Near-Time Persistency Checker (NTPCkr) Frequently Asked Questions
Answers to frequently asked questions about the NTPCkr:
Q: What is the NTPCkr?
A: A program which sits at the end of our data pipeline and scans SETI@home results soon after they are validated and determines if we've previously seen similar signal types at similar frequencies at that exact point in the sky (i.e. a persistent signal).
A: Individual signals reported in your SETI@home results are never interesting no matter how strong they are. They only get interesting if they persist over multiple observations (i.e. if we look at the same point in the sky, say, a year later do we see the same exact type of signal at the same frequency?). This is why we need a tool to hunt for persistent signals.
A: Yes and no. The name of the game in SETI has always been to look for persistent signals. Individual spikes, Gaussians, etc. are uninteresting as they are commonly found due to random noise, or radio frequency interference (RFI). They are far more interesting when the same signals are seen over many observations.
In the past we didn't have the computing power to do this kind of analysis in "real time," i.e. as new data arrive. Instead there was a painful process of accumulating resources to analyze our entire, large data set in one pass - what we called "turning the crank." Finding pairs (or triplets, etc.) of similar signals in a database of billions of singals is quite difficult - imagine playing a game of concentration with billions of cards. That's why it usually took years between each time we turned the crank, during which our hardware/tools evolved enough to require reinventing the wheel again and again. However the NTPCkr keeps up with incoming data close to real time, updating our list of most interesting candidates every day (or hour, or minute!).
A: It sounds exciting, but we always found it difficult to come up with less exciting-sounding yet meaningful terminology in SETI. Think of it this way: there are always lots of candidates for U.S. president. A "candidate" simply means it has non-zero potential for interest.
We actually go further than that: a candidate is simply a point in the sky. We divide our observable space into pixels just like on a computer monitor, each identified with a unique number. Every spot on the sky is a candidate, even if we haven't seen anything there.
For more information about how we pixelize the sky, see here.
A: They are ranked by score. The score is the probability that the exact set of signals we observed at that point in the sky would occur due to random chance. So the lower the score, the better.
A: These may be our current top candidates, but they are most certainly due to our own earth's radio frequency interference. We're a very noisy planet - in fact there's a half dozen radar signal patterns we commonly see in our data from Arecibo. When a candidate stays near the top of the list, even after our best efforts to minimize the interference, then that's a little more interesting.
But I still wouldn't get too excited. Remember our data set contains billions and billions of signals - and so the natural random noise out in space will still cause some curious candidates. At that point we'd tag these candidates for reobservation. Only if we see it again during these reobservations will we start raising our eyebrows.
In short, what you see on the NTPCkr page is just the very first step in finding E.T., and it's highly likely that 100% of the candidates that show up on this page are noise or interference.
A: Remember this is currently a list of "top" candidates ranked by score, and therefore it is highly likely a single short burst of earth radio interference (which we haven't rejected yet) is affecting the scores of many candidates. Once these are determined to be uninteresting, they will be dropped from the top of the list.
A: Quite often the telescope at Arecibo is "parked" when not in use by other projects. When it's parked it is sitting at a single line of Declination (while the Right Ascension changes due to earth rotation). However, since we are collecting all the time we get an excess of data from these parked Declinations (like 18, which is quite common).
A: No - this could be for several reasons. Here are four of them:
1. When a candidate gets a good score, it is automatically tagged for "cleaning." We'll check it for RFI contamination, and re-score it. Chances are very, very likely it is RFI contaminated, and so the score will increase (i.e. get worse) and the candidate will drop down in the list.
2. A candidate may have a good score because, say, we observed there 5 times and saw a Gaussian there each time. Then it just so happens the telescope passes over that point in the sky again, but this time saw nothing. The NTPCkr will rescore this candidate, and now that it only saw 5 Gaussians out of 6 observations, the score gets worse and the candidate will drop down in the list.
3. You could imagine that our scoring algorithms are quite complicated, given the varied nature of the signal types, the chaotic nature of our observation schedule, etc. We may find over time we need to adjust our algorithms, and this may cause some previously good candidates to become less good.
4. The NTPCkr will always be a work in progress, and due to testing/debugging we may find reason to scrap our current set of candidates and start from scratch. This isn't destructive: if a candidate is truly interesting it will soon reappear in our new top candidate list.
|1||14683503||19.529297||21.442044||770 (6/308)||148 (0/0)||273 (0/121)||196 (0/49)||0||-1.280627e+5||0||9 Jun 2009 18:49:42 UTC||skyplot|
|id||type||ang dist||freq||chirp||period||snr||score||# det|
Example (for a spike):
|id||result||time||peak power||det freq||fft||chirp||rfi c/f||chi sqr||null chi sqr||max power||period||snr||thresh||len_prof||score|
A: A waterfall plot shows all spike signals observed in a given time window by their frequencies. It's called a "waterfall plot" because it sometimes actually looks like a waterfall.
These plots are useful for quickly identifying certain frequencies that are both strong and constant. In short, if you see anything resembling a vertical line, this is radio frequency interference from earth. We know this because as the earth rotates and the telescope moves, constant frequencies must be local, i.e. from our own planet. Chances are if you look at these waterfall plots, you'll find lots of our "candidates" living on one of these vertical lines.
More information about waterfall plots can be found in this old science newsletter.
A: We have several schemes, most of which we used in earlier SETI projects, for automatically detecting and rejecting obvious RFI. However, we are currently devising new (and hopefully better) methods, including using many human eyeballs to identify questionable candidates (i.e. ones that live on or near interference). These eyeballs could include yours, if you're interested.
A: That is showing you the border of the "pixel" which makes up this particular candidate. Code to generate those borders was donated by Tiaan Geldenhuys. Thanks Tiaan!
A: Yes, over here.
|Copyright © 2013 University of California|