Total Lunar
Eclipse - 10 December 11
|
| stage | Phase | time (IST) |
| 1 |
Moon enters penumbra |
17:03:23 |
| 2 |
Moon enters umbra |
18:15:13 |
| 3 |
Start of totality |
19:36:26 |
| 4 |
Maximum eclipse |
20:01:50 |
| 5 |
End of totality |
20:27:16 |
| 6 |
Moon leaves umbra |
21:48:09 |
| 7 |
Moon leaves penumbra |
22:00:12 |
The diagram below shows various stages of passage of
the Moon through the Earths shadow corresponding to the numbers above
Duration of the Penumbral Phase :5h 59m 53s
Duration of the Umbral Phase :3h 32m 54s
Duration of the total Phase :0h 52m 16s

The side of the Earth as seen from the Moon at
various stages of eclipse
The eclipse geometry
A lunar eclipse takes
place when the Moon enters the shadow of the Earth.
On this night the
Earth is directly between the Moon
and the Sun,
blocking the
sunlight reaching the Moon. Or casting its shadow on the Moon.
The event obviously takes place on the full moon night. On this night the
Moon and the Sun are in opposite side of the Earth.
The diagram below shows the geometry of total Lunar Eclipse or what is technically called In this case the the Sun, Earth and the Moon are nearly on one straight line. The Moon is in total shadow of the Earth or it is in Umbra region.

(The diagram above not to the scale and it is is for the
purpose of illustration only.)
You can visualize the Umbra and Penumbra region by looking at a shadow of a disk (say 50p coin) kept far away from the sheet. You can see that the central part of the shadow is dark but towards the edge you can see a defuse shadow.
Why would the Moon look red in colour during the
total phase
The
Earth's atmosphere plays it's role here. If the Earth had no
atmosphere the Moon would have 'simply vanished' from the sky at the
total phase. However the Earth's atmosphere plays a role - exactly the
same way it does with the rising or setting Sun (or Moon).

As the sunlight passes through the atmosphere of the Earth, the light is scattered and bent slightly. The light is scattered by the constituent atmospheric particles. The blue component of the sunlight is scattered most but the red rays pass through. Absence of the blue rays and presence of the red rays make rising or setting Sun appear red in colour. And the bending of like takes place as it goes from one medium to other, it this case from vacuum to the Earth's atmosphere.
Some of the red rays escape or come out of the Earth's atmosphere reaching the Moon and giving the Eclipsed Moon its red hue.
As indicated above the Earth's atmosphere contaminated by the volcanic ash is likely to have its pronounced effect on how dark the eclipsed moon would be..
Why we do not have a lunar eclipse every full moon?
This is because the plane in which the Moon orbits the Earth is slightly
inclined to the plane in which the Earth orbits the Sun. The planes are
inclined by 5.145 degrees.
The diagram below is nearly to the scale showing the relative sizes of the Earth (the blue dot) - the Moon (the red dot) and the distance between them (the black line). The area between the red lines the inclination zone of the lunar orbit. At any given time the moon will be between this limit at average distance of 384403 k.m. The blue lines shows the shadow zone of the Earth. Only when the Moon is in the shadow zone we observe the lunar eclipse.

When the Moon is between blue and red lines we see the full moon but no eclipse. As one can see form the above diagram The Earth Moon distance is very large and the orbital inclination is just about 5 degrees that on the night of full moon the the Moon and the Sun are in opposite side of the Earth and therefore the side of the Moon facing the Earth is seen fully illuminated by the sunlight.
How many eclipses in a year?
It can be calculated that maximum number of eclipses possible in a year is
7, of which 4 are solar and 3 lunar or 5 solar and 2 lunar. The least
possible eclipses during a year is 2, and these are both solar eclipses..
The year 2011 has six eclipses - four solar eclipses and 2 lunar.
|
January 4 |
partial solar eclipse |
|
June 1 |
partial solar eclipse |
|
June 15 |
Total Lunar eclipse |
|
July 1 |
partial solar eclipse |
|
November 25 |
partial solar eclipse |
|
December 10 |
Total Lunar eclipse |
Can I or my
students do some astronomical observations?
Yes of course. With
naked eyes, binoculars or low power telescope on can do exercises in
crater timing and estimating the eclipse darkness on Danjon scale.
Please visit NASA web site by Fred Espenak Danjon Scale and Crater timings
A
quick note on Danjon scale
The French astronomer Andre-Louis Danjon proposed a useful five
point scale for evaluating the visual appearance and brightness of the
Moon during total lunar eclipses. 'L' values for various luminosities
are defined as follows:
L = 0 Very dark eclipse.
Moon almost invisible, especially at mid-totality.
L = 1 Dark Eclipse, gray or brownish in coloration.
Details distinguishable only with difficulty.
L = 2 Deep red or rust-colored eclipse.
Very dark central shadow, while outer edge of umbra
is relatively bright.
L = 3 Brick-red eclipse.
Umbral shadow usually has a bright or yellow rim.
L = 4 Very bright copper-red or orange eclipse.
Umbral shadow has a bluish, very bright rim.
The assignment of an 'L' value to lunar eclipses is best done with the naked eye, binoculars or a small telescope near the time of mid-totality.