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Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
SEPTEMBER 2010
During September 2010, 504 satellite-tracked surface drifting buoys,
79% with subsurface drogues attached for measuring mixed layer currents,
were reporting from the tropical Pacific. The westard NEC and SEC, and
eastward NECC, were all stronger than normal in September. Strong
equatorial anomalies persisted from previous months, but were not well
observed by the drifter array. Cold SST anomalies of -0.5 to -1.5C were
measured by most drifters east of the dateline from 20S to 20N, with very
cold anomalies of -1.5 to -3.0C common in the northeast corner of the domain.
In contrast, warm anomalies of +0.5 to +3.0C were measured by drifters in
the Kuroshio system.

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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