Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-08T09:25:51.964Z Has data issue: false hasContentIssue false

An Unusual Meteor Spectrum

Published online by Cambridge University Press:  12 April 2016

A. F. Cook
Affiliation:
Smithsonian Astrophysical Observatory and Harvard College ObservatoryCambridge, Massachusetts
C. L. Hemenway
Affiliation:
State University of New York at Albany and Dudley ObservatoryAlbany, New York
P. M. Millman
Affiliation:
National Research Council of CanadaOttawa, Ontario
A. Swider
Affiliation:
State University of New York at Albany and Dudley ObservatoryAlbany, New York

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

An extraordinary spectrum of a meteor at a velocity of about 18.5±1.0 km s-1 (approximate uncertainty) was observed from the Springhill Meteor Observatory with an image-orthicon camera at 1970 August 10 d2h 48m 518 UT. The radiant of the meteor was at an altitude of about 49°. It was first seen shoioing a yellow-red continuous spectrum alone at a height of 137±8 km (estimated uncertainty) which we ascribe to the first positive group of nitrogen bands. At 1.608 after its initial appearance the meteor had descended to 116±6 km above sea-level when it brightened rapidly from its previous threshold brighness into a uniform continuum. After a further 0.738 at a height of 106±6 km the D-line of neutral sodium appeared and 0.148 later (height 105±5 km) all the other lines of the spectrum also appeared. The continuum remained dominant to the end 0.408 later (height 87±5 km) or 3.878 after initial appearance.

Water of hydration and entrained carbon flakes of characteristic dimension about 0.2 micron or less are proposed as constituents of the meteoroid to explain these phenomena.

Type
Research Article
Copyright
Copyright © NASA 1971

References

Anon, ., 1962. U.S. Standard Atmosphere, 1962, U.S. Committee on Extension of the Standard Atmosphere, Supt. of Documents, Washington.Google Scholar
Ceplecha, Z., 1968. Discrete levels of meteor beginning height, Smithson. Astrophys. Obs., Spec. Rept. No. 279.Google Scholar
Cook, A. F., 1968. The physical theory of meteors, Physics and Dynamics of Meteors, ed. by Kresák, L. and Millman, P. M., D. Reidel Publ. Co., Dordrecht, Holland, 149160.Google Scholar
Hemenway, C. L., Swider, A., and Bowman, C., 1971. Meteor spectroscopy using an image orthicon, Can. J. Phys., 49, 13611364.Google Scholar
Jacchia, L. G., and Whipple, F. L., 1961. Precision orbits of 413 photographic meteors, Smithson. Contrib. Astrophys., 4, 97129.Google Scholar
Millman, P. M., Cook, A. F., and Hemenway, C. L., 1971. Spectroscopy of Perseid meteors with an image orthicon, Can. J. Phys., 49, 13651373.Google Scholar
Moore, C. E., 1945. A multiplet table of astrophysical interest, Contrib. Princeton Univ. Obs. No. 20.Google Scholar
Olivier, C. P., 1925. Meteors, Williams and Wilkins, Baltimore, 173.Google Scholar
Öpik, E. J., 1958. Physics of Meteor Flight in the Atmosphere, Interscience, New York.Google Scholar
Schönfeld, E. and Krüger, A., 1899. Atlas des nördlichen gesternten Himmels, 2nd. ed., edited and corrected by Küstner, F., Marcus, and Weber, , Bonn, .Google Scholar