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  2. Polar alignment - Wikipedia

    en.wikipedia.org/wiki/Polar_alignment

    In the Northern Hemisphere, rough alignment can be done by visually aligning the axis of the telescope mount with Polaris.In the Southern hemisphere or places where Polaris is not visible, a rough alignment can be performed by ensuring the mount is level, adjusting the latitude adjustment pointer to match the observer's latitude, and aligning the axis of the mount with true south or north by ...

  3. Campbell–Stokes recorder - Wikipedia

    en.wikipedia.org/wiki/Campbell–Stokes_recorder

    The unit is designed to record how many hours of bright sunshine were experienced on a given day. A Campbell–Stokes sunshine recorder. This basic unit is still in use today with very little change. It is widely used outside the United States (the Marvin sunshine recorder is generally the instrument used by the U.S. National Weather Service).

  4. Sidereal time - Wikipedia

    en.wikipedia.org/wiki/Sidereal_time

    A year has about 365.24 solar days but 366.24 sidereal days. Therefore, there is one fewer solar day per year than there are sidereal days, similar to an observation of the coin rotation paradox. [5] This makes a sidereal day approximately ⁠ 365.24 / 366.24 ⁠ times the length of the 24-hour solar day.

  5. Six planets align in the sky on June 3: Where, how to see it

    www.aol.com/six-planets-align-sky-june-070015219...

    Those who end up missing this month's event have three more times to catch a major alignment in the next year. Six planets will align again on Aug. 28, Jan. 18., 2025 and Aug. 29, 2025. Seven ...

  6. Celestial navigation - Wikipedia

    en.wikipedia.org/wiki/Celestial_navigation

    The calculation of noon can be made more easily and accurately with a small, exactly vertical rod driven into level ground—take the time reading when the shadow is pointing due north (in the northern hemisphere). Then take your local time reading and subtract it from GMT (Greenwich Mean Time), or the time in London, England. For example, a ...

  7. Magnetic declination - Wikipedia

    en.wikipedia.org/wiki/Magnetic_declination

    In the northern hemisphere, declination can therefore be approximately determined as the difference between the magnetic bearing and a visual bearing on Polaris. Polaris currently traces a circle 0.73° in radius around the north celestial pole, so this technique is accurate to within a degree.

  8. Equinox - Wikipedia

    en.wikipedia.org/wiki/Equinox

    In the Northern Hemisphere, the March equinox is called the vernal or spring equinox while the September equinox is called the autumnal or fall equinox. In the Southern Hemisphere, the reverse is true. During the year, equinoxes alternate with solstices. Leap years and other factors cause the dates of both events to vary slightly. [6]

  9. A rare five-planet alignment will be visible in the sky this ...

    www.aol.com/5-planets-form-rare-alignment...

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