CHAPTER VI

THE TIME DEPARTMENT

One day two Scotchmen stood just outside the main entrance

of Greenwich Observatory, looking intently at the great

twenty-four-hour clock, which is such an object of attention to the

passers through the Park. 'Jock,' said one of them to the other,

'd'ye ken whaur ye are?' Jock admitted his ignorance. 'Ye are at the

vara ceentre of the airth.'

Geographers tell us that there is a sense in which this statement as

it stands may be accepted as true. For if the surface of the globe

be divided into two hemispheres, so related to each other that the

one contains as much land as possible, and the other as little, then

London will occupy the centre or thereabouts of the hemisphere with

most land.

This was not, however, what the Scotchman meant. He meant to tell

his companion that he was standing on the prime meridian of the

world, the imaginary base line from which all distances, east or

west, are reckoned; in short, that he was on 'Longitude Nought.'

He was not absolutely correct, however, for the great

twenty-four-hour clock does not mark the exact meridian of

Greenwich. To find the instrument which marks it out and defines it

we must step inside the Observatory precincts, and just within the

gate we see before us on the left hand a door which leads through

a little lobby straight into the most important room of the whole

Observatory--the Transit Room.

[Illustration: THE GREAT CLOCK AND PORTER'S LODGE.

(_From a photograph by Mr. Lacey._)]

This room is not well adapted for representation by artist or

photographer. Four broad stone pillars occupy the greater part of

the space, and leave little more than mere passage room beside. Two

of these pillars are tall, as well as broad and massive, and stand

east and west of the centre of the room, carrying between them the

fundamental instrument of the Observatory, the transit circle. The

optical axis of this telescope marks 'Longitude Nought,' which is

further continued by a pair of telescopes, one to the north of it,

the other to the south, mounted on the third and fourth of the

pillars alluded to above.

This room has not always marked the meridian of Greenwich, for it

stands outside the original boundary of the Observatory. But it is

only a few feet to the east of the first transit instrument which

was set up by Halley, the second Astronomer Royal, in the extreme

N.-W. corner of the Observatory domain, a distance equivalent to

very much less than one-tenth of a second of time, an utterly

insensible quantity with the instruments of two hundred years ago.

It would be a long story to tell in detail how the Greenwich transit

room has come to define one of the two fundamental lines that

encircle the earth. The other, the equator, is fixed for us by the

earth itself, and is independent of any political considerations,

or of any effort or enterprise of man. But of all the infinite

number of great circles which could be drawn at right angles to the

equator, and passing through the north and south poles, it was not

easy to select one with such an overwhelming amount of argument in

its favour as to obtain a practically universal acceptance. The

meridians of Jerusalem and of Rome have both been urged, upon what

we may call religious or sentimental grounds; that of the Great

Pyramid at Ghizeh has been pressed in accordance with the fantastic

delusion that the Pyramid was erected under Divine inspiration and

direction; that of Ferro, in the Canaries, as being an oceanic

station, well to the west of the Old World, and as giving a base

line without preference or distinction for one nation rather than

another.

The actual decision has been made upon no such grounds as these.

It has been one of pure practical convenience, and has resulted

from the amazing growth of Great Britain as a naval and commercial

power. Like Tyre of old, she is 'situate at the entry of the sea,

a merchant of the people for many isles,' and 'her merchants are

the great men of the earth.' To tell in full, therefore, the

steps by which the Greenwich meridian has overcome all others is

practically to tell again, from a different standpoint, the story

of the 'expansion of England.' The need for a supreme navy, the

development of our empire beyond the seven seas, the vast increase

of our carrying trade--these have made it necessary that Englishmen

should be well supplied with maps and charts. The hydrographic and

geographic surveys carried on, either officially by this country, or

by Englishmen in their own private capacity, have been so numerous,

complete, and far-reaching as not only to outweigh those of all

other countries put together, but to induce the surveyors and

explorers of not a few other countries to adopt in their work the

same prime meridian as that which they found in the British charts

of regions bordering on those which they were themselves studying.

