Possible Effect of Mount Reventador`s Nov
03, 2002 Eruption on the
Brightness of the 2003 and 2004 Total Lunar
Eclipses
by
Helio C. Vital (Eclipses Section/REA/Brazil)
The idea of using total lunar eclipses as
indicators of global levels of aerosols of volcanic origin was originally
proposed by Richard Keen who has successfully proved its
feasibility. According to Keen, strong volcanic explosions may darken total
lunar eclipses considerably. The author has used published data as well as REA`s observations covering a total of 24 eclipses
(1956-2001) to get a correlation between umbral eclipse magnitude (Umag)
and the Moon`s magnitude (Mag) and apparent radius (SD, in arc minutes) at
mid-eclipse. The events found to be definitely affected by volcano explosions
were left out of the input data used to obtain a second similar correlation for
aerosol-free events only. The resulting improved correlation (r2=0.88)
is:
Mag = -1.4 + 4.3 Umag - 5 log(SD)
It has been used it to predict the Moon`s magnitude.
Comparing such predictions with estimates made by several REA`s members who used a perfected version of the reversed binoculars method to obtain the Moon`s magnitude during the eclipses in May and
Nov., 2003 and May and Oct., 2004 yielded the table and plot shown below. The
magnitude differences found have been plotted as a function of time elapsed
since the explosion of Mount Reventador in Ecuador on November 03, 2002 (volcanic
explosivity index=4) that injected a significant amount of aerosols into
Earth`s stratosphere.
|
Eclipse Date |
Umbral Eclipse Mag (Umag) |
Moon`s Observed Mag (O) |
Moon`s Predicted Mag (P) |
Δ (O-P) Mag |
Optical Thickness (±0.005) |
|
May 16, 2003 |
1.13 |
-2.6 |
+0.5 |
+0.013 |
|
|
Nov.09, 2003 |
1.02 |
-2.8 |
-0.5 |
-0.013 |
|
|
May 04, 2004 |
1.31 |
-2.3±0.3 |
-1.8 |
-0.5 |
-0.013 |
|
Oct. 28, 2004 |
1.31 |
-2.2±0.2 |
-1.7 |
-0.5 |
-0.013 |

Since the amplitude of the effect is very small (with a maximum 0.5
magnitude loss), the possibility that it is due to experimental errors alone
cannot be ruled out. However the data seem to consistently indicate that two
years after the eruption the global level of stratospheric volcanic aerosols has
dropped to a level even lower than the one assigned as šaerosol-freeš by the
correlation.
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to REA`s Eclipses: Lunissolar
Observational
Astronomy Network (REA/Brazil)
Copyright
2004@Helio C. Vital
Authorized
reproduction of this material is allowed provided due credit is given to the
author