GLOBAL COLOR AND ALBEDO VARIATIONS ON TRITON

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

Global multispectral mosaics of Triton have been produced from Voyager approach images; six spectral units are defined and mapped. The margin of the south polar cap (SPC) is scalloped and ranges in latitude from + 10° to −30°. A bright fringe is closely associated with the cap's margin; from it, diffuse bright rays extend north‐northeast for hundreds of kilometers. Thus, the rays may consist of fringe materials that were redistributed by northward‐going Coriolis‐deflected winds. From 1977 to 1989, Triton's foil‐disk spectrum changed from markedly red and uv‐dark to nearly neutral white and uv‐bright. This spectral change can be explained by new deposition of nitrogen frost over both the northern hemisphere and parts of a formerly redder SPC. Frost deposition in the southern hemisphere during southern summer is possible over relatively high albedo areas of the cap (Stansbeny et al, 1990), which helps to explain the apparent stability of the unexpectedly large SPC and the presence of the bright fringe.

Original languageEnglish (US)
Pages (from-to)1765-1768
Number of pages4
JournalGeophysical Research Letters
Volume17
Issue number10
DOIs
StatePublished - 1990
Externally publishedYes

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polar caps
albedo
frost
color
caps
margins
rays
Southern Hemisphere
Northern Hemisphere
summer
nitrogen
mosaic
material

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

GLOBAL COLOR AND ALBEDO VARIATIONS ON TRITON. / McEwen, Alfred S.

In: Geophysical Research Letters, Vol. 17, No. 10, 1990, p. 1765-1768.

Research output: Contribution to journalArticle

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