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

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Figure

Figure 2. Scheme of internal solitary waves of the second modewith positive (left) and negative (right) polarity.
Figure 3. An example of the vertical profile of the densityBrunt–Väisälä frequency (a) and (b) of a quasi-two-layer marine environ-ment.
Figure 5. (a) Location scheme of the South China Sea (http://www.nationsonline.org/oneworld/map/South-China-Sea-political-map.htm);(b) bathymetry of the South China Sea extracted from the GDEM database (Carnes, 2009).
Figure 7. (a) Map of the vertical location of the normalised zero-crossing depth(b) z0/H of the mode function in July in the South China Sea; histogram of values of z0/H
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