An intercomparison of mesoscale simulations during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) experimental field campaign

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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	Jiménez Cortés, M. Antònia
dc.contributor.author	Angevine, Wayne M.
dc.contributor.author	Bazille, Eric
dc.contributor.author	Couvreux, Fleur
dc.contributor.author	Cuxart Rodamillans, Joan
dc.contributor.author	Pino González, David
dc.contributor.author	Sastre Marugas, Mariano
dc.date	2014
dc.identifier.citation	Jiménez, M. [et al.]. An intercomparison of mesoscale simulations during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) experimental field campaign. A: European Geosciences Union General Assembly. "Geophysical Research Abstracts, vol. 16". Vienna: 2014.
dc.identifier.citation	1607-7962
dc.identifier.uri	http://hdl.handle.net/2117/27652
dc.language.iso	eng
dc.relation	http://meetingorganizer.copernicus.org/EGU2014/EGU2014-1629-1.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	Boundary layer
dc.subject	Capa límit (Meteorologia)
dc.title	An intercomparison of mesoscale simulations during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) experimental field campaign
dc.type	info:eu-repo/semantics/publishedVersion
dc.type	info:eu-repo/semantics/conferenceObject
dc.description.abstract	The Convective (diurnal, CBL) and Stably stratified (nocturnal, SBL) Boundary Layers over land have been extensively observed and relatively successfully modeled. But the early morning transition, when the CBL emerges from the nocturnal boundary layer, and the late afternoon transition, when the CBL decays to an intermittently turbulent residual layer overlying a SBL, are difficult to observe and model due to the intermittency and anisotropy of turbulence, horizontal heterogeneity and rapid changes in time
dc.description.abstract	Peer Reviewed

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