An exciting new paper came out in yesterday’s issue of Science magazine, with HiRISE team member Shane Byrne as the lead author. Water ice has been discovered being exposed by fresh Martian craters!

This is exciting for several reasons: first, these are very tiny craters – only a few meters (yards) across. This means they’re not excavating very deep into the crust of Mars. So the ice has to be really shallow – less than a few feet below the surface! Secondly, the location of these craters is surprising – they’re between 40-55 degrees north latitude. This is far from the polar regions, where we’d expect to find ice (for example, where the Phoenix mission landed at 68 degrees north, ice was found by digging down into the dirt).

The third exciting aspect of this ice is its purity. We’d expect this ice to be mixed in with dirt and dust and rock. Instead, we found that it’s 99% pure ice! (Only 1% is dirt mixed in.) This can be measured because we watched the ice disappear over time. By taking repeated images of the same spot, HiRISE got a time sequence as the ice slowly faded. It faded so slowly that it has to be almost all ice – a dirtier mixture would have faded much faster as it sublimated (went directly from a solid to a gas) in Mars’s extremely dry atmosphere.

Speaking of dry atmospheres, this also has interesting implications about the history of the Martian climate – there had to have been more water vapor in the atmosphere in the recent past than we previously thought. We still have lots of questions about how this ice formed, how much of it there is, and how many more of these craters we’ll find. Luckily, we’ve got a long mission ahead of us to explore these issues!

This discovery is also a great example of how the instruments on MRO work together. CTX initially detected these new craters as “dark spots,” and HiRISE followed up to confirm that they’re really impact craters. Some of those HiRISE images revealed some very bright white material, and then CRISM confirmed that material really is water ice. The instruments worked together to accomplish the best combined science. Go team! ☺

Here are some more detailed stories, images, and multi-media:

• Really nice movie with Shane Byrne talking about the discovery and excellent animations showing the locations of the craters and the time-evolution of the ice disappearing: NASA multimedia – then go to “Video Gallery” on the right, and click on “Mars – Exposed”.

• NASA press release, and all of the images and materials from the press conference

• UA news story

We’ve seen many more news stories & blogs – thanks for the interest, everyone! It’s great that everyone thinks this is as exciting as we do! ☺

You might remember that we were planning on releasing HiRISE images to the public on a monthly basis. That plan was delayed by issues with our processing software, hardware and other events. A productive summer working on these issues culminated last week with one of our larger releases of Mars images!  Here are some statistics about our September 2009 release, which includes the images the HiRISE camera took of the Martian surface between Mars Reconnaissance Orbiter (MRO) orbits 12,600 to 14,199, or roughly April 4 through August 6, 2009:

• 2,996 RDRs, 1 TB
• 42,370 EDRs, 1 TB
• 34,481 RDR Extras, 1.6 TB
• 83,784 EDR Extras, 0.02 TB
• 636 Anaglyphs, 0.01 TB

Totals for this release: 163,631 image products, 3.6 TB

This brings our total released product numbers and data volume to:

• 22,676 RDRs, 12 TB
• 317,120 EDRs, 10.4 TB
• 192,270 RDR Extras, 15.3 TB
• 612,769 EDR Extras, 0.1 TB
• 2,892 Anaglyphs, 0.5 TB

Total: 1,148,363 images, 37.5 TB

In summary, we released nearly 1500 observations, most of those with both black & white and color RDR products. Several newer observations matched up with older observations from a slightly different angle of the same location on the surface, resulting in 636 awesome new anaglyphs. The RDRs are the fully processed, geometrically projected products best for scientific inquiry. If you really want to, though, anyone can download and process HiRISE data from scratch. You can do this using ISIS software, which is publicly available for free download. See the ISIS Web site for download information, processing instructions, and tutorials.

Starting this week, I will be looking over the observations taken August 6 through August 26 before MRO went into safe mode and make sure they are ready for release. We plan to release these images in early October. We are also in the process of reprocessing those Extended Science Phase mission images prior to all the latest processing pipeline fixes and updates.  Once we are satisfied with that data set, we will release them to the public and then start reprocessing the images from the Primary Science Phase…a major project that should keep me and the rest of Downlink busy for several months!

