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This document dispels common myths about the aurora and explains its true causes, as well as providing information about nasa's polar spacecraft and its mission to study the aurora and earth's interaction with the solar wind. It also covers the importance of the aurora, its appearance on other planets, and the patterns and colors of the aurora.
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Auroras are caused by sunlight reflecting off of the polar ice cap.
atmosphere.Auroras are caused by moonlight reflecting off of ice crystals in the
guided by Earth’s magnetic field into the polar atmosphere.Auroras are caused by electrons arriving directly from the Sun and
http://istp.gsfc.nasa.gov/istp/polar
http://www.phy6.org/Education/Intro.html The Aurora Explained http://www.alaskascience.com/aurora.htm Windows to the Universe http://www.windows.ucar.edu/spaceweather/ Mission to Geospace http://istp.gsfc.nasa.gov/istp/outreach
The Northern Light: From Mythology to Space Research. (^) New York: Springer-Verlag, 1983. Michael Carlowicz and Ramon Lopez. (^) Storms from the Sun - The Emerging Science of Space Weather. (^) Washington, DC: The Joseph Henry Press, 2002. Robert Eather. Majestic Lights: The Aurora in Science, History, and the Arts. Washington, DC: AGU, 1980. Sten Odenwald. (^) The 23rd Cycle - Learning to Live with a Stormy Star. (^) New York: Columbia University Press, 2000. Kenny Taylor. Auroras, Earth’s Grand Show of Lights. National Geographic, 200(5), 2001.
Polar Mission, Mail Code 696 Greenbelt, Maryland 20771 Goddard Space Flight Center Space AdministrationNational Aeronautics and
This cavity is called the magnetosphere, and it stretches
NP-2002-5-459-GSFC J.T. Trauger (JPL) and NASA Steele Hill NASA
atmosphere. The electrons
which come from the can emit enough light for the eye to detect.When a large number of these collisions occur, the oxygen and nitrogenemit photons, small bursts of energy in the form of light.“excited.” As they “calm down” and return to their normal state, they- transfer energy to the oxygen and nitrogen gases, making themmagnetosphere, the region of space controlled by Earth’s magnetic field This ghostly light will in the daytime.aurora is much dimmer than sunlight, it cannot be seen from the groundthe light comes from altitudes between 60 and 200 miles. Since theproduce the dance of colors in the night sky we call the aurora. Most of
areas circling the Themagnetic poles of the Earth. rings expand and andin central Canada, Alaska,places to see auroras areauroral activity. The bestcontract with the level of Greenland, northern
Simultaneous ovals are
beingoxygen or nitrogen - isdepends on which gas - The color of the aurora excited by the electrons, and on how excited it becomes. Oxygen produce purples, pinks, and white.light. The blending of these colors can alsolight; nitrogen generally gives off a bluemost familiar color of the aurora) or a redemits either a greenish-yellow light (the The
The shape of the of a single night.atmosphere. Dramatically different shapes can be seen over the courseand on the processes that cause the electrons to precipitate into theaurora depends on the source of the electrons in the magnetosphere Polar/VIS, NASA/U. Iowa Polar/VIS, NASA/U. Iowa Michel Tournay Jan Curtis Jan Curtis Jan Curtis Jan Curtis Jan Curtis Background image: Jan Curtis