The usual steps to analyze array data to construct a calibrated image are:
The simple calibration described above is successful when applied to bright objects (down to a few percent of the background level) but is inefficient when applied to faint source detection (below 1% of the background) with ISOCAM. At first order, this can be improved by modeling the flat-field, instead of using a library flat-field. The position of the lens of ISOCAM varies slightly between settings, and the optical flat-field varies as a function of the lens position by 2 to 20% from the center to the border of the array. In the case of empty fields (and more generally when most of the map covers an empty field), a simple median of the cube of data gives a very good flat-field, which allows us to reach a detection level of a few percent of the background level (Starck et al. 1999).
However, at second order, one encounters the main difficulty in
dealing with ISOCAM faint source detection: the combination of the
cosmic ray impacts (glitches) and the transient behavior of the
detectors. For glitches producing single fast increases and
decreases of the signal, a simple median filtering produces a fairly
good deglitching. The ISOCAM glitch rate is one per second,
and each glitch on average has an impact on
eight pixels (Claret et al. 1999). However, 5 to 20% of the
total number of readouts, depending on the integration time and
the strength of the selection criterion, are affected by memory effects,
which can produce false detections. Consequently, the main limitation
here is not the detection limit of the instrument, which is quite low,
but the false detections, whose number increases with the sensitivity.
Three types of glitches can be isolated, those creating:
The two first pixels are taken from a four by four raster observation of the
Lockman hole, with a
pixel field of view of 6 arc second, an individual integration time
of 2.1 second,
the LW3 filters (15 m), a gain of 2, and 56 readouts for the first raster
position and 27 readout for the others
(observation number:03000102).
The last pixel is from another observation, with the same parameters except for the number of readouts per raster position, which is equal to 22 instead of 27 (observation number:02600404).
Finally, the signal measured by a single pixel as a function of time is the combination of memory effects, cosmic ray impacts and real sources: memory effects begin with the first readouts, since the detector faces a flux variation from an offset position to the target position (stabilization), then appear with long-lasting glitches and following the detection of real sources. Clearly one needs to separate all these components of the signal in each pixel before building a final raster map, and to keep the information of the associated noise before applying a source detection algorithm.
In Sect. 3, we will show that the concept of pattern recognition using a multi-resolution algorithm leads to an efficient calibration procedure, free of the major problems described above. Simulations and real data analysis will be presented in a Sect. 4.
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