We had an incredibly successful test cruise of our new turbulence instrumentation last week. The team worked tirelessly to get the epsilometer working, and to design the new "epsi-fastCTD" vehicle up and running. All went well and now we can measure turbulence in several new, modular and flexible ways!
MOD graduate student extraordinaire successfully passed her qualifying exam this week. The last hurdle to the PhD besides actually writing the thesis!
Nice work Effie.
MOD is inspired by Mai Bui, who wanted to help after hurricane Harvey and took the simple - but not easy - action of jumping on a plane and pitching in. In addition to spending several days packing food and cleaning up, her group raised over $14,000 for the people of Houston.
You're amazing Mai!
We are really making progress on the Navy-funded epsilometer! It is now capable of streaming serial data or writing to compact flash, has a 1000-m pressure case, and can run for a couple of days on AA batteries. We're beginning to put it on everything, including wire walkers and a newly designed fast CTD vehicle.
We have a test early November on R/V Sproul and are hoping for excellent results.
We are currently looking for a postdoc to work with us on the Samoan Passage project. Research tasks include analysis of a dense 3D dataset of moorings and tows resolving hydraulically controlled flows, breaking internal waves, turbulent mixing and other processes in the Samoan Passage, a constriction in the abyssal Pacific Ocean. In addition, we have results from a very high resolution numerical model of the region at hand to help with the analysis.
Scientists from ours and other groups at Scripps, as well as other institutions around the country, are gearing up for a major initiative to better understand the "inner shelf". This is the region just offshore of the surf zone (yes that is the technical term) but still in the relatively shallow water of the coastal ocean. This area is governed by unique but complex physical processes, including wind-driven circulation, upwelling, breaking waves, wakes and instabilities, and internal waves (that ride on density interfaces below the surface). Funded by the Office of Naval Research, we will spend the next couple months observing and trying to detangle the complexities of this system using a combination of mooring and ship-based observations. Befitting the complexities of this part of the ocean, we are attacking with with everything but the kitchen sink, including a staggering 119 moorings(!), 7 ships (!) working in concert, arrays of drifters, dedicated scientific aircraft surveys, and more. We're just loading up gear right now, more details once we get underway! https://scripps.ucsd.edu/projects/innershelf/readying-gear-on-the-rv-sally-ride/
MPL interns Eli Simmons, Louise Xu and Drew Vagen have been hard at work in our lab this summer. Among their many accomplishments: creation of a new travel-time acoustic current meter (Louise), calculation of the flow through the Samoan Passage from a high-resolution model (Drew), and design and construction of many new mechanical devices (Eli). Thanks to all of you for your talent and hard work this summer! Since Louise is a UCSD student, we're happy that she'll continue with us this fall.
Last February, we branched out pretty substantially from our usual bailiwick of internal waves and mixing, and grabbed some huge pumps and tanks in order to create artificial salty plumes of water that we then sampled with an ROV to watch them descend. Why on earth would we do this? Possible future deep sea mining operations will need to return the "tailings" they bring up from the sea floor, so it is crucial to know how they will descend and disperse.
In November we'll be continuing this on a cruise funded by the UC ship funds program. First we'll create plumes with massive tanks of salt water and pumps. We'll then use an ROV, an AUV, our Phased Array Doppler sonar, and side-scan sonars to image the plumes as they descend. Finally, we'll use our towed bodies to track them as the ambient currents sweep them laterally.
The ultimate goal is to inform future policy on responsible practices.
Sea-going oceanographers, like those aboard the R/V Sikuliaq today, have a cautionary principle that they always keep in the back of their minds. When an expensive piece of scientific equipment, the vital infrastructure that makes up most of the budget for an ocean research team, goes over the side of a ship and into the sea you can’t expect for certain you will ever see it again. The oceanographer designs every effort, makes every plan, and works every day to get the equipment and data back, but should never take as given that what goes in the sea will all return.
The ArcticMix mooring stands 3452 meters tall in the middle of the Beaufort Sea and when it was deployed early in September the scientists and crew of the R/V Sikuliaq literally watched as they let slip into the deep over half a million dollars worth of technology. And while there are plans and backup plans for how we will again find this undersea treasure, everyone aboard will sleep better when each meter of wire and scientific baubles are again tied to the deck. Still there is no better way to measure the ocean across its entire depth over a long period of time than employing ocean moorings. These hard-won scientific data from the real ocean are essential to formulating and tuning the global climate computer simulations that inform decision-makers and regularly make the headlines
The primary study zone for the ArcticMix voyage is right on top of what the National Snow and Ice Data Center (NSIDC) has called ‘a striking feature of the late 2015 melt season’, a period that has ended as the fourth lowest Arctic sea-ice minimum on record. Over 19 days, as the R/V Sikuliaq made additional ocean observations nearby, the ArticMix mooring stood steady listening and learning about its patch of the Beaufort Sea.
The Arctic is a strange place oceanographically, an up-side down version of the normal ocean in that the surface water is cold and fresh while lurking below is a reservoir of warmer, saltier water, heavier than the surface layer due to its high salt content. One hypothesis in a rapidly-changing Arctic is that increasing open water allows storms to mix this deeper ocean heat upward through the generation of undersea beams of energy called ‘internal waves’, in turn melting more ice. The peculiar nature of the Arctic is what makes a hypothesis of a positive climate change feedback based on vertical mixing possible.
