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The Nautical Almanac

printed in advance, and checked twice
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The word computer appears here in both of its senses, and the article does not distinguish them typographically. Wherever the article is describing how the book was made before the twentieth century it means a person: the Almanac employed several dozen, by post, from their own houses, and the arrangement they worked under is the one the machines were later built to imitate. From 1984, where the word next appears, it means a machine doing a different thing entirely, which the section on method sets out. Editors are asked not to gloss either use, and not to assume that the second sense is the more accurate of the two.

For the problem it was created to solve, see the longitude problem.
The Nautical Almanac
and Astronomical Ephemeris, from 1767
A page from an eighteenth-century almanac headed SEPTEMBER 1772 and, beneath it, Distances of the Moon's Centre from Stars, and from the Sun east of her. The table is ruled into a column of days, a column of star names including Antares, Aldebaran, Pollux and Regulus, and four wide columns headed 12 Hours, 15 Hours, 18 Hours and 21 Hours, each subdivided into degrees, minutes and seconds
The reason the book exists: the Moon's distance from Antares, Aldebaran, Pollux, Regulus, the Sun and four more, for September 1772, at twelve, fifteen, eighteen and twenty-one hours of Greenwich time. The heading reads east of her, so this is half the table; the other half faced it. Every figure was worked out twice, by two men not allowed to compare notes, two years before the month it describes.
First volumeFor the year 1767
Founded byNevil Maskelyne
Published continuously since1767
Reckoned fromGreenwich, from the first page
How it was made
Each figure computedTwice, independently
ByTwo computers, who were people
Reconciled byA third, called the comparer[2]
The lunar tables
Printed from1767
Printed untilThe volume for 1906[4]
Worked examples until1919
How it is computed
To 1983Analytic series, by hand
From 1984Numerical integration[8]
Bodies carriedSun, planets, Pluto, Moon, 343 asteroids
RelativityIncluded, and required

The Nautical Almanac and Astronomical Ephemeris was established by Nevil Maskelyne, Astronomer Royal, and first appeared in 1766 for the year 1767, by which date the almanacs of Europe had mostly stopped disagreeing about what day it was: see 30 February 1712. It has been published every year since, which makes it one of the longest continuously running publications in the world, and it is the reason that longitude is counted from Greenwich.[1]

Its original purpose was to let a ship find its longitude without a clock. The Moon moves against the fixed stars fast enough to serve as one, and the Almanac tabulated, years ahead, the angular distance between the Moon and selected stars at three-hour intervals of Greenwich time. A navigator measured the same angle where he was, looked up the Greenwich time at which it would occur, compared that with his local time, and had his longitude. The method is the lunar distance, one branch of celestial navigation, and it required a book of numbers that were right.

Two computers and a comparer

The problem with a book of numbers is that a wrong one cannot be seen. A misprint in a novel is obvious and a misprint in a table is invisible, and a navigator using it will be confidently in the wrong place.

Maskelyne's answer, in operation from the first volume, was to have every computation performed twice, by two men working separately, and the two results compared by a third man whose job title was the comparer.[2] The computers worked from their own homes, scattered around the country, and were not collaborators: the whole point was that they should not confer, because two people who confer make the same mistake. The job outlasted the Almanac's need for it by a century and a half, and was still being done by hand, on plates, at Harvard in 1902: see Henrietta Swan Leavitt.

The scheme is worth naming plainly, because it is the one every safety-critical system has arrived at since. Duplicate the work, isolate the workers, reconcile the outputs, and treat a disagreement as information rather than as an embarrassment. It was running in 1767, on paper, by post.

The people are documented. Henry Andrews computed for the Almanac from 1768 to 1815, forty-seven years. The Rev. Malachy Hitchins was comparer from the first volume until his death in 1809, forty-two years, and stepped in as a computer as well when William Bayly was sent away to observe the transit of Venus in 1769.[2]

What else is in it

The lunar distances were the famous part, and they were never the bulk of it.

