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Jupiter's Para-H2 Distribution from SOFIA/FORCAST and Voyager/IRIS 17-37 µm Spectroscopy

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posted on 01.12.2016, 12:26 by Leigh N. Fletcher, I. de Pater, W. T. Reach, M. Wong, G. Orton, P. G. J. Irwin, R. D. Gehrz
Spatially resolved maps of Jupiter’s far-infrared 17–37 µm hydrogen-helium collision-induced spectrum were acquired by the FORCAST instrument on the Stratospheric Observatory for Infrared Astronomy (SOFIA) in May 2014. Spectral scans in two grisms covered the broad S(0) and S(1) absorption lines, in addition to contextual imaging in eight broad-band filters (5–37 µm) with spatial resolutions of 2–4″. The spectra were inverted to map the zonal-mean temperature and para-H2 distribution (fp, the fraction of the para spin isomer with respect to the ortho spin isomer) in Jupiter’s upper troposphere (the 100–700 mbar range). We compared these to a reanalysis of Voyager-1 and -2 IRIS spectra covering the same spectral range. Tropospheric temperature contrasts match those identified by Voyager in 1979, within the limits of temporal variability consistent with previous investigations. Para-H2 increases from equator to pole, with low-fp air at the equator representing sub-equilibrium conditions (i.e., less para-H2 than expected from thermal equilibration), and high-fp air and possible super-equilibrium at higher latitudes. In particular, we confirm the continued presence of a region of high-fp air at high northern latitudes discovered by Voyager/IRIS, and an asymmetry with generally higher fp in the north than in the south. Far-IR aerosol opacity is not required to fit the data, but cannot be completely ruled out. We note that existing collision-induced absorption databases lack opacity from (H2)2 dimers, leading to under-prediction of the absorption near the S(0) and S(1) peaks. There appears to be no spatial correlation between para-H2 and tropospheric ammonia, phosphine and cloud opacity derived from Voyager/IRIS at mid-infrared wavelengths (7–15 µm). We note, however, that para-H2 tracks the similar latitudinal distribution of aerosols within Jupiter’s upper tropospheric and stratospheric hazes observed in reflected sunlight, suggesting that catalysis of hydrogen equilibration within the hazes (and not the main clouds) may govern the equator-to-pole gradient, with conditions closer to equilibrium at higher latitudes. This gradient is superimposed onto smaller-scale variations associated with regional advection of para-H2 at the equator and poles.

Funding

This work was based on observations made with the NASA/DLR Stratospheric Observatory for Infrared Astronomy (SOFIA), and was financially supported through SOF0012 to the University of California, Berkeley. SOFIA is jointly operated by the Universities Space Research Association, Inc. (USRA), under NASA contract NAS2-97001, and the Deutsches SOFIA Institut (DSI) under DLR contract 50 OK 0901 to the University of Stuttgart. We are grateful for all those involved in the telescope engineering, operations support and the flight crews. We thank Luke Keller, Matthew Bellardini and Joseph Quinn (Ithaca College) and Joseph Adams for their assistance with the initial planning and calibration of the SOFIA data. Fletcher was supported by a Royal Society Research Fellowship at the University of Leicester. The UK authors acknowledge the support of the Science and Technology Facilities Council (STFC). A portion of this work was performed by Orton at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA. Gehrz received partial support from the United States Air Force. This research used the ALICE High Performance Computing Facility at the University of Leicester.

History

Citation

Icarus 2016

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Physics and Astronomy

Version

VoR (Version of Record)

Published in

Icarus 2016

Publisher

Elsevier for Academic Press

issn

0019-1035

Acceptance date

04/10/2016

Copyright date

2016

Available date

01/12/2016

Publisher version

http://www.sciencedirect.com/science/article/pii/S0019103516301269

Language

en

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