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#5578 From: hexagram14@...
Date: Tue Apr 10, 2012 9:52 pm
Subject: Cassini Enceladus Flyby - April 14, 2012
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Cassini Enceladus Flyby - April 14, 2012

Enceladus 'E-18' Flyby -- Destination: Plumes

The Fields, Particles and Waves instruments are prime (particularly the
ion and neutral mass spectrometer [INMS]) to study the composition,
density, three-dimensional structure and variability of plumes; with
E-14, and E-17, this flyby provides good coverage of south polar
regions.

Enceladus Flyby at a Glance

Date
April 14, 2012 (SCET)

Altitude
46 miles (74 kilometers)

Speed
17,000 mph
(7.5 km/sec)
 
 
HR

#5579 From: hexagram14@...
Date: Thu Apr 12, 2012 5:22 pm
Subject: Image: Shadow of Mimas On Saturn's Clouds
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Image: Shadow of Mimas On Saturn's Clouds




The shadow of the moon Mimas creates a smudge on the southern hemisphere of Saturn in this view from the Cassini spacecraft.



Mimas does not appear here, but it does cast its shadow on the planet in the lower left of the image. The shadows cast by the rings dominate the upper right of the image. This view looks toward the southern, unilluminated side of the rings from about 1 degree below the ringplane.



The image was taken with the Cassini spacecraft narrow-angle camera on Jan. 21, 2012 using a spectral filter sensitive to wavelengths of near-infrared light centered at 750 nanometers. The view was acquired at a distance of approximately 1.6 million miles (2.6 million kilometers) from Saturn and at a Sun-Saturn-spacecraft, or phase, angle of 70 degrees. Image scale is 9 miles (15 kilometers) per pixel.



The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate in Washington. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging team is based at the Space Science Institute, Boulder, Colo.



For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov or http://www.nasa.gov/cassini . The Cassini imaging team homepage is at http://ciclops.org .



Credit: NASA/JPL-Caltech/Space Science Institute. Full-Res: PIA14603

 

HR


#5580 From: hexagram14@...
Date: Thu Apr 12, 2012 10:23 pm
Subject: Cassini Significant Events 04/04/2012 - 04/10/2012
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Cassini Significant Events 04/04/2012 - 04/10/2012

 

The most recent spacecraft tracking and telemetry data were collected April 11 using the Deep Space Network's 34 meter High-Efficiency Station 45 at Canberra, Australia. Aside from the issues in work with the Ultrastable Oscillator (see the January 5, 2012 Significant Events) and the Cosmic Dust Analyzer, the Cassini spacecraft is in an excellent state of health. Its subsystems are operating normally as the spacecraft orbits, nearly in Saturn's equatorial plane, once every 17.8 days.

 

The S73 command sequence began execution onboard the spacecraft this week, representing the culmination of a long and involved process. Only after scientists' working teams had decided how to allocate spacecraft pointing control time to the various instrument teams did the Sequence Implementation Process begin, about five months ago. On Friday, S73 took control of the spacecraft.

 

 

Wednesday, April 04 (DOY 095)

 

Realtime commands were uplinked to perform a test of the Cosmic Dust Analyzer (CDA) to determine the cause of the instrument's packet errors seen last week. At the end of the test, the commands turned CDA off. The instrument remained off for the rest of this week, but will be turned back on prior to the Enceladus encounter coming up on Saturday.

 

 

Thursday, April 05 (DOY 096)

 

Cassini passed through apoapsis today, having slowed to 5,496 kilometers per hour relative to Saturn. This marked the beginning of Cassini's 164th orbit.

 

Orbit Trim Maneuver (OTM) 315 was cancelled because the optimum delta-V was too small to be implemented. Instead, OTM-316 on April 11 will accomplish the final orbit correction for the Enceladus E-18 flyby on April 14.

 

A realtime command was sent to clear the Solid State Power Switch (SSPS) trip counter following the unexpected trip last week of the Helium Latch Valve Driver-B switch.

 

The Encounter Strategy Meeting for the Enceladus E-18 and E-19 fly-bys was held today.

 

On the last day under control of the S72 sequence, the Visible and Infrared Mapping Spectrometer (VIMS), the Imaging Science Subsystem (ISS), and the Composite Infrared Spectrometer (CIRS) performed a 15 hour observation of Saturn's G ring and E ring; the latter is made up of icy particles ejected in jets from the moon Enceladus.

 

 

Friday, April 06 (DOY 097)

 

Realtime commands were sent to execute an end-of-sequence Reaction Wheel Assembly (RWA) bias to adjust the wheel speeds.

 

The S73 Sequence began execution. The Radio and Plasma Wave Science instrument (RPWS), the Ultraviolet Imaging Spectrograph (UVIS), ISS, and VIMS loaded their instrument-expanded-block commands from Cassini's solid-state data recorder; they will come into play as S73 continues during the next ten weeks.

 

 

Saturday, April 07 (DOY 098)

 

The Magnetometer performed an eight hour calibration while rotating the spacecraft about its X-axis; this head-over-heels motion is called pitch, as compared with roll and yaw.

 

 

Sunday, April 08 (DOY 099)

 

ISS, CIRS and VIMS performed an observation in the Titan monitoring campaign, the first of 26 such observations scattered throughout the S73 sequence to generate a long time baseline of cloud activity. For this observation, Titan was at a distance of 1.8 million kilometers. ISS then performed another observation in the Satellite Orbit Campaign.

 

 

Monday, April 09 (DOY 100)

 

The Deep Space Network station 55 in Madrid, Spain, participated in an Operations Readiness Test in preparation for a Radio Science Enceladus gravity experiment coming up on May 2. Station 25 at Goldstone, California, performed a calibration of monopulse, which is a fine-pointing capability used in Radio Science experiments.

 

The image "Smudge of a Shadow" was highlighted today, showing an elongated shadow of the small icy moon Mimas on Saturn's cloud tops.

http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4496

 

 

Tuesday, April 10 (DOY 101)

 

A web page was created for the upcoming Enceladus E-18 flyby:

http://saturn.jpl.nasa.gov/mission/flybys/eenceladus20120414/

 

 

HR


#5581 From: hexagram14@...
Date: Fri Apr 13, 2012 1:09 am
Subject: Cool picture of the day
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#5582 From: hexagram14@...
Date: Mon Apr 16, 2012 6:47 pm
Subject: Cassini Successfully Flies over Enceladus
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Cassini Successfully Flies over Enceladus

Jet Propulsion Laboratory
April 16, 2012

These raw, unprocessed images of Saturn's moons Enceladus and Tethys
were taken on April 14, 2012, by NASA's Cassini spacecraft.

Cassini flew by Enceladus at an altitude of about 46 miles (74
kilometers). This flyby was designed primarily for the ion and neutral
mass spectrometer to analyze, or "taste," the composition of the moon's
south polar plume as the spacecraft flew through it. Cassini's path
took it along the length of Baghdad Sulcus, one of Enceladus' "tiger
stripe" fractures from which jets of water ice, water vapor and organic
compounds spray into space. At this time, Baghdad Sulcus is in darkness,
but that was not an obstacle for another instrument, the composite
infrared spectrometer, which can see features by their surface
temperatures and which also took measurements during this flyby.

As soon as daylight passed into the spacecraft's remote sensing
instruments' line of sight, Cassini's cameras acquired images of the
surface. The wide-angle-camera image included in the new batch, taken
from around the time of closest approach, has some smearing from the
movement of the spacecraft during the exposure, but still shows the
surface in vivid detail.

Cassini's cameras also imaged Enceladus' south polar plume at a high
phase angle as the satellite appeared as a thin crescent and the plume
was backlit.

After the Enceladus encounter, Cassini passed the moon Tethys with a
closest approach distance of about 5,700 miles (9,100 kilometers). This
was Cassini's best imaging encounter with Tethys since a targeted
encounter in September 2005. The 2005 encounter, with a closest approach
distance of about 930 miles (1,500 kilometers), provided the images of
Tethys with the best resolution and captured views of the side of Tethys
that faces Saturn in its orbit. This new encounter examined the opposite
side of Tethys, providing some of the highest-resolution images of the
side that faces away from Saturn. Cassini acquired a 22-frame mosaic of
this side, which features the large impact basin named Odysseus.
Scientists will use these new data in conjunction with images from
previous encounters to create digital elevation maps of the moon's surface.

The Cassini-Huygens mission is a cooperative project of NASA, the
European Space Agency and the Italian Space Agency. NASA's Jet
Propulsion Laboratory in Pasadena manages the mission for the agency's
Science Mission Directorate in Washington. The Cassini orbiter and its
two onboard cameras were designed, developed and assembled at JPL. The
imaging operations team is based at the Space Science Institute in
Boulder, Colo. JPL is a division of Caltech.

For more information about the Cassini-Huygens mission, visit
http://saturn.jpl.nasa.gov <http://saturn.jpl.nasa.gov/> and
http://www.nasa.gov/cassini .

Jia-Rui C. Cook 818-354-0850
Jet Propulsion Laboratory, Pasadena, Calif.
jia-rui.c.cook@...

http://www.jpl.nasa.gov/news/news.cfm?release=2012-106
 
HR

#5583 From: hexagram14@...
Date: Wed Apr 18, 2012 3:26 pm
Subject: Rings, Titan and Enceladus
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Rings, Titan and Enceladus
 
Saturn s rings, Titan and Enceladus
Saturn’s rings, Titan and Enceladus
 

18 April 2012

Saturn’s icy moon Enceladus hangs below the gas giant’s rings while Titan lurks in the background, in this new image taken by the Cassini spacecraft.

 
Faint detail of the tiger stripe markings can be seen on Enceladus’ surface, which is framed against Titan, Saturn’s largest moon. With jets of water ice and vapor streaming from Enceladus’ south pole, and liquid hydrocarbon lakes pooling beneath Titan’s thick atmosphere, these are two of Saturn’s most enigmatic moons.


The northern, sun-lit side of Saturn’s rings are seen from just above the ring plane in this image, which was taken in visible green light by Cassini’s narrow-angle camera on 12 March while it was approximately one million kilometers from Enceladus. The image scale is six kilometers per pixel on Enceladus. 
 
 
HR

#5584 From: hexagram14@...
Date: Thu Apr 19, 2012 5:38 pm
Subject: Far-off cousin of part-time African lake found on Titan
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Far-off cousin of part-time African lake found on Titan

European Space Agency
19 Apr 2012

A region on Saturn's moon Titan has been found to be similar to the
Etosha Pan in Namibia, Africa. Both are ephemeral lakes - large, shallow
depressions that sometimes fill with liquid.

Ontario Lacus is the largest lake in the southern hemisphere of Saturn's
moon, Titan. It is a little smaller than its namesake, Lake Ontario in
North America, but otherwise differs from it in some major ways.

It is filled with liquid hydrocarbons, not water, and it is only a few
meters deep at most, located in an extremely shallow depression in a
flat sedimentary basin, surrounded by small mountain ranges.

