Our Solar System

Lesson plan · Expert · Adults · 40 minutes

The equation of time and the analemma

Why a sundial at Greenwich runs up to 16.5 minutes fast and 14.2 minutes slow: the eccentricity and obliquity terms of the equation of time, their sizes, the dates of the extremes in 2027, and solar noon found on the viewer's own globe.

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Level
Ages
Adults
To present
40 minutes
Steps presented
4
Steps for pupils
7
Questions
4
Pupil tasks
2

The lesson

The class finds the moment the Sun crosses the Greenwich meridian on the viewer's globe, separates the equation of time into its eccentricity and obliquity terms and sizes each, and dates the four turning points of 2027 against the US Naval Observatory. Pupils then stop the clock at true solar noon themselves on two dates, and the lesson ends with the figure of eight those noons trace.

What they take away

The equation of time is apparent minus mean solar time: a yearly term of amplitude 2e, 7.7 minutes, from the eccentric orbit and a half-yearly term of amplitude tan²(ε/2), 9.9 minutes, from the tilted ecliptic. In 2027 they combine to +16.5 minutes on 3 November and −14.2 minutes on 11 February, and the viewer's globe puts the Sun over Greenwich within 15 seconds of JPL Horizons on every date checked.

Step by step

The caption is what the class reads on screen; the talking points are in your notes drawer (N) when you present. Steps marked Pupils only appear only in the pupil lesson.

  1. 01

    Clock noon and sundial noon

    Presented and for pupils

    Caption

    On 3 November 2027 the Sun crosses the Greenwich meridian at 11:43:33 UTC, 16.5 minutes before mean noon. A sundial there is 16.5 minutes fast: that is the equation of time.

    Talking points

    • USNO glossary: "equation of time: the difference apparent solar time minus mean solar time." Apparent solar time is "based on the diurnal motion of the true Sun"; mean solar time on "the fictitious mean Sun, with uniform motion along the celestial equator". Universal Time is "loosely, mean solar time on the Greenwich meridian (previously referred to as Greenwich Mean Time)".
    • Hughes, Yallop and Hohenkerk (1989) write it as E = GHA(apparent Sun) − GHA(mean Sun), or equally the right ascension of the mean Sun minus that of the apparent Sun, and note that older textbooks reverse the sign.
    • NOAA: solar noon in minutes of UTC is 720 − 4 × longitude − E. At Greenwich on 3 November 2027, E = +16.49 minutes, so noon is at 11:43:30. JPL Horizons has the Sun's local hour angle at Greenwich passing zero at 11:43:33.5 UTC, and the US Naval Observatory lists the upper transit at 11:44 (to the minute).
    • The viewer computes no equation of time for the globe. It turns the Earth by the IERS Earth rotation angle and points it at a Sun placed by JPL's elements, and on this date that puts the Sun over Greenwich at 11:43:28 UTC. Greenwich is marked at the Airy transit circle, latitude 51° 28′ 38″ N, longitude 0 by definition.
    • This scene opens paused at 11:43:30 UTC, with the Sun-overhead marker and Greenwich on the same meridian to within a few seconds of time. The view is from the Sun's side at true scale.

    Sources 1 2 5 6 9 10 12Present from this step

  2. 02

    Two causes

    Presented and for pupils

    Caption

    Two effects add. The Sun moves unevenly along an eccentric orbit, and it moves along the ecliptic while clocks keep time along the equator. To first order, E = −2e sin M + tan²(ε/2) sin 2L.

    Talking points

    • USNO glossary: the rate of the true Sun's diurnal motion "undergoes seasonal variation caused by the obliquity of the ecliptic and by the eccentricity of the Earth's orbit".
    • Derivation. The mean Sun has right ascension L, the Sun's mean longitude. The true Sun's ecliptic longitude is λ = L + 2e sin M + (5/4)e² sin 2M + …, M the mean anomaly. Its right ascension follows from tan α = cos ε tan λ, which expands as α = λ − tan²(ε/2) sin 2λ + ½ tan⁴(ε/2) sin 4λ − … (Hughes et al., eq. 5). So E = L − α ≈ −2e sin M + tan²(ε/2) sin 2L, Hughes et al.'s eq. 7, which they find within 18 seconds of the full expression at the present epoch.
    • Hughes et al.: the ellipticity term has a period of a year, an amplitude under 8 minutes, and crosses zero at perihelion and aphelion; the obliquity term has an amplitude of about 9.9 minutes and crosses zero at the equinoxes and solstices, and is only quasi-sinusoidal because the seasons differ in length.
    • The viewer's equationOfTimeMinutes (src/orbits/earthframe.js) is NOAA's calcEquationOfTime term for term: y sin 2L₀ − 2e sin M + 4ey sin M cos 2L₀ − ½y² sin 4L₀ − (5/4)e² sin 2M, with y = tan²(ε/2), turned into minutes at 4 minutes a degree. NOAA says its calculations are based on Meeus's Astronomical Algorithms.
    • Constants: e = 0.0167 and obliquity 23.44° (NASA Earth Fact Sheet; the formula uses e = 0.016708634 and ε = 23.4393° at J2000). One radian of hour angle is 180/π × 4 = 229.18 minutes of time. Earth's spin axis is drawn in this view.

