A&A 430, L37-L40 (2005)
DOI: 10.1051/0004-6361:200400127
Letter
A dual origin for Neptune's carbon monoxide?
E. Lellouch1, R. Moreno1 and G. Paubert 21 Laboratoire d'Études Spatiales et d'Instrumentation en Astrophysique (LESIA), Observatoire de Paris, 92195 Meudon, France
e-mail: emmanuel.lellouch@obspm.fr
2 Institut de Radio-Astronomie Millimétrique, 18080 Granada, Spain
(Received 5 November 2004 / Accepted 14 December 2004)
Abstract
Heterodyne observations of Neptune have provided a measurement
of the CO(2-1) line profile with a total bandpass of almost
8 GHz and a resolution of 4 MHz. The lineshape indicates that the CO mole
fraction in Neptune's atmosphere is not uniform, but increases by a factor of
~2 from the troposphere/lower stratosphere (0.5 ppm at
p>20 mbar)
to the upper stratosphere (1 ppm at
p<20 mbar). This indicates the existence
of both external and internal sources of CO. The equivalent flux associated
with the external source is ~
cm
-2 s
-1. We
propose that the stratospheric CO results from a large (2 km) cometary
impact that occurred ~200 years ago, although there remains problems
with this hypothesis.
Key words: planets and satellites: Neptune -- radio-lines: solar system
© ESO 2005
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