(meteorobs) the population indices
RainerArlt
rarlt at aip.de
Mon Jan 31 05:56:13 EST 2005
Hello Sahar and all,
> [...]
> This equation delivers a set of corresponding <Delta m>. Using Table,
> we converted <Delta m> into population indices (this will give us the
> r-values for our main effective observing periods.).
> r <Delta m> r <Delta m>
> 1.5 5.830 3.1 2.750
> 1.6 5.301 3.2 2.682
> 1.7 4.894 3.3 2.618
> 1.8 4.568 3.4 2.559
> 1.9 4.298 3.5 2.503
> 2.0 4.069 3.6 2.450
> 2.1 3.872 3.7 2.400
> 2.2 3.700 3.8 2.353
> 2.3 3.549 3.9 2.308
> 2.4 3.413 4.0 2.266
> 2.5 3.291 4.1 2.226
> 2.6 3.180 4.2 2.187
> 2.7 3.079 4.3 2.151
> 2.8 2.987 4.4 2.116
> 2.9 2.902 4.5 2.082
> 3.0 2.823
>
> But we wants to know where this table come from and how can we
> account them. Can you tell us about it?
The conversion table is obtained by computer simulations. One does
the opposite way of determining the population index: one assumes
a population index. So the true distribution of meteors over
magnitudes is known (exponential). You generate random numbers
with this distribution. You also have to know the perception
probabilities of a meteor at a given distance from the limiting
magnitude. These are taken from Koschack & Rendtel
(http://www.imo.net/articles/results.html), which has recently
been reviewed by Pete Gural an WGN. You have to convolve the
meteors generated also with this distribution. After generating
a million meteors, you get a distribution as if it would have
been observed. You compute the average Delta-m and get the
value in the second column of the Table.
Best wishes,
Rainer
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