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The Crowd and the Cosmos: Adventures in the Zooniverse

Page 15

by Lintott, Chris

Brooke on bulgeless galaxies—are just two examples of the

  things that are made possible by the careful classifications pro-

  vided by Galaxy Zoo volunteers. It’s been incredibly satisfying to

  watch the project team use our volunteers’ efforts to understand

  more about the Universe, and to see the use to which other

  people have put them.

  I have, though, continually been distracted while the frenzy of

  astrophysical research unleashed by the availability of the Galaxy

  Zoo results was playing out. Almost as soon as the project started

  116 Into the ZoonIverse

  I began to get phone calls and emails from other scientists, in

  fields about as far removed from my own as is possible to imagine,

  who wondered whether our Galaxy Zoo volunteers might be

  willing to help them out, too. The enquiries ranged from the

  polite to the pleading, but they revealed what I should have

  known already. Astronomers were not the only researchers

  struggling with the sheer volume of data now accessible to them;

  whether ancient historian or zoologist, they were likely suffering

  from the same set of problems, and citizen science, Galaxy Zoo-

  style, seemed like a way out.

  By this point—somewhere in 2008, a year after the launch of

  Galaxy Zoo—I’d abandoned any pretence of doing the work

  Oxford had employed me for in the first place, and was thinking

  about citizen science full-time. We were given a small amount of

  money by Microsoft, part of a fund set up by the company to

  commemorate their leading computer scientist, Jim Gray, who

  had vanished while sailing near San Francisco in early 2007. (Our

  project appealed partly because of the response to Gray’s disap-

  pearance; his colleagues and friends organized a distributed

  search for signs of his boat in satellite images, a task which was

  eerily reminiscent of the kind of thing we’d ask Galaxy Zoo vol-

  unteers to do in the years ahead.) A grant from the wonderful

  Leverhulme Trust followed (I love an application form which

  includes the question ‘why won’t anyone else fund this?’), and for

  the first time we could think about expanding.

  From this point on ‘we’ includes a diverse cast of wonderful,

  slightly bonkers web developers and escaping scientists who

  deserve a lot of credit for the last ten years. This isn’t a formal history, so I won’t stop along the way to describe who did what, but

  you should be very aware that this is a team effort. My first hire

  was Arfon Smith, a cheerful Welsh presence who I’d first encoun-

  tered when we were PhD students. Arfon studied astrochemistry

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  from a chemist’s perspective, but had realized research was not

  for him and become a web developer. (He now heads the grandly

  titled Data Science Mission Office at the Space Telescope Science

  Institute in Baltimore, the home of Hubble, and so his attempt to escape academic research hasn’t gone brilliantly.)

  With Arfon’s expertise on board we could build something a

  bit less jury-rigged to support Galaxy Zoo, and also try out some

  new things. We were planning the Zooniverse—a platform con-

  sisting of many projects—rather than just a single website. As

  we thought hard about how to build a system that could be what

  we wanted, we slowly acquired a set of test projects, all ambi-

  tiously different from each other. One of the first came when I

  found out that the team at the Royal Observatory Greenwich

  were thinking of developing a similar project using solar data.

  I’ve always loved visiting Greenwich—arriving there on the boat

  which runs from central London and spying the green dome of

  the old observatory up on the hill, behind the beautiful old

  Royal Naval College and Queen’s House, is absolutely thrilling.

  I was also intrigued by the idea of working within a museum;

  the success of Galaxy Zoo had meant we were suddenly com-

  municating with a huge number of people in a fairly novel way,

  and the idea of a place where there were experts in communi-

  cating with the public seemed useful. More to the point, as far as

  I was concerned if anyone was going to do such a project it was

  going to be us.

  I recruited Chris Scott (then at the Rutherford Appleton Lab,

  now at the University of Reading), who I’d interviewed several

  times on the topic of solar weather. Chris is one of the team

  behind a very special pair of cameras, the Heliospheric Imagers

  (HIs) on the twin STEREO spacecraft. STEREO’s mission was to study solar weather, the activity on the surface of our star which

  can affect the whole Solar System. At any given time, particles

  118 Into the ZoonIverse

  are flowing away from the Sun in a stream known as the solar

  wind, but occasionally things get more spectacular.

  The Sun is a ball of ionized gas (otherwise known as plasma).

