Stellar Occultation Investigations of Pluto's Atmosphere
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Stellar Occultation Investigations of Pluto's Atmosphere by Colette Salyk Submitted to the Department of Earth, Atmospheric and Planetary Sciences in Partial Fulfillment of the Requirements for the Degree of Bachelor of Science at the Massachusetts Institute of Technology June 2003 2003 Colette Salyk All rights reserved The author hereby grants to MIT permission to reproduce and to distribute publicly paper and electronic copies of this thesis document in whole or in part. Signature of Author Signature redacted Department of Earth, Atmospheric and Planetary Sciences May 9, 2003 Certified by Signature rec acted Professor Jim L. Elliot U Professor of Earth, Atmospheric and Planetary Sciences Professor of Physics Thesis Supervisor Accepted by Signature rE d acted Professor Brian Evans Chairman. 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This is the most complete copy available. 21 2 Stellar Occultation Investigations of Pluto's Atmosphere by Colette Salyk Submitted to the department of Earth, Atmospheric and Planetary Sciences in Partial Fulfillment of the Requirements for the Degree of Bachelor of Science in Earth, Atmospheric and Planetary Sciences ABSTRACT We investigate the shape of Pluto's atmosphere using data from the occultation of the V=15.7 star P131.1 by Pluto on 2002 Aug 21 (UT). We find that Pluto's atmosphere, as projected onto the sky, is noticeably non-circular. This implies an overall ellipsoidal shape, which could be an indication of high winds and/or latitudinal stratification. We decide to compare our results to those obtained from datasets of the occultation of P8 by Pluto on 1988 June 9 (UT). Previous analyses of these datasets by Millis et al. (1993) had led to the conclusion that Pluto's atmospheric shape did not deviate from that of a sphere. However, we find that the 1988 datasets do not conclusively demonstrate that this is the case. We conclude that Pluto's atmosphere is currently non-spherical and could have been non- spherical at the time of the 1988 occultation. Implications for high winds and/or latitudinal stratification present exciting possibilities to be investigated by the upcoming New Horizons mission to Pluto. Thesis Supervisor: James L. Elliot Professor of Earth, Atmospheric and Planetary Sciences Professor of Physics 3 1. Introduction The planet Pluto, discovered in the year 1930, is the furthest solar system planet from our sun. With an apparent magnitude of -15 at the time of discovery, it was difficult to observe with available techniques, and remained, for many years, an object of interest and speculation. As early as 1994, Kuiper (1944) used stability considerations to propose that Pluto may have an atmosphere. Other speculations about the possible presence of or characteristics of an atmosphere on Pluto arose in the early 1970's. A pair of papers proposed and discussed an atmosphere composed primarily of Ne, with an additional brief mention of the possibility of an N 2 atmosphere (Hart, 1974, Golitsyn, 1975). The first observational results about Pluto came in 1976, when methane frost was detected by spectroscopy (Cruikshank 1976). Stem, Trafton and Gladstone (1987) used this information, as well as observations that Pluto's albedo changed with both time and location, to argue that Pluto should have an atmosphere. This result was to be confirmed in 1988. In 1988, an observed stellar occultation by Pluto confirmed the presence of an atmosphere. Stellar occultations are one of the most important observational techniques for studying distant planets, because they return extremely high spatial resolution information about a body's atmosphere or rings. Occultations occur when a planet passes in front of a star as viewed from Earth. If we measure the received starlight as the star is occulted and an atmosphere surrounds the body, we observe a reduction in starlight because the atmosphere refracts the starlight away from our line of sight. Because the star is essentially a point source, the spatial resolution of the observations are limited only by Fresnel diffraction, which translates to a resolution of just a few kilometers at Pluto. Observers of the 1988 occultation by Pluto saw a reduction in starlight due to refraction and concluded that Pluto did, indeed, possess a thin atmosphere, which they believed to be composed of CH4, but 4 mentioned that it was also consistent with a primarily N 2 atmosphere (Elliot et al. 1989). In addition, they noted that Pluto's atmosphere had a roughly isothermal upper layer as well as a lower layer that either acted as