If youre camping near the United States/Canada border or points farther north, you might see an eerie glow in the night sky. Sometimes it can look like twilight. At other times it can look like a glowing, dancing ribbon of light. The light may be green, red, blue or a combination of these colors. What you are seeing is called the aurora borealis, or simply an aurora. Auroras have signified different things to different cultures. The Vikings thought that auroras were reflections off the armor of the mythical Valkyries. To the native Eskimos of Greenland and nearby Canada, auroras were communications from the dead. To American Indians, they were lights from huge campfires far to the north. In medieval times, auroras were omens of war or disasters, such as plague. Today, we know that theyre a light phenomenon caused by high-energy particles from the suns solar winds interacting with the Earths magnetic field. However, knowing the physical reason for auroras certainly doesnt detract from these beautiful natural light shows. Because auroras are caused by the interaction of solar winds with the Earths magnetic field, you can see them most often near the poles, both north and south. In the north, theyre called aurora borealis, or Northern Lights. Aurora is the name of the Roman goddess of the dawn, and boreal means north in Latin. In the southern hemisphere, auroras are called aurora australis (Latin for south). Auroras follow solar cycles and tend to be more frequent in the late autumn and early spring (October, February and March are the best months for seeing them). Around the Arctic Circle in northern Norway and Alaska, you can see them almost nightly. As you travel south, their frequency diminishes. Around southern Alaska, southern Norway, Scotland and the United Kingdom, they might show up about one to 10 times per month. Near the United States/Canada border, you may see them two to four times a year. Once or twice a century, they might pop up in the southern United States, Mexico and the equatorial regions.
Posted on: Wed, 23 Oct 2013 16:29:27 +0000
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