| Scripps technician Megan Roadman deploys 'Aquaty.' |
Welcome to SOCCOM at Sea, the blog of the Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) project! Join in the adventure as we deploy a biogeochemical observing system in the ocean around Antarctica.
Wednesday, January 27, 2021
All Floats Deployed
Wednesday, January 13, 2021
The Northern Floats
Since leaving Hawaii more than two weeks ago, we've made our way steadily south. Hawaii is 19 degrees North of the equator and we're now at 44 degrees South. We've deployed four of the SOCCOM floats so far.
| Chief Scientist Barney Balch and Scripps restech Charlie prepare to deploy SOCCOM float "Hawk-eye." Photo by Megan Roadman. |
The other big news is that we were allowed to stop wearing masks on day 15. People onboard seem very grateful for the change, though it definitely takes some getting used to. I find myself touching my chin or reaching into my pocket at times, panicked that I'm not wearing a mask when I should be. We get to enjoy this time after spending two weeks in hotel isolation and then another two weeks social distancing once we got underway. I know I'll have to go back to it once the cruise is over, so I'm planning to enjoy the next six weeks of being relatively stress-free about the pandemic.
We're also able to serve ourselves buffet-style at meals. For the first two weeks, our cooks Richard and Ruth had been serving us. I'm sure they're happy for the change! We also had set meals windows and sat only two people to a table that could fit six. Sitting right next to and right across from people at meals feels like such a luxury!
It's only been a few days, but we're definitely missing the calm seas of the tropics. We're in the roaring 40s now and headed as far as 60 degrees South. With 6 more floats to go, we'll be busy. Check back for more updates!
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| Missing that blue water from the deployment at 30 degrees South. |
Sunday, January 3, 2021
Float Decorating Party!
R/V Revelle left Honolulu the day after Christmas. We spent December 23-26 loading the ship and preparing everything onboard. I knew the loading days would be busy, but I hadn’t realized for how unprepared I was for them physically after two weeks in a hotel room. We should have been training! On day 10, stand for one hour and then steadily increase that each day. Even just wearing shoes felt different.
We worked all day on Christmas, pausing to make phone calls and Zoom appearances with friends and family. The cooks, Richard and Ruth, made a great dinner. I brought a small Christmas tree and set it up in my lab. It was quickly surrounded by presents as our chief scientist / St. Nick brought chocolate bars for all of us and we did a white elephant gift exchange. Though the actual exchange was delayed a few days due to weather since we had to hold it outside due to the COVID protocols.
We crossed into the Southern Hemisphere with only a few hours left in 2020. Again, because of COVID protocols, we are delaying any crossing ceremony until we are sure we’re all healthy and can do so safely.
We’ve been at sea for 8 days and still have a few more before we start deploying SOCCOM floats. In the downtime, I got a bunch of the scientists to help out with decorating them based on their names and designs from the schools that adopted them. It was easy to find volunteers for a fun arts and crafts project on the sunny back deck in calm, tropical waters. It was only then they realized that it also came with some manual labor to unstack and restack the heavy crates.
Some of the floats are black and can only be decorated with metallic sharpies, while the yellow ones have a broader range of colors that will show up. It was fun to work within those restrictions though, and I think the floats all turned out beautifully. I was so grateful to have had help. I am not very artistic and usually only decorate a few at time before running out of ideas. This time around, all 13 floats were decorated inside of an hour.
Check back for posts about the floats as they get deployed and other exploits from aboard R/V Revelle!
Monday, December 28, 2020
Hotel Quarantine
**To ensure everyone’s health and safety, the entire 22 person science party and 14 relief crew members spent 14 days in the Laylow Hotel in Waikiki in preparation for this research cruise. We then moved aboard R/V Roger Revelle and are headed south to deploy floats, collect and analyze seawater, and many other science initiatives too!