In addition, a new study shows that these landforms and the climatic
conditions in the region are similar to those of semi-arid regions on
Earth, such as the salt pans of southern Africa.

The observations were made by the Cassini orbiter, part of the NASA, ESA
and Italian Space Agency Cassini-Huygens mission to Saturn's system.

While Ontario Lacus was previously thought to be permanently filled with
liquid methane, ethane and propane, these latest observations, published
in the journal Icarus, suggest otherwise.

By combining data from Cassini's imaging, spectroscopic and radar
instruments - each of which observed Ontario Lacus twice - scientists
led by Thomas Cornet of the Universite de Nantes, France, found evidence
for channels etched into the lake bed within the southern boundary of
the depression. These channels remained visible between December 2007
and January 2010, each time the spatial resolution was able to resolve them.

"We conclude that the solid floor of Ontario Lacus is most probably
exposed in those areas," says Cornet.

By comparing observations made by Cluster and Mars Express, the
scientists found that the rate of increase in O+ losses was the same
order of magnitude on both planets under these different conditions.
Since the scientists have already shown the protective role of Earth's
magnetic field, they propose that the similar rate of increase is
attributed to Mars' greater distance from the Sun. This is the first
observational evidence that distance plays an important role in the
evolution of planetary atmospheres.

In addition, Cassini shows sediments around Ontario Lacus that also
indicate the liquid level has been higher in the past.

This is similar to ephemeral lakes on Earth. The researchers suggest its
nearest cousin is the Etosha Pan in Namibia. This salt lake bed fills
with a shallow layer water, provided by the rise of the underground
aquifer during the rainy season, before evaporating to leave sediments
like tide marks showing the previous extent of the water.

Cornet and colleagues thus believe that Ontario Lacus is also the result
of subsurface hydrocarbon fluids occasionally welling up and flooding
the depression, before then partially drying out again.

Beyond Earth, Titan is the only other world known to bear stable liquids
on its surface. Where Earth has a water cycle, Titan has a full
hydrocarbon cycle, based on hydrogen, carbon and nitrogen, taking place
between the atmosphere, the surface and the subsurface. Titan's lakes
are an integral part of this process.

"These results emphasize the importance of comparative planetology in
modern planetary sciences: finding familiar geological features on alien
worlds like Titan allows us to test the theories explaining their
formation," says Nicolas Altobelli, ESA's Cassini-Huygens project
scientist.

 
HR

#5585 From: hexagram14@...
Date: Sat Apr 21, 2012 1:43 am
Subject: Watch the skies
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Space Weather News for April 21,  2012
http://spaceweather.com

LYRID METEOR SHOWER: The annual Lyrid  meteor shower peaks this weekend on
the night of April 21-22 when Earth passes  through a stream of debris from
ancient Comet Thatcher. Usually the shower is  mild (10-20 meteors per hour)
but unmapped filaments of dust in the comet's tail  sometimes trigger
outbursts ten times stronger. This year's peak coincides with  a new Moon, so
lunar interference will not be a problem.  The promise of a  good display has
prompted NASA to plan an unusual 3D meteor photography  experiment combining
observations from the ground, a research balloon, and the  International
Space Station.  More information, observing tips, and live  audio from a meteor
radar are available on today's edition of  http://SpaceWeather.com


HR

#5586 From: hexagram14@...
Date: Mon Apr 23, 2012 4:12 pm
Subject: Cassini Significant Events 04/11/2012 - 04/17/2012
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Cassini Significant Events 04/11/2012 - 04/17/2012

 

The most recent spacecraft tracking and telemetry data were collected April 18 using the Deep Space Network's 34 meter Beam-Waveguide Station 55 at Madrid, Spain. Beyond the issues in work with the Ultrastable Oscillator (see the January 5, 2012 Significant Events) and the Cosmic Dust Analyzer, the Cassini spacecraft is in an excellent state of health. Its subsystems are operating normally as the spacecraft orbits, nearly in Saturn's equatorial plane, once every 17.8 days. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

E-18, the targeted flyby of Enceladus on Saturday, was this week's highlight. The Ion and Neutral Mass Spectrometer (INMS) and the other Magnetospheric and Plasma Science (MAPS) instruments were prime for closest approach and flight through the plume. View the E-18 web page here: http://saturn.jpl.nasa.gov/news/cassinifeatures/feature20120416/.

 

Among Cassini's routine activities this week were three observations in the Titan monitoring campaign to look for cloud activity over a long time baseline. There were also two observations in the Satellite Orbit Campaign, in which the Imaging Science Subsystem (ISS) measures positions of small satellites, improving knowledge of their orbits. One reason for these frequent observations is that over the mission's duration it may be possible to measure small changes in their orbits. Such changes could potentially provide an independent determination of the mass of Saturn's rings or of certain of the icy satellites such as Mimas.

 

ISS also undertook searches at the L4 and L5 Lagrange points in Rhea's orbit about Saturn, looking for any small satellites that might be trapped in these stable points 60 degrees ahead and behind Rhea, respectively. So far, none has been discovered.

 

 

Wednesday, April 11 (DOY 102)

 

Orbit Trim Maneuver (OTM) 316, the Enceladus 18 approach maneuver, was performed today. As usual, the maneuver was designed based on the latest navigation data, and translated into commands that were transmitted to the spacecraft only a few hours before they would execute. The RCS thrusters fired for 25.5 seconds, providing Cassini 31 mm/s of delta-V. In the target plane, the aim-point was intentionally biased by about 4 kilometers off the nominal trajectory because doing so would save propellant and simplify implementation.

 

Realtime commands were uplinked today that will turn on the Cosmic Dust Analyzer (CDA) shortly before the E-18 encounter on Saturday. Commands in the background sequence (S73) turned on CDA heaters for roughly ten hours today to perform a routine decontamination of the instrument.

 

 

Thursday, April 12 (DOY 103)

 

The Navigation Team took five images of Saturn's moon Dione against the background stars for optical navigation purposes, then the Ultraviolet Imaging Spectrograph (UVIS) began a 13 hour observation of Saturn's aurora.

 

The main engines' protective cover was deployed to its closed position.

 

 

Friday, April 13 (DOY 104)

 

When UVIS completed its aurora observation, the spacecraft turned to point its high-gain antenna (HGA) to Earth, and downlinked all the telemetry data that had been stored on the Solid-State Recorders (SSRs). The Canberra, Australia, 70 meter diameter Deep Space Network (DSN) station captured every bit. This was one of seven routine DSN tracking activities for the week.

 

The E-18 flyby filled up the SSRs with new data. It began with long Enceladus plume observations led by the Visible and Infrared Mapping Spectrometer (VIMS) and ISS at a low latitude and at a variety of spatial scales, to be used for morphological studies and context.

 

 

Saturday, April 14 (DOY 105)

 

As the E-18 encounter continued, the Composite Infrared Spectrometer (CIRS) led Optical Remote-Sensing (ORS) viewing of Enceladus's night-side anti-Saturn-facing hemisphere, with dark sky behind, to search for possible hot spots away from the "tiger stripe" crevasses. At this time, the commands uplinked on Wednesday took effect, powering CDA on for the encounter.

 

Closing in on the icy target, the spacecraft turned to give INMS prime status for closest approach, going 27,000 km/h with respect to Enceladus. The purpose of this series of observations was to understand variability in Enceladus's activity and to map the plume's three-dimensional structure. As the spacecraft then proceeded outbound from Enceladus (though still inbound to Saturn), CIRS made observations to complete its coverage and to search for additional hot spots on the day-side Saturn-facing hemisphere.

 

Following the E-18 encounter, VIMS performed a stellar occultation experiment. This means that VIMS kept its telescope trained on the bright star Procyon (alpha Canis Minoris) and watched it for 2 hours 40 minutes while Cassini's motion caused the star to set slowly into Saturn's atmosphere, to gain information about the atmosphere.

 

Before the stellar occultation was finished, Cassini passed through periapsis, the low point in its orbit about Saturn, going 68,123 km/h. (Compare this to its Saturn-relative speed of 5,496 km/h at the high point in its orbit last week.)

 

Next came a series of observations of the moon Tethys from a close-approach distance of 9,053 kilometers by various ORS instruments. These observations will provide data to extend the mapping of Tethys's geologic features, and to understand the interaction of the E ring and energetic electrons with the icy moon's surface. The observations from this non-targeted flyby should help refine mapping of Tethys's "pacman" feature, similar to that seen on Mimas, caused by the varying thermal inertia across the surface. For reference, see http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=3919.

 

 

Sunday, April 15 (DOY 106)

 

Today's task was to downlink all the E-18 telemetry data at rates up to 142,201 bits (binary digits) per second. Thanks to the 70 meter diameter DSN stations in Canberra, Australia and Madrid, Spain, the data were captured flawlessly.

 

After the E-18 flyby, CDA stopped producing data. It was turned off by real-time command today after members of the flight team held an anomaly meeting.

 

Cassini's ORS instruments made an observation of Saturn's icy moon Rhea as a small dark crescent with dark sky behind.

 

The main engine cover was stowed to its open position. This was the 73rd in-flight cycle.

 

Saturn comes closest to Earth today as Saturn and Earth orbit the Sun. The ringed planet is at opposition, so it rises in the East at sunset, and sets near dawn. This highlights a season of great viewing opportunities for anyone who has access to even a small telescope. See "Viewing Saturn in 2012": http://saturn.jpl.nasa.gov/education/saturnobservation/viewingsaturn/.

 

 

Monday, April 16 (DOY 107)

 

CIRS began a 12 hour Saturn observation to measure oxygen compounds (H2O, CO2) in the stratosphere, then the magnetometer executed a calibration while rolling the spacecraft about its Z-axis, keeping the HGA facing Earth all the while for communication.

 

The DSN station 34 in Canberra, Australia, acquired the Ka-band (32 GHz) signal from Cassini to perform a calibration of monopulse, the fine-pointing capability used in Radio Science experiments. This occurred at the same time as X-band (8 GHz) communications and tracking were in progress.

 

Sequence Implementation Process team members held a Science Forum meeting for development of the S75 command sequence, which is scheduled to be uplinked in August.

 

OTM-317, the E-18 clean-up maneuver that was scheduled for April 18, was cancelled today. This was because the propellant cost of making the maneuver implementable was found to be about equal to the downstream cost of canceling it.

 

An image of Enceladus in front of Titan and Saturn's rings is featured today:

http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4497

 

 

Tuesday, April 17 (DOY 108)

 

The Navigation Team took five images of Saturn's moon Iapetus against the background stars for optical navigation purposes.

 

JPL software developers identified a fix in an upcoming delivery of ground software for a problem that prevented remote Science Operations Planning Computers from querying the JPL-based Telemetry Delivery System.

 

 HR


#5587 From: hexagram14@...
Date: Mon Apr 23, 2012 10:32 pm
Subject: Cassini Spacecraft Sees New Objects Blazing Trails in Saturn Ring
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RELEASE : 12-128
 
 
Cassini Spacecraft Sees New Objects Blazing Trails in Saturn Ring
 
 
WASHINGTON -- Scientists working with images from NASA's Cassini spacecraft have discovered strange, half-mile-sized objects punching through one of Saturn's rings and leaving glittering trails behind them. The results will be presented tomorrow at the European Geosciences Union meeting in Vienna, Austria.

