70°N · December 21 — noon altitude -3.44°, daylight 0 h 0 min (Polar night)
At 70°N · December 21 the noon sun stands -3.44° above the horizon and the day runs 0 h 0 min (Polar night). That altitude is 90° − |latitude − declination| with a declination of -23.44° for the date, and the times are apparent solar time — no refraction, no equation of time.
- Latitude
- 70°N
- Date
- December 21 · December solstice
- Day of the year
- 355
- Declination
- -23.44°
- Noon altitude
- -3.44°
- Sun at noon
- To the south
- Length of day
- 0 h 0 min (Polar night)
- Sunrise and sunset
- Polar night
- Half-day angle
- 0°
- Shadow of a 1 m pole
- none
Times are apparent solar time, with noon set to 12:00 when the sun crosses the meridian.
A shadow is the tangent of the altitude, read backwards
If the noon altitude is h, a pole 1 m tall casts 1 ÷ tan h metres of shadow. Measure the shadow instead and the altitude falls out, and from the altitude you can work back to a date or a latitude — that is how Eratosthenes measured the earth in antiquity. Shadows stretch fast as the sun drops: at 45° the shadow equals the height, at 30° it is 1.7 times as long, and at 5° more than eleven times.
- 1 m ÷ tan -3.44°none
What this leaves out
Sunrise here means the centre of the sun crossing the geometric horizon, an altitude of 0°. The usual convention adds refraction and the sun’s own radius and uses −0.833°, which makes the day 8 to 10 minutes longer at mid-latitudes. The clock is apparent solar time: to reach civil time you still have to add the equation of time (±16 minutes), the gap between your longitude and your time zone, and any summer time. The declination formula carries an error of up to 1.5°, leap years are not counted, so dates after February sit one day out, and neither the observer’s elevation nor hills and buildings on the horizon are in here.
A high sun is a strong sun
The higher the sun, the less air its light passes through, and the stronger the ultraviolet. As a rule of thumb, when your shadow is shorter than you are, the ultraviolet is near its peak for the day — how long skin lasts before it reddens depends on the index and the skin type.
See burn times by UV indexNearby cells
Same latitude, other dates
Same date, other latitudes
Worth knowing
- Declination δ = 23.44° × sin(360° × (284 + N) ÷ 365), where N counts the days from 1 January.
- Noon altitude = 90° − |latitude − declination|; at the June solstice that is 90° − φ + 23.44° in the north.
- Length of day = 2H ÷ 15 hours with cos H = −tan(latitude) × tan(declination); beyond |cos H| = 1 lies polar day or night.
- Shadow = height ÷ tan(altitude). Times are apparent solar time, with refraction and the equation of time left out.
Common questions
Q. How high is the noon sun at 70°N · December 21?
-3.44° above the horizon. That is 90° − |latitude − declination|, with a declination of -23.44° that day, and the day itself runs 0 h 0 min (Polar night).
Q. How long is the day at 70°N · December 21?
0 h 0 min (Polar night). There are no sunrise or sunset times to give — the sun does not cross the horizon that day.
Q. How long is the noon shadow?
There is none: even at noon the sun stays below the horizon, and the noon altitude is -3.44°.