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Free Content Origin of the Luzon Undercurrent

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The origin of the Luzon Undercurrent (LUC) was studied by a climatological simulation using a high-resolution quasi-global HYbrid Coordinate Ocean Model, configured with climatological European Centre for Medium-Range Weather Forecasts wind and heat forcing. Lagrangian trajectory analysis suggests that the LUC generally originates from the confluence region of the Kuroshio and Oyashio, with its shallow, middle, and deep parts originating from corresponding parts of the North Pacific intermediate Water (NPIW). About 86.0% (77%–93% = 95% confidence interval) of the LUC at 18°N conveys low-salinity NPIW southward. The LUC plays an important role in the southward intrusion of NPIW into the tropical Pacific.

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Document Type: Research Article

Publication date: 2012-01-01

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  • The Bulletin of Marine Science is dedicated to the dissemination of high quality research from the world's oceans. All aspects of marine science are treated by the Bulletin of Marine Science, including papers in marine biology, biological oceanography, fisheries, marine affairs, applied marine physics, marine geology and geophysics, marine and atmospheric chemistry, and meteorology and physical oceanography.
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