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  4. Estimating propagation speed and direction, and vertical displacement of second-mode nonlinear internal waves from ADCP measurements
 
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Estimating propagation speed and direction, and vertical displacement of second-mode nonlinear internal waves from ADCP measurements

Journal
Continental Shelf Research
Journal Volume
233
Date Issued
2022
Author(s)
Endoh T
Tsutsumi E
Hong C.-S
Baek G.-N
Chang M.-H  
Yang Y.J  
Matsuno T
Jae Hak Lee
DOI
10.1016/j.csr.2021.104644
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85122613724&doi=10.1016%2fj.csr.2021.104644&partnerID=40&md5=6064a2daa7e7d2308a558daf13a94d22
https://scholars.lib.ntu.edu.tw/handle/123456789/606383
Abstract
Propagation speed and direction, and vertical displacement of the second-mode nonlinear internal waves (NLIWs) over the continental shelf of the East China Sea are estimated by applying the iterative method, previously validated only for the first-mode NLIWs, to the along-beam velocities measured with the standard acoustic Doppler current profiler (ADCP). Two ADCPs mounted in trawl-resistance bottom mounts were deployed in upward looking configurations on the seabed at stations spaced 7.4 km apart, perpendicular to isobaths of the continental slope. During the observation period of two days, two wave trains arrived at an interval of approximately one day, whereas the flow was dominated by the semi-diurnal internal tide with a diurnal modulation. The results of the iteration show that the second-mode NLIWs of the convex type propagate shoreward at a speed of 0.44 (0.36) m s?1 at the offshore (onshore) station. The amplitude of the leading wave is estimated to be about 20 m at the offshore station, which is reduced to about 10 m at the onshore station. All the parameters agree remarkably well with those estimated independently from the backscatter signal of the ADCPs. The propagation time of 6.8 h estimated for the averaged propagation speed and direction is also consistent with a 6.9-h lag of the arrival time of the wave train between the two stations. In addition to the propagating features of the second-mode NLIWs, the iterative method reveals the wave-induced velocity associated with the radiation of short, small-amplitude first-mode waves from the second-mode NLIW, which has been observed only with shipboard echo sounders. ? 2022 The Authors
Subjects
Acoustic Doppler current profiler
East China Sea
Iterative method
Nonlinear internal waves
Second mode
Acoustic Doppler Current Profiler
backscatter
continental shelf
displacement
internal tide
China
Pacific Ocean
South China Sea
SDGs

[SDGs]SDG13

[SDGs]SDG14

Type
journal article

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