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Project Cyclops, A Design... - Department of Earth and Planetary ...

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needto process this spectral information in some<br />

automated system in a manner that will assure detection<br />

<strong>of</strong> any faint coherent signals that may be present <strong>and</strong> yet<br />

not give too many false alarms because <strong>of</strong> noise alone. In<br />

this section we will describe some possible ways <strong>of</strong> doing<br />

thi_ processing.<br />

The power spectra will show a Boltzmann distributed<br />

background intensity due to noise. This background will<br />

differ in detail from sample to sample but the statistics<br />

are stationary <strong>and</strong> the long-term average at any point<br />

will approach a constant value. If there is a strong<br />

coherent signal present, there will be a bright spo t in the<br />

spectrum at the frequency <strong>of</strong> the signal. If the coherent<br />

signal is weak-comparable in power to the noise power<br />

in a resolvable interval-the intensity in successive<br />

samples will fluctuate, being sometimes stronger, sometimes<br />

weaker than the average noise brightness; but the<br />

average intensity over many samples will be greater than<br />

that produced by noise alone. Thus, if the coherent<br />

signals showed no frequency drift, a simple detection<br />

scheme would be to integrate the power spectrum for a<br />

sufficient time <strong>and</strong> then scan it for points having a<br />

greater intensity than that likely to be produced by<br />

noise alone.<br />

Unfortunately, because <strong>of</strong> Doppler rates <strong>and</strong> inherent<br />

source instability, we must expect any coherent signal<br />

spot in the power spectrum to drift in position with<br />

time. This means that if we are to detect weak drifting<br />

signals we must accumulate the power spectra with<br />

successive samples shifted by a constant amount frame to<br />

frame corresponding to an assumed drift rate. Since we<br />

do not know the drift rate a priori we must do this<br />

accumulation for a range <strong>of</strong> assumed drift rates, positive<br />

<strong>and</strong> negative, up to the maximum rate expected (or up<br />

to the maximum rate that will allow full response in the<br />

spectrum analyzer). Because Doppler drift rates change<br />

slowly with time <strong>and</strong> because interstellar sources,<br />

particularly beacons, may be assumed to be inherently<br />

rather stable, we probably need only allow for constant<br />

drift rates during any observation period.<br />

Our problem is illustrated nicely by Figure 11-7,<br />

which is actually a photograph <strong>of</strong> a pulsar pulse. Each<br />

scanning line in the picture is the power output <strong>of</strong> a<br />

receiver as a function <strong>of</strong> time. The receivers in adjacent<br />

scanning lines are tuned to adjacent fiequency b<strong>and</strong>s.<br />

Because <strong>of</strong> dispersion in the interstellar medium, the<br />

lower the frequency to which the receiver is tuned, the<br />

tater the pulsar pu_:_ arrives, lfwe covet all but _me line at<br />

:_ time, i_ b._co.n.e_,evident that the pulsaJ v oi_Id not be<br />

'.'isib!e h_,;he ,_!p<br />

,t <strong>of</strong> any single receiver. Y_.:-_i!s signature<br />

stamts o'_' cie,:_ly in faster <strong>of</strong> traces prod_;ced by all<br />

_'.,e receivers.<br />

°<br />

Figure 11-7. Signature <strong>of</strong> a pulsar produced by simultaneous<br />

observation on ad/acent frequency channels.<br />

(Photograph courtesy <strong>of</strong> Martin Ewing, Calif. Inst. <strong>of</strong><br />

Technology)<br />

For our purposes we can take the photo to represent<br />

the intensity versus distance along a particular raster<br />

line, in the output <strong>of</strong> an optical spectrum analyzer, for<br />

successive samples <strong>of</strong> the power spectrum. The noise<br />

background has the same significance as before, but the<br />

"pulsar" is now a coherent signal drifting at a constant<br />

rate. Again it is evident that this signal could not be<br />

detected in any single sample <strong>of</strong> the power spectrumthat<br />

is, any single line <strong>of</strong> the photo-but the drifting<br />

trace st<strong>and</strong>s out clearly in the raster <strong>of</strong> lines.<br />

If the photo were to be scanned with a vertical slit,<br />

which moved horizontally across the picture, <strong>and</strong> the<br />

average brightness measured through this slit were<br />

plotted versus displacement, the resulting curve would<br />

show a small fluctuation about a mean value. So long as<br />

part <strong>of</strong> the signal trace were in the slit, the fluctuations<br />

might appear to be about a slightly higher mean value,<br />

but it is doubtful if this difference would be visible. If<br />

the slit were now tilted to be parallel to the signal trace<br />

<strong>and</strong> again scanned horizontally, the same sort <strong>of</strong><br />

fluctuations about a mean value would occur until the<br />

trace lay entirely within the slit. At this point, there<br />

would be a large pulse in brightness clearly in excess <strong>of</strong><br />

the normal noisefluctuations. By scanning the picture in<br />

this fashion we have converted the pattern, clearly<br />

visible to the eye, into a waveform clearly "visible" to<br />

threshold decision circuits. This is the principle we<br />

propose for use for the atttomatic detection <strong>of</strong> coherent<br />

signals.<br />

Oplical<br />

Processing<br />

!i _mc '.,.'ere simply to, fl.,!_rgraph successive samples<br />

,)f the p_:xv,v spcctru:n 2p,d ._r,"a'lge to p:ojcct #z such<br />

O

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