The Sun in Celestial Navigation

The Sun is the navigator's most accessible celestial body — visible every clear day, unmistakable in identity, and capable of yielding a reliable fix through a well-planned sequence of sights.

Why the Sun Is the Primary Celestial Body

For the practicing offshore navigator, the Sun offers advantages that no other celestial body can match. It is visible on any clear day, it is unmistakably bright, it requires no identification, and it rises and sets predictably — providing a regular daily schedule of usable observations from dawn to dusk.

Brightness and ease of identification make the Sun the only celestial body suitable for daytime sights. Unlike stars, which require twilight conditions and a visible horizon simultaneously — a narrow window — the Sun can be observed whenever the sky is clear and the horizon is sharp. A beginner can take their first Sun sight without any prior knowledge of star identification or the star finder.

A predictable daily geometry means the Sun's altitude and azimuth change in a regular, calculated way throughout the day. In the morning, the Sun is in the east and rising. At local noon, it reaches its highest point and crosses the meridian. In the afternoon, it is in the west and declining. This geometry creates natural observation opportunities that have defined the rhythm of celestial navigation since the earliest ocean voyages.

The Sun's limitation is that it is a single body. Stars and planets can be observed simultaneously from multiple directions at twilight, giving multiple crossing lines of position and an instant fix. The Sun provides only one line of position at any given moment. To obtain a fix from Sun sights alone, the navigator must take sights at different times and advance earlier LOPs to account for the vessel's movement — the running fix technique. This requires additional care in track-keeping and introduces the vessel's dead reckoning accuracy into the celestial fix.

In practice, the Sun-run-Sun sequence — a morning sight, a noon latitude, and an afternoon sight — is the fundamental daytime navigation schedule for offshore passages. When complemented by a dawn or twilight star fix at the bookends of the day, the Sun provides all the position information a navigator needs for a safe ocean crossing.

A navigator at the shrouds of an offshore sailboat bringing the Sun's lower limb down to touch the sea horizon with a sextant, with clear sky and a sharp horizon visible
A Sun lower limb sight underway. The navigator rocks the sextant gently to find the exact moment the Sun's limb kisses the horizon at its lowest point of swing. The time is recorded the instant the arc touches the horizon.
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Take multiple Sun sights in quick succession — four to six sights in two minutes — and average them rather than relying on a single reading. A single sight can be affected by a momentary swell obscuring the horizon, a brief cloud shadow, or an unsteady hand. A set of averaged sights smooths these errors and produces a more reliable Ho.

Check Your Understanding 1 Question

What is the primary navigation limitation of using only Sun sights, compared to a round of star sights at twilight?

Local Apparent Noon

Local Apparent Noon (LAN) is the moment when the Sun reaches its greatest altitude for the day — the instant it transits the observer's meridian and is due north or due south, depending on whether its declination is higher or lower than the observer's latitude. This moment is the foundation of the oldest latitude-finding technique in ocean navigation.

At the instant of LAN, the Sun is on the observer's meridian, meaning the geometry of the sight is simplified enormously. The altitude of the Sun at LAN is directly related to the observer's latitude and the Sun's declination by a simple formula: Latitude = Declination ± (90° − Ho at noon). No sight reduction tables are needed. No LHA calculation is required. The noon latitude is computed with arithmetic alone from the peak altitude and the day's declination from the almanac.

The sign rule follows the relationship between the observer's latitude and the Sun's declination. If the Sun is bearing south at noon (observer is north of the Sun's declination — the most common case in northern latitudes), the formula is: Lat = Dec + (90° − Ho). If the Sun bears north at noon (observer south of the Sun's declination), the formula becomes: Lat = (90° − Ho) − Dec. In both cases, the computation takes less than a minute with a simple calculator.

Predicting the time of LAN is important because the Sun's altitude changes very slowly near noon — the altitude curve flattens out near the peak. If the navigator starts taking sights too late, the Sun has already begun to descend and the peak altitude is missed. LAN time is predicted from the equation of time (printed in the Nautical Almanac) and the vessel's longitude. The navigator begins tracking the Sun's altitude about 20 minutes before predicted LAN and takes sights every two minutes as the altitude approaches its maximum.

Practical technique at LAN is to observe the Sun's altitude carefully as it rises toward its peak, holding the Sun on the horizon and adjusting the sextant to follow it up. When the altitude stops rising and begins to fall — the moment the Sun 'hangs' — that is the peak altitude and the moment of LAN. The navigator notes the final maximum altitude and records it for the noon latitude calculation. The exact time of LAN is less critical than the exact altitude, since the latitude formula requires only the peak altitude.

Combining the noon latitude with a morning Sun line gives a running fix: the morning LOP is advanced along the vessel's track to the time of LAN and crossed with the noon latitude line. This noon fix has been the primary daily position determination method for offshore sailors for centuries.