Originally posted at Spaced Out (Again):

We are going to try to Twitter a planning cycle for the HiRISE (http://hirise.lpl.arizona.edu) experiment. The idea is to give people a feeling of all the work we have to do to get images from Mars out of a very special piece of equipment. Here are a couple of things you need to know to follow what is going on.

The scientist in charge of the scientific support for the cycle is called the CIPP. For cycle 75, that is @nick_space. Nick will be assisted by his Post-Doc., Anya, who is @mozhetbyt

The targeting specialist ensures that the plan produced can be implemented and keeps the CIPP from doing anything stupid. The targeting specialist is called the HiTS and for cycle 75 that is @laughingrid.

The HiRISE project has its own Twitter account (@HiRISE) which can also be followed.
We will try to use #hitwycle as a search hashtag for tweets.

(more…)

The HiRISE team met up this summer in Whitefish, Montana. In between meetings, we were also able to take several geologic field trips and hikes. Glacier National Park has many cool (haha) glacial features, of course, and we also learned about some interesting sedimentology that occurred in the ancient geologic past. The patterns we saw in the sedimentary rocks are similar to those discovered by the Mars Opportunity Rover – cross-bedding and festooned ripples that form when sand is laid down under a body of water. The shape and direction of the ripples can tell you how much water was present, how fast it was flowing, and whether it was a river, a lake, or an ocean. These are important questions we’d like to answer about the history of water on Mars.

The park also has wonderful examples of glacial geology. HiRISE has taken images of many features thought to be related to glaciers, so it’s important to understand the terrestrial analogs that lead scientists to think these are evidence of flowing ice on Mars. For example, we hiked along a moraine composed of jumbled rocks the Grinnell Glacier left behind as it flowed downhill. In addition to the remains of the (rapidly disappearing) glacier itself, we also saw typical glacial erosional structures such as U-shaped valleys, hanging valleys, and cirques. For a HiRISE image of cirque-like features, see PSP_005730_1405.

On one of our field trips, we were accompanied by reporter Michael Jamison of The Missoulian. This story was on the front page of the paper the following day:

“Martians invade Glacier – Mars scientists visit park to study, compare rocks.”

I thought the story was really good – a quirky (but so are we!) description of why we would want to stare at the rocks in such a magnificent setting, and their relevance to our mission to Mars. We all thought it was funny when he called Alfred McEwen, our Principle Investigator, a “Marsman”!

HiRISE Team in Glacier National Park, in front of a classic U-shaped valley carved by glacial erosion.

We were pleased to welcome Linda Ronstadt (!!!) to the HiRISE Operations Center last week. We gave her and a few of her friends & family a presentation about the HiRISE mission, and we showed them some of our images in false color, 3-D and on the HiWall. Linda was incredibly nice and enthusiastic, and she had lots of great questions for us. Turns out rock stars love HiRISE! At least, we hope she enjoyed it as much as we did!

It’s summer again in the southern hemisphere of Mars, so we’re continuing our mosaic of the landing ellipse for the lost Mars Polar Lander. ESP_013368_1035 was the first of the new images to be released, and we’ve gotten a lot of people asking where to send their candidates. You can either contact us directly, or add to the comments in our previous blog post about the search.

The Unmanned Spaceflight forums have a long discussion on the previous search efforts. Many candidates were proposed, and the community’s discussion about them is quite enlightening.

Emily Lakdawalla at the Planetary Society also started a coordinated search effort last year. I don’t know if that effort is still ongoing, but her page on how to use HiRISE images in the search is still a great resource. It includes examples of known hardware, cosmic ray hits and other artifacts, and more tips on searching.

In addition to the list of images on the previous blog entry, these new images have been released: (we’ll try to keep this list up to date as more are released)

• ESP_013368_1035
• ESP_013078_1030
• ESP_013223_1025
• ESP_013289_1035
• ESP_013566_1025
• ESP_013500_1035
• ESP_013711_1030
• ESP_013724_1030
• ESP_013935_1030
• ESP_013790_1035
• ESP_014001_1040
• ESP_014080_1040

Thanks for all your interest, and good luck searching!

