A&A 409, 395-410 (2003)
DOI: 10.1051/0004-6361:20031099
A. M. Read1,2 - T. J. Ponman1
1 - School of Physics and Astronomy, University of
Birmingham, Edgbaston, Birmingham B15 2TT, UK
2 -
Deptartment of
Physics and Astronomy, Leicester University, Leicester LE1 7RH, UK
Received 9 April 2003 / Accepted 11 July 2003
Abstract
XMM-Newton background maps for the 3 EPIC instruments in their
different instrument/mode/filter combinations and in several energy
bands have been constructed using a superposition of 72 pointed
observations. Event datasets, with point sources excised, for the
different instrument/mode/filter combinations have also been
assembled, with longer exposure times than previously available
files. The construction of the background maps and event files,
together with their properties and usage are described here. Also
given are statistical properties of the photon and particle
components of the XMM-Newton EPIC background, based on the analysis
of the 72 datasets.
Key words: surveys - X-rays: diffuse background - X-rays: general
The XMM-Newton observatory (Jansen et al. 2001) provides unrivalled capabilities for detecting low surface brightness emission features from extended and diffuse galactic and extragalactic sources, by virtue of the large field of view of the X-ray telescopes with the EPIC MOS (Turner et al. 2001) and pn (Strüder et al. 2001) cameras at the foci, and the high throughput yielded by the heavily nested telescope mirrors. The satellite has the largest collecting area of any imaging X-ray telescope.
In order to exploit the excellent EPIC data from extended objects, the EPIC background, known now to be higher than estimated pre-launch, needs to be understood thoroughly. With a good model of the particle and photon background, one can correctly background-subtract images and spectra extracted over different energy bands and from different areas of the detectors.
Here we provide details of a project to use a large number of XMM-Newton pointed observations to help define the EPIC background and to produce background maps for each of the three EPIC instruments (pn, MOS1 & MOS2) in several different energy bands. Also, significantly improved background event files, useful for spectral analysis, with longer exposures than previously produced files, and specific to several particular instrument/mode/filter combinations, have been created as part of the analysis. The co-addition of many fields allows the minimization of any "cosmic variance'', resulting from variations in the local diffuse X-ray emission or contamination from pathologically bright sources.
This paper is intended as an aid when studying or working with the EPIC background, and in particular, when using these files. The current understanding of the XMM-Newton background is described briefly in Sect. 2. Section 3 describes the methods used in the creation of the background products. Information on how to use the background images for XMM EPIC background analysis is given in Sect. 4, along with caveats as to their use. The relevant information for the event files can be found in Sect. 5, followed by some concluding remarks.
Table 1: Summary of the components within the XMM-Newton EPIC Background; temporal, spatial and spectral properties.
All the background product files (maps, event files, related software etc.), together with other scripts and procedures for XMM-Newton background analysis are available from http://www.sr.bham.ac.uk/xmm3/
The EPIC background has been shown (via the work of Lumb et al. 2002 and many others; see Appendix) to comprise solar soft protons, cosmic rays, electronic noise and cosmic X-ray photon background. We now briefly discuss the properties of these contributions:
During quiescent periods (i.e. with no significant soft proton contamination), the remaining components are:
Table 1 gives a brief summary of the temporal, spatial and spectral properties of these, the major components contributing to the XMM-Newton EPIC background.
The present analysis is related in several respects to the work of Lumb et al. (2002), and the reader is encouraged to consult this work. Additional notes regarding other related work on the EPIC background can be found in the Appendix.
Source-subtracted, high-background-screened and exposure- and source-corrected images (maps) of the particle and photon components of the EPIC background have been created separately for each EPIC instrument, and in several different energy bands. This has been performed separately per observation, over a large number of individual observations.
The individual background maps for a particular instrument and in a
particular energy band have then been collected together (for the same
instrument mode/filter combination) over the whole set of
observations. Via various cleaning, filtering and "
-clipping''
techniques, a "mean'' background map is created (for each particular
background component/instrument/energy band/mode/filter combination).
Procedures have been written to perform the different aspects of the analysis, making extensive use of the XMM-SAS tasks, Chandra CIAO tools and HEASOFT's FTOOLS utilities.
