Issue |
A&A
Volume 430, Number 2, February I 2005
|
|
---|---|---|
Page(s) | L37 - L40 | |
Section | Letters | |
DOI | https://doi.org/10.1051/0004-6361:200400127 | |
Published online | 20 January 2005 |
Letter to the Editor
A dual origin for Neptune's carbon monoxide?
1
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
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 mbar)
to the upper stratosphere (1 ppm at
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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