Authors: Dava Sobel
Pluto spins around its own axis once every six days, rotating the dim splotches of its vague landscape in and out of view. Like Uranus, Pluto lies on its side, the victim of a prior collision. Indeed, planetary scientists believe that a single impactor knocked down Pluto and chipped off its moon Charon in one blow.
Pluto and Charon, only about twelve thousand miles apart, lock each other in orbit around a point partway between them. They both rotate at the same pace while jointly circling this point, so that each keeps the same face always turned toward the other. The uniqueness of their orbital engagement has recast Pluto and Charon as “Pluto-Charon,” the first known example of a true “double” or “binary planet.”
Less than a decade after Charon’s discovery, Pluto and Charon oriented themselves in space so as to take turns eclipsing one another, as viewed from Earth. Such a fortuitous arrangement can occur only twice during Pluto’s orbit, or once every 124 years. Beginning in 1985, astronomers took advantage of the numerous mutual occultations to derive the best possible approximations of the two bodies’ mass, diameter, and density. At about twice the density of water, both Pluto and Charon are more dense than any of their gaseous giant neighbors, though not half so dense as the iron-rich terrestrial planets Mercury, Venus, and Earth.
Perhaps two-thirds to three-quarters of Pluto consists of rock, and the rest ice. Above Pluto’s bedrock of water ice, patches of frozen nitrogen, methane, and carbon monoxide have been identified from afar. When Pluto warms itself inside Neptune’s orbit for two decades every two
centuries during its nearest approach to the Sun, ices on the planet’s surface partially evaporate to form a puffy, rarefied atmosphere. Later, as Pluto recedes from the Sun and its temperature drops back to a frigid normal (about two hundred below zero Centigrade), the atmosphere falls down and coats the ground, especially around the poles, with fresh, exotic snow. In this regard Pluto behaves somewhat like a comet (which would also heat up and blow off icy gas upon nearing the Sun), though it remains too distant to create any great display.
By the time the Sun’s light reaches Pluto, distance has dimmed it a thousand-fold, so that the Sunlit planet in daytime resembles a winter evening by Moonlight. On Pluto’s reflective landscape, bright surface frosts coexist with dark areas that may represent rock outcrops or deposits of organic compounds extorted from the ice by the Sun’s ultraviolet light. Polymers in carbon-rich colors—pink, red, orange, black—probably proliferate on Pluto.
Despite the Pluto-Charon similarity in composition and the pair’s shared common origin, the moon’s smaller mass and lower gravity cause it to lose its grip on gases. Molecules vaporized from
Charon’s surface do not hover aboveground waiting to return as snowflakes; they simply escape into space. As a result, Charon reflects considerably less light than Pluto, and its surface will most likely appear dull-neutral in photographs when the binary worlds of Pluto-Charon are eventually visualized by a visiting spacecraft.
All past attempts to mount a mission to Pluto failed at the funding stage—before any craft could reach the launch pad, much less begin the long journey. Now, after the disappointing cancellations of projects such as “Pluto Express” and “Pluto Fast Flyby,” Plutophiles finally have a scout being readied for the Kuiper Belt. NASA’s minimalist “New Horizons,” equipped to map and image Pluto, Charon, and at least one other KBO at close range, should see its promised lands in 2015. By then, the number of known KBOs may have increased exponentially, from the several identified to date, to the hundreds of thousands more anticipated.
Already the demographics of the Kuiper Belt hint at great waves of migration that characterized early Solar System history. All the KBOs, it seems, were exiled to their present locations, from positions closer to the Sun, at the time the giant
planets were completing their own accretion. Jupiter and Saturn swallowed some small planetesimals in their vicinity and accelerated many more with such force that the bodies were banished from the Solar System. While Uranus and Neptune also participated in this planetesimal diaspora, they lacked the power to hurl objects entirely beyond the Sun’s reach, and relegated them instead to the Kuiper Belt.
