National Geographic: Cyclone! Page #2
- Year:
- 1995
- 401 Views
and remain a cornerstone of
tornado science.
Although they occur
around the world,
three out of four tornadoes streak
the skies over the United States.
They favor the springtime, and the
warm hours between noon and sunset.
We say a tornado "touches down".
near the ground
and carries it upward in a spiral.
Most range from 150 to 1200 feet
in width,
and travel over land at about
a tube of condensed water vapor
that takes on the color of dust
and debris.
In North America, most tornadoes
rotate counterclockwise.
Perhaps one in a thousand spins
in the opposite direction.
Twisters appear in many guises.
They can bring to mind
the snapping of a bullwhip...
or the delicate dance of ghosts.
A single storm can spawn several
distinct funnels
"family."
For all their fury,
most tornadoes are short-lived.
Many last only minutes.
To the scientists who would study
them, they are elusive prey.
How to penetrate the twister's
secrets?
instrumented rockets into tornadoes
All right. Three. Two. One.
Fire!
There! Perfe...
No.
In the 1980's, researchers at the
tested the "totable tornado
observatory", nicknamed TOTO,
after Dorothy's dog
in The Wizard of Oz.
This four-hundred pound package
of sensors
was to record what no human can
even approach
without risking life and limb.
But predicting the path of a tornado
proved to be nearly impossible.
TOTO had one close call,
no direct hits.
For now, the safest way to see
inside tornadoes
is to probe them from afar with
Doppler radar.
Like an x-ray of a storm,
the system displays wind speed
and direction.
In 1981, scientists first detected
Today, the system is used to
issue warnings to the public.
Still, we're not exactly sure
why twisters form at all.
For Howard Bluestein,
Professor of Meteorology
at the University of Oklahoma,
there's only one way to find out.
Satellite pictures are nice.
Radar pictures are nice.
But you need to look out the window
and see the clouds at a
very very fine scale
to get a feeling for
what's happening.
I don't understand
how one can study a phenomenon
without actually experiencing it.
Seeing it or feeling it
or tasting it.
To me, that sets everything
in motion.
That makes me want to understand
why it's there,
what causes it,
They just issued a tornado warning
Every spring, Bluestein exercises
two considerable talents:
chasing tornadoes, and measuring
them with the latest technology.
Portable Doppler radar is like
a meteorological magnifying glass.
It allows Bluestein to measure
wind speed in very fine detail,
in specific regions of a tornado.
Okay, we better get going quickly.
That thing is starting to form
a nice funnel.
Actually, hold it.
Hold it. Hold it!
Can you turn it on?
It is starting to form a funnel
and it's not that far away.
I'm on the left side of that
tight circulation.
Bluestein's success rate is
better than most storm chasers'
to our north, northwest.
We're packing up the radar...
He estimates one
in nine expeditions ends
with an encounter.
OK, tornado is crossing the path
of the radar.
Debris in the air.
Strong tornadoes almost always form
under the southwest edge of a storm.
Bluestein plots his course
accordingly,
and tries to place his team roughly
two miles from touchdown.
Center it right on the funnel!
Oh, what a classic!
Should I go to FM?
Only if you have a good CW signal.
We're detectives.
We're looking for lots of bits
of evidence.
And the more pieces of evidence
we have,
the more likely it will be
that we'll be able to solve
the puzzle of why tornadoes form
and what's their structure.
April 26th, 1991.
Bluestein and his team track
the outbreak
that will ravage Andover, Kansas.
A spectacular funnel stops them
in Red Rock, Oklahoma.
Their Doppler radar will capture
the fastest windspeed on record:
nearly 280 miles an hour.
In the heat of the chase, even
Bluestein can miss a beat.
Let's get out of here fast,
let's go!
For less frenzied fieldwork,
Bluestein turns to these hunting
grounds:
the Florida Keys.August, 1993.
Atmospheric Administration,
and the National Geographic
Society
reunite Bluestein
with Dr. Joseph Golden,
expedition chief scientist.
As a graduate student,
Bluestein once joined Golden to
explore the skies over Key West.
This expedition marshals
state-of-the-art scientific
and photographic technology.
The quarry?
these tranquil waters.
In 1967, on a vacation trip,
Golden took a sightseeing flight
over the Florida Keys,
and had a chance encounter with
one of our atmosphere's most
startling apparitions.
Since that time,
he has become the world's leading
expert on waterspouts.
Our knowledge of these ethereal
ribbons was once based largely
on mariners' accounts.
Golden first emphasized their
similarities to tornadoes.
twister over land.
They form in gentler weather
than most violent tornadoes,
allowing close inspection.
Smoke flares will help visualize
airflow near the sea surface.
For Bluestein, this is an
unparalleled ringside seat.
When we're out in the great
plains looking at tornadoes,
we cannot see what's happening
right at the ground very clearly,
nor can we see what's happening
at cloud base extremely clearly.
The perspective that we get
from the helicopter
in that we can look down
at the sea surface...
and see the effect of rotation
at the ground level
and also be at cloud base
and practically kiss...
the condensation funnel
that's right outside the window
is really spectacular.
Ultimately, the ghostly waterspout
that trigger tornadoes.
Joe, I guess climatology works.
That was incredible!
Book a seat on the Space Shuttle for
the perfect view of these monsters
- over 500 miles wide,
and some ten miles high.
Creatures of the sea,
they breed in the warm oceans of
the tropics.
Depending on their birthplace,
we call then 'cyclones',
'typhoons', or 'hurricanes'.
These giants can stir up
more than a million cubic miles of
the earth's atmosphere every second,
and travel across an ocean at up to
Yet they have humble beginnings.
In the summer and fall,
the sun heats vast stretches of
tropical ocean
to over 82 degrees Fahrenheit.
Warm, moist air rises over these
hot spots,
forming bands of thunderstorms.
systems westward,
as surface winds spiral into the
low pressure beneath the clouds.
Occasionally,
one such spinning wheel
of thunderstorms gathers strength,
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