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commentary Strange news from other Raymond T. Pierrehumbert The dawn of discovery has unearthed a rich tapestry of planets different from anything encountered in the . Geoscientists can and should be in the vanguard of investigating what is out there in the Universe.

he frontispiece chosen for Gerard confirmed planet outside the Solar System, that call into question current understanding Kuiper’s 1949 book The Atmospheres there are now more than 600 confirmed of planet formation, composition and Tof the Earth and Planets1 was an aerial in the catalogue3. And over evolution: ‘Hot ’, ‘Black Jupiters’ and photograph of the Earth from a sounding 2,300 additional objects of interest from ‘Puffy Jupiters’ (see Box 1). rocket, labelled “The Earth as a Planet.” The the Kepler space mission are very Fans of small rocky planets are not left out book recognized the commonality in physics probably going to be added to the store4. either. Super Earths are planets with a governing the Earth and other planets of The era of exoplanet exploration opens up larger than Earth’s but too small to accrete the Solar System. With its publication, the vast opportunities for Earth scientists of enough hydrogen to turn into a gas giant. subject of comparative planetology was born. all stripes. They range from rocky specimens with a Before the 1950s, astrophysics, planetary What we know about these new additions permanent molten magma ocean to planets science and the Earth sciences — including to the planetary family comes from two with carbon-rich cores that may be made of study of Earth’s atmosphere and ocean — had main techniques used for finding exoplanets. diamond, and onwards to an unanticipated proceeded along largely separate tracks. All surveys detect the wobble in class of Super Earths of such low density that these fields were, however, pursuing closely a ’s motion caused by an orbiting planet, they must be largely or entirely composed related phenomena2. When these disciplines and surveys detect the slight dimming of light volatile materials such as water, broke out of their individual cages, goaded in in starlight when a planet passes between a hydrogen or carbon dioxide. part by the emergence of space exploration, star and the observer. To be able to observe a There are even bodies with super-hot it unleashed a creative storm that led to transit, a needs to be lined atmospheres, where it may snow rubies and seminal work on a number of crossover up just right. But there are a lot of stars with sapphires7. These extrasolar planetary set- problems between disciplines. planets out there, so the method still yields ups challenge the conventional boundaries For example, it became clear that the a rich bounty of planets. From either transit of what we consider to be a mineral, or even reduced of the early would or radial velocity observations, we learn at an atmosphere. Nevertheless, the underlying imply, all other things being equal, that the least the of the exoplanets (that is, the thermodynamic principles are precisely the Earth should have spent billions of length of ) and distance from the host same. Atmospheric scientists will learn to as a frozen snowball, which it manifestly star. Together with the star’s luminosity, these think of rock as just another kind of ice. did not; work on resolving this ‘faint young parameters provide a basis for estimating the Exoplanets provide the opportunity to Sun’ problem shed a great deal of light on planet’s climate. The radial velocity method observe processes that are key to planetary the climate of the ancient Earth. On the hot yields the eccentricity of the , as well as evolution, but no longer active in the Solar side of climates, the concept of a runaway the planet’s minimum mass, or even its actual System. Understanding how atmospheres are greenhouse effect, where incoming solar mass if the planet is known to be transiting. blown off planets through hydrodynamics radiation to a planet with an ocean can no Furthermore, the transit method yields is, for example, very important: a suitable longer be balanced by radiation of heat to the planet’s size and — for stars with multiple atmosphere is a great asset for habitability. space, was developed and then applied to planets — estimates of mass and eccentricity Dim red M stars are the most common kind Venus, suggesting a way our neighbour through analysis of subtle variations in the of star in the Universe. They are long lived, planet’s water could have been lost. The timing of transits. In those cases where a host many planets and would be excellent enigma of an evidently warm and wet early planet’s mass and radius are both known, candidates for habitability — were it not Mars, despite its current cold and dry state, we’ve hit the jackpot: mass and radius for the threat that their planets are subject was discovered. Inquiry into the range of together determine the density and hence to an extreme level of ultraviolet radiation distances from a planet’s star within which a constrain what the planet might be made that would be expected to blast away liquid water ocean can exist, given a suitable of. In some cases, the spectrum of starlight their atmospheres. atmosphere, led to the concept of habitable blocked by a transiting planet, or of planetary If very hot planets can retain hydrogen, zones. Missions to the bodies of the Solar emission blocked by the star when the planet it bodes well for the possible expansion of System have continued to yield spectacular passes behind it, provides information about the habitable zone through use of hydrogen discoveries. With so much learned from just the composition of the planet’s atmosphere. as a greenhouse gas. Cooler planets should eight planets and a stray object, There has been a focus on the search be able to retain hydrogen more easily8. think what could be done if only we had for Earth twins. However, it turns out that The signature of escaping hydrogen can be more planets to play with. there are a lot of interesting bodies out there seen in the Lyman-alpha ultraviolet lines Well, now we do — in fact, a whole lot that challenge conventional concepts. For of stars. This signature has been observed more. A mere seventeen years after the first example, there are three types of gas giants for a number of Hot Jupiters, where it is