The penetration occurred in the outermost of Saturn's main rings, called the F ring, which has a circumference of 550,000 miles (881,000 kilometers). Scientists are calling the trails in the F ring "mini-jets." Cassini scientists combed through 20,000 images and found 500 examples of these rogues during the seven years Cassini has been at Saturn.

"Beyond just showing us the strange beauty of the F ring, Cassini's studies of this ring help us understand the activity that occurs when solar systems evolve out of dusty disks that are similar to, but obviously much grander than, the disk we see around Saturn," said Linda Spilker, Cassini project scientist at NASA's Jet Propulsion Laboratory (JPL) in Pasadena, Calif.

Scientists have known relatively large objects can create channels, ripples and snowballs, or clumps of icy material, in the F ring. However, scientists did not know what happened to these snowballs after they were created. Some were broken up by collisions or tidal forces in their orbit around Saturn. Scientists now have evidence some of the smaller ones survived, and their differing orbits mean they go on to strike through the F ring on their own.

"I think the F ring is Saturn's weirdest ring, and these latest Cassini results go to show how the F ring is even more dynamic than we ever thought," said Carl Murray, a Cassini imaging team member based at Queen Mary University of London, U.K. "These findings show us that the F ring region is like a bustling zoo of objects from a half-mile (0.8-kilometer) in size to moons like Prometheus a hundred miles (160.9 kilometers) in size, creating a spectacular show."

These small objects appear to collide with the F ring at gentle speeds about 4 mph (2 meters per second). The collisions drag glittering ice particles out of the F ring with them, leaving a trail of 20-110 miles (40-180 kilometers) long.

In some cases, the objects traveled in packs, creating mini-jets that looked exotic, like the barb of a harpoon. Other new images show grand views of the entire F ring and the swirls and eddies from the different kinds of objects moving through and around it.

Saturn's rings are comprised primarily of water ice. The chunks of ice that make up the main rings spread out 85,000 miles (140,000 kilometers) from the center of Saturn. Scientists believe the rings' average thickness is approximately 30 feet (10 meters).

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. JPL manages the mission for NASA's Science Mission Directorate in Washington. The imaging team is based at the Space Science Institute in Boulder, Colo.

New images and movies of the mini-jets are available at:

http://www.nasa.gov/mission_pages/cassini/whycassini/cassini20120423.html


For information about Cassini, visit:

http://www.nasa.gov/cassini

 

- end -

 

 

HR


#5588 From: hexagram14@...
Date: Tue Apr 24, 2012 3:57 pm
Subject: Cassini movie shows blazing trails in Saturn’s F-ring
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Blazing trails in Saturn s F-ring seen by Cassini
Blazing trails in Saturn’s F-ring seen by Cassini
 
Cassini movie shows blazing trails in Saturn’s F-ring

 
 
24 April 2012
New images from the Cassini spacecraft reveal rogue kilometer-sized objects punching through Saturn’s F-ring as the source of ‘mini-jets’ seen emanating from the ring.

 
Saturn’s narrow F-ring is already known to host a variety of dynamic features including channels, ripples and ‘snowballs’ that are created by the gravitational influence of nearby moon Prometheus. While some snowballs are likely broken up by collisions and tidal forces, the new images reveal five hundred separate cases where small surviving fragments punch through the F-ring, dragging icy ring particles with them.
 

The objects collide with the ring at low speeds of around two meters per second, resulting in ‘mini-jets’ that extend between 40 and 180 kilometers from the ring. In some cases the snowball impacts occur in groups, creating exotic patterns as they drag through the ring.

The new results were presented today at the European Geosciences Union meeting in Vienna, Austria.  
 

 
HR

#5589 From: hexagram14@...
Date: Tue Apr 24, 2012 9:01 pm
Subject: Cassini Investigates Titan's Chemical Factory
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Cassini Investigates Titan's Chemical Factory

Jet Propulsion Laboratory
April 24, 2012

Saturn's giant moon Titan hides behind a thick, smoggy atmosphere that's
well known to scientists as one of the most complex chemical
environments in the solar system. It's a productive "factory" cranking
out hydrocarbons that rain down on Titan's icy surface and cloak it in
soot. With a brutally cold surface temperature of around minus 270
degrees Fahrenheit (minus 170 degrees Celsius), the hydrocarbons form
lakes of liquid methane and ethane.

However, the most important raw ingredient in Titan's chemical factory
is methane gas. Methane is a molecule made up of one carbon atom joined
to four hydrogen atoms. It should not last long because it's being
continuously destroyed by sunlight and converted to more complex
molecules and particles. New research from NASA-funded scientists
attempts to estimate how long this factory has been operating. The
results are presented in two papers appearing in the April 20 issue of
the Astrophysical Journal.

These papers used data collected by two instruments onboard NASA's
Cassini spacecraft in orbit around Saturn and one instrument on the
European Space Agency's Huygens probe that landed on Titan's surface in
January 2005. All three instruments were built at NASA's Goddard Space
Flight Center in Greenbelt, Md. A paper led by Conor Nixon of the
University of Maryland, College Park uses infrared signatures (spectra)
of methane from Cassini's composite infrared spectrometer to estimate
how much "heavy" methane containing rare isotopes is present in Titan's
atmosphere.

Isotopes are versions of an element with different weights, or masses.
For example, carbon 13 is a heavier (and rare) version of the most
common type of carbon, called carbon 12. Occasionally, a carbon-13 atom
replaces a carbon-12 atom in a methane molecule. Because methane made
with carbon 12 is slightly lighter, the chemical reactions that convert
it to more complex hydrocarbons happen a bit faster. This means
carbon-12 methane gets used up at a slightly faster rate than heavy
carbon-13 methane, so the concentration of heavy methane in Titan's
atmosphere increases slowly.

By modeling how the concentration of heavy methane changes over time,
the scientists predicted how long Titan's chemical factory has been running.

"Under our baseline model assumptions, the methane age is capped at 1.6
billion years, or about a third the age of Titan itself," said Nixon,
who is stationed at Goddard. "However, if methane is also allowed to
escape from the top of the atmosphere, as some previous work has
suggested, the age must be much shorter -- perhaps only 10 million years
-- to be compatible with observations."

Both scenarios assume that methane entered the atmosphere in one burst
of outgassing, probably from the restructuring of Titan's interior as
heavier materials sank towards the center and lighter ones rose toward
the surface.

"However, if the methane has been continuously replenished from a
source, then its isotopes would always appear 'fresh' and we can't
restrict the age in our model," said Nixon. Possible sources include
methane clathrates, basically a methane molecule inside a "cage" or
lattice of ice molecules. Methane clathrates are found in the frigid
depths of Earth's oceans, and some scientists think there could be an
ocean of liquid water mixed with ammonia (acting as antifreeze) beneath
Titan's water-ice crust. If this is so, methane might be released from
its clathrate cages during the eruptions of proposed 'cryovolcanoes' of
water-ammonia slurry, or more simply could slowly seep out through
fractures in the crust.

The second Titan paper by Kathleen Mandt of the Southwest Research
Institute, San Antonio, and colleagues also models the time-evolution of
methane. In this work, the concentration of the heavy methane is
determined from measurements by Cassini's ion and neutral mass
spectrometer, which counts molecules in the atmosphere of different
masses (weights). Measurements made by the Huygens gas chromatograph
mass spectrometer, which also counts molecules of different masses, were
used to constrain the impact of escape on the heavy methane in the
atmosphere.

"We compute that, even if methane has been replenished from the interior
over time to match or exceed the amounts fed into the atmospheric
chemical factory, the process must have been running for a maximum of
one billion years," said Mandt. "If the process had started any earlier,
we would see a build-up of methane in the lakes on the surface and in
the atmosphere beyond what is observed today."

Together these papers add important new perspectives and constraints on
the history of Titan's methane atmosphere, confirming that it must have
formed long after Titan itself. Previous work considering the evolution
of Titan's interior predicted the last major methane eruption occurred
350 million to 1.35 billion years ago, while crater counting has put the
age of the current surface at 200 million to one billion years. (Crater
counting works on the principle that an older surface has more craters,
just as the longer you're in a paintball game, the more hits you'll get.)

The present work for the first time estimates the methane age from the
atmosphere itself, at less than one billion years, considering both papers.

This research was supported by the NASA Cassini Mission and the NASA
Cassini Data Analysis Program grant NNX09AK55G. The Cassini-Huygens
mission is a cooperative project of NASA, the European Space Agency and
the Italian Space Agency. The Jet Propulsion Laboratory, a division of
the California Institute of Technology in Pasadena, manages the mission
for NASA's Science Mission Directorate, Washington.

For related images to this story, please visit:
http://www.nasa.gov/mission_pages/cassini/whycassini/factory20120420.html
 
HR

#5590 From: hexagram14@...
Date: Thu Apr 26, 2012 9:03 pm
Subject: Cassini Finds Saturn Moon has Planet-Like Qualities
happy_rasta
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JPL/NASA News

News feature: 2012-119                                                                     April 26, 2012

Cassini Finds Saturn Moon has Planet-Like Qualities

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.cfm?release=2012-119&cid=release_2012-119

PASADENA, Calif. -- Data from NASA's Cassini mission reveal Saturn's moon Phoebe has more planet-like qualities than previously thought.

Scientists had their first close-up look at Phoebe when Cassini began exploring the Saturn system in 2004. Using data from multiple spacecraft instruments and a computer model of the moon's chemistry, geophysics and geology, scientists found Phoebe was a so-called planetesimal, or remnant planetary building block. The findings appear in the April issue of the Journal Icarus.

"Unlike primitive bodies such as comets, Phoebe appears to have actively evolved for a time before it stalled out," said Julie Castillo-Rogez, a planetary scientist at NASA's Jet Propulsion Laboratory in Pasadena, Calif. "Objects like Phoebe are thought to have condensed very quickly. Hence, they represent building blocks of planets. They give scientists clues about what conditions were like around the time of the birth of planets and their moons."

Cassini images suggest Phoebe originated in the far-off Kuiper Belt, the region of ancient, icy, rocky bodies beyond Neptune's orbit. Data show Phoebe was spherical and hot early in its history, and has denser rock-rich material concentrated near its center. Its average density is about the same as Pluto, another object in the Kuiper Belt. Phoebe likely was captured by Saturn's gravity when it somehow got close to the giant planet.

Saturn is surrounded by a cloud of irregular moons that circle the planet in orbits tilted from Saturn's orbit around the sun, the so-called equatorial plane. Phoebe is the largest of these irregular moons and also has the distinction of orbiting backward in relation to the other moons. Saturn's large moons appear to have formed from gas and dust orbiting in the planet's equatorial plane. These moons currently orbit Saturn in that same plane.

