Mercury,
January/February 1997 Table of Contents
Tom
Van Flandern
Meta Research
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Trade-off.
As viewers venture away from the center line of the eclipse
path, the eclipse lasts for a shorter time (smooth line), but
edge effects such as Baily's beads persist for longer (spiked
line). The duration of edge effects is longest when viewers
are about 95 percent of the way from the center line to the
edge of the eclipse path. From that vantage point, the eclipse
lasts a third as long as it does at the center line. Diagram
by Tom Van Flandern. |
Traditionally,
eclipse observers have flocked to the very center of the eclipse
path, where the Moon obscures the Sun for the longest time. Yet
eclipses are much more spectacular when viewed from near the edge
of the path.
In
1925, the shadow of a total solar eclipse passed over New York City.
Ernest Brown, an expert on lunar motion, planned on observing the
eclipse from near the center line with the many other astronomers
who did not wish to miss a single second of totality. Brown also
put out an appeal to the residents of New York to climb to the roofs
of their apartment buildings and report on whether the eclipse was
total or not, so that he could determine the exact location of the
path edge. Many who saw the eclipse from near the path edges, even
those slightly outside the shadow of totality, were thrilled by
the experience. But another half-century would pass before astronomers
realized that Brown had sacrificed the best view of the eclipse
to those citizen volunteers.
For
two centuries, astronomers have been able to predict the location
of the narrow track across the surface of the Earth made roughly
once a year by the Moon's shadow. They have then traveled into the
path of the shadow, where they could observe a total eclipse. But
until fairly recently, astronomers simply assumed that the best
place to be was in the middle of the path. The eclipse is longest
on the center line of the path; the rare view of the Sun's beautiful
white outer atmosphere, the corona, which can be seen only during
eclipses, is also longest there. So without much further thought,
astronomers concluded that all interesting phenomena were best seen
from the center line.
That
remained the situation until the 1960s, when astronomer David Dunham
popularized observations of grazing occultations of stars by the
Moon in effect, short eclipses of stars by the edge of the
Moon. Grazes in general, and edge proximity in particular, proved
to have advantages for observation and data collection. In March
1970, Dunham, Joan Bixby-Dunham, and I tested this idea on a solar
eclipse for the first time.
For
just a single example of how wrong the old notion was, consider
the most colorful part of the Sun's atmosphere: the innermost part
above the Sun's visible disc, the chromosphere. On the eclipse center
line, the chromosphere is visible only for a few seconds between
the disappearance of the Sun's visible disc and the moment when
the chromosphere itself disappears behind the Moon. During those
precious few seconds, astronomers have tried to take spectra of
the chromosphere in order to learn its composition. So brief is
the appearance that successful results are referred to as the flash
spectrum [see "Observing the Sun During Eclipses," July/August 1981,
p. 108].
How
foolish those astronomers might have felt if they had realized they
could have been watching from near the edges of the path. There,
the disc of the Moon slides by the disc of the Sun for a prolonged
period and the chromosphere remains visible for 90 seconds
or more. Because of the chromosphere's rich redness, eclipse photos
taken from near the path edges have more color in them than do photos
from the center line.
It
is not just the chromosphere view that is prolonged near the path
edges (see diagram above). The mysterious "shadow bands" are far
more likely to be seen from sites near the edges, and they usually
last two to five times longer than on the center line. The diamond
ring and Baily's beads will usually last up to 10 times longer.
Moreover, while just a few beads may form and stay in place for
center-line viewers, edge viewers can see numerous beads form and
dissolve constantly; they seem to travel along the limb as the two
discs glide past one another. Finally, prominences giant
eruptions from the Sun's surface can be seen for longer.
For
most total solar eclipses:
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As one moves off the center line by as much as 20 percent of
the distance to the edge, the average duration of totality drops
merely 2 percent. The true duration of totality is governed
by irregularities (mountains, craters, valleys) at the Moon's
limb, so the longest eclipse may occur almost anywhere within
this central 20-percent zone. Precise positioning on the center
line has no real value.
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The best overall views of the eclipse and related phenomena
are generally seen at 95 percent of the way to the edge of the
path, where the duration of totality is one-third of the center-line
duration.
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Usually, people who still view from the center line do so for
historical reasons, or because the relative merits of the choice
have never been presented to them. They may not realize they
may have missed the most spectacular view. Astronomers who in
recent years have gone both to the center line and to the path
edges seldom go back to the center line.
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Perhaps Guy Ottewell, veteran eclipse viewer and author of the
annual Astronomical Calendar, captured it best: "In 1991 I found
[viewing from the edge] to work dramatically well. I watched
shadow-bands unmistakably for the first time; the Diamond Ring
was overpowering; and the red chromosphere, which I had never
before glimpsed, lingered throughout totality."
TOM
VAN FLANDERN is an astronomer at Meta Research in Washington, D.C.
He directed the Celestial Mechanics Branch of the United States
Naval Observatory from 1978 to 1983. He is author of the 1993 book,
Dark Matter, Missing Planets and New Comets. Van Flandern will lead
expeditions, open to the public, to the edge of the February 1998
(Galapagos Islands) and August 1999 (Europe) eclipses. His email
address is metares@well.com.
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