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| In this wildfire simulation, as the
fire spreads, it evolves into a shape well-known to fire managers.
The "head" is the leading edge of the fire where the heat is focused.
Along the side are two "flanks", where the winds blow
parallel to the edge of the fire. The "Back" is the slowest moving
part of the fire and creeps against the wind.
In addition, an animation of the vertical vorticity (rotation of
air) shows the presence of fire whirls. Wildfires can contain fire
whirls of greatly varied intensity, duration and size - from a few
meters in diameter, to where the entire smoke-filled updraft (perhaps
1 km wide) is rotating. Most are small, but they have been known
to break off trees more than a meter in diameter. |
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| Universal Fire
Shape -
Tracer Field (Smoke) |
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Fire Whirls -
Vertical Vorticity |
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QuickTime
| Real
| MPEG 9 MB |
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QuickTime
| Real
| MPEG 14 MB |
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| The fire starts as
a line with constant easterly winds of 3 m/s driving the fire from
behind. The misty field is smoke, denser and more red where the
fire is burning most intensely.
The heat from the fire rises in updrafts
that the winds focus at the head of the fire. These updrafts draw
warm air into their base from all directions, guiding the wind to
flow along the flanks and focus the heat at the front. In this way,
the interaction of the fire with environmental winds creates a self-perpetuating
universal shape that is observed in fires in many conditions all
around the world.
As the fire grows, perturbations
(seen in the vorticity animation to be fire whirls) occur along
the fire flank and are brought forward to the head, which gets stronger.
These fire whirls change the airflow all around the fire, directing
some parts of the fire into fresh fuel, creating local heat, and
even creating more fire whirls. This increase in intensity is not
due to the environment, which remains constant, or to the fuel,
which is the same throughout the domain, but purely the fire-induced
winds. |
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Vorticity (the rotation of air)
is formed by the strong difference in temperature between the
fire-heated air and the cooler environment and is a very important
part of fires. This animation demonstrates how and where fire
whirls form along the fire line.
The red whirls represent positive
vertical vorticity (counter-clockwise rotation when viewed from
above the fire). Blue whirls are negative (clockwise).
This animation shows fire whirls
at the head of the fire, and forming along the flanks at the intersection
of the edge of the fire with unburned fuel. This is where the strongest
gradients are, where the winds created by the fire bring them forward
to the head. Note the suddenly strong and erratic wind vectors as
the whirls move by. |
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The high windspeeds in a fire whirl allow it to pick up debris and toss
it out the top from short distances up to several miles ahead of the fire.
They depend on a supply of heated, buoyant air that rises in columns and
draws in more heated air near the surface. Once the rotation starts, a
result of the gradients between hot/cold air or fast/slow moving air,
the rotation is intensified by stretching as the hot column pulls the
air upwards.
The fuel is "chaparral", a brush common in parts of CA, AZ, and the central
Rocky Mountains. Wildfire control in chaparral, a species that has adapted
itself to recurring fires, is notoriously difficult, because coupling
Santa Ana winds, with droughts, long summers, and often steep terrain,
creates intense, rapidly spreading fires.
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| Data |
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Time Evolution: |
~1.5 hours |
Time Resolution: |
6 sec |
| Domain |
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Vertical Real World: |
750 meters |
Horizontal Resolution: |
90x90 |
Vertical Resolution: |
100 |
| Visualization |
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Visualization: |
Tim Scheitlin |
Software: |
Vis5D |
| Project |
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Scientists: |
Janice Coen, Ph.D. |
Date Catalogued: |
2002-08-12 |
Rights: |
© 2002, UCAR,
All rights reserved. |
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