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solely caused by rain-induced effects up to wind speeds of 8 m s
-1
. As al-
ready pointed out by Braun et al. (2002) these effects may comprise stalks
and cavities, or secondary drops.
Fig. 6.
Same as Figure 5, but for cross polarisation (HV)
Finally, the wind-dependence of the backscattered radar power (
ı
rel
) has
been studied under different conditions. The results are shown in Figure 7,
where the stars denote
ı
rel
values measured at a slick-free water surface
and with rain, the circles denote
ı
rel
values measured at a slick-covered wa-
ter surface and with rain, the crosses denote
ı
rel
values measured at a slick-
