The Earth, as seen by the Apollo 17 astronauts. © NASA

December solstice

Dominic Ford, Editor
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22 December will be the shortest day of 1987 in the northern hemisphere, midwinter day.

This is the day when the Sun's annual journey through the constellations of the zodiac reaches its most southerly point in the sky, in the constellation of Capricornus at a declination of 23.5°S. This day is counted by astronomers to be the first day of winter in the northern hemisphere.

In the southern hemisphere, the Sun is above the horizon for longer than on any other day of the year, and astronomers define this to be the first day of summer.

At the solstice, the Sun appears overhead at noon when observed from locations on the tropic of Capricorn, at a latitude 23.5°S.

Date Sunrise Noon Sunset
24Nov07:2112:2117:20
28Nov07:2512:2217:19
02Dec07:2912:2417:18
06Dec07:3312:2517:18
10Dec07:3612:2717:18
14Dec07:3912:2917:19
18Dec07:4212:3117:20
22Dec07:4412:3317:22
26Dec07:4612:3517:24
30Dec07:4712:3717:27
03Jan07:4712:3917:30
07Jan07:4812:4017:34
11Jan07:4712:4217:37
15Jan07:4612:4417:41
Sunrise and sunset times for Washington
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Sunrise and sunset times

The table to the right lists the sunrise and sunset times in Washington around the solstice. At this time of year, noon – the moment when the Sun appears highest in the sky – moves around a minute later each day.

This phenomenon is described by the equation of time, and is caused by slight variations in the length of each day depending on the time of year.

In some months, days can be up to 20 seconds longer or shorter than 24 hours, in a predictable pattern which repeats every year. This arises from two effects:

  1. The rate of the Sun's eastward movement through the constellations changes over the course of the year. It is fastest at the solstices, and slowest at the equinoxes.
  2. The Earth's orbit around the Sun is not a perfect circle, but is slightly elliptical. This means that its orbital speed changes through the year.

Both these effects very slightly alter the rate of movement of the Sun across the sky, adding or subtracting a few seconds from the time it takes to get from noon on one day to noon the next day.

Clocks, however, continue to run at a constant rate at all times of year. This means that, at those times of year when days are shorter than 24 hours, noon drifts earlier in the day. When days are longer than 24 hours, the noon comes later each day.

In December, each solar day lasts fractionally longer than 24 hours, and so the time of noon moves around a minute later each day.

The shift also affects sunrise and sunset times, and means that the latest sunrise and earliest sunset do not occur on the day of the solstice itself. Instead, the earliest sunset occurs a couple of weeks beforehand, and the latest sunrise is a couple of weeks later.

Solstice geometry

Solstices occur because the axis of the Earth's spin – its polar axis – is tilted at an angle of 23.5° to the plane of its orbit around the Sun.

The direction of the Earth's spin axis remains fixed in space as it circles around the Sun, while the Earth's sight line to the Sun moves through the constellations of the zodiac. As a result, sometimes the Earth's north pole is tilted towards the Sun (in June), and at other times it is tilted away from it (in December). This gives rise to the Earth's seasons:

The origin of the Earth's seasons

The date of the solstice

Year Time of solstice
198322 Dec 03:23 MST
198421 Dec 09:17 MST
198521 Dec 15:03 MST
198621 Dec 21:00 MST
198722 Dec 02:46 MST
198821 Dec 08:30 MST
198921 Dec 14:26 MST
199021 Dec 20:12 MST
199122 Dec 02:00 MST

The Earth orbits the Sun once every 365.242 days, and this is the time period over which the cycle of solstices and equinoxes, and consequently all the Earth's seasons, repeat from one year to the next.

In any year which is not a leap year, the solstices occur roughly 5 hours and 48 minutes – just under a quarter of a day – later from one year to the next.

This is why the seasons would drift later in the year if it was not for an additional day being inserted inserted into every fourth year on 29 February.

The chart below shows the time when the December solstice falls in each year. The gradual drift of the four-year cycle earlier in the month is due to the equinoxes repeating 12 minutes less than a quarter of a day later each year.

In the Gregorian calendar, this is fixed by omitting leap years in three out of every four century years, e.g. 1700, 1800 and 1900, but not 2000.

The date of Christmas

Christmas borrows its date from ancient pagan midwinter festivals, even though in the modern calendar Christmas now falls a few days after astronomical midwinter.

This anomaly has come about because the system of leap days which are sometimes inserted into our calendar on February 29 was only refined to its present form by the Gregorian calendar reforms of the 16th century. Before this, the average length of each year did not quite match the period of time with which the seasons repeat – 365.2422 days – and so the seasons drifted through the year by a small amount each century. So, in the distant past, the winter solstice occurred a few days later than it does today.

The 1987 solstice

The exact position of the Sun when it reaches its most southerly declination in 1987 will be (J2000.0 coordinates):

Object Right Ascension Declination Constellation Angular Size
Sun 18h00m 23°26'S Sagittarius 32'31"

The sky on 28 Mar 2024

The sky on 28 March 2024
Sunrise
07:22
Sunset
19:52
Twilight ends
21:21
Twilight begins
05:54

18-day old moon
Waning Gibbous

87%

18 days old

Planets
Rise Culm. Set
Mercury 07:55 14:38 21:20
Venus 06:47 12:34 18:22
Moon 22:26 03:44 08:54
Mars 06:04 11:33 17:02
Jupiter 09:10 16:03 22:56
Saturn 06:29 12:06 17:44
All times shown in MDT.

Source

The circumstances of this event were computed using the DE430 planetary ephemeris published by the Jet Propulsion Laboratory (JPL).

This event was automatically generated by searching the ephemeris for planetary alignments which are of interest to amateur astronomers, and the text above was generated based on an estimate of your location.

Image credit

The Earth, as seen by the Apollo 17 astronauts. © NASA

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Washington

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Longitude:
Timezone:

37.13°N
113.51°W
MDT

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