Search results
Results from the WOW.Com Content Network
The temperature of the thermopause could range from nearly absolute zero to 987.547 °C (1,810 °F). Below this, the atmosphere is defined to be active [clarification needed] on the insolation received, due to the increased presence of heavier gases such as monatomic oxygen. The solar constant is thus expressed at
The border between the thermosphere and exosphere is known as the thermopause. The highly attenuated gas in this layer can reach 2,500 °C (4,530 °F). Despite the high temperature, an observer or object will experience low temperatures in the thermosphere, because the extremely low density of the gas (practically a hard vacuum ) is ...
The height of the thermopause varies considerably due to changes in solar activity. [22] Because the thermopause lies at the lower boundary of the exosphere, it is also referred to as the exobase. The lower part of the thermosphere, from 80 to 550 kilometres (50 to 342 mi) above Earth's surface, contains the ionosphere.
Within the mesosphere, temperature decreases with increasing height.This is a result of decreasing absorption of solar radiation by the rarefied atmosphere having a diminishing relative ozone concentration as altitude increases (ozone being the main absorber in the UV wavelengths that survived absorption by the thermosphere). [7]
AOL fonctionne mieux avec les dernières versions des navigateurs. Vous utilisez un navigateur obsolète ou non pris en charge, et certaines fonctionnalités de AOL risquent de ne pas fonctionner correctement. Mettez à jour la version de votre navigateur dès maintenant. Plus d’infos
U.S. stocks ripped higher and carried the S&P 500 to records as the economy kept growing and the Federal Reserve began cutting interest rates. The year featured many familiar winners, such as Big ...
Bob Uecker delivered a virtuoso performance as baseball announcer Harry Doyle in the 'Major League' movies. Check out these hilarious clips.
The atmosphere of planet Earth: The tropopause is between the troposphere and the stratosphere. Rising from the planetary surface of the Earth, the tropopause is the atmospheric level where the air ceases to become cool with increased altitude and becomes dry, devoid of water vapor.