Wednesday, February 9, 2022

Belet Is Equatorial Dark Albedo Feature on Titan's Anti-Saturn Side


Summary: Belet is an equatorial dark albedo feature on Titan's anti-Saturn side that is recognized as the largest of Titan's three largest sand seas.


Topographic maps show Belet's dark dunes, with heights of 100 to 150 meters (300 to 500 feet), and lighter, elevated, dune-less areas; maps in equirectangular projection, with north at top, created from images obtained during Cassini spacecraft's T8 flyby of Oct. 28, 2005, and T21 flyby of Dec. 12, 2006; black-and-white image (above) is color-coded (below) for elevations; map region, which covers about 450 kilometers (280 miles), is centered near 9 degrees south latitude, 290 degrees west longitude; image addition date 2009-03-24; image credit NASA/JPL-Caltech/ASI/USGS: May be used for any purpose without prior permission, via NASA JPL Photojournal

Belet is an equatorial dark albedo feature on Titan's anti-Saturn side that numbers as the largest of the Saturnian moon's three largest sand seas.
Belet is centered at minus 5 degrees south latitude, 255 degrees west longitude, according to the International Astronomical Union’s (IAU) Gazetteer of Planetary Nomenclature. The Gazetteer places the low albedo feature's northernmost and southernmost latitudes at its center latitude of minus 5 degrees south and its easternmost and westernmost longitudes as its center longitude of 255 degrees west longitude.
Belet lies to the west of Adiri, the anti-Saturn side's bright equatorial albedo feature. Adiri is centered at minus 10 degrees south latitude, 210 degrees west longitude. Adiri's center coordinates are given as the high albedo feature's northernmost-southernmost latitudes and easternmost-westernmost longitudes.
Belet lies to the east of the Saturn-facing side's far western dark albedo features, Aaru and Senkyo. Northern equatorial-centered Aaru is positioned above southern equatorial-centered Senkyo in Titan's equatorial belt.
Aaru is centered at 10 degrees north latitude, 340 degrees west longitude. Its northernmost-southernmost latitudes and easternmost-westernmost longitudes coincide with its center coordinates.
Senkyo is centered at minus 5 degrees south latitude, 320 degrees west longitude. Its center latitude and longitude are identified as the low albedo feature's northernmost-southernmost latitudes and easternmost-westernmost longitudes, respectively.
Belet heads Shangri-La and Fensal as the largest of Titan's three largest sand seas, according to planetary geophysicist Antoine Lucas and seven co-authors in their study, "Texture and Composition of Titan's Equatorial Sand Seas Inferred From Cassini SAR Data," published in the October 2019 issue of Journal of Geophysical Research JGR: Planets. Dark albedo feature Shangri-La has center coordinates of minus 10 degrees south latitude, 165 degrees west longitude. the anti-Saturn side resident's center latitude and longitude are recorded as its northernmost-southernmost latitudes and easternmost-westernmost longitudes, respectively. Dark albedo feature Fensal is centered at 5 degrees north latitude, 30 degrees west longitude. The Saturn-facing side occupant's center coordinates are given as its northernmost-southernmost latitudes and easternmost-westernmost longitudes.
Belet's extensive sand sea sprawls across Titan's trailing hemisphere. Titan's largest dune field stretches latitudinally from 25 degrees north to minus 30 degrees south and longitudinally from 65 degrees west to 150 degrees west, according to planetary geologist Bradley Bishop and three co-authors in "Dune Width and Spacing in Titan's Belet Sand Sea in Relation to Topography Highlights Potential Sediment Transport Patterns," their presentation at the 47th Lunar and Planetary Science Conference, held March 21-25, 2016, at The Woodlands Waterway Marriott Hotel and Convention Center in The Woodlands, Texas.
Altitude and latitude influence the sizes and patterns of dunes, according to NASA Jet Propulsion Laboratory's (JPL) Photojournal post, "Dune Patterns," published Jan. 23, 2012. Images of dark albedo features Belet and Fensal obtained by the Cassini spacecraft's radar instrument on Oct. 28, 2005, and April 10, 2007, reveal the wide dunes, with thicker blanketed interdunes, associated with Belet's low altitude and longitude. Thin, widely separated dunes with thinly covered interdunes characterize Fensal's higher elevation and latitude. In a comparison with Earth's deserts, Belet's dunes resemble the abundant sediment available in the Oman dunes of Oman, Saudi Arabia, United Arab Emirates and Yemen. Known as Rub' al Khali (Arabic: "Empty Quarter"), the Oman dunes occur as a southern extension of the Arabian Peninsula's vast Arabian Desert. Contrastingly, Fensal's dunes are reminiscent of the limited sediment found in the Kalahari (Tswana: Kgala, "the great thirst,",or Kgalagadi, "a waterless place") sand dunes of Botswana, Namibia and South Africa in Southern Africa.
The International Astronomical Union approved Belet's name in 2006. The Gazetteer of Planetary Nomenclature traces the dark equatorial albedo feature's name to the "Malay afterworld reached by a flower-lined bridge." The IAU convention for Titan's albedo features draws names of "Sacred or enchanted places, paradise, or celestial realms from legends, myths, stories, and poems of cultures from around the world," according to the Gazetteer's page on “Categories (Themes) for Naming Features on Planets and Satellites."

