internal wave वाक्य
उदाहरण वाक्य
मोबाइल
- This vertical break up of internal waves causes significant diapycnal mixing and turbulence.
- Internal waves in a continuously stratified medium may propagate vertically as well as horizontally.
- Waves on the pycnocline, called internal waves, are ubiquitous in Pelorus Sound.
- An internal wave is a gravity wave that moves along density stratification within the ocean.
- When a water parcel encounters a different density it will oscillate and create internal waves.
- Internal wave amplitudes of around have been observed, generating flow speeds as great as.
- Where the ignimbrite was dammed by older lava flows, it formed internal wave structures.
- As tides interact with varying bathymetry and wind mixes with surface water, internal waves are created.
- It is for this reason that internal waves move in slow-motion relative to surface waves.
- In analogy with the Merian formula, the expected period of the internal wave can be expressed as:
- In particular, this shows that the buoyancy frequency is an upper limit of allowed internal wave frequencies.
- Another example is internal waves, which can be transmitted along the interface of two water masses of different densities.
- Other solitons occur as the undersea internal waves, initiated by seabed topography, that propagate on the oceanic pycnocline.
- Internal waves can act as nutrient pumps, bringing plankton and cool nutrient-rich water up to the surface.
- Similarly, as internal waves and bores move vertically, surface-dwelling larval organisms are carried toward the shore.
- Internal waves are usually distinguished from Rossby waves, which are influenced by the change of Coriolis frequency with latitude.
- The dispersion relation for such waves is curious : For a freely-propagating internal wave propagation within a waveguide.
- Improvement of tide modeling by observing more long period components such as costal interactions, internal waves, and tidal energy dissipation.
- Water can be moved through coral reefs in various ways, including current rings, surface waves, internal waves and tidal changes.
- These are a form of internal wave driven by the local tidal flow forcing the stratification against sloping areas of the shelf face.
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