"By combining Cassini data with modeling techniques previously applied to other solar system bodies, we've been able to go back in time and clarify why it is so different from the rest of the Saturn system," said Jonathan Lunine, a co-author on the study and a Cassini team member at Cornell University, Ithaca, N.Y.

analyses suggest that Phoebe was born within the first 3 million years of the birth of the solar system, which occurred 4.5 billion years ago. The moon may originally have been porous but appears to have collapsed in on itself as it warmed up. Phoebe developed a density 40 percent higher than the average inner Saturnian moon.

Objects of Phoebe's size have long been thought to form as "potato-shaped" bodies and remained that way over their lifetimes. If such an object formed early enough in the solar system's history, it could have harbored the kinds of radioactive material that would produce substantial heat over a short timescale. This would warm the interior and reshape the moon.

“From the shape seen in Cassini images and modeling the likely cratering history, we were able to see that Phoebe started with a nearly spherical shape, rather than being an irregular shape later smoothed into a sphere by impacts," said co-author Peter Thomas, a Cassini team member at Cornell.

Phoebe likely stayed warm for tens of millions of years before freezing up. The study suggests the heat also would have enabled the moon to host liquid water at one time. This could explain the signature of water-rich material on Phoebe's surface previously detected by Cassini.

The new study also is consistent with the idea that several hundred million years after Phoebe cooled, the moon drifted toward the inner solar system in a solar-system-wide rearrangement. Phoebe was large enough to survive this turbulence.

More than 60 moons are known to orbit Saturn, varying drastically in shape, size, surface age and origin. Scientists using both ground-based observatories and Cassini's cameras continue to search for others.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. JPL manages the mission for the agency's Science Mission Directorate in Washington. The California Institute of Technology in Pasadena manages JPL for NASA.

For more information on the Cassini mission, visit: http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov .

Jia-Rui C. Cook 818-354-0850
Jet Propulsion Laboratory, Pasadena, Calif.
jccook@...

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@...


- end -



HR

#5591 From: hexagram14@...
Date: Tue May 1, 2012 4:18 pm
Subject: Cassini Enceladus Flyby - May 2, 2012
happy_rasta
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Cassini Enceladus Flyby - May 2, 2012
May. 02, 2012

Enceladus 'E-19' Flyby: Completing the Trilogy

E-19 is the third of three fly-bys (along with E-9 and E-12 designed
to understand the internal structure of Enceladus, particularly the
concentration of mass under the south polar region. Data collected in
this area may provide insight into the plume activity on the moon.
During E-19, radio science (RSS) will have its usual three periods of
observation: two wings and closest-approach. The fields, particles and
waves instruments' pointing will be optimized to gather data near
closest approach.

Other highlights:

* During the dark approach, the composite infrared spectrometer
(CIRS) will be observing the anti-Saturnian hemisphere to
monitor hot spots, and discover new ones to understand the
global energy balance of Enceladus. During the exit leg, CIRS
will be observing near the equator during the day (again to
understand the global energy balance).

* After E-19, there is a 5,010 mile (8,063 kilometer) Dione
untargeted flyby with imaging science subsystem (ISS) and CIRS
prime. This flyby is designed to seek hot spots and possible
emission from Dione, and to map poorly observed regions.

* Other observations include a plume observation similar to one
taken on the previous pass, to understand plume variability on
the scale of weeks; and two 10-hour irregular satellite
observations to derive their lightcurve and rotational states,
to give further information on the collisional environment in
the outer Saturnian system.

Enceladus Flyby at a Glance

Date
May 2, 2012 (SCET)

Altitude
46 miles (74 kilometers)

Speed
17,000 mph
(7.5 km/sec)

http://saturn.jpl.nasa.gov/mission/flybys/enceladus20120502/
 
HR

#5592 From: hexagram14@...
Date: Thu May 3, 2012 4:44 pm
Subject: Cassini Significant Events 04/25/2012 - 05/01/2012
happy_rasta
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Cassini Significant Events 04/25/2012 - 05/01/2012

 

The most recent spacecraft tracking and telemetry data were collected on May 2 using the Deep Space Network's 34 meter high-efficiency Station 34 at Canberra, Australia. Aside from the issue in work with the Ultrastable Oscillator (see the January 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health. Its subsystems are operating normally as the spacecraft orbits Saturn, nearly in the equatorial plane, once every 17.8 days. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

This week's events included preparations for the Enceladus E-19 targeted flyby on May 2, which will bring the spacecraft to within 74 kilometers of the icy satellite and make measurements of its gravity field. More information on E-19 may be found here: http://saturn.jpl.nasa.gov/mission/flybys/enceladus20120502/.

 

On the ground, Cassini flight team members made progress working on science observation plans for sequences S74, which goes active in June, S75 (August), S76 (November), and S77 (January 2013).

 

 

Wednesday, April 25 (DOY 116) 

 

The Spacecraft Operations Office held an Engineering Activities Review for the S76 command sequence. The Radio Science Support team held a meeting with members of the DSN and Realtime Operations teams to finalize operations for the E-19 gravity observation.

 

 

Thursday, April 26 (DOY 117)

 

A 34 meter diameter Deep Space Network (DSN) station in Canberra, Australia, participated in an Operational Readiness Test, preparing for the E-19 realtime Radio Science gravity measurement during closest approach on May 2.

 

A news release titled, "Cassini Finds Saturn Moon Has Planet-Like Qualities" describes new findings about Saturn's outer, retrograde moon Phoebe. It may be viewed here:

http://saturn.jpl.nasa.gov/news/newsreleases/newsrelease20120426/

 

 

Friday, April 27 (DOY 118)

 

The Attitude and Articulation Control (AACS) team performed a reaction-wheel assembly (RWA) bias maneuver, stabilizing the spacecraft via thrusters and setting the RWAs to the required speeds while the DSN was tracking the spacecraft. AACS also performed a calibration of the spacecraft's backup inertial reference unit (gyros). These calibrations are performed about once per year and require rotating the spacecraft about its X, Y and Z axes.

 

 

Saturday, April 28 (DOY 119)

 

ISS performed another observation in the Satellite Orbit Campaign. VIMS performed a Saturn storm watch observation.

 

Commands were sent to the spacecraft that were time-tagged to power the Cosmic Dust Analyzer (CDA) back on just prior to the E-19 flyby. Additional commands were sent to do a live update within the AACS Inertial Vector Propagator to refine pointing information on the location of Dione, which will be observed during the non-targeted encounter following E-19.

 

Orbit Trim Maneuver (OTM) 319, the E-19 approach maneuver, operated the Reaction Control Subsystem thrusters for 29.5 seconds, resulting in a delta-V of 0.034 meters per second.

 

Saturn was the featured attraction at two local Astronomy Day activities attended by Cassini outreach specialists.

 

 

Sunday, April 29 (DOY 120)

 

The DSN provided eight tracking sessions for Cassini using stations in Canberra, Australia, and Goldstone, California this week. There were several small data outages.

 

 

Monday, April 30 (DOY 121)

 

The Ultraviolet Imaging Spectrograph (UVIS) performed a 10 hour observation of Saturn's aurora.

 

The main engine protective cover was deployed to its closed position.

 

The Attitude and Articulation Control Subsystem executed an RWA Y-bias maneuver to adjust wheel speeds while Cassini was off Earth point, out of communication.

 

An image titled "Moon Specks", showing Tethys and Enceladus, is featured here:

http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4516.

 

 

Tuesday, May 1 (DOY 122)

 

ISS observed an irregular outer satellite for nearly 10 hours to gather data for a light curve to give further information on the collisional environment in the outer Saturnian system. VIMS performed a 3-hour solar-port calibration activity.

 

DSN station 25, a 34 meter aperture at Goldstone, California, began a gravity science enhancement observation prior to tomorrow's E-19 flyby. Station 25's X-band (8 GHZ) uplink provided for an X-band and Ka-band (32 GHz) coherent downlink from Cassini. The Doppler data contained in these signals will add to knowledge of Enceladus's gravity field.

 

 

HR


#5593 From: hexagram14@...
Date: Fri May 4, 2012 6:59 pm
Subject: Video of the Week
happy_rasta
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Saturn Stunning Close-Ups


ShareShare  ShareEmail  PrintPrint



Video of the Week #41 May 3rd, 2012

 

From: Saturn Is Alive, No CGI by Caleb A. Scharf at Life, Unbounded.

 

Source: Sander van den Berg

 

The Netherlands-based director and editor Sander van den Berg has put together a stunning series of Cassini still images to produce “Outer Space.” The short film covers a remarkable amount of what’s going on in the Saturnian ‘hood (and a litle bit of Jupiter as well) – including some incredible shots of moonlets interacting with the rings, storms and circulations on Saturn itself, and the endless to-ing and fro-ing of moons, light, and shadow.

 

http://blogs.scientificamerican.com/video-of-the-week/2012/05/03/saturn-stunning-close-ups/?WT_mc_id=SA_DD_20120504

 

HR


#5594 From: hexagram14@...
Date: Thu May 10, 2012 2:25 pm
Subject: Saturn's Brightly Reflective Moon Enceladus
happy_rasta
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Image of the Day Gallery

 

#5595 From: hexagram14@...
Date: Fri May 11, 2012 12:23 am
Subject: Cassini Significant Events 05/02/2012 - 05/08/2012
happy_rasta
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Cassini Significant Events 05/02/2012 - 05/08/2012

 

The most recent spacecraft tracking and telemetry data were collected on May 9 using the Deep Space Network's 70 meter Station 43 at Canberra, Australia. Aside from the issues in work with the Cosmic Dust Analyzer (CDA) and the Ultrastable Oscillator (see the January 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health and its subsystems are operating normally. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

This week's highlight was the targeted E-19 close encounter with Saturn's 500 kilometer diameter snow-white moon Enceladus on Wednesday. The flyby delivered the final in a set of three Enceladus encounters designed to give real-time Radio Science measurements of Enceladus's gravity field. It also included another pass through the plume from the geysers. More information on E-19 may be found here: http://saturn.jpl.nasa.gov/mission/flybys/enceladus20120502/ .

 

 

Wednesday, May 2 (DOY 123)

 

During the Enceladus E-19 flyby, the spacecraft turned frequently under control of the Attitude and Articulation Control (AACS) Reaction Wheel Assemblies (RWA) to properly point the Optical Remote Sensing (ORS) instruments and the Magnetospheric and Plasma Science (MAPS) instruments. All the telemetry data from their many observations went to the Solid-State Recorder (SSR) for later playback to Earth. Radio Science experiments operate differently. For long periods around and during closest approach to Enceladus (74 kilometers), Cassini was oriented to keep its high-gain antenna dish pointed to Earth while receiving a frequency-stable signal from the Deep Space Network (DSN). Cassini's downlink, locked to this reference signal, was received on Earth an hour and 13 minutes later. Its Doppler shift was accurately measured, providing the Radio Science data that contains information about mass distribution within Enceladus. Not to waste any Earth-pointed time, though, telemetry data were also played back from the SSR during the Radio Science experiment.

