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Harrison Nicholls (he/him)

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Research theme

  • Astronomy and astrophysics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Planetary Climate Dynamics
harrison.nicholls@physics.ox.ac.uk
  • About
  • Publications

Convective shutdown in the atmospheres of lava worlds

(2024)

Authors:

Harrison Nicholls, Raymond T Pierrehumbert, Tim Lichtenberg, Laurent Soucasse, Stef Smeets

Magma ocean evolution at arbitrary redox state

ArXiv 2411.19137 (2024)

Authors:

Harrison Nicholls, Tim Lichtenberg, Dan J Bower, Raymond Pierrehumbert

Exploring the evolution of lava planets using planet-resolving models

Copernicus Publications (2024)

Authors:

Harrison Nicholls, Tim Lichtenberg, Raymond Pierrehumbert

Distinguishing Oceans of Water from Magma on Mini-Neptune K2-18b

The Astrophysical Journal Letters American Astronomical Society 962:1 (2024) L8-L8

Authors:

Oliver Shorttle, Sean Jordan, Harrison Nicholls, Tim Lichtenberg, Dan J Bower

Abstract:

Mildly irradiated mini-Neptunes have densities potentially consistent with them hosting substantial liquid-water oceans ("Hycean" planets). The presence of CO2 and simultaneous absence of ammonia (NH3) in their atmospheres has been proposed as a fingerprint of such worlds. JWST observations of K2-18b, the archetypal Hycean, have found the presence of CO2 and the depletion of NH3 to 4 渭m region, where CO2 and CO features dominate: magma ocean models suggest a systematically lower CO2/CO ratio than estimated from free-chemistry retrieval, indicating that deeper observations of this spectral region may be able to distinguish between oceans of liquid water and magma on mini-Neptunes

Temperature鈥揷hemistry coupling in the evolution of gas giant atmospheres driven by stellar flares

Monthly Notices of the Royal Astronomical Society Oxford University Press 523:4 (2023) 5681-5702

Authors:

Harrison Nicholls, Olivia Venot

Abstract:

The effect of enhanced UV irradiation associated with stellar flares on the atmospheric composition and temperature of gas giant exoplanets was investigated. This was done using a 1D radiative-convective-chemical model with self-consistent feedback between the temperature and the non-equilibrium chemistry. It was found that flare-driven changes to chemical composition and temperature give rise to prolonged trends in evolution across a broad range of pressure levels and species. Allowing feedback between chemistry and temperature plays an important role in establishing the quiescent structure of these atmospheres, and determines their evolution due to flares. It was found that cooler planets are more susceptible to flares than warmer ones, seeing larger changes in composition and temperature, and that temperature鈥揷hemistry feedback modifies their evolution. Long-term exposure to flares changes the transmission spectra of gas giant atmospheres; these changes differed when the temperature structure was allowed to evolve self-consistently with the chemistry. Changes in spectral features due to the effects of flares on these atmospheres can be associated with changes in composition. The effects of flares on the atmospheres of sufficiently cool planets will impact observations made with JWST. It is necessary to use self-consistent models of temperature and chemistry in order to accurately capture the effects of flares on features in the transmission spectra of cooler gas giants, but this depends heavily on the radiation environment of the planet.

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