As a result of these displacements, Jupiter lost some of its orbital energy and moved in closer to the Sun. Saturn, Uranus, and Neptune, in contrast, gained energy and edged farther away. Pluto, which is thought to have occupied a round, regular orbit at this early stage, was shoved outward by the gravitational influence of Neptune. Over tens of millions of years, Neptune forced Pluto, the ultimate expatriate, to follow an ever more tilted, more elliptical course.
Pluto and the other Kuiper Belt residents have thus been worked over by events in the Solar System. Although scientists had hoped the Kuiper Belt might preserve pristine material, unchanged since the formation of the Sun, they now see it as a war zone where bodies have been deposited and left to fray each other. The true, untainted
genealogical roots of the solar family must be pursued at a still further remove.
Today, ever more distant worldlets are swimming into view beyond the Kuiper Belt. The planetoid Sedna, discovered in 2003 and named for the Inuit goddess of the icy sea, is currently the coldest, most distant known member of the Solar System. About half the size of Earth’s Moon, Sedna seems to ply an orbit that reaches to nine hundred times Earth’s distance from the Sun, and that takes ten thousand years to complete.
Farther on, between the dim body of Sedna and the bright spectacle of the distant stars, astronomers expect to encounter a spherical swarm of trillions more small objects surrounding the Solar System. Among these frozen leftovers of creation lie perhaps the profoundest answers to the question of where we came from.
The outlying ancient debris distributes itself over such a distended area that the Solar System’s periphery is transparent as a crystal ball. Through the bubble of its outer boundary we can see forever—across the Milky Way home of our Sun, into the other galaxies that twirl like pinwheels strewn across the Universe, their many billion stars frothing with planets.
Sometimes the stupefying view into deep space can send me burrowing like a small animal into the warm safety of Earth’s nest. But just as often I feel the Universe pull me by the heart, offering, in all its other Earths elsewhere, some larger community to belong to.
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Like “planet,” the word “life” poses similar difficulties for astrobiologists: A wildfire, for example, exhibits lifelike behavior as it takes in oxygen, grows, moves, consumes, even generates new fires with its own sparks, but it is not “alive.”
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Pluto last dipped within the orbit of Neptune in 1979 and emerged in 1999. At perihelion, in 1989, Pluto lay approximately one billion miles closer to Earth than it had been when discovered in 1930.
T
here was a big party at Andy Ingersoll’s house in Pasadena the night after the
Cassini
spacecraft flawlessly inserted itself into orbit around Saturn in the summer of 2004. The music and dancing, the food and drink, the camaraderie were really intended for the scientists and engineers whose years of work had led to such happy cause for celebration, but a few outsiders standing in the right place at propitious moments had also been invited.
When I arrived, too early, I found our host, a senior and much venerated planetary scientist at the nearby Jet Propulsion Laboratory, fabricating a model Saturn to hang at the driveway as a location
marker for the couple hundred guests. He had an old red tether ball with the cord still attached to it, and there on the cleared kitchen table he was cutting poster-board rings of the proper proportion to tape in place around it. A colleague came in through a back door and casually began offering technical advice, as though the current prank were some new research challenge. Within minutes, they had Saturn on a string, dangling from a branch.
Ingersoll, tall and bony, excels at modeling planetary atmospheres. He works the data points collected by telescopes and spacecraft—temperature readings, gas abundances, fluid pressures, wind speeds, cloud patterns—into sophisticated weather analyses. His journal publications have titles such as “The runaway greenhouse: A history of water on Venus,” “Dynamics of Jupiter’s cloud bands,” and “Seasonal buffering of atmospheric pressure on Mars.” He could likely match wits with any of the most famous astronomers in history, but he is unlikely to dominate the future, the way a Cassini or a Huygens persists today, because the nature of science itself has changed, from a field for lone geniuses to a collaborative effort.
