Ocean mesoscale phenomena such as eddies and current convergence zones
can often be seen in synthetic aperture radar (SAR) images due to cha
racteristic patterns caused by natural film induced damping of the wav
es. Such films have also been found to exert a significant effect on a
ir-sea gas exchange, which may be important for the global scale clima
te system. Satellite SAR may prove very useful to quantify the extent
of natural film. To investigate the composition of these films and the
ir effect on radar return, we compared samples of the sea surface with
ERS 1/2 SXR images of coastal ocean areas during the COASTWATCH'95 ex
periment, Simultaneous observations were made with a shipmounted C ban
d dual-polarized Doppler radar, and surface drifters were deployed to
investigate the surface current variations in the vicinity of differen
t slicks (areas where the short surface waves sensed by a radar are da
mped). One confirmed case of natural film was thus verified to be caus
ed by a convergence zone. The study also showed that the films investi
gated during COASTWATCH'95 were generally less concentrated and origin
ated from marine organisms, compared to the films with terrestrial inf
luences found in a previous experiment in a fjord [Espedal et al,, 199
6]. The dependence of the existence of the films on wind speed is also
investigated, and an estimate of natural film distribution during the
experiment period is given? using a total of 71 ERS 1/2 SAR images co
llected over the same coastal area under a variety of wind conditions.
Up to 40% natural film coverage was found for 2.5 m/s wind speeds, wh
ile already at 5-10 m/s all SAR imagery had under 5% film coverage.