Turbulence and Turbulent Transport
- Turbulence: Ubiquitous in
Nature
- Plasmas (laboratory to galactic scales)
- Geophysical systems (oceans, atmospheres and
magnetospheres)
- Most man-made fluid and gas systems (pipes, chemical
mixing tanks, etc.)
- Turbulent transport
(anomalous diffusion): important mechanism for relaxing
gradients
- Temperature, pressure and density gradients in
plasmas
- Constituent gradients in the atmosphere and ocean
(pollution, water vapor etc)
- Flows (external or
self-generated) often exist in turbulent systems
- Strong shear flows in laboratory and space
plasmas
- Jets and coherent structures in atmospheres and
oceans
- Differential rotation in stellar systems
Turbulence in a soap film. This beautiful experiment is done at
the University of Pittsburgh, for more information visit their
site
Turbulence in the ash plume of the Mt. Spurr volcano as it
erupts. The turbulence speeds the mixing of the ash in the atmosphere
and spreads it much more quickly then otherwise. For more information
on Mt. Spurr see the USGS
site.
Turbulence in the Sun (a fusion plasma). The turbulence in
plasmas is very important for transporting heat and particles from
one place to another, for example from the core of the sun to the
edge. For more information on, and pictures of, the sun see the
NASA site.
- Simplified models are used to understand the underlying
physics of the turbulence and transport
- More complete "primitive equation" models are used to study
the full turbulent dynamics for many systems.
- Resistive MHD
- DTEM
- Resistive G-mode
- TAE
Recent Papers and Presentations
Home
This was last changed on 11 Nov
1998
This page is maintained by David
Newman