19 research outputs found
Observations of nonlinear internal waves at a persistent coastal upwelling front
We collected high-resolution observations of nonlinear internal waves (NLIWs) at a persistent upwelling front in the shallow coastal environment (~20 m) of northern Monterey Bay, CA. The coastal upwelling front forms between recently upwelled waters and warmer stratified waters that are trapped in the bay (upwelling shadow). The front propagates up and down the coast in the along-shore direction as a buoyant plume front due to modulation by strong diurnal wind forcing. The evolution of the coastal upwelling front, and the subsequent modulation of background environmental conditions, is examined using both individual events and composite day averages. We demonstrate that regional-scale upwelling and local diurnal wind forcing are key components controlling local stratification and the formation of internal wave guides that allow for high-frequency internal wave activity. Finally, we discuss the ability of theoretical models to describe particularly large-amplitude internal waves that exist in the presence of a strong background shear and test a fully nonlinear model (i.e., the Dubreil–Jacotin–Long equation)
Turbulence and Fossil Turbulence in Oceans and Lakes
Turbulence is defined as an eddy-like state of fluid motion where the
inertial-vortex forces of the eddies are larger than any of the other forces
that tend to damp the eddies out. Energy cascades of irrotational flows from
large scales to small are non-turbulent, even if they supply energy to
turbulence. Turbulent flows are rotational and cascade from small scales to
large, with feedback. Viscous forces limit the smallest turbulent eddy size to
the Kolmogorov scale. In stratified fluids, buoyancy forces limit large
vertical overturns to the Ozmidov scale and convert the largest turbulent
eddies into a unique class of saturated, non-propagating, internal waves,
termed fossil-vorticity-turbulence. These waves have the same energy but
different properties and spectral forms than the original turbulence patch. The
Gibson (1980, 1986) theory of fossil turbulence applies universal similarity
theories of turbulence and turbulent mixing to the vertical evolution of an
isolated patch of turbulence in a stratified fluid as its growth is constrained
and fossilized by buoyancy forces. These theories apply to the dynamics of
atmospheric, astrophysical and cosmological turbulence.Comment: 31 pages, 11 figures, 2 tables, see http://www-acs.ucsd.edu/~ir118
Accepted for publication by the Chinese Journal of Oceanology and Limnolog