Weak genetic structure among populations of marine species is a predicted outcome of large larval dispersal distances in biophysical modeling experiments, in which strong currents advect
weakly swimming larvae across great distances (e.
The LCB measurement strategy using the current scan geometry and lidar capabilities is well suited to capture lower wind speed cases, which allow sampling a feature several times before it advects
out of the domain, but this scan geometry is not suited to high wind speed cases, where a feature may advect
out of the domain before it is properly sampled.
All that's needed is a wind of about 10-15 knots or more to advect
VOF methods utilize cell face normal velocities to advect
volume fractions .
From there, it only requires the typical anti-cyclonic circulation over southern Africa to advect
the moisture south across Namibia.
The high productivity of the California Current (CC) is primarily the result of local wind-driven seasonal upwelling and the interaction of alongshore currents with prominent coastal features such as capes, headlands, and bays that advect
upwelled water masses into complex patterns of offshore filaments and coastal retentive eddies (Davis, 1985; Gan and Allen, 2002).
These offshore winds advect
warmer air from the south into the region and push the ice offshore, and both actions accelerate ice breakup.
In this region, fresh water input is substantial, tides are relatively weak, coastline geometry is complex, and Loop Current eddies at the shelf break have been observed to advect
water far across the shelf.
For example, if the Bermuda High is positioned farther to the west than normal, light westerly winds advect
dry continental air into the Southeast.
U(x, y, t) and V(x, y, t) are the current velocities in the x and y directions, respectively, that advect
Regardless of its evolution, the pelagic lifestyle exposes larval fishes to hydrodynamic transport processes that may advect
them to new places.
Tidal currents not only advect
(transport) plankton, pollutants, and other floatables, but, if for some reason (usually related to variable water depth) the tidal currents show a variation in strength or direction, this variation itself is advected
by the tidal current.