If you must spend 14 days in a hotel room by yourself, there are certainly worse options than the Laylow Hotel in Waikiki. The suites are room numbers 1,4,5,14 &15 on every floor and each has a slightly different layout and even furniture and artwork. One wall is covered in what can only be described as Wes Anderson Hawaiian chic wallpaper. It makes a perfect Zoom background. Interestingly, roughly 1 in 4 rooms has the same pattern with the opposite color scheme.
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| My Scripps teammates. |
Unless one only wants a parking garage view, ask for a room on the 7th floor or above. Make no mistake, every room comes with a view of a parking garage, this is just if you want anything additional to look at. More specifically, suites 1,14,15 have partial ocean views. If you are about to spend 2 months with only the ocean for scenery, suites 4-5 view the mountains instead. All get rainbows, but only rooms 1,4,15 see to the southwest in case of remarkable once every 800 year views of conjunctions of planets. Rooms 5,14 overlook the Laylow’s pool for those who enjoy watching other people relax on daybeds and pool loungers.
Thankfully, the walls of the hotel are sound proof. Despite every room coming with its own ukulele, there is no assault from the noise of dozens of people learning to play said instrument. The Hideout restaurant is visible from rooms 4-5 and comes with nightly live music from 6-9pm and caterwauling drunk people from 9:01-10pm. The balcony doors are thick and block most of the sound. If one enjoys 1-2 guitar toting young people playing covers of ‘90s R&B plus Beyonce, it is actually a lovely addition to warm tropical evenings. Currently there is a one week rotation of talent, all good but Tuesday night is the standout.
| Daily rainbows are a lovely feature. |
The WiFi is adequate, except on days when 36 people are trying to download everything they can think of in preparation for 2 months without any internet. If you bring a Chromecast, be prepared to have to resync it at least once a day for no apparent reason. And if you bring a Nintendo Switch to play MarioKart with your new friends, only one of you can be on the hotel WiFi, again for no apparent reason. The rest must use their phones as a hotspot. The "Smart" TVs do have Netflix, if you can remember your brother's password.
The toiletries smell pleasant, not too floral and not too musky. The robes are soft and big enough for a plus sized person. There are no microwaves or even coffee machines. BYO bottle opener and corkscrew as well, the hotel only has a few loaners. Once the knick knacks (is it art or is it a cup?) are moved, there is ample shelf space for snacks and any holiday decorations you may have brought. Lighting is also a bit lacking, the front desk will deliver an extra lamp if requested (or if yours smokes when you turn it on). The lamp hanging over the table is inexplicably low and covered in spines. Moving the table and looping the lamp’s cable can help, but if one has a hard had that is the only way to ensure injury-free use of the table.
| An early tally, me versus the urchin lamp |
The hotel staff are superstars, willing to shuttle presents, booze, and snacks from one room to another for those who cannot so much as step out of their room. They also accommodate delivery services with ease. Every food imaginable is available, including Hawaiian favorites such as malasadas, poke, plate lunches, and pineapple in every conceivable form. The hotel meal plan is apparently lacking in variety, vegetables, and heat, so stick with Doordash and other delivery services. Foodland delivers alcohol.
After two weeks and four negative COVID tests, you'll be ready to set sail!
Enjoy your stay at The Laylow!
Tuesday, June 9, 2020
Science Continues During the Pandemic
Researchers with the SOCCOM project scramble to save their season and plan for the next.
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| Deployment of a SOCCOM float from R/V Mirai. |
Racing the Clock Aboard the Mirai
| The science party of R/V Mirai. SOCCOM technician Melissa Miller is in red. |
Unexpected Endings on the Palmer
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| Rosso describes cruising through the Gerlache Strait as one of the most memorable experiences of her life. |
Rosso usually takes a run upon reaching port, an impossible luxury at sea. But that wasn’t an option this time. Instead, the only opportunity to leave the ship was so Chilean health officials could take everyone’s temperature.
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| Rosso (far left) and the American scientists from Palmer in the Punta Arenas airport. |
Cancellation of the Investigator
| Matsumoto (far right) and scientists aboard the Investigator. |
Sailing Home on the Brown
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| Prend prepares to deploy a SOCCOM float from the Brown. |
What’s Next?
