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A helo flight to prepare for next year

Posted on July 23rd, 2010 by Marc Seibert

On the way back from Kelly Lake, we swung by Pavilion Lake to take some shots of the live sub operations underway. This is a very beautiful part of the world.

Next year the team will be diving into a lake called Kelly Lake, and potentially Pavilion Lake at the same time.  This creates a challenge for the communications team.  Both sites must have broadband access to the Space Network Research Federation (SNRF) and the Internet, and be able to communicate from site to site at all times.

Satellite connectivity is great, but in this environment the “terrain mask” (steep rise of the terrain all around us) makes it difficult to hit a satcom “bird” in the sky from these high northern latitudes.  On top of this, satellite transponder time can be expensive (especially considering the amount of “megahertz” or transponder we need!), and adds a significant “latency” to the communications link (in both directions) because the satellites are orbiting so far above the Earth.  This latency can cause problems for some of the operations conducted by this team, and terrestrial interfaces tend to have very low latency.

We took a Trackstick with us in the helicopter, and you can see the path we flew here (thanks to Google Earth!)

So we took off in a helicopter in Lillooet, and flew to Kelly Lake to visit and survey the terrestrial (ground/mountain-based) communications options for communications near the lake.  If we can avoid using a satcom link, we’ll have greater bandwidth and network performance at the 2011 test operations.

We found several options for connectivity or relay on a few mountains surrounding Kelly Lake, and even some options to link the two lakes together for next year’s mission.  This begins a year’s worth of planning “now”.  ; )

- Marc

Pavilion Lake, looking south

One of the DeepWorker chase boats, looking south.

Pavilion Lake Research Project: Wrapping up 2010

Posted on July 20th, 2010 by Allyson Brady

The PLRP 2010 field season has come to a close and I am both saddened by the fact that operations are finished for another year but excited by the prospect of adding the data we’ve collected this year to our growing body of knowledge about this unique lake. I am in awe of the work that has been done by this amazing team and of how much we’ve grown, while maintaining the sense of adventure and camaraderie that to me, helps to define the PLRP.

We’ve taken great strides towards answering many of our research questions and in the process, with every answer we have come up with many more questions that will keep the PLRP team occupied for quite some time. Fortunately, our family continues to grow and every year we welcome new individuals who bring a unique perspective and desire to tease out the mysteries Pavilion has to offer. We have also been blessed this year by the addition of two little members to the PLRP family, Darlene Lim’s daughter Amelia and Greg Slater’s son Joseph. We look forward to the day when they are exploring the lake alongside us.

DeepWorker Pilots and Nuytco Team: 2010

The PLRP provides a wealth of research opportunities, and not just those focused on understanding the processes leading to the formation of the structures at Pavilion Lake but also to understanding fundamental biological, chemical and physical processes. The research contributions from our participating scientists and graduate students have resulted in a number of recent publications and are essential to increasing our understanding of Earth and astrobiological systems. We’re very proud of the role that the PLRP has played in developing operational technologies and protocols that not only help us meet our science objectives but provide important input into future space science missions.

With the addition of our two newest scientist pilots, astronauts Chris Hadfield and Stan Love, we had 34 DeepWorker missions over 10 days of operations. This year we were aided greatly in our pre-season flight planning by the wonderful team from NASA Ames led by Matt Deans and David Lees who developed an amazing flight planning tool that enabled us to search images and flight paths from previous years while building flight plans in Google Earth. Flights this year were planned to collect images of the remaining unexplored regions of the lake, to record detailed images of areas of interest identified from 2008 and 2009 data and to use the submersibles in combination with other analytical tools such as a conductivity, temperature and depth (CTD) instrument and our autonomous underwater vehicle(s) (AUV). Our ability to review post-flight video data in the field, an effort pioneered in 2009, added greatly to our productivity as this information was used immediately by the science backroom team to modify existing flight plans to best optimize our data collection. As part of the daily flight debriefs, we have also continued to apply metrics associated with scientific productivity to understand factors that influence scientific exploration. New this year to the DeepWorker flight repertoire were long ~ 5 hour flights and two night flights to investigate the grazing activity that we suspect may occur in the lake. To add to the innovations this year, Nick Wilkinson designed a fantastic, interactive program for use in classifying the microbialite images. This new tool will allow us to efficiently organize and process our field data over the coming months. Stay tuned for updates.

The Amazing Pavilion Lake Research Project Team: 2010!

