Atmosphere and Ocean



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Rayleigh scattering

Atmosphere and Ocean - 2


Nitrogen cycle Yeah!


nitrogen - 78% of the atmosphere; inert gas; dilutes oxygen; mostly useless for animals in its pure form; bacteria “fix” nitrogen and turn it into nitrates and nitrites which are used by plants and animals to make proteins and DNA


8% at 8 min = fatal;

24% max for no effect
oxygen - 20% of the atmosphere; used by plants and animals for respiration - breathing and making food; includes ozone - a poisonous bluish form of oxygen with a strong odor; when ozone is produced on the ground from cars and factories, it is harmful and forms smog; from the middle to the top of the stratosphere is the ozone layer; the ozone layer acts like a shield that absorbs the sun’s ultraviolet (UV) energy which is destructive to life and causes cancer.

water vapor - varies between 1 to 4% of the atmosphere; heavy greenhouse gas; absorbs heat


carbon cycle Yeah!
argon - 1% of the atmosphere; inert gas (does not combine with anything); used in welding

carbon dioxide CO2 - 0.04% of the atmosphere; produced when materials burn (combustion) and when humans and animals breathe out (respiration); heavy greenhouse gas; absorbs heat


trace = small amount
methane, hydrogen, CFC’s - trace greenhouse gases, less than 1 % of the atmosphere

helium, neon, krypton, xenon, radon - other inert trace gases, less than 1 % of the atmosphere




Inert means that it will not chemically react with anything, won’t stick to anything
Radon: dolomite sedimentary rock – crushing the rock is a physical change not a chemical change


Atmosphere and Ocean - 3

The atmosphere has five main layers which are identified mainly by their:

change in temperature – main way we tell them apart


If heavy gases sink, what do light gases do?

pressure/density – how heavy are the gasses

content – what types of gasses




The atmosphere extends out about 41,000 miles from earth’s surface to outer space, but most of the air is concentrated into the bottom two layers (troposphere and stratosphere - 0 to 30 miles above the ground) due to gravity. The layers beginning from the surface are:


these two are the lower atmosphere


these two are the upper atmosphere

troposphere, stratosphere

mesosphere, thermosphere




thermosphere:

ionosphere = lower thermosphere; exosphere = upper thermosphere





Heavier gases separate from lighter ones and are near the surface. Different gases absorb different amounts and types of solar energy. This is why the temperatures change through the layers. From the ground, the temperature first decreases, then increases, then decreases, then increases, then decreases to outer space. Each layer has a top part, called a pause, where the temperature stays the same for a distance.

Atmosphere and Ocean - 4



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