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The Columbia Encyclopedia, Sixth Edition.  2001-07.
 
isotherm
 
 
line drawn on a map of a particular region of the earth’s surface connecting points of equal temperature; each point reflects one temperature reading or an average of several readings over a period of time. The relative spacing of the isothermal lines indicates a temperature gradient, i.e., the amount of temperature change over a given distance.
 
 
The Columbia Encyclopedia, Sixth Edition. Copyright © 2007 Columbia University Press.

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