Sentence examples for ocean gravity from inspiring English sources

In a strict sense, it is known that the density structure of the real ocean contributes to the slow propagation of ocean gravity waves.

The geophysical signal retrieved by Swarm is mainly hydrology because the tides are modelled and the non-tidal atmospheric and ocean gravity field variations are either modelled (as is the case with the ASU and IfG solutions) or shown to have no significant influence in the solutions of AIUB (cf. Jäggi et al. 2014, Figure 4, for the case of GOCE).

There you'll find electric oceans, gravity-defying sludge, people made from bubbles, and worlds within worlds within worlds.

Ocean surface gravity waves play a major role in many engineering and environmental problems, both in the open ocean and in coastal zones.

It is conjectured that tsunami waves in the ocean generate gravity waves that propagate obliquely upwards and interact with the ionospheric electron density.

These include self-organized behavior of beach morphology, the fractal nature of ocean surface gravity waves, the self-organization of beach cusps and simulation models of ripples and dune patterns.

We test this claim with a "full-physics" integrated dynamic rupture and tsunami model that couples the elastic response of the Earth to the linearized acoustic-gravitational response of a compressible ocean with gravity; the model self-consistently accounts for seismic waves in the solid Earth, acoustic waves in the ocean, and tsunamis (with dispersion at short wavelengths).

In addition to Cryosphere applications, this mission is of great interest to the Hydrosphere and Oceanographic communities since it allows for quantitative assessment of expected enhanced altimetric capabilities in coastal monitoring, ocean floor topography, gravity field and inland water monitoring.

We solve the elastic wave equation in the solid Earth and the acoustic wave equation in the compressible, inviscid ocean, and incorporate gravity via a modified free surface boundary condition.

Susanto and Song (2015) used altimeter sea surface height (the sea level difference between any point in the western Pacific and in the eastern Indian Ocean) and gravity ocean bottom pressure data, to derive an ITF proxy.

Democracy would not have prevented the ocean tides, driven by gravity, from drowning Canute if he had stayed on his throne, and a referendum will not turn back the economic tides driven by globalisation.