This page represents work in progress on looking at the energy
resolution ofthe VERITAS array. The basic idea is to use the wavefront
timing information todetermine the altitude of maximum Cherenkov
emission. Our
Compton symposiumpaper of wavefront timing suggests a correlation
between structure inthe Cherenkov wavefront and the altitude of
emission of the photons. Thecorrelation is strongest near the shower
center, and least at the well knownannulus. In the VERITAS array, we
will be able to determine the location of theshower core, thus we can
use the timing information to estimate the altitude ofmaximum emission.
With this information we should be able to improve on ourenergy
resolution. Motivated by the spectral work of Carter-Lewis and
Mohanty,we have constructed an energy estimator. In our case the
estimator is based onrather simple geometric arguments. Our energy
estimator is given by:
e_est = constant * ( b**2 + h**2) * size
where b is the impact parameter (which will be determined by the
array), h isthe mean emission altitude (which will be determined by the
timing) and size isthe amount of light in the image (the same as our
cuurent size parameter).
The following are a series of plots exploring these ideas. The monte
carlo dataset used is the gamma ray data set at an altitude of 1300 m.
The triggercondition was 15 pe's on three or more pmt's. All plots are
selected for smallimpact parameters (b<40m) and for indident energy
greater than 300 GeV. In somecases additional shape cuts have been
made, either an alhpa cut (alpha < 15)alone, or what I call "simple
shape cuts" which are given by: alpha less than 15,length between 0.1
and 0.44, and width is less than 0.16.
The first set of plots is of the energy estimator, e_est, given
above forvarious cuts. These plots use an un-normalized e_est (i.e. the
constant = 1) Next is a series of plots showing the distribution of
differencesbetween the energy estimated by e_est (normalized as
described below) and the actual value of the energy fromthe monte
carlo. To findthe normalizing constant in the above equation, I plotted
size*(b**b+h**2)/(monte carlo energy) and fitted this to a gaussian.
The meanof the gaussian is the value of the normalization constant.
- Figure 1: This is a plot of the
unnormalized e_est(that is the constant = 1) with no image shape cuts.
Superimposed on this plotare the distributions os e_est for events
selected by monte carlo energies of400, 600, 800 and 1000 GeV.
- Figure 2: The same as figure 1, but with
analph cut of alpa <15.
- Figure 3: The same as figure 1 but with
simpleshape cuts as described above.
- Figure 4: Energy residuals energy,
e_est -energy, for no image shape cuts.
- Figure 5: The same as figure 4, but
with simple image shape cuts
The standard deviation of the gaussian fit to the energy residuals
in figure5 suggests that with this simple geometric energy estimator,
theuncertainty in our energy estimation is on the order of 54 GeV.
The next series of plots looks at emmision altitude as a function
of medianarrival time. The plots are for monte carlo events selected
for small impactparameter (b<40 m) and energy greater 300 GeV.
- Figure 6: This plot shows therelation
between emission altitude and median time. Note that this is the
timespread only due to the arrival times of the photons. The mirror
time aberationsare not included.
- Figure 7: This plot shows a 2nd
order polynomial fit to theemission altitude as a function of median
time.
- Figure 8: This plot shows
thedistribution of e_est using emission altitude (in black, this isthe
same as the black curve in figure 1), and the energy estimate using
median timeto estimate the emission altitude (in red).
I am working on energy residual plots using the median time in the
energyestimator.
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Last updated: 24 Oct, 2005