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Exam (elaborations)

UMIAMI GSC 103 EXAM 3 WITH COMPLETE SOLUTIONS NEW UPDATE!!

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UMIAMI GSC 103 EXAM 3 WITH COMPLETE SOLUTIONS NEW UPDATE!!...

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UMIAMI GSC 103
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UMIAMI GSC 103 EXAM 3 WITH COMPLETE SOLUTIONS
NEW UPDATE!!


Photosynthesizers - ANSWER Earth didn't have oxygen until these came about



Composition of dry air today - ANSWER Mostly nitrogen and oxygen. Little carbon
dioxide and other gases



Troposphere - ANSWER gets colder as you go up



Stratosphere - ANSWER gets warmer as you go up



Mesosphere - ANSWER gets colder as you go up



Thermosphere - ANSWER gets warmer as you go up, BUT less density so it feels
freezing



lapse rate - ANSWER the rate at which temperature falls with increased altitude



Ozone (O3) - ANSWER stuff found in the ozone layer

formed by single atoms of oxygen bumping into O2

absorbs UV light and converts into heat



Relative humidity and temperature - ANSWER As temperature decreases, relative
humidity increases

, low pressure zone - ANSWER A region where relatively warm, lower density air is rising.



high pressure zone - ANSWER A region where relatively cool, dense air is sinking.



The Intertropical Convergence Zone - ANSWER a belt of low pressure which circles the
Earth in the tropical latitudes



Polar Cell - ANSWER Cells of air circulation occurring between 60 degrees north and
south and each pole.

Descending cold, dry air



Ferrel Cell - ANSWER Cell that moves air form 30 degrees to 60 degrees latitude

Rising moist Air



Hadley Cell - ANSWER a large-scale atmospheric convection cell in which warm moist
air rises at the equator and sinks cool dry air at medium latitudes, typically about 30°
north or south.



Coriolis effect - ANSWER Causes moving air and water to turn left in the southern
hemisphere and turn right in the northern hemisphere due to Earth's hemisphere.



downdraft - ANSWER cool air with rain descending out of storm



updraft - ANSWER warm moist air rising into storm



runoff - ANSWER water running across land



downcutting - ANSWER the process in which water flowing through a channel cuts into
the substrate and deepens the channel relative to its surroundings

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