In the first weeks of of our voyage the ArcticMix oceanographers witnessed remarkable levels of subsurface mixing. Their sensitive instruments, leashed to the back of the R/V Sikuliaq by high-tech cables wrapped around specialized winches, saw billows of turbulence that looked just like a wave breaking on the beach, but much larger. These underwater waves could easily reach into these regions of warmer water below the ice, possibly moving some of this heat upward when they break.
While the ArcticMix scientists darted across the Beaufort looking for signs of ocean mixing over wider swaths, the undersea mooring witnessed conditions minute by minute at a single location that serves as a scientific reference for the entire voyage. The time comes to return to the scientific backbone of the entire experiment and find both the mooring equipment and all the invaluable data stored on many tiny memory cards, not unlike those in your nice camera except they are 3000 meters under the ocean.
The morning of the recovery breaks with fair winds and calm seas, the decks of the R/V Sikuliaq awash with sun for the first time since we had left Nome over 3 weeks earlier. Best of all there was no ice to be seen. Sea-ice, driven by the wind and currents, was completely out of our control and could easily have moved to cap the sea here, freezing our scientific assets beyond the reach of Sikuliaq. The ArcticMix team won another calculated roll of the dice, as the risk of mooring a five hundred thousand dollar scientific bet in an ice-filled Arctic looked to be paying off.
A button is pushed and a special transducer puts a coded ping of sound into the water. Somewhere, well over two miles below the stern of our ship, another device hears the command and releases its grip on the bottom. The ArcticMix mooring rises slowly to the surface, four feet or so every second, and within 45 minutes it’s at the surface. The top buoy is hooked and bit by bit and inch by inch the mooring is brought aboard in the Arctic sunshine. Instruments are quickly washed and rushed back into the science lab for data transfer. A team of graduate students and scientists swarm over the gigabytes of data filling the ships server and soon the first preliminary plots fill our computer screens. The mooring has witnessed exactly the kind of wind generated internal waves we’ve been looking for.
One of the measurements captured on the undersea mooring is the velocity of currents through a wide range of ocean depths. When these currents are displayed as a long series over time the clear signature of internal waves can be seen. These beams of energy, generated by the storm that passed over the Beaufort Sea weeks earlier, descend into the deeper layers of the ocean where they can “break”, and as we observed elsewhere in the Arctic, heat can be mixed into surface waters a bit like hot coffee in cold cream.
What we have seen so far in the Arctic has certainly not refuted the hypothesis there there could be a positive feedback in regional changes in sea-ice cover that could lead to an increased rate of melting. The marked energetic mixing we have seen here at the heart of the Arctic ice-melt zone could be a key in understanding a potential new climate feedback. But for now the hard work lies ahead of the ArcticMix scientists for they must carefully untangle the complex processes involved to to distinguish typical seasonal melting from longer term change, with the goal of providing new insights that will help improve the accuracy of climate forecasts for the Arctic region.
[by: Thomas Moore, for the ArcticMix team]
For most of us in our daily lives we think of our world in three dimensions. We need to get up out of bed, across the floor, and through the door to the kitchen to make the coffee. But when it comes to observing the physical nature of planet earth what is happening at a given location in three-dimensional space is only half of the story.
As part of their training one of the fundamental skills an oceanographer learns is to think beyond three dimensions, to include time and the change at a given location over time in their scientific perspective. It’s not enough to go somewhere and have a look just once. Without gathering data and building computer models in this fourth dimension we wouldn’t know that the sea-ice at the very spot in the ocean we are floating on at the moment has changed rapidly over the past twenty years.
So scientists talk about things they are observing in terms of space and time, scales of ocean measurement that fundamentally define how rich or spare their digital libraries of data become. And how well sea-going oceanographers can see things over these scales are ultimately dependent on the scientific gadgets in their tool box and which ones they choose to put into water.
The research vessel Sikuliaq is a capable moving platform for our suite of custom ocean tools and her role is to take this technology all across the Beaufort Sea where it can best be put to use. But a ship can’t be everywhere in the Arctic at the same time and so there are gaps, blind spots, but we can help fill those by deploying what ocean researchers call a mooring.
A mooring is a towering string of scientific instruments thousands of metres tall supported by giant floats at the top and held to the seabed by a beefy weight. And on this mooring, this undersea science station, we put robots.
Deploying an ocean mooring in over 3000 meters of water is no mean feat, it is one of the bread and butter professional competencies that a group like the ArcticMix team must have and work relentlessly to maintain. A highly technical and often hazardous operation that can take many hours on the back deck of a ship like the Sikuliaq, mooring deployments are often exposed to whatever weather and waves the sea decides is right for the occasion.
This voyage the weather and seas were mostly kind and the ArcticMix mooring was happily fastened to the mud on the bottom of the Beaufort, its top float suspended in the ocean currents a bit like a giant balloon on a string swaying in a watery breeze.
Attached to this mooring are unique, recently developed ocean instruments called McLane profilers (MP’s). MP’s are “wire-crawlers”, programable robots that descend and climb the mooring wire over and over and over again, one million metres worth of travel in their large internal lithium battery packs.
These profilers come jammed with an array of instruments that measure pressure, temperature, salinity, and most importantly current velocity across a longer vertical reach than any other tool in our oceanographic toolbox. The following figure, calculated from MP data collected in the South China Sea in 2007, shows the kind of ocean current information that can be measured as time passes. Scientists call it a “time series”.
While the ArcticMix team aboard Sikuliaq spends the coming month exploring elsewhere, our mooring, fixed in one location, can observe ocean parameters over a long period giving us a base of consistent information to anchor the wider story of Arctic change.
[ by: Thomas Moore, for the ArcticMix team ]