4.7 Article Proceedings Paper

M2 baroclinic tide variability modulated by the ocean circulation south of Japan

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 120, Issue 5, Pages 3681-3710

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015JC010739

Keywords

M-2 baroclinic tide; ocean circulation; OGCM simulation

Categories

Funding

  1. JSPS KAKENHI [26400468]
  2. Grants-in-Aid for Scientific Research [26400468] Funding Source: KAKEN

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We analyze a concurrent simulation result of the ocean circulation and tidal currents using a data-assimilative ocean general circulation model covering the Western North Pacific with horizontal resolution of 1/36 degrees to investigate possible interactions between them. Four sites of active M-2 internal tide variability in open ocean (hot spots), such as Tokara Strait, Izu Ridge, Luzon Strait, and Ogasawara Ridge, are detected from both the satellite observation and the simulation. Energy cycle analysis of the simulated M-2 baroclinic tide indicates two types of the hot spots: dissipation (Tokara Strait and Izu Ridge) and radiation (Luzon Strait and Ogasawara Ridge) dominant sites. Energy conversion from barotropic to baroclinic M-2 tides at the hot spots is modulated considerably by the lower-frequency changes in the density field. Modulation at the two spots (Tokara Strait and Izu Ridge) is affected by the Kuroshio path variation together with the seasonal variation of the shallow thermocline. At the other two sites, influence from changes in the relatively deep stratification through the Kuroshio intrusion into South China Sea (Luzon Strat) and mesoscale eddy activity (Ogasawara Ridge) is dominant in the modulation.

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