 

Cassini passed periapsis, this orbit's closest point to Saturn at 136,000 kilometers above the clouds, going 68,213 kilometers per hour relative to the planet.

 

The busy day concluded with Cassini turning its ORS instruments to Dione 8,000 kilometers away (for which pointing vectors were updated last week via realtime command). With Dione squarely in view, the Composite Infrared Spectrometer (CIRS) and Imaging Science Subsystem (ISS) scanned its equatorial latitudes on the leading hemisphere, with a chance to observe the fractured region and do further searches for evidence of out-gassing or recent activity.

 

The illustrated feature "Cassini, Saturn Moon Photographer" was published on the Cassini website:

http://saturn.jpl.nasa.gov/news/cassinifeatures/feature20120502/ .

 

 

Thursday, May 3 (DOY 124)

 

The Cosmic Dust Analyzer (CDA) exhibited telemetry packet production problems again, and was powered off by realtime command following an anomaly meeting today.

 

The Ultraviolet Imaging Spectrograph (UVIS) performed an instrument calibration, and ISS made a 9-hour observation of one of Saturn's outer irregular satellites, Ymir, a tiny, dark body in a retrograde orbit 23 million kilometers away.

 

The AACS team performed an RWA Y-bias maneuver, stabilizing the spacecraft via thrusters and setting the RWAs to the required speeds. Thrusters usually impart a small delta-V. Since the spacecraft was out of communication with Earth, the Navigation team relied on telemetry played back later to estimate the effect on Cassini's orbit.

 

The main engines' protective cover was stowed to its open position.

 

 

Friday, May 4 (DOY 125)

 

The Cassini Plasma Spectrometer (CAPS), a direct-sensing instrument, measured the ambient co-rotating plasma at low latitude in Saturn's magnetosphere for half the day. The spacecraft was 1.5 million kilometers from Saturn as it continued coasting outbound from periapsis.

 

 

Saturday, May 5 (DOY 126)

 

Playback of telemetry from the icy satellite observations, including Enceladus and Dione, was completed this morning after three daily sessions with the DSN's 70 meter aperture station at Goldstone.

 

The MAPS instruments, directly sensing ambient conditions, continued to acquire measurements in Saturn's outer magnetosphere and magnetosheath. By doing this once every four to six months, these instruments are able to observe Saturn's magnetosphere over a solar cycle, from one solar minimum to the next, and investigate periodicities and how the Saturn kilometric radiation period is imposed on the magnetosphere.

 

 

Sunday, May 6 (DOY 127)

 

OTM-320, the E-19 clean-up maneuver scheduled for today, was found to be unnecessary because of the small E-19 target miss, and was canceled.

 

 

Monday, May 7 (DOY 128)

 

The MAPS instruments continued their observations in Saturn's outer magnetosphere.

 

An image of Saturn's 200 kilometer wide, cratered moon Janus, which orbits outside the F ring, is featured at:

http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4519 .

 

 

Tuesday, May 08 (DOY 129)

 

On three days this week including today, ISS monitored distant Titan, with CIRS and the Visible and Infrared Mapping Spectrometer (VIMS) also taking measurements.

 

 

 HR


#5596 From: hexagram14@...
Date: Sat May 12, 2012 10:29 pm
Subject: "Saturn's Strange Voice" -- Radio Waves Vary at Its North and South Hemispheres
happy_rasta
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"Saturn's Strange Voice" -- Radio Waves Vary at Its North and South Hemispheres
 

 

                    Saturn2


Data from NASA's Cassini spacecraft show that the variation in radio waves controlled by the planet's rotation is different in the northern and southern hemispheres. Moreover, the northern and southern rotational variations also appear to change with the Saturnian seasons, and the hemispheres have actually swapped rates.

 

Click to hear Saturn's Eerie Voice

 

"The rain of electrons into the atmosphere that produces the auroras also produces the radio emissions and affects the magnetic field, so scientists think that all these variations we see are related to the sun's changing influence on the planet," said Stanley Cowley, co-investigator on Cassini's magnetometer instrument.

 

"These data just go to show how weird Saturn is," said Don Gurnett, Cassini's radio and plasma wave science instrument team leader, and professor of physics at the University of Iowa, Iowa City. "We thought we understood these radio wave patterns at gas giants, since Jupiter was so straightforward. Without Cassini's long stay, scientists wouldn't have understood that the radio emissions from Saturn are so different." 

 

Saturn emits radio waves known as Saturn Kilometric Radiation, or SKR for short that sound like bursts of a spinning air raid siren, since the radio waves vary with each rotation of the planet. This kind of radio wave pattern had been previously used at Jupiter to measure the planet's rotation rate, but at Saturn, as is the case with teenagers, the situation turned out to be much more complicated.

 

When NASA's Voyager spacecraft visited Saturn in the early 1980s, the radiation emissions indicated the length of Saturn's day was about 10.66 hours. But as its clocking continued by a flyby of the joint ESA-NASA Ulysses spacecraft and Cassini, the radio burst varied by seconds to minutes. A paper in Geophysical Research Letters in 2009 analyzing Cassini data showed that the Saturn Kilometric Radiation was not even a solo, but a duet, with two singers out of sync. Radio waves emanating from near the north pole had a period of around 10.6 hours; radio waves near the south pole had a period of around 10.8 hours.

 

A new paper led by Gurnett shows that, in Cassini data, the southern and northern SKR periods crossed over around March 2010, about seven months after equinox, when the sun shines directly over a planet's equator. 

 

The southern SKR period decreased from about 10.8 hours on Jan. 1, 2008 and crossed with the northern SKR period around March 1, 2010, at around 10.67 hours. The northern period increased from about 10.58 hours to that convergence point.

 

Seeing this kind of crossover led the Cassini scientists to go back into data from previous Saturnian visits. With a new eye, they saw that NASA's Voyager data taken in 1980, about a year after Saturn's 1979 equinox, showed different warbles from Saturn's northern and southern poles. They also saw a similar kind of effect in the Ulysses radio data between 1993 and 2000. The northern and southern periods detected by Ulysses converged and crossed over around August 1996, about nine months after the previous Saturnian equinox.

 

Cassini scientists don't think the differences in the radio wave periods had to do with hemispheres actually rotating at different rates, but more likely came from variations in high-altitude winds in the northern and southern hemispheres.

 

Two other papers involving Cassini investigators were published in December, with results complementary to the radio and plasma wave science instrument - one by Jon Nichols, University of Leicester, and the other led by David Andrews, also of University of Leicester. 

 

In the Nichols paper, data from the NASA/ESA Hubble Space Telescope showed the northern and southern auroras on Saturn wobbled back and forth in latitude in a pattern matching the radio wave variations, from January to March 2009, just before equinox. The radio signal and aurora data are complementary because they are both related to the behavior of the magnetic bubble around Saturn, known as the magnetosphere. 

 

The paper by Andrews, a Cassini magnetometer team associate, showed that from mid-2004 to mid-2009, Saturn's magnetic field over the two poles wobbled at the same separate periods as the radio waves and the aurora.

 

As the sun continues to climb towards the north pole of Saturn, Gurnett's group has continued to see the crossover trend in radio signals through Jan. 1, 2011. The period of the southern radio signals continued to decrease to about 10.54 hours, while the period of the northern radio signals increased to 10.71 hours.

 

"These papers are important in helping to explain the complicated dance between the sun and Saturn's magnetic bubble, something normally invisible to the human eye and imperceptible to the human ear," said Marcia Burton, a Cassini fields and particles scientist at NASA's Jet Propulsion Laboratory.



The image top of page: NASA/ESA's Hubble Space Telescope from early 2009 features Saturn with the rings edge-on and both poles in view, offering a stunning double view of its fluttering auroras. credit: NASA/ESA/STScI/University of Leicester. Image credit: NASA/ESA/STScI/University of Leicester

 
 
HR

#5597 From: Buddy Lortie <alortie4@...>
Date: Mon May 14, 2012 5:43 pm
Subject: OT: New blog - Who Let the Dog Out?
neversurrender8
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Not sure if promoting this is a no-no here, but its a another look at the Pluto demotion ...
 
My blog this week focuses on the fact that I’m getting dumber every day.
 
Oh, its not because of a faltering memory, wiseasses, but because The-Powers-That-Be keep changing the damn rules!
 
 
Art Lortie, a fan of Underdog, as well

#5598 From: hexagram14@...
Date: Tue May 15, 2012 9:48 pm
Subject: Solar eclipse this weekend!
happy_rasta
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NASA Science News for May 15, 2012

On  Sunday, May 20th, the Moon will pass in front of the Sun, producing an
annular  solar eclipse visible across the Pacific side of Earth from China
to the United  States.

FULL STORY:
http://science.nasa.gov/science-news/science-at-nasa/2012/15may_sunday/

VIDEO: http://www.youtube.com/watch?v=7YX2blo1eRk

HR

#5599 From: hexagram14@...
Date: Fri May 18, 2012 12:01 am
Subject: And the most profitable asteroid is...
happy_rasta
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With the recent announcement of the asteroid mining company, Planetary
Resources, some of the most-asked questions about this enticing but complex
endeavor include, what asteroids do we mine? Which are the easiest asteroids
to  get to? Could it really be profitable?

While Planetary Resources officials said they hope to identify a few
promising targets within a decade, the initial answers to those questions are
available now on a new website that estimates the costs and rewards of mining
rocks in space. Called Asterank, the website uses available data from
multiple  scientific sources on asteroid mass and composition to try and compute
which  asteroids would be the best targets for mining operations.


So, which  asteroids are most profitable, valuable, easily accessible and
cost  effective?

The winners are, according to Asterank:

Most  Profitable: 253 Mathilde, a 52.8 km-diameter C-type (carbonaceous)
asteroid that  has an estimated value of over $100 trillion and estimated
profit of $9.53  trillion (USD)

Most Cost Effective: 2000 BM19, a very small O-type asteroid (less than  1
km wide) that makes several close approaches to Earth. Its estimated value
is  $18.50 trillion and an estimated profit of $3.55 trillion.

Most Valuable: 253 Mathilde (see above)

Most Accessible: 2009  WY7, another small asteroid with regular close
approaches of less than 1 AU.  This is an S-type asteroid, a silicaceous or
“stony
” object that has a high  accessibility score on Asterank of 7.6577.


Asterank combines both the  economic and scientific features of over
580,000 asteroids in our solar system,  looking specifically for platinum-group
metals and water. It was created by Ian  Webster, a software engineer in the
San Francisco Bay Area.