an extinction layer, or had a radically different scale height from the upper atmosphere. The shape of Pluto's atmosphere was also investigated and determined to be circular (Millis et al. 1993). Succeeding the exciting discovery of Pluto's atmosphere, Yelle and Lunine (1989) determined, theoretically, that a predominantly CH4 atmosphere was not consistent with the occultation results. Owen et al. (1993) soon after detected N2 , CH4 , and CO on Pluto's surface, and reasoned that due to N2 being both the most abundant and most volatile of the three molecules, N 2 should be the most abundant atmospheric constituent. After these significant studies, our knowledge of Pluto's atmosphere did not have a chance to expand until the occurrence of the next stellar occultation. Because the probability of a stellar occultation occurrence depends directly on the area of sky subtended by the occulting body, stellar occultations by Pluto are rare. The next occultation by Pluto occurred in summer 2002. On July 27 2002, Pluto occulted the R=12.3 star P126A. Unfortunately, due to difficulties in predicting the occultation's location, only a couple of mobile telescopes were able to collect data (Buie et al. 2002). Luckily, another occultation occurred shortly afterwards on the 2 111 of August. This occultation was observed at six different observatories and on ten telescopes. Four telescopes were located on Mauna Kea; observers at these telescopes were focused on providing an explanation for the lower atmospheric layer observed in 1988 and noting any differences from the observed features of the 1988 occultation (Elliot et al. 2003). The other five locations were used to provide a large spatial baseline across the globe, and therefore, across Pluto's disk as seen from Earth. This baseline 5 is essential for correctly determining the location of the star's path along Pluto's disk. It also provides a means for investigating the shape of Pluto's atmosphere. The shape of a planet's atmosphere can be determined by observing an occultation from several different locations on Earth. The shape, in turn, gives us information about the atmospheric structure, from which one may infer wind speeds, if the oblateness is not likely to be caused by the rotation of the planet. Stellar occultation measurements of Saturn's moon Titan resulted in the surprising finding of a significantly ellipsoidal atmosphere (ellipticity - 0.016), implying very high winds and a possibly latitudinally-stratified wind structure (Hubbard et al. 1993). Stellar occultation measurements of Neptune's moon Triton in the 90's showed that its atmosphere was even more ellipsoidal (ellipticity ~ 0.040) than Titan's (Elliot et al. 2000). Looking back at the Pluto occultation of 1998, we find that, although similar analyses were performed by Millis et al. (1993), the possibility of an ellipsoidal atmosphere was not mentioned. We investigate here the shape of Pluto's atmosphere by using 2002 occultation data as well as by re-examining the data points from the 1998 occultation. 2. Observations The occultation of the V = 15.7 star P13 1.1 by Pluto occurred on 2002 Aug 8 at approximately 6:59 (UT) (Elliot et al. 2003). The total event duration, from immersion to emersion, was about five minutes. The details of all observations, including locations, telescopes, event times and instrumentation specifics can be found in Table 1. For our purposes, we note that observers on Mauna Kea observed in several different wavelength bands and with generally high S/N ratios. Other, smaller telescopes, despite necessarily 6 lower signal collecting abilities, were utilized at several different locations to maximize the spatial coverage of the event. The data interpreted in our analysis include datasets from Haleakala Observatory on Maui, Lick and Palomar Observatories in California and Lowell Observatory in Arizona, along with one high S/N dataset from Mauna Kea, obtained on the University of Hawaii's 2.2m telescope. Each dataset consisted of a series of CCD frames that captured images of both P13 1.1 and Pluto. In general, each dataset spanned a time period beginning at least several minutes before the starlight's immersion into Pluto's atmosphere, and ending several minutes afterwards. A notable exception is the dataset taken at Haleakala. Because of instrument- setup problems, observers were only able to capture the emersion portion of the event. Image integration times and cycle times (the time required for the reading out of the CCD chip) varied from location to location; the time resolution, therefore, ranged from 0.0001 seconds to 2.4 seconds. (These details can also be found in Table 1). 3.