Nightglow in the Upper Atmosphere of Mars and Implications for Atmospheric Transport
dc.contributor.author | Bertaux, J.-L. | |
dc.contributor.author | Leblanc, F. | |
dc.contributor.author | Perrier, S. | |
dc.contributor.author | Quemerais, E. | |
dc.contributor.author | Korablev, O. | |
dc.contributor.author | Dimarellis, E. | |
dc.contributor.author | Reberac, A. | |
dc.contributor.author | Forget, F. | |
dc.contributor.author | Simon, P.C. | |
dc.contributor.author | Stern, S.A. | |
dc.contributor.author | Sandel, B. | |
dc.contributor.author | the SPICAM team | |
dc.date | 2005 | |
dc.date.accessioned | 2016-12-07T10:36:06Z | |
dc.date.available | 2016-12-07T10:36:06Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/4641 | |
dc.description | We detected light emissions in the nightside martian atmosphere with the SPICAM (spectroscopy for the investigation of the characteristics of the atmosphere of Mars) ultraviolet (UV) spectrometer on board the Mars Express. The UV spectrum of this nightglow is composed of hydrogen Lyman α emission (121.6 nanometers) and the γ and δ bands of nitric oxide (NO) (190 to 270 nanometers) produced when N and O atoms combine to produce the NO molecule. N and O atoms are produced by extreme UV photodissociation of O 2, CO2, and N2 in the dayside upper atmosphere and transported to the night side. The NO emission is brightest in the winter south polar night because of continuous downward transport of air in this region at night during winter and because of freezing at ground level. | |
dc.language | eng | |
dc.title | Nightglow in the Upper Atmosphere of Mars and Implications for Atmospheric Transport | |
dc.type | Article | |
dc.subject.frascati | Physical sciences | |
dc.audience | Scientific | |
dc.subject.free | Martian surface analysis | |
dc.subject.free | Nitric acid | |
dc.subject.free | Photodissociation | |
dc.subject.free | Spectroscopic analysis | |
dc.subject.free | Ultraviolet spectrometers | |
dc.subject.free | Upper atmosphere | |
dc.subject.free | Martian atmosphere | |
dc.subject.free | Nightglow | |
dc.subject.free | UV spectrum | |
dc.subject.free | Light emission | |
dc.subject.free | nitric oxide | |
dc.subject.free | Mars | |
dc.subject.free | article | |
dc.subject.free | astronomy | |
dc.subject.free | atmospheric transport | |
dc.subject.free | dissociation | |
dc.subject.free | freezing | |
dc.subject.free | light | |
dc.subject.free | priority journal | |
dc.subject.free | spectroscopy | |
dc.subject.free | ultraviolet radiation | |
dc.subject.free | winter | |
dc.subject.free | Atmosphere | |
dc.subject.free | Carbon Dioxide | |
dc.subject.free | Extraterrestrial Environment | |
dc.subject.free | Hydrogen | |
dc.subject.free | Mars | |
dc.subject.free | Nitric Oxide | |
dc.subject.free | Nitrogen | |
dc.subject.free | Oxygen | |
dc.subject.free | Seasons | |
dc.subject.free | Spacecraft | |
dc.subject.free | Spectrophotometry, Ultraviolet | |
dc.subject.free | Temperature | |
dc.subject.free | Ultraviolet Rays | |
dc.source.title | Science | |
dc.source.volume | 307 | |
dc.source.issue | 5709 | |
dc.source.page | 566-569 | |
Orfeo.peerreviewed | Yes | |
dc.identifier.doi | 10.1126/science.1106957 | |
dc.identifier.scopus | 2-s2.0-19944432374 |