Naturally, the meridian of Greenwich has not only been adopted

for Great Britain, but also for the British possessions over-sea,

and, from these, for a large number of foreign countries; whilst

our American cousins retain it, an historic relic of their former

political connection with us. The victories of Clive at Arcot and

Plassy, of Nelson at the Nile and Trafalgar, the voyages and surveys

of Cook and Flinders, and many more; the explorations of Bruce,

Park, Livingstone, Speke, Cameron, and Stanley; these are some of

the agencies which have tended to fix 'Longitude Nought' in the

Greenwich Transit Room.

There are two somewhat different senses in which the meridian of

Greenwich is the standard meridian for nearly the entire world. The

first is the sense about which we have already been speaking; it

constitutes the fundamental line whence distances east and west are

measured, just as distances north and south are measured from the

equator. But there is another, though related sense, in which it has

become the standard. _It gives the time to the world._

There are few questions more frequently put than, 'What time is

it?' 'Can you tell me the true time?' A stickler for exactitude

might reply, 'What kind of time do you mean?' 'Do you mean solar

or sidereal time?' 'Apparent time or mean time?' 'Local time or

standard time?' There are all these six kinds of time, but it is

only within the last two generations, within, indeed, the reign of

our Sovereign, Queen Victoria, that the subject of the differences

of most of these kinds of time has become of pressing importance to

any but theorists.

In one of the public gardens of Paris a little cannon is set up

with a burning-glass attached to it in such a manner that the

sun itself fires the cannon as it reaches the meridian. This, of

course, is the time of Paris noon--apparent noon--but it would be

exceedingly imprudent of any traveller through Paris who wished,

say, to catch the one o'clock express, to set his watch by the gun.

For if it happened to be in February, he would find when he reached

the railway station that the station clock was faster than the sun

by nearly a full quarter of an hour, and that his train had gone;

whilst towards the end of October or the beginning of November, he

would find himself as much too soon.

Until machines for accurately measuring time were invented, apparent

time--time, that is to say, given by the sun itself, as by a

sun-dial--was the only time about which men knew or cared. But when

reasonably good clocks and watches were made, it was very soon seen

that at different times in the year there was a marked difference

between sun-dial time and that shown by the clock, the reason being

simply that the apparent rate of motion of the sun across the sky

was not always quite the same, whilst the movement of the clock was,

of course, as regular as it could be made.

This difference between time as shown by the actual sun and by a

perfect clock is known as the 'equation of time.' It is least about

April 15, June 15, August 31, and December 25. It is greatest,

the sun being after the clock, about February 11; and the sun

being before the clock, about November 2. Flamsteed, before he

became Astronomer Royal, investigated the question, and so clearly

demonstrated the existence, cause, and amount of the equation of

time as entirely to put an end to controversy on the subject.

We had thus, early in the century, the two kinds of time in common

use, apparent time and mean time, or clock time. But as the sun can

only be on one particular meridian at any given instant, the time

as shown by the clocks in one particular town will differ from that

of another town several miles to the east or west of it. It is thus

noon at Moscow 1 hr. 36 min. before it is noon at Berlin, and noon

at Berlin 54 min. before it is noon in London.

This was all well enough known, but occasioned no inconvenience

until the introduction of railway travelling; then a curious

difficulty arose. Suppose an express train was running at the rate

of sixty miles an hour from London to Bristol. The guard of the

train sets his watch to London time before he leaves Paddington,

but if the various towns through which the train passes, Reading,

Swindon, etc., each keep their own local time, he will find his

watch apparently fast at each place he reaches; but on his return

journey, if he sets to Bristol time before starting, he will in a

similar way find it apparently slow by the Swindon, Reading, and

Paddington clocks as he reaches them in succession.

It became at once necessary to settle upon one uniform system of

time for use in the railway guides. Apart from this, a passenger

taking train, say, at Swindon, might have been very troubled to

know whether the advertised time of his train was that of Exeter,

the place whence it started, or Swindon, the station where he was

getting in, or London, its destination. 'Railway time,' therefore,

was very early fixed for the whole of Great Britain to be the same

as London time, which is, of course, time as determined at Greenwich

Observatory. At first it was the custom to keep at the various

stations two clocks, one showing local time, the other 'railway,' or

Greenwich time, or else the clocks would be provided with a double

minute hand, one branch of which pointed to the time of the place,

the other to the time of Greenwich.

It was soon found, however, that there was no sufficient reason

for keeping up local time. Even in the extreme West of England the

difference between the two only amounted to twenty-three minutes,

and it was found that no practical inconvenience resulted from

saying that the sun rose at twenty-three minutes past six on March

22, rather than at six o'clock. The hours of work and business were

practically put twenty-three minutes earlier in the day, a change of

which very few people took any notice.

