Now showing items 1-7 of 7

  • Boundary Layer Late Afternoon and Sunset Turbulence: the BLLAST 2011 experiment 

    Pino González, David; Lothon, Marie; Lohou, Fabienne; Pardyjak, Erick; Reuder, Joaquim; Legain, Dominique; Durand, Pierre; Couvreux, Fleur; Vilà-Guerau de Arellano, Jordi (2012)
    Conference report
    Open Access
  • Evolution of the turbulence during the afternoon transition of the convective boundary layer: a spectral analysis 

    Darbieu, Clara; Lohou, Fabienne; Lothon, Marie; Couvreux, Fleur; Pino González, David; Durand, Pierre; Blay Carreras, Estel; Vilà Guerau de Arellano, Jordi (American Meteorological Society, 2014)
    Conference report
    Open Access
    The transition from a well-mixed convective boundary layer to a residual layer overlying a stabilized nocturnal layer raises several issues, which remain difficult to address from both modeling and observational perspectives. ...
  • Overview of the Chemistry-Aerosol Mediterranean Experiment/aerosol direct radiative forcing on the Mediterranean climate (ChArMEx/ADRIMED) summer 2013 campaign 

    Mallet, Marc; Dulac, F; Formenti, P; Nabat, Pierre; Sciare, J.; Roberts, Gareth E.; Pelon, Jacques; Ancellet, Gerard; Tanré, Didier; Parol, F; Dejean, C.; Brogniez, G.; di Sarra, G; Alados Arboledas, Lucas; Arndt, Dorthe; Auriol, F.; Blarel, L.; Bourrianne, T.; Chazette, P; Chevaillier, S.; Claeys, Maxim; D'Anna, B.; Derimian, Y.; Desboeufs, K.; Di Iorio, Tatiana; Doussin, J.F.; Durand, Pierre; Feron, A.; Franay, E.; Gaimoz, C.; Goloub, Philppe; Gomez Amo, J.L.; Granados Muñoz, María José; Sicard, Michaël (2016)
    Article
    Open Access
    The Chemistry-Aerosol Mediterranean Experiment (ChArMEx; http://charmex.lsce.ipsl.fr) is a collaborative research program federating international activities to investigate Mediterranean regional chemistry-climate interactions. ...
  • Studying the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) 

    Vilà-Guerau de Arellano, Jordi; Pino González, David; Pardyjak, Erick; Mahrt, Larry; Lohou, Fabienne; Jonker, Harm J. J.; Gioli, Beniamino; Gibert, Fabien; Durand, Pierre; Lothon, Marie; Lenschow, Donald; Angevine, Wayne; Bange, Jens; Beare, Robert; Canut, Guylaine; Couvreux, Fleur; Delbarre, Hervé (2010)
    Conference report
    Open Access
    At the end of the afternoon, when the surface heat fluxes start to sharply decrease, the CBL turns from a convective well-mixed layer to an intermittently turbulent residual layer overlying a stably-stratified ...
  • Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings 

    Pietersen, Henk; Vilà Guerau de Arellano, Jordi; Augustin, P; van de Boer, Anneke; de Coster, Olivier; Delbarre, Hervé; Durand, Pierre; Fourmentin, M; Gioli, Beniamino; Hartogensis, Oskar; Lohou, Fabienne; Lothon, Marie; Ouwersloot, Huug; Pino González, David; Reuder, Joachim (2015-04-24)
    Article
    Open Access
    We study the influence of the large-scale at- mospheric contribution to the dynamics of the convective boundary layer (CBL) in a situation observed during the Boundary Layer Late Afternoon and ...
  • The Boundary Layer Late Afternoon and Sunset Turbulence 2011 field experiment (BLT) 

    Lothon, Marie; Lohou, Fabienne; Durand, Pierre; Couvreux, Fleur; Hartogensis, Oskar; Legain, Dominique; Pardyjak, Erick; Pino González, David; Reuder, Joaquim; Vilà-Guerau de Arellano, Jordi (2012)
    Conference report
    Open Access
    Growth of the CBL over land in the middle of the day has been extensively observed and relatively successfully modeled. However the late afternoon transition (LAT), like the morning transition, is difficult to observe ...
  • Turbulence vertical structure of the boundary layer during the afternoon transition 

    Darbieu, Clara; Lohou, Fabienne; Lothon, Marie; Vilà Guerau de Arellano, Jordi; Couvreux, Fleur; Durand, Pierre; Pino González, David; Patton, Edward; Nilsson, Erik; Blay-Carreras, Estel; Gioli, Beniamino (2015-09-09)
    Article
    Open Access
    We investigate the decay of planetary boundary layer (PBL) turbulence in the afternoon, from the time the surface buoyancy flux starts to decrease until sunset. Dense observations of mean and turbulent parameters ...