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A possible influence of the density of ice accretions on their heat transfer coefficient

2005; Wiley; Volume: 131; Issue: 605 Linguagem: Inglês

10.1256/qj.03.211

1477-870X

Guillermo G. Aguirre Varela, Nesvit E. Castellano, Eldo E. Ávila,

Heat Transfer and Optimization

Quarterly Journal of the Royal Meteorological SocietyVolume 131, Issue 605 p. 377-379 Research Article A possible influence of the density of ice accretions on their heat transfer coefficient Guillermo G. Aguirre Varela, Guillermo G. Aguirre Varela Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Search for more papers by this authorNesvit E. Castellano, Nesvit E. Castellano Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Search for more papers by this authorEldo E. Avila Fa. M.A.F., Corresponding Author Eldo E. Avila Fa. M.A.F. [email protected] Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Universidad Nacional de Córdoba, Ciudad Universitaria, 5000 Córdoba, Argentina.Search for more papers by this author Guillermo G. Aguirre Varela, Guillermo G. Aguirre Varela Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Search for more papers by this authorNesvit E. Castellano, Nesvit E. Castellano Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Search for more papers by this authorEldo E. Avila Fa. M.A.F., Corresponding Author Eldo E. Avila Fa. M.A.F. [email protected] Facultad de Matemática Astronomía y Física, Universidad Nacional de Córdoba, Argentina Universidad Nacional de Córdoba, Ciudad Universitaria, 5000 Córdoba, Argentina.Search for more papers by this author First published: January 2005 Part A https://doi.org/10.1256/qj.03.211Citations: 2 Members of Consejo Nacional de Investigaciones Cientificas y Tecnologicas (CONICET). AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinkedInRedditWechat Abstract The heat transfer coefficient of ice accretions was reported by Avila and co-workers who found that it depends on the cloud droplet spectrum used for the accretion. In the present work, these data are re-examined and a new parametrization of the heat transfer coefficient is proposed as a function of accreted-ice density. Copyright © 2005 Royal Meteorological Society Citing Literature Volume131, Issue605January 2005 Part APages 377-379 RelatedInformation