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Box 1 | Exoplanetary diversity

Exoplanet exploration has revealed a great upi ot J ters diversity of planets radically different H Variously pu y, from anything encountered in the Solar evaporating, super-rotating System. Figure B1 displays these new types of planets in the context of their size and Cold Hot TrES 2b climate regime, with a few Solar System S/Searth 4 5 bodies for comparison. 0.001 0.010.1 110 100 1000 10 10

Gas giants Hot Jupiters. These are hydrogen-rich Black Jupiter tu gas giants in orbits so close to their stars Nep ne 10 that there would not be enough hydrogen Cancri earth -e available to form them in situ. Their very 55

existence shakes up theories of planetary R/R Diamond migration. 5 planet or gas midget? Black Jupiters. TrES 2b is an as-yet all Eart b hs ye ? unexplained Black Jupiter, a gas giant that is E epler-10b darker than coal. The kind of atmospheric 0 K chemistry that could account for this effect are he epler-11f ou re K Y 214 at present remains a mystery. GJ1 b

Puffy Jupiters. These hot gas giants Magma ocean? are larger than they ought to be, based Hot water Hot gas on conventional ideas about interior Super Earth midget temperatures. An unknown mechanism to deliver heat to deep interiors of gas giants is Figure B1 | The radius of the planet, relative to Earth’s, is shown on the vertical axis. The horizontal axis required to explain their existence. gives the amount of energy incident on the planet from its host star, relative to that incident on Earth

from the Sun. A planet with S/Searth = 1 would have the same climate as Earth if it had the same mass Super Earths and the same kind of atmosphere. The small blue dots are planet candidates identified by the Kepler Kepler-10b. With a radius 1.4 times that of space telescope. The relative lack of cold planets is due to difficulty of detection, as cold planets our own Earth and a density high enough generally orbit their stars at great distances, and also have long-period orbits that require several years to make it rocky, Kepler-10b is in an orbit of observation to detect. so close to its star that it is probably tide- locked, always presenting the same side inwards. Kepler-10b’s dayside would be hot times as much energy from its star as the it would have a magma ocean similarly enough to maintain a permanent molten Earth does from the Sun. During the star’s to Kepler-10b. Alternatively, 55 Cancri-e magma ocean. If so, the magma ocean youth, GJ1214b should have been blasted could be a carbon-rich solid planet without would outgas a rock-vapour atmosphere by massive fluxes of atmosphere-busting much volatile envelope6. What kind of that, cooling as it flowed towards the extreme ultraviolet radiation. How a large atmosphere such a planet would outgas nightside, would rain or snow out various volatile inventory could have been retained — and what this atmosphere would look minerals to the surface. If some of that under those conditions is an open question. like as (and if) it escapes into space — is atmosphere escapes to space, future a puzzle. The interior structure would, in observations of the starlight blocked by the Kepler-11f. This is another low-density any event, be novel: it would be composed escaping plume could provide information Super Earth in a hot orbit. A hydrogen largely of diamond. about the composition of the planet. envelope remains possible for this planet. Eyeball Earths GJ1214b. This exoplanet is similar in size 55 Cancri-e. Even more bizarre is 55 This is a hypothetical climate state expected to Kepler-10b, but its density is extremely Cancri-e, whose star can be seen with the for tide-locked ocean worlds in the outer low. GJ1214b is probably composed entirely in the . It portions of the habitable zone about M of a light volatile such as water5. GJ1214b is dense enough to require a rocky core, stars. Most of the ocean is frozen over, but orbits a dim red M star — the coolest class but light enough to require a volatile a pool of open water is maintained on the of stars — but so closely that it receives 16 envelope. Yet it is in such a close orbit that side of the planet. expected, but not for 55 Cancri-e, where it System’s distant past, including the runaway Most of the grand challenge questions would be equally expected if the planet has greenhouse and globally glaciated snowball that geoscientists have pondered for decades a hydrogen-rich envelope9. Planets can have states, have not yet been seen on exoplanets. need to be re-thought and generalized to magma oceans such as those that prevailed But with so many planets out there, it is deal with exoplanets. In this enterprise, the on the very early Earth, albeit with a different surely only a matter of time before we are cornucopia of exoplanets has something for cause. Other processes from the Solar able catch them in action. everybody. For geodynamicists, there is the

