The mean structure and variability of the currents east of Mindanao are investigated through 2 year mooring observations at about 8N, 1273'E from December 2010 to December 2012. The strong southward Mindanao Current (MC) exists in the upper 600 m with a maximum mean velocity of 73 cm/s and a standard deviation of 17 cm/s at 100 m. A northward mean flow is observed below 600 m to the depth deeper than 1000 m, which has been called the Mindanao Undercurrent (MUC) with a maximum mean velocity of about 10 cm/s at 950 m and a standard deviation of 19 cm/s. Further analysis with hydrographic data and an eddy-resolving model outputs also suggests this northward mean current to be the MUC. Intraseasonal variability with a period of 60-80 days is revealed through the whole water column from 200 m down to about 900 m. This intraseasonal variability appears to be closely related to subthermocline eddies, which translate westward and intensify near the Mindanao coast. © 2014. American Geophysical Union. All Rights Reserved.
CITATION STYLE
Zhang, L., Hu, D., Hu, S., Wang, F., Wang, F., & Yuan, D. (2014). Mindanao Current/Undercurrent measured by a subsurface mooring. Journal of Geophysical Research: Oceans, 119(6), 3617–3628. https://doi.org/10.1002/2013JC009693
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