Other countries besides England felt the same difficulty, and solved

it in the same way, each country as a rule taking as its standard

time the time of its own chief city.

There were two countries for which this expedient was not

sufficient--the United States and Canada. The question was of no

importance until the iron road had linked the Atlantic to the

Pacific in both countries. Then it became pressing. No fewer than

seventy different standards prevailed in the United States only some

twenty years ago. The case was a very different one here from that

of England, where east and west differed in local time by only a

little over twenty minutes. In North America, in the extreme case,

the difference amounted to four hours, and it seemed asking too much

of men to call eight o'clock in their morning, or it might be four

o'clock in their afternoon, their noonday.

The device was therefore adopted of keeping the minutes and seconds

the same for all places right across the continent, but of changing

the hour at every 15° of longitude. The question then arose what

longitude should be adopted as the standard. The Americans might

very naturally have taken their standard time from their great

national observatory at Washington, or from that of their chief

city, New York, or of their principal central city, Chicago. But,

guided partly no doubt by a desire to have their standard times

correspond directly to the longitudes of their maps, and partly

from a desire to fall in, if possible, with some universal time

scheme, if such could be brought forward, they fixed upon the

meridian of Greenwich as their ultimate reference line, and defined

their various hour standards as being exactly so many hours slow of

Greenwich mean time.

The decision of the United States and of Canada brought with it

later a similar decision on the part of all the principal States

of Europe; and Greenwich is not only 'Longitude Nought' for the

bulk of the civilized world, but Greenwich mean time, increased or

decreased by an exact number of hours or half-hours, is the standard

time all over the planet.

No; the statement requires correction. Two countries hold out, both

close to our own doors. France, instead of adopting Greenwich time

as such, adopts _Paris time less_ 9 m. 21 s. (that being the precise

difference in longitude between the two national observatories).

Ireland disdains even such a veiled surrender, and Dublin time is

the only one recognized from the Hill of Howth to far Valentia. So

the distressful country preserves her old grievance, that she does

not even get her time until after England has been served.

The alteration in national habits following on the adoption of

this European system has had a very perceptible effect in some

cases. Thus, Switzerland has adopted Mid-European time, one hour

fast of Greenwich; the true local time for Berne being just half

an hour later. The result of putting the working hours this thirty

minutes earlier in the day has had such a noticeable effect on

the consumption of gas, as to lead the gas company to contemplate

agitating for a return to the old system.

Thus, Greenwich time, as well as the Greenwich meridian, has

practically been adopted the world over.

It follows, then, that the determination of time is the most

important duty of the Royal Observatory; and the Time Department,

the one to which is entrusted the duty of determining, keeping, and

distributing the time, calls for the first attention.

Entering the transit room, the first thing that strikes the

visitor is the extreme solidity with which the great telescope is

mounted. It turns but in one plane, that of 'longitude nought,'

and its pivots are supported by the pair of great stone pillars

which we have already spoken of as occupying the principal part of

the transit-room area, and the foundations of which go deep down

under the surface of the hill. On the west side of the telescope,

and rigidly connected with it, is a large wheel some six feet in

diameter, and with a number of wooden handles attached to it,

resembling the steering-wheel of a large steamer. This wheel carries

the setting circle, which is engraved upon a band of silver let

into its face near its circumference, a similar circle being at the

back of the wheel nearer the pillar. Eleven microscopes, of which

only seven are ordinarily used, penetrate through the pier, and are

directed on to this second circle.

The present transit is the fourth which the Observatory has

possessed, and its three predecessors, known as Halley's, Bradley's,

and Troughton's, respectively, are still preserved and hang on

the walls of the transit room, affording by their comparison an

interesting object-lesson in the evolution of a modern astronomical

instrument.

The watcher who wishes to observe the passing of a star must note

two things: he must know in what direction to point his telescope,

and at what time to look for the star. Then, about two minutes

before the appointed time, he takes his place at the eyepiece. As

he looks in he sees a number of vertical lines across his field

of view. These are spider-threads placed in the focus of the

eye-piece. Presently, as he looks, a bright point of silver light,

often surrounded by little flashing, vibrating rays of colour, comes

moving quickly, steadily onward--'swims into his ken,' as the poet

has it. The watcher's hand seeks the side of the telescope till his

finger finds a little button, over which it poises itself to strike.

