Icarus 148, 347–369 (2000) doi:10.1006/icar.2000.6508, available online at http://www.idealibrary.com on The Prediction and Observation of the 1997 July 18 Stellar Occultation by Triton: More Evidence for Distortion and Increasing Pressure in Triton’s Atmosphere J. L. Elliot,1,2 M. J. Person, and S. W. McDonald Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, Massachusetts 02139-4307 E-mail:
[email protected] M. W. Buie, E. W. Dunham, R. L. Millis, R. A. Nye, C. B. Olkin, and L. H. Wasserman Lowell Observatory, 1400 West Mars Hill Road, Flagstaff, Arizona 86001-4499 L. A. Young3 Center for Space Physics, Boston University, Boston, Massachusetts 02215 W. B. Hubbard and R. Hill Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721 H. J. Reitsema Ball Aerospace, P.O. Box 1062, Boulder, Colorado 80306-1062 J. M. Pasachoff and T. H. McConnochie4 Astronomy Department, Williams College, Williamstown, Massachusetts 01267-2565 B. A. Babcock Physics Department, Williams College, Williamstown, Massachusetts 01267-2565 R. C. Stone U.S. Naval Observatory, Flagstaff Station, P.O. Box 1149, Flagstaff, Arizona 86002-1149 and P. Francis Mt. Stromlo Observatory, Private Bag, Weston Creek Post Office, Weston, ACT 2611, Australia Received December 21, 1999; revised June 20, 2000 1 Also at Lowell Observatory, 1400 West Mars Hill Road, Flagstaff, AZ 86001-4499. 2 A variety of CCD astrometric data was used to predict the lo- Also at Department of Physics, MIT, and guest observer, Cerro Tololo Inter- cation of the path for the occultation of the star we have denoted American Observatory, National Optical Astronomy Observatories, operated by “Tr176” by Triton, which occurred on 1997 July 18, and was visible the Association of Universities for Research in Astronomy, Inc., under cooper- ative agreement with the National Science Foundation.