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IUE observations of H Lyman-[alpha] in comet P/Giacobini-Zinner

dc.contributor.authorCombi, Michael R.en_US
dc.contributor.authorFeldman, Paul D.en_US
dc.date.accessioned2006-04-10T15:11:31Z
dc.date.available2006-04-10T15:11:31Z
dc.date.issued1992-06en_US
dc.identifier.citationCombi, Michael R., Feldman, Paul D. (1992/06)."IUE observations of H Lyman-[alpha] in comet P/Giacobini-Zinner." Icarus 97(2): 260-268. <http://hdl.handle.net/2027.42/30005>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6WGF-4731CW2-JS/2/c21c0a29329c614d269d4b8f7dc2255aen_US
dc.identifier.urihttps://hdl.handle.net/2027.42/30005
dc.description.abstractComet P/Giacobini-Zinner (1985 XIII) was observed during the flyby of the International Cometary Explorer (ICE) satellite and during the 3 preceding months by the International Ultraviolet Explorer (IUE) satellite. Models for the hydrogen abundance and spatial distribution, which were previously used to reproduce the observed spatial distribution of the wide-field Lyman-[alpha] comae of Comets Kohoutek and Halley measured by rocket and spacecraft borne instruments, have now been successfully applied to these IUE observations. Vectorial models, which implicitly assume production of cometary OH by dissociation of water molecules, have been routinely used to infer global water production rates from various nucleus-centered IUE observations of comets. However, because of modeling complexities, a large base of Lyman-[alpha] observations has not generally been analyzed. One of these modeling complexities is that often the H atom column densities are high enough so that the coma is optically thick to solar Lyman-[alpha] radiation which cannot be treated by the standard optically thin models (Haser, vectorial, or Monte Carlo). A spherical radiative transfer model, adapted for application to the H coma, has been used to analyze the IUE observations. This analysis yields water production rates in very good agreement with those calculated from vectorial model analysis of OH observations. The H model makes essentially the same physical assumptions as the vectorial model for OH except for optical density. A further interesting aspect of this dataset is that various offset observations of the Lyman-[alpha] brightness were made on August 12, and September 10 and 11, 1985, at sampling distances of 7,500 to 41,000 km. This is much higher spatial resolution that is typically available from the usual rocketborne cameras which have made most of the wide-field measurements of the H distribution in comets. The same H model, in combination with the radiative transfer calculation, also reproduces the observed spatial distribution of H in the inner coma.en_US
dc.format.extent909883 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleIUE observations of H Lyman-[alpha] in comet P/Giacobini-Zinneren_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelAstronomyen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumSpace Physics Research Laboratory, Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, USAen_US
dc.contributor.affiliationotherDepartment of Physics and Astronomy, The Johns Hopkins University, Baltimore, Maryland 21218, USAen_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/30005/1/0000373.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0019-1035(92)90132-Qen_US
dc.identifier.sourceIcarusen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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