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(a)
(b)
Fig. 5 Monthly average surface circulation from altimetry data (1993-2011) during (a) April
and (b) August
Snidvongs ( 1999 ). Two anti-cyclonic eddies have formed in the south and
southeast of Natuna Island centred at (3 N, 108E) and (2.5N, 109E), respec-
tively. Meanwhile, two cyclonic eddies are observed near the Sarawak coastal area
and northeast of Natuna Island centred at (3N, 111E) and (6N, 110E),
respectively.
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