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dc.creatorNielsen-Gammon, John
dc.creatorKeyser, Daniel
dc.date.accessioned2016-10-28T18:55:54Z
dc.date.available2016-10-28T18:55:54Z
dc.date.issued2000-08-01
dc.identifier.citationNielsen-Gammon, J. W., and D. Keyser, 2000: Effective stratification for pseudoadiabatic ascent. Mon. Wea. Rev., 128, 3007-3010.en
dc.identifier.urihttps://hdl.handle.net/1969.1/158222
dc.description© Copyright 2000 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (https://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyrights@ametsoc.org.en
dc.description.abstractEffective stratification can be interpreted as the resistance to upward motion of saturated air parcels experiencing condensation. Previously published expressions for effective stratification conflict with each other, and the most widely distributed expression contains an O(1) error. A derivation of effective stratification is presented that exposes its physical interpretation and that reveals the origin of the flaw in the incorrect derivation.en
dc.description.sponsorshipNational Science Foundationen
dc.language.isoen_US
dc.publisherAmerican Meteorological Society
dc.subjectequivalent potential temperatureen
dc.titleEffective Stratification for Pseudoadiabatic Ascenten
dc.typeArticleen
local.departmentAtmospheric Sciencesen
dc.identifier.doi10.1175/1520-0493(2000)128<3007:ESFPA>2.0.CO;2


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