On comes the star, 'without haste, without rest,' till it reaches

one of the gleaming threads. Tap! The watcher's finger falls sharply

on the button. Some three or four seconds later and the star has

reached another 'wire,' as the spider-threads are commonly called.

Tap! Again the button is struck. Another brief interval and the

third wire is reached, and so on, until ten wires have been passed,

and the transit is over. The intervals are not, however, all the

same, the ten wires being grouped into three sets, two of three

apiece, and the third of four.

[Illustration: THE CHRONOGRAPH.]

Each tap of the observer's finger completed for an instant an

electric circuit, and recorded a mark on the 'chronograph.' This

is a large metal cylinder covered with paper, and turned by a

carefully-regulated clock once in every two minutes. Once in every

two seconds a similar mark was made by a current sent by means of

the standard sidereal clock of the Observatory. The paper cover of

the chronograph after an hour's work shows a spiral trace of little

dots encircling it some thirty times. These dots are at regular

intervals, about an inch apart, and are the marks made by the clock.

Interspersed between them are certain other dots, in sets of ten;

and these are the signals sent from the telescope by the transit

observer. If, then, one of the clock dots and one of the observer's

dots come exactly side by side, we know that the star was on one

of the wires at a given precise second. If the observer's dot comes

between two clock dots, it is easy, by measuring its distance from

them with a divided scale, to tell the instant the star was on

the wire to the tenth of a second, or even to a smaller fraction.

Whilst, since the transit was taken over ten wires, and the distance

of each wire from the centre of the field of view is known, we have

practically ten separate observations, and the average of these

will give a much better determination of the time of transit than a

single one would.

But let the watcher be ever so little too slow in setting his

telescope, or ever so little late in placing himself at his

eye-piece, and the star will have passed the wire, and as it

smoothly, resistlessly moves on its inexorable way, will tell the

tardy watcher in a language there is no mistaking, 'Lost moments can

never be recalled.' The opportunity let slip, not until twenty-four

hours have gone by will another chance come of observing that same

star.

It is the stars that are chiefly used in this determination, partly

because the stars are so many, whilst there is but one sun. If,

therefore, clouds cover the sun at the important moment of transit,

the astronomer may well exclaim, so far as this observation is

concerned, 'I have lost a day!' The chance will not be offered him

again until the following noon. But if one star is lost by cloud,

there are many others, and the chance is by no means utterly gone.

Beside, the sun enables us to tell the time only at noon; the stars

enable us to find it at various times throughout the entire night;

indeed, throughout both day and night, since the brighter stars can

be observed in a large telescope even during the day.

There are two great standard clocks at the Observatory: the mean

solar clock and the sidereal clock. The latter registers twenty-four

hours in the precise time that the earth rotates on its axis. A

'day' in our ordinary use of the term is somewhat longer than this;

it is the average time from one noon to the next, and as the earth

whilst turning round on its axis is also travelling round the sun,

it has to rather more than complete a rotation in order to bring the

sun again on to the same meridian. A solar day is therefore some

four minutes longer than an actual rotation of the earth, _i.e._ a

sidereal day, as it is called, since such rotation brings a star

back again to the same meridian.

The sidereal clock can therefore be readily checked by the

observation of star transits, for the time when the star ought to

be on the meridian is known. If, therefore, the comparison of the

transit taps on the chronograph with the taps of the sidereal clock

show that the clock was not indicating this time at the instant

of the transit, we know the clock must be so much fast or slow.

Similarly, the difference which should be shown between the sidereal

and solar clocks at any moment is known; and hence when the error of

the sidereal clock is known, that of the solar can be readily found.

It is often quite sufficient to know how much a clock is wrong

without actually setting its hands right; but it is not possible

to treat the Greenwich clock so, for it controls a number of other

clocks continually, and sends hourly signals out over the whole

country, by which the clocks and watches all over the kingdom are

set right.

