Freezing index

From Glossary of Meteorology
Revision as of 14:16, 20 February 2012 by imported>Perlwikibot
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)



freezing index

(Also called "coldness sun.") As used by the U. S. Army Corps of Engineers, the number of Fahrenheit degree-days (above and below 32°F) between the highest and lowest points on the cumulative degree-days time curve for one freezing season.

For a critical review of the topic see Sakari Tuhkanen (1980). "The freezing index is used as a measure of the combined duration and magnitude of below freezing temperatures occurring during any given freezing season. The index determined for air temperatures at 4.5 feet above the ground is commonly designated as the air freezing index, while that determined for temperatures immediately below a surface is known as the surface freezing-index." (from Glossary of Arctic and Subarctic Terms 1955).
Compare thawing index.

Tuhkanen, S. 1980. Climatic parameters and indices in plant geography. Acta phytogeographica Suecica. 67. Svenska Vaxgeografiska Sallekapet, Uppsala, . 105 pp.

Arctic, Desert, Tropic Information Center (ADTIC) Research Studies Institute 1955. Glossary of Arctic and Subarctic Terms. ADTIC Pub. A-105, Maxwell AFB, AL, . 90 pp.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.