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Tanya Harrison

CTX and MARCI -- The OTHER Cameras on Mars Reconnaissance Orbiter

Posted by Tanya Harrison

25-01-2010 19:45 CST

Topics: Mars, Mars Reconnaissance Orbiter

The following was written for The Planetary Society Blog by Tanya Harrison. Tanya is on the science operations team for NASA's Mars Reconnaissance Orbiter (MRO) Context Camera (CTX) and Mars Color Imager (MARCI) at Malin Space Science Systems. She selects targets for, and then analyzes the geology of CTX images, and is one of the writers for the weekly MARCI weather reports. I'm grateful to Tanya for this contribution, since I've been doing a terrible job covering the terrific images coming out of all of Mars Reconnaissance Orbiter's cameras. --ESL


"What?" you might say, "There are cameras other than HiRISE?"

Yes indeed, there are. There are two other cameras aboard MRO: the Context Camera (CTX) and Mars Color Imager (MARCI). CTX acquires grayscale images at a resolution of about six meters per pixel covering areas up to 9,390 square kilometers in one picture. MARCI acquires color images (in seven wavelength bands) at 1 to 10 kilometers per pixel to create a daily global mosaic of Mars in order to monitor the weather. Today, I'm just going to talk about CTX. 

Comparison of CTX, HiRISE, and MOC NA image footprints

NASA / JPL / MSSS / Tanya Harrison

Comparison of CTX, HiRISE, and MOC NA image footprints
CTX, HiRISE, and MOC are three cameras that have provided high-resolution images of Mars. This diagram compares their typical footprint sizes across Ius and Tithonium Chasmata, Mars. Each camera's design makes different trades among resolution and areal extent. MOC on Mars Global Surveyor acquired long, skinny strips at about 6 meters per pixel. CTX on Mars Reconnaissance Orbiter provides images of the same resolution, but covering a much larger area. HiRISE, also on Mars Reconnaissance Orbiter, can take much higher resolution images at about 0.3 meters per pixel, but covers a proportionally smaller area. The base map to this image is the Viking Orbiter MDIM or global mosaic.

Maybe CTX is neglected because of its name. It sounds like all it does is take context images for HiRISE (and CRISM, the imaging spectrometer on Mars Reocnnaissance Orbiter), but that's not the case. CTX's almost 10,000-square-kilometer pictures makes it well-suited to create mosaics of large regions. For example, we have nearly complete coverage of the entire Valles Marineris canyon system; we have nearly half of the planet covered in total. CTX has also already covered 12 percent of the planet in stereo and produced mosaics of the entire south polar cap in both winter and summer so scientists could monitor how it recedes.

CTX also monitors (that is, repeatedly images) several locations on Mars for changes or activity such as new impact craters, gully flows, dust devils, wind streaks, dune movement, and slope streaks. This monitoring has paid off, as we've found over 80 new impact sites, noticed a plethora of new slope streaks, and documented thousands of gully locations. But some of the most exciting things we've found thanks to our monitoring efforts are multiple new gully flows, first reported at the 41st Division of Planetary Sciences meeting in Puerto Rico last October.

Martian middle- and high-latitude gullies were first observed in Mars Global Surveyor Mars Orbiter Camera (MOC) images in 1999. Appearing to be geologically young, they were repeatedly imaged by MOC to determine whether they were changing. This led to identification of two sites where new flows occurred between 1999 and 2005, including this one in Terra Sirenum:

New gully deposit in Naruko Crater, Mars (flicker animation)

NASA / JPL / MSSS / Emily Lakdawalla

New gully deposit in Naruko Crater, Mars (flicker animation)
This animation flickers between two Mars Orbiter Camera views of a gully in Naruko Crater in Terra Sirenum, Mars. The two images were captured in December 2001 and April 2005, and show that, between those two dates, liquid water flowed down the gully and left a light-toned deposit. The movement of other features in the image is due to the different points of view obtained by Mars Global Surveyor on the sloped crater wall in the two observations.

These features generated a lot of buzz because the deposits were thought to have formed through a mechanism involving liquid water, as gullies appear to be fluvial features. Now, CTX continues the MOC gully monitoring effort, routinely imaging over 600 locations (craters, massifs, pits, etc.) to look for changes in gullies. We compare new CTX images to all pre-existing datasets of sufficient resolution (including MOC, HiRISE, Mars Express HRSC, Mars Odyssey THEMIS VIS, and previous CTX coverage). When a change is suspected, we then direct HiRISE to its location for higher-resolution imaging.

