GeminiFocus October 2015 | Page 9

voked — “cold start” and “hot start” — lead to very different observable properties. For instance, in the cold start scenario, gas accretion reaches a runaway stage, producing shocks that radiate away all the incoming energy, resulting in a low temperature, low luminosity planet. In the hot start scenario, the shocks are radiatively ineffective, resulting in a planet with both high luminosity and high temperature. Of course, intermediate models are possible with initial entropy varying between these two extreme cases. The only way to determine the initial conditions is, therefore, to study young planetary systems. Previous directly-imaged exoplanets had luminosities only compatible with those predicted by the hot start scenario, whereas 51 Eri b is faint enough to be reproduced by both scenarios. The cold start scenario is usually associated with the core accretion formation mechanism, in which a core is built from planetesimal agglomerations followed by rapid gas capture. This mechanism is the adopted hypothesis to explain the formation of the gas giants in the Solar System. Therefore, 51 Eri b might have formed like Jupiter, with modest extensions to the classical core accretion model; like the pebble accretion which facilitates planet formation at larger distances than the typical 1-5 AU from the central star. Tip of the Iceberg? 51 Eri b is the first exoplanet found by GPI. It belongs to a low mass, low temperature, methane dominated, close-in category to which earlier instruments were not sensitive enough to detect in previous exoplanet searches. We hope it represents the tip of October 2015 the iceberg of extrasolar planets that will be directly imaged in the next few years — especially by instruments such as GPI, and its European cousin: the Spectro-Polarimetric High-contrast Exoplanet Research (SPHERE) at the Very Large Telescope. The direct exoplanet imaging community is undertaking large-scale campaigns, which will hopefully lead to additional discoveries that will place our own Solar System in the context of other extrasolar systems. Studies such as these are the key to understanding the formation of giant planets, their evolution, and, ultimately, how they interact with potentially life-bearing terrestrial planets, which will undoubtedly be discovered with future instruments. Figure 5. An artist’s visualization of the Jupiter-like exoplanet, 51 Eri b, seen in the near-infrared light that shows the hot layers deep in its atmosphere glowing through clouds. Because of its young age, this young cousin of our own Jupiter is still hot and carries information on the way it was formed 20 million years ago. Credit: Danielle Futselaar & Franck Marchis (SETI Institute). Julien Rameau is a postdoctoral fellow at the Institut de Recherche sur les Exoplanètes, Université de Montréal. He can be contacted at: [email protected] Robert De Rosa is a postdoctoral fellow at the University of California Berkeley. He can be contacted at: [email protected] GeminiFocus 7