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question of whether plate tectonics occurs among exoplanets. We are therefore Raymond T. Pierrehumbert is in the Department of on rocky Super Earths10,11, with implications confronted with a real need to understand Geophysical Sciences at the University of Chicago, 5734 for atmospheric composition through its the climates of planets that may receive South Ellis Avenue, Chicago, Illinois 60637, USA. effect of recycling carbonate carbon back a hundred times as much illumination e-mail: [email protected] into the atmosphere. Fluid dynamicists during the brief periods of close approach will be interested to see how atmospheric as they do during their long, dark winters. References super-rotation — an atmosphere that rotates And given that planets orbiting reddish 1. Kuiper, G. P. The Atmospheres of the Earth and Planets (Univ. faster than the underlying planet — plays M stars appear to be common, we need Chigaco Press, 1949). out on a grander scale. According to theory, to come to an understanding of how the 2. Pierrehumbert, R. T. Tyndall Lecture, AGU 2012 Fall Meeting 12 abstr. GC431–01. Video available at http://fallmeeting.agu. Hot Jupiters should super-rotate , and greenhouse effect differs when a high org/2012/events/tyndall-lecture-gc43i-successful-predictions- super-rotation on exoplanets has already proportion of the incoming sunlight is near- video-on-demand/ (American Geophys. Union, 2012). been observed through its effect on the infrared and thus subject to absorption by 3. Wright, J. T. et al. Publ. Astron. Soc. Pac. 123, 412–422. Data 13 available at http://exoplanets.org (2011). time-course of infrared emission . Climate greenhouse gases. 4. Batalha, N. M. et al. Astrophys. J. Preprint at http://arXiv.org/ scientists may widen their horizons, too, Earth scientists are well placed to mine abs/1202.5852 Data available at http://planetquest.jpl.nasa.gov/ when considering habitable-zone planets this rich lode of new problems. They simply kepler (2012). 5. Bean, J. L., Kempton, E. M.-R. & Homeier, D. Nature around dim red M stars that are likely to be need to shed Earth-centric preconceptions, 468, 669–672 (2010). tide-locked, always presenting the same face and learn to extract general physical 6. Madhusudhan N., Lee, K. K. M. & Mousis, O. Astrophys. J. Lett. to their star. Already, the weak temperature principles of planetary climate from the 759, L40 (2012). 15 7. Helling, C. & Rietmeijer, F. J. M. Int. J. Astrobiol. 8, 3–8 (2009). gradient theory — worked out for the lessons learned from their work on Earth . 8. Pierrehumbert, R. T. & Gaidos, E. Astrophys. J. Lett. 734, L13 (2011). Earth’s tropics — has turned out to be the As new observing platforms such as the 9. Ehrenreich, D. et al. Astron. Astrophys. Preprint at http://arXiv. key to understanding when horizontal heat Giant Magellan telescope and the James org/abs/1210.0531 (2012). transports are strong enough to keep the Webb Space telescope come online, the 10. Valencia, D., O’Connell, R. J. & Sasselov, D. D. Astrophys. J. Lett. 670, L45 (2007). atmospheres of tide-locked planets from present flood of planetary data is poised to 11. Lenardic, A. & Crowley, J. W. Astrophys. J. 755, 132 (2012). snowing out on the nightside14. become a veritable torrent. It’s going to be 12. Showman, A. P. & Polvani, L. M. Astrophys. J. 738, 71 (2011). In contrast to the rather boring, nearly a wild ride down the rapids. Geoscientists 13. Knutson, H. A. et al. Nature 447, 183–186 (2007). 14. Pierrehumbert, R. T. Astrophys. J. Lett. 726, L8 (2011). circular orbits that prevail in the Solar should hold on to their hats and jump right 15. Pierrehumbert, R. T. Principles of Planetary Climate (Cambridge System, high eccentricities are common on board — the more, the merrier. ❐ Univ. Press, 2010).

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