Sunrise Sunset Calculator

–sunrise, solar noon and sunset in your browser’s timezone
LatitudeMar 20Jun 21Sep 22Dec 21
-60°12h 13m5h 52m12h 12m18h 52m
-40°12h 08m9h 19m12h 08m15h 01m
-20°12h 07m10h 55m12h 07m13h 20m
0°12h 07m12h 07m12h 07m12h 07m
20°12h 07m13h 20m12h 07m10h 55m
40°12h 09m15h 01m12h 09m9h 19m
60°12h 14m18h 52m12h 15m5h 52m
70°12h 21mpolar12h 22mpolar
The computation is the NOAA sunrise equation (the compact form behind NOAA GML’s Solar Calculator): Julian cycle, equation of center, solar declination, then the -0.833° zenith that bakes in atmospheric refraction and the solar disc’s radius. Times render in your browser’s own timezone from the longitude you enter. Almanacs add a few minutes of local terrain and weather correction - expect agreement within a couple of minutes. Bottom line: at the equinoxes, day length is ~12 hours everywhere on Earth (the tables above prove it from -60° to +70°), and the poles break the math entirely - enter latitude 70 in June and the Sun simply never sets. Day-length cousin: daylight hours calculator; golden light golden hour calculator; the clock shift DST dates table; burning risk UV index table.

Sunrise and sunset are pure geometry: your latitude, the date, and the Sun’s declination. This calculator runs the NOAA sunrise equation live - Julian cycle, equation of center, solar declination, and the standard -0.833° zenith that accounts for refraction and the solar disc - and renders the times in your browser’s own timezone.

The latitude table shows the underlying pattern across the year: equinox days are ~12 hours everywhere on Earth, while June and December swing wildly with latitude until the poles break the math entirely.

How to use

  1. Enter latitude and longitude (south and west are negative), pick a date - times appear in your local timezone.
  2. Use the city chips for quick checks; the table below compares day lengths at eight latitudes across the four seasonal markers.
  3. Enter latitude 66+ in June or December to see the polar-night and midnight-sun cases detected honestly.

Frequently asked questions

Why are the times a couple of minutes off my almanac?

NOAA’s own calculator warns the same: the equation computes the geometric event, while printed almanacs layer local terrain, pressure and temperature corrections on top. Expect agreement within a couple of minutes - closer than any watch-based rule.

What is solar noon and why is it not 12:00?

Solar noon is when the Sun crosses your meridian - the true midpoint of daylight. It drifts from 12:00 clock time because of your offset within your timezone and the equation of time: cities at the eastern edge of a timezone see solar noon well before noon.

What does the -0.833 degree zenith mean?

Sunrise is defined when the Sun’s upper edge appears, and atmospheric refraction lifts it about 0.57° visually. Using a zenith of 90.833° instead of 90° folds both effects into the equation - the convention every almanac shares.

When does the calculator return “no sunrise” or “no sunset”?

Polar night and midnight sun: above the Arctic or Antarctic circles at the solstices, the cosine term leaves its valid range and the Sun either never rises or never sets. The tool reports those cases honestly instead of returning nonsense times.

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