The measures
of four images of the recent total lunar eclipse indicated that the umbral
semi-diameter decreased towards fourth contact and it is expected that this was
due primarily to increased cloud cover, causing reduced transparency at a
longitude near 90 degrees WEST of the observing point.
The observations were conducted
at longitude 20 degrees East, so the atmospheric conditions at 70 degrees West
are of interest. The only known data available is from the TOMS satellite, and
two charts are presented below from this source showing Total Ozone on the eclipse date and secondly, the Reflectivity of the atmosphere also on the eclipse
date.
It can be seen at the longitude of interest that the total ozone over the
east coast of the USA is near 400 Dobson units with the area preceding it over
the North Atlantic at around 275 to 380 Dobson units.
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It can be seen at the longitude of interest that the reflectivity over the
east coast of the USA is low at around 30-40 % with a clearer area preceding it
over the North Atlantic.
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Conclusion
The TOMS data is taken over a period of time
so it is impossible to refine the effect that total ozone and reflectivity
would influence the transparency of the upper atmosphere during the end of this
lunar eclipse where the umbral semi-diameter change was greatest.
However, there is obviously a change in the
atmospheric conditions at the longitude of observation and that at 90 degrees
West of where the images were captured.
One could imply that this would cause the
umbral change during this lunar eclipse, however, further study and correlation
of data are obviously necessary.
Prepared by the Calwell
Lunar Observatory, Australia / 2001 February 5