Central Middle School - Ceejay Yearbook (Kansas City, MO)

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f'-X llHlli5l!lESlliE!ll?ElIHIQIEEIELEIHIIIEEEHIIEN- KJ Clhe elflidniglit Sun ru.xNCr:s POWELL AND MAXINE KENNEDY, '25 The unusual appearance of the Midnight Sun attracts many visitors to the north- ern countries. In summer there are only three or four hours of darkness and in winter only .three or four hours of daylight. The radiance of the sun varies in intensity de- pending upon the moisture or clearness of the atmosphere, presence of clouds and other factors. One day it will be as red as orange, and so dull in radiance that it can be looked upon with the naked eye. At another time it glows like a live flame. There are, also, days when it is a bluish-white color, like the moon. The most curious thing about the sun is its motion. It does not once hide itself from May 13th to July 29th, while from November 21st to January 21st it is seen but a very few hours. At the North pole every direction is due south. Therefore it is evident that the sun moves round us in a gigantic circle roughly par- allel to the horizon. It gradually ascends in a slow spiral until it grazes the horizon. Next it is cut in half, then only the upper part shows. This disappears, and after a period of twi- light the long Arctic night sets in. Although the sky is no darker than ours at twilight, the long night is relieved by a huge electric light which is kept burning during this season. The beautiful Aurora Borealis, too, lights up the winter sky with its streamers of light. The path of light usually forms a fiery arch across the northern sky, with its streams of light ascending from a line of haze or cloud, sometimes to a point almost directly over- head. Its rays are transient and constantly in motion, varying in color from a greenish hue or a pale yellow to a deep, blood red, and its shapes are infinite in num- ber. These auroras are caused by the passage of electricity through the rarified upper atmosphere. A similar effect is produced by passing electrical currents through rari- fied air or gases. During the appearance of an aurora the magnetic needle is subject to disturbance, showing a close connection between the aurora and magnetism. The aurora australis is the corresponding light seen in the southern hemisphere. The return of spring is just the reverse of that of winter-Hrst, the twilight, then a faint rim of light crawling round the edge of the land- scape, making complete circles, until finally it is day. When this summer sun does smile upon the Northland, all life quickly responds. Plants sometimes grow three inches in a day. Vege- tables and fruits mature in six weeks. Flowers do not close in sleep and birds fly all night upon their way. Directions in these Northern coun- tries are quite as confusing as the time of day. To see the sun in the north at midnight, watch it ascend Without having dipped out of sight, and t circle about in the heavens through the day, is bewildering to one accustomed to see it rise in the east and set in the west. Note the two illustrations. In the Summer the sun is continually rising, never ' k' lehind the earth while in winter it rises above the horizon only as high as sin ing J L I , , the lowest point during the summer. then sinking out of sight behind the earth. Photos by Lomen Bros, Nome, Alaska. 1'lf.' ZIfI.L.'.5'.'.. ZZ'TfI'f . Ell!Ei'l!?'IIEll5Sii'I!!lIi5.K' 512HiEfi!III5EHIEii!E-'?lilE!E5ZI'.iiliQi5lSlii!!l l 9. .il2'l54l3l?F'l.El'!alhi nll59,!l nl!-.ll29'l-Jil I el-r Przyr' ow 11,.m1f.- 1 ow.:

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