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dc.contributor.authorLothon, Marie
dc.contributor.authorLohou, Fabienne
dc.contributor.authorPino González, David
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Física Aplicada
dc.identifier.citationLothon, M.; Lohou, F.; Pino, D. The BLLAST field experiment: boundary-layer late afternoon and sunset turbulence. "Atmospheric chemistry and physics", 16 Octubre 2014, vol. 14, p. 10931-10960.
dc.description.abstractDue to the major role of the sun in heating the earth’s surface, the atmospheric planetary boundary layer over land is inherently marked by a diurnal cycle. The after-noon transition, the period of the day that connects the day-time dry convective boundary layer to the night-time stable boundary layer, still has a number of unanswered scientific questions. This phase of the diurnal cycle is challenging from both modelling and observational perspectives: it is transitory, most of the forcings are small or null and the turbulence regime changes from fully convective, close to homogeneous and isotropic, toward a more heterogeneous and intermittent state
dc.format.extent30 p.
dc.rightsAttribution 3.0 Spain
dc.subjectÀrees temàtiques de la UPC::Física
dc.subject.lcshBoundary layer (Meteorology)
dc.titleThe BLLAST field experiment: boundary-layer late afternoon and sunset turbulence
dc.subject.lemacCapa límit (Meteorologia)
dc.contributor.groupUniversitat Politècnica de Catalunya. DF - Dinàmica No Lineal de Fluids
dc.rights.accessOpen Access
dc.description.versionPostprint (published version)
local.citation.authorLothon, M.; Lohou, F.; Pino, D.
local.citation.publicationNameAtmospheric chemistry and physics

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Attribution 3.0 Spain
Except where otherwise noted, content on this work is licensed under a Creative Commons license : Attribution 3.0 Spain