Wednesday, March 25, 2020
Musings from the R/V Ron Brown (March-April 2020)
the United States. Most recent posts will be at the top.
After a long transit home, we’re just a few days away from port in Virginia. In certain ways, being at sea has prepared me for going into quarantine. I’m certainly familiar with life confined to small spaces. The social isolation, however, will be very new. Since everyone on the ship is healthy, we don’t have to worry about social distancing. I will miss the many conversations about science and life with all on board, which have been the highlight of the cruise.
A few weeks ago, we had a barbecue outside on the ship’s fantail to celebrate crossing the equator. The air was thick with moisture, but everyone was in high spirits. Some people were playing cornhole. Others were splashing around in an inflatable kiddie pool. I remember observing the whole scene from a picnic table and realizing: once I’m back on land, it could be weeks or even months before I’m at a gathering with this many people. It was a sobering thought.
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| The view from the fantail of the R/V Ron Brown |
Sometimes I think about the SOCCOM floats, and picture what interesting processes they are observing, wherever they might be. Out here, the immensity of the ocean is perceptible, which makes it even more amazing to me that these tiny floats are changing our understanding of the climate system.
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| The blog author just before the final SOCCOM float deployment several weeks ago. |
- Channing
The ocean regulates the climate system by absorbing nearly one-third of global carbon dioxide (CO2) emissions. Once dissolved, CO2 causes chemical reactions that lower the pH of seawater, a measure of its acidity. This means that the ocean is becoming more acidic as it takes up the excess carbon emitted by burning fossil fuels, shifting the carbonate equation and causing a phenomenon known as ocean acidification. Ocean acidification is bad news for millions of tiny organisms, like the pteropod below, whose shells’ get corroded in these conditions. Therefore, monitoring pH levels in the ocean, for example by using the pH sensors on the SOCCOM floats, is necessary to determine how climate change will impact marine ecosystems.
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| Unhealthy pteropod with dissolving shell ridges showing the effects of ocean acidification (NOAA Fisheries Collection) |
In addition to telling us about ocean acidification, the pH of seawater can also reveal important information about the carbon cycle. Since pH levels are directly related to ocean carbon uptake through known chemical reactions, they can be used to calculate the amount of dissolved CO2 in seawater. This, in turn, allows scientists to estimate air-sea carbon fluxes, as described in a recent paper led by University of Washington professor Alison Gray. The Southern Ocean is typically thought to play an outsized role in the global ocean carbon uptake, but Alison’s study showed that it may not be absorbing as much CO2 as we thought. In fact, certain regions even released carbon into the atmosphere, acting as a source rather than sink for atmospheric CO2.
Much of this previously undetected ocean carbon release occurred in winter in the icy regions close to Antarctica, highlighting (as we’ve seen before) the importance of year-round sampling and expanded data coverage. Accurately quantifying air-sea carbon exchange, through studies like Alison’s, is essential to improve global climate models. Furthermore, combining information from all the different float sensors can help us untangle the complex set of physical, chemical, and biological processes that control the fluxes of carbon between the ocean and atmosphere.
While I’ve focused each post in this series on a particular sensor, the temperature, salinity, bio-optical properties, nitrate, oxygen, and pH of the ocean are all connected. In fact, we’ve seen that some of the most groundbreaking science happens when we consider how these properties interact and influence each other. Another key theme has been the unprecedented spatial and temporal resolution provided by the float array. The Southern Ocean is inaccessible, and numerous scientific discoveries resulted simply from having measurements during winter and in ice-covered regions. Only by continuing to observe these remote places can we hope to understand and predict how the climate will change in the future.
