This series of plots shows significant wave height (in meters, indicated by color scale) in the western Arctic Ocean during the 2016 Arctic cyclone, from August 14 to August 16, 2016, as predicted by
a numerical wave model (WAVEWATCH III), run at the Naval Research Laboratory (NRL).
Not exact matches
«This information is often used in
numerical modeling of landslide - generated tsunami
waves.»
«We computed this tsunami - like
wave with our
numerical models and found its energy to be very similar to
waves from past tsunamis in the Pacific,» says Roeber.
French used
numerical simulations to compute all components of the seismic
waves, such as their scattering and diffraction, and tweaked the
model repeatedly to fit recorded data using a method similar to statistical regression.
Professor Ranasinghe comments: «Plans are under - way to investigate the
wave attenuation characteristics over the reef in more detail, using sophisticated
numerical modelling.
Simmons, with the help of the Arctic Region Supercomputer Center, which is part of the UAF Geophysical Institute, used math equations to make detailed
numerical simulations, or high - resolution
models, of under - ocean
wave processes.
According to their
numerical 3D
models of an earthquake and resultant tsunami on the Pitas Point and Red Mountain faults — faults located offshore Ventura, Calif. — a magnitude 7.7 earthquake would result in many parts of the regional coastline being inundated a few kilometers inland by a tsunami
wave, with inundation in places greater than that indicated by the state of California's current reference inundation line.
They are collecting data from their
numerical modeling and experimental research to benefit
wave energy technology with improved methodologies, strategic control systems design and testing practices for
wave energy converters.
But then the effective heat capacity, the surface temperature, depends on the rate of mixing of the ocean water and I have presented evidence from a number of different ways that
models tend to be too diffusive because of
numerical reasons and coarse resolution and
wave parameter rise, motions in the ocean.
These
waves are sometimes called finite difference
waves, because of the finite difference
numerical modeling techniques used to calculate their propagation characteristics.
That requires considerable sensitivity research with state - of - the art
numerical weather prediction (and climate)
models... This hand -
waving theory may not hold up when a rigorous scientific hypothesis is tested, yet McKibben does not provide a citation or reference aside from Masters» quotations, which are not peer - reviewed in the slightest.»
Features of the
model described here include the following: (1) tripolar grid to resolve the Arctic Ocean without polar filtering, (2) partial bottom step representation of topography to better represent topographically influenced advective and
wave processes, (3) more accurate equation of state, (4) three - dimensional flux limited tracer advection to reduce overshoots and undershoots, (5) incorporation of regional climatological variability in shortwave penetration, (6) neutral physics parameterization for representation of the pathways of tracer transport, (7) staggered time stepping for tracer conservation and
numerical efficiency, (8) anisotropic horizontal viscosities for representation of equatorial currents, (9) parameterization of exchange with marginal seas, (10) incorporation of a free surface that accommodates a dynamic ice
model and
wave propagation, (11) transport of water across the ocean free surface to eliminate unphysical «virtual tracer flux» methods, (12) parameterization of tidal mixing on continental shelves.