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Black Hole

Lensing of space time around a black hole. At Oxford we study black holes observationally and theoretically on all size and time scales - it is some of our core work.

Credit: ALAIN RIAZUELO, IAP/UPMC/CNRS. CLICK HERE TO VIEW MORE IMAGES.

Dr Jake Taylor (he/him)

Glasstone Fellow

Research theme

  • Astronomy and astrophysics
  • Exoplanets and planetary physics

Sub department

  • Astrophysics

Research groups

  • Exoplanet atmospheres
  • Exoplanets and Stellar Physics
jake.taylor@physics.ox.ac.uk
Denys Wilkinson Building, room 463
  • About
  • Prizes, awards and recognition
  • Publications

APPLESOSS: A Producer of ProfiLEs for SOSS. Application to the NIRISS SOSS Mode

Publications of the Astronomical Society of the Pacific IOP Publishing 134:1040 (2022) 104502-104502

Authors:

Michael Radica, Loïc Albert, Jake Taylor, David Lafrenière, Louis-Philippe Coulombe, Antoine Darveau-Bernier, René Doyon, Neil Cook, Nicolas Cowan, Néstor Espinoza, Doug Johnstone, Lisa Kaltenegger, Caroline Piaulet, Arpita Roy, Geert Jan Talens

Abstract:

Abstract The SOSS mode of the Near Infrared Imager and Slitless Spectrograph instrument is poised to be one of the workhorse modes for exoplanet atmosphere observations with the newly launched James Webb Space Telescope (JWST). One of the challenges of the SOSS mode, however, is the physical overlap of the first two diffraction orders of the G700XD grism on the detector. Recently, the ATOCA algorithm was developed and implemented as an option in the official JWST pipeline, as a method to extract SOSS spectra by decontaminating the detector—that is, separating the first and second orders. Here, we present A Producer of ProfiLEs for SOSS (APPLESOSS), which generates the spatial profiles for each diffraction order upon which ATOCA relies. We validate APPLESOSS using simulated SOSS time series observations of WASP-52 b, and compare it to ATOCA extractions using two other spatial profiles (a best and worst case scenario on-sky), as well as a simple box extraction performed without taking into account the order contamination. We demonstrate that APPLESOSS profiles retain a high degree of fidelity to the true underlying spatial profiles, and therefore yield accurate extracted spectra. We further confirm that the effects of the order contamination for relative measurements (e.g., exoplanet transmission or emission observations) is small—the transmission spectrum obtained from each of our four tests, including the contaminated box extraction, is consistent at the ∼1 σ level with the atmosphere model input into our noiseless simulations. We further confirm via a retrieval analysis that the atmosphere parameters (metallicity and C/O) obtained from each transmission spectrum are consistent with the true underlying values.

ATOCA: an Algorithm to Treat Order Contamination. Application to the NIRISS SOSS Mode

PUBLICATIONS OF THE ASTRONOMICAL SOCIETY OF THE PACIFIC 134:1039 (2022) ARTN 094502

Authors:

Antoine Darveau-Bernier, Loic Albert, Geert Jan Talens, David Lafreniere, Michael Radica, Rene Doyon, Neil J Cook, Jason F Rowe, Romain Allart, Etienne Artigau, Bjorn Benneke, Nicolas Cowan, Lisa Dang, Nestor Espinoza, Doug Johnstone, Lisa Kaltenegger, Olivia Lim, Tyler Pauly, Stefan Pelletier, Caroline Piaulet, Arpita Roy, Pierre-Alexis Roy, Jared Splinter, Jake Taylor, Jake D Turner

Identification of carbon dioxide in an exoplanet atmosphere.

Nature (2022)

Abstract:

Carbon dioxide (CO2) is a key chemical species that is found in a wide range of planetary atmospheres. In the context of exoplanets, CO2 is an indicator of the metal enrichment (that is, elements heavier than helium, also called 'metallicity')1-3, and thus the formation processes of the primary atmospheres of hot gas giants4-6. It is also one of the most promising species to detect in the secondary atmospheres of terrestrial exoplanets7-9. Previous photometric measurements of transiting planets with the Spitzer Space Telescope have given hints of the presence of CO2, but have not yielded definitive detections owing to the lack of unambiguous spectroscopic identification10-12. Here we present the detection of CO2 in the atmosphere of the gas giant exoplanet WASP-39b from transmission spectroscopy observations obtained with JWST as part of the Early Release Science programme13,14. The data used in this study span 3.0-5.5 micrometres in wavelength and show a prominent CO2 absorption feature at 4.3 micrometres (26-sigma significance). The overall spectrum is well matched by one-dimensional, ten-times solar metallicity models that assume radiative-convective-thermochemical equilibrium and have moderate cloud opacity. These models predict that the atmosphere should have water, carbon monoxide and hydrogen sulfide in addition to CO2, but little methane. Furthermore, we also tentatively detect a small absorption feature near 4.0 micrometres that is not reproduced by these models.

Impact of variable photospheric radius on exoplanet atmospheric retrievals

Monthly Notices of the Royal Astronomical Society: Letters 513:1 (2022) L20-L24

Abstract:

Inverse techniques are used to extract information about an exoplanet's atmosphere. These techniques are prone to biased results if the appropriate forward model is not used. One assumption used in a forward model is to assume that the radius of the planet is constant with wavelength; however, a more realistic assumption is that the photospheric radius varies with each wavelength. We explore the bias induced when attempting to extract the molecular abundance from an emission spectrum, which was generated with a variable radius. We find that for low-gravity planets, the retrieval model is not able to fit the data if a constant radius model is used. We find that biased results are obtained when studying a typical hot Jupiter in the MIRI LRS wavelength range. Finally, we show that high-gravity planets do not suffer a bias. We recommend that future spectral retrievals that interpret exoplanet emission spectra should take into account a variable radius.

Impact of Variable Photospheric Radius on Exoplanet Atmospheric Retrievals

ArXiv 2203.01839 (2022)

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