Solar Noon Calculator

Calculate the exact time of solar noon, sunrise, sunset, and day length for any location and date. Includes equation of time, solar declination, and twilight times.

Solar Noon
11:53 AM
Sun at highest point
Sunrise
5:03 AM
Civil dawn: 4:29 AM
Sunset
6:44 PM
Civil dusk: 7:18 PM
Day Length
13h 41m
Sunrise to sunset
Eq. of Time
+2.6 min
Sundial correction
Solar Declination
14.27°
Northern

Day/Night Breakdown

13.7h daylight
10.3h night

Monthly Solar Data

MonthSolar NoonDay LengthDeclinationEoT (min)
Jan12:05 PM9h 23m-21.3°-9.3
Feb12:11 PM10h 26m-13.3°-14.6
Mar12:06 PM11h 41m-2.8°-9.7
Apr11:56 AM13h 6m9.4°-0.2
May11:52 AM14h 16m18.8°+3.8
Jun11:56 AM14h 54m23.3°-0.2
Jul12:02 PM14h 39m21.5°-5.6
Aug12:00 PM13h 37m13.8°-4.2
Sep11:51 AM12h 15m2.2°+5.5
Oct11:41 AM10h 53m-9.6°+14.9
Nov11:41 AM9h 41m-19.1°+14.9
Dec11:52 AM9h 6m-23.3°+4.2
Planning notes, formulas, and examples

About the Solar Noon Calculator

The Solar Noon Calculator finds the moment when the sun reaches its highest point for a given location and date.

Solar noon is not the same as 12:00 PM on the clock. It shifts with longitude, time zone choice, and the equation of time, so the local solar peak can fall before or after noon by several minutes. The calculator also reports sunrise, sunset, twilight, day length, and solar declination so you can see the full daylight window around that point.

That makes it useful whenever you need both the daily solar peak and the surrounding daylight times in one place.

When This Page Helps

Solar noon is the anchor point for a lot of daylight planning. Once you know where that peak lands, sunrise, sunset, and twilight are easier to interpret for photography, solar work, and general daylight planning.

How to Use the Inputs

  1. Enter your latitude and longitude (or use a city preset).
  2. Set the UTC timezone offset for your location.
  3. Select a date or leave as today's date.
  4. View solar noon, sunrise, sunset, and day length.
  5. Check twilight times and the equation of time correction.
  6. Explore how solar noon shifts throughout the year in the annual table.
Formula used
Solar Noon = 12:00 - Longitude/15 + Timezone - EoT/60. Equation of Time (EoT) uses the Spencer formula. Solar Declination = 23.45° × sin(360/365 × (284 + day_of_year)). Sunrise/Sunset Hour Angle = acos(-tan(lat) × tan(declination)).

Example Calculation

Result: Solar noon: 12:58 PM, Sunrise: 5:25 AM, Sunset: 8:31 PM

New York City on the summer solstice. Solar noon is 12:58 PM (not exactly noon) because NYC is west of its timezone center. Day length: 15h 6m — the longest day of the year.

Tips & Best Practices

  • Solar noon is latest (~12:45-1:05 PM) on the western edges of time zones.
  • The longest day of the year is the summer solstice (~June 21 in Northern Hemisphere).
  • Earliest sunrise doesn't coincide with the solstice — it's typically a week earlier.
  • The analemma (figure-8 of sun positions at noon) is caused by the equation of time.
  • At the equator, day length varies only ±15 minutes throughout the year.

The Equation of Time

The equation of time has two components: (1) the eccentricity of Earth's orbit causes the sun to appear to speed up and slow down relative to a perfect clock, and (2) the obliquity (tilt) of the ecliptic causes the sun's apparent motion along the celestial equator to be non-uniform even if Earth's orbit were perfectly circular.

These two effects combine to create the familiar figure-8 analemma. The maximum deviation is about +14 minutes in early February (sundial runs fast) and -16 minutes in early November (sundial runs slow).

Seasonal Daylight Patterns

At the equator, day length is nearly constant at 12 hours year-round. With increasing latitude, seasonal variation grows dramatically. At 45°N, the longest day is about 15.5 hours and the shortest about 8.5 hours. At the Arctic Circle (66.5°N), the sun doesn't set for at least one day at the summer solstice and doesn't rise for at least one day at the winter solstice.

Practical Applications

Solar panel installers use solar noon to determine the optimal azimuth (south-facing in the Northern Hemisphere). Solar declination determines the optimal tilt angle. Farmers and gardeners use day length to plan planting. Astronomers need astronomical twilight times to plan observations. And sundial enthusiasts need the equation of time to convert sundial readings to clock time.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • Two reasons: (1) Your longitude within the time zone — time zones span 15° but use a single clock time, so locations east of the zone center see solar noon earlier than noon. (2) The equation of time — Earth's orbital eccentricity and axial tilt cause solar time to deviate from clock time by up to ±16 minutes.