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This article is from the Encyclopedia of North Carolina edited by William S. Powell. Copyright © 2006 by the University of North Carolina Press. Used by permission of the publisher. For personal use and not for further distribution. Please submit permission requests for other use directly to the publisher.

Isothermal Belt

by Paul L. McCraw, 2006

The isothermal belt is a zone in western North Carolina, primarily in Rutherford and Polk Counties, in which temperature inversion resulting in milder temperature contributes to longer growing seasons than in the immediate surrounding region. The phenomenon usually occurs on the southern slopes of mountains and foothills protected from frost and freezing temperatures by higher mountains to the north and northwest. The temperature inversion, possible at any time, usually develops in the early spring. The condition is advantageous for tender plant life and early blooming trees as well as for the cultivation of fruit, especially apples and grapes.

In 1858 Silas McDowell of Franklin coined the name "isothermal belt" based on the concept of the isotherm, a line on a weather map linking all points that have an identical mean temperature for a given time. Since then the term has been widely used and modified by scientists and area residents to sometimes exaggerate the advantages of the area. The names of Thermal City in Rutherford County and Isothermal Community College, which serves Rutherford and Polk Counties, are derived from this term.


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