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| Northern Lights over North Pole, Alaska |
These
northern lights (also called aurora) could’ve been easily confused with dawn
which did gradually encroach on the light display. Because of this similarity,
northern lights are also called “Northern Dawn” or “False Dawn”. The Latin
meaning of aurora borealis is “Northern Dawn”.
The
aurora can light up the sky like dawn but when active the swirling, rippling
and overhead displays cannot be mistaken for anything else. Legends and folk
tales provide many reasons for the aurora, including ancestors dancing in the
sky, but scientists know that solar particles and gas molecules create the
aurora.
The
northern lights are similar to neon lights which glow when energy (in the form
of electricity) is added to tubes of gas. With the northern lights, the energy
comes from the sun and the atmosphere is the tube of gas. The sun emits energized particles that are
carried toward earth on the solar wind. The earth’s magnetosphere (a protective
shield created by the Earth’s magnetic field) prevents the majority of particles
from bombarding earth but a small portion penetrates the barrier.
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| A recent increase in solar activity produced a spectacular display over North Pole, AK. |
These
energized particles collide with gas molecules in the atmosphere and transfer
their energy, much like cue balls. But instead of using the energy to move
across a pool table, the gas molecules emit a flash of light, which is the
light we see. We cannot see just one flash; we only see the aurora when there are
millions of flashes.
The
light can be green, red and even blue or purple—the color depends on the gas
molecule. Oxygen molecules emit green and red light, nitrogen emits violet and
blue light, and hydrogen emits red light. Often seen before dawn, blue and
purple aurora is caused by sunlight striking the top of extremely high rays in
the atmosphere. When the aurora is weak it often appears colorless because
there isn’t enough color for our eyes to detect.
The
aurora can extend over a hundred miles into the atmosphere and even though it
may seem to touch the horizon the lowest aurora is 40 miles above Earth’s
surface. Sometimes the rays can be straight overhead or a bright band in the
northern sky. Displays higher in the sky are more common at higher latitudes
while mid-latitudes typically see aurora on the horizon. However, when solar
activity is high, the northern lights can be seen further south, higher in the
sky, and often red (which is less common).
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| A hint of red fringes green arcs of aurora. |
The
northern lights have been extremely active this spring and are predicted to be
more active through 2013 because the solar cycle is at its maximum point. The
11-year solar cycle corresponds to the wax and wane of sunspots, with the
maximum occurring during times of increased sunspot activity and the minimum
occurring during minimal sunspot activity. More sunspots equates to an
increased flow of energized particles carried towards earth on the solar wind.
The few
hours around midnight are the best time to observe northern lights but they can
be seen anytime during the night if they are extremely active. For an auroral
forecast, check the University of Alaska Fairbanks Geophysical Institute’s website
at http://www.gi.alaska.edu/AuroraForecast (there is even an app).
When
the northern lights are swirling across the sky, I find it easy to forget about
the energized particles and gas molecules creating the light and simply enjoy
the show.
Note: Published in the Bonners Ferry Herald on March 29, 2012.



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