The ebullient early-bird volleyball game in the Ingersolls’ backyard ended about half an hour later, when caterers came to lay out the long buffet and set up tables and folding chairs around and under the trees. In the group I happened to sit with, half the people were speaking Italian, and the other half a British-accented English. The party grew steadily more multinational because the
Cassini
spacecraft is global in every way. As the joint project of NASA, ESA (European Space Agency), and ASI (Agenzia Spaziale Italiana),
Cassini
represents seventeen countries and the pooled talents of some five thousand individuals, including a team of seamstresses who custom-tailored the spacecraft’s golden lamé thermal suit, to protect its instruments from dust-sized micrometeoroids and the extreme cold of the near-Saturn environment.
Each wave of latecomers to the party brought fresh bulletins from the lab. Some of them hadn’t slept in days, and looked it, but they relished the cause of their exhaustion. The news from
Cassini,
chattering into the Deep Space Network’s receivers in Spain, Australia, and California, was all good. Ideal, in fact. The craft’s first close-up pictures of Saturn’s rings exposed such depth of exquisite
detail that one astronomer had accused another, farther up in the data stream, of doctoring the images as a practical joke.
The adrenaline rush that most of these men and women had experienced the previous evening during
Cassini
’s passage through Saturn’s rings now mellowed into a general euphoria, a veritable Saturnalia. As the revelers toasted the present success, they also hailed the mission’s next major phase—the delivery, six months hence, of
Cassini
’s robotic passenger, the
Huygens
probe, to Saturn’s largest moon, Titan. That grand satellite, a body bigger than Mercury or Pluto, and possessed of a thick orange atmosphere as rich in nitrogen as our own air, had long intrigued scientists for its promised insights into conditions on the early Earth before life began. No one yet knew what lay on the smog-obscured surface of Titan, but many scientists were willing to wager great lakes filled with chill liquid methane and other hydrocarbons.
“I dream of landing in an ocean,”
Huygens
project scientist Jean-Pierre Lebreton had said the day before the party at a press briefing. “To go to Titan now is like going back in time to Earth four billion years ago.”
From the moment Christiaan Huygens first saw
Titan from The Hague in 1655, he called it simply “Saturn’s moon.” Jean Dominique Cassini, who found four other Saturnian moons between 1672 and 1684, was content to refer to them by number. And when Sir William Herschel sighted the
next
two in 1789, he, too, applied numerical designations. But Sir William’s son, Sir John Herschel, chose names for them all from Greek mythology, beginning with “Titan,” an ancient race of giants, the youngest of whom was Saturn.
*
* * *
IN DECEMBER
2004, on schedule,
Cassini
released the
Huygens
probe it had carried on its seven-year journey from Cape Canaveral, and nudged it toward Titan. For the next three weeks
Huygens,
still asleep, obediently coasted to its rendezvous, while
Cassini
executed another long loop around Saturn and returned in time for the planned excitement.
On January 14, 2005,
Huygens
’s internal alarm woke its systems to prepare for action at Titan.
The probe hit the atmosphere with its heat shield forward, decelerated in the friction of the thick air, and parachuted to a perfect landing. It sampled the clouds and haze all during its two-and-a-half-hour descent, and when it got close enough to the moon’s frigid surface (about thirty miles, as measured by the onboard radar) it photographed that, too, then relayed its findings to
Cassini,
and
Cassini
forwarded them to Earth.
On Titan,
Huygens
saw sights as familiar as clouds changing shape, as strange as the novel landscapes of an alien world, too unusual to be parsed.
The fact that
Huygens
survived touchdown and continued to broadcast evidence of its own robust health for several hours upset the widespread expectation of its drowning in a methane sea. However, the great dark expanse where
Huygens
laid itself to rest, now called Xanadu, cannot be viewed as the site of a failed prediction. Rather, it is the embarkation point for another new way of imagining the content of the Solar System, and of other solar systems as well. In July 2006,
Cassini
located several of the long-sought hydrocarbon lakes near Titan’s north pole.