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
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.