FREQUENTLY
ASKED AURORA QUESTIONS FROM STUDENTS AND TEACHERS:
What
causes the aurora?
The aurora is caused by a powerful electrical discharge in the sky, similar to
lightning. High-energy electrons generated by the discharge hit atoms and molecules
in the upper atmosphere, which give off light. The auroral discharge is far more
powerful than lightning.
-- Asahi
Aurora Classroom, UAF Geophysical Institute
I know the aurora in the northern hemisphere
is called the aurora borealis, but what is the aurora called in the
southern hemisphere?
The aurora in the southern hemisphere is called the aurora australis.
Interestingly, the aurora australis is almost a mirror image of the
aurora borealis.
-- Lori Schoening, Aurora Alive Education Specialist
Where can the aurora borealis be seen?
The aurora borealis can be seen best along the belt that connects
central Alaska, the Great Slave Lakes (Yellowknife) in Canada,
the southern timp of Greenland, Iceland, and the northern tip of
Scandinavia.
-- Asahi
Aurora Classroom, UAF Geophysical Institute
Intense auroras can be seen in the continental U.S., particularly
in the north, when solar activity is high.
-- Aurora Information Sheet, UAF Geophysical Institute
When is the best time to see the aurora?
The aurora is likely to be visible from September to March and especially
around the time of the equinoxes (September 21 and March 21).
The spring months of January through April are often the best time
to view the aurora because of better weather, however fall can
be just as cooperative weather-wise. Best viewing time is at 1:30
a.m. daylight-saving time in Alaska's time zone. From mid-August
through the beginning of May, weekly forecasts of auroral activity
can be accessed through the UAF Geophysical Institute's Web site
at www.gi.alaska.edu.
-- Neal Brown, Assistant Professor of Physics and Aurora Alive
Professional Development Instructor
Is the aurora harmful?
The aurora can cause a variety of problems. It can disrupt radio
communications, damage satellites, and disrupt power stations and
power lines resulting in power outages. The high-enery electrons
that produce the aurora may be hazardous to astronauts in space
so they should remain in the spacecraft when it flies through an
aurora. Here on earth's surface we are safe. We live and travel
in only the first 14km (8 miles)
of Earth's atmosphere, nearly 100km (60 miles) below the aurora.
Because of the protective role of the atmosphere, the aurora
and the high-energy electrons that produce it (under normal conditions)
pose no known health risks, such as those from radiation or
electric shock.
-- Asahi
Aurora Classroom, UAF Geophysical Institute
Can an airplane fly through the aurora?
No. The lower edge of the auroral curtain is 60 to 70 miles above Earth,
which is about ten times higher than a jet aircraft flies.
-- Aurora
Information Sheet, UAF Geophysical Institute
What causes the different colors of the aurora?
Auroral color depends on the type of atoms and molecules struck by
the energetic particles that rain down along Earth's magnetic field
lines in the discharge process. Earth atmospheric gas glows with
a specific color. For instance, green is produced by oxygen atoms
at roughly 60 miles altitude.
-- Aurora Information Sheet, UAF Geophysical Institute
Is it true that Earth's magnetic field could disappear
within the next 1,000 years?
No. As long as Earth has a liquid core we will have a magnetic
field, and Earth will have a liquid core for a few billion years
to come.
-- Dirk Lummerzheim, Aurora Alive Scienctist Mentor
Is it true that, without a stable magnetic field,
Earth would not have northern or southern lights (aurora)?
That is, in fact, the case. If the magnetic field were to get
weak and unstable, and lose its dipole structure, we also would
lose the present magnetosphere. Then, we would not have the processes
that shape and make the aurora as we know it. Instead, we would
have the solar wind interacting with the upper atmosphere or
remaining unstructured magnetosphere. This would still produce
aurora, but that aurora would look very different from today's
aurora. It woud endeed be everywhere, but it would be dim and
diffuse, not the exciting curtains we see nowadays. There is
an example of this happening in our own solar system on Venus.
Venus has no magnetic field, but a nice, thick atmosphere. The
aurora there is so weak that only the most sensitive instruments
can see any of it at all. So, if we have just a little bit of a
magnetic field, we would have aurora somewhere between the Venusian
aurora (almost non-existent) and the spectacular Earth aurora.
-- Dirk Lummerzheim, Aurora Alive Scienctist Mentor
Are Earth's magnetic poles going to shift soon?
In the history of Earth, the magnetic field often has reversed
direction. Over the last 4 million years there have been 13 documented
reversals. They tend to happen either right after one another,
or at fairly large time intervals. Many reverslas have about 300,000
to 500,000 years in between, but several only have about 50,000
years in between. The last one was about 700,000 years ago, so
you might think we are due for another one.
Nobody really knows how such a reversal is going to happen, or
how long it is going to take. Some theories predict that it would
take about 1,000 years to switch from one direction to the opposite.
