Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
NOVEMBER 2011
During November 2011, 331 satellite-tracked surface drifting buoys, 56% with
subsurface drogues attached for measuring mixed layer currents, were reporting
from the tropical Pacific. Across the basin, drifters in the South Equatorial
Current measured westward anomalies of O(20 cm/s) at 15-20S. Four drifters
immediately north of the equator measured strong westward anomalies between
180-160W, but the robustness of this is difficult to determine from drifters
alone due to the small sample size. Elsewhere, currents were near their
climatological November values. Many drifters north of 10N and west of 160W
measured SSTs warmer than normal by 0.5-3.0C, while drifters to the south and
east measured SSTs at or slightly cooler (0-1.5C) than climatological November
values.

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 1993-2010 (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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