Organised lines of convective clouds (cumuli), quite often in an otherwise lightly cloudy area (over land or sea). The appearance is
white in VIS-, grey in IR- and yellowish white to white in RGB124-image
Downwind the cumuli grow and sometimes reach the shower stage:
White parallel lines downwind disturbed by white bulges in the satellite images (IR, VIS and RGB124)
Weather Events
Relevant numerical parameters and their typical distribution
Surface wind speed
Wind direction in boundary layer
Temperature inversion height
Humidity in boundary layer
Stability in boundary layer
Physical Background
The physical processes are shown in schematic 1, the physical conditions are seen in schematic 2.
Presence of an temperature-inversion at height (H)
Convergence (C) at surface: rising air parcels;
Divergence (D): descending air.
Condensation just beneath inversion height
Wind profile in boundary layer as boundary condition
A typical cross section perpendicular on the cloud streets