The present paper deals with the adaptation of the Multiple Analytical Dopp
ler (MANDOP) analysis to Doppler radar observations over complex orography.
The objective, in the context of the Mesoscale Alpine Programme (MAP), is
to design a reliable and flexible tool able to process any kind of radar da
ta (airborne/ground based) in order to retrieve mesoscale three-dimensional
wind fields over complex terrain with a convective-scale resolution. The v
arious effects of the orography on the wind field (slope winds) and on the
radar sampling (ground clutter, shadowing effect) are considered and taken
into account in each step of the wind synthesis. In addition to these speci
fic aspects, some numerical improvements are presented that make the method
quicker and more objective. The method is validated with quasi-real simula
ted data, and three different boundary conditions are compared (bottom, top
, and both). The analysis is eventually applied to real data gathered durin
g IOP2b of the MAP special observing period (SOP) by the C-band Ronsard and
Monte Lema Doppler radars, allowing interpretation of the reflectivity and
velocity patterns in close correlation with the orography.