Gs. Young et al., APPLICATION OF OVER-THE-HORIZON RADAR OBSERVATIONS TO SYNOPTIC AND MESOANALYSIS OVER THE ATLANTIC, Weather and forecasting, 12(1), 1997, pp. 44-55
Over-the-horizon (OTH) radar observations of surface wind direction of
fer a high-resolution (15 km) resource for synoptic and mesoscale wind
field analysis. With horizontal resolution at the lower end of the me
soscale and areal coverage in the synoptic scale, OTH radar has the po
tential to contribute significantly to the amelioration of the data sp
arseness that has long plagued over-ocean surface analysis. Because of
a twofold ambiguity in the OTH radar algorithm for determining surfac
e wind direction, however, mapping surface wind directions unambiguous
ly would normally require two radars with overlapping coverage. Altern
atively, the single-radar ambiguity can be resolved by combining NWP m
odel analyses and incidental surface wind observations with meteorolog
ical insight. An approach to the latter, less expensive solution is pr
esented that relies on the classic principles of streamline analysis a
nd an easy-to-use graphical wind field editor developed specifically f
or this task. A case study demonstrates the utility of the resulting O
TH radar analyses of surface wind direction over the tropical Atlantic
Ocean. Existing military OTH radars in several countries could be use
d for such monitoring with little impact on their primary mission.