9/2/09: ETA new images released in September PDS release.

Planetary scientists used to keep new data from the spacecraft explorers of the solar system within the mission team for a lengthy period of time so they could make all the cool initial discoveries. Only later would the mission’s data sets be archived on the public Planetary Data System (PDS). Once archived, these data could then be used by the scientific community and public for further research and discovery.

Dr. Alfred McEwen, HiRISE principal investigator, decided early on that this incredibly powerful instrument should be “The People’s Camera”. This meant, among other things, that we would endeavor to make the data returned by HiRISE available to the scientific community and public as quickly as possible. We have PDS release requirements, but our goal has always been to beat those requirements. To do so, we needed to develop automated software pipelines to take the raw data and turn them into useful calibrated and geometrically mapped products. We also needed to develop the right PDS release tools, train a talented group of operations staff to validate the data and fix problems, and develop a website to effectively and beautifully showcase HiRISE images.

We now believe we have reached the point to be able to support a monthly release of recent HiRISE images to the public! This week we released the observations HiRISE took of Mars between orbits 11,600 and 12,599, or between January 16 and April 04, 2009. This makes us the first mission to release a data set to the PDS so quickly! Here are the statistics for this release, including the number of each product type released and their respective data volumes (EDRs are the individual uncalibrated image channels and RDRs are the calibrated, mosaicked, and geometrically-projected observations):

• 1,179 RDRs, 520 GB
• 16,861 EDRs, 459 GB
• 13,512 RDR Extras, 788 GB
• 33,152 EDR Extras, 7 GB
• 342 Anaglyphs, 51 GB

Totals for this release: 64,704 image products, 1.7 TB

This brings our total released product numbers and data volume to:

• 19,667 RDRs, 11 TB
• 278,807 EDRs, 9.5 TB
• 166,816 RDR Extras, 13.7 TB
• 529,095 EDR Extras, 0.1 TB
• 2,892 Anaglyphs, 0.5 TB

Total: 993,277 images, 34 TB

Those are various products for about 9998 Mars observations, and another reason why it makes no sense to hoard our data; there is too much of it and too few of us! The team scientists have plenty to do and there are plenty of discoveries to be made, old hypotheses to update, and new mysteries to solve.  The operations staff are now hard at work getting observations from orbits 12,600 through 12,999, or between April 04 and May 5, 2009, ready for the June PDS release. This involves making sure each observation has been processed by our software pipelines correctly, fixing any problems, and checking and double checking that the relevant image products are ready for release.  Sometimes we have to manually force an observation through the pipelines because some of its channels were lost during transmission to the Earth, or we might stumble across an observation we somehow forgot to send on to the color pipelines after it had been calibrated. There are spreadsheets to maintain, lists of problematic observations to keep (see the ERRATA.TXT file), and a variety of other tasks that need to be completed before the latest data set is ready for release.

Over the next few months we will see how this goes! It is a lot of work, but our desire for you to see these beautiful images of Mars as quickly as possible is strong. No promises, but we will also explore releasing completed observations even faster!

New feature on the HiRISE website! HiFlyers made of released images like this one:

These are 11×17 PDFs showing cutouts of new releases, so you can print your own posters. Currently these are available for weekly releases starting 3/25/09 – look for more with each week’s new images!

They’re all available on this page. There are also links to the flyers on the individual image pages such as this one: http://hirise.lpl.arizona.edu/ESP_011425_1775 (Look for the “HiFLYER” link in the lower right hand side.)

Enjoy!

If you are anything like me, then you spent a lot of time with the planets as a kid.  Growing up in the 1980s was amazing because of the Voyager spacecrafts. I was always hunting for the latest images from Uranus and Neptune in the daily newspaper and in magazines, so I could cut them out and paste them into my scrapbook. At the same time I was impatient for another mission to Mars.

