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Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
AUGUST 2007
During August 2007, 303 satellite-tracked surface drifting buoys, 71%
with subsurface drogues attached for measuring mixed layer currents,
were reporting from the tropical Pacific. The strongest current
anomalies were likely associated with the well-developed TIW train on
and north of the equator. Weaker, but basin-wide, westward anomalies of
10-20 cm/s were measured between 10-20S. In the northern tropical
Pacific, currents were near their climatological August strengths.
Drifters west of 160W measured slightly warm SST, with anomalies of
+0.5C to +1.5C common. East of 160W, SSTs were close to climatology
(apart from very cold anomalies measured by drifters at 130-140W, 4-6N,
associated with TIW advection of equatorial cold water).
FIGURE A1.1
a) Top: Movements of drifting buoys in the tropical Pacific Ocean.
The linear segments of each trajectory represent a one week displacement.
Trajectories of buoys which have lost their subsurface drogues are gray; those with
drogues are blue.
b) Middle: Monthly mean currents calculated from all buoys 1993-2002 (gray),
and currents measured by the drogued buoys this month (black) smoothed by an
optimal filter.
c) Bottom: Anomalies from the climatological monthly mean currents for this month.
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