The phenomenon that is shown in the image of Guadalupe
Island at the top of this page (acquired on August 20, 1999) features a
ubiquitous occurrence in the motion of fluids—a vortex street, which is a
linear chain of spiral eddies called von Karman vortices. Von Karman
vortices are named after Theodore von Karman, who first described the
phenomenon in the atmosphere. Dr. von Karman was a co-founder of NASA's Jet
Propulsion Laboratory.
von Karman vortices form nearly everywhere that fluid flow
is disturbed by an object. In the cloud images shown on this page, the
"object" that is disturbing the fluid flow is an island or group of islands.
As a prevailing wind encounters the island, the disturbance in the flow
propagates downstream of the island in the form of a double row of vortices
which alternate their direction of rotation. The animation below shows how a
von Karman vortex street develops behind a cylinder moving through a fluid.
Both the ocean and atmosphere are fluids, in constant
motion. On our limited “human”-scale, we are aware of this motion when we feel
the wind blow, or when we encounter a current running along the beach
while swimming. Yet our eyes alone can rarely observe the larger scale of fluid
motion in the ocean and atmosphere.
Technical description: As a fluid particle flows
toward the leading edge of a cylinder, the pressure on the particle rises
from the free stream pressure to the stagnation pressure. The high fluid
pressure near the leading edge impels flow about the cylinder as
boundary layers develop about both sides. The high pressure is not sufficient
to force the flow about the back of the cylinder at high Reynolds
numbers. Near the widest section of the cylinder, the boundary layers
separate from each side of the cylinder surface and form two shear layers
that trail aft in the flow and bound the wake. Since the innermost
portion of the shear layers, which is in contact with the cylinder, moves
much more slowly than the outermost portion of the shear layers, which is
in contact with the free flow, the shear layers roll into the near wake,
where they fold on each other and coalesce into discrete swirling
vortices. A regular pattern of vortices, called a vortex street, trails
aft in the wake.
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