Vertical transport of pollutants by shallow cumuli from large eddy simulations

Different parameterization schemes for mi- crophysics, radiation transport, cumulus convection and the boundary layer are used to investigate their abilities in repro- ducing

of vertical transport by measuring u ∗ directly, and under katabatic conditions, estimate boundary layer depth (Ne ff et al., 2007) as well as giving wind speed, direction

In this work, we presented the modified cumulus convection parametrisation scheme, which computes the mass of air transported upward in a cumulus cell using conser- vation of

The blue shaded regions represent the physical transport by deep cumulus convection, the or- ange shading represents the balance between the component of mean large-scale

To estimate an absolute transport of SACW from the eddy generation area at the eastern boundary into the open ocean, the mean percentages of SACW contained inside the dif- ferent

Key words: Mixed convection, local similarity, variable viscosity, chemical reaction, thermal stratification, suction parameter, boundary layer, foreign mass, vertical

In the dataset used, no layer shaped structures were found, but as a solitary event, in the upper boundary of the PMSE a large deviation from the zenith in both meridional and

(c) uncertainty in the diurnal PBL height due to uncertainties in the parameterization of vertical transport and (d) the un- certainties in the driving of the atmospheric mixing by