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LONGCAMP.COM'S
NOVA ALBION ANNEX
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An Experiment in the
Determination of
Latitude
by Bob Graham
In his book, Drake's Bay, Unravelling California's
Greatest Maritime Mystery, regarding Francis Drake's
ability to determine his latitude for those positions taken
on land, Brian Kelleher has shown by statistical analysis
that "...the mean deviation between the reported
position and the actual latitude is about minus two minutes
within a range of minus fifteen minutes to plus fifteen
minutes and the standard deviation is about eleven
and a half minutes." This in not only remarkable accuracy
for the late sixteenth century, but it provides powerful
evidence in the search for the actual landing site that
Drake made on the coast of California in 1579. Brian
Kelleher's has concluded that Drake did not land at what is
now called Drake's Bay, but rather at Campbell Cove on
Bodega Head.
Subsequent to the publication of Brian's book, and after
hearing Brian speak on the subject, I embarked on a study of
sixteenth century navigation which resulted in the paper
DETERMINATION OF LATITUDE BY
FRANCIS DRAKE ON THE COAST OF CALIFORNIA IN 1579
which is posted
here. That paper not only supports Brian's conclusion
that Drake landed at Campbell Cove, but it explains the
reasons for, and quantifies the errors that Drake
unavoidably made which show up in Brian's statistical
examination of the reported latitudes. On September 2, 1999,
the following experiment was conducted to test the
conclusions drawn in the paper.
An astrolabe of 9 inches diameter was constructed of heavy
card stock. The lower right quadrant was divided into 90
degrees. The alhidada, also constructed of card
stock, has two vanes, or sights, one inch square, each
pierced in the center by a common paper punch. Like
sixteenth century astrolabes, this astrolabe is suspended by
a double articulation that allows it to hang vertical in
both vertical planes, but does not allow it to swing in the
horizontal plane. It is accurately made, but of course, the
materials are totally unsuitable for wind and weather.
Examination for index error by back sighting
showed that it was smaller than I was able to detect. As
explained in the article referred to, with an astrolabe
there is no correction necessary for dip of the
horizon (it is its own horizon, referrenced by gravity)
or semi-diameter of the sun (it takes the center of
the sun). The corrections forparallax and
refraction are too small to matter in this case with
this or similar instruments).
About a quarter to noon on September 2 (with noon occurring
at approximately 12:56 A.M. PDT in my longitude (119 West),
I began to track the sun. The alhidada was moved to
keep the light passing through the fore sight centered in
the hole of the back sight. The holes in the two, being of
equal size, left a halo of light around the edge of the hole
of the back sight. This halo of light, and the same on the
vane itself around the shadow of the front vane, were of
great assistance in keeping the alhidada constantly
aligned. Note the spot of light on the back sight in the
photo at the bottom of the page.
As noon approached, less frequent correction was
necessary. Then, for several minutes (at this resolution
time is not too critical), the sun seemed to stop its ascent
and remain stationary. Gradually it became obvious that the
sun was descending and that noon had indeed occurred and
that further movement of the alhidada was
unnecessary.
The index on the alhidada was found to be
indicating 59 1/2 degrees, the observed altitude of
the sun, which I called 59° 30'. Referring to an online
site which provides solar
declinations, I found the declination for
noon at Greenwich for the day to be 8° 09'. This
subtracted from the observed altitude gives 51°
21' for the true altitude of the sun. Since
Sacramento is about 8 hours (1/3 of the way around the
earth) behind Greenwich, I needed to correct for longitude
121° W. The difference in declination between September
2nd and September 3rd is about 18', so 1/3 of that was added
to the true altitude, so that it became 51° 27'.
Subtracting 51° 27' from the 90°, the result was
latitude 38° 33' North. The actual latitude of
my back yard in Sacramento is in fact 38° 33' 06".
What
would Francis Drake have determined had he been here on
this date in the 20th century with his instruments and
William Bourne's A Regiment for the Sea?
