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Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
DECEMBER 2007
During December 2007, 310 satellite-tracked surface drifting buoys, 80% with
subsurface drogues attached for measuring mixed layer currents, were reporting
from the tropical Pacific. Strong current anomalies were associated with
well-developed instability waves, particularly at 5N, 130-140W. Elsewhere,
currents exhibited uniformly westward anomalies (stronger NEC, SEC; weaker
NECC). These anomalies were ~10 cm/s across the basin. Cold anomalies of
-0.5 to -1.5 C were measured by most drifters east of 130W and south of the
equator, a persistent anomaly for the last three months, with larger anomalies
of -1.5C to -3.0C common east of 100W. Comparable cold anomalies were seen in
the northern TIW train, associated with advection of upwelled equatorial water.
Also seen since October, warm anomalies were common west of the dateline.

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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