Showing posts with label Saturn. Show all posts
Showing posts with label Saturn. Show all posts
Monday, January 21, 2013
APOTD: Saturn's Glowing Aurora
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Image: NASA/JPL/University of Arizona/University of Leicester[high-resolution] |
Caption: Cassini Solstice team
This false-color composite image, constructed from data obtained by NASA's Cassini spacecraft, shows the glow of auroras streaking out about 1,000 km (600 miles) from the cloud tops of Saturn's south polar region. It is among the first images released from a study that identifies images showing auroral emissions out of the entire catalogue of images taken by Cassini's visual and infrared mapping spectrometer.
In this image constructed from data collected in the near-infrared wavelengths of light, the auroral emission is shown in green. The data represents emissions from hydrogen ions in of light between 3 and 4 microns in wavelength. In general, scientists designated blue to indicate sunlight reflected at a wavelength of 2 microns, green to indicate sunlight reflected at 3 microns and red to indicate thermal emission at 5 microns. Saturn's rings reflect sunlight at 2 microns, but not at 3 and 5 microns, so they appear deep blue. Saturn's high altitude haze reflects sunlight at both 2 and 3 microns, but not at 5 microns, and so it appears green to blue-green. The heat emission from the interior of Saturn is only seen at 5 microns wavelength in the spectrometer data, and thus appears red. The dark spots and banded features in the image are clouds and small storms that outline the deeper weather systems and circulation patterns of the planet. They are illuminated from underneath by Saturn's thermal emission, and thus appear in silhouette.
The composite image was made from 65 individual observations by Cassini's visual and infrared mapping spectrometer on 1 November 2008. The observations were each six minutes long.
Monday, January 14, 2013
APOTD: Tectonics on Enceladus
On Oct. 5, 2008, just after coming within 25 kilometers (15.6 miles)
of the surface of Enceladus, NASA's Cassini captured this stunning
mosaic as the spacecraft sped away from this geologically active moon of
Saturn.
Craters and cratered terrains are rare in this view of the southern
region of the moon's Saturn-facing hemisphere. Instead, the surface is
replete with fractures, folds, and ridges—all hallmarks of remarkable
tectonic activity for a relatively small world. In this enhanced-color
view, regions that appear blue-green are thought to be coated with
larger grains than those that appear white or gray.
Portions of the tiger stripe fractures, or sulci, are visible along the
terminator at lower right, surrounded by a circumpolar belt of
mountains. The icy moon's famed jets emanate from at least eight
distinct source regions, which lie on or near the tiger stripes.
However, in this view, the most prominent feature is Labtayt Sulci, the
approximately one-kilometer (0.6 miles) deep northward-trending chasm
located just above the center of the mosaic.
Near the top, the conspicuous ridges are Ebony and Cufa Dorsae. This
false-color mosaic was created from 28 images obtained at seven
footprints, or pointing positions, by Cassini's narrow-angle camera. At
each footprint, four images using filters sensitive to ultraviolet,
visible and infrared light (spanning wavelengths from 338 to 930
nanometers) were combined to create the individual frames. The mosaic is
an orthographic projection centered at 64.49 degrees south latitude,
283.87 west longitude, and it has an image scale of 196 kilometers
(122.5 miles) per pixel. The original images ranged in resolution from
180 meters (594 feet) to 288 meters (950 feet) per pixel and were
acquired at distances ranging from 30,000 to 48,000 kilometers (18,750
to 30,000 miles) as the spacecraft receded from Enceladus. The view was
acquired at a Sun-Enceladus-spacecraft, or phase, angle of 73 degrees.
Image: NASA/JPL/Space Science Institute [high-resolution]
Caption: NASA
Sunday, December 16, 2012
Nile-like River of Liquid Hydrocarbons On The Surface On Titan
Text and image VIA: JPL Website
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Image credit: NASA/JPL–Caltech/ASI |
Scientists deduce that the river, which is in Titan's north polar region, is filled with liquid hydrocarbons because it appears dark along its entire length in the high-resolution radar image, indicating a smooth surface.
"Though there are some short, local meanders, the relative straightness of the river valley suggests it follows the trace of at least one fault, similar to other large rivers running into the southern margin of this same Titan sea," said Jani Radebaugh, a Cassini radar team associate at Brigham Young University, Provo, Utah. "Such faults – fractures in Titan's bedrock -- may not imply plate tectonics, like on Earth, but still lead to the opening of basins and perhaps to the formation of the giant seas themselves."
Titan is the only other world we know of that has stable liquid on its surface. While Earth's hydrologic cycle relies on water, Titan's equivalent cycle involves hydrocarbons such as ethane and methane. In Titan's equatorial regions, images from Cassini's visible-light cameras in late 2010 revealed regions that darkened due to recent rainfall. Cassini's visual and infrared mapping spectrometer confirmed liquid ethane at a lake in Titan's southern hemisphere known as Ontario Lacus in 2008.
"Titan is the only place we've found besides Earth that has a liquid in continuous movement on its surface," said Steve Wall, the radar deputy team lead, based at NASA's Jet Propulsion Laboratory, Pasadena, Calif. "This picture gives us a snapshot of a world in motion. Rain falls, and rivers move that rain to lakes and seas, where evaporation starts the cycle all over again. On Earth, the liquid is water; on Titan, it's methane; but on both it affects most everything that happens."
The radar image here was taken on Sept. 26, 2012. It shows Titan's north polar region, where the river valley flows into the sea called Ligeia Mare. The real Nile River stretches about 4,100 miles (6,700 kilometers). The processes that led to the formation of Earth's Nile are complex, but involve faulting in some regions.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and ASI, the Italian Space Agency. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington. The Cassini orbiter was designed, developed and assembled at JPL. The radar instrument was built by JPL and the Italian Space Agency, working with team members from the US and several European countries. JPL is a division of the California Institute of Technology in Pasadena."
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