Evolution of the Thorpe and Ozmidov scales at the lower atmospheric and planetary boundary layer

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dc.contributor	Universitat Politècnica de Catalunya. Departament de Física Aplicada
dc.contributor	Universitat Politècnica de Catalunya. DF - Dinàmica No Lineal de Fluids
dc.contributor.author	Lopez Gonzalez-Nieto, Pilar
dc.contributor.author	Cano Marchante, Jose Leandro
dc.contributor.author	Redondo Apraiz, José Manuel
dc.date	2010
dc.identifier.citation	Lopez, P.; Cano, J.; Redondo, J. Evolution of the Thorpe and Ozmidov scales at the lower atmospheric and planetary boundary layer. A: Summer School and Workshop on Environmental Turbulence. "SSWET". Madrid: Universidad Complutense de Madrid (UCM), 2010, p. 1-18.
dc.identifier.uri	http://hdl.handle.net/2117/15343
dc.language.iso	eng
dc.publisher	Universidad Complutense de Madrid (UCM)
dc.relation	http://www.ucm.es/info/fluidos/MADRID/POSTER_ARTICLE_LOPEZ_CANO_REDONDO.pdf
dc.rights	Attribution-NonCommercial-NoDerivs 3.0 Spain
dc.rights	info:eu-repo/semantics/openAccess
dc.rights	http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject	Àrees temàtiques de la UPC::Física
dc.subject	Boundary layer (Meteorology)
dc.subject	Capa límit atmosfèrica
dc.title	Evolution of the Thorpe and Ozmidov scales at the lower atmospheric and planetary boundary layer
dc.type	info:eu-repo/semantics/submittedVersion
dc.type	info:eu-repo/semantics/conferenceObject
dc.description.abstract	Turbulence affects the dynamics of atmospheric processes by enhancing the transport of mass, heat, humidity and pollutants. The global objective of our work is to analyze some turbulent descriptors which reflect the mixing processes in the atmospheric boundary layer (ABL). In this paper we present results related to the Thorpe displacements dT, the maximum Thorpe displacement (dT)max, the Thorpe scale LT and the Ozmidov scale, LO, and their time evolution in the ABL during a day cycle. A tethered balloon was used to obtain vertical profiles of the atmospheric physical magnitudes up to 1000 m. We discuss their vertical and time variability, and also their relationships.

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