Graph showing the Sun's altitude throughout the day forming a smooth arc, with Local Apparent Noon marked at the peak where the curve is flattest, and the noon latitude formula annotated
The Sun's altitude curve through the day, showing LAN at the peak. The Sun's altitude changes slowly near noon, making the peak easy to identify by tracking — but the curve is flat enough that a precise time is less critical than a precise altitude. The noon latitude formula requires only the peak Ho and the day's declination.
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Start tracking the Sun's altitude toward noon 20 minutes before your predicted LAN time. Take a sight every two to three minutes and record the altitudes in sequence. The moment the altitude stops increasing and the sextant arc requires downward adjustment to keep the Sun on the horizon — that is your noon altitude. Pre-computing LAN time using the almanac's equation of time prevents you from starting late and missing the peak.

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Do not confuse Local Apparent Noon with Local Mean Noon (12:00 local time). Due to the equation of time, the Sun can transit your meridian up to 16 minutes before or after 12:00 local mean time, depending on the time of year. Always compute predicted LAN from the almanac rather than assuming it occurs at local clock noon.

Check Your Understanding 2 Questions

At LAN, the observed altitude Ho of the Sun is 62° 14.0'. The Sun's declination is N 18° 32.0' and it is bearing south. What is the observer's latitude?

Why is it important to predict LAN time from the almanac rather than assuming noon occurs at 12:00 local time?

The Running Fix with Sun Sights

Because the Sun is a single body, obtaining a fix from Sun sights alone requires taking observations at different times and advancing the earlier line of position to the time of the later one. This technique — the running fix — requires accurate dead reckoning of the vessel's movement between sights.

The standard Sun navigation day begins with a morning Sun line: a sight taken when the Sun is at a convenient altitude in the eastern sky, typically two to four hours after sunrise. This sight produces a Sun LOP running approximately northwest-southeast (in the northern hemisphere with the Sun in the east). On its own, this LOP tells the navigator which line they are on, but not where along it.

At noon, the noon latitude gives the observer's latitude directly (see previous section). By advancing the morning Sun LOP along the vessel's track — the course steered and distance run between the morning sight and LAN — the advanced morning LOP crosses the noon latitude line at the running fix. This running noon fix is the traditional daily position for offshore sailing passages.

The Sumner Line (or Marcq St Hilaire intercept method) underpins modern Sun fix work. The American sea captain Thomas Sumner (1802–1876) discovered in 1837 that a celestial sight defines a circle of equal altitude on the Earth's surface — and that any straight-line segment of that circle can serve as a line of position. This insight, independently developed by Marcq St Hilaire, is the foundation of all modern sight reduction: the LOP is a short segment of the circle of equal altitude, perpendicular to the azimuth.

Advancing a line of position is done geometrically on the chart or plotting sheet. The navigator plots the original LOP, then draws a line parallel to it shifted in the direction of the vessel's track by the distance run between the sights. This shifted line — the advanced LOP — represents where the original LOP would be if the vessel had not moved since the first sight. When a second LOP (or the noon latitude line) is plotted, its intersection with the advanced LOP is the running fix.

For the most accurate Sun running fix, an afternoon Sun sight can be added to the sequence. By afternoon, the Sun has moved significantly westward and its LOP has a very different orientation than the morning line. Crossing the advanced morning LOP with an afternoon LOP (also advanced to a common time) gives a Sun-run-Sun fix with good crossing geometry. This three-sight sequence — morning, noon, afternoon — is the most complete Sun navigation day.

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When advancing an LOP for a running fix, use the course made good and the distance made good over the entire run — not just the compass course and engine hours. Account for current, leeway, and any course changes. The running fix is only as accurate as the dead reckoning used to advance the LOP, so keep a precise log between sights.

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A large position error from a running fix is most often caused by current or leeway that was not accounted for in the advancing of the LOP — not by errors in the sights themselves. If your running fix seems inconsistent with your DR position, re-examine the track kept between sights before assuming the sights are wrong.

Check Your Understanding 1 Question

What additional information is needed to advance a morning Sun LOP to noon for a running fix?

Taking Sun Sights in Practice

Practical Sun sighting technique is developed through repetition. The mechanical skill of bringing the Sun's limb precisely to the horizon, holding it there while rocking the sextant, and recording the time at the exact moment of tangency takes practice — but it is a learnable skill that improves rapidly with use.

Upper limb vs lower limb: The Sun is too large to observe its center directly. Navigators observe either the bottom edge (the lower limb) or the top edge (the upper limb) and apply the semi-diameter correction to find the center altitude. The lower limb is standard for most observations — it is easier to bring to the horizon because you are setting the limb to touch the horizon from above, and the semi-diameter correction is added. The upper limb is used when the lower limb is obscured by clouds or haze near the horizon. When using the upper limb, the semi-diameter is subtracted. The almanac's altitude correction tables are pre-calculated for both cases.

Rocking the sextant is the fundamental technique for finding the exact vertical angle. As the sextant is tilted left and right from the vertical (rocked), the reflected image of the Sun describes an arc. The lowest point of the arc — the nadir of the swing — is where the sextant is perfectly vertical and the altitude is correctly measured. The navigator brings the lower limb to just touch the horizon at the nadir of the rocking motion. This eliminates the error introduced by holding the sextant at a slight tilt.

