, the Earth's atmosphere has a more-or-less uniform composition (apart from water vapor) as described above; this constitutes the homosphere.[1] However, above about 100 km, the Earth's atmosphere begins to have a composition which varies with altitude. This is essentially because, in the absence of mixing, the density of a gas falls off exponentially with increasing altitude, but at a rate which depends on the molar mass. Thus higher mass constituents, such as oxygen and nitrogen, fall off more quickly than lighter constituents such as helium, molecular hydrogen, and atomic hydrogen. Thus there is a layer, called the heterosphere, in which the earth's atmosphere has varying composition. As the altitude increases, the atmosphere is dominated successively by helium, molecular hydrogen, and atomic hydrogen. The precise altitude of the heterosphere and the layers it contains varies significantly with temperature.[2]
artists
Air DISCOGRAPHY