In the lower computing room, below the south window, we find the

Time-Desk, the head-quarters of the Time Department. This is a very

convenient place for the department, since one of the chronometer

rooms, formerly Bradley's transit room, opens out of the lower

computing room; the transit instrument is just beyond; it is

close to the main gate of the Observatory, and so convenient for

chronometer makers or naval officers bringing chronometers or coming

for them, whilst just across the courtyard is the chronograph room,

with the Battery Basement, in which the batteries for the electric

currents are kept, and the Mean Solar Clock lobby, with the winch

for the winding of the time-ball at the head of the stairs above it.

These rooms do not exhaust the territory of the department, since it

owns two other chronometer rooms on the ground floor and first floor

respectively of the S.-E. tower.

At the time-desk means are provided for setting the clock right very

easily and exactly. Just above the desk are a range of little dials

and bright brass knobs, that almost suggest the stops of a great

organ.

Two of these little dials are clock faces, electrically connected

with the solar and sidereal standard clocks, so that, though these

clocks are themselves a good way off, in entirely different parts

of the Observatory, the time superintendent, seated here at the

time-desk, can see at once what they are indicating. Between the

two is a dial labelled 'Commutator.' From this dial a little handle

usually hangs vertically downwards, but it can be turned either

to the right or to the left, and when thus switched hard over, an

electric current is sent through to the mean solar clock. If now

we leave the computing room and cross the courtyard to the extreme

north-west corner, we find the Mean Solar Clock in a little lobby,

carefully guarded by double doors and double windows against rapid

changes of temperature. Opening the door of the clock case, we

see that the pendulum carries on its side a long steel bar, and

that this bar as the pendulum swings passes just over the upper

end of an electro-magnet. When the current is switched on at the

commutator, this electro-magnet attracts or repels the steel bar

according to the direction of the current, and the action of the

clock is accordingly quickened or retarded. To put the commutator

in action for one minute will alter the clock by the tenth of a

second. As the error of the clock is determined twice a day, shortly

before ten o'clock in the morning, and shortly before one o'clock in

the afternoon, its error is always small, usually only one or two

tenths. These two times are chosen because, though time-signals are

sent over the metropolitan area every hour from the Greenwich clock

through the medium of the Post Office, at ten and at one o'clock

signals are also sent to all the great provincial centres. Further,

at one o'clock the time balls at Greenwich and at Deal are dropped,

so that the captains of ships in the docks, on the river, or in the

Downs may check their chronometers.

The Time-Ball is dropped directly by the mean solar clock itself.

It is raised by means of a windlass turned by hand-power to the top

of its mast just before one o'clock. Connected with it is a piston

working in a stout cylinder. When the ball has reached the top of

the mast, the piston is lightly supported by a pair of catches.

These catches are pulled back by the hourly signal current, and

the piston at once falls sharply, bringing the ball with it. But

after a fall of a few feet, the air compressed by the piston acts

as a cushion and checks the fall, the ball then gently and slowly

finishing its descent. The instant of the beginning of the fall is,

of course, the true moment to be noted.

The other dials on the time-desk are for various purposes connected

with the signals. One little needle in a continual state of

agitation shows that the electric current connecting the various

sympathetic clocks of the Observatory is in full action. Another

receives a return signal from various places after the despatch

of the time-signal from Greenwich, and shows that the signal has

been properly received at the distant station, whilst all the many

electric wires within the Observatory or radiating from it are made

to pass through the great key-board, where they can be at once

tested, disconnected, or joined up, as may be required.

[Illustration: THE TIME-DESK.]

The distribution of Greenwich time over the island in this way is

thus a simple matter. The far more important one of the distribution

of Greenwich time to ships at sea is more difficult. The difficulty

lay in the construction of a clock or watch, the rate of which

would not be altered by the uneasy motion of a ship, or by the

changes of temperature which are inevitable on a voyage. Two hundred

years ago it was not deemed possible to construct a watch of

anything like sufficient accuracy. They would not even keep going

whilst they were being wound, and would lose or gain as much as a

minute in the day for a fall or rise of 10° in temperature. This

was owing to the extreme sensitiveness of the balance spring--which

takes the place in a watch of a pendulum in a clock--to the effects

of temperature. The British Government, therefore, in 1714 offered

a prize of the amount of £20,000 for a means of finding the

longitude at sea within half a degree, or, in other words, for a

watch that would keep Greenwich time correct to two minutes in a

voyage across the Atlantic. In 1735, James Harrison, the son of a

Yorkshire carpenter, succeeded in solving the problem. His method

was to attach a sort of automatic regulator to the spring which

should push the regulator over in one direction as the temperature

rose, and bring it back as it fell. This he effected by fastening

together two strips of brass and steel. The brass expanded with heat

more rapidly than the steel, and hence with a rise of temperature

the strip bent over on the steel side. This was the first germ of

the idea of making watches 'compensated for temperature;' watches,

that is, which maintain practically the same rate whether they are

in heat or cold, an idea now brought to great perfection in the

modern chronometer.