    Ask the class

    Compute the amplitude of the obliquity term, tan²(ε/2), in minutes of time, with ε = 23.44°.

    Answer9.86 minutes. Answers from 9.81 to 9.91 are marked right.

    Whyε/2 = 11.72°, tan 11.72° = 0.20745, squared 0.043037 rad; × 229.18 minutes per radian = 9.86 minutes. Hughes et al. give about 9.9. Using sin²(ε/2) instead gives 9.46, outside the tolerance.

    Sources 1 2 3 4 11Present from this step

  3. 03

    The eccentricity term

    Pupils only

    Caption

    At perihelion, early in January, the true Sun and the mean Sun are together in longitude, and the true Sun then runs ahead. How large does that yearly term get?

    Talking points

    • USNO: perihelion on 3 January 2027 at 02:33 UTC and aphelion on 5 July at 05:06 UTC. The scene opens at that perihelion.
    • Hughes et al.: the ellipticity component crosses zero at perihelion and at aphelion, and its amplitude is under 8 minutes.
    • The first-order term is −2e sin M, so its amplitude is 2e radians of hour angle.

    Pupil question

    With e = 0.0167, what is the amplitude of the eccentricity term, 2e, in minutes of time?

    Answer7.66 minutes. Answers from 7.61 to 7.71 are marked right.

    Why2e = 0.0334 rad; × 229.18 minutes per radian = 7.65 minutes (7.66 with the formula's e = 0.016709). Hughes et al.: under 8 minutes. Taking e alone gives 3.83.

    Sources 2 7 11Open this step as a pupil

  4. 04

    The year of 2027

    Presented and for pupils

    Caption

    In 2027 the sundial is slowest, 14.2 minutes behind, on 11 February and fastest, 16.5 minutes ahead, on 3 November, with smaller turns of +3.6 minutes in May and −6.6 minutes in July.

    Talking points

    • From the viewer's equationOfTimeMinutes: minimum −14.22 minutes on 11 February, maximum +3.64 on 14 May, minimum −6.57 on 26 July, maximum +16.49 on 3 November; zero on 15 April, 13 June, 1 September and 25 December.
    • JPL Horizons puts the Sun on the Greenwich meridian (local apparent hour angle zero) at 12:14:12 UTC on 11 February, 11:56:22 on 14 May, 12:06:33 on 26 July and 11:43:34 on 3 November, and within 6 seconds of 12:00 on each zero date. The US Naval Observatory's transits, to the minute, agree: 12:14, 11:56, 12:07, 11:44 and 12:00. The viewer's globe is within 15 seconds of Horizons on all eight dates (12:14:07, 11:56:13, 12:06:24, 11:43:28).
    • Why the two big turns differ: at 12:00 UTC on 3 November the two first-order terms are +6.7 (eccentricity) and +9.8 (obliquity) minutes; on 11 February they are −4.7 and −9.6. Perihelion (3 January 2027, 02:33 UTC) comes 12.2 days after the December solstice (21 December 2026, 20:50 UTC), so the yearly term is not in step with the half-yearly one.
    • This scene opens at 12:14 UTC on 11 February 2027, the Sun over Greenwich 14 minutes after mean noon.

    Ask the class

    Why is the November maximum (+16.5 minutes) larger than the February minimum (−14.2 minutes)?

    1. In early November both terms are positive and near their peaks (+6.7 and +9.8 minutes); in February the eccentricity term is smaller in size (−4.7 beside −9.6)Right answer
    2. Earth is closest to the Sun in November
    3. The obliquity of the ecliptic is larger in November
    4. Daylight saving time adds an hour in February

    WhyThe two terms have periods of a year and half a year and are out of step, because perihelion (3 January 2027) is not at a solstice. Their sum peaks at +16.5 in November and bottoms at −14.2 in February.

    Sources 2 3 6 7 8 9Present from this step

  5. 05

    Your turn: solar noon in November

    Pupils only

    Caption

    The clock runs at a minute a second from 11:25 UTC on 3 November 2027. Pause it at true solar noon at Greenwich.

    Talking points

    • Solar noon is 12:00 UTC minus the equation of time at Greenwich: 12:00 − 16.5 minutes = 11:43:30. JPL Horizons gives 11:43:33.5, the viewer's globe 11:43:28 and the US Naval Observatory 11:44.
    • The check passes within 3 minutes of 11:43:30 with the clock paused, so mean noon (12:00) and the wrong sign (12:16:30) both fail. The clock under the task shows UTC to the minute, and the readout gives local mean time at Greenwich, which there is UTC.

    Pupil task

    Pause the clock when the Sun is due south at Greenwich, at true solar noon.

