Pluto's atmosphere from the May 22, 2011 stellar occultation

Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012.

Dades bibliogràfiques
Autor principal: Sallum, Stephanie E
Altres autors: Richard P. Binzel.
Format: Thesis
Idioma:eng
Publicat: Massachusetts Institute of Technology 2018
Matèries:
Accés en línia:http://hdl.handle.net/1721.1/114349
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author Sallum, Stephanie E
author2 Richard P. Binzel.
author_facet Richard P. Binzel.
Sallum, Stephanie E
author_sort Sallum, Stephanie E
collection MIT
description Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012.
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spelling mit-1721.1/1143492019-04-10T14:45:00Z Pluto's atmosphere from the May 22, 2011 stellar occultation Sallum, Stephanie E Richard P. Binzel. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012. Cataloged from PDF version of thesis. Includes bibliographical references (pages 40-41). This paper reports the observations and atmospheric fitting results from the May 22, 2011 stellar occultation by Pluto. Of the nine sites across the United States that attempted to observe the event, three obtained light curves at the predicted midtime without being clouded out. Simultaneous fitting of these three light curves utilizing a model fully detailed in Elliot and Young [1992] resulted in a best fit half-light radius of 1309 ± 25 km, a calculated temperature of 94 ± 4 K, and a calculated pressure scale height of 55 ± 2 km. These parameters, in the context of the previous occultations, reveal a trend in which Pluto's half-light radius has been increasing slightly since an initial dramatic increase between 1988 and 2002. While the pressure scale height has remained relatively constant, the temperature has decreased slightly over the recorded events. The changes in half-light radius agree with frost migration models in which Pluto's surface has a low thermal inertia [Hansen and Paige, 1996; Elliot et al., 2007], but further constraints on frost migration model parameters such as substrate and frost albedo, frost emissivity, and the supply of N2 require additional observations. The New Horizons spacecraft should encounter a dynamic atmosphere on Pluto during the scheduled fly by in 2015. by Stephanie E. Sallum. S.B. 2018-03-27T14:18:38Z 2018-03-27T14:18:38Z 2012 2012 Thesis http://hdl.handle.net/1721.1/114349 1028750393 eng MIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission. http://dspace.mit.edu/handle/1721.1/7582 vi, 44 pages application/pdf zpl---- Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences.
Sallum, Stephanie E
Pluto's atmosphere from the May 22, 2011 stellar occultation
title Pluto's atmosphere from the May 22, 2011 stellar occultation
title_full Pluto's atmosphere from the May 22, 2011 stellar occultation
title_fullStr Pluto's atmosphere from the May 22, 2011 stellar occultation
title_full_unstemmed Pluto's atmosphere from the May 22, 2011 stellar occultation
title_short Pluto's atmosphere from the May 22, 2011 stellar occultation
title_sort pluto s atmosphere from the may 22 2011 stellar occultation
topic Earth, Atmospheric, and Planetary Sciences.
url http://hdl.handle.net/1721.1/114349
work_keys_str_mv AT sallumstephaniee plutosatmospherefromthemay222011stellaroccultation