The data produced helps us to not only see the ruins, but also understand more about how they interact
with the tidal currents and sea bed.»
Not exact matches
Tides and
tidal currents help mix cold arctic waters
with warmer waters in the tropics.
There is the pleasant cunning of making the wind take us where we want to go, and there are charts to read,
with their soundings and buoys and markers, and the tide tables, and the
tidal current tables, and the
tidal current charts, and knots and splices to learn.
After the powerful
current of the East River — which is actually a
tidal channel — damaged the rotors and broke off some of the original fiberglass and steel blades, the company earlier this month whittled its test bed down to two turbines
with new aluminum — magnesium blades 16 feet (five meters) in diameter.
The models were not sophisticated enough to cope
with the combination of «relatively coarse
tidal and
current data» and a general inability to predict the movement of oil on the surface in a complex inshore location.
Balazs and his colleagues report in the
current issue of the Marine Pollution Bulletin how 300 pellets a day were washing up on Kualoa Beach: «A general review of data for
tidal cycles, moon phases, wind speed and direction, and surf conditions failed to identify any consistent correlation
with the erratic fluctuations in daily faecal counts.»
A report in the journal Nature cites the discovery of a new planet, WASP - 18b, which challenges assumptions about
tidal interactions — it's too close and orbiting too fast not to have collided
with its star, according to
current knowledge.
According to Doug Armstrong, Ocean Beach Patrol Supervisor, Ocean Beach's exposure to multiple swell directions coupled
with its proximity to the
tidal exchange at the mouth of the Golden Gate Strait make it subject to a tremendous amount of rip
currents — and the rip
currents change every day.
Langebaan Lagoon extends in a finger of water away from Saldanha Bay, its 16 kilometres controlled by
tidal currents, tailing off into salt marshes and a cluster of salt pans, rich
with water bird life.
Ride the
currents through
tidal channels filled
with schooling sharks.
The Channel itself is about 30 ft (9 meters) deep,
with occasionally strong
tidal currents.
To reach the lighthouse we had to cross Christie Passage, a narrow waterway
with strong
tidal currents.
There were an estimated 31 fish eating orca working the
tidal currents, and mixed in
with them were humpback whales who were also feeding!
Predicting sea ice extent is easy if you can mentally calculate wind variations, momentum, sea
currents, multi year ice compression ratios,
tidal synergy
with weather patterns, the AO, the temperature of ice sea water and air, how cloudy it will be, salinity, pycnocline convection rates, sea surface to air interface, CO2 exchange, ice thickness distributions.....
Tidal variability in more complex regional models that include sea ice, ice shelves, and ocean
currents that vary
with depth, is obtained by using global models to set tides at the regional model's open boundaries.
However the
tidal currents coming into contact
with the relief of the ocean bottom (even if this is very deep) creates waves which are propagated at the interface between two layers of different densities.
Most existing
tidal currents devices have been based on horizontal axis propeller - type designs, much like wind turbines, mounted on fixed towers or on the sea - bed, sometimes
with ducts to enhance the flow.
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.
The Piscataqua River is a
tidal estuary
with a swift
current, but forms a good natural harbor.