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  2. Daytime - Wikipedia

    en.wikipedia.org/wiki/Daytime

    This phenomenon of more daylight than night is not unique to the poles. In fact, at any given time slightly more than half of the earth is in daylight. The 24 hours of summer daylight is known as the midnight sun that is famous in some northern countries. To the north, the Arctic Circle marks this 23.44° boundary.

  3. Sunrise equation - Wikipedia

    en.wikipedia.org/wiki/Sunrise_equation

    A contour plot of the hours of daylight as a function of latitude and day of the year, using the most accurate models described in this article. It can be seen that the area of constant day and constant night reach up to the polar circles (here labeled "Anta. c." and "Arct. c."), which is a consequence of the earth's inclination.

  4. Polar night - Wikipedia

    en.wikipedia.org/wiki/Polar_night

    Polar night is a phenomenon that occurs in the northernmost and southernmost regions of Earth when the Sun remains below the horizon for more than 24 hours. This only occurs inside the polar circles. [1] The opposite phenomenon, polar day or midnight sun, occurs when the Sun remains above the horizon for more than 24 hours.

  5. 39th parallel north - Wikipedia

    en.wikipedia.org/wiki/39th_parallel_north

    At this latitude the sun is visible for 14 hours, 54 minutes during the summer solstice and 9 hours, 26 minutes during the winter solstice. [1] Daylight along the 39th parallel north falls under 10 hours a day starting on 18 November and returns to over ten hours a day beginning 24 January.

  6. Midnight sun - Wikipedia

    en.wikipedia.org/wiki/Midnight_sun

    As an example, at the North Cape of Norway at midnight on June 21/22, the longitude of 25.9 degrees east makes the moment 103.2 minutes earlier by clock time; but the local time, 2 hours ahead of GMT in the summer, makes it 120 minutes later by clock time. The equation of time at that date is -2.0 minutes.

  7. Sun path - Wikipedia

    en.wikipedia.org/wiki/Sun_path

    All days of the year, solstices included, have the same length of 12 hours. Solstice day arcs as viewed from 20° latitude. The Sun culminates at 46.56° altitude in winter and 93.44° altitude in summer. In this case an angle larger than 90° means that the culmination takes place at an altitude of 86.56° in the opposite cardinal direction.

  8. 44th parallel north - Wikipedia

    en.wikipedia.org/wiki/44th_parallel_north

    The 44th parallel north is a circle of latitude that is 44 degrees north of the Earth's ... the dusk is visible circa 15 hours 29 minutes before the dawn during the ...

  9. 56th parallel north - Wikipedia

    en.wikipedia.org/wiki/56th_parallel_north

    The 56th parallel north is a circle of latitude that is 56 degrees north of the Earth's equatorial plane. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean. At this latitude the sun is visible for 17 hours, 37 minutes during the summer solstice and 6 hours, 57 minutes during the winter solstice. [1]