From diffraction-limited images produced by the near-IR camera NICMOS aboar
d the Hubble Space Telescope we derived maps of Titan's surface in the meth
ane windows near 1.1, 1.6, and 2.0 mu m. Each part of Titan's atmosphere an
d surface was imaged at least twice over a time period of 24 h to look for
moving clouds. Despite careful analysis we found no evidence for cloud acti
vity. On the contrary, we were able to reproduce most of the features ident
ified by previous mapping efforts, indicating that the albedo landscape rem
ained stable over several years and is most likely indigenous to the surfac
e. At the 3 sigma level we confirmed two brightness peaks in the prominent,
continent-sized bright feature on the leading side of Titan. Many smaller
landmarks could be mapped, including distinct surface structures on the dar
k, trailing side of Titan. These rule out the presence of a single large et
hane ocean on the "backside" of Titan. No obvious differences could be seen
between the maps at different wavelengths, other than a gradual loss of sp
atial resolution due to the diffraction limit of the 2.4-m primary mirror.
(C) 2000 Academic Press.