I’m sure
many people know this, but a “great circle” is a circle that goes clear around
the entire globe, and whose center is at the center of the globe. A “meridian”,
on the other hand, is a great circle that passes through the poles. Lines of
longitude are meridians, for example, while the Equator is a great circle. And
the “Prime Meridian” is the line of longitude that goes through both poles ..
and right through the Greenwich Observatory.
On the other side of the planet is the Prime Meridian also called the
“International Date Line”.
If you know the exact time the sun rises where
you happen to be, then you know which line of longitude you are on. Easy as
that (with the usual caveats, refraction, etc.) … but only if you know exactly,
to the second, what time it is. And that was why lots of seamen died before
John Harrison invented his chronometer … they didn’t know what time it was, so
they didn’t know where they were. The
Longitude Prize was a reward offered by the British government for a simple and
practical method for the precise determination of a ship's longitude. The
prize, established through an Act of Parliament (the Longitude Act) in 1714,
was administered by the Board of Longitude.
Harrison's invention of a clock that could keep correct time, while at
sea, and the concept that time equaled longitude won the £20,000 (worth well
over a million dollars in todays money) for a method that could determine
longitude within 30 nautical.
To use time
to determine the longitude of a ship a map of the world is divided into 24
segments, each representing one hour.
The clock on board the ship was set to the same time at Greenwich, now
called Greenwich Mean Time, then as the ship sailed east or west of Greenwich
to determine their longitued they had only to find the local time using a
sexton. To do this they use the noonday
sun and the horizon of the sea, when it was getting near noon the navigator
would start measuring the angle between the sun and the horizon. He would keep taking the measurement until
the angle stoped increasing and started to decrease. That point was local noon. Then all he had to do was to count the hours,
minutes, and seconds on his chart from Greenwich and that point was his
longitued. For the latitude he had to
wait until dark and use either the North Star or the Southern Cross is
depending which side of the equator he was.
The further north the ship went the higher went the North Star from the
horizon. So in those days a sailor could only know where he was precisely east to west in the world once a day, the rest of the day was guess work called dead reckoning.
To close
this post I would like to talk about the earth's wobble. Throughout the year the earth wobbles on its
axes as it goes around the sun, with the results that the sun appears to set
way down in the south in the winter. As it goes south each day gets shorter while each night gets longer, when it get as
far south as it will go we have the longest night of the year, and that night
is called the winter soloist. After that
night it starts its moves to the north for the summer with each day getting
longer and each night getting shorter, when it gets as far north as it will go
we have the longest day of the year which is called the summer soloist. Then it starts on its journey back to the
south. On the 22nd of September the sun
will be its halfway point on its journey south and marks the first day of
Fall. On this day the day is called the
fall equinox and night and day are of equal length. This will happen again next spring with the
sun on its way back north, but it will be called the spring equinox. For Christians the first Sunday after the
first full moon after the spring equinox is Easter.
The Greek
astronomer, Hipparchus of Nicea by comparing observations more than a century
apart, Hipparchus proposed that the axis around which the heavens seemed to
rotate shifted gradually, though very slowly.
Around the year 130 BC, Hipparchus compared ancient observations to his
own and concluded that in the preceding 169 years those intersections had moved
by 2 degrees. How could Hipparchus know the position of the Sun among the stars
so exactly, when stars are not visible in the daytime? By using not the Sun but
the shadow cast by the Earth on the moon, during an eclipse of the Moon! During
an eclipse, Sun, Earth and Moon form a straight line, and therefore the center
of the Earth's shadow is at the point on the celestial sphere which is exactly
opposite that of the Sun.
And we think
that we are smart today.
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