Recent current measurements have shown that the subthermocline equatorial circulation in the central Pacific is considerably more complicated than had been thought. Below 1500 m depth on 159°W there are three currents south of the equator that appear to be permanent. Eastward currents are found at 1700 m and 3100 m, and a westward current is found at 4000 m. The 1700‐m current is at the southern edge of the 3°S to 3°N range of current measurements, so its meridional extent and its transport are unknown. The 3100‐m and 4000‐m currents have 16‐month mean transports of about 6 − 7 × 106m3s−1. All three of these currents may be important components of the general circulation.
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Eric Firing (1989) studied this question.
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