image of dark albedo feature Belet acquired Jan. 15, 2010, by Cassini spacecraft's Narrow-Angle Camera (NAC), with 938 nanometer near-infrared light wavelength-centered spectral filter; trailing hemisphere image obtained at an approximately distance of 1.2 million kilometers (746,000 miles) from Titan and at Sun-Titan-spacecraft, or phase, angle of 51 degrees; image addition date 2010-04-20; image credit NASA/JPL/Space Science Institute: May be used for any purpose without prior permission, via NASA JPL Photojournal

Acknowledgment
My special thanks to talented artists and photographers/concerned organizations who make their fine images available on the internet.

Image credits:
Topographic maps show Belet's dark dunes, with heights of 100 to 150 meters (300 to 500 feet), and lighter, elevated, dune-less areas; maps in equirectangular projection, with north at top, created from images obtained during Cassini spacecraft's T8 flyby of Oct. 28, 2005, and T21 flyby of Dec. 12, 2006; black-and-white image (above) is color-coded (below) for elevations; map region, which covers about 450 kilometers (280 miles), is centered near 9 degrees south latitude, 290 degrees west longitude; image addition date 2009-03-24; image credit NASA/JPL-Caltech/ASI/USGS: May be used for any purpose without prior permission, via NASA JPL Photojournal @ https://photojournal.jpl.nasa.gov/catalog/PIA11829
image of dark albedo feature Belet acquired Jan. 15, 2010, by Cassini spacecraft's Narrow-Angle Camera (NAC), with 938 nanometer near-infrared light wavelength-centered spectral filter; trailing hemisphere image obtained at an approximately distance of 1.2 million kilometers (746,000 miles) from Titan and at Sun-Titan-spacecraft, or phase, angle of 51 degrees; image addition date 2010-04-20; image credit NASA/JPL/Space Science Institute: May be used for any purpose without prior permission, via NASA JPL Photojournal @ https://photojournal.jpl.nasa.gov/catalog/PIA12615

