Abstract

Internal solitary waves (ISWs) in the South China Sea (SCS) have received considerable attention. This paper reports on a strong ISW captured northeast of Dong-Sha Atoll on 22 May 2011 by shipboard Acoustic Doppler Current Profiler (ADCP), which had the largest velocity among the ISWs so far reported in the global ocean. The peak westward velocity (u) was 2.94 m/s, and the peak downward velocity (w) was 0.63 m/s, indicating a first baroclinic mode depression wave. The amplitude of ISW inferred from ADCP backscatter was about 97 m. 2.2 h later, a trailing wave was captured with a peak westward velocity and downward velocity of 2.24 m/s and 0.42 m/s, respectively, surprisingly large for a trailing wave, suggesting that the ISW is type-A wave. The estimated baroclinic current induced by the leading ISW was much larger than the barotropic current. The Korteweg-De Vries (KdV) theoretical phase speed and the phase speed inferred from the satellite images were 1.76 m/s and 1.59 m/s, respectively. The peak horizontal velocity exceeded the phase speed, suggesting the ISW was close to or already in the process of breaking and may have formed a trapped core.

Highlights

  • IntroductionSouth China Sea (SCS) [1]

  • Internal solitary waves (ISWs) are ubiquitous in some marginal seas, especially in theSouth China Sea (SCS) [1]

  • The barotropic tide velocity can reach in the order of 10 cm/s in the northern SCS [22], which may contribute to the horizontal velocity in Acoustic Doppler Current Profiler (ADCP) measurements

Read more

Summary

Introduction

South China Sea (SCS) [1] They are supposedly generated near the Batan Islands of Luzon Strait and propagate northwestward in the deep basin with long crest lengths ranging from about 100 to 250 km [2,3], shoal onto the continental shelf and dissipate on the plateau [4]. Strong ISWs have been observed near Dong-Sha Atoll by moorings and shipboard surveys with amplitudes ranging from 70 to 173 m and peak westward velocities from 0.73 to 2.4 m/s [4,5,6,7,8,9,10,11,12].

Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call