A page of printed tables headed, from left to right, TABLE I, The Refractions of the Heavenly Bodies in Altitude; TABLE II, Depression or Dip of the Horizon of the Sea, with a column of the height of the eye in feet against a column of the dip in minutes and seconds; and TABLE III, The Sun's Parallax in Altitude
Not from the Almanac. Page 1 of Tables Requisite, the companion volume, carrying three of the four corrections named above side by side: refraction, the dip of the horizon against height of eye, and the Sun's parallax. One foot of eye height costs fifty-seven seconds of arc; ten feet costs three minutes and one second.

An angle measured at sea is wrong before it is written down. The sextant altitude of a star must be corrected for the observer's height above the water, because from a deck the sea horizon lies below true horizontal by an amount that grows with the height of the eye: that is the dip of the horizon. Then for refraction, which lifts everything near the horizon. Then, for the Moon, for parallax, and for the semidiameter of a disc whose edge is what you actually measured.

None of those tables is in the Almanac, though its prefaces report observations behind them: the volume for 1772 notes that Bradley "made several curious Observations of the Depression of the Horizon of the Sea at various Altitudes above its Level", and prints them.[7] The tables themselves Maskelyne issued the same year as a separate volume, Tables Requisite to be used with the Nautical Ephemeris, and the division is deliberate: the ephemeris changes every year and is thrown away, and the corrections do not change at all. A navigator bought the second book once and the first one annually, which is a publishing arrangement and also a statement about which parts of the problem move.

None of these is difficult and all of them are tedious, and every one of them is a place to make an arithmetical slip in a small cabin in bad light. The Almanac's real subject is not the sky. It is the set of small, certain, boring adjustments between what an instrument reports and where a ship is, and its authority rests on those being right in the ten-thousandth volume as reliably as in the first.

Superintendence

From 1818 to 1829 the Almanac was superintended by Thomas Young, whose work on the wave theory of light is elsewhere in this encyclopedia and whose administration of the Almanac was not admired.[5]

The complaint was that under him the Almanac had stopped being the best in the world and had not noticed. It was pressed hardest by the astronomer Sir James South, who in 1829 published eighty pages under the title Refutation of the numerous mistatements and fallacies contained in a paper presented to the Admiralty by Dr. Thomas Young, and who argued in it, among much else, that what the Almanac needed was "a new and efficient Board of Longitude".[5] Young left the superintendence that year. His Majesty's Nautical Almanac Office was established as a separate body in 1832.

Why Greenwich

The Almanac's tables were computed for the meridian of the Royal Observatory, because that was where Maskelyne worked. Nothing more principled than that was involved at the outset.

The consequence was that any navigator who used the Almanac was, without deciding anything, reckoning his longitude from Greenwich. Other nations adopted the method, and in adopting the method adopted the meridian, because recomputing the tables for Paris or Cadiz was a great deal of work to avoid a small humiliation. By the time the International Meridian Conference met at Washington in 1884 and resolved, twenty-two votes to one, that longitude should be counted from Greenwich, it was ratifying a practice rather than choosing one.[3]

That vote is why Null Island is in the Gulf of Guinea rather than somewhere else. The origin of the coordinate system that now locates everything on Earth sits where it does because an English almanac was cheap, accurate and already on the shelf.

The tables that would not die

The chronometer was supposed to end all this. Harrison's H4 was tested in 1761–62, and a clock that keeps Greenwich time in a ship's cabin makes the Moon unnecessary.

The Almanac went on printing lunar-distance tables until the volume for 1906, and worked examples of the method until 1919.[4] The reason is not sentiment. A chronometer is an object and can stop, be dropped, or drift, and a method that needs only the sky and a book cannot. The two were carried together on purpose for a century, the clock for daily use and the Moon for when the clock was in doubt, which is the same argument as computing every figure twice.

How the numbers have been made

The Almanac has been produced by three quite different methods, and the difference between them is the whole of the answer to a common objection: that an ephemeris is only the extrapolation of cycles already seen, and therefore proves nothing about how the solar system is arranged.

