Now showing items 1-4 of 4

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

      Jiménez Cortés, M. Antònia; Angevine, Wayne M.; Bazille, Eric; Couvreux, Fleur; Cuxart Rodamillans, Joan; Pino González, David; Sastre Marugas, Mariano (2014)
      Conference lecture
      Open Access
      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 ...
    • Evaluation of the diurnal cycle in the atmospheric boundary layer over land as represented by a variety of single-column models: the second GABLS experiment 

      de Bruijn, E.I.F.; Svensson, G.; Holtslag, A.A.M.; Kumar, V; Mauritsen, T.; Steeneveld, G-J.; Angevine, Wayne M.; Bazile, E.; Beljaars, A; Mailhot, J.; Lock, A.; Larson, V.E.; Kitagawa, H.; Freedman, F.; Falk, M.J.; Ek, M.; Cuxart, J.; Conangla Triviño, Laura; Cheng, A.; Masson, V.; Zampieri, M.; Söderberg, S.; Weng, W.; Park, S.; Pleim, J. (2011-08)
      Article
      Restricted access - publisher's policy
    • Land surface spinup for episodic modeling 

      Angevine, Wayne M.; Bazille, Eric; Legain, Dominique; Pino González, David (2014-08-14)
      Article
      Open Access
      Soil moisture strongly controls the surface fluxes in mesoscale numerical models, and thereby influences the boundary layer structure. Proper initialization of soil moisture is therefore critical for faithful simulations. ...
    • Studying the Boundary Layer Late Afternoon nd Sunset Turbulence (BLLAST) 

      Pino González, David; Lothon, Marie; Angevine, Wayne M.; Bange, Jens; Beare, R.J.; Beyrich, Frank; Canut, Guylaine; Couvreux, Fleur; Delbarre, Hervé; Gibert, Fabien; Jonker, Harm J. J.; Lenschow, Donald; Lohou, Fabienne; Mahrt, Larry; Pardyjak, Eric; Sorbjan, Zibgniew; Vilà-Guerau de Arellano, Jordi (2010)
      Conference lecture
      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 boundary ...