Graham's Magazine, Vol. XXX, No. 1, January 1847Various
General
Graham's Magazine, Vol. XXX, No. 1, January 1847
Various
Literature -- Periodicals; Literature, Modern -- 19th century -- Periodicals
“The reason of which is,” resumed Mulford, “because the clocks of each
place keep the time of that place. Now, it is different with the
chronometers, they are set in the observatory of Greenwich, and keep the
time of Greenwich. This watch chronometer was set there, only six months
since, and this time, as you see is near nine o’clock, when in truth it
is only about four o’clock, here, where we are.”
“I wonder you keep such a watch, Mr. Mulford!”
“I keep it,” returned the mate smiling, “because I know it to keep good
time. It has the Greenwich time; and, as your watch has the New York
time, by comparing them together, it is quite easy to find the longitude
of New York.”
“Do you, then, keep watches to compare with your chronometers?” asked
Rose, with interest.
“Certainly not, as that would require a watch for every separate part of
the ocean, and then we should only get known longitudes. It would be
impracticable, and load a ship with nothing but watches. What we do, is
this: We set our chronometers at Greenwich, and thus keep the Greenwich
true time, wherever we go. The greatest attention is paid to the
chronometers, to see that they receive no injuries, and usually there
are two, and often more of them, to compare one with another, in order
to see that they go well. When in the middle of the ocean, for instance,
we find the true time of day at that spot, by ascertaining the height of
the sun. This we do by means of our quadrants, or sextants; for, as the
sun is always in the zenith at twelve o’clock, nothing is easier than to
do this, when the sun can be seen, and an arc of the heavens measured.
At the instant the height of the sun is ascertained by one observer, he
calls to another, who notes the time on the chronometer. The difference
in these two times, or that of the chronometer and that of the sun,
gives the distance in degrees and minutes, between the longitude of
Greenwich and that of the place on the ocean, where the observer is; and
that gives him his longitude. If the difference is three hours and
twenty minutes, in time, the distance from Greenwich is fifty degrees of
longitude, because the sun rises there three hours and twenty minutes
sooner in London, than in the fiftieth degree of west longitude.”
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account