For further information:
Bishop, B. (Bradley); R.C. Lewis; J. (Jani) Radebaugh; and E.H. Christiansen. "Dune Width and spacing in Titan's Belet Sand Sea in Relation to Topography Highlights Potential Sediment Transport Patterns." 47th Lunar and Planetary Science Conference, March 21-25, 2016, The Woodlands Waterway Marriott Hotel and Convention Center in The Woodlands, Texas.
Available @ https://www.hou.usra.edu/meetings/lpsc2016/pdf/2663.pdf
Brossier, J. F. (Jeremy Florian): S. (Sébastien) Rodriguez; T. Cornet; A. Lucas; J. Radebaugh; L. (Luca) Maltagliati; S. (Stéphane) Le Mouélic; A. (Anezina) Solomonidou; A. (Athena) Coustenis; M. (Mathieu) Hirtzig; R. (Ralf) Jaumann; K. Stephan; and C. Sotin. "Geological Evolution of Titan's Equatorial Regions: Possible Nature and Origin of the Dune Material." Journal of Geophysical Research JGR Planets, vol. 123, issue 5 (May 2018): 1089-1112.
Available via Wiley Online @ https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2017JE005399
Available via Wiley Online @ https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2017JE005399
Brossier, Jeremy. "What Is Happening in Titan's Equatorial Belt?" Planetary Geomorphology Image of the Month, June 1, 2018.
Available @ https://planetarygeomorphology.wordpress.com/2018/06/01/what-is-happening-in-titans-equatorial-belt/
Daley, Jason. "First Global Map of Saturn’s Moon Titan Reveals Secrets of Earth’s ‘Deranged’ Twin." Smithsonian Magazine > SmartNews. Nov. 20, 2019.
Available @ https://www.smithsonianmag.com/smart-news/first-map-earths-deranged-twin-and-saturns-moon-titan-completed-180973607/
Florian Brossier, Jeremy; Sébastien Rodriguez; Luca Maltagliati; Stéphane Le Mouélic; Anezina Solomonidou; Athena Coustenis; Mathieu Hirtzig; Ralf Jaumann; and Robert H. Brown. "Equatorial Belt of Titan: Aaru Region as Seen by VIMS/Cassini." American Astronomical Society, 48th Division for Planetary Sciences (DPS) / 11th European Planetary Science Congress (EPSC) International Conference, Oct. 10-16, 2016, Pasadena, California.
Available via DLR (Deutsches Zentrum für Luft- und Raumfahrt) elib @ https://elib.dlr.de/105102/
Available via Harvard ADSABS (NASA Astrophysics Data System Abstracts) @ https://ui.adsabs.harvard.edu/abs/2016DPS....4841206F/abstract
Greicius, Tony, page ed. "Dune Patterns." NASA > Missions > Cassini-Huygens > Multimedia. Last updated Jan. 23, 2012.
Available @ https://www.nasa.gov/mission_pages/cassini/multimedia/pia15225.html
Huber, Lyle, cur. "Cassini RADAR Titan SAR Images." NASA PDS: The Planetary Atmosphere Node > Data and Services > Atmospheres Data.
Available @ https://atmos.nmsu.edu/data_and_services/atmospheres_data/Cassini/inst-radar-sar.html
International Astronomical Union (IAU) / U.S. Geological Survey (USGS) Gazetteer of Planetary Nomenclature. “Categories (Themes) for Naming Features on Planets and Satellites.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature > Documentation > Surface Feature Categories.
Available @ https://planetarynames.wr.usgs.gov/Page/Categories
International Astronomical Union (IAU) / U.S. Geological Survey (USGS) Gazetteer of Planetary Nomenclature. “Coordinate Systems for Planets and Satellites.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature > Documentation > Target Coordinate Systems.
Available @ https://planetarynames.wr.usgs.gov/TargetCoordinates
International Astronomical Union (IAU) / U.S. Geological Survey (USGS) Gazetteer of Planetary Nomenclature. “Descriptor Terms (Feature Types).” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature > Documentation > Descriptor Terms.
Available @ https://planetarynames.wr.usgs.gov/DescriptorTerms
International Astronomical Union (IAU) / U.S. Geological Survey (USGS) Gazetteer of Planetary Nomenclature. “Target: Saturn.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature > Nomenclature > Saturn.
Available @ https://planetarynames.wr.usgs.gov/Page/TITAN/target
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Aaru.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated Oct. 1, 2006.