Before discussing the analysis in depth, we describe some of the files and terms used, and the structure of some of the final products.
We first define a number of terms used below:
Table 2:
The coordinate systems of the 1
background detector
maps and the 4![]()
detector maps used in the analysis.
The initial analysis is essentially the same for each observation, and is detailed in the following steps:
#XMMEA_EM or #XMMEA_EP. E.g. for PN, using the
following expression for the XMM-SAS task evselect;
PI in [10000:15000] &&#XMMEA_EP &&PATTERN==0
Good Time Interval (GTI) files are created from these lightcurves by applying an upper count rate threshold of 100 (PN) or 35 (M1/M2) ct/100 s. The event files are then filtered, keeping the low count rate time periods. The amount of time lost due to periods of high background flaring can be seen in Fig. 1, where the distribution of the fraction of data left after flare-screening is shown for all the datasets analysed.
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Figure 1: The effects of high background flaring: The usable fraction of data available after flare-screening is shown for all the datasets analysed. |
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#XMMEA_EM/P FLAG expressions, excepting that events from
outside the field of view (out-of-FOV) are kept.
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Figure 2:
A non-vignetted (4 |
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Figure 3: Histogram distributions for the 72 clean observations of (from left to right) the observation revolution number, the Galactic hydrogen column, and the live exposure time (after cleaning for high background times) for M1 (thick line) and PN (filled region). |
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The above preparatory analysis has been performed for 116 XMM-Newton observations, spanning a range in instrumental modes, filters, exposure times, and degree and duration of high-background flaring.
In order to produce the final background maps, the observations have been grouped together in terms of instrument/mode/filter etc. We then discarded datasets suffering from any of the following deficiencies:
The remaining 72 "clean'' observations used in the production of the final background files are summarized in Table 3, which lists the revolution number, the RA and Dec, the Galactic hydrogen column, and a code giving the instrumental mode and filter for, respectively, M1, M2 and PN [f - full-frame mode, e - full-frame-extended mode, t - thin filter, m - medium filter]. Also given are a nominal M1 exposure time, and the fraction of the exposure time remaining after removal of high-background periods and accounting for deadtime effects (here the PN fraction is given).
It is instructive to study some properties of the 72 clean observations. Figure 3 shows the distributions of (from left to right) the revolution number of the observation, the Galactic hydrogen column density, and the live exposure time, after cleaning for times of high background.
Almost all of the observations were taken in a 100-revolution period
between the end of June 2001 and the middle of January 2002. The
Galactic hydrogen column density distribution shows that the majority
of the observations are pointed in directions of low to medium
column. A very small number of observations are pointed in directions
of very high column. The post-flare-removal exposure-weighted mean
value of the hydrogen column over all the 72 observations is
cm-2. The post-flare-removal exposure times
show a systematically larger exposure time for the MOS instruments
than for the pn (the M2 distribution is essentially identical to the
M1 distribution shown). This is partly due to the pn being slightly
more sensitive to proton flaring, but is mainly due to the fact that
operational overheads generally lead to the pn having shorter exposure
times (by
5 ks) than the MOS. Mean values of the live
post-flare-removal exposure times are: M1: 22.0 ks (standard
deviation 13.8 ks), M2: 22.2 ks (s.d. 13.8 ks), PN: 14.8 ks
(s.d. 11.9 ks).
Table 3: Summary of the final cleaned and filtered observations used in the production of the EPIC background files. Given is the revolution number, the J2000.0 equinox RA and Dec, and the Galactic hydrogen column (in units of atoms cm-2) towards these coordinates. Also given is a code giving the instrumental mode and filter for M1, M2 and PN [f - full-frame mode, e - full-frame-extended mode , t - thin filter, m - medium filter], plus the nominal exposure time, and the fraction of the pn exposure time remaining after removal of high-background periods.
Table 4 summarizes the final cleaned observation information in terms of the different combinations of instrument, instrument mode and filter used. The nominal exposure time is the sum of the individual LIVETIMEs i.e. corrected for periods of high-background and deadtime (see however the discussion of the exposure maps in Sect. 5.1).