“I’ve always  had a strong interest in astronomy and especially space
exploration,” Webster  said via an email to Universe Today. “The
commercialization of space through  ventures like asteroid mining really excites
me
because I believe it’ll open  space to the rest of us and improve human
quality of
life. My day job is at a  startup unrelated to space, but my hobbies
include building rockets and many  side projects like this one. I have a lot of
fun applying computer science in  different ways and I hope that Asterank will
educate and inspire people.”

more:
http://phys.org/news/2012-05-profitable-asteroid.html

HR

#5600 From: hexagram14@...
Date: Fri May 18, 2012 10:40 pm
Subject: Cassini Titan Flyby: Looking at Lakes Again
happy_rasta
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Cassini Titan Flyby (T-83): Looking at Lakes Again

May. 22, 2012

Radar uses synthetic aperture radar (SAR, a technique which uses that
spacecraft's flight path to simulate a very large radar aperture) to
detect changes in small lakes seen on the T-16
<http://saturn.jpl.nasa.gov/mission/flybys/titan20060722/> and T-19
<http://saturn.jpl.nasa.gov/mission/flybys/titan20061009/> flybys. There
is some overlap with territory expected to be seen in T-95, which is set
to take place in October 2013.

Other RADAR observations include inbound and outbound radiometry, high
synthetic aperture radar (HiSAR, a method like SAR that can be used when
the target is too far away or at the wrong angle for conventional SAR)
and altimetry, along with outbound scatterometry.

Inbound, the visible and infrared mapping spectrometer (VIMS) looks for
specular reflection on the Northern lakes and also looks to detect
clouds to monitor climatic changes after the equinox. The imaging
science subsystem (ISS) rides along with VIMS' and the composite
infrared spectrometer's (CIRS') observations to image Titan's surface
and atmosphere, including Adiri and the region where changes were
observed in Fall 2010.

With closest approach slightly in the dayside ionosphere, the dual
technique magnetometer (MAG) will be able to study the diffusion of the
external magnetic field at low altitudes and high solar zenith angles.

Titan Flyby at a Glance

Titan Flyby
May 22, 2012 [SCET)

Altitude
593 miles (955 kilometers)

Speed
13,000 mph (5.8 km/sec)
 
 
HR

#5601 From: hexagram14@...
Date: Mon May 21, 2012 4:22 pm
Subject: Cassini Significant Events 05/09/2012 - 05/15/2012
happy_rasta
Send Email Send Email
 

Cassini Significant Events 05/09/2012 - 05/15/2012

 

The most recent spacecraft tracking and telemetry data were collected on May 15 using the Deep Space Network's 70 meter Station 14 at Goldstone, California. Aside from the issues in work with the Ultrastable Oscillator (see the Jan. 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health with all its subsystems operating normally. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

As the spacecraft proceeded out toward apoapsis, Magnetospheric and Plasma Science (MAPS) observations again made in-situ measurements of Saturn's outer magnetosphere and magnetosheath at low latitude, which means near Saturn's equatorial plane where the spacecraft is currently orbiting. These observations continued through Monday. Interspersed with these activities, the Imaging Science Subsystem (ISS) led the pointing for the optical remote sensing instruments to take repeated measurements of Titan this week to monitor cloud formations at different phase angles and distances.

 

 

Wednesday, May 9 (DOY 130)

 

Part 2 of the 10-week S73 background sequence was uplinked through the Deep Space Network (DSN) to the spacecraft today; its 7649 commands were confirmed aboard after one round-trip light time of 2 hours, 27 minutes.

 

 

Thursday, May 10 (DOY 131)

 

Negotiations for DSN antenna allocations to support the ten-week S74 sequence that is in work were completed for the first six weeks of the sequence. Work also continued on the ten-week sequences S75, S76, and S77.

 

 

Friday, May 11 (DOY 132)

 

Cassini's orbit count incremented to 166 with apoapsis passage at 2.4 million kilometers from Saturn (about twice the distance of Titan's orbit) going 5,488 kilometers per hour with respect to the planet.

 

S73 Part-2 commands began controlling the spacecraft.

 

ISS observed Saturn's moon Erriapus for 8 hours. This dark body is less than 10 kilometers in diameter, and orbits the planet once each 871 days at a distance of more than 17 million kilometers from Saturn.

 

 

Saturday, May 12 (DOY 133)

 

After approval of the maneuver and the command file, Orbit Trim Maneuver (OTM) 321 was uplinked to the spacecraft.

 

Realtime commands were sent to the spacecraft that will power the Cosmic Dust Analyzer (CDA) back on this Tuesday.

 

 

Sunday, May 13 (DOY 134)

 

Five optical navigation images were taken of Rhea against the background stars.

 

OTM 321 successfully turned the spacecraft and fired the main engine, providing 8.3 meters per second delta-V. This brought Cassini onto the planned trajectory for the Titan T-83 flyby at 955 kilometers above its surface on May 22.

 

 

Monday, May 14 (DOY 135)

 

The Magnetometer executed a sensor-offset calibration by rotating the spacecraft about its X axis.

 

The Ultraviolet Imaging Spectrograph began a series of observations that will continue over the next several days, with the Visible and Infrared Mapping Spectrometer, ISS, and the Composite Infrared Spectrometer riding along, to study Saturn's aurora by performing a mixture of slews and fixed pointings at the auroral oval.

 

 

Tuesday, May 15 (DOY 136)

 

The CDA power-on commands executed, and the instrument began operating normally.

The Cassini Plasma Spectrometer team updated some of its instrument's parameters by realtime command using the automated sequence processor.

 

HR


#5602 From: hexagram14@...
Date: Mon May 21, 2012 7:58 pm
Subject: Cassini Spots Tiny Moon, Begins to Tilt Orbit
happy_rasta
Send Email Send Email
 

Cassini Spots Tiny Moon, Begins to Tilt Orbit
Jet Propulsion Laboratory
May 21, 2012

NASA's Cassini spacecraft made its closest approach to Saturn's tiny
moon Methone as part of a trajectory that will take it on a close flyby
of another of Saturn's moons, Titan. The Titan flyby will put the
spacecraft in an orbit around Saturn that is inclined, or tilted,
relative to the plane of the planet's equator. The flyby of Methone took
place on May 20 at a distance of about 1,200 miles (1,900 kilometers).
It was Cassini's closest flyby of the 2-mile-wide (3-kilometer-wide)
moon. The best previous Cassini images were taken on June 8, 2005, at a
distance of about 140,000 miles (225,000 kilometers), and they barely
resolved this object.

Also on May 20, Cassini obtained images of Tethys, a larger Saturnian
moon that is 660 miles (1,062 kilometers) across. The spacecraft flew by
Tethys at a distance of about 34,000 miles (54,000 kilometers).

Cassini's encounter with Titan, Saturn's largest moon, on May 22, is the
first of a sequence of flybys that will put the spacecraft into an
inclined orbit. At closest approach, Cassini will fly within about 593
miles (955 kilometers) of the surface of the hazy Titan. The flyby will
angle Cassini's path around Saturn by about 16 degrees out of the
equatorial plane, which is the same plane in which Saturn's rings and
most of its moons reside.

Cassini's onboard thrusters don't have the capability to place the
spacecraft into orbits so inclined. But mission designers have planned
trajectories that take advantage of the gravitational force exerted by
Titan to boost Cassini into inclined orbits. Over the next few months,
Cassini will use several flybys of Titan to change the angle of its
inclination, building one on top of the other until Cassini is orbiting
Saturn at around 62 degrees relative to the equatorial plane in 2013.
Cassini hasn't flown in orbits this inclined since 2008, when it orbited
at an angle of 74 degrees.

This set of inclined orbits is expected to provide spectacular views of
the rings and poles of Saturn. Further studies of Saturn's other moons
will have to wait until around 2015, when Cassini returns to an
equatorial orbit.

"Getting Cassini into these inclined orbits is going to require the same
level of navigation accuracy that the team has delivered in the past,
because each of these Titan flybys has to stay right on the money," said
Robert Mitchell, Cassini program manager at NASA's Jet Propulsion
Laboratory, Pasadena, Calif. "However, with nearly eight years of
experience to rely on, there's no doubt about their ability to pull this
off."

Cassini discovered Methone and two other small moons, Pallene and Anthe,
between the orbits of Mimas and Enceladus between 2004 and 2007. The
three tiny moons, called the Alkyonides group, are embedded in Saturn's
E ring, and their surfaces are sprayed by ice particles originating from
the jets of water ice, water vapor and organic compounds emanating from
the south polar area of Enceladus.

The Cassini-Huygens mission is a cooperative project of NASA, the
European Space Agency and the Italian Space Agency. JPL manages the
mission for the agency's Science Mission Directorate in Washington. The
California Institute of Technology in Pasadena manages JPL for NASA.
 


For more information on the Cassini mission, visit:
http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov .

 
HR

#5603 From: hexagram14@...
Date: Fri May 25, 2012 4:08 pm
Subject: Cassini Significant Events 05/16/2012 - 05/22/2012
happy_rasta
Send Email Send Email
 

Cassini Significant Events 05/16/2012 - 05/22/2012

 

The most recent spacecraft tracking and telemetry data were collected on May 23 using the Deep Space Network's 70 meter Station 14 at Goldstone, California. Aside from the Ultrastable Oscillator (see the Jan. 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health with all its subsystems operating normally. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

This week's highlight was the Titan encounter (T-83), which included acquiring another high-resolution Synthetic Aperture Radar (SAR) image strip about 6,000 kilometers long. Among ongoing observations in the days before Tuesday morning's encounter, the Ultraviolet Imaging Spectrograph (UVIS) continued its series of observations, with the Visible and Infrared Mapping Spectrometer (VIMS), the Imaging Science Subsystem (ISS), and the Composite Infrared Spectrometer (CIRS) riding along, to study Saturn's aurora with slews and fixed pointings at the auroral oval.

 

 

Wednesday, May 16 (DOY 137)

 

Today, as on nearly every day, the Realtime Operations Team sent commands to reset the command-loss timer, which is one of several fault-protection programs running aboard the spacecraft.

 

The Radio Science Subsystem performed periodic instrument maintenance activities on the Radio Frequency Instrument Subsystem.

 

 

Thursday, May 17 (DOY 138)

 

Today and the next day, ISS led the pointing with CIRS and VIMS also taking measurements in the Titan Monitoring Campaign, watching cloud formations at different phase angles and ranges.

 

 

Friday, May 18 (DOY 139)

 

Commands were sent to overlay telemetry-rate commands in the S73 sequence. This was necessary because Deep Space Network (DSN) antenna allocations were incomplete even as S73 began executing last month. Other command data sent to Cassini made a "live" update to the Inertial Vector Propagator to refine pointing directions for Saturn's satellite Methone. Finally, commands were sent that would perform Orbit Trim Maneuver (OTM) 322 the next day.

 

 

Saturday, May 19 (DOY 140)

 

Nearing periapsis, the Cassini Plasma Spectrometer (CAPS) led spacecraft pointing for Magnetospheric and Plasma Science (MAPS) measurements of the equatorial inner magnetosphere.

 

OTM-322, the T-83 approach maneuver, executed during its backup window. This was a reaction control subsystem thruster burn with a duration of 73.5 seconds, providing approximately 83 millimeters per second delta-V. The maneuver was delayed to the backup window to allow orbit determination solutions more time to converge.

