next up previous contents
Next: The Late SWTCs Up: The Early SWTCs Previous: Examples of nontriggered GRBs   Contents

Benefits and Drawbacks

One of the most relevant benefits of the GRB quest performed with the SWTCs resides in the very small number of bins that cannot be scanned: actually, the only case corresponds to the occurrence of ``very short'' data intervals: more precisely, when their durations are lower than $N$ s. This case has been found to occur very rarely, especially in the earlier observations, when sometimes in the ratemeters there were bunches of data gaps. A nice example of a detected bright burst occurred just before a SAGA passage is shown in fig. [*]: this is an OTB, that triggered the GRBM on board at 22:09 UT, on March 15, 1997. Another advantage from using the SWTCs is the detection of very weak (in the 40-700 keV band) and soft bursts, with peak fluxes of $\sim 0.1\rm ph\ \rm cm2\ \rm s1$, like the cases discussed above (tab. [*], fig. [*], [*]).

Figure: The OTB 970315 (left: 40-700 keV, right: $>$100 keV) occurred just before the SAGA transit (unit 1, 40-700 keV energy band). The parabolic background fit is overplotted: this was estimated after visual inspection, by using a proper interval preceding the burst.
\begin{figure}\begin{center}
\epsfig{file=grb970315_220919_grbm1.eps, width=7.7cm}\epsfig{file=grb970315_220919_ls1.eps, width=7.7cm}\end{center}\end{figure}

The drawback of these SWTCs is the background estimate: since this is computed with a simple moving average, involving only the bins preceding the scanned bin, several NTBs are biased, owing bad background subtraction.

Another consequence of the wrong background estimate is the detection of many false NTBs, that do not correspond to any real transient increase in the ratemeters, but are simply due to medium- or long-term variations in the background level. This unfortunate feature prevented the author from applying the early SWTCs to the on-line GRB quest; otherwise, there would be an excess of spurious triggers, in addition to strongly biased estimates of duration, peak count rate, total counts for many real bursts.

In summary, the early SWTCs are good in detecting many transient events occurring near ``critical'' points in the ratemeter time histories; nevertheless, owing to the naive method used for the background fit, some relevant characteristics, like peak count rate, duration, total counts, have to be further refined after visual inspection.


next up previous contents
Next: The Late SWTCs Up: The Early SWTCs Previous: Examples of nontriggered GRBs   Contents
Cristiano Guidorzi 2003-07-31