With this monitoring effort, we have found nine more of these types of features where there are images of the gully channels both before and after the flows formed. All of them formed since 2001. For some, we have before-and-after images that constrain their formation dates to within a one-year range. Many of these, such as the example pictured below, are even better demonstrations of how the formation of these features likely involves liquid water than the two flows reported in 2006.

A new gully flow in Pursat Crater

NASA / JPL / MSSS / UA / annotated by Tanya Harrison

A new gully flow in Pursat Crater
These images explore the southwest wall of Pursat, an 18-kilometer-diameter crater in Mars' southern highlands. The leftmost image was taken by Mars Reconnaissance Orbiter CTX in February 2008 (P16_007185_1425_XN_37S228W). The center image shows the same location as seen one Earth year later (B06_011958_1425_XN_37S229W). During the time separating the two images, a new light-toned flow appeared in the crater wall. The rightmost panel contains a view of the new flow feature as seen by HiRISE in March, 2009 (ESP_012380_1425). The flow exhibits a number of features characteristic of debris flows: evidence for the flow traveling around obstacles, for ponding of the flow in topographic depressions, for the flow overtopping those depressions and spilling over, for raised deposits on channel banks, for braiding of the flow bed where it meets the lower slope of the crater floor, long runout onto the crater floor, and lobate ends of the flow deposit.

In addition to gully monitoring, we document the locations of every gullied landform on the surface of Mars as the CTX images come down from the spacecraft each day (yes, it's as incredibly tedious as it sounds, as CTX has acquired over 25,000 images thus far in the MRO mission!). So far, MOC and CTX combined have covered about half of Mars. In that area, we've imaged over 4,500 separate gullied landforms (craters, massifs, mesas, etc.) -- that means tens of thousands of individual gullies. In Nirgal Vallis alone there are about 500 individual gullies! This documentation effort has confirmed that gullies are only found in one latitude strip in each hemisphere, from about 27 to 80 degrees north and also from 27 to 80 degrees south.

Some authors have claimed that there are gullies in the equatorial regions as well, but those landforms are not "gullies" in the sense that they lack incised channels. The equatorial features are dry mass movement chutes with alcoves and aprons. While the original definition of a gully given by Malin and Edgett in 2000 consisted of an alcove, channel, and apron, many gullies lack alcoves and/or aprons, and therefore the channel is the key identifier. CTX is capable of resolving over 95% of the gullies on Mars; serendipitously, gullies don't appear to occur in extremely small craters (less than a few hundred meters in diameter), so unless the gully channels are incredibly fine or partially obscured by something like dunes, CTX can pick them out.

I'll leave you with some CTX eye candy of just a few of these tens of thousands of gullies on Mars. If you'd like to browse CTX images, some of them plot on Mars in Google Earth, and there is also a map interface available here. The number-and-letter codes underneath each image take you to a page where you can browse the full CTX photo.

Start exploring!

Gullies in Nigral Vallis

NASA / JPL / MSSS

Gullies in Nigral Vallis
Mars Reconnaissance Orbiter Context Camera (CTX) view of gullies in Nirgal Vallis. This image was acquired on November 4, 2007. The full image can be viewed here.
Gullies and dunes in the Nereidum Montes

NASA / JPL / MSSS

Gullies and dunes in the Nereidum Montes
Mars Reconnaissance Orbiter Context Camera (CTX) image of gullies and dunes in the Nereidum Montes, the steep mountains north of the massive Argyre impact basin. The full CTX image can be viewed here.
Gullies in Asimov Crater

NASA / JPL / MSSS

Gullies in Asimov Crater
Mars Reconnaissance Orbiter Context Camera (CTX) view of gullies in Asimov Crater in Noachis Terra. The full CTX image can be viewed here.
Gullied crater in Terra Cimmeria

NASA / JPL / MSSS

Gullied crater in Terra Cimmeria
Mars Reconnaissance Orbiter Context Camera (CTX) view of an unnamed gullied crater in Terra Cimmeria, near 39.1°S, 200.7°W. The full CTX image can be viewed here.
 
See other posts from January 2010

 

Or read more blog entries about: Mars, Mars Reconnaissance Orbiter

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