Table 4: Summary of the cleaned and filtered observations used in the production of the EPIC background files, separated into the different combinations of instrument, instrument mode and filter used. The exposure time is the sum of the individual LIVETIMEs i.e. corrected for periods of high-background and deadtime. The post-flare-removal exposure-weighted mean value of the hydrogen column is also tabulated.
Here we describe the production of a single "averaged'' background map from many background maps over different observations. At any given position in DETX/Y coordinates, a subset of the datasets used may be affected by contamination or diffuse sources. Such effects can be removed by clipping outliers, before taking the mean of the remaining "good'' images at this position.
In order to produce a particular set of background maps (in the different energy bands) for a particular instrument/mode/filter combination, the following steps are taken. Let us take for example the first entry in Table 4, i.e. MOS1, full-frame mode, thin filter.
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Figure 4:
A 3D "imagecube'' of dimensions DETX, DETY and
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Figure 5:
A 3D "clipcube'' of dimensions DETX, DETY and
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-clipped, and averaged, exposure-corrected background maps
have been created as described above for each instrument/mode/filter
combination analysed (of 8) and in each energy band (of 6). Photon and
particle maps have been created separately, as have maps with the two
components recombined. This leads to a total of 144 background maps,
and these are shown in Figs. 6-9. The maps can be obtained from
http://www.sr.bham.ac.uk/xmm3/.
A1_ft0000_cphim4M1.fits is, as an example of the file naming,
an exposure-corrected photon background map. A particle map is named
*cpaim*, instead of *cphim*, and a particle and photon
combined map *cim*. The example above is a MOS1 map (M1
instead of M2 or PN), and is in energy band 4 (of
0-6). The mode is full-frame (given by the f),
as opposed to (for PN) extended full-frame mode (e), and the
filter is thin (t), as opposed to medium (m). The six
character mode+filter string is as in Table 3, hence the corresponding
PN file is named A1_0000ft_cphim4PN.fits. The A1
indicates a first release of these background maps.
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Figure 6:
The final |
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Figure 7:
The final |
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Figure 8:
The final |
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Figure 9:
The final |
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When might an observer with their own EPIC data want to make use of these background maps? In order to analyse extended objects, and make background-subtracted images, estimate low-surface brightness flux levels, create radial profiles or perform 1- or 2D surface brightness fitting, one needs a map of the appropriate background. Sometimes however, the diffuse, extended nature of the user's target source is such that the determination of the background from their own dataset is difficult or impossible. Also, using a background from a significantly spatially removed section of the same data leads to problems with vignetting and detector variations. Hence the need for the independently-produced background maps created here.
What follows is a recipe for how an observer can make use of the background maps in conjunction with their own source data. Caveats, and problems that can occur when the recipe is not or can not be followed are given thereafter.
1 If such a flare-rejection method as used here leads to zero or very few Good Times, then the user's data is heavily flare-contaminated, and the background maps are therefore not suitable for source data extracted from the whole dataset. Small discrepancies due to slightly different flare-rejection methods may be accounted for by the subsequent scaling.
2 Though the user should work using the same energy bands (bands 0-5) as used in the present analysis, note that the standard XID/PPS bands have been used, and that extension to larger energy bands can easily be performed by summing individual band images. For example, band 1 is heavily contaminated by detector noise in the particle background, so the user may prefer to work in band (2+3+4+5).
3 If source-free regions within the FOV do exist within the source dataset, then the user is advised to work as above with the particle and photon ("cpaim'' & "cphim'') maps separately. The particle and photon scaling factors may be different (hence the fact that separate particle and photon background maps have been made available). If no source-free regions exist, the user may be forced to assume that the scalings are the same. Here, just the "cim'' images need be used. A script for comparing out-of-FOV counts (from event files), compareoutofFOV, is available on http://www.sr.bham.ac.uk/xmm3/. Note especially that at the very edges of the map FOVs, there are a few pixels with unusually large and small values. This is due to extremely small exposure values in the original observation maps amplifying the noise. These areas should be avoided when calculating scaling values.