In case our DeepWorker operations didn’t keep us busy enough, we had a number of other important activities included in the field schedule this year. The UBC and University of Delaware AUV teams produced fantastic images of the lake bottom that were often used to compliment the DeepWorker flights and give us a better picture of where interesting structures and features are in the lake. Numerous SCUBA dives were performed by our intrepid team of divers to collect water and microbialite samples that were shared between various research groups in an effort to combine and compliment analytical findings. These samples will be characterized from a virology, microbial lipid, isotopic and genetic point of view to provide more information about the role of biology in the formation of the microbialites and what biosignatures may be left behind. Water samples were collected from nearby lakes including Crown, Turquoise, Pear and Kelly Lake to continue to help us put Pavilion Lake in context. Kelly Lake, which also hosts microbialites and has been an area of interest to the PLRP team for many years, was also the focus of significant AUV activities this year. Microbial mats were once again collected from the Cariboo Plateau lakes and giant pancakes were eaten by all (well, almost all). As a new participatory activity this year, our visiting teacherswere given the task of selecting a SCUBA dive based on their understanding of the research questions of interest (on their first day no less!). I’m happy to report that they eagerly interviewed members of the team before presenting their selected dive and rationale to the group for inclusion in the next day’s diving schedule. Community Day was another great success this year with the team happy to show off our work and answer questions from the many visitors we had to the site. Busy indeed!

We plan on continuing our updates throughout the year as we analyze samples and work through the amazing amount of data that were collected. Thanks to all who have read about our activities and through this process, have joined in our adventure. See you next year!

~ Allyson

Dr. Love’s Underwater Blog, Part 5

Posted on July 12th, 2010 by Stanley Love

What a week it has been!  Today is the last of my six full days here at Pavilion Lake, and it feels like we’ve done a month’s worth of work.  Days begin with breakfast at 7 am and a team meeting at 7:30, and conclude with science debriefs that often end at 10 or 11 pm.  The pace is not quite as fast and relentless as a Shuttle flight…but it’s close.  It’s one more way in which Pavilion Lake is a good analog for an actual space flight.  (Differences include the excellent food and, on the rare occasions when time permits, being able to go fo a long jog with fresh air and lovely mountain scenery!)

Stan preparing for flight in DeepWorker

With two more “flights” in the Deepworker submarine under my belt since last I wrote, I’ve gotten a lot more familiar with the machine.  Although the miniature submarine looks nothing like a space suit, there are a lot of similarities.  And someday, when humans visit near-Earth asteroids or other objects with very low surface gravity, I expect they’ll do their spacewalks in something that looks a lot more like a Deepworker than a traditional person-shaped space suit. Here’s why.  A small asteroid has such weak gravity that even the slightest nudge with a hand or foot would send a spacewalking astronaut soaring high above the surface, and it might take hours to come back down.  A stronger shove might send an astronaut away at a speed higher than the escape velocity, in which case gravity would not bring them back ever!  Not so good.  On the International Space Station, which of course has no noticeable gravity of its own, astronauts keep from floating away by holding on to special handrails.  Asteroid do not come equipped with handrails.  They do have rough surfaces which might provide hand- and foot-holds, but unfortunately most asteroids are not solid blocks of material.  Instead they are “rubble piles,” flying clumps of sand, gravel, and boulders held together not by material strength, but by their own weak self-gravity.  So if you were moving hand-over-hand across the surface of the asteroid and accidentally pushed yourself off on a suborbital trajectory, you could grab onto a rock to keep yourself down–and the rock would simply come away with you! The practical result is that hands and feet are probably not the best way to move around an asteroid.  Better might be a suit with tiny thrusters that you could use to maneuver yourself around the landscape.  But if you’re not using your hands and feet to move around like a person climbing a tree, there’s no need to enclose them in a flexible suit.  Instead, you could keep them inside a hard pressure shell where they could be used to control thrusters, manipulators, and onboard systems.  Such an arrangement might look a lot like a Deepworker.  As a side benefit, the operator might be a bit more comfortable than in a traditional space suit.

Stan and DeepWorker 7.

Our underwater work here at Pavilion Lake ends this afternoon.  I’ll be the pilot for one of the last two “flights.”  The flight planner, Dr. “Mars” Marinova (who was just recently awarded her Ph.D. from the Geological and Planetary Sciences division at Caltech, where I worked as a postdoc more years ago than I care to admit), set up an especially interesting flight plan for me.  I’ll visit one of the “deep mounds,” outcroppings of microbialites growing on isolated boulders on the otherwise rather flat and monotonous central floor of the lake.  Then I’ll head off to do some vertical transects along the western shore.  These transects begin in deep water, then move upslope through the depth zone where the microbialite population is richest.  As I fly the transects I’ll record video of what I see from the submarine, and keep a running monologue (also recorded on board) of my observations.  It should be a lot of fun…and I’m sure I’ll miss piloting the submarines when the field season ends.
This wraps up Dr. Love’s Underwater Blog.  If I’m fortunate enough to be able to participate here next field season and spend more quality time underwater, I’ll be sure to reactivate the blog.
-Stan

Pavilion Lake and Beyond: How to Effectively Explore Other Worlds?

