Dissipation of Titan's south polar clouds

Nearly all adaptive optics images of Titan taken between December 2001 and November 2004 showed tropospheric clouds located within 30° of the south pole. We report here on a dissipation of Titan's south polar clouds observed in twenty-nine Keck and Gemini images taken between December 2004 and...

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Published in:Icarus
Main Authors: Schaller, Emily L., Brown, Michael E., Roe, Henry G., Bouchez, Antonin H., Trujillo, Chadwick A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2006
Subjects:
Online Access:https://doi.org/10.1016/j.icarus.2006.05.025
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spelling ftcaltechauth:oai:authors.library.caltech.edu:rt6es-xcf54 2024-10-13T14:10:51+00:00 Dissipation of Titan's south polar clouds Schaller, Emily L. Brown, Michael E. Roe, Henry G. Bouchez, Antonin H. Trujillo, Chadwick A. 2006-10 https://doi.org/10.1016/j.icarus.2006.05.025 unknown Elsevier https://doi.org/10.1016/j.icarus.2006.05.025 eprintid:34390 info:eu-repo/semantics/closedAccess Other Icarus, 184(2), 517-523, (2006-10) Titan Infrared observations Atmospheres dynamics Meteorology info:eu-repo/semantics/article 2006 ftcaltechauth https://doi.org/10.1016/j.icarus.2006.05.025 2024-09-25T18:46:45Z Nearly all adaptive optics images of Titan taken between December 2001 and November 2004 showed tropospheric clouds located within 30° of the south pole. We report here on a dissipation of Titan's south polar clouds observed in twenty-nine Keck and Gemini images taken between December 2004 and April 2005. The near complete lack of south polar cloud activity during this time, and subsequent resurgence months later at generally higher latitudes, may be the beginning of seasonal change in Titan's weather. The ∼5 month decrease in cloud activity may also have been caused by methane rainout from a large cloud event in October 2004. Understanding the seasonal evolution of Titan's clouds, and of any precipitation associated with them, is essential for interpreting the geological observations of fluid flow features observed over a wide range of Titan latitudes with the Cassini/Huygens spacecraft. © 2006 Elsevier Inc. Received 22 January 2006; revised 12 May 2006. Available online 18 July 2006. We thank Robert West and an anonymous reviewer for helpful comments. E.L.S. is supported by an NASA Graduate Student Research Fellowship. H.G.R. is supported by an NSF Astronomy and Astrophysics Postdoctoral Fellowship under Award AST-0401559. Additional support was provided by an NSF Grant to M.E.B. (AST-0307929). The W.M. Keck Observatory is operated as a scientific partnership among the California Institute of Technology, the University of California, and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W.M. Keck Foundation. The Gemini Observatory is operated by the Association of Universities for Research in Astronomy, under a cooperative agreement with the NSF on behalf of the Gemini partnership: the NSF, the Particle Physics and Astronomy Research Council (UK), the National Research Council (Canada), Comision Nacional de Investigacion Cientfficay Tecnologica (CONICYT) (Chile), the Autralian Research Council (Australia), Conselho Nacional de ... Article in Journal/Newspaper South pole Caltech Authors (California Institute of Technology) Canada South Pole Gemini ENVELOPE(-62.500,-62.500,-66.133,-66.133) Titan ENVELOPE(33.629,33.629,67.560,67.560) Icarus 184 2 517 523
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic Titan
Infrared observations
Atmospheres
dynamics
Meteorology
spellingShingle Titan
Infrared observations
Atmospheres
dynamics
Meteorology
Schaller, Emily L.
Brown, Michael E.
Roe, Henry G.
Bouchez, Antonin H.
Trujillo, Chadwick A.
Dissipation of Titan's south polar clouds
topic_facet Titan
Infrared observations
Atmospheres
dynamics
Meteorology
description Nearly all adaptive optics images of Titan taken between December 2001 and November 2004 showed tropospheric clouds located within 30° of the south pole. We report here on a dissipation of Titan's south polar clouds observed in twenty-nine Keck and Gemini images taken between December 2004 and April 2005. The near complete lack of south polar cloud activity during this time, and subsequent resurgence months later at generally higher latitudes, may be the beginning of seasonal change in Titan's weather. The ∼5 month decrease in cloud activity may also have been caused by methane rainout from a large cloud event in October 2004. Understanding the seasonal evolution of Titan's clouds, and of any precipitation associated with them, is essential for interpreting the geological observations of fluid flow features observed over a wide range of Titan latitudes with the Cassini/Huygens spacecraft. © 2006 Elsevier Inc. Received 22 January 2006; revised 12 May 2006. Available online 18 July 2006. We thank Robert West and an anonymous reviewer for helpful comments. E.L.S. is supported by an NASA Graduate Student Research Fellowship. H.G.R. is supported by an NSF Astronomy and Astrophysics Postdoctoral Fellowship under Award AST-0401559. Additional support was provided by an NSF Grant to M.E.B. (AST-0307929). The W.M. Keck Observatory is operated as a scientific partnership among the California Institute of Technology, the University of California, and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W.M. Keck Foundation. The Gemini Observatory is operated by the Association of Universities for Research in Astronomy, under a cooperative agreement with the NSF on behalf of the Gemini partnership: the NSF, the Particle Physics and Astronomy Research Council (UK), the National Research Council (Canada), Comision Nacional de Investigacion Cientfficay Tecnologica (CONICYT) (Chile), the Autralian Research Council (Australia), Conselho Nacional de ...
format Article in Journal/Newspaper
author Schaller, Emily L.
Brown, Michael E.
Roe, Henry G.
Bouchez, Antonin H.
Trujillo, Chadwick A.
author_facet Schaller, Emily L.
Brown, Michael E.
Roe, Henry G.
Bouchez, Antonin H.
Trujillo, Chadwick A.
author_sort Schaller, Emily L.
title Dissipation of Titan's south polar clouds
title_short Dissipation of Titan's south polar clouds
title_full Dissipation of Titan's south polar clouds
title_fullStr Dissipation of Titan's south polar clouds
title_full_unstemmed Dissipation of Titan's south polar clouds
title_sort dissipation of titan's south polar clouds
publisher Elsevier
publishDate 2006
url https://doi.org/10.1016/j.icarus.2006.05.025
long_lat ENVELOPE(-62.500,-62.500,-66.133,-66.133)
ENVELOPE(33.629,33.629,67.560,67.560)
geographic Canada
South Pole
Gemini
Titan
geographic_facet Canada
South Pole
Gemini
Titan
genre South pole
genre_facet South pole
op_source Icarus, 184(2), 517-523, (2006-10)
op_relation https://doi.org/10.1016/j.icarus.2006.05.025
eprintid:34390
op_rights info:eu-repo/semantics/closedAccess
Other
op_doi https://doi.org/10.1016/j.icarus.2006.05.025
container_title Icarus
container_volume 184
container_issue 2
container_start_page 517
op_container_end_page 523
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