Pages that link to "Item:Q980710"
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The following pages link to Tsunamis and acoustic-gravity waves from underwater earthquakes (Q980710):
Displaying 19 items.
- Wavemaker theories for acoustic-gravity waves over a finite depth (Q1700617) (← links)
- Progressive waves in a compressible-Ocean with an elastic bottom (Q1756450) (← links)
- The effect of compressed ice-shelf on acoustic-gravity wave propagation in a compressible ocean having elastic bottom (Q2124149) (← links)
- Acoustic-gravity waves generated by surface disturbances (Q2681460) (← 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)
- On the steady-state resonant acoustic–gravity waves (Q4582975) (← links)
- Observations and modeling of the elastogravity signals preceding direct seismic waves (Q4646017) (← links)
- (Q4648625) (← 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)
- Depth-integrated equation for large-scale modelling of low-frequency hydroacoustic waves (Q5417338) (← 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)