Posted on July 7th, 2010 by Mike Gernhardt

Mike Gernhardt with the DeepWorker barge in the background

This is my third year as a submarine pilot/scientist on the Pavilion Lake Research Project (PLRP) and it is really exciting and informative to be part of this team and to watch the progression and trends in the science and operational methods that are being applied to this expedition.  I originally became involved in the PLRP because of the use of the dual DeepWorker submersible system as an operational analog to the dual Lunar Electric Rover system that my team at NASA is developing.  The really special thing about PLRP is that it’s not a simulation, its real world-class science and the methods that we use to plan the flights collect and analyze the data, and the lessons we learn are directly relevant to future space exploration. It’s also pretty cool that we are seeing things that human eyes have never seen before and in that sense it’s analogous to finding life on Mars or some other planet.

Mike Gernhardt and Bill Todd (front) work as CapCom on the surface vehicle, while Steve Wittig (back) captains the nav boat

The main contributions of our NASA Exploration Analogs and Mission Development team (EAMD) are to perform the operational research necessary to characterize the productivity and effectiveness of the operation and then systematically analyze the data and use the results to refine the operational methods over a multi-year period with the aim of achieving the highest level of scientific return from the human and machine assets deployed during the expedition.  To this end we have developed a variety of metrics that characterize the data, and observation quality along with the operational performance and timeline data.  These metrics are then correlated with the scientific merit metrics that we have developed with the PLRP team to understand the right balance between operational discipline and scientific flexibility. Is the right answer going to be totally rigid flight plans and flight rules to control every minute or the exploration dives, or complete scientific flexibility to explore whatever seems most interesting at the time? Probably neither,  the optimal mix is most likely  somewhere in between and this multi-year research program provides a unique opportunity to find that optimal mix here on earth so that we don’t have to learn those lesson out in space were the expense and consequences are much higher.

-Mike

Mike Gernhardt, ready for deployment in DeepWorker.

Exploring the Herms: Bekah Shepard

Posted on July 6th, 2010 by Bekah Shepard

Magical! Driving a sub through the “herms” of Pavilion Lake is absolutely magical! Imagine this: a snow of particulates streaks around the dome. A yellow light permeates the water column as it filters through the planktonic cloud and bounces through the Chara. Microbialites rise up from the bottom like castles shrouded in a mist of microalgae. The natural world is like poetry to an observational scientist, and a dive in the herms is high art. Of course, to someone who studies the shapes and forms of microbialites (like I do), a dive in the herms is also like candy! Microbialites cover up to 90 percent of the lake bottom, and exhibit a variety of different shapes in a space of only a few meters. For a microbialite scientist – Yum!

View from the pilot's seat.

Today I was lucky enough to pilot such a dive to the herms. The herms are an area near the center of Pavilion Lake. Their name is a bit of a misnomer – in fact, it is more of a nickname that stuck! Herms is short for bioherms, which refers to a build up of biological organisms, usually into a mound that rises above the surrounding sea or lake floor. Our Pavilion herms are mounds, but they are probably just sediment mounds that are covered in lots of microbialites, rather than being mounds build up exclusively by microbialites. Nevertheless, they remain a favorite area of the PLRP scientific team, because of the small area, dense ecology, and interesting geochemical and limnological environment.

My mission was to completely circumnavigate two of the herms that we had not mapped in previous years. Navigating the subs through an area of such dense mounds and interesting features has been challenging in the past. The topography can make communication between the surface and subs problematic, and our maps have not always been as accurate as they are now. However, as our research has continued, our knowledge of the area has improved, our communications infrastructure has grown by leaps and bounds, and I daresay, some of us are even getting better at flying these subs! I am proud to say that the circumnavigation went smoothly and we were able to fill in some missing areas in our maps of the herms!

Exploring the herms at 40 feet.

