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Solar Insolation by Latitude

Sun-hours above the atmosphere and day length for any latitude and month: 8.8 sun-hours and 14.8 h of daylight at 40°N in June. Not peak sun hours. How it works

Use the Solar Insolation by Latitude

Range: -90° (South Pole) to 90° (North Pole). Positive for Northern hemisphere.

Top-of-atmosphere sun-hours
8.8 hours/day
Latitude 40.0° · Month June

For latitude 40.0° in June

Daylight, sunrise to sunset: 14.8 hours

Not peak sun hours. This is sunlight above the atmosphere in hours at the solar constant; the ground receives less.

Monthly top-of-atmosphere sun-hours at 40.0° latitude

0612JFMAMJJASOND
MonthSun-hours (hrs/day)Daylight (hrs)
January2.99.5
February4.010.5
March5.511.7
April7.113.1
May8.314.2
June8.814.8
July8.514.5
August7.613.5
September6.112.2
October4.510.9
November3.29.7
December2.79.2

Daylight is astronomical day length, 2 × sunset hour angle ÷ 15° per hour, from sunrise to sunset for a point sun. It is not hours of sunshine, and it ignores refraction and cloud.

The figure is the sun's daily energy above the atmosphere, in hours at the solar constant, with a fixed sun-distance factor (the Earth-Sun distance changes it by about 3% through the year). Clouds, haze, air mass and shading reduce the energy that reaches the ground, so this figure is not a sizing value for solar arrays or battery systems. Use a site-specific irradiance dataset for that.

About the Solar Insolation by Latitude

At 40°N the top-of-atmosphere sun-hours are 8.8 hours a day in June and 2.7 in December, and the day from sunrise to sunset lasts 14.8 hours in June and 9.2 in December. The sun-hours figure is the sun’s daily energy on a flat surface above the atmosphere, counted in hours of full-strength sun (the solar constant) shining straight down. It is not peak sun hours and not what a panel on the ground receives, so do not use it to size an array or a battery bank.

Top-of-atmosphere sun-hours (hours a day) by month and latitude

Month0°25°N40°N50°N60°N
January7.14.72.91.70.6
February7.45.64.02.91.6
March7.66.75.54.53.3
April7.57.77.16.45.6
May7.28.38.38.07.6
June7.08.58.88.78.6
July7.18.48.58.48.2
August7.48.07.67.16.5
September7.67.16.15.24.2
October7.56.04.53.42.1
November7.25.03.22.00.9
December7.04.52.71.50.4

The values the page shows, to one decimal. They are sunlight above the atmosphere, not on the ground. A Southern Hemisphere latitude mirrors the seasons: −40° in December gives 8.8 and in June 2.7.

Day length, sunrise to sunset (hours) by month and latitude

Month0°25°N40°N50°N60°N
January12.010.69.58.36.3
February12.011.210.59.88.8
March12.011.811.711.611.3
April12.012.613.113.514.2
May12.013.214.215.216.8
June12.013.514.816.118.3
July12.013.414.515.717.6
August12.012.913.514.215.3
September12.012.112.212.312.4
October12.011.410.910.49.6
November12.010.89.78.77.1
December12.010.59.27.95.6

Astronomical day length for a point sun, 2 × sunset hour angle ÷ 15° per hour, on the same day per month. Refraction and the width of the sun’s disc make a real day a little longer, and it says nothing about cloud.

How to use this tool

  1. Type a latitude from −90 to 90, positive for the Northern Hemisphere. The page starts at 40.
  2. Choose a month. The page starts at June.
  3. Read the sun-hours and the day length for that month, then the chart and the table of all twelve months at the same latitude.

Frequently asked questions

Is this the same as peak sun hours?
No. Peak sun hours describe energy on the ground: a day with 1 kWh/m² is about one peak sun hour, and a Department of Energy slide notes that kWh/m² is sometimes called a sun-hour. This page works above the atmosphere, and clouds, haze and shading cut what reaches a roof. For ground-level figures at a US location, NREL’s PVWatts calculator draws on measured solar resource data for the address you enter.
Why is the equator about 7 hours all year?
Day and night at the equator are each about 12 hours in every month, and the noon sun is never more than about 23° from overhead, so the daily total changes little. The page gives 7.6 in March and September and 7.0 in June and December at 0°.
Why does 60°N get more sun-hours than the equator in June?
The June day at 60°N is far longer than 12 hours, and the extra hours outweigh the lower sun. The page gives 8.6 at 60°N in June against 7.0 at 0°. In December the same latitude drops to 0.4, because the sun is up for a short time and stays close to the horizon.
What happens near the poles?
The formula limits the sunset hour angle in polar night and midnight sun. At 90°N it gives 9.4 hours in June and 0 in December; at 70°N it gives 8.8 in June and 0 in December. Latitude must be from −90 to 90.
Does it work for the Southern Hemisphere?
Yes. Enter a negative latitude. At −40° the page gives 8.8 hours in December and 2.7 in June, the mirror of 40°N, because the seasons are reversed.
How many hours of daylight are there at my latitude?
The page shows the day length beside the sun-hours: twice the sunset hour angle, at 15° per hour. At 40°N that is 14.8 hours in June and 9.2 in December; at 60°N, 18.3 and 5.6; at the equator 12.0 all year. It is the time the sun is above the horizon, not hours of sunshine.

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