This all - new sequel to the legendary arcade hit features amazing
dynamic water physics, transformable rocket - powered boats, gorgeous visuals and over-the-top interactive environments.
Hydro Thunder Hurricane (28th July 2010) This all - new sequel to the legendary arcade hit features amazing
dynamic water physics, transformable rocket - powered boats, gorgeous visuals and over-the-top interactive environments.
Next Gen Water Racing - Vector Unit's first game since Hydro Thunder Hurricane to be designed from the ground up for modern consoles, RGP: R sets the bar for dynamic water racing, with breathtaking
dynamic water physics, splash - tastic spray effects, and more!
So, next gen water racing is heading to Xbox One, utilising
dynamic water physics and new spray - effects.
It often resembles BioShock in both theme and setting, but stands out mostly due to
the dynamic water physics.
Not exact matches
Physics is sufficiently advanced today to define many substances very perfectly, in their very essence, in terms of those causes which constitute them, and in this we see that the active relationship by which, let us say, oxygen and hydrogen are defined as causes of
water in a given relativity, is an active potency in those causes of
dynamic finality with respect to the composite substance which is
water.
Some sources are going on about the
water physics in the game for some reason, which seem to be quite
dynamic indeed.
Radiative Transfer
Physics does not depend entirely on the simple absorbtivity of CO2, which by the way is effectively permanent in air when added by burning fossil fuels, compared to
water which saturates and precipitates out depending on climate conditions, such as warming due the GHE, as a marginal shift in the
dynamic equilibrium through feedbacks.
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.