Improving our maps also means raising more questions; such is the nature of exploration, and this dive was no exception. Although many of the morphological trends that I observed were similar to those I have noticed before (adding strength to some of our hypotheses), new subtleties leapt into view. Why, for example, do many of the microbialites along the bottom of the mounds look roughed-up, slightly broken, whitish, and all together kind of crummy? Does it have to do with fluctuating sediment levels at the bases of the mounds? Perhaps. That leads me to questions of how precisely sediment is transported around the mounds: what is the source of the sediment? How often do large sediment flows come down from the surrounding walls? Are the microbialites buried and exposed regularly or does it happen on a timescale of decades or centuries!? For each answer there are new questions, and for each new question there are a handful of associated questions.

Returning to the surface to see a smiling Susan Winnitoy, guiding me back to the barge.

The abundance of new questions is thrilling, and is what keeps bringing us back here. I often find myself chatting with people who are surprised that we haven’t uncovered all of the details of microbialite formation, development, and growth – after all, we have been studying Pavilion Lake for a number of years. Yet that is the appeal of studying microbialites! Microbialite mounds are subject to nearly countless variables – biological, chemical, and physical processes that change through time. Untangling each of those influences is a process – a process that is being helped along by the phenomenal amount of data that we are collecting with the DeepWorker subs, with the GAVIA AUVs, and with our team of SCUBA divers. So, do we understand everything about microbialite formation yet? Nope. Not by far. But with dives like my magical one through the herms, we are getting ever closer! The microbialites of Pavilion Lake have a story to tell, and through our exploration we are listening to the telling.

- Bekah

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Pavilion Lake Research Project Operations Tour

Posted on July 5th, 2010 by Heather Paul

Learn about the PLRP’s operations, and tour the field site with Heather and Ben!

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Bekah looks at the highway-side of Pavilion Lake

Posted on July 2nd, 2010 by Ben Cowie

Bekah Shepard explores the highway side of the North Basin of Pavilion Lake. Click the wrench icon in the Google Earth plugin window to slow down the animation speed.

Download the KMZ file for your Google Earth software here: 20100629C

Ask a Scientist: What’s the Difference between an AUV and an ROV?

Posted on July 2nd, 2010 by Ben Cowie

Stephanie Nebel and Jonathan Gutsche answer an important distinction between two very different underwater vehicles! To ask your question, visit www.astrobio.net and search for the Pavilion Lake Research Project, or click this link: www.tinyurl.com/askplrp.

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Happy Canada Day! This blog rocks!

Posted on July 1st, 2010 by Mary Beth Wilhelm

Hello from Pavilion Lake and happy Canada Day!! My name is Mary Beth and I am one of the more junior members of the PLRP team. I am half way through my undergrad at Cornell University in New York and am an intern at NASA Ames Research Center in California.

I just arrived back to land a half hour ago after being out on the lake for over 6 hours! And while it was a lot of fun to be outside, I had to pull out my jacket that I only use during the winter in New York. It has been a very busy day as the PLRP team conducts a full suite of submersible, autonomous underwater vehicle, and SCUBA dive operations.

I had two major jobs today. The first was keeping a log of all of the science notes that sub pilots called up to the surface while following the sub in a boat that is equipped with walkie-talkies capable of communicating with the pilot while he was underwater. Astronaut Mike Gernhardt was piloting one of the subs today, conducting an extended 5 hour dive around the south basin. It was exciting to listen to all of Mike’s observations and discoveries in real time!

My second job today was taking rock samples for my own summer research project. I am investigating the role of rocks in the formation and morphology of microbialites. We think that microorganisms may prefer to start forming microbialites on solid surface substrates, like rocks, and our team has observed many microbialites throughout the lake that have formed on top of both really big and small rocks. Pilot Margarita imaged rock slides of interests in the DeepWorker subs on Monday, and after reviewing the data with the science team, we decided to revisit a few of these slides with divers to collect rocks to study. So, today I had pro divers Mike D. and Gary take a few rock samples every 10 ft. from a rock slide in the central basin that went from about 80 feet below the surface all the way up to the shore.

After collecting these samples, I will analyze them in our outdoor wet lab, recording basic physical observations and measurements, and looking for trends in the data that will help us understand how factors like size of the rock and depth may affect microbialite growth. Hopefully my observations will help elucidate factors that control microbialite growth on rocks and even give us more clues to how microbialites are first formed.

-MB

First flights of 2010 – Alex and Mars get underwater

Posted on June 29th, 2010 by Ben Cowie

I had the pleasure of being on board for the first launch of the 2010 field season. For this post, I’m going to let the photos speak for themselves.  You can view the rest of the photos from the day on Picasa here.

Enjoy, - Ben