[Illustration: HARRISON'S CHRONOMETER.]

The great reward the Government had offered stimulated many men to

endeavour to solve the problem. Of these, Dr. Halley, the second

Astronomer Royal, and Graham, the inventor of the astronomical

clock, were the most celebrated. But when Harrison, then poor and

unknown, came to London in 1735, and laid his invention before them,

with an utter absence of self-seeking, and in the true scientific

spirit, they gave him every assistance.

Harrison's first four time-keepers are still preserved at the

Royal Observatory. He did not, however, receive his reward until

a facsimile of the fourth had been made by his apprentice, Larcum

Kendall. The latter is preserved at the Royal Observatory. There is

a Larcum Kendall at the Royal Institution which is said to have been

used by Captain Cook. Harrison's chronometer was sent on a trial

voyage to Jamaica in 1761, and on its return to Portsmouth in the

following year it was found that its complete variation was under

the two minutes for which the Government had stipulated.

Since Harrison's day the improvement of the chronometer has been

carried on almost to perfection, and now the care and rating of

chronometers for the Royal Navy is one of the most important duties

of the Observatory.

[Illustration: THE CHRONOMETER ROOM.]

A visitor who should make the attempt to compare a single

chronometer with a standard clock would probably feel very

disheartened when, after many minutes of comparison, he had got out

its error to the nearest second, were he told that it was his duty

to compare the entire army here collected, some five hundred or

more, and to do it not to the second, but to the nearest tenth of a

second. Practice and system make, however, the impossible easy, and

one assistant will quietly walk round the room calling out the error

of each chronometer as he passes it, as fast as a second assistant

seated at the table can enter it at his dictation in the chronometer

ledgers. The seconds beat of a clock sympathetic with the solar

standard, rings out loud and clear above the insect-like chatter

of the ticking of the hundreds of chronometers, and wherever the

assistant stands, he has but to lift his eyes to see straight before

him, if not a complete clock-face, at least a seconds dial moving in

exact accordance with the solar standard.

The test to which chronometers are subjected is not merely one of

rate, but one of rate under carefully altered conditions. Thus

they may be tried with the XII pointing in succession to the four

points of the compass, or, in the case of chronometer watches,

they may be laid flat down on the table or hung from the ring or

pendant, or with the ring right or left, as it would be likely to

be when carried in the waistcoat pocket. But the chief test is the

performance of a chronometer when subjected to considerable heat

for a long period. This is a matter of great consequence, since

a chronometer travelling from England to India, Australia, or the

Cape, would necessarily be subjected to very different conditions

of temperature from those to which it would be exposed in England.

They are therefore kept for eight weeks in a closed stove at a

temperature of about 85° or 90°. At one time a cold test was also

applied, and Sir George Airy, the late Astronomer Royal, in one of

his popular lectures, drew a humorous comparison between the unhappy

chronometers thus doomed to trial, now in heat and now in frost,

and the lost spirits whom Dante describes as alternately plunged

in flame and ice. The cold test has, however, been done away with.

It is perfectly easy on the modern ship to keep the chronometer

comfortably warm even on an Arctic expedition. The elaborate cold

testing applied to Sir George Nares' chronometers before he started

on his polar journey was found to have been practically quite

superfluous; the chronometers were, if anything, kept rather too

warm. The exposure of the chronometer in the cooling box, moreover,

was found to be attended with a risk of rusting its springs.

[Illustration: THE CHRONOMETER OVEN.]

Once the determination of the longitude at sea became possible,

it was clearly the next duty to fix with precision the position

of the principal places, cities, ports, capes, islands, the world

over. Of all the work done in this department none has ever been

done better, in proportion to the means at command, than that

accomplished by Captain Cook in his celebrated three voyages. As has

already been pointed out, it is the extent and thoroughness of the

hydrographic surveys of the British Admiralty which have largely

contributed to the honour done to England by the international

selection of the English meridian, and of English standard time, as

in principle those for the whole civilized world. The generosity and

public spirit therefore which led the second Astronomer Royal to

help forward and support his rival, has almost directly led to this

great distinction accruing to the Observatory of which he was the

head.

