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Thesis: "Submesoscale turbulence in the upper ocean" Thesis: "Geochemistry of deep-sea hydrothermal vent fluids from the Mid-Cayman Rise, Caribbean Sea".
Measurements of turbulence in the upper part of the near-neutral PBL are limited to few experiments in the marine PBL but numerical model results indicate exponential decrease of σu/u*, etc., with height.
With a continuing interest in the dynamics and impacts of sub-mesoscale turbulence in the upper ocean, Callies is focusing on fronts and currents 1-10 kinometers in horizontal extent, which are thought to achieve important exchanges of heat, carbon, and other tracers between the surface and interior ocean.
The density-dependence of inertial pressure losses has been widely attributed to the presence of turbulence in the upper airways and bronchi; however, several authors have noted that even under laminar flow conditions pressure losses may maintain an inertial dependence due to convective acceleration occurring as flow changes direction, for example, at airway bifurcations [ 12- 14, 22, 23].
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Turbulence, whether in the upper or lower atmosphere, generates unstable regions of varying densities, diminishing the atmosphere's ability to allow a beam of light to pass straight through with unchanging intensity.
Propagating upward, AGWs can become unstable and produce turbulence and irregularities in the upper atmosphere.
The inclusion of baffles around the membrane modules promoted turbulence and increased shear in the upper section of the membrane module by approximately 30%.
It seems, however, that crowd turbulence occurred even earlier in the upper part of the ramp; a video showing this with the file name http://video.web.de/watch/7678046 was apparently linked to the following web.de article: NRW erhebt schwere Vorwürfe gegen Veranstalter von Love Parade Video, but it is not accessible anymore.
We then discuss recent experimental results showing that 1. neutral air turbulence is regularly found only in the upper part of a PMSE layer and 2. that PMSE exist even if only a minor fraction of the overall negative charge is bound to aerosol particles.
Robert H. Kraichnan, an innovative physicist who shed light on the dynamics of turbulence in ocean waters and winds in the upper atmosphere, died on Feb. 26 in Santa Fe, N.M.
Significant entrainment of particles in wakes of rising bubbles observed in the lower region of the column, whereas, turbulence seemed to dominate the dispersion in the upper region of the tank.
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