Constraints on Titan's middle atmosphere ammonia abundance from Herschel/SPIRE sub-millimetre spectra

被引:31
|
作者
Teanby, N. A. [1 ]
Irwin, P. G. J. [2 ]
Nixon, C. A. [3 ]
Courtin, R. [4 ]
Swinyard, B. M. [5 ,6 ]
Moreno, R. [4 ]
Lellouch, E. [4 ]
Rengel, M. [7 ]
Hartogh, P. [7 ]
机构
[1] Univ Bristol, Sch Earth Sci, Bristol BS8 1RJ, Avon, England
[2] Univ Oxford, Dept Phys, Clarendon Lab, Oxford OX1 3PU, England
[3] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[4] Univ Paris Diderot, Univ Paris 06, CNRS, LESIA,Observ Paris, F-92195 Meudon, France
[5] Rutherford Appleton Lab, Sci & Technol Facil Council, RAL Space, Didcot OX11 0QX, Oxon, England
[6] UCL, Dept Phys & Astron, London WC1E 6BT, England
[7] Max Planck Inst Sonnensyst Forsch, D-37191 Katlenburg Lindau, Germany
基金
英国科学技术设施理事会;
关键词
Titan; Atmosphere; Composition; Photochemistry; Herschel; Sub-millimetre; ROTOTRANSLATIONAL ABSORPTION-SPECTRA; RADIATIVE-TRANSFER; STRATOSPHERE; TEMPERATURES; PAIRS; PHOTOCHEMISTRY; HYDROCARBONS; CHEMISTRY; PROFILES; AEROSOLS;
D O I
10.1016/j.pss.2012.11.008
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Sub-millimetre spectra measured with Herschel's SPIRE Fourier Transform Spectrometer were used to search for ammonia (NH3) in Titan's stratosphere. Observations were taken during 2010 and 2011, just after Titan's northern spring equinox, which occurred in mid-2009. In our analysis we used high spectral resolution data (0.074 cm(-1) apodised) from the SPIRE shortwave spectrometer array (SSW), which provided the best possible signal-to-noise ratio for detecting any NH3 emission features. These data have the most sensitivity to NH3 spectral emission of any currently available observations, although despite this we did not detect any significant emission features above the noise. However, we can place an improved 3-sigma upper limit on NH3 abundance of <0.19 ppb for altitudes 65-110 km (75 km peak sensitivity), or alternatively a column abundance of <1.23 x 10(15) molecules/cm(2). These observations provide modest constraint for future photochemical models and are consistent with most current stratospheric predictions. Scaling of photochemical model profiles, in order to fit elevated abundances observed at 1100 km by Cassini's INMS instrument, are for the most part also consistent with our observations. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:136 / 147
页数:12
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