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| Map of the SOCCOM float array as of March 29, 2020, including the 6 floats we deployed on this cruise! (SOCCOM) |
And that is the power of SOCCOM! The new insights gained from this novel dataset are changing our understanding of the Southern Ocean and its impact on global biogeochemical cycles. Furthermore, the SOCCOM project has a team of world-renowned climate modelers using those findings to inform models and improve future climate projections. The breadth of work being done is truly remarkable, and the studies I’ve featured in this series are just the tip of the iceberg (more than 100 publications have already resulted from this program!). And as the size of the float array increases, so too will the number of questions that we’re able to answer about the ocean and its role in the climate system.
- Channing
In the last two posts, we talked about phytoplankton, microscopic algae that play a key role in marine ecosystems and the global climate. You’ve heard about how phytoplankton absorb carbon dioxide (CO2) through photosynthesis, but they also produce oxygen (O2) through this process. In fact, phytoplankton photosynthesis is responsible for roughly half of the oxygen in our atmosphere, which makes earth habitable. So be sure to thank these tiny organisms the next time you take a breath!
Oxygen is also central to the carbon cycle and can be used by scientists to partition ocean and land carbon sinks from atmospheric data. This is because terrestrial carbon uptake, by trees and other land plants, leaves an imprint on atmospheric oxygen levels in a known ratio based on the chemical reaction that takes place during photosynthesis. Ocean carbon uptake, on the other hand, occurs independently from air-sea oxygen exchange and thus does not affect atmospheric O2. The different influences of these processes can be used to separate the total global carbon uptake into land and ocean components from measurements of atmospheric O2 and CO2. The largest source of uncertainty in this calculation, however, is air-sea oxygen fluxes, which are poorly constrained due to lack of observations. Therefore, oxygen concentrations in seawater, which can be measured using the oxygen sensor on the SOCCOM floats, contain essential information about the climate system.
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| Schematic of the global carbon cycle showing both land and ocean sinks (NASA Earth Observatory) |
Using the float temperature and salinity data, Seth determined that this wintertime oxygen uptake was driven by ventilation, the process by which surface waters are transported into the ocean interior and away from their source region. These results highlight the value of the SOCCOM dataset, both by increasing the number of ocean oxygen measurements and by allowing us to relate that information to specific physical drivers. The improved estimates of ocean oxygen uptake, stemming from the float data, can reduce the uncertainty in the quantification of ocean and land carbon sinks from atmospheric O2 and CO2 measurements. This, in turn, will help reconcile differences between observations and models of the global climate.
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| Map showing location of SOCCOM float profiles (left) compared to all previously available data collected by ships (right) (Bushinsky et al., 2017) |
- Channing
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| Microscope image of diatoms, a major phytoplankton group in the Southern Ocean (Wikimedia Commons). |
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| Floats used to estimate biologically-driven carbon export in Ken’s paper. There are many more floats now than when the paper was published! (Johnson et al., 2017). |
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| October (spring in the southern hemisphere) satellite chlorophyll in the Southern Ocean showing the signature of the Scotia Sea phytoplankton bloom. Image created by Channing Prend. |
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| Schematic showing how vertical mixing at topography can deliver nutrients (in this case iron or Fe) to the upper ocean and support phytoplankton growth. Image created by Channing Prend. |
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| Satellite image of the 2017 polynya at Maud Rise (NASA Earth Observatory) |
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| Schematic of the global overturning circulation, which is driven, in part, by gradients in density due to temperature and salinity changes (Robert Simmon via Wikimedia Commons) |
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| Floaty McFloatface ready to join the fleet of SOCCOM floats collecting data in the Southern Ocean. - photo by Channing Prend |
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| The blog author enjoying sunrise over the Atlantic before deploying Sylvia Whirl (photo by Susan Becker) |
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| The blog author standing proudly with Knight Drifter just before deployment. photo by Molly Martin. |
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| See Turtles ready to begin its journey around the Southern Ocean. Photo by Channing Prend> |
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March 24, 2020
| Bobcat's Be-bopping Bobber on the deck of the R/V Ron Brown before deployment. Photo by Channing Prend |
| Gloria's Gulper takes the plunge into the cold Southern Ocean waters. Photo by Channing Prend |

























