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TOPIC: Titan


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RE: Titan
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This image of Titan was taken by the Cassni spaceprobe on November 19, 2007, when the moon was approximately 131,739 kilometres away.

tita_e6
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Credit: NASA/JPL/Space Science Institute

The image was taken using the CB3 and CL2 filters.

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Titan T37
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TITAN 052TI (T37) MISSION DESCRIPTION
Forty-eight days after Cassinis Titan-36 flyby, the spacecraft returns to Titan for its thirty-eighth targeted encounter. The closest approach to Titan occurs on Monday, Nov. 19, at 2007-323T00:47:25 spacecraft time at an altitude of 1000 kilometres above the surface and at a speed of 6.3 kilometres per second. The latitude at closest approach is 22 degrees S and the encounter occurs on orbit number 52.
This encounter is set up with two manoeuvres: an apoapsis manoeuvre on Nov. 1, and a Titan approach manoeuvre, scheduled for Nov. 15. T37 is the second in a series of outbound encounters that will last until the end of the prime mission, and it occurs less than two days after Saturn closest approach. This is the second in a series of seven Titan southern hemisphere encounters.

TITAN_e4
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The dark, equatorial region known as Shangri-la is visible here. Cassini radar images show that Shangri-la and other dark regions around the moon's middle are filled with vast stretches of parallel dunes. These regions appear to be lowland areas surrounded by brighter, higher terrain.

titan9774e2
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Credit: NASA/JPL/Space Science Institute/University of Colorado

Lit terrain seen here is on the anti-Saturn side of Titan. North is up and rotated 21 degrees to the right.
The image was taken with the Cassini spacecraft narrow-angle camera on Oct. 19, 2007 using a combination of spectral filters sensitive to wavelengths of polarized infrared light centred at 746 and 938 nanometers.
The view was acquired at a distance of approximately 1.4 million kilometres from Titan and at a Sun-Titan-spacecraft, or phase, angle of 80 degrees. Image scale is 8 kilometres per pixel.

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Title: Titan's rotation: A 3-dimensional theory
Authors: B. Noyelles, A. Lemaitre, A. Vienne

We study the forced rotation of Titan seen as a rigid body at the equilibrium Cassini state, involving the spin-orbit synchronization. We use both the analytical and the numerical way. We analytically determine the equilibrium positions and the frequencies of the 3 free librations around it, while a numerical integration associated to a frequency analysis give us a more synthetic complete theory, where the free solution is split from the forced one. We find a mean obliquity of 2.2 arcmin, and the fundamental frequencies of the free librations of about 2.0977, 167.4883 and 306.3360 years. Moreover, we enlighten the main role played by Titan's inclination on its rotation, and we suspect a likely resonance involving Titan's wobble.

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This image of Titan was taken by the Cassini spaceprobe on October 22, 2007, when it was approximately 516,699 kilometres away.

titange1
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Credit: NASA/JPL/Space Science Institute/University of Colorado

The image was taken using the CL1 and CB3 filters.

-- Edited by Blobrana at 21:37, 2007-10-24

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This image of Titan was acquired from less than a degree above Saturn's ringplane by the Cassini spaceprobe on Aug. 1, 2007, at a distance of approximately 2.4 million kilometers.

titan_age3
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Credit: NASA/JPL/Space Science Institute

Images taken using red, green and blue spectral filters were combined to create this natural colour view.

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"Titan is indeed the land of lakes and seas. It will be interesting to see the differences between the north and south polar regions" -  Rosaly Lopes, Cassini radar scientist at NASA's Jet Propulsion Laboratory.

 It is now summer at Titan's south pole. A season on Titan lasts nearly 7.5 years, one quarter of a Saturn year, which is 29.5 years long. Monitoring seasonal changes in the lakes will help scientists understand the processes at work there.

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VLT and Keck near-infrared images of Titan's surface and lower troposphere can be subtracted to reveal widespread cirrus-like clouds of frozen methane (lower images) and a large patch of liquid methane (dark area within box) interpreted as clouds and morning drizzle above the huge continent of Xanadu (outline).

tita_oct3
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[Normal - JPEG: 980 x 800 pix - 516k]
[Full Res - JPEG: 2028 x 1655 pix - 1.4M]
[Full Res - TIFF: 2028 x 1655 pix - 10M]

Credit ESO

At left is a chart of Titan's aerosol haze versus altitude, indicating higher density haze over portions of the south pole and the heights of frozen and liquid methane clouds. Credit: Máté Ádámkovics/UC Berkeley.



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Cassini's radar instrument finds lakes in the southern hemisphere of Titan during the most recent Titan flyby. This is the first confirmation of lakes in the southern hemisphere with the radar instrument. Hundreds of lakes have already been discovered and imaged by radar at Titan's north pole. This finding is important to scientists who are trying to understand how Titan's environment works.
Cassini completed its 37th flyby of Saturn's moon Titan on Oct. 2, 2007, allowing the Cassini Titan Radar Mapper to obtain this southernmost image to date.

PIA10018.jpg
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Credit:    NASA/JPL/USGS

Shown here is a portion of the image swath and an inset with details of a small portion in false colour. Titan's south pole is at the bottom centre. The nature and similarities between the northern and southern near-polar regions supports the idea that much of Titan's poles are climate-driven.
A few small dark patches - liquid-hydrocarbon-filled lakes - stand out, at about 70 degrees south, and are highlighted in the insert (lakes are coloured blue). Other features in the scene include broad, steep-sided depressions adjoined to sinuous depressions, interpreted to be empty topographic basins or drained lakes fed by channels, and complex mottled terrain, akin to those at similar northern latitudes. Similarities in features between northern and southern hemispheres imply that the climatic conditions are also similar.
The image shown here is a 1.4-kilometer  resolution, 2,250-kilometer  subsection of a 4,500-kilometer  long swath, which is 150 kilometres  wide at the narrowest point. The insert is 90 by 90 kilometres, centred at 70.5 degrees south and 113.9 degrees west. Future southern flybys will image closer to the pole and are expected to show more lakes.


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Click on the image for movie of
Titan's North Polar Region
Credit: NASA/JPL/USGS



This Cassini false-colour mosaic shows all synthetic-aperture radar images to date of Titan's north polar region. Approximately 60 percent of Titan's north polar region, above 60 degrees north latitude, is now mapped with radar. About 14 percent of the mapped region is covered by what is interpreted as liquid hydrocarbon lakes.
Features thought to be liquid are shown in blue and black, and the areas likely to be solid surface are tinted brown. The terrain in the upper left of this mosaic is imaged at lower resolution than the remainder of the image.
Most of the many lakes and seas seen so far are contained in this image, including the largest known body of liquid on Titan. These seas are most likely filled with liquid ethane, methane and dissolved nitrogen.

-- Edited by Blobrana at 02:54, 2007-10-13

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