Available @ https://planetarynames.wr.usgs.gov/Feature/6981
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Adiri.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated Oct. 1, 2006.
Available @ https://planetarynames.wr.usgs.gov/Feature/6982
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Belet.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated Oct. 1, 2006.
Available @ https://planetarynames.wr.usgs.gov/Feature/6984
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Fensal.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated Oct. 1, 2006.
Available @ https://planetarynames.wr.usgs.gov/Feature/7011
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Senkyo.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated Oct. 1, 2006.
Available @ https://planetarynames.wr.usgs.gov/Feature/6989
International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). “Shangri-La.” USGS Astrogeology Science Center > Gazetteer of Planetary Nomenclature. Last updated April 20, 2009.
Available @ https://planetarynames.wr.usgs.gov/Feature/6990
Jet Propulsion Laboratory. "PIA03068: Titan Radar Swath (T-8 Flyby, Oct. 28, 2005)." NASA JPL Photojournal. Image addition date 2005-10-28.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA03068
Jet Propulsion Laboratory. "PIA07732: Monitoring 'Fensal-Aztlan.'" NASA JPL Photojournal. Image addition date 2005-09-13.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA07732
Jet Propulsion Laboratory. "PIA11829: Titan's 'Sand Sea' Belet." NASA JPL Photojournal. Image addition date 2009-03-24.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA11829
Jet Propulsion Laboratory. "PIA12615: Behold Belet." NASA JPL Photojournal. Image addition date 2010-04-20.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA12615
Jet Propulsion Laboratory. "PIA12647: Belet Close-Up." NASA JPL Photojournal. Image addition date 2010-06-03.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA12647
Jet Propulsion Laboratory. "PIA12671: A Look at Belet." NASA JPL Photojournal. Image addition date 2010-07-07.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA12671
Jet Propulsion Laboratory. "PIA12818: Titanic Deluge." NASA JPL Photojournal. Image addition date 2011-03-17.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA12818
Jet Propulsion Laboratory. "PIA15225: Dune Patterns." NASA JPL Photojournal. Image addition date 2012-01-23.
Available @ https://photojournal.jpl.nasa.gov/catalog/PIA15225
Le Gall, A. (Alice); M.A. Janssen; L.C. Wye; A.G. (Alexander Gerard) Hayes; J. (Jani) Radebaugh; C. Savage; H. Zebker; R.D. Lorenz; J.I. Lunine; R.L. Kirk; R.M.C. Lopes; S. Wall; P. Callahan; E.R. Stofan; T. Farr; and Cassini Radar Team. "Cassini SAR, Radiometry, Scatterometry and Altimetry Observations of Titan’s Dune Fields." Icarus, vol. 213, issue 2 (June 2011): 608-624.
Available via ScienceDirect @ https://www.sciencedirect.com/science/article/abs/pii/S0019103511001175?via%3Dihub
Lorenz, R.D.; S. Wall; J. (Jani) Radebaugh; G. Boubin; E. Reffet; M. Janssen; E. Stofan; R. Lopes; R. Kirk; C. Elachi; J. Lunine; K. Mitchell; F. Paganelli; L. Soderblom; C. Wood; L. Wye; H. Zebker; Y. Anderson; S. Ostro; M. Allison; R. Boehmer; P. Callahan; P. Encrenaz; G.G. Ori; G. Francescetti; Y. Gim; G. Hamilton; S. Hensley; W. Johnson; K. Kelleher; D. Muhleman; G. Picardi; F. Posa; L. Roth; R. Seu; S. Shaffer; B. Stiles; S. Vetrella; E. Flamini; and R. West. "The Sand Seas of Titan: Cassini RADAR Observations of Longitudinal Dunes." Science, vol. 312 (May 5, 2006): 724-727. DOI:10.1126/science.1123257.
Available via NASA GISS (Goddard Institute for Space Studies) @ https://pubs.giss.nasa.gov/docs/2006/2006_Lorenz_lo05000n.pdf
Lucas, Antoine; Sébastien Rodriguez; Florentin Lemonnier; A. (Alice) Le Gall; Shannon McKenzie; C. Ferrari; Philippe Paillou; and Clement Narteau. "Texture and Composition of Titan's Equatorial Sand Seas Inferred From Cassini SAR Data: Implications for Aeolian Transport and Dune Morphodynamics." The Journal of Geophysical Research JGR: Planets (October 2019).
