7 August, 2000
August 7 , 2000
Matanuska Glacier, Alaska
Today has been an absolutely beautiful day here with sunny skies and
warm temperatures. Unfortunately the work for the day was to analyze the
samples collected yesterday. It would have been a good day to be out on
the ice and not stuck in camp. At any rate we got good results once
again and it allows us to compare what’s going on during high and low
flow. Our only other experiment that successfully yielded data for both
M-1 and Mega Vent simultaneously was Dye Experiment #4. In both
experiments the dye appears at Mega Vent just before arriving at M-1
despite the fact that M-1 is actually closer to the moulin. It also
turns out that the concentrations at M-1 are always lower than those at
Mega Vent. We are discussing possible explanations for these results.
Late last night the sky cleared up and I again watched for a possible
display of the Northern Lights. And once again I had to go to sleep
disappointed that there was no show. It was still an enjoyable evening
to be out and for the first time I was able to see the Big Dipper in the
sky. As I expected it was much higher in the sky than what I’m used to
at home due to the tilt of the earth and the more northern latitude. I
had been wondering for about a week whether or not a certain bright star
in the north was the North Star. I doubted that it was because it seemed
too low in the sky. But I thought perhaps the Talkeetna Mountains to the
north gave the illusion of the star being low. With the Dipper as a
reference I was able to see that this bright star was not the North
Star. The North Star was actually very high in the sky. I also noticed
numerous satellites zooming by as well.
The Northern Lights are also known as the Aurora Borealis, a name first
used by Galileo in 1619 to suggest the likeness to an early dawn in the
northern sky. He wrongly thought that the aurora was caused by sunlight
reflecting from the high atmosphere. It is actually a light source
created high in the atmosphere. It is a glow given off by the atoms and
molecules when they are struck by charged parcticles, mostly electrons
and protons, that originate on the sun. Moving charged parcticles are
deflected by magnetic fields and the earth’s field tends to guide these
parcticles toward the poles where they enter the atmosphere and make it
glow. For this reason the displays are more common near the polar
regions. In the southern hemisphere this glow is called the Southern
Lights or Aurora Australis.
There are many familiar examples of light being produced by the flow of
charged parcticles through gases. Lightning or sparks from static
electricity discharges are simple, natural examples of this.
Fluorescent and neon lights give off their light when electricity
(electron flow) passes through the gas filled tubes. A television set
works because electrons are guided toward certain locations on the TV
screen where they cause substances in the screen called phosphors to
glow. The picture tube has plates in the back that produce changing
magnetic fields which cause the path of the electrons to change as well.
The result is the constantly changing scene on the TV screen. If you
have a black and white TV just pass a magnet over the surface of the
screen and watch what happens. DO NOT try this on a color set or
computer monitor as it can cause permanent damage to the color display.
I have seen the Northern Lights on two occasions in my lifetime. Several
years ago I watched them in the Boundary Waters Canoe Area in northern
Minnesota. I also happened to see them at home in Indiana one early
evening a few years ago. I’m still hopeful that one of these remaining
nights will offer an opportunity to watch this amazing phenomenon.
Marvin Giesting
Beautiful sunny mornings such as today provide great views up Glacier Creek directly across from camp.
Graph comparing the results of a low flow test (Experiment 4) and high flow (Experiment 6). The interesting things we see are that: dye appears at Mega Vent before M-1 in spite of being farther from the moulin; concentrations at Mega are always higher than M-1; dye appears more quickly at high flow; and concentrations are lower at high flow. Some of this is simple to interpret but it also raises questions too. The area under each curve is an approximation of the amount of dye that passes through. At high flow where does a lot of the dye go? Apparently we've answered a question we had earlier as to whether or not other conduits are filled when the water rises.
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