Pages that link to "Item:Q5417338"
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The following pages link to Depth-integrated equation for large-scale modelling of low-frequency hydroacoustic waves (Q5417338):
Displaying 16 items.
- An extension of the Boussinesq-type models to weakly compressible flows (Q2056037) (← links)
- A two-dimensional, depth-integrated model for internal wave propagation over variable bathymetry (Q2387569) (← links)
- Dynamic modeling of the propagation of low-frequency seismic acoustic fields in the oceanic medium (Q2900768) (← links)
- Acoustic–gravity waves from multi-fault rupture (Q3388850) (← links)
- Hydro-acoustic precursors of gravity waves generated by surface pressure disturbances localised in space and time (Q3448441) (← links)
- HYBRID ALGORITHM OF THE DEPTH SOLVER FOR WAVENUMBER INTEGRATION TECHNIQUE IN AN OCEAN WAVEGUIDE WITH A POROUS BOTTOM (Q4907771) (← links)
- Effects of the sound speed vertical profile on the evolution of hydroacoustic waves (Q5205725) (← links)
- Sound signals of tsunamis from a slender fault (Q5226210) (← links)
- On the propagation of acoustic–gravity waves under elastic ice sheets (Q5226295) (← links)
- Hydro-acoustic frequencies of the weakly compressible mild-slope equation (Q5364418) (← links)
- On the propagation of acoustic–gravity waves due to a slender rupture in an elastic seabed (Q5875855) (← links)
- Time-domain wave response of a compressible ocean due to an arbitrary ocean bottom motion (Q6043279) (← links)
- Acoustic and gravity waves in the ocean: a new derivation of a linear model from the compressible Euler equation (Q6095208) (← links)
- Effect of static compression on near-field tsunami waves: three-dimensional solution (Q6572787) (← links)
- Surface wave generation from a constant-slope-inducing asymmetric ocean floor motion: influence of compressible ocean (Q6640550) (← links)
- Well-posedness and potential-based formulation for the propagation of hydro-acoustic waves and tsunamis (Q6667318) (← links)
