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Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
MARCH 2009
During March 2009, 352 satellite-tracked surface drifting buoys, 83% with
subsurface drogues attached for measuring mixed layer currents, were
reporting from the tropical Pacific. Across the basin, the westward SEC
was stronger by 5-20 cm/s than its climatological February strength, with
the strongest anomalies at 20S. Strong eastward anomalies in the NECC and
at 110-120W, 5S may have been associated with advection by instability waves.
Between 10N and 20S, most SSTs were close to climatological March values.
Many drifters north of 10N and west of 130W measured anomalously cold
(-0.5 to -1.5C) SSTs. South of 20S, warm anomalies of +0.5 to +3.0C wer
measured across the basin.
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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