Session 2 |
| | Cloudy Boundary Layers 1 |
| | Chair: David A. R. Kristovich, ISWS, Champaign, IL
|
| 8:00 AM | 2.1 | Influence of convective clouds on the turbulence structure of the boundary layer measured by Doppler Lidar
Andreas Wieser, Institut für Meteorologie und Klimaforschung Forschungszentrum Karlsruhe / Universitaet Karlsruhe, Eggenstein-Leopoldshafen, Germany; and R. Huckle, N. Kalthoff, and U. Corsmeier |
| 8:15 AM | 2.2 | The diurnal cycle of the summer cloud-capped Arctic boundary layer  
Michael Tjernström, CIRES/Univ. of Colorado, Boulder, CO |
| 8:30 AM | 2.3 | A simple parameterization for detrainment in shallow cumulus
Wim C. De Rooy, Royal Netherlands Meteorological Institute (KNMI), De Bilt, Utrecht, Netherlands; and A. P. Siebesma |
| 8:45 AM | 2.4 | The influence of the sub-cloud moisture field on cloud size distributions and the consequences for entrainment
Harm J.J. Jonker, Delft University of Technology, Delft, Netherlands; and R. A. Verzijlbergh, T. Heus, and A. P. Siebesma |
| 9:00 AM | 2.5 | Large-eddy simulation of evaporatively driven entrainment in cloud-topped mixed layers
Takanobu Yamaguchi, Colorado State Univ., Fort Collins, CO; and D. A. Randall |
| 9:15 AM | 2.6 | Entrainment rate and droplet sedimentation in stratocumulus-capped mixed layers
Christopher S. Bretherton, University of Washington, Seattle, WA; and P. N. Blossey and J. Uchida |
| 9:30 AM | 2.7 | Entrainment and the fine structure of the stratocumulus cloud top
Qing Wang, Naval Postgraduate School, Monterey, CA; and M. S. Horner, S. Wang, and J. Kalogiros |
| 9:45 AM | 2.8 | Why do descending Shells around Cumulus Clouds exist?
Thijs Heus, Delft University of Technology, Delft, Netherlands; and H. J. J. Jonker |