Solstice Calculator

Find the exact dates of summer and winter solstices for any year.

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What is a Solstice?

A solstice occurs when the Sun reaches its highest or lowest point in the sky at noon, resulting in the longest or shortest day of the year. The June solstice marks the beginning of summer in the Northern Hemisphere, while December solstice marks winter.

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June Solstice 2026

Sunday, June 21, 2026
08:51 UTC
Past
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December Solstice 2026

Monday, December 21, 2026
20:53 UTC
157 days away

Solstice Facts

Northern Hemisphere
June = Summer Solstice (longest day)
December = Winter Solstice (shortest day)
Southern Hemisphere
June = Winter Solstice (shortest day)
December = Summer Solstice (longest day)
Approximate Daylight (45 N)
June: ~16 hours 30 minutes
December: ~8 hours 30 minutes

What Is a Solstice?

A solstice is one of the two moments each year when Earth's rotational axis is tilted most directly toward or away from the Sun, causing that hemisphere to experience its longest or shortest day of the year. The word comes from the Latin solstitium — sol (sun) + sistere (to stop) — referring to the sun's apparent pause at its extreme northern or southern position before reversing direction.

The June solstice (typically June 20–21) marks the moment when the Northern Hemisphere is tilted most directly toward the Sun. The North Pole experiences 24 hours of sunlight; locations above the Arctic Circle (66.5°N) see the midnight sun. For the Northern Hemisphere, this is the summer solstice — the longest day of the year. For the Southern Hemisphere, it is the winter solstice.

The December solstice (typically December 21–22) is the reverse: the Southern Hemisphere tilts toward the Sun, creating the Northern Hemisphere's winter solstice (shortest day) and the Southern Hemisphere's summer solstice (longest day). The South Pole experiences continuous sunlight while regions north of the Arctic Circle are in polar night.

This calculator uses the Meeus polynomial algorithm to compute precise Julian Day Ephemeris (JDE) values for both solstices in any year from 1 CE to 9999, then converts to Gregorian calendar dates and UTC times.

Solstice Calculation Formula (Meeus Algorithm)

The solstice dates are computed using polynomial expressions that approximate the Julian Day of each solstice, based on Jean Meeus's Astronomical Algorithms.

June Solstice JDE

JDE₀ = 2451716.56767 + 365242.37391·Y + 0.05259·Y² − 0.00159·Y³

Where:

  • JDE₀= Julian Day Ephemeris of the June solstice
  • Y= (year − 2000) / 1000 — centuries from J2000.0 epoch, scaled to millennia
  • December solstice= JDE₀ = 2451900.05952 + 365242.74049·Y − 0.06223·Y² + 0.00823·Y³
  • jdeToDate= Standard Julian Day to Gregorian calendar conversion algorithm (Meeus Chapter 7)

Season Lengths and Perihelion

The four astronomical seasons are defined by the equinoxes and solstices, but they are not equal in length. Earth moves faster through its orbit when closer to the Sun (perihelion, early January) and slower when farther away (aphelion, early July). This causes Northern Hemisphere summer (spring equinox to autumn equinox, ~186 days) to be longer than Northern Hemisphere winter (~179 days).

Season (Northern Hemisphere) Duration Bounded By
Spring~92.8 daysMarch equinox → June solstice
Summer~93.6 daysJune solstice → September equinox
Autumn~89.8 daysSeptember equinox → December solstice
Winter~89.0 daysDecember solstice → March equinox

How to Use This Calculator

  1. Enter a Year: Type any year from 1 to 9999.
  2. View Solstice Dates: Both the June and December solstice dates are shown with their exact UTC times.
  3. Use Navigation: Previous/Next buttons step through years for quick multi-year comparison.

Cultural and Scientific Significance

Solstices have been central to human culture for millennia. Stonehenge is precisely aligned with the midsummer sunrise; Newgrange in Ireland with the midwinter sunrise. The ancient Egyptians, Maya, Inca, Chinese, and virtually every agricultural civilization marked solstices with festivals, rituals, and calendrical records because they provided reliable anchors for planting and harvest seasons.

In solar energy engineering, the December solstice determines the worst-case solar angle for Northern Hemisphere installations — the day with the lowest sun angle and minimum energy collection. Solar panel tilt angles and seasonal energy forecasts are calculated from solstice geometry.

The June solstice marks the beginning of astronomical summer and the Persian New Year in some traditional calendars. The December solstice is the astronomical beginning of winter and influenced the placement of Christmas and many mid-winter festivals across cultures.

