Internal waves in a summer pycnocline of the East China Sea

被引:10
作者
Lozovatsky, Iossif [1 ]
Jinadasa, Priyantha [1 ,3 ]
Lee, Jae-Hak [4 ]
Fernando, Harindra Joseph [1 ,2 ]
机构
[1] Univ Notre Dame, Dept Civil Engn Environm & Earth Sci, Notre Dame, IN 46556 USA
[2] Univ Notre Dame, Dept Aerosp & Mech Engn, Notre Dame, IN 46556 USA
[3] Natl Aquat Resources Res & Dev Agcy NARA, Crow Isl 15, Colombo, Sri Lanka
[4] Korean Inst Ocean Sci & Technol, Ansans Si 426744, Gyeonggi Do, South Korea
关键词
Internal tide; High-frequency internal waves; Spectra; Tidal currents; East China Sea; YELLOW SEA; M-2; TIDE; GENERATION; PROPAGATION; VARIABILITY; EVOLUTION; CURRENTS; ENERGY; SHELF; SHEAR;
D O I
10.1007/s10236-015-0858-2
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The bottom-mounted acoustic Doppler current profiler (ADCP) data obtained over a 70-h period in the East China Sea, about 80 miles to the southwest of the Jeju Island, are used to study internal waves in relation to tidal cycle. The spectral densities of the horizontal velocities followed E (h) aEuro parts per thousand f (-aEuro parts per thousand 1) between f (0) aEuro parts per thousand 0.8 cph and the buoyancy frequency, where f (0) is a transition point connecting the f (-aEuro parts per thousand 1) subrange and the steep falloff of energy from the semidiurnal spectral maximum at f (M2) toward higher frequencies. Manifestation of large-amplitude internal waves in the pycnocline has been mostly observed during a transition phase from high to low barotropic tide.
引用
收藏
页码:1051 / 1061
页数:11
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