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Air Pressure and Air Masses

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Air pressure is one factor that plays a role in the weather.  The atoms and molecules in the atmosphere are constantly moving around.  When more molecules go to one area the number of strikes per unit of time and area also increases.  This air pressure can be exerted in all directions.  The higher the elevation, the less air pressure there is.  Warm air is far less dense than cold air.
 
The unit for air pressure is the Pascal (Pa), named after Blaise Pascal, has been used by Meteorologists since 1929.  One pascal equals .01 millibar.  The two most common units are "Inches of Mercury" and "Millibars".  The standard air pressure is 29.92 in inches of Mercury and 1013.2 in millibars.  Weather maps show the highest air pressure by the blue H's and the lowest by the red L's.
 
When the barometer falls in hot weather it stands for thunder or high wind, in cold it means thaw, in wet weather expect a lot more, and in fair expect a lot of rain and wind in a couple days.  The barometer always falls the lowest for wind and rain together.
 
When it rises in winter it means frost is coming, in frost it means snow, if fair happens right after it rises, expect it to last for a short time.  When it rises very high in wet weather, and remains, fair weather will come in a couple days, but if it suddenly jumps the fair weather won't last very long.  The barometer rises highest for north and east winds.
 
When there is unsteady pressure expect unsteady weather.  When it motions upwards there's good weather coming, but if it lowers storms are approaching.
 
In general, high pressure is good and low pressure is bad.
 

warmandcoldfronts.jpg
http://images.google.com/images?hl=en&q=cold+and+warm+fronts&btnG=Search+Images&gbv=2

Fronts

When two air masses hit one is forced to go up and one is forced down.  A warm front is a more smooth slide over each other and makes calm weather.  A cold front is steep and forces air up which creates a thin line of storms called "Squall Lines".

Fronts are detectable on earth's surface by a change in winds (where they converge), change in temperature, and change in air pressure.

http://www.srh.weather.gov/jetstream/synoptic/airmass.htm