Short-term fluctuations south of Japan and their relationship with the Kuroshio path: 8- to 36-day fluctuations
To detect short-term fluctuations south of Japan, we applied wavelet analysis to ocean reanalysis data of the Japan Coastal Ocean Predictability Experiment 2 with a horizontal resolution of 1/36°. It was found that fluctuations of the 8- to 36-day period band appear as frontal waves in the Kuroshio...
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Veröffentlicht in: | Ocean dynamics 2014-04, Vol.64 (4), p.537-555 |
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description | To detect short-term fluctuations south of Japan, we applied wavelet analysis to ocean reanalysis data of the Japan Coastal Ocean Predictability Experiment 2 with a horizontal resolution of 1/36°. It was found that fluctuations of the 8- to 36-day period band appear as frontal waves in the Kuroshio Current. The amplitude of the fluctuations increases toward the downstream of Cape Shionomisaki. The fluctuations have a wavelength of about 300 km, and the signals propagate eastward. The fluctuations of the 8- to 36-day period band are stronger during the period of the nearshore non-large-meander Kuroshio path than during the period of the offshore non-large-meander Kuroshio path. We suggest that the 8- to 36-day fluctuation is a result of the instability of the accelerated velocity of the Kuroshio Current downstream of Cape Shionomisaki. |
doi_str_mv | 10.1007/s10236-014-0701-1 |
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subjects | Atmospheric Sciences Earth and Environmental Science Earth Sciences Fluctuations Fluid- and Aerodynamics Geophysics/Geodesy Marine Monitoring/Environmental Analysis Norway 17-20 June 2013 Ocean currents Oceanography Topical Collection on the 5th International Workshop on Modelling the Ocean (IWMO) in Bergen Velocity Wavelet transforms |
title | Short-term fluctuations south of Japan and their relationship with the Kuroshio path: 8- to 36-day fluctuations |
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