Three different methods have successively been used in the

determination of longitudes of distant places. In each case the

problem required was to ascertain the time at the standard place,

say Greenwich, at the same time that it was being determined in

the ordinary way at the given station. One method of ascertaining

Greenwich time when at a distance from it was, as stated in Chapter

I., to use the moon, as it were, as the hand of a vast clock, of

which the sky was the face and the stars the dial figures. This is

the method of 'lunar distances,' the distances of the moon from a

certain number of bright stars being given in the _Nautical Almanac_

for every three hours of Greenwich time.

As chronometers were brought to a greater point of perfection, it

was found easier and better in many cases to use 'chronometer runs,'

that is, to carry backwards and forwards between the two stations

a number of good chronometers, and by constant comparison and

re-comparison to get over the errors which might attach to any one

of them.

[Illustration: THE TRANSIT PAVILION.

(_From a photograph by Mr. Lacey._)]

But of late years another method has proved available. Distant

nations are now woven together across thousands of miles of ocean

by the submarine telegraph. The American reads in his morning

paper a summary of the debates of the previous night in the House

of Commons at Westminster. The Londoner watches with interest

the scores of the English cricket team in Australia. It is now

therefore possible for an astronomer in England to record, should

he so desire, the time of the transit of a star across the wires

of his instrument, not only on his own chronograph, but upon that

of another observatory, it may be 2000 miles away. Or, much more

conveniently, each observer may independently determine the error of

his own clock, and then bring his clock into the current, so that

it may send a signal to the chronograph of the other station.

In one way or another this work of the determination of geographical

longitudes has been an important part of the extra-routine work

at Greenwich, part of the work which has built up and sustained

its claim to define 'longitude nought'; and many distinguished

astronomers, especially from the leading observatories of the

Continent, have come here from time to time to obtain more

accurately the longitude of their own cities. The traces of their

visits may be seen here and there about the Observatory grounds in

flat stones which lie level with the surface, and bear a name and

date like the gravestones in some old country churchyard. These are

not, as one might suppose, to mark the burial-places of deceased

astronomers, but record the sites where, on their visits for

longitude purposes, different foreign astronomers have set up their

transit instruments. Now, however, a permanent pier has been erected

in the courtyard, and a neat house--the Transit Pavilion--built over

it, so that in all probability no fresh additions will be made to

these sepulchral-looking little monuments.

It might be asked, What reason is there for a foreign observer to

come over to England for such a purpose? Would it not be sufficient

for the clock signals to be exchanged? But a curious little fact

has come out with the increase of accuracy of transit observation,

and that is, that each observer has his own particular habit or

method of observation. A hundred years ago, Maskelyne, the fifth

Astronomer Royal, was greatly disturbed to find that his assistant,

David Kinnebrook, constantly and regularly observed a star-transit

a little later than he did himself. The offender was scolded,

warned, exhorted, and finally, when all proved useless to bring

his observations into exact agreement with the Astronomer Royal's,

dismissed as an incompetent observer. As a matter of fact, poor

Kinnebrook has a right to be regarded as one of the martyrs of

science, and Maskelyne, by this most natural but mistaken judgment,

missed the chance of making an important discovery, which was not

made until some thirty years later. Astronomers now would be more

cautious of concluding that observations were bad simply because

they differed from what had been expected. They have learnt by

experience that these unexpected differences are the most likely

hunting-ground in which to look for new discoveries.

In a modern transit observation with the use of the chronograph

it will be seen at once that before the observer can register a

star-transit on the chronograph, he has to perceive with his eye

that the star has reached the wire, he has to mentally recognize

the fact, and consciously or unconsciously to exert the effort of

will necessary to bring his finger down on the button. A very slight

knowledge of character will show that this will require different

periods of time for different people. It will be but a fraction

of a second in any case, but there will be a distinct difference,

a constant difference, between the eager, quick, impulsive man

who habitually anticipates, as it were, the instant when he sees

star and wire together, and the phlegmatic, slow-and-sure man

who carefully waits till he is quite sure that the contact has

taken place, and then deliberately and firmly records it. These

differences are so truly personal to the observer that it is quite

possible to correct for them, and after a given observer's habit has

become known, to reduce his transit times to those of some standard

observer. It must, of course, be remembered that this 'personal

equation' is an exceedingly minute quantity, and in most cases is

rather a question of hundredths of seconds than of tenths.