Until the 1830s, that objection was very nearly a fair description. Maskelyne's lunar positions came from Tobias Mayer's tables, which were a theory of the Moon's motion fitted to observation and patched where it disagreed, and the tables themselves were extended by taking differences between successive entries and carrying the pattern forward. That is arithmetic on a series, and it is exactly what a machine can do without knowing what the numbers mean: it is why Babbage's difference engine was called a difference engine, and why he expected it to produce the tables.

From the late nineteenth century to 1983 it was analysis rather than pattern. Simon Newcomb's planetary theories, published from 1898, and Ernest Brown's lunar theory of 1919 were solutions to the gravitational problem: series expansions of the equations of motion, derived by hand, running to thousands of terms. The Almanac's inner planets and Sun came from Newcomb and Ross until 1983, and the Moon from Brown, patched, into the early 1980s.[8] Nothing in a Newcomb series is a repeated observation; it is a consequence of an assumed law of gravitation, and it can be wrong in ways a fitted cycle cannot be. It was: Mercury's perihelion came out 43 seconds of arc per century short, and stayed short until general relativity supplied the missing term.

Since 1984 it has been neither. In that year the almanacs adopted the Jet Propulsion Laboratory's DE200, and the method has not changed since: the equations of motion are integrated forward numerically, step by step, from a set of initial conditions.[8] The current model carries the Sun, the eight planets, Pluto and the Moon, together with 343 asteroids, being about ninety per cent of the mass of the main belt; the mutual Newtonian accelerations and their relativistic corrections, in a modified form of the Einstein–Infeld–Hoffmann equations; a model of the Moon's librations; and the acceleration caused by the tidal distortion of the Earth, which is why the Moon in it recedes by about four centimetres a year.

What the objection would have to explain

The reason the extrapolation account cannot be rescued is that the modern ephemeris is fitted to measured distances, and a pattern has none in it.

A photograph on the lunar surface: a tilted panel of small square corner-cube reflectors in a white frame, standing on grey dust scattered with boot prints, with a leg and gold foil of the Lunar Module at the upper left, a camera on a stand at the right, and black sky above the horizon
What the modern almanac is checked against. The Apollo 11 crew left this panel of corner reflectors on the Moon in 1969; a laser fired at it comes back, and the round trip gives the distance to a few millimetres. It is also how the recession is known to be about four centimetres a year.

The observations it is reconciled against are radar ranging to the planets, radio ranging to spacecraft, very-long-baseline interferometry of those spacecraft against distant quasars, and laser ranging to the reflectors left on the Moon.[9] Those are lengths, in metres, in three dimensions. Two millennia of naked-eye records contain no distances at all – only angles, and only from here – so no amount of cycle-matching can produce them, and a model that reproduces them is being tested on a quantity the cycles never contained.

Nor could a pattern be flown. An ephemeris of this kind is used to send an object to a body it has never been near, arriving at a place and a second computed years in advance, and the arrival is the test. A table extended by differences can only say what has already happened again.

One part of the almanac genuinely is observation, and it is not the part usually named. The Earth's rotation is irregular and cannot be predicted; the difference between uniform time and the turning of the planet has to be measured and published after the fact, which is what leap seconds are for. The sky is calculated and the ground is watched. The objection points at the calculated half.

The office

The office survives. It has moved from Greenwich to Herstmonceux to Cambridge to Didcot to Taunton, and it now supplies, by its own account, "astronomers, mariners, aviators, surveyors, the military, police, lawyers, religious groups, architects, schools, diary and calendar manufacturers, photographers and film crews".[6] A book begun so that a ship could find out where it was is now consulted by people establishing what the sky was doing on the night in question.

In this encyclopedia

Two of its appearances here are worth collecting.

Charles Babbage and John Herschel were checking tables of this kind, one evening in 1821, when they found them disagreeing page after page and Babbage said he wished to God the calculations could be executed by steam. The engines that followed were an attempt to remove the computers from the process, and the process had already been built to survive them.

And the Concordant Orrery, a brass model built in the 1860s to demonstrate a flat and stationary Earth without recourse to globe mathematics, was set throughout from the Almanac – computed, as ever, for a turning globe. It agreed with the sky in every particular, having been told in advance what the sky would do.

