Tropical Pacific Drifting Buoys
Rick Lumpkin / Mayra Pazos, AOML, Miami
SEPTEMBER 2011
During September 2011, 354 satellite-tracked surface drifting buoys, 49% with
subssurface drogues attached for measuring mixed layer currents, were reporting
from the tropical Pacific. Few drifters measured near-equatorial currents in
the western half of the basin. Very strong northward anomalies measured by
three near-equatorial drifters at 129W are likely associated with a tropical
instability wave. Between 110W and the date line, strong equatorial westward
anomalies of O(50 cm/s) were measured by a number of drifters between the
equator and 5S. Most drifters between 10N and 10S measured SSTs cooler by 0.5
to 1.5C than the the climatological September value.
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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