Cold low

From Glossary of Meteorology



cold low

(Or cold cyclone;
also called cold-core low, cold-core cyclone.) At a given level in the atmosphere, any low that is generally characterized by colder air near its center than around its periphery; the opposite of a warm low.

A significant case of a cold low is that of a cut-off low, characterized by a completely isolated pool of cold air within its vortex. The cyclonic intensity of a cold low increases with height in accordance with the thermal wind equation.


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.