It will be seen from the foregoing description how little of what

may be termed the picturesque or sensational side of astronomy

enters into the routine of the Time Department, the most important

of all the departments of the Observatory. The daily observation of

sun and of many stars--selected from a carefully chosen list of some

hundreds, and known as 'clock stars'--the determination of the error

of the standard clock to the hundredth of a second if possible, and

its correction twice a day, the sending out of time signals to the

General Post Office and other places, whence they are distributed

all over the country; the care, winding, and rating of hundreds of

chronometers and chronometer watches, and from time to time the

determination of the longitude of foreign or colonial cities, make

up a heavy, ceaseless routine in which there is little opportunity

for the realization of an astronomer's life as it is apt to be

popularly conceived.

Yet there is interest enough in the work. There is the charm

which always attaches to work of precision, the delight of using

delicate and exact instruments, and of obtaining results of steadily

increasing perfection. It may be akin to the sporting passion for

record-breaking, but surely it is a noble form of it which has led

the assistants, in recent years, to steadily increase the number of

observations in a normal night's work up to the very limit, taking

care the while that their accuracy has in no degree suffered. In

longitude work also 'the better is the enemy of the good,' and there

is the ambition that each fresh determination shall be markedly

more precise than all that have preceded it. The constant care of

chronometers soon reveals a kind of individuality in them which

forms a fresh source of interest, whilst if a man has but a spark

of imagination, how easily he will wrap them round with a halo of

romance!

Glance through the ledgers, and you will see how some of them have

heard the guns at the siege of Alexandria, others have been carried

far into the frozen north, others have wandered with Livingstone or

Cameron in the trackless forests of equatorial Africa.

More striking still are those pages across which the closing line

has been drawn; never again will the time-keeper there scheduled

return to the kindly inquisition of Flamsteed Hill. This sailed away

in the Wasp, and was swallowed up in the eastern typhoon; that went

down in the sudden squall that smote the Eurydice off the Isle of

Wight; these foundered with the Captain. The last fatal journey of

Sir John Franklin to find the North-West Passage leaves its record

here; the chronometers of the Erebus and Terror will never again

appear on the Greenwich muster roll. Land exploration claims its

victims too. Sturt's ill-fated expedition across Australia, and

Livingstone's last wandering, are represented.

[Illustration: 'LOST IN THE BIRKENHEAD.']

Sometimes an amusing entry interrupts the silent pathos of these

closed pages. 'Lost by Mr. Smith on the coast of Africa,' reads at

first sight like a rather thin attempt of some one to shift the

responsibility of his own carelessness on to the broad shoulders of

Mr. Nobody. In reality it probably gives a hint of the necessary,

dangerous, and exciting work of slave-dhow chasing which gives

employment to our ships on the African coast. 'Mr. Smith' was no

doubt a petty officer who was told off to carry the chronometer for

a boat's crew sent to search for a slave-dhow up some equatorial

estuary. Probably the dhow was found, and the Arabs who manned it

gave so stout a resistance that 'Mr. Smith' and his men had other

things to do than take care of chronometers before they could

overcome them. We may take it that the real story outlined here was

one of courage and hard fighting, not of carelessness and shirking.

Stories of higher valour and nobler courage yet are also hinted:

the calm discipline of the crew of the Victoria as she sank from

the ram of the Camperdown, the yet nobler devotion of the men of

the Birkenhead, as they formed up in line on deck and cheered the

boats that bore away the women and children to safety, whilst they

themselves went down with the ship into the shark-crowded sea.

'There rose no murmur from the ranks, no thought

By shameful strength, unhonoured life to seek;

Our post to quit we were not trained, nor taught

To trample down the weak.

'What followed, why recall? The brave who died

Died without flinching in that bloody surf.

They sleep as well beneath that purple tide

As others under turf.'

The Royal Observatory, Greenwich: A Glance at Its History and Work · 第 6 / 13 章