Some theories predict that the magnetic field will get weak, almost
go away, and eventually pop up again, and maybe do this many times
over a period of 1,000 years. In that case, the whole process of
reversal also would take 1,000 years, but that millenium would
almost be without a field, or at least with a very variable and
chaotic field.
-- Dirk Lummerzheim, Aurora Alive Scienctist Mentor
Is it true that within the next thirty years
the aurora will
disappear...a student's mom said she heard it on the discovery
channel or the news?
I believe this story is based on an American Geophysical Union contribution from
a physicist working in paleo-magnetic field. He had studied the ancient history
of Earth's magnetic field and compared that to contemporary
observations. From that he draws the conclusion that the current
movement of the dip-pole is likely to continue. This would place the
dip-pole, which is currently in northern Canada and moving
north-east, close to the Siberian coast in about 50-100 years.
As you know from the Aurora Alive, there is a difference between the
dip pole (where the magnetic field is vertical at the surface of
Earth) and the dipole pole, which is the one that the aurora cares
about. Historical evidence shows that the dipole pole also moves
whenever the dip-pole moves, so it is likely that the dipole will
also move towards the NE, but at a slower pace and not as far. The
aurora would thus only move slowly towards the north in Alaska. That
means that in 100 years, instead of having the most probable auroral
occurance over Ft Yukon, it would be over the Brooks Range or Barrow
or something like that.
-- Dirk Lummerzheim, Aurora Alive Scienctist Mentor
View FREQUENTLY ASKED QUESTIONS about Aurora Alive Return to top of page
LINKS FOR STUDENTS: About the University of Alaska: About the aurora: Return to top of page
TEACHER-SUGGESTED
READING:
Light Shows in the Night Sky: Auroras, by Donna Walsh Shepherd
The
Sun: Living With the Stormy Star, in National Geographic Magazine,
July 2004
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SCIENTIST MENTORS AND VILLAGES
SERVED:
ROGER SMITH, Geophysical Institute Director
Smith studies aurora dynamics at high latitudes. Smith mentors Aurora
Alive students in the villages of SAVOONGA, GAMBELL and DIOMEDE.
SYUN AKASOFU, International Arctic Research
Center Director
Akasofu's world-renowned research has become the foundation of
aurora studies around the globe. Akasofu mentors Aurora Alive students
in the villages of ARCTIC VILLAGE, STEVENS VILLAGE and BEAVER.
WILLIAM BRISTOW, Assistant Professor, Geophysical
Institute
Bristow uses a network of radars to study the aurora. Bristow mentors
Aurora Alive students in the villages of UNALAKLEET, ST. MICHAEL
and STEBBINS.
JOHN CRAVEN, Professor of Physics, Geophysical
Institute
Craven designs instruments for spacecraft used to study the aurora.
CHARLES DEEHR, Professor Emeritus, Geophysical
Institute
Deehr produces international Internet aurora forecasts. Deehr
mentors Aurora Alive students in the villages of STEVENS VILLAGE, HUGHES
and HUSLIA.
NETTIE LA BELLE-HAMER, Alaska Satellite Facility
Director, Geophysical Institute
La Belle-Hamer studies radar images of Alaska that can be used
in auroral research. La Belle-Hamer mentors Aurora Alive students
in the villages of MINTO, RUBY and GALENA.
DIRK LUMMERZHEIM, Research Professor, Geophysical
Institute
Lummerzheim studies aurora processes and arc formation. Lummerzheim
mentors Aurora Alive students in the villages of SHISHMAREF, TELLER
and BREVIG MISSION.
DANA MOUDRY, Post-doctoral Fellow, Geophysical
Institute
Moudry uses remote sensing to study the ionosphere, where the aurora
occurs. Moudry mentors Aurora Alive students in the villages of
FT. YUKON, VENETIE and CHALKYITSIK.
ANTONIUS OTTO, Physics Professor, Geophysical
Institute
Otto researches aurora dynamics and structures. Otto mentors Aurora
Alive students in the villages of CIRCLE, NULATO and NOME.
WEI SUN, Research Associate, Geophysical Institute
Sun studies aurora magnetic storms and space weather. Sun mentors
Aurora Alive students in the villages of ARCTIC VILLAGE, KOYUKUK, and
NULATO.
BRENTON WATKINS, Physics Professor, Geophysical
Institute
Watkins uses radar to perform research and numerical modeling
of aurora phenomena. Watkins mentors Aurora Alive students in the villages
of KOYUK, SHAKTOOLIK and WALES.
HEINZ WIECHEN, Associate Professor, Geophysical
Institute
Wiechen researches aurora-related dynamics and magnetospheric processes.
Wiechen mentors Aurora Alive students in the villages of WHITE
MOUNTAIN, GOLOVIN and ELIM.
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