To make sense of temperature and weather patterns over a large area,
meteorologists use the concepts of air masses and fronts. In this
module, we have defined the concepts and looked at fronts on current
surface maps to determine their relationship to temperature. When the
weather conditions are changing at a particular station because of
temperature advection, it is necessary to look elsewhere on the map
to forecast the weather. We identified two techniques. The first
involves estimating the wind speed and looking upstream to see what
the air which will be over our station tomorrow is doing today. The
second involves looking at current conditions at places with the same
relative position with respect to fronts and the pressure pattern as the
forecast city will have tomorrow. After considering changes in
temperature due to changing cloud cover, winds, or changes in elevation,
a reasonably accurate forecast can be made.
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Questions or Comments
Technical: E-mail John Fulton < jdfult@nimbus.met.tamu.edu >
Scientific: E-mail Dr. John Nielsen-Gammon. < nielsen@ariel.met.tamu.edu >
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Texas A&M Atmospheric Sciences Department and
Dr. John Nielsen-Gammon.
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