Drake would have read 59 1/2 degrees just as I did. He
would have called it 59° 30' as I did. He would have
referred to Bourne's Tables of Declination and found the
figure for the date (23rd July, old calander) to be 8°
18' declination. Not quite right, as explained in the
original article, because of errors in tables of the time.
Drake would have subtracted the declination from his
observed altitude and found the true altitude
to be 51° 48'.
Drake could not correct the declination for
longitude. We know that he did not, and could not, because
when he had returned to England after the circumnavigation,
he stated that the day was, "...Monday in the just and
ordinary reckoning of those that had stayed at home in one
place or country, but in our computation was the Lord's Day,
or Sunday." Therefore, he would have subtracted his true
altitude from the 90° of the celestial pole,
and determined the latitude to be 38° 12'.
In spite of the accuracy of Drake's instruments, and his
ability to use them, because of errors in the best
declination tables of his time, and his inability to correct
for longitude, his determination of latitude in this
particular case would have been, on this day of the year, at
this longitude, 11' too low.
I
have since made a new mariner's astrolabe of more
substantial materials (a plastic bread board). I find that
it is possible to estimate 1/4, 1/3, 1/2, 2/3, 3/4 degrees
quite accurately. That
gives readings of 15', 20', 30', 40', 45, and anything just
less than or more than a degree can be called 1/8, or 07'
30". Depending on the day, my determinations during
September and early October have all been within 5 minutes
of latitude, but that is the extreme error, and most are
within 3 minutes or less (about 3 miles).
I have also experimented with determinations from the
pole star.There are four positions during the 24 hours that
Drake could have used for the best results--two 0 correction
times and two maximum correction times. The 0 correction
positions are when a line between ursa major an cassiopea is
horizontal to the horizon; the max correction is with this
line vertical, or perpendicular to the horizon.The 0
correction times seem like a good bet, but I find, so
far, that it is much more difficult to shoot the north star
and center it. This is eye to star thru the holes in the
sights. Holding the instrument above eye level is also
dfficult. I think it is +/- 15 minutes, but I don't really
have a good sky for observing. The other problem with the 0
correction time is that the rate of declination change to
either side is rapid.
At the positions of maximum correction the declination
change is the slowest, but there is the extra error from the
various Sixteenth Century miscalculations of the distance of
polaris from the celestial pole. These distances ranged from
4 degrees 9 minutes to 3 degrees 30 minutes. Just after
Drake's voyage, the number was refined by Edward Wright to 2
degrees 52 minutes.
The pole star has since moved closer to the pole, and the
maximum correction today is about 1 degree added or
subtracted from the observed altitude of polaris. Drake
would have known from comparisons of determinations that the
best he could expect to do with the pole star would be a 30
mile fix compared to a 5 or 10 mile fix by the sun. Indeed,
William Bourne, in a REGIMENT FOR THE SEA, cautioned against
the use of Polaris (See previous article). Polaris would be
very useful at sea though, for a fix several times during
the night!
In working through recorded polaris sights taken by John
Charles Frémont in the Sierra Nevada in the winter of
1844, I have found that he chose to make his shots at the
published times of greatest correction. This meant rising at
very inconvenient hours, but the apparent change in position
is slowest at these times; important because he was having
problems with his chronometer maintining its rate, so he did
nor have his time precisely. The correction needed was often
nearly 1 1/2 degrees.
It is easier and more accurate to measure the sun with
the astrolabe because; (1) it is a projection, and (2) the
position from which the reading is taken is comfortable and
steady. I find that a seated position, with the elbows on
the knees, and the astrolabe hanging just above ground level
is the best position.
For an actual on-site determination of latitude at Campbell
Cove, see A Day at the
Cove.
Timothy Burke has an interesting page The Astrolabe
on the De Soto Expedition.
interest, comments, or
questions.
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