A fundamental quantity in signal analysis is the metric g ab on parameter space, which quantifies the fractional "mismatch" m between two (time-or frequency-domain) waveforms. When searching for weak gravitational-wave or electromagnetic signals from sources with unknown parameters λ (masses, sky locations, frequencies, etc.) the metric can be used to create and/or characterize "template banks". These are grids of points in parameter space; the metric is used to ensure that the points are correctly separated from one another. For small coordinate separations dλ a between two points in parameter space, the traditional ansatz for the mismatch is a quadratic form m = g ab dλ a dλ b . This is a good approximation for small separations but at large separations it diverges, whereas the actual mismatch is bounded. Here we introduce and discuss a simple "spherical" ansatz for the mismatch m = sin 2 ( g ab dλ a dλ b ). This agrees with the metric ansatz for small separations, but we show that in simple cases it provides a better (and bounded) approximation for large separations, and argue that this is also true in the generic case. This ansatz should provide a more accurate approximation of the mismatch for semi-coherent searches, and may also be of use when creating grids for hierarchical searches that (in some stages) operate at relatively large mismatch.
I. MATCHED FILTERING AND THE OVERLAP BETWEEN TEMPLATESMore than two decades ago, when the first generation of interferometric gravitational wave (GW) detectors were still in the planning stages, a handful of pioneers investigated the techniques that would be needed to detect GW signals [1][2][3][4][5][6][7][8][9][10]. At that time there were three main challenges. First, the signals were weak in comparison with the noise from the detectors, so needed to be "teased out" of the data stream with optimal or nearoptimal methods. Second, the parameters describing the signals (such as the object masses in a binary system, or the rotation frequency and spindown rate of a neutron star) were not known. This required repeated searches for signals with many different parameter combinations, creating a significant computational challenge. Lastly, even if the parameters were known precisely, for some sources the waveforms could only be calculated approximately. The errors could be estimated but not sharply quantified.The solution to the first problem is to use "matched filtering" [3,[6][7][8][11][12][13][14][15][16]. In the simplest case [17] the time-dependent output S(t) of the detector is correlated with a template T (t) to produce a statistic ρ = (T, S).(1.1)If the template is normalized (T, T ) = 1 then ρ is called the signal-to-noise ratio (SNR). This is reviewed in a signal-processing context in [18,19] and in the GW context in [20] and [21]. The positive-definite inner product in Eq. (1.1) can be expressed in different ways. For example if the instrument noise is white (or the signal is confined to a narrow enough range of frequency that the noise is white in that band) then...