chapter 3 Flashcards
what does atmosphere do
protect us from hostile radiation and particles from the sun and beyond
components of air
a simple misture of gases N2 (78%), O2 (21%), others (1%), and water vapor H2O (0 to 4%), CO2 (0.0035%) that is naturally odourless colourless, tasteless, and formless, blended so thoroughly that it behaves as if it were a single gas
how big is the atmosphere
480 km above Earth’s surface
exosphere
outer sphere
, lightweight hydrogen and helium atoms with some oxygen atoms and nitrogen molecules, weakly bound by gravity as far as 32 000 km from earth, beyond the thermopause
Air pressure
pressure produced by the motion, size, and number of gas molecules in the aire and exerted on surfaces in contact with the air
why is the air denser near Earth’s surface
because gravity compress the air downward
what percentage of the atmosphere remains above an altitude of 50 km
only 0,1%
Heterosphere
80 to 480 km altitude, a zone of the atmosphere above the mesopause, includes the ionosphere, less than 0,001% of the atmospheres mass, because of gravity the gases or not uniform, hydrogen and helium at the top, and oxygen and nitrogen at the bottom
Homosphere
earths surface to 80 km altitude, composed of an even mixture of gases, nitrogen, oxygen, argon, carbon dioxide, and trace gases, ozone layer from 19 to 50 km above sea level
Nitrogen
78% percentage by volume, unreactive and unavailable, originating principally from volcanic sources, integrated into our bodies through compounds in food ,sinks; nitrogen fixation, lightning
Oxygen
21%, reacts via oxidation, by-product of photosynthesis, one-fifth of the atmosphere, forms compounds that compose about half of earths crust, sinks; weathering, combustion, aerobic decomposition
Carbon dioxide CO2
natural by-product of life processes, cellular respiration, wildfires, combustion of fossil fuels, small percentage in atmosphere, the CO2 percentage has increased as a result of human activities, principally the burning of fossil fuels and deforestation, greenhouse gas, sinks; photosynthesis, dissolution in oceans
Argon
comes from slow accumulation over millions of years, less than 1% of the homosphere
Methane
0,00018% second greenhouse gas, human activity
Temperature
measure of the average kinetic energy of individual molecules
Heat
is the flow of kinetic energy from one body to another resulting from a temperature difference between them, depends on density or mass of a substance; where little density or mass exists, the amount of heat will be small
why is the temperature high in the atmosphere but not hot
because the density is low, it will feel cold because the number of molecule is not great enough to transfer heat to our skin