instrumentation: spectrographs; space vehicles: instruments; planets and satellites: atmospheres; planets and satellites: individual: Mars; planets and satellites: composition
Abstract :
[en] We have obtained the first continuous disk averaged spectrum of Mars from 450 to 1550 Ghz using the Herschel-SPIRE Fourier-transform spectrometer. The spectrum was obtained at a constant resolution of 1.4 GHz across the whole band. The flux from the planet is such that the instrument was operated in “bright source” mode to prevent saturation of the detectors. This was the first successful use of this mode and in this work we describe the method used for observing Mars together with a detailed discussion of the data reduction techniques required to calibrate the spectrum. We discuss the calibration accuracy obtained and describe the first comparison with surface and atmospheric models. In addition to a direct photometric measurement of the planet the spectrum contains the characteristic transitions of [SUP]12[/SUP]CO from J 5-4 to J 13-12 as well as numerous H[SUB]2[/SUB]O transitions. Together these allow the comparison to global atmospheric models allowing the mean mixing ratios of water and [SUP]12[/SUP]CO to be investigated. We find that it is possible to match the observed depth of the absorption features in the spectrum with a fixed water mixing ratio of 1×10[SUP]-4[/SUP] and a [SUP]12[/SUP]CO mixing ratio of 9×10[SUP]-4[/SUP]. Herschel is an ESA space observatory with science instruments provided by European-led Principal Investigator consortia and with important participation from NASA.
Disciplines :
Space science, astronomy & astrophysics
Author, co-author :
Swinyard, B. M.; STFC Rutherford Appleton Laboratory, Harwell Innovation Campus, Didcot, OX11 0QX, UK
Hartogh, P.; Max Planck Institute for Solar System Research, Katlenburg-Lindau 37191, Germany
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Bibliography
Biver, N., Lecacheux, A., Encrenaz, T., et al 2005, A&A, 435, 765
Burgdorf, M. J., Encrenaz, Th., Lellouch, E., et al 2000, Icarus, 145, 79
Clancy, R. T., Grossman, A. W.,Wolff, M. J., et al 1996, Icarus, 122, 36
Encrenaz, T., Lellouch, E., Paubert, G., & Gulkis, S 2001, Planet. Space Sci. 49(7) 731
Encrenaz, T., Fouchet, T., Melchiorri, R., et al 2008, A&A, 484, 547
Encrenaz, Th., Fouchet, T., Melchiorri, R. et al 2006, A&A, 459, 265
Fouchet, T., Lellouch, E., Ignatiev, N. I., et al 2007, Icarus, 190, 32
Forget, F., et al 1999, J. Geophys. Res., 104, Issue E10, 24155
Fulton, T., et al 2008, Proc SPIE 7010, 70102T
Griffin, M. J., et al 2010, A&A, 518, L3
Gurwell, M. A., Bergin, E. A., Melnick, G. J., et al 2000, ApJ, 539, L143
Hartogh, P., et al 2004, J. Geophys. Res. 109, D18303, 2004
Hartogh, P., Lellouch, E., Crovisier, J., et al 2009, Planetary and Space Science, 57, 1596
Hartogh, P., et al 2010, J. Geophys. Res., 115, D00I17
Irwin, P. G. J. 2009, RADTRANS, Oxford Planetary Group Document NIMS/OX/PGJI/SW/136
Krasnopolsky, V. A. 2007, Icarus, 190, 93
Lefevre, F., et al 2004, J. Geophys. Res., 109, E07004
Lellouch, E., Paubert, G., Encrenaz, T., et al 1991, Planet. Space Sci., 39, 219
Lellouch, E., et al 2008, http://www.lesia.obspm.fr/perso/ emmanuel-lellouch/mars/
Lewis, S. R., et al 1999, J. Geophys. Res., 104, Issue E10, 24177
Medvedev, A. S., & Hartogh, P. 2007, Icarus, 186, 97
Moreno, R. 1998, These de Doctorat, Universite` de Paris VI
Moreno, R., 2010, Neptune and Uranus brightness temperatures, available from ESA Herschel Science Centre
Parkinson, T. D., & Hunten, M. D. 1972, J. Atmos. Sci., 29, 1380
Spinrad, H., Mu¨nch, G., Kaplan, L. D., et al 1963, ApJ, 137, 1319
Sprague, A. L., et al 1996, J. Geophys. Res. 101 (E10), 23229
Smith, M. D. 2002, J. Geophys. Res. 107
Smith, S. D., et al 2009, J. Geophys. Res., 114
Swinyard, B. M., et al 2010, A&A, 518, L4
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