A NUMERICAL-MODEL OF THE CLOUD-TOPPED PLANETARY BOUNDARY-LAYER - RADIATION, TURBULENCE AND SPECTRAL MICROPHYSICS IN MARINE STRATUS

Citation
A. Bott et al., A NUMERICAL-MODEL OF THE CLOUD-TOPPED PLANETARY BOUNDARY-LAYER - RADIATION, TURBULENCE AND SPECTRAL MICROPHYSICS IN MARINE STRATUS, Quarterly Journal of the Royal Meteorological Society, 122(531), 1996, pp. 635-667
Citations number
43
Categorie Soggetti
Metereology & Atmospheric Sciences
ISSN journal
00359009
Volume
122
Issue
531
Year of publication
1996
Part
A
Pages
635 - 667
Database
ISI
SICI code
0035-9009(1996)122:531<635:ANOTCP>2.0.ZU;2-L
Abstract
A numerical model of the cloud-topped planetary boundary-layer is pres ented. The model is one-dimensional with special emphasis on a detaile d description of cloud microphysical processes. Aerosols and cloud dro plets are treated in a two-dimensional particle-distribution whereby t he activation of aerosols is calculated explicitly by solving the drop let-growth equation at all relative humidities. Atmospheric radiation is determined with a S-two-stream radiation scheme. Turbulent fluxes a re parametrized as a function of the turbulent kinetic energy. Numeric al results are presented which are obtained by utilizing measurements made over the North Sea. The interaction between radiation, turbulence and cloud processes for maintaining the quasi-steady state of stratif orm cloud fields is emphasized.