Publication Abstracts

Lunine et al. 2008

Lunine, J.I., C. Elachi, S.D. Wall, M.A. Janssen, M.D. Allison, Y. Anderson, R. Boehmer, P. Callahan, P. Encrenaz, E. Flamini, G. Franceschetti, Y. Gim, G. Hamilton, S. Hensley, W.T.K. Johnson, K. Kelleher, R.L. Kirk, R.M. Lopes, R. Lorenz, D.O. Muhleman, R. Orosei, S.J. Ostro, F. Paganelli, P. Paillou, G. Picardi, F. Posa, J. Radebaugh, L.E. Roth, R. Seu, S. Shaffer, L.A. Soderblom, B. Stiles, E.R. Stofan, S. Vetrella, R. West, C.A. Wood, L. Wye, H. Zebker, G. Alberti, E. Karkoschka, B. Rizk, E. McFarlane, C. See, and B. Kazeminejad, 2008: Titan's diverse landscapes as evidenced by Cassini RADAR's third and fourth looks at Titan. Icarus, 195, 415-433, doi:10.1016/j.icarus.2007.12.022.

Cassini's third and fourth radar flybys, T7 and T8, covered diverse terrains in the high southern and equatorial latitudes, respectively. The T7 synthetic aperture radar (SAR) swath is somewhat more straightforward to understand in terms of a progressive poleward descent from a high, dissected, and partly hilly terrain down to a low flat plain with embayments and deposits suggestive of the past or even current presence of hydrocarbon liquids. The T8 swath is dominated by dunes likely made of organic solids, but also contain somewhat enigmatic, probably tectonic, features that may be partly buried or degraded by erosion or relaxation in a thin crust. The dark areas in T7 show no dune morphology, unlike the dark areas in T8, but are radiometrically warm like the dunes. The Huygens landing site lies on the edge of the T8 swath; correlation of the radar and Huygens DISR images allows accurate determination of its coordinates, and indicates that to the north of the landing site sit two large longitudinal dunes. Indeed, had the Huygens probe trajectory been just 10 km north of where it actually was, images of large sand dunes would have been returned in place of the fluvially dissected terrain actually seen — illustrating the strong diversity of Titan's landscapes even at local scales.

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BibTeX Citation

@article{lu06000k,
  author={Lunine, J. I. and Elachi, C. and Wall, S. D. and Janssen, M. A. and Allison, M. D. and Anderson, Y. and Boehmer, R. and Callahan, P. and Encrenaz, P. and Flamini, E. and Franceschetti, G. and Gim, Y. and Hamilton, G. and Hensley, S. and Johnson, W. T. K. and Kelleher, K. and Kirk, R. L. and Lopes, R. M. and Lorenz, R. and Muhleman, D. O. and Orosei, R. and Ostro, S. J. and Paganelli, F. and Paillou, P. and Picardi, G. and Posa, F. and Radebaugh, J. and Roth, L. E. and Seu, R. and Shaffer, S. and Soderblom, L. A. and Stiles, B. and Stofan, E. R. and Vetrella, S. and West, R. and Wood, C. A. and Wye, L. and Zebker, H. and Alberti, G. and Karkoschka, E. and Rizk, B. and McFarlane, E. and See, C. and Kazeminejad, B.},
  title={Titan's diverse landscapes as evidenced by Cassini RADAR's third and fourth looks at Titan},
  year={2008},
  journal={Icarus},
  volume={195},
  pages={415--433},
  doi={10.1016/j.icarus.2007.12.022},
}

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RIS Citation

TY  - JOUR
ID  - lu06000k
AU  - Lunine, J. I.
AU  - Elachi, C.
AU  - Wall, S. D.
AU  - Janssen, M. A.
AU  - Allison, M. D.
AU  - Anderson, Y.
AU  - Boehmer, R.
AU  - Callahan, P.
AU  - Encrenaz, P.
AU  - Flamini, E.
AU  - Franceschetti, G.
AU  - Gim, Y.
AU  - Hamilton, G.
AU  - Hensley, S.
AU  - Johnson, W. T. K.
AU  - Kelleher, K.
AU  - Kirk, R. L.
AU  - Lopes, R. M.
AU  - Lorenz, R.
AU  - Muhleman, D. O.
AU  - Orosei, R.
AU  - Ostro, S. J.
AU  - Paganelli, F.
AU  - Paillou, P.
AU  - Picardi, G.
AU  - Posa, F.
AU  - Radebaugh, J.
AU  - Roth, L. E.
AU  - Seu, R.
AU  - Shaffer, S.
AU  - Soderblom, L. A.
AU  - Stiles, B.
AU  - Stofan, E. R.
AU  - Vetrella, S.
AU  - West, R.
AU  - Wood, C. A.
AU  - Wye, L.
AU  - Zebker, H.
AU  - Alberti, G.
AU  - Karkoschka, E.
AU  - Rizk, B.
AU  - McFarlane, E.
AU  - See, C.
AU  - Kazeminejad, B.
PY  - 2008
TI  - Titan's diverse landscapes as evidenced by Cassini RADAR's third and fourth looks at Titan
JA  - Icarus
VL  - 195
SP  - 415
EP  - 433
DO  - 10.1016/j.icarus.2007.12.022
ER  -

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