Simulation
of the MOST time series on Procyon
The aim of this homepage is
to present a number of key issues related to the simulations of time-series
data on Procyon. The simulations are related to
the published null result on Procyon
obtained by the Canadian MOST satellite and published by Matthews et al. in
Nature.
The present analysis is based
on a software package developed to provide time-series simulations for the
Danish MONS/Rømer space mission as well as for the
ESA Eddington mission. The software package
contains a set of routines that can be used to simulate noise as well as p-mode
oscillation signal.
The software can be used to
simulate the noise using a number of filtered 1/f (in amplitude) noise sources
(e.g. granulation) as well as periodic noise and white noise (from e.g. photon
noise) terms. Oscillation p-mode signal is simulated using a set of equations
that allows one to create stochastically excited oscillations, specifying mode
life-time, mean amplitude and frequency for a large number of individual modes.
The figures below show
simulations of Procyon using a sampling of one
data point per 100 sec. The first figure shows the time series indicating the
p-mode signal (black) and a simulation of granulation at the solar level (red).
Using the velocity power
excess measured by Martic et al. (2004), we
estimate an amplitude in photometry of 7-8 ppm per mode (Kjeldsen and
Bedding, Astronomy and Astrophysics, 293,
p. 87-106). The mode lifetime is assumed to be around 1.9 days as inferred from
the velocity time-series data.
Based on this we have done a
number of simulations using different levels of the granulation power
background. Below we show the simulated Procyon
amplitude spectrum for 3 different levels of the granulation power (solar
level, 2 times solar power and 4 times solar power).
We recall that a power level of 2 times solar is in agreement with the measured
upper limits from ground-based observations (Kjeldsen
et al. 1999).
We have also simulated
ground-based data sets, e.g. the velocity time series obtained by Martic et al. (2004). Again we use a p-mode amplitude of
1.8 times solar (40 cm/s in velocity and 7-8 ppm
in photometry), a damping time of 1.9 days per oscillation mode and a
granulation background of 2 times solar (in power). The result of those simulations
are shown in the figure below, where data corresponding to a full MOST series
is shown in velocity (not photometry as measured by MOST) and compared with the
7 times 8 hour data segments obtained by Martic
et al. (2004). We also show one figure including instrumental noise (ELODIE
noise).
Finally we show a direct
comparison between the p-mode and granulation signal in Procyon (for an observation without instrumental noise;
black) and a simulation of the MOST time series (grey). It is based on such a
simulation that we conclude that MOST has not detected the granulation signal
in Procyon, but that non-stellar noise is making
a significant noise contribution that does not allow detection of p modes nor
granulation power.