  That means that as it rotates, it doesn’t do so in the way a solid

  body does. If you could stand at the solar equator (a terrible idea

  for many reasons), you would complete one rotation every 24.5

  Earth days. If you stood at the solar poles—a no less terrible

  idea—it would take thirty-eight days to rotate. The Sun also has

  a strong magnetic field, and this differential rotation has a pro-

  found effect on it. The magnetic field becomes tangled, and every

  so often releases energy by springing back to an untangled form,

  expelling material into space as it does so.*

  These events are known as coronal mass ejections, or CMEs

  for short (Plate 7). In Chris’ phrasing, each consists of a billion

  tons of matter moving at about a million miles an hour. They are

  spectacular and dramatic, but they are interesting for practical

  reasons too. Every so often, the Earth happens to get in the way

  of one of these CMEs. If conditions are right (again, the details

  depend on the complexities of interacting magnetic fields and

  charged particles), the particles from the CME can cause a change

  in the Earth’s upper atmosphere, creating glorious displays of

  what are called the aurorae, the Northern and Southern Lights.

  The background flow of particles from the Sun means that at

  least a faint display of aurora is visible on most nights. I used to

  act as a tour guide on special flights to go view the Northern

  * The actual physics of this are, from my perspective, unbelievably complicated, and as a result I have the utmost respect for the scientists brave enough to take on trying to understand the Sun as their life’s work. If you want to bamboo-zle most astronomers, just ask if they have considered the effect of magnetic fields; the answer is almost always ‘no’. I have the liberty in my work of looking at distant stars and galaxies and deciding that they look simple; with the Sun, we have no such option and must confront its complexities.

  Into the ZoonIverse 119

  Lights; we’d fly north towards Iceland, turn the lights in the plane

  off (and sometimes those on the plane’s wings too), and peer out

  of the windows. I took something like forty flights, and only once

  did we have a complete failure. Most of the time, though, what

  we could see was a
faint, grey curtain. It might flicker a little, and change shape over the course of the hour or so we’d watch, but

  my job as the on-board astronomer was to make sure people

  were excited by seeing something so unspectacular.

  After all, most of the people on board the flights were there

  because they’d seen footage or photos of brilliant and brightly

  coloured aurorae, lighting up a snow-covered landscape with red

  and green shadows as the lights dance overhead. I’ve seen such a

  display only once, on a trip to Tromsø in northern Norway. Local

  aurora expert Kjetil Skogli had taken our group out to a frozen

  lake, but as we headed to the site we could already see something

  spectacular was happening.

  Before too long, I was lying on my back in the snow looking up

  into a clear night sky that was like nothing I’d ever seen before.

  The horizon was lit up with a bright green curtain that seemed to

  change ethereally even while we looked at it. Bright streamers

  reached up, high into the sky, suddenly brightening and fading as

  I looked. Eventually, the sky far above me was encircled with red,

  a feature known as an auroral crown (Plate 8) which I’d only read

  about before. It was utterly magical, a transformative hour or so

  that I will never forget, a few moments’ glory powered by the

  arrival of a CME, with particles from one of these events pouring

  down onto the Earth’s atmosphere and exciting the particles

  there to glow brightly for our entertainment.

  The next night we went back out, and drove through a blizzard

  to the Finnish border to find a gap in the clouds. Despite this, we

  were rewarded only with a faint glow. The Sun, and its interaction

  with the Earth, is capricious in the extreme. Yet particularly large

  120 Into the ZoonIverse

  or energetic CMEs can have consequences that reach beyond the

  success of a sightseeing trip. The electric currents induced by

  such activity are a serious threat to much of our electronic infra-

  structure; a power blackout that affected large parts of North

  America and Canada in 1989 was blamed on a solar storm. The

  famous Carrington Event, a dramatic flare observed during the

  nineteenth century, affected telegraph systems—the high-tech

  communications infrastructure of the time. Much of our infra-

  structure is now in space, with satellites in the firing line and vulnerable to the effect of CMEs.

  With warning, most of these negative consequences can be

  prevented. Understanding solar weather, and predicting whether

  an observed event might hit the Earth, has thus become a prior-

  ity. To this end, the STEREO mission was supposed to provide a unique perspective. It consisted of two separate spacecraft, each

  placed on an orbit which meant it drifted slowly away from the

  Earth. One was ahead of our planet and one behind, flying with

  cameras turned to study the Sun and its environment.

  The HI cameras the twin spacecraft carried had a different job.

  They were designed with a series of internal baffles, made of

  some of the blackest material available, all in the service of reduc-

  ing internal reflections. That’s necessary, because these cameras

  had the job of staring at the space between the Sun and the Earth,

  watching for the faint trace of coronal mass ejections travelling

  through space.

  The images from the HI, turned into low-resolution video, are

  strangely beautiful. You see nothing but a background starfield

  at first, drifting slowly past the camera as the spacecraft moves.