Worked Examples

June Solstice 2026

Problem:

When does the June solstice occur in 2026?

Solution Steps:

  1. 1Y = (2026 − 2000) / 1000 = 0.026
  2. 2JDE₀ = 2451716.56767 + 365242.37391×0.026 + 0.05259×0.026² − 0.00159×0.026³
  3. 3= 2451716.56767 + 9496.302 + 0.0000356 ≈ 2461212.87
  4. 4Convert JDE 2461212.87 to Gregorian → approximately June 21, 2026 at 08:50 UTC

Result:

June solstice 2026: approximately June 21, 2026 at 08:50 UTC.

Day Length at Summer Solstice

Problem:

How long is the day in London (latitude 51.5°N) on the June solstice?

Solution Steps:

  1. 1Solar declination at June solstice = +23.45°
  2. 2cosHourAngle = −tan(51.5°) × tan(23.45°) = −1.252 × 0.434 = −0.543
  3. 3hourAngle = arccos(−0.543) = 122.9°
  4. 4daylightHours = 2 × 122.9 / 15 = 16.39 hours ≈ 16 hours 23 minutes

Result:

London experiences approximately 16 hours 23 minutes of daylight on the June solstice — the longest day of the year.

Winter Solstice Day Length at Helsinki

Problem:

How short is the day in Helsinki (latitude 60°N) on the December solstice?

Solution Steps:

  1. 1Solar declination at December solstice = −23.45°
  2. 2cosHourAngle = −tan(60°) × tan(−23.45°) = −1.732 × (−0.434) = +0.752
  3. 3hourAngle = arccos(0.752) = 41.3°
  4. 4daylightHours = 2 × 41.3 / 15 = 5.5 hours

Result:

Helsinki has only about 5.5 hours of daylight on the December solstice — the shortest day of the year.

Tips & Best Practices

  • The June solstice marks the longest day in the Northern Hemisphere but the shortest day in the Southern Hemisphere — it's winter in Australia.
  • Solar panel output is lowest around the December solstice (lowest sun angle) and highest around the June solstice in the Northern Hemisphere.
  • The midnight sun starts appearing at latitudes above 66.5° (Arctic/Antarctic Circles) around the solstice.
  • Solstice times are given in UTC — convert to your local timezone to find the exact local time of the astronomical event.
  • The 'shoulder' periods around the solstices have the slowest day-length changes; day length changes fastest around the equinoxes.
  • Stonehenge aligns with midsummer sunrise — visit on June 21 to see the sun rise directly over the Heel Stone.

Frequently Asked Questions

The solstice date shifts because the tropical year (365.2422 days) doesn't divide evenly into calendar years. The Gregorian calendar's leap year system keeps the average calendar year close to the tropical year, but the solstice still oscillates within a ~3-day window as the calendar correction catches up. The solstice shifts ~6 hours later each year (one quarter of a day beyond 365) until a leap year 'resets' it ~18 hours earlier.
No — the summer solstice is the longest day but not usually the hottest. Peak summer temperatures typically occur 4–8 weeks after the solstice due to 'seasonal lag': the oceans, soil, and atmosphere absorb heat gradually through the long days and release it later. Similarly, the coldest temperatures are typically in January–February, 4–8 weeks after the December solstice.
The midnight sun is the phenomenon where the Sun remains visible above the horizon for 24 consecutive hours, occurring above the Arctic Circle (66.5°N) around the June solstice and above the Antarctic Circle (66.5°S) around the December solstice. At the North Pole, the Sun stays above the horizon continuously from the March equinox to the September equinox — approximately 6 months of daylight followed by 6 months of polar night.
Astronomical seasons are defined by the equinoxes and solstices — summer begins at the June solstice (around June 20–21). Meteorological seasons are fixed calendar periods: summer = June, July, August in the Northern Hemisphere. Meteorologists prefer the fixed calendar definition because it aligns weather data to consistent month groupings, making statistics and forecasts easier to compute and compare across years.
Yes — a solstice is a specific astronomical moment that occurs simultaneously worldwide. What changes by location is the local clock time. For example, if the June solstice occurs at 08:00 UTC, it is simultaneously 3:00 AM in New York (UTC−5) and 17:00 in Tokyo (UTC+9). The date may even differ by location if the UTC time is near midnight.

Sources & References

Last updated: 2026-06-06

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Editorial Note

MyCalcBuddy Editorial Team

This page is maintained as an educational calculator reference.

Source

Formula Source: Standard Mathematical References

by Various

UpdatedLast reviewed: May 2026
CheckedFormula checks are based on standard references and internal QA review.

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