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Length of Day

   Also found in: Medical, Acronyms, Wikipedia 0.01 sec.
Length of Day 

the interval of time between sunrise and sunset, during which the sun is above the horizon. The length of day depends upon the geographic latitude of a place and upon the inclination of the sun. At the equator, the length of day is constant and equals 12 hours. In the northern hemisphere, the length of day is more than 12 hours during the positive inclination of the sun (that is, in the spring and summer) and less than 12 hours during the negative inclination of the sun (in the autumn and winter). At the equinoxes (spring and autumn), the day equals the night (if one does not consider refraction) everywhere on the earth. The longest day is the summer solstice and the shortest is the winter solstice. Within the polar circles, the length of day in the summer can exceed 24 hours (the polar day), and at the poles daytime lasts six months.



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Some of the potential challenges of a four-day school week include the length of day for young students, the need to keep students focused during the longer day, child care and supervision of students on the unscheduled day, and the fact that 20 percent more instructional time is lost when a teacher or student misses a day.
It is also important to note that the current difference in the length of day from 86 400 seconds is the accumulation over nearly two centuries, not just the previous year.
The first dial gives the time and the phases of the moon, with shutters in the arch above showing the varying length of day and night.
 
 
 
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