Available via ResearchGate GmbH @ https://www.researchgate.net/publication/313519792_Texture_and_composition_of_Titan%27s_equatorial_sand_seas_inferred_from_Cassini_SAR_data_Implications_for_aeolian_transport_and_dune_morphodynamics
Marriner, Derdriu. "Aaru Is Equatorial Dark Albedo Feature on Titan's Saturn-Facing Side." Earth and Space News. Wednesday, Jan. 19, 2022.
Available @ https://earth-and-space-news.blogspot.com/2022/01/aaru-is-equatorial-dark-albedo-feature.html
Marriner, Derdriu. "Adiri Is Equatorial Bright Albedo Feature on Titan's Anti-Saturn Side." Earth and Space News. Wednesday, Jan. 26, 2022.
Available @ https://earth-and-space-news.blogspot.com/2022/01/adiri-is-equatorial-bright-albedo.html
Marriner, Derdriu. "Aztlan Is Equatorial Dark Albedo Feature on Titan's Saturn-Facing Side." Earth and Space News. Wednesday, Feb. 2, 2022.
Available @ https://earth-and-space-news.blogspot.com/2022/02/aztlan-is-equatorial-dark-albedo.html
Marriner, Derdriu. "Christiaan Huygens Discovered Saturnian Satellite Titan March 25, 1655." Earth and Space News. Wednesday, March 21, 2012.
Available @ https://earth-and-space-news.blogspot.com/2012/03/christiaan-huygens-discovered-saturnian.html
Marriner, Derdriu. "Titan Has Eight Low Albedo Features That Darken Its Surface." Earth and Space News. Wednesday, Jan. 12, 2022.
Available @ https://earth-and-space-news.blogspot.com/2022/01/titan-has-eight-low-albedo-features.html
Marriner, Derdriu. "Titan Has Five High Albedo Features That Brighten Its Surface." Earth and Space News. Wednesday, Jan. 5, 2022.
Available @ https://earth-and-space-news.blogspot.com/2022/01/titan-has-five-high-albedo-features.html
Marriner, Derdriu. "Visible and Infrared Mapping Spectrometer VIMS Shows Titanean Surface." Earth and Space News. Wednesday, March 29, 2012.
Available @ https://earth-and-space-news.blogspot.com/2012/03/visible-and-infrared-mapping.html
Radebaugh, J. (Jani): R.D. Lorenz; J.I. Lunine; S.D. Wall; G. Boubin; E. Reffet; R.L. Kirk; R.M. Lopes; E.R. Stofan; L. Soderblom; M. Allison; M. Janssen; P. Paillou; P. Callahan; C. Spencer; and the Cassini Radar Team. "Dunes on Titan Observed by Cassini Radar." Icarus, vol. 194 (April 2008): 690–703.
Available via ScienceDirect @ https://www.sciencedirect.com/science/article/abs/pii/S001910350700512X
Available @ https://d1wqtxts1xzle7.cloudfront.net/44246392/Dunes_on_Titan_observed_by_Cassini_Radar20160330-7000-2bsp9z-with-cover-page-v2.pdf?Expires=1629834589&Signature=eUT0V8Bkps0T60GbJJVaUUFJVnKGYqYAJxHAqcaoIJA3uKF4RRJr7vM1oqRECb0rw~hrHcYPLuiGa--fxmqX1NFvobbJDhvrgDCGlWcekZd-do~zPgPE1gtKXsVZt4cMJwkGKQHAIe5KN9YBOg0A-UszU~cR3SYx~MbrPzHB3uKu1CVYsXCLadmvtuJi80PZX0rlIdh7RI0USrx4WUxIwelq07FGgVPJ5zCmcRBgYkBnzOl0EXbzTYWZaDO7mHwJK4CTFqo8M3-tgHjFNn6Trpygwzvs4SNDbnXh2MUffGGxsH4Zpo8J~4agJr06qrQrLIOKbi2dLiyH91Ui5HgfRw__&Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA
Schoenfeld, Ashley M.; Rosaly M.C. Lopes; Michael J. Malaska; Anezina Solomonidou; David A. Williams; Samuel P.D. Birch; Alexander G. (Gerard) Hayes; Paul Corlies; Alice Le Gall; Michael A.Janssen; Stéphane Le Mouélic; Elizabeth Turtle; Meghan Florence; and Tiffany Verlander. "Geomorphological Map of the South Belet Region of Titan."Icarus, vol. 366 (Sep. 15, 2021): 114516.
Available via ScienceDirect @ https://www.sciencedirect.com/science/article/pii/S0019103521001913
Stiles, Bryan. Cassini Radar Basic Image Data Records SIS Version 1.4. D-27889. Pasadena CA: NASA Jet Propulsion Laboratory, California Institute of Technology, Sep. 27, 2005.
Available @ https://pds-imaging.jpl.nasa.gov/data/cassini/cassini_orbiter/CORADR_0051/DOCUMENT/BIDRSIS.HTML
Watanabe, Susan, page ed. "Monitoring 'Fensal-Aztlan.'" NASA > Missions > Current Missions > Cassini-Huygens > Multimedia. Sep. 13, 2005.
Available @ https://www.nasa.gov/mission_pages/cassini/multimedia/pia07732.html


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