See also

  • The longitude problem – the question it was published to answer, and the clock that answered it too
  • Null Island – at the origin this book put there
  • Charles Babbage – who checked tables like these, disliked the experience, and designed a machine
  • Thomas Young – its superintendent for eleven years, and better at optics
  • Dip of the horizon – the first of the corrections, which this book pointedly did not carry
  • The Concordant Orrery – which was set from it, in order to disprove the world it was computed for

References

  1. ^ Established by Nevil Maskelyne, fifth Astronomer Royal, under the Commissioners of Longitude; first issue printed in 1766 for the year 1767. Publication has been annual and unbroken since. Since 1958, for the volume of 1960 onwards, it has been produced jointly by His Majesty's Nautical Almanac Office and the United States Naval Observatory.
  2. ^ The computations were performed in duplicate by two independent computers and compared by a third person known as a comparer. Henry Andrews (1744–1820) worked on the Almanac from 1768 to 1815; the Rev. Malachy Hitchins (1741–1809) was comparer from 1767 until his death, and covered for William Bayly during the transit of Venus of 1769. The word computer means a person throughout this section, and went on meaning one, in this trade, into the 1960s.
  3. ^ International Meridian Conference, Washington, 1884: Resolution II, adopted 13 October, twenty-two in favour, San Domingo against, France and Brazil abstaining. The Almanac's priority is not a claim of the conference's own making; it is simply that the tables were computed for Greenwich from 1767 and everybody used them.
  4. ^ Lunar-distance tables ran from the first volume to the volume for 1906; worked examples of the method continued to 1919. The first ten editions took the Moon's position from Tobias Mayer's tables. Greenwich Mean Time replaced apparent time in the volume for 1834.
  5. ^ Thomas Young was Superintendent of the Nautical Almanac from 1818 to 1829. James South, Refutation of the numerous mistatements and fallacies contained in a paper presented to the Admiralty by Dr. Thomas Young, (superintendent of the nautical almanac) (London, 1829), viii + 80 pages: a title that states its case before the reader reaches the text. This encyclopedia takes no view on how much of it Young deserved, and notes only that eighty pages is a great deal of refutation.
  6. ^ HM Nautical Almanac Office's own description of its users. The list is quoted because no summary of it is as good.
  7. ^ Tables Requisite to be used with the Nautical Ephemeris, for finding the Latitude and Longitude at Sea, published by order of the Commissioners of Longitude in 1767, the same year as the first Almanac. The Bradley observations are in the preface to the volume for 1772, alongside the timings of the transit of Venus of 3 June 1769. The plate is from the second edition, whose preface Maskelyne signed at Greenwich on 10 February 1781, and whose page 1 carries, in order, Table I the refractions, Table II the depression or dip of the horizon of the sea, Table III the Sun's parallax in altitude, Table IV the augmentation of the Moon's semidiameter, and Table V the dip at distances short of the horizon. Modern editions of the Almanac itself do carry correction tables in the front, which is why the eighteenth-century arrangement is easy to state backwards.
  8. ^ Newcomb's planetary theories were published from 1898, and the Astronomical Almanac derived its inner planets and Sun from Newcomb and Ross through 1983; Brown's lunar theory appeared in 1919 and was corrected and re-corrected into the early 1980s. DE200/LE200, fully numerically integrated and fitted to modern observations, was adopted for 1984 and used to 2002; the current series is DE440, which spans 1550 to 2650, and DE441, which spans −13,200 to 17,191 less accurately. The distinction of art is between general perturbations, meaning analytic series, and special perturbations, meaning step-by-step numerical integration.
  9. ^ The fits use planetary radar, spacecraft radio ranging, VLBI positions of spacecraft, transit and CCD observations, and lunar laser ranging to the retroreflectors of Apollo and Lunokhod. Lunar laser ranging is also the direct measurement of the recession: the round-trip distance to the Moon is known to a few millimetres, and it lengthens.
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