Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/5662
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dc.contributor.authorJenniskens, P-
dc.contributor.authorTedesco, Ed-
dc.contributor.authorMurthy, J-
dc.contributor.authorLaux, C. O-
dc.contributor.authorPrice, S-
dc.date.accessioned2012-01-18T14:13:55Z-
dc.date.available2012-01-18T14:13:55Z-
dc.date.issued2002-08-
dc.identifier.citationMeteoritics & Planetary Science, Vol. 37, No. 8, pp. 1071-1078en
dc.identifier.urihttp://hdl.handle.net/2248/5662-
dc.description.abstractWe used the ultraviolet to visible spectrometers onboard the midcourse space experiment to obtain the first ultraviolet spectral measurements of a bright meteor during the 1997 Leonid shower. The meteor was most likely a Leonid with a brightness of about -2 magnitude at 100 km altitude. In the region between 251 and 310 nm, the two strongest emission lines are from neutral and ionized magnesium. Ionized Ca lines, indicative of a hot T ?10 000 K plasma, are not detected. The Mg and Mg + line intensity ratio alone does not yield the ionization temperature, which can be determined only by assuming the electron density. A typical air plasma temperature of T = 4400 K would imply a very high electron density: ne = 2.2 x 10-18 m-3 , but at chondritic abundances of Fe/Mg and Si/Mg ~ 1. For a more reasonable local-thermodynamic-equilibrium (LTE) air plasma electron density, the Mg and Mg + line ratio implies a less than chondritic Fe/Mg = 0.06 abundance ratio and a cool non-LTE T = 2830 K ionization temperature for the ablation vapor plasma. The present observations do not permit a choice between these alternatives. The new data provide also the first spectral confirmation of the presence of molecular OH and NO emission in meteor spectra.en
dc.language.isoenen
dc.publisherWileyen
dc.relation.urihttp://adsabs.harvard.edu/abs/2002M%26PS...37.1071Jen
dc.titleSpaceborne ultraviolet 251-384 nm spectroscopy of a meteor during the 1997 Leonid showeren
dc.typeArticleen
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