Dealing with clouds: A thin haze over the Sun's disk requires using a darker shade glass to maintain visibility of the limb. When clouds partially obscure the Sun, take sights in the gaps and average the results. If the Sun passes behind a cloud bank at the moment of LAN, track the altitude carefully before and after — the peak altitude can often be estimated from the symmetry of the altitude curve on either side of the transit.

Multiple sights for averaging: The most reliable way to reduce sighting error is to take four to six sights in rapid succession (within two minutes) and average both the altitudes and the times. Sights that differ by more than 1 to 2 arcminutes from the average should be discarded as outliers — likely caused by a wave obscuring the horizon or an unsteady sextant. The averaged altitude and averaged time are then used for a single sight reduction, producing a more accurate Ho than any individual sight could provide.

Recording the sight: Develop a consistent routine. At the moment the Sun's limb touches the horizon at the nadir of the rocking motion, call out 'mark' (or have a partner read the time), immediately read the sextant arc, and record both time (to the second) and altitude in the sight log. Do not try to read the sextant and check the time simultaneously — the time error will be unacceptably large. A two-person sight team — one on the sextant, one on the watch — is far more accurate than a single navigator attempting both.

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Pre-shade your sextant to the correct shade glass combination before bringing the Sun down to the horizon. Setting the arc to the predicted altitude before starting the sight — from the 2102-D or a mental estimate — lets you find the Sun quickly in the telescope without wasting time scanning. Once found, the final rocking-and-touching motion takes only a few seconds.

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Never look at the Sun through the sextant telescope without shade glasses in place. The telescope magnifies solar radiation to levels that can cause immediate and permanent retinal damage. Always verify the shade glasses are in position before raising the instrument. When in doubt, use a darker shade than necessary — it is easier to adjust once the Sun is found than to risk eye injury.

Check Your Understanding 2 Questions

Why does the navigator 'rock' the sextant from side to side when taking a Sun sight?

When should a navigator use the Sun's upper limb rather than the lower limb for a sight?

Summary

The Sun is the primary celestial body for daytime navigation — always identifiable, bright, and available throughout the day on any clear day at sea.

Local Apparent Noon (LAN) yields latitude directly from the peak altitude: Lat = Dec ± (90° − Ho), with no sight reduction tables required.

The standard Sun navigation day is the sun-run-sun sequence: morning sight, advanced to noon for a running fix with the noon latitude, followed by an optional afternoon sight for a second crossing LOP.

Advancing an LOP requires accurate track-keeping between sights — the running fix is only as accurate as the dead reckoning used to advance the LOP.

Take four to six sights in rapid succession and average the results; discard outliers more than 2 arcminutes from the mean.

Rock the sextant to find the nadir of the Sun's arc, confirming the instrument is vertical; always use shade glasses and never observe the Sun without them.

Key Terms

Local Apparent Noon (LAN)
The moment when the Sun reaches its maximum altitude for the day, transiting the observer's meridian; used to determine latitude directly without sight reduction tables
Noon latitude formula
Latitude = Declination ± (90° − Ho at LAN); the sign depends on whether the Sun bears north or south at noon
Equation of time
The difference between Local Apparent Noon and Local Mean Noon (clock noon), caused by Earth's elliptical orbit and axial tilt; can be up to 16 minutes and must be applied when predicting LAN time
Running fix
A position fix obtained by advancing an earlier line of position along the vessel's track to cross with a later LOP; requires accurate dead reckoning between the observations
Advanced LOP
A line of position shifted parallel to its original orientation by the vessel's course and distance run between two observations, allowing it to be crossed with a later LOP for a running fix
Sumner line
A line of position derived from a celestial sight, representing a short segment of the circle of equal altitude; the foundation of modern sight reduction technique, named after Captain Thomas Sumner
Lower limb
The bottom edge of the Sun's disk; the standard limb for sextant observations, to which the semi-diameter correction is added when computing Ho
Rocking the sextant
Tilting the sextant from side to side during a sight to find the nadir of the reflected body's swing, which confirms the instrument is held vertically and the altitude measurement is correct

The Sun in Celestial Navigation Quiz

5 Questions Pass: 75%
Question 1 of 5

At LAN, the observed altitude Ho is 47° 22.0' and the Sun's declination is S 12° 08.0'. The Sun bears north. What is the observer's latitude?

Question 2 of 5

Why does the altitude curve flatten near Local Apparent Noon, and what practical technique does this suggest?

Question 3 of 5

A morning Sun sight taken at 08h 45m produces an LOP. The navigator then runs 42 NM on course 270°T to the time of a noon latitude sight. How should the morning LOP be advanced for the running fix?

Question 4 of 5

A navigator takes five rapid Sun sights with the following Ho values: 38° 14.2', 38° 15.8', 38° 14.6', 38° 28.3', and 38° 14.9'. How should these be processed?

Question 5 of 5

What is the difference between the Sumner Line and the intercept method of sight reduction?

References & Resources