Nemesis

Nemesis, by Alfred Rethel (1837)

About NEMESIS

NEMESIS is a general-purpose radiative transfer and retrieval code, designed to be applicable to any planetary atmosphere (solar system and exoplanets) and can handle a wide range of observation geometries. The NEMESIS code actually has two components, the NEMESIS retrieval tool itself and also the more general radiative transfer code, RADTRAN, from which it was developed. The Nemesis project is a collaborative effort and is continually being developed and extended. It is managed with Github and the repository can be found here. Scientists interested in running either NEMESIS or RADTRAN to analyse their data are very welcome to contact us.

NEMESIS

NEMESIS (Non-linear optimal Estimator for MultivariatE spectral analySIS) is the general purpose correlated-k/LBL retrieval code developed from the RADTRAN project. The original version, developed in 2003 and used for analysing Cassini/CIRS observations of Jupiter, Saturn and Titan, was based on the correlated-k approximation. However, NEMESIS now also now works in line-by-line (LBL) mode. It has been designed to be generally applicable to any planet and with any observing mode and so is suitable for both solar-system studies and also exoplanetary studies. The reference NEMESIS paper is "The NEMESIS planetary atmosphere radiative transfer and retrieval tool", J. Quant. Spectrosc. and Rad. Trans., 109, 1136-1150, 2008. (DOI: 10.1016/j.jqsrt.2007.11.006): the accepted manuscript of this paper is here. For more details please see our Manuals page.

RADTRAN

RADTRAN is a general purpose planetary radiative transfer model for computing the transmission of atmospheric paths and/or the radiances emitted by planetary atmospheres. The code is general purpose and not hard-wired to any specific planet. RADTRAN evolved from Genlbl, which was a general purpose planetary line-by-line model, developed by Dr Simon Calcutt. RADTRAN extended the functionality of this program to also allow the computation of planetary spectra using both band model approximations and also the correlated-k approximation. The code has also been extended to incorporate both multiple scattering and single scattering calculations. For more details please see our Manuals page.

Team NEMESIS

Originated in Oxford in 2003, NEMESIS has since grown and become used by many groups around the world. Many individuals have contributed to the development of NEMESIS, including:

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    Patrick Irwin

    Patrick Irwin is a Professor of Planetary Physics at the University of Oxford and is the lead developer of NEMESIS, developing the original version in 2003. He works in the fields of both solar system and exoplanetary atmospheres and specialises in modelling the scattering effects of clouds. He has over 20 years experience in remote sensing of planetary atmospheres from satellite observations and more recently ground-based observations. He is the principal author or co-author of over 200 papers published in the open scientific literature.


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    Leigh Fletcher

    Leigh Fletcher is an Associate Professor in Planetary Science at the University of Leicester and is a lead contributer to NEMESIS in the field of solar system science. More bio. to be added.


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    Nick Teanby

    Nick Teanby is a Reader in Planetary Science at the University of Bristol and is a lead contributer to NEMESIS in the field of solar system science from the sub-mm to mid-IR. In particular the atmospheres of Titan and the ice giants, but also the gas giants and Mars.


Other biographies and links to be added here.

References

Irwin, P.G.J., N.A. Teanby, R. de Kok, L.N. Fletcher, C.J.A. Howett, C.C.C. Tsang, C.F. Wilson, S.B. Calcutt, C.A. Nixon, P.D. Parrish, The NEMESIS planetary atmosphere radiative transfer and retrieval tool, J. Quant. Spectrosc. and Rad. Trans., 109, 1136-1150, 2008. doi:10.1016/j.jqsrt.2007.11.006. The accepted open-access manuscript is here.

Irwin, P. G. J., S. B. Calcutt and F. W. Taylor, Radiative transfer models for Galileo NIMS studies of the atmosphere of Jupiter. Adv. Space. Res. 19, doi:10.1016/S0273-1177(97)00266-4.

Why is it called NEMESIS?

Nemesis is traditionally known as the Goddess of Vengeance and Retribution. Some authors connect the name with “to feel just resentment” or “righteous anger”. However, the word Nemesis originally meant the distributor of fortune, whether good or bad, in due proportion to each man according to his deserts.

As Nemesis/Fortuna, a conflation of the Greek deity of fate with the Roman Fortuna, she was perceived not as bringer of retribution, but as having the power of changing fortune. Hence, she was an ideal deity to make patron goddess of gladiators. It is thought that gladiators made offerings to this “goddess of fortune” before fighting in the Roman arenas. It is the “goddess of fortune” view of Nemesis, which inspired the naming of this retrieval code in her honour. It is hoped that Nemesis will bring good fortune and will considerably improve the retrieval of atmospheric properties from remotely-sensed infrared planetary spectra.