    HintTrue solar noon is 12:00 UTC minus the equation of time, which is +16.5 minutes on this date. Watch Greenwich come round to the meridian of the Sun-overhead marker, and use Backwards if you pass it.

    The viewer checks the task as the pupil works and says when it is done.

    Sources 5 6 9 12Open this step as a pupil

  6. 06

    Your turn: solar noon in February

    Pupils only

    Caption

    Now 11 February 2027, when the equation of time is −14.2 minutes. Pause the clock at true solar noon at Greenwich.

    Talking points

    • 12:00 UTC + 14.2 minutes = 12:14:13 from the formula; JPL Horizons gives 12:14:12, the viewer's globe 12:14:07 and the US Naval Observatory 12:14.
    • The check passes within 3 minutes of 12:14:13 with the clock paused.

    Pupil task

    Pause the clock at true solar noon at Greenwich on 11 February 2027.

    HintThe equation of time is negative now, so the sundial is slow and noon comes after 12:00 UTC.

    The viewer checks the task as the pupil works and says when it is done.

    Sources 5 6 9 12Open this step as a pupil

  7. 07

    The analemma

    Presented and for pupils

    Caption

    Mark the Sun at the same clock time every day and it traces a figure of eight, the analemma: declination up and down, the equation of time east and west. The viewer does not draw it, though its Sun-overhead point traces it on the ground.

    Talking points

    • At a fixed UT the subsolar point sits at latitude δ and longitude −E/4 degrees (E in minutes; earthframe.js gives the Sun's longitude as −15° × (UT − 12 h) − E/4). Over a year it draws the analemma on the globe; on the sky the same figure is drawn by the Sun at a fixed clock time.
    • Shape: δ runs once up and down in a year (from −23.44° to +23.44°, NASA's obliquity), while the obliquity term of E runs twice. A curve whose x has twice the frequency of its y is a figure of eight with equal loops; the yearly eccentricity term added to x makes one loop larger than the other.
    • Size in 2027: from −14.22 to +16.49 minutes is 30.7 minutes of time, 7.7° of hour angle east to west, against 46.9° north to south.
    • In this scene, 12:00 UTC on 3 November 2027, the Sun-overhead marker is west of Greenwich by E/4.

    Ask the class

    At 12:00 UTC on 3 November 2027, with E = +16.49 minutes, at what longitude is the Sun overhead? Give degrees east (west is negative).

    Answer-4.12 degrees east. Answers from -4.17 to -4.07 are marked right.

    WhyLongitude = −15° × (UT − 12 h) − E/4 = 0 − 16.49/4 = −4.12°, 4.12° west of Greenwich; NOAA's noon formula, 720 − 4 × longitude − E = 720 minutes, gives the same. The viewer's globe puts the Sun overhead at 4.13° W then.

    Sources 2 3 5 11Present from this step

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Sources

Every fact in this lesson comes from these sources, and each step lists the ones it uses.

  1. Glossary, US Naval Observatory Astronomical Applications
  2. Hughes, D. W., Yallop, B. D. and Hohenkerk, C. Y. (1989), The Equation of Time, Monthly Notices of the Royal Astronomical Society 238, 1529, doi:10.1093/mnras/238.4.1529
  3. NOAA Solar Calculator source code (calcEquationOfTime), NOAA Global Monitoring Laboratory
  4. Solar Calculation Details, NOAA Global Monitoring Laboratory
  5. General Solar Position Calculations (solar noon), NOAA Global Monitoring Laboratory
  6. Sun rise, set and transit at Greenwich (51.4772 N, 0 E), US Naval Observatory data service, 2027 dates
  7. Earth's seasons and apsides, 2027, US Naval Observatory data service
  8. Earth's seasons and apsides, 2026, US Naval Observatory data service
  9. Horizons System (the Sun from Greenwich, site 000, local apparent hour angle), JPL Solar System Dynamics
  10. IERS Conventions (2010), IERS Technical Note 36, chapters 1 and 5
  11. Earth Fact Sheet, NASA NSSDCA
  12. Airy transit circle, Paris Observatory dictionary of astronomy

More Expert lessons

Our Solar System · 3dsolarsystem.online/teachers/lessons/equation-of-time/

The equation of time and the analemma

NameDate
  1. Compute the amplitude of the obliquity term, tan²(ε/2), in minutes of time, with ε = 23.44°.

    minutes

  2. With e = 0.0167, what is the amplitude of the eccentricity term, 2e, in minutes of time?

    minutes

  3. Why is the November maximum (+16.5 minutes) larger than the February minimum (−14.2 minutes)?

    • A. In early November both terms are positive and near their peaks (+6.7 and +9.8 minutes); in February the eccentricity term is smaller in size (−4.7 beside −9.6)
    • B. Earth is closest to the Sun in November
    • C. The obliquity of the ecliptic is larger in November
    • D. Daylight saving time adds an hour in February
  4. At 12:00 UTC on 3 November 2027, with E = +16.49 minutes, at what longitude is the Sun overhead? Give degrees east (west is negative).

    degrees east

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