For each of the instrument/mode/filter combinations, and for each of
the energy bands 0-5, mean count rates (in units of ct ks-1arcmin-2) and standard deviations about these mean values have
been calculated using all of the contributing observations listed in
Table 3. This has been done separately for the photons and for
particles. For the photons, the mean values were calculated within the
central
,
to avoid the small number of pixels
discussed above with unusually large and small values. Table 5 lists
these values for the photons, Table 6 lists them for the particles.
Table 5:
Mean count rates for the photon background maps (over
the central 16
16
), for the different instrument,
mode and filter combinations, and for each of the six (five plus
total) standard energy bands.
Table 6: Mean count rates for the particle background maps for the different instrument, mode and filter combinations, and for each of the six (five plus total) standard energy bands.
Several features are evident from the tables. For a particular instrument, the photon and particle background count rates are of the same order, the values for the pn being a factor of a few greater than for the MOS.
Whereas, for the photons, the decline in intensity (in ct ks-1 arcmin-2 keV-1
with increasing energy is quite steep, for
the particles, it is far flatter, emphasizing the points made in
Table 1, i.e. that the particle component of the background appears
essentially flat, and dominates above 5 keV over the photon
(
1.4 power law + soft thermal lines) component. This can be seen
in Figs. 6-9 also; at low energies, the photon maps are brighter,
whilst at higher energies, the particle maps dominate. In studying the
actual values, one can see that, on average, for the MOS, the photons
dominate the background over most of the spectrum, the particles only
attaining a comparable count rate in the highest energy band. For the
pn however, the particles attain a comparable count rate to the
photons at a lower energy, and are then far more dominant at the
highest energies. Again, this can be seen in Figs. 6-9.
The standard deviation in the mean values represents the scatter in the mean background count rates over the different observations. Note though there is likely some contribution from errors introduced in the separating of particles from photons, a large contributor being the presence of the extremely small exposure values in the original observation maps amplifying the noise in the out-of-FOV regions. This effect is more prevalent in the pn datasets (where the out-of-FOV regions are smaller). Also, there will be some contribution to the scatter due to the Poissonian variation in the out-of-FOV counts used to normalise the particle contribution. For the lower-exposure datasets, this can approach 10% in some energy bands.
As regards the particles, the scatter seen in the MOS particle background rates is small, about 10%, and appears roughly constant with energy. The pn experiences a larger scatter of about 20%, and of this, the greatest scatter (50%) is observed at lower energies. Not all of this scatter however, is thought due to variations in the actual particle count rates (see above). The photons show quite a range in count rate scatter (from 30-60% and beyond), with no particular trend with energy or instrument.
Figure 10 shows an example of the distribution of background count rates
observed within the sample. Shown are (thick line) the M1 0-band
full-frame thin filter photon count rate distribution [49 entries;
Table 4] (the equivalent M2 distribution appears almost identical),
and (filled region) the PN 0-band full-frame-extended thin filter
photon count rate distribution [32 entries]. The pn distribution has a
mean value (in this example) some
2.5 times that for the MOS,
and has quite a larger scatter.
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Figure 10: (Thick line) the M1 0-band full-frame thin filter photon count rate distribution, and (filled region) the PN 0-band full-frame-extended thin filter photon count rate distribution |
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Usually, of course, the user will work in sky coordinates (RA and Dec),
not detector coordinates, and to a much finer resolution than
1
.
With that in mind, software has been developed to rebin and
reproject onto the sky any provided background map (scaled or
otherwise) to the spatial scale and sky position of a user-input
image.
BGrebinimage2SKY is a shell script plus FORTRAN routine to convert the
low-resolution DETX/DETY background maps into high-resolution sky
(X/Y) images by interpolation. The user gives a template image
containing the attitude information and the pixel numbers and sizes,
and an associated event file (ideally the one used to create the
template image file) for general header purposes. A rebinned
background map is produced with the same resolution and at the same
sky position as the template image. The radius of the circle over
which interpolation is performed can be given (note that the
background DETX/DETY maps are of 1
resolution, so an
interpolation radius of this or slightly larger is recommended). An
example of the task in use can be seen in Fig. 11.
