Not exact matches
However, this was the first, comprehensive, large - scale study of the
influence of an entire offshore reef system on
ocean wave transmission.
Based on the various factors that determine the overall ratio, the team determined the point at which a delta would no longer be a smooth outline, shaped by
ocean waves, but instead, a pointy coastline,
influenced more by the river.
As the
ocean conditions are ever changing and the
waves are
influenced by swells, winds and currents, I suggest checking with the life guards at any county or state beach park during your visit.
This would be some combination of warmings and coolings due to natural and / or human
influences such as aerosols, instabilities in
ocean currents, Length - Of - Day (LOD) fluctuations, the stadium
wave (Wyatt and Curry), the 3M effect (me, December 17, Global Environmental Change section, this AGU Fall Meeting), etc. etc..
These areas of open water
influence: (1) the land by allowing more
ocean waves and more coastal erosion, (2) Greenland outlet glaciers by exposing the glacier fronts to warmer
ocean waters, and (3) the atmosphere by providing a source of heat and moisture during autumn.
Today, considerable scientific research focuses on the global nature of tides, including their
influence on other physical processes in the
ocean such as circulation, mixing, and
wave generation.
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 she
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 she
ocean free surface to eliminate unphysical «virtual tracer flux» methods, (12) parameterization of tidal mixing on continental shelves.