  You might notice a couple of stars that are much more brilliant

  than the others. These aren’t stars, but planets—Venus, or even

  the Earth drifting slowly through the field of view. The fact that

  we can launch a spacecraft capable of capturing a beautiful

  Into the ZoonIverse 121

  image of our own planet, as just one drifting object among a

  myriad stars, is something that stops me dead in my tracks from

  time to time, but this—and the occasional spectacular movie of

  a comet having its tail removed by the fast-moving particles of

  the solar wind—is very much beside the point. The main goal for

  the STEREO HI imagers, and the other cameras on board, was to understand how the solar wind gets launched and then travels

  through the Solar System.

  Picking out the ghostly trace of a passing coronal mass ejection

  against a background of stars is difficult—exactly the sort of pat-

  tern recognition task that computers still struggle with and at

  which our biological, evolution-honed senses excel at. With the

  help of those in Greenwich, Chris’ team, and others, we created a

  project, Solar Stormwatch,* which asked volunteers to watch vid-

  eos, spot CMEs, and trace their progress across the Solar System.

  This was a difficult task for us, as we had to build a whole new

  set of tools capable of dealing with video and allowing the care-

  ful marking that was needed to produce scientifically useful

  results from such a task. It was also difficult for the volunteers,

  who had to look carefully to find even the faintest traces of activ-

  ity in very busy images. Of special importance were the first few

  frames of any particular event, when the particles that made up

  the CME had just been launched from near the surface of the

  Sun; as they travelled through the lower atmosphere of their star,

  they would have interacted with the magnetic fields that thread

  the region, producing what could sometimes be a dramatic

  effect.

  * Most of the development was done by the talented Jim O’Donnell, then a web developer in the team at the museum in Greenwich but more recently a stalwart of the Zooniverse team in Oxford.

  122 Into the ZoonIverse

  To our delight, Solar Stormwatch was a hit. While not receiv-

  ing the publicity that Galaxy Zoo had, tens of thousands of

  people took part, and there were a couple of immediate scientific

  results from the Solar Stormwatch project. First of all, Chris’

  team showed that—partly because of the unique vantage point

  afforded by the two STEREO spacecraft and partly because of the

  care taken by volunteers to achieve incredible accuracy—using

  classifications from citizen scientists provided a better warning

  of the approach of a CME towards Earth than existing automated

  systems. If you’re a company with commercial satellites, you

  would literally be better off consulting our crowd (and, yes,

  launching your own version of STEREO, as the vagaries of orbital mechanics have since seen the two spacecraft drift to less useful

  positions) than relying on your resident machine-learning

  experts. Machine learning for this sort of problem is still in its

  infancy, and professional forecasters, it turns out to my surprise,

  still inspect the data by eye, but perhaps the Solar Stormwatch

  results might provide a gold standard set on which future storm-

  hunting robots could be trained.

  There was also a scientifically interesting result. I described

  CMEs earlier as if they were the result of a sudden event, after

  which they just coast out into the Solar Sys
tem. Instead, our data

  confirms what had been seen in images from the SOHO satellite further from the Sun’s surface; the particles that make up the

  CME accelerate away from the surface of the Sun. Rather than

  just setting off into the Solar System, they get pushed on their

  way by the complex magnetic fields that exist close to the solar

  surface.

  Or at least that’s what seems to be going on. Unfortunately,

  I for one didn’t realize this was going to be the interesting bit, and so we designed the Solar Stormwatch interface without paying

  special attention to the few frames the STEREO cameras capture

  Into the ZoonIverse 123

  around the point where the CME is just beginning to head out

  into the Solar System. We’ve fixed that now, and a newer version

  of the project has asked classifiers to pay particular attention to

  this most interesting of regions, but the results are still awaited

  eagerly.

  Solar Stormwatch seems a large jump from Galaxy Zoo, but

  we were looking in other directions too. I knew that a large num-

  ber of planetary scientists spent their days counting craters, the

  better to understand the history of the worlds they were study-

  ing, and the task seemed ripe for citizen scientists to sink their

  teeth into.

  The principle behind crater counting is simple. Imagine that,

  at some point in the Solar System’s five-billion-year history, the

  great volcanoes of the Martian range sputtered into life, with lava

  flowing out to cover the surrounding plains. The new surface

  would be, at least when seen from orbit, smooth and new. Wait a

  few million years, though, and a meteorite large enough to sur-

  vive a fall through the thin Martian atmosphere is likely to hit,

  burying itself into the surface or vaporizing near impact, in either

  case leaving behind an impact crater. Wait a little longer, a sec-

  ond meteorite might hit. And then another. And another. Even

  seemingly rare events become common over the billions of years

  of cosmic history.

  From today’s perspective, we can count the craters to work

  out how old the surface is, at least relative to others on the

  same planet. The cratered surface of the Martian highlands, for

  example, is clearly older than the volcanic and smooth slopes of

  the Tharsis Montes. Play this game on the Moon, and there’s an

 

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