* Astronomy

Preferentially Earth-sized planets with lots of water

Computer simulations by astrophysicists at the University of Bern of the formation of planets orbiting in the habitable zone of low mass stars such as Proxima Centauri show that these planets are most likely to be roughly the size of the Earth and to contain large amounts of water.
In August 2016, the announcement of the discovery of a terrestrial exoplanet orbiting in the habitable zone of Proxima Centauri stimulated the imagination of the experts and the general public. After all this star is the nearest star to our sun even though it is ten times less massive and 500 times less luminous. This discovery together with the one in May 2016 of a similar planet orbiting an even lower mass star (Trappist-1) convinced astronomers that such red dwarfs (as these low mass stars are called) might be hosts to a large population of Earth-like planets.
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Title: Atmospheric dynamics of terrestrial exoplanets over a wide range of orbital and atmospheric parameters
Author: Yohai Kaspi, Adam P. Showman

The recent discoveries of terrestrial exoplanets and super-Earths extending over a broad range of orbital and physical parameters suggest that these planets will span a wide range of climatic regimes. Characterization of the atmospheres of warm super-Earths has already begun and will be extended to smaller and more distant planets over the coming decade. The habitability of these worlds may be strongly affected by their three-dimensional atmospheric circulation regimes, since the global climate feedbacks that control the inner and outer edges of the habitable zone including transitions to Snowball-like states and runaway-greenhouse feedbacks depend on the equator-to-pole temperature differences, patterns of relative humidity, and other aspects of the dynamics. Here, using an idealized moist atmospheric general circulation model including a hydrological cycle, we study the dynamical principles governing the atmospheric dynamics on such planets. We show how the planetary rotation rate, stellar flux, atmospheric mass, surface gravity, optical thickness, and planetary radius affect the atmospheric circulation and temperature distribution on such planets. Our simulations demonstrate that equator-to-pole temperature differences, meridional heat transport rates, structure and strength of the winds, and the hydrological cycle vary strongly with these parameters, implying that the sensitivity of the planet to global climate feedbacks will depend significantly on the atmospheric circulation. We elucidate the possible climatic regimes and diagnose the mechanisms controlling the formation of atmospheric jet streams, Hadley and Ferrel cells, and latitudinal temperature differences. Finally, we discuss the implications for understanding how the atmospheric circulation influences the global climate.

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Title: Atmospheric Circulation of Terrestrial Exoplanets
Authors: Adam P. Showman, Robin D. Wordsworth, Timothy M. Merlis, Yohai Kaspi

The investigation of planets around other stars began with the study of gas giants, but is now extending to the discovery and characterisation of super-Earths and terrestrial planets. Motivated by this observational tide, we survey the basic dynamical principles governing the atmospheric circulation of terrestrial exoplanets, and discuss the interaction of their circulation with the hydrological cycle and global-scale climate feedbacks. Terrestrial exoplanets occupy a wide range of physical and dynamical conditions, only a small fraction of which have yet been explored in detail. Our approach is to lay out the fundamental dynamical principles governing the atmospheric circulation on terrestrial planets--broadly defined--and show how they can provide a foundation for understanding the atmospheric behaviour of these worlds. We first survey basic atmospheric dynamics, including the role of geostrophy, baroclinic instabilities, and jets in the strongly rotating regime (the "extratropics") and the role of the Hadley circulation, wave adjustment of the thermal structure, and the tendency toward equatorial superrotation in the slowly rotating regime (the "tropics"). We then survey key elements of the hydrological cycle, including the factors that control precipitation, humidity, and cloudiness. Next, we summarise key mechanisms by which the circulation affects the global-mean climate, and hence planetary habitability. In particular, we discuss the runaway greenhouse, transitions to snowball states, atmospheric collapse, and the links between atmospheric circulation and CO2 weathering rates. We finish by summarising the key questions and challenges for this emerging field in the future.

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Title: A Plateau in the Planet Population Below Twice the Size of Earth
Authors: Erik A. Petigura, Geoffrey W. Marcy, Andrew W. Howard

We carry out an independent search of Kepler photometry for small transiting planets with sizes 0.5--8.0 times that of Earth and orbital periods between 5 and 50 days, with the goal of measuring the fraction of stars harbouring such planets. We use a new transit search algorithm, TERRA, optimised to detect small planets. We restrict our stellar sample to include the 12,000 stars having the lowest photometric noise in the Kepler survey. We report 129 planet candidates having radii less than 6 Earth-radii found in 3 years of Kepler photometry. Forty-seven of these candidates are not in Batalha et al. (2012). We gather Keck HIRES spectra for the majority of these targets leading to precise stellar radii and hence precise planet radii. We inject synthetic dimmings from mock transiting planets into the actual Kepler photometry and analyse that photometry with TERRA to assess detection completeness. We compute the occurrence of planets as a function of planet radius and period, correcting for the detection completeness. The resulting distribution of planet sizes exhibits a power law rise in occurrence from 5.7 Earth-radii down to 2 Earth-radii, as found in Howard et al. (2012). That rise clearly ends at 2 Earth-radii. The occurrence of planets is consistent with constant from 2 Earth-radii toward 1 Earth-radius. This unexpected plateau in planet occurrence at 2 Earth-radii suggests distinct planet formation processes for planets above and below 2 Earth-radii. We find 15.1% of solar type stars---roughly one in six---has a 1--2 Earth-radii planet with P = 5--50 days.

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