Back then it was common to hear that there were probably few if any planets around other stars, unlike in the movies. The limited evidence for the existence of exoplanets suggested to some scientists that planet-making was a difficult process, and that our home star was unique in all the galaxy.  Now we know this is not the case.  Exoplanets are everywhere! Although the detection technologies we use today are biased to huge Jupiter-sized or bigger exoplanets close to their parent stars, the rapid pace of exoplanetary discovery suggests that planetary formation is in fact widespread.  Detection technology is also improving so that we can start exploring other regions around stars. Might there be planets in habitable zones around other stars, the same zone around the Sun we find our own watery, pleasant, life-covered Earth?

Last Friday, the Kepler spacecraft was successfully launched to begin a multi-year mission to look for just those types of planets.  Kepler will observe thousands of stars, looking for extremely slight variations in brightness that may indicate transits, or events where planets move in front of their parent star from the spacecraft’s viewing perspective. The detector on board the spacecraft is so powerful that it could possibly detect Earth-like planets in Earth-like orbits around distant stars.

As an operations specialist on a Mars-related mission, I cannot say that I am “bored” with our solar system.  On the contrary, in a galaxy with trillions of planets, might not our own planets be like snowflakes, unique unto themselves? What I can say is that missions like Kepler keep expanding, and confirming, my interest in planetary science! Meanwhile, Mars keeps surprising us, suggesting that exoplanets will also be unique and complex targets for further exploration. Is it possible to have too much of a good thing? In planetary science, the answer is a resounding “No!” Best success to Kepler and its team!

Image credit: Kepler Mission website – “Target Region in Milky Way (2)“

Using the HiRISE camera to take a special observation of a non-Mars target is a difficult but always interesting event for HiRISE Operations. While we have developed somewhat of a routine for regular imaging of the Martian surface, special observations require additional work that impacts our normal workflow as well as the science gathering of the other instruments onboard the Mars Reconnaissance Orbiter. Targeting specialists from Uplink already have so much work to do on a routine basis; adding in a special observation adds that much more work. Special observations are selected because they offer some scientific value that warrants the extra time, effort, and delay in routine science gathering.

We do not accept requests from the public directly regarding special observations.  Our very knowledgeable science team determines months in advance that the right geometry for a unique observation of a non-Mars target with scientific value is coming up. Over several iterations between Uplink and the science team, the target is planned in detail. For a target like Deimos, the smaller and more distant moon of Mars, the spacecraft needs to slew away from Mars to point the camera correctly. This is a dance that requires coordination between HiRISE, the other instruments (who will generally not be observing during this period), and the MRO platform.

For this opportunity,  we took two images of Deimos. The plan was to capture Deimos in the center of our CCD array so that the satellite would fall across our RED, BG, and IR color filters.  Uplink did a fantastic job with their targeting!  In the first observation – ESP_012065_9000 – Deimos lay across two channels of each color filter at the center of our array: RED4_0 and RED5_1, BG12_0 and BG13_1, and IR10_0 and IR11_1.  In the second observation – ESP_012068_9000 – Deimos was fully contained within RED5_1, BG13_1, and IR11_1. You can find more information about these observations here.

What did it take for Downlink to put these images together?  Well, Audrie and I came in on a Sunday (!) to wait for the observations.  Then I spent some time putting together preliminary images to send out to the team. During the following week I worked on registering the color filters to create the false color images.  See both images side by side here. Notice that green fringe around the first observation on the left? That is a bit of misregistration, something I could not seem to correct despite tweaking the position of the three color layers a pixel at a time. The first observation also required two separate stacks: (1) RED4_0, BG12_0, and IR10_0, and (2) RED5_1, BG13_1, and IR11_1.  After registering the two sides separately, I stitched them together using an ISIS tool called hiccdstitch.  That little notch you see at the top of the first observation is how the two sides almost but not quite line up. The two sides are slightly offset because their geometry is just slightly different.

Compared to the first observation, the second observation, confined to one channel each in the color filters, was wonderful to work with: no color balancing required, no stitching, and a relatively easy registration process!

GuyMac also helped make these Deimos observations a little easier to deal with than past special observations: he created a custom version of one of our processing pipelines that sharpens the image and brings out the colors a little bit. Once I had the observations registered, all I had to do was run them through his script for the really nice false color products you are now enjoying!