 

 

Sunday, May 20 (DOY 141)

 

There were three major observing campaigns today. First came high spatial resolution optical studies of Tethys, the third major moon out from Saturn. CIRS took the lead in mapping its leading hemisphere to confirm the previously detected thermal anomaly, to determine thermal surface properties inside and outside of the anomaly, and to characterize the anomaly's shape and spatial extent. The higher daytime temperatures provided enough signal for CIRS to use its FP3 (focal-plane 3) high spatial resolution detector. The CIRS scans allowed ISS and VIMS to mosaic the surface to contribute to a global map of the moon; UVIS rode along to measure variations in Tethys' albedo across its surface.

 

Going 68,460 kilometers per hour relative to Saturn while viewing Tethys, Cassini passed through periapsis just outside the orbit of Mimas, the innermost of Saturn's major satellites.

 

ISS then viewed the tiny moon Methone, for which new pointing vectors were uplinked Friday. This close flyby, less than 2,000 kilometers, offered the first opportunity to characterize Methone's geology, to obtain compositional information, and to understand the relationship of the moon to Saturn's ring system. Its orbit lies about 8,500 kilometers outside that of Mimas.

 

Finally, CAPS took control and turned Cassini to an attitude that allowed optimal measurements of ions and electrons in Saturn's inner magnetosphere. These observations were taken in parallel with higher time resolution measurements by all the MAPS instruments. These latter observations, performed roughly every six months on equatorial orbits, are for the purpose of studying long-term solar cycle and seasonal variability in Saturn's magnetosphere. They are also used to investigate magnetospheric periodicities and their coupling to the ionosphere.

 

 

Monday, May 21 (DOY 142)

 

The image "Serene Scene" with Saturn and Tethys was featured here today:

 

http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4527.

 

Cassini pointed the Optical Remote Sensing instruments to the growing disk of Titan to start conducting many observations, which are detailed on the T-83 encounter page (see below).

 

 

Tuesday, May 22 (DOY 143)

 

During the Titan encounter today, the spacecraft rotated repeatedly about all three axes to aim its telescopes, point the large dish antenna for Radar observations, and expose in-situ instruments in desired directions. For closest approach, attitude control switched from reaction wheels to thrusters for increased control authority over atmosphere-generated torques around closest approach. Full information may be found here on the T-83 encounter page:

 

http://saturn.jpl.nasa.gov/mission/flybys/titan20120522/.

 

By flying closely over Titan's north pole, gravity enabled an "elastic collision" connecting Cassini with some of Titan's orbital momentum. The result of this gravity-assist flyby increased the inclination of the spacecraft's orbit plane from near-equatorial (0.4 degrees) to 15.8 degrees. This is the first of eight gravity-assisted steps that will bring Cassini's inclination to a maximum of 61.7 degrees above the equatorial plane about a year from now. More information on the inclined orbits, and on Methone, may be found here:

 

http://saturn.jpl.nasa.gov/news/cassinifeatures/feature20120521/.

 

The DSN's 70 meter aperture stations in Madrid, Spain, and Goldstone, California, captured every bit of telemetry that was stored on the solid-state recorders during T-83, while providing Doppler and ranging data for navigation. At the same time, both stations participated in an Operations Readiness Test (ORT) preparing for an upcoming Radio Science ring and atmosphere occultation experiment, which is possible to do now that Cassini's orbital plane has been rotated somewhat out of the ring plane. Cassini's S-band (2 GHz), X-band (8 GHz), and Ka-band (32 GHz) transmissions were received during the ORT.

 

 

 HR


#5604 From: theophanes raptis <t_raptis2005@...>
Date: Fri May 25, 2012 4:47 pm
Subject: Σχετ: [Cassini Huygens] Cassini Significant Events 05/16/2012 - 05/22/2012
t_raptis2005
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Theophanes Raptis   
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Division of Applied Technologies, R & D Unit   NCSR Demokritos  
Ag. Paraskevi, Attikh, Greece  153 10 
tel      : +30 210 6514544/6511020 (secr)  
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Skype: raptis.theophanes
http://cag.dat.demokritos.gr/raptis.php 
e-mail:rtheo@... /  t_raptis2005@...
Strength & Honor
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~  


Απο: "hexagram14@..." <hexagram14@...>
Προς: cassinihuygens@yahoogroups.com
Στάλθηκε: 7:08 μ.μ. Παρασκευή, 25 Μαΐου 2012
Θεμα: [Cassini Huygens] Cassini Significant Events 05/16/2012 - 05/22/2012

 
Cassini Significant Events 05/16/2012 - 05/22/2012
 
The most recent spacecraft tracking and telemetry data were collected on May 23 using the Deep Space Network's 70 meter Station 14 at Goldstone, California. Aside from the Ultrastable Oscillator (see the Jan. 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health with all its subsystems operating normally. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.
 
This week's highlight was the Titan encounter (T-83), which included acquiring another high-resolution Synthetic Aperture Radar (SAR) image strip about 6,000 kilometers long. Among ongoing observations in the days before Tuesday morning's encounter, the Ultraviolet Imaging Spectrograph (UVIS) continued its series of observations, with the Visible and Infrared Mapping Spectrometer (VIMS), the Imaging Science Subsystem (ISS), and the Composite Infrared Spectrometer (CIRS) riding along, to study Saturn's aurora with slews and fixed pointings at the auroral oval.
 
 
Wednesday, May 16 (DOY 137)
 
Today, as on nearly every day, the Realtime Operations Team sent commands to reset the command-loss timer, which is one of several fault-protection programs running aboard the spacecraft.
 
The Radio Science Subsystem performed periodic instrument maintenance activities on the Radio Frequency Instrument Subsystem.
 
 
Thursday, May 17 (DOY 138)
 
Today and the next day, ISS led the pointing with CIRS and VIMS also taking measurements in the Titan Monitoring Campaign, watching cloud formations at different phase angles and ranges.
 
 
Friday, May 18 (DOY 139)
 
Commands were sent to overlay telemetry-rate commands in the S73 sequence. This was necessary because Deep Space Network (DSN) antenna allocations were incomplete even as S73 began executing last month. Other command data sent to Cassini made a "live" update to the Inertial Vector Propagator to refine pointing directions for Saturn's satellite Methone. Finally, commands were sent that would perform Orbit Trim Maneuver (OTM) 322 the next day.
 
 
Saturday, May 19 (DOY 140)
 
Nearing periapsis, the Cassini Plasma Spectrometer (CAPS) led spacecraft pointing for Magnetospheric and Plasma Science (MAPS) measurements of the equatorial inner magnetosphere.
 
OTM-322, the T-83 approach maneuver, executed during its backup window. This was a reaction control subsystem thruster burn with a duration of 73.5 seconds, providing approximately 83 millimeters per second delta-V. The maneuver was delayed to the backup window to allow orbit determination solutions more time to converge.
 
 
Sunday, May 20 (DOY 141)
 
There were three major observing campaigns today. First came high spatial resolution optical studies of Tethys, the third major moon out from Saturn. CIRS took the lead in mapping its leading hemisphere to confirm the previously detected thermal anomaly, to determine thermal surface properties inside and outside of the anomaly, and to characterize the anomaly's shape and spatial extent. The higher daytime temperatures provided enough signal for CIRS to use its FP3 (focal-plane 3) high spatial resolution detector. The CIRS scans allowed ISS and VIMS to mosaic the surface to contribute to a global map of the moon; UVIS rode along to measure variations in Tethys' albedo across its surface.
 
Going 68,460 kilometers per hour relative to Saturn while viewing Tethys, Cassini passed through periapsis just outside the orbit of Mimas, the innermost of Saturn's major satellites.
 
ISS then viewed the tiny moon Methone, for which new pointing vectors were uplinked Friday. This close flyby, less than 2,000 kilometers, offered the first opportunity to characterize Methone's geology, to obtain compositional information, and to understand the relationship of the moon to Saturn's ring system. Its orbit lies about 8,500 kilometers outside that of Mimas.
 
Finally, CAPS took control and turned Cassini to an attitude that allowed optimal measurements of ions and electrons in Saturn's inner magnetosphere. These observations were taken in parallel with higher time resolution measurements by all the MAPS instruments. These latter observations, performed roughly every six months on equatorial orbits, are for the purpose of studying long-term solar cycle and seasonal variability in Saturn's magnetosphere. They are also used to investigate magnetospheric periodicities and their coupling to the ionosphere.
 
 
Monday, May 21 (DOY 142)
 
The image "Serene Scene" with Saturn and Tethys was featured here today:
 
 
Cassini pointed the Optical Remote Sensing instruments to the growing disk of Titan to start conducting many observations, which are detailed on the T-83 encounter page (see below).
 
 
Tuesday, May 22 (DOY 143)
 
During the Titan encounter today, the spacecraft rotated repeatedly about all three axes to aim its telescopes, point the large dish antenna for Radar observations, and expose in-situ instruments in desired directions. For closest approach, attitude control switched from reaction wheels to thrusters for increased control authority over atmosphere-generated torques around closest approach. Full information may be found here on the T-83 encounter page:
 
 
By flying closely over Titan's north pole, gravity enabled an "elastic collision" connecting Cassini with some of Titan's orbital momentum. The result of this gravity-assist flyby increased the inclination of the spacecraft's orbit plane from near-equatorial (0.4 degrees) to 15.8 degrees. This is the first of eight gravity-assisted steps that will bring Cassini's inclination to a maximum of 61.7 degrees above the equatorial plane about a year from now. More information on the inclined orbits, and on Methone, may be found here:
 
 
The DSN's 70 meter aperture stations in Madrid, Spain, and Goldstone, California, captured every bit of telemetry that was stored on the solid-state recorders during T-83, while providing Doppler and ranging data for navigation. At the same time, both stations participated in an Operations Readiness Test (ORT) preparing for an upcoming Radio Science ring and atmosphere occultation experiment, which is possible to do now that Cassini's orbital plane has been rotated somewhat out of the ring plane. Cassini's S-band (2 GHz), X-band (8 GHz), and Ka-band (32 GHz) transmissions were received during the ORT.
 
 
 HR



#5605 From: hexagram14@...
Date: Thu May 31, 2012 9:03 pm
Subject: Crossing the Sun: The Last Transit of Venus until 2117
happy_rasta
Send Email Send Email
 
Next week will be the last opportunity this  century to see the planet
Venus as a little black dot moving across the solar  disk--a rare event with a
long, important history in astronomy.

On June 5  in the Americas and June 6 in the rest of the world, people will
be able to see  one of the rarest predictable events in astronomy: a solar
transit of the planet  Venus. Over a six-hour period the disk of Venus will
be silhouetted against the  sun. Seeing it safely requires a special
eye-protection filter, available for a  dollar or so—alternately, a telescope
or
binoculars can safely project an image  onto a wall or sheet of paper. But if
you miss it, your next chance won't come  until the year 2117.

Every century or so, the relative orbital motions of  Earth and Venus bring
them into perfect alignment with the sun, producing a pair  of transits
separated by eight years. Only six transits have been observed in  history: in
1639; 1761 and 1769; 1874 and 1882; and 2004. Observing them was  once the
"noblest problem in astronomy" (as an English Astronomer Royal put it),
because until the 20th century it was the only way to determine the distance
from Earth to the sun. Hundreds of expeditions went as far north and as far
south as possible to make giant triangles with Venus and thereby maximize the
  precision of the measurement. The most famous was probably Captain Cook's
voyage  to Tahiti in 1769.

