Warwick Astronomy PhD Projects

Remnants of planetary systems around white dwarfs

We know over 7000Link opens in a new window extrasolar planets, with the overwhelming majority orbiting solar-like stars. Thinking about the long-term evolution of these planets, some of the following questions come to mind: What is the future of these planetary systems as their host stars evolve off the main sequence? What will happen to our solar system once the Sun dies? And what information can we learn from those evolved planetary systems that is other inaccessible?

The final fate of planetary systems:

As the planet host stars evolve into red giants, and eventually into white dwarfs, they lose substantial amounts of mass. This lost layers of mass can be seen for some time as planetary nebulae. Consequently, the orbits of the planets, and all minor bodies, asteroids, and comets, will widenLink opens in a new window, with many of them moving far beyond the maximum radius that the star will reach during the red giant phase. In our solar system, Mars, the asteroid belt, and all the giant planets will escape evaporationLink opens in a new window. In other words, in ~6Gyr, the solar system will consist of a white dwarf with one rocky planet, four giant planets, and countless asteroids and comets. Thus, what we expect to be left behind by the 1000s of known planetary systems are white dwarfs, bearing the remnants of planetary systems.

Artist impression of the gaseous debris disc formed from the disruption of a rocky asteroid in the strong gravitational field of a white dwarf. It is very likely that the solar system will undergo episodes like this once the Sun has evolved into a white dwarf in ~6 Gyr from now - studying systems like this allows a glimpse into the remote future of our own planetary system. (c) Mark Garlick and University of Warwick.

Planets orbiting white dwarfs:

The first detections of planetary systems around white dwarfs came not in the form of their planets, but asteroids. Just as we know about sun-grazing asteroids, ever now and then an extrasolar asteroid will have its orbit perturbed by a larger body, venture too close to the white dwarf, and by tidally shreddedLink opens in a new window and form a debris disc of dustLink opens in a new window and gasLink opens in a new window.

Whereas 100s of white dwarfs are known to still have asteroid belts, the detection of planets has proven more difficult. The reason is that the standard methods to identify planets are much, much harder in the case of white dwarfs. Measuring the Doppler wobbleLink opens in a new window requires high-resolution spectroscopy, and most white dwarfs are too faint for current instruments (that will change with the E-ELTLink opens in a new window). Similarly, the detection of transitsLink opens in a new window requires a line of sight very closely aligned with the orbital plane of the planet. Because the chances of that are relatively low, vast numbers of stars need to be monitored photometrically, and, again because of their faintness, that has remained a challenge (but see below).

In 2019, we discovered the first evidence for a giant planetLink opens in a new window in a close orbit around a white dwarf, that is being evaporated by the strong ultraviolet radiation from the white dwarf. This led us to think again more carefully about the future of the solar system, and we realised that the white dwarf left behind by the Sun will be be so luminous in the ultraviolet that it will drive detectable amounts of mass lossLink opens in a new window from Jupiter, Saturn, Uranus and Neptune. Detectable by some alien astronomer who, in 6Gyr, points their telescope at the solar white dwarf.

This animation shows the white dwarf WDJ0914+1914 and its Neptune-like exoplanet. Since the icy giant orbits the hot white dwarf at close range, the extreme ultraviolet radiation from the star strips away the planet’s atmosphere. While most of this stripped gas escapes, giving the planet a comet-like tail, some of it swirls into a disc, itself accreting onto the white dwarf. (c) ESO/M. Kornmesser

Only a year later, the first transiting giant planet candidateLink opens in a new window has been found from the analysis of TESS observations of a white dwarf. This is extremely exciting, as this white dwarf is only ~25pc away, so such systems may not be so rare after all! However, since 2020, no other transiting planets orbiting white dwarfs have been found.

Be part of this exciting area of exo-planet research:

Within your PhD, you will become involved in this exciting and novel research area. You will use the latest and most powerful photometric surveys to search for transiting planets and transits from disintegrating planetesimals. You will use of the "epoch photometry" from the Gaia space missionLink opens in a new window, which will become available in December 2026, as well as the unrivalled photometry from the Vera Rubin ObservatoryLink opens in a new window - and later the Warwick-led Digital TelescopeLink opens in a new window, a novel design that continuously scans the sky without any moving part. You will study the physical properties of the planets found in this project using optical and infrared follow-up observations obtained with the Very Large Telescope of the European Southern Observatory and the James Webb Telescope, respectively, and thereby learn about the physical processes in planetary atmospheres. You will have the opportunity to investigate in detail the disruption of planetesimals, and the formation and evolution of debris discs. Your PhD project will contribute to our overall understanding of the formation, structure, and evolution of planets in a way that cannot be achieved from studies of "normal" planets orbiting main-sequence planets.

If you have any questions regarding this project, please get in touch by e-mail (Boris.Gaensicke@warwick.ac.uk).

Supervisor: Boris GänsickeLink opens in a new window