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Aubrey Weese
Explaining Science Using Examples - Final Revision
Changes in the magnetic field of the sun affect us here on earth in a number
of interesting ways. This
For example, the aurora borealis, or "Northern Lights" we see in the sky
are much brighter during a solar maximum. They are also more spread out over
the sky. In normal years the northern lights can only be seen
Another example of the way the sun interacts with the earth is solar flares.
Remember that sunspots occur when magnetic field lines are twisted below
the surface of the sun, well, solar flares occur when magnetic field lines
are twisted above the surface of the sun. Solar flares are huge explosions
on the surface of the sun that occur near sunspots. They can release as much
energy as a billion megatons of TNT.
A third example of how the sunspot cycle effects the earth is more interesting, but also more controversial. Scientists have found that the 11-year solar cycle isn't the same every time. The sun goes through this cycle like a pendulum, but the pendulum is an unstable one. Sometimes the pendulum can "overshoot" and throw things out of whack, causing there to be long periods where solar maximums are very violent, or are very calm. The most well known example of this is the "Maunder Minimum," which occurred from 1645 to 1715. It was a 50 year where period there are almost no sunspots at all, even during solar maximum. This period is called "the quiet sun." The interesting thing is, during this Maunder Minimum, the average temperature of the earth went down, glaciers advanced, and we had a "little ice age." New England had summertime frosts, the Thames River froze abruptly in London, and there was no aurora borealis in the sky at all. The pendulum can also swing the other way, such as during the 11th and 12th centuries, when we had a long period of an overly active sun. And, interestingly, during this period, the average temperature of the earth went up. Much of the northern cool areas thawed, which was probably was a factor in the Vikings being able to find and inhabit Greenland.
The Maunder Minimum and other periods like it were verified by looking at
tree rings. A radioactive isotope of carbon, Carbon 14, is formed in the
earth's atmosphere when it is struck by cosmic rays from the sun. When the
sun's magnetic field is strong (during a solar maximum), less cosmic rays
strike the earth, and when it is weak (during a solar minimum), many cosmic
rays strike the earth. Trees record in their rings how much carbon 14 is
in the atmosphere, and during the Maunder Minimum
Thus, there seems to be a link between the sunspot cycle and the climate of the earth, with solar minimum bringing cooler temperatures and solar maximum bringing warmer ones. This, plus the beautiful displays of northern lights, and the threatening danger of solar flares, are just three ways we are effected by the solar cycle of the sun.
References for information and pictures Solar Physics. Hathaway, David H. NASA. March 17, 2000. Sunspots as Predictors. Younce, Matthew Wiley. The Sun-Earth Connection. NASA/GSFC. USB/S Introducing the Aurora. Terry, Kathee and Anderson, Hugh. July 12, 1999.
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