As part of the analysis, for each observation, event files have been
created, in the same manner as Lumb et al. (2002), filtered for times
of high background and with all sources removed, as described in
Sect. 3. The relevant event files have been merged together for
each instrument/mode/filter combination (Tables 3 and 4), and eight
separate event files have therefore been created (with nominal
exposure times given as in Table 4), each having an extension
containing a calibrated event list in the same format as produced by
the XMM-SAS. The event files have had sky coordinates assigned to them
for a pointing on the sky of
,
,
.
These event files (or
indeed any) can be reprojected onto any point in the sky via e.g. skycast (see http://www.sr.bham.ac.uk/xmm3/).
It is believed that these event files offer several improvements over
previous versions (e.g. those of Lumb et al. 2002, themselves
improvements on previously-created versions) for several
reasons. Important points are as follows (note that many of these
points apply not only to the event files, but also to the background
maps discussed above);
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Figure 11: Usage of BGrebinimage2SKY to rebin and sky-project a given low-resolution DETX/Y background map (top left, specifically the M1 thin-filter 0-band particle background map from Fig. 6) to the spatial binning and sky position of a user-created high-resolution sky image (top right). The resultant high-resolution sky background image is shown at the bottom. The dark areas in the background map are due mainly to CCD gaps. |
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Figure 12: Flux histograms of the detected and thereafter removed sources for each of the instrument/mode/filter combinations. (Top) Thin filter: MOS1, MOS2 and pn full-frame, pn full-frame extended. (Bottom) the same but for medium filter. All plots are to the same scale. |
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Figure 13:
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expmap_ft0000_M1.fits is a MOS1
full-frame, thin filter exposure map). The eight exposure maps are
shown in Fig. 13.
The eight event files are available from
http://www.sr.bham.ac.uk/xmm3/ and are named in a similar
manner to the background maps. E1_ft0000_M1.fits is a MOS1
full-frame, thin filter event file. PN and M2 are for
the pn and MOS2 instruments, an e denotes extended full-frame
mode, and an m, medium filter.
Before using the event files for background analysis, it is strongly suggested consulting Lumb et al. (2002). Because of the above improvements, a number of the caveats noted by Lumb et al. do not apply to the present files. Many however, are still valid:
At the time of writing, there has been only limited experience gained
in using the maps, the event files and the related software. Any
feedback on using the datasets would be very useful and is most
welcome (please email any comments to amr30@star.le.ac.uk).
It is hoped that further releases of the datasets, created using larger numbers of pointed observations, and perhaps using further modes and filters, will be made available in the future. This will be announced in the usual manner and via the URL http://www.sr.bham.ac.uk/xmm3/.
Acknowledgements
This paper is partially based on data which are proprietary. These data were made available by the XMM-Newton project scientist specifically for this purpose. We wish to thank Monique Arnaud, Jean Ballet, Laurence Jones, Dave Lumb, Silvano Molendi, Wolfgang Pietsch & Steve Snowden for very useful discussions during this work, and Mike Denby for help in obtaining many of the XMM datasets. We also thank the referee, Fred Jansen, for useful comments which have improved the paper. AMR acknowledges the support of PPARC funding.
There have been various studies of the XMM-Newton EPIC background, and many of these are described in Marty (2002), Lumb (2002) & especially Lumb et al. (2002).
A number of datasets have also been analysed and merged together, in a similar manner to that presented here. Two sets of data are particularly relevant to the present paper:
(i) Background datasets have been produced (Lumb 2002; Lumb et al. 2002) for the three EPIC instruments by source-subtracting and co-adding a few long observations. These event files can be obtained from http://xmm.vilspa.esa.es/ccf/epic/#background .
(ii) Event lists combining several CLOSED observations have been created by Phillipe Marty, and these have proven very useful in the analysis and background-subtraction of extended objects (see Sect. 3.2). These data can be obtained from ftp://www-station.ias.u-psud.fr/pub/epic/Closed
In addition, several novel methods have been used to analyse very extended and diffuse X-ray sources, where the extraction of the background is difficult. Many of these are described in Marty et al. 2002. Of special interest are the works of Arnaud et al. (2001, 2002), de Luca & Molendi (2002), Ghizzardi et al. (2000), Molendi (2001), and Pratt & Arnaud (2002).