Transits have lost none of their capacity to surprise  astronomers. At the
time of the 2004 event, nobody alive had seen one. I  remember watching it
on images streaming back from NASA spacecraft. When Venus  was about halfway
onto the sun's edge, the planet’s atmosphere became visible,  bending
sunlight toward us. This unexpected phenomenon has led us to plan  worldwide
observations of Venus's atmosphere during the upcoming event. We  should be able
to detect a dimming of the sun by a tenth of a percent as Venus  blocks that
much of the sun's disk. Our view should help researchers  interpreting
Venus's atmosphere with the European Space Agency's Venus Express  spacecraft.
In addition, it provides ground truth for the Kepler spacecraft's
observations of exoplanetary transits around other  stars.

more:
http://tinyurl.com/2012-Venus-transit


HR

#5606 From: hexagram14@...
Date: Thu May 31, 2012 10:10 pm
Subject: Enceladus Plume is a New Kind of Plasma Laboratory
happy_rasta
Send Email Send Email
 
 
JPL/NASA News

News release: 2012-149                                                                     May 31, 2012

Enceladus Plume is a New Kind of Plasma Laboratory

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.cfm?release=2012-149&cid=release_2012-149

PASADENA, Calif. – Recent findings from NASA’s Cassini mission reveal that Saturn’s geyser moon Enceladus provides a special laboratory for watching unusual behavior of plasma, or hot ionized gas. In these recent findings, some Cassini scientists think they have observed “dusty plasma,” a condition theorized but not previously observed on site, near Enceladus.

Data from Cassini’s fields and particles instruments also show that the usual “heavy” and “light” species of charged particles in normal plasma are actually reversed near the plume spraying from the moon’s south polar region. The findings are discussed in two recent papers in the Journal of Geophysical Research.

“These are truly exciting discoveries for plasma science,” said Tamas Gombosi, Cassini fields and particles interdisciplinary scientist based at the University of Michigan, Ann Arbor. “Cassini is providing us with a new plasma physics laboratory.”

Ninety-nine percent of the matter in the universe is thought to be in the form of plasma, so scientists have been using Saturn as a site other than Earth to observe the behavior of this cloud of ions and electrons directly. Scientists want to study the way the sun sends energy into Saturn's plasma environment, since that jolt of energy drives processes such as weather and the behavior of magnetic field lines. They can use these data to understand how Saturn's plasma environment is similar to and different from that of Earth and other planets.

The small, icy moon Enceladus is a major source of ionized material filling the huge magnetic bubble around Saturn. About 200 pounds (about 100 kilograms) of water vapor per second – about as much as an active comet – spray out from long cracks in the south polar region known as “tiger stripes.” The ejected matter forms the Enceladus plume – a complex structure of icy grains and neutral gas that is mainly water vapor. The plume gets converted into charged particles interacting with the plasma that fills Saturn’s magnetosphere.

The nature of this unique gas-dust-plasma mixture has been revealed over the course of the mission with data from multiple instruments, including the Cassini plasma spectrometer, magnetometer, magnetospheric imaging instrument, and the radio and plasma wave science instrument. What scientists found most interesting is that the grains range continuously in size from small water clusters (a few water molecules) to thousandths of an inch (100 micrometers). They also saw that a large fraction of these grains trap electrons on their surface. Up to 90 percent of the electrons from the plume appear to be stuck on large, heavy grains.

In this environment, Cassini has now seen positively charged ions become the small, “light” plasma species and the negatively charged grains become the “heavy” component. This is just the opposite of “normal” plasmas, where the negative electrons are thousands of times lighter than the positive ions.

In a paper published in the December issue of the journal, a team of Swedish and U.S. scientists on the Cassini mission examined radio and plasma wave science instrument observations from four flybys of Enceladus during 2008. They found a high plasma density (both ions and electrons) within the Enceladus plume region, although the electron densities are usually much lower than the ion densities in the plumes and in the E ring. The team concluded that dust particles a hundred millionth to a hundred thousandth of an inch (a nanometer to micrometer) in size are sweeping up the negatively charged electrons. The mass of the observed “nanograins” ranges from a few hundred to a few tens of thousands of atomic mass units (proton masses), and must therefore contain tens to thousands of water molecules bound together. At least half of the negatively charged electrons are attached to the dust, and their interaction with the positively charged particles causes the ions to be decelerated. Because the dust is charged and behaves as part of the plasma cloud, this paper distinguishes this state of matter from dust that just happens to be in plasma.

“Such strong coupling indicates the possible presence of so-called ‘dusty plasma’, rather than the ‘dust in a plasma’ conditions which are common in interplanetary space,” said Michiko Morooka from the Swedish Institute of Space Physics, lead author of the paper and a Cassini radio and plasma wave science co-investigator. “Except for measurements in Earth’s upper atmosphere, there have previously been no in-situ observations of dusty plasma in space.”

In a dusty plasma, conditions are just right for the dust to also participate in the plasma’s collective behavior. This increases the complexity of the plasma, changes its properties and produces totally new collective behavior. Dusty plasma are thought to exist in comet tails and dust rings around the sun, but scientists rarely have the opportunity to fly through the dusty plasma and directly measure its characteristics in place.

A separate analysis, based on data obtained by the Cassini plasma spectrometer, revealed the presence of nanograins having an electric charge corresponding to a single excess electron. “The Cassini plasma spectrometer has enabled us to discover and analyze new classes of charged particles that were wholly unanticipated when the instrument was designed and built in the 1980s and 90s,” said Tom Hill, the study’s lead author and a co-investigator based at Rice University in Houston.

The nature of the Enceladus plume has been revealed over time due to the synergistic nature of the fields and particles instruments on Cassini, which has been in residence in Saturn’s magnetosphere since 2004. Following the original detection of the plume based on magnetometer measurements, Sven Simon from the University of Cologne, Germany, and Hendrik Kriegel from the University of Braunschweig, Germany, found that the observed perturbation of Saturn’s magnetic field required the presence of negatively charged dust grains in the plume. These findings were reported in the April and October 2011 issues of Journal of Geophysical Research Space Physics. Previous data obtained by the ion and neutral mass spectrometer revealed the complex composition of the plume gas, and the cosmic dust analyzer revealed that the plume grains were rich in sodium salts. Because this scenario can only arise if the plume originated from liquid water, it provides compelling evidence for a subsurface ocean.

Cassini will continue to study the complex nature of the plume region in the three planned additional flybys of Enceladus. The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington. More Cassini information is at http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov .

Jia-Rui C. Cook 818-354-0850
Jet Propulsion Laboratory, Pasadena, Calif.
jccook@...


- end -



HR

#5607 From: hexagram14@...
Date: Thu May 31, 2012 10:14 pm
Subject: Cassini Significant Events 05/23/2012 - 05/29/2012
happy_rasta
Send Email Send Email
 

Cassini Significant Events 05/23/2012 - 05/29/2012

 

The most recent spacecraft tracking and telemetry data were collected on May 30 by the Deep Space Network's 34 meter Station 15 at Goldstone, California. Aside from the Ultrastable Oscillator (see the Jan. 5, 2012 Significant Events), the Cassini spacecraft is in an excellent state of health with all its subsystems operating normally. Information on the present position of the Cassini spacecraft may be found on the "Present Position" page at: http://saturn.jpl.nasa.gov/mission/presentposition/.

 

Cassini began a year-long phase, starting with the Titan flyby on May 22, during which Titan flybys will continue to increase the spacecraft's orbital inclination. Periapses will continue coming about as close to Saturn as the broad E ring. This plan is designed to provide opportunities for ring occultation experiments by Radio Science and the Ultraviolet Imaging Spectrograph (UVIS), as well as optical remote sensing observations of the rings.

 

The Imaging Science Subsystem (ISS) performed three observations in the ongoing Satellite Orbit Campaign this week, measuring positions of small satellites to improve knowledge of their orbits. ISS, the Composite Infrared Spectrometer (CIRS), and the Visible and Infrared Mapping Spectrometer (VIMS) performed two observations in the Titan monitoring campaign.

 

Negotiations to schedule Deep Space Network (DSN) antennas to support Cassini's S74 sequence, which goes active June 18, are proving difficult due to contentions related to Mars Science Laboratory's requirements for support during atmospheric entry, descent, landing, and initial surface operations early this August.

 

 

Wednesday, May 23 (DOY 144)

 

The Navigation Team took five images for optical navigation purposes.

 

ISS, CIRS, UVIS and VIMS performed a joint observation of the faint D and G rings at low phase angle.

 

 

Thursday, May 24 (DOY 145)

 

The Cosmic Dust Analyzer (CDA) performed a 5 hour measurement of interstellar dust.

 

Using the Automated Sequence Processor, the Cassini Plasma Spectrometer team sent commands that reconfigured their ion beam spectrometer settings to adapt the instrument to current environmental conditions.

 

ISS and VIMS telemetry processing halted because of erroneously set flags in data from the DSN regarding earth-receive times. A labor-intensive workaround was devised so that processing can continue while this ground-based anomaly is resolved. The Instrument Operations team initiated Incident-Surprise-Anomaly report (ISA) #52211 to document the problem.

 

 

Friday, May 25 (DOY 146)

 

ISS observed the star Vega for 15 hours to perform a photometric calibration.

 

 

Saturday, May 26 (DOY 147)

 

CDA performed a 13.5 hour interstellar dust observation.

 

 

Sunday, May 27 (DOY 148)

 

Station 25, one of the DSN's 34 meter diameter antennas at Goldstone, California, participated in an Operations Readiness Test (ORT) preparing for the Radio Science ring and atmosphere occultation experiment on June 4.

 

The Magnetometer Team performed an instrument calibration by rolling the spacecraft about its Z-axis during DSN communications with the high-gain antenna pointed to Earth.

 

 

Monday, May 28 (DOY 149)

 

Cassini passed apoapsis at about 2.3 million kilometers from Saturn, having slowed to 5,771 kilometers per hour relative to the planet.

 

CDA took advantage of the spacecraft's distance from Saturn to perform another 13.5 hour interstellar dust observation.

 

An image titled "Splitting Titan" was featured on the Cassini website, illustrating seasonal atmospheric changes in Titan's northern and southern hemispheres. The image may be seen at: http://saturn.jpl.nasa.gov/photos/imagedetails/index.cfm?imageId=4536 .

 

 

Tuesday, May 29 (DOY 150)

 

ISS spent 11 hours observing the irregular moon Ymir. The tiny dark body is in a retrograde orbit 23 million kilometers from Saturn.

 

Station 25 participated in another Radio Science ORT preparing for the June 4 experiment.

 

Orbit Trim Maneuver 324, a 21.4 second maneuver using the main engine, was performed just before midnight, targeting to the Titan encounter on June 7. It provided a delta-V of 3.71 m/s.

 

 HR


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