HST hot Jupiter Transmission Spectral Survey: A detection of Na and strong optical absorption in HAT-P-1b

(2013)

Authors:

N Nikolov, DK Sing, F Pont, AS Burrows, JJ Fortney, GE Ballester, TM Evans, CM Huitson, HR Wakeford, PA Wilson, S Aigrain, D Deming, NP Gibson, GW Henry, H Knutson, A Lecavelier des Etangs, AP Showman, A Vidal-Madjar, K Zahnle

The optical transmission spectrum of the hot Jupiter HAT-P-32b: clouds explain the absence of broad spectral features?

(2013)

Authors:

NP Gibson, S Aigrain, JK Barstow, TM Evans, LN Fletcher, PGJ Irwin

HST hot Jupiter transmission spectral survey: evidence for aerosols and lack of TiO in the atmosphere of WASP-12b

ArXiv 1309.5261 (2013)

Authors:

DK Sing, A Lecavelier des Etangs, JJ Fortney, AS Burrows, F Pont, HR Wakeford, GE Ballester, N Nikolov, GW Henry, S Aigrain, D Deming, TM Evans, NP Gibson, CM Huitson, H Knutson, AP Showman, A Vidal-Madjar, PA Wilson, MH Williamson, K Zahnle

Abstract:

We present HST optical transmission spectra of the transiting hot Jupiter WASP-12b, taken with the STIS instrument. From the transmission spectra, we are able to decisively rule out prominent absorption by TiO in the exoplanet's atmosphere. Strong pressure-broadened Na and K absorption signatures are also excluded, as are significant metal-hydride features. We compare our combined broadband spectrum to a wide variety of existing aerosol-free atmospheric models, though none are satisfactory fits. However, we do find that the full transmission spectrum can be described by models which include significant opacity from aerosols: including Rayleigh scattering, Mie scattering, tholin haze, and settling dust profiles. The transmission spectrum follows an effective extinction cross section with a power-law of index alpha, with the slope of the transmission spectrum constraining the quantity alphaT = -3528+/-660 K, where T is the atmospheric temperature. Rayleigh scattering (alpha=-4) is among the best fitting models, though requires low terminator temperatures near 900 K. Sub-micron size aerosol particles can provide equally good fits to the entire transmission spectrum for a wide range of temperatures, and we explore corundum as a plausible dust aerosol. The presence of atmospheric aerosols also helps to explain the modestly bright albedo implied by Spitzer observations, as well as the near black body nature of the emission spectrum. Ti-bearing condensates on the cooler night-side is the most natural explanation for the overall lack of TiO signatures in WASP-12b, indicating the day/night cold-trap is an important effect for very hot Jupiters. These finding indicate that aerosols can play a significant atmospheric role for the entire wide range of hot-Jupiter atmospheres, potentially affecting their overall spectrum and energy balance.(abridged)

HST hot Jupiter transmission spectral survey: evidence for aerosols and lack of TiO in the atmosphere of WASP-12b

(2013)

Authors:

DK Sing, A Lecavelier des Etangs, JJ Fortney, AS Burrows, F Pont, HR Wakeford, GE Ballester, N Nikolov, GW Henry, S Aigrain, D Deming, TM Evans, NP Gibson, CM Huitson, H Knutson, AP Showman, A Vidal-Madjar, PA Wilson, MH Williamson, K Zahnle

Nonlinear Phenomena in Atmospheric and Oceanic Sciences

Springer, 2013

Authors:

George Carnevale, Raymond T Pierrehumbert

Abstract:

This IMA Volume in Mathematics and its Applications NONLINEAR PHENOMENA IN ATMOSPHERIC AND OCEANIC SCIENCES is based on the proceedings of a workshop which was an integral part of the 1989-90 IMA program on "Dynamical Systems and their ...