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T48 and T49 RADAR Swaths |
Oct 2 2009, 01:43 AM
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#1
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![]() Senior Member ![]() ![]() ![]() ![]() Group: Moderator Posts: 3242 Joined: 11-February 04 From: Tucson, AZ Member No.: 23 |
The latest PDS release for Cassini is now online at http://pds-imaging.jpl.nasa.gov/data/cassi...assini_orbiter/
I've posted the RADAR swaths from T48 and T49 at http://pirlwww.lpl.arizona.edu/~perry/RADAR/ . These swaths include observations of the ISS playa, Tui Regio (yep, it does look a lot like Hotei Regio), Shikoku Facula, Belet, and the southern mid-latitudes. One image I want to highlight is from one of the T48 swaths. It covers northern Shikoku Facula. You can see a river channel running from a playa in the center of northern Shikoku east out to the margin between the Shangri-la dune fields and Shikoku. Very cool stuff. http://pirlwww.lpl.arizona.edu/~perry/RADA...koku_Facula.jpg -------------------- &@^^!% Jim! I'm a geologist, not a physicist!
The Gish Bar Times - A Blog all about Jupiter's Moon Io |
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Oct 2 2009, 02:32 AM
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![]() Senior Member ![]() ![]() ![]() ![]() Group: Moderator Posts: 2785 Joined: 10-November 06 From: Pasadena, CA Member No.: 1345 |
Very cool!
Thank you for hosting these! -------------------- Some higher resolution images available at my photostream: http://www.flickr.com/photos/31678681@N07/
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Oct 2 2009, 11:55 AM
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#3
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Senior Member ![]() ![]() ![]() ![]() Group: Members Posts: 3516 Joined: 4-November 05 From: North Wales Member No.: 542 |
Great stuff. What happens when the liquids meet the dunes is a crucial question with big implications - for relative timescales of active processes amongst many others. At first glance that dunefield looks to me like it's been attacked and partly erased by the liquid flow, perhaps in a sudden brief event??
In the T49 I noticed what could be a similar situation, though less well resolved. A stream seems to originate just above a possible crater remnant and flow off to the left, cutting through dunes at right angles. |
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Oct 2 2009, 03:36 PM
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#4
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
"I've posted the RADAR swaths from T48 and T49 at http://pirlwww.lpl.arizona.edu/~perry/RADAR/ .
Much thanks VP for the posting! The T48 and T49 swaths (especially the latter) jump around a bit and I've included a context map of the swaths modified from Spilker's presentation http://saturn.jpl.nasa.gov/files/20090728_...5yr_Spilker.pdf as the swaths are not labeled on the Perry SAR swath site overview map. |
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Oct 3 2009, 12:09 AM
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#5
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
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Oct 3 2009, 07:48 PM
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#6
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
There was overlap to the T49 playa swath and the T36 southern latitudes swath. As these were over a year apart and the overlap (-75S and85W) area was relatively near the lakes that had formed between 2004 and 2005 (see PIA11147) http://photojournal.jpl.nasa.gov/catalog/PIA11147 and were in the process of drying up I thought it might be worthwhile to look for changes. Looking at the overlap area it seems some variation relates to SAR viewing direction and swath resolution but also there may be changes related to playa drying up between T36 (10/2/07) and T49 (12/2/08). What do ya think!? (I know I'm probably all 'wet' on this one)
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Oct 3 2009, 09:34 PM
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#7
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Junior Member ![]() ![]() Group: Members Posts: 64 Joined: 11-October 05 Member No.: 525 |
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Oct 4 2009, 04:25 PM
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#8
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
Great stuff. What happens when the liquids meet the dunes is a crucial question with big implications - for relative timescales of active processes amongst many others. At first glance that dunefield looks to me like it's been attacked and partly erased by the liquid flow, perhaps in a sudden brief event?? Absolutely! Seeing changes over several years would also help answer a crucial 'timescale' question whether channels erase dunes or dunes cover channels. Looking at Shikoku over the time period 2006-2009 (click on graphic) seems to show no definitive changes in that regard. (main changes relate to SAR look angle and resolution). |
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Oct 7 2009, 09:57 AM
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#9
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![]() Senior Member ![]() ![]() ![]() ![]() Group: Moderator Posts: 3242 Joined: 11-February 04 From: Tucson, AZ Member No.: 23 |
I have added to the RADAR SAR page maps for the north and south poles (RADAR only). These are complete through T49:
North Pole Map South Pole Map -------------------- &@^^!% Jim! I'm a geologist, not a physicist!
The Gish Bar Times - A Blog all about Jupiter's Moon Io |
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Oct 7 2009, 12:18 PM
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#10
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Senior Member ![]() ![]() ![]() ![]() Group: Members Posts: 3516 Joined: 4-November 05 From: North Wales Member No.: 542 |
Those are brilliant! - at least the bits I could see before my computer blanked out half way through opening them. Could you please post versions at, say, 64 resolution?
EDIT: tried it at home and got the whole thing fine. |
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Oct 8 2009, 06:52 AM
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#11
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
Those are brilliant! - at least the bits I could see before my computer blanked out half way through opening them. Could you please post versions at, say, 64 resolution? Here's a combination of the S pole swaths VP has posted with the ISS map of the same. I've added some grid markers and swath labels. A very cool area appears at top where the T39 river and the T7 shoreline appear. As VP has mentioned in the changing lakes thread when the south pole wet season returns the Mezzoramia Basin that these 2 swaths relate to may be the big lake on Titan! |
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Oct 10 2009, 06:16 AM
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#12
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
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Oct 11 2009, 04:30 AM
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#13
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Member ![]() ![]() ![]() Group: Members Posts: 718 Joined: 1-April 08 From: Minnesota ! Member No.: 4081 |
From the T28 north polar swath an extensive river system is seen near 255W and 75N (see below). One SARTopo strip runs along the river and is shown in place on the map. The river runs approximately 375 km and from its upper tributaries to its lowest reaches there is a drop of around 500 m. This gives an overall gradient of 500 m/375km or 1.33 m per km or around 5 feet per mile, not much different from many terrestrial streams!
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Oct 11 2009, 04:38 AM
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#14
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Merciless Robot ![]() ![]() ![]() ![]() Group: Admin Posts: 8791 Joined: 8-December 05 From: Los Angeles Member No.: 602 |
That's almost literally fantastic! How odd to contemplate this...
-------------------- A few will take this knowledge and use this power of a dream realized as a force for change, an impetus for further discovery to make less ancient dreams real.
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