No detection of methane on Mars from early ExoMars Trace Gas Orbiter observations

Nature Springer Nature (2019)

Authors:

Oleg Korablev, Ann Carine Vandaele, Franck Montmessin, Anna A Fedorova, Alexander Trokhimovskiy, François Forget, Franck Lefèvre, Frank Daerden, Ian R Thomas, Loïc Trompet, Justin T Erwin, Shohei Aoki, Séverine Robert, Lori Neary, Sébastien Viscardy, Alexey V Grigoriev, Nikolay I Ignatiev, Alexey Shakun, Andrey Patrakeev, Denis A Belyaev, Jean-Loup Bertaux, Kevin S Olsen, Lucio Baggio, Juan Alday, Yuriy S Ivanov, Bojan Ristic, Jon Mason, Yannick Willame, Cédric Depiesse, Laszlo Hetey, Sophie Berkenbosch, Roland Clairquin, Claudio Queirolo, Bram Beeckman, Eddy Neefs, Manish R Patel, Giancarlo Bellucci, Jose-Juan López-Moreno, Colin F Wilson, Giuseppe Etiope, Lev Zelenyi, Håkan Svedhem, Jorge L Vago

A brightening of Jupiter’s auroral 7.80-μm CH4 emission during a solar-wind compression

Nature Astronomy Nature Research 3:2019 (2019) 607-613

Authors:

J Sinclair, G Orton, J Fernandes, Y Kasaba, T Sato, T Fujiyoshi, C Tao, F Vogt, G Grodent, B Bonfond, J Moses, T Greathouse, W Dunn, R Giles, F Tabataba-Vakili, L Fletcher, Patrick Irwin

Abstract:

Enhanced mid-infrared emission from CH4 and other stratospheric hydrocarbons has been observed coincident with Jupiter’s ultraviolet auroral emission1,2,3. This suggests that auroral processes and the neutral stratosphere of Jupiter are coupled; however, the exact nature of this coupling is unknown. Here we present a time series of Subaru-COMICS images of Jupiter measured at a wavelength of 7.80 μm on 11–14 January, 4–5 February and 17–20 May 2017. These data show that both the morphology and magnitude of the auroral CH4 emission vary on daily timescales in relation to external solar-wind conditions. The southern auroral CH4 emission increased in brightness temperature by about 3.8 K between 15:50 UT, 11 January and 12:57 UT, 12 January, during a predicted solar-wind compression. During the same compression, the northern auroral emission exhibited a duskside brightening, which mimics the morphology observed in the ultraviolet auroral emission during periods of enhanced solar-wind pressure4,5. These results suggest that changes in external solar-wind conditions perturb the Jovian magnetosphere in such a way that energetic particles are accelerated into the planet’s atmosphere, deposit their energy as deep as the neutral stratosphere, and modify the thermal structure, the abundance of CH4 or the population of energy states of CH4. We also find that the northern and southern auroral CH4 emission evolved independently between the January, February and May images, as has been observed at X-ray wavelengths over shorter timescales6 and at mid-infrared wavelengths over longer timescales7.

Ethane in Titan's Stratosphere from Cassini CIRS Far- and Mid-infrared Spectra

ASTRONOMICAL JOURNAL 157:4 (2019) ARTN 160

Authors:

Nicholas A Lombardo, Conor A Nixon, Melody Sylvestre, Donald E Jennings, Nicholas Teanby, Patrick JG Irwin, F Michael Flasar

Corrigendum to “Neptune's carbon monoxide profile and phosphine upper limits from Herschel/SPIRE” (Icarus, vol 319, p86–98, 2019) (Icarus (2019) 319 (86–98), (S0019103518304457), (10.1016/j.icarus.2018.09.014))

Icarus 322 (2019) 261-261

Authors:

NA Teanby, PGJ Irwin, JI Moses

Abstract:

© 2018 The authors would like to publish the below information which was incorrectly published in its original version. Page 90: The equation for saturation vapour pressure should be PSVP(T) =exp(a+b/T +cT). Page92: TheD/HratiomeasuredbyFeuchtgruberetal.(2013)fromHerschelPACSshouldbe 4.1±0.4×10−5. References Feuchtgruber, H., Lellouch, E., Orton, G., de Graauw, T., Vandenbussche, B., Swinyard, B., Moreno, R., Jarchow, C., Billebaud, F., Cavali´e, T., Sidher, S., Hartogh, P., 2013. The D/H ratio in the atmospheres of Uranus and Neptune from Herschel-PACS observations. Astron. Astrophys. 551, 1–9.

Particle Size Effects on Mid‐Infrared Spectra of Lunar Analog Minerals in a Simulated Lunar Environment

Journal of Geophysical Research Planets American Geophysical Union (AGU) 124:4 (2019) 970-988

Authors:

KA Shirley, TD Glotch