Solitary wave effects north of Strait of Messina

• Published in: Ocean modelling (Oxford) Vol. 18; no. 2; pp. 97 - 121
• Main Authors: Warn-Varnas, A., Hawkins, J., Smolarkiewicz, P.K., Chin-Bing, S.A., King, D., Hallock, Z.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 2007
• Subjects: Barotropic tide; CTD chain data; Marine; Messina sill; Ocean models; Solitary waves; Wavelet analysis; MED, Tyrrhenian Sea; MED, Italy, Messina Strait; Wavelet analysis; Ocean models; Solitary waves; CTD chain data; Messina sill; Barotropic tide
• ISSN: 1463-5003; 1463-5011
• DOI: 10.1016/j.ocemod.2007.03.003

We present new results from a joint ocean-acoustic modeling study of solitary wave generation in the Strait of Messina, their propagation in the Tyrrhenian Sea and subsequent shoaling in the Gulf of Gioia. The nonhydrostatic 3D EULAG model is used for the oceanographic predictions. The simulations are initialized with measured temperature and salinity profiles from an October 1995 survey of the Messina region, and forced with semidiurnal tidal magnitudes predicted by a barotropic tidal model. Parameter sensitivity studies are performed. The predicted solitary wave trains are compared with CTD chain measurements. The model results and data are examined through a wavelet analysis. The wavelengths are tracked by the spines (maximum intensity for each wavelength) at various times. From the slope of the variations, phase speeds are derived as a function of wavelength. For the parameters extracted from CTD measurements and existing tidal conditions, phase speed distribution for wavelengths ranging from about 0.6
m to 1.6
km are obtained. The model predicted phase speed magnitudes range from 0.85
m
s
−1 to 0.93
m
s
−1. The phase speeds derived from data range from 0.77
m
s
−1 to 0.88
m
s
−1. The model predicted phase speed versus wavelength distribution has similar trends to the phase speed versus wavelength distribution derived from data. The shoaling of the solitary waves in the Gulf of Gioia is studied. Calculations of the acoustical field are conducted, along the solitary wave propagation path, with the parabolic (PE) acoustical model.