Articles | Volume 24, issue 4
Nonlin. Processes Geophys., 24, 645–660, 2017
https://doi.org/10.5194/npg-24-645-2017
Nonlin. Processes Geophys., 24, 645–660, 2017
https://doi.org/10.5194/npg-24-645-2017

Research article 19 Oct 2017

Research article | 19 Oct 2017

Kinematic parameters of internal waves of the second mode in the South China Sea

Oxana Kurkina et al.

Related authors

Exceedance frequency of appearance of the extreme internal waves in the World Ocean
Tatyana Talipova, Efim Pelinovsky, Oxana Kurkina, Ayrat Giniyatullin, and Andrey Kurkin
Nonlin. Processes Geophys., 25, 511–519, https://doi.org/10.5194/npg-25-511-2018,https://doi.org/10.5194/npg-25-511-2018, 2018
Short summary
Propagation regimes of interfacial solitary waves in a three-layer fluid
O. E. Kurkina, A. A. Kurkin, E. A. Rouvinskaya, and T. Soomere
Nonlin. Processes Geophys., 22, 117–132, https://doi.org/10.5194/npg-22-117-2015,https://doi.org/10.5194/npg-22-117-2015, 2015
Short summary
Features of fluid flows in strongly nonlinear internal solitary waves
S. Semin, O. Kurkina, A. Kurkin, T. Talipova, E. Pelinovsky, and E. Churaev
Nonlin. Processes Geophys. Discuss., https://doi.org/10.5194/npgd-1-1919-2014,https://doi.org/10.5194/npgd-1-1919-2014, 2014
Revised manuscript not accepted
Short summary

Related subject area

Subject: Nonlinear Waves, Pattern Formation, Turbulence | Topic: Climate, atmosphere, ocean, hydrology, cryosphere, biosphere
Particle clustering and subclustering as a proxy for mixing in geophysical flows
Rishiraj Chakraborty, Aaron Coutino, and Marek Stastna
Nonlin. Processes Geophys., 26, 307–324, https://doi.org/10.5194/npg-26-307-2019,https://doi.org/10.5194/npg-26-307-2019, 2019
Short summary
Explosive instability due to flow over a rippled bottom
Anirban Guha and Raunak Raj
Nonlin. Processes Geophys., 26, 283–290, https://doi.org/10.5194/npg-26-283-2019,https://doi.org/10.5194/npg-26-283-2019, 2019
Short summary
Internal waves in marginally stable abyssal stratified flows
Nikolay Makarenko, Janna Maltseva, Eugene Morozov, Roman Tarakanov, and Kseniya Ivanova
Nonlin. Processes Geophys., 25, 659–669, https://doi.org/10.5194/npg-25-659-2018,https://doi.org/10.5194/npg-25-659-2018, 2018
Short summary
On the phase dependence of the soliton collisions in the Dyachenko–Zakharov envelope equation
Dmitry Kachulin and Andrey Gelash
Nonlin. Processes Geophys., 25, 553–563, https://doi.org/10.5194/npg-25-553-2018,https://doi.org/10.5194/npg-25-553-2018, 2018
Short summary
Laboratory and numerical experiments on stem waves due to monochromatic waves along a vertical wall
Sung Bum Yoon, Jong-In Lee, Young-Take Kim, and Choong Hun Shin
Nonlin. Processes Geophys., 25, 521–535, https://doi.org/10.5194/npg-25-521-2018,https://doi.org/10.5194/npg-25-521-2018, 2018
Short summary

Cited articles

Cai, S., Long, X., and Gan, Z.: A numerical study of the generation and propagation of internal solitary waves in the Luzon Strait, Oceanol. Acta, 25, 51–60, 2002.
Carnes, M. R.: Description and evaluation of GDEM V3.0, NRL Rep. NRL/MR/ 7330099165, Nav. Res. Lab., 1–27, 2009.
Fofonoff, N. and Millard Jr., R.: Algorithms for computation of fundamental properties of seawater, UNESCO Technical Paper in Marine Science, 44, 15–25, 1983.
Grimshaw, R., Pelinovsky, E., and Talipova, T.: The modified Korteweg – de Vries equation in the theory of large – amplitude internal waves, Nonlin. Processes Geophys., 4, 237–250, https://doi.org/10.5194/npg-4-237-1997, 1997.
Grimshaw, R., Pelinovsky, E., Talipova, T., and Kurkin, A.: Simulation of the transformation of internal solitary waves on oceanic shelves, J. Phys. Oceanogr., 34, 2774–2791, 2004.
Download
Short summary
Large internal waves may be a great danger to offshore structures. The breaking of such waves may strongly modify the seabed. Their core properties depend on how temperature and salinity vary in the water column. These variations are represented by three vertical locations and four coefficients of the relevant equation. We established how these seven quantities vary in the South China Sea for waves of the second mode (which create compressions or expansions of the intermediate water layer).