EXPERIMENTING WITH FLUIDS Winter 2008
Geophysical Fluid Dynamics Laboratory
Room 107 Ocean Sciences Building, School of Oceanography
P.B.Rhines 543-0593, cell 360-643-0740
web
E.G.Lindahl 543-2515
R.Koon 543-2515
Mr. Wizard (Don Herbert)
Focus the Nation: Thursday 31
Jan....attend as many
of these events as you can...free snacks and coffee will be one reward (and
there
will hopefully be others)! depts.washingon.edu/focus
Water has a more extensive molecular structure than previously thought: see UW Annual Faculty Lecture: Gerald Pollack on Water, Energy and Life: Fresh
Views from the Water's Edge 7.00pm Weds. 30 Jan, 130 Kane Hall
...see
this link
Students:
- Jordan Allen-Flowers, AMath.. internal gravity waves
optical visualization and mean-flow generation
- Maggie Avener, CEE.. a tidally pumped river plume entering the ocean, imaging
with optical altimetry
- Joey Duncan, AA.. vortex dynamics near a free water surface and
vortex line dynamics with Earth's rotation
- Vivian Leung, ESS.. flow and sediment movement in a river blocked by a
porous logjam
- Hallie Torrey, AMath.. summer and winter beach building and erosion by surf,
and wave pumping of porous flow in the sand
- Yeping Yuan, CEE.. two rivers entering the ocean: interaction of plumes
- Eleanor Williams, Ocean.. baroclinic fronts at a ridge separating Arctic and
subpolar basins
LINKS
glass spheres coated with fluorescein make perfect vertical dye lines which then
trace the swirling entrainment of this jet (the jet flows downward at the center of
the image)
long strings of yarn showing flow round an obstacle in the water channel (the re-entrant
flume).
combination of mountain induced gravity waves and shear instability
frontal instability of a dense water mass in a rotating basin (with a cylindrical mountain),
seen from above
vortex ring formation with a free surface (left: optical deformation of a grid placed beneath the
tank; right: sunlit image)
This series of pictures (taken with
an obviously non-stationary camera) shows the flow through sediment as driven by a
"winter" wave. The line of dark sand verifies a guess that the sand, over a
relatively short time period, does not move. This line also shows how the flow --
or perhaps the dye -- is affected by a different type of sediment. (The dark sand
was much finer than the rest.) Though it cannot be shown by the pictures, it is
interesting to note that the flow of the fluid through the sediment is not
oscillatory like the waves that drive the motion, but instead seems almost
constant along the flow lines.
river source flow
dye deformation on an internal surface of constant density with internal gravity waves
convective 'tornados' in the river plume experiment on the rotating table
(click to enlarge)
Leonardo daVinci's Studies of water passing obstacles and falling, circa
1508-09.
Flow vizualization
fluorescein dye line wrapped up by a vortex (the line is 'injected' by dropping
a glass sphere coated with dye, which is initially vertical and straight)
Time exposure phototgraphy for internal waves in a uniformly stratified fluid
(yet with a mixed layer at the top; J.Renwick, GFD projects course).