Introduction
Most lunar eclipses observed and studied by the Calwell Lunar Observatory have been either total or partial, that is where the moon passes through the most dense central part of the shadow cast by the earth, known as the umbra. In 1998 it was shown that it is possible to observe and capture images of the less dense outer penumbral shadow during a lunar eclipse where the moon enters only the feint penumbra.
As there are three penumbral lunar eclipses in 2002, my experiment to explore images of the low density penumbra is continued, where I hope to analysing the density and geometry of the elusive penumbral shadow. The three eclipses are illustrated below by the diagrams produced by Fred Espanak .

This eclipse will be visible in North America except in the east, Central America, South America except the extreme east, India, Australia, New Zealand, most of Antarctica, eastern Asia and the Pacific Ocean. The world map produced by Fred Espenak, shows the area where this eclipse will be visible (in the unshaded parts).


Exact times have been computed for the expected moon contacts or departure from the penumbra with an estimate of the variation in each of these timings using an oblateness for the penumbral equal to that observed for the umbra. This oblateness was derived from the analysis of over 30 recent lunar eclipses where a value of 1/102 has been found for the out-of- roundness of the umbra due to the oblateness of earth's upper atmosphere. These timing variations are shown in Table 1, compared with the standard contact times where the only allowance made is for the oblateness of the earth's geoid (using the classical value of 1/298.257). This classical value ignores the effects of the flattening of the atmosphere.
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