Wednesday, January 27, 2021

All Floats Deployed

Scripps technician Megan Roadman deploys 'Aquaty.'



Apologies for the time between posts, but it's been very busy onboard Roger Revelle! We deployed six more SOCCOM floats since my last post and did dozens of CTD casts. There won't be any more deployments on this trip, but we still have nearly a month left onboard and I will post more about life at sea during that time. 

There's also a science writer onboard who is posting blogs about the work going on and the quirks of life at sea, especially during a pandemic. Check that out here.

We've been experiencing good weather, with relatively calm seas. All ten of the SOCCOM floats were deployed successfully and have reported profiles of the water column.

There was about a week where we didn't see the sun though, and as someone who lives in Southern California, I missed it! I could tell my mood was off. The sun reemerged a day or two ago and it was so exciting. Though it's still quite chilly out.





Scripps technician Matt Durham deploys 'Lizzy.'








We also saw a humpback whale, which came very close to the ship and hung out for awhile. Someone pointed out later that it was hump day, halfway through our time at sea. A humpback whale on hump day! There have been a collection of birds - albatross, petrels, and prions - following the ship.

As we headed to our most southern point, 60 degrees South, the bridge saw a few icebergs on the radar. But we didn't see any in person due to the fog. The ship slowed down to make sure we transited safely.

Morale onboard is good, we are enjoying a life without masks and social distancing while we can. Everyone has friends and family back home that are doing their best to stay safe and healthy. It's hard to be away, but thankfully our internet speeds have been conducive to keeping in touch. 

Thanks for following along. I'll be sure to post more often!

 



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!


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.


Christmas tree atop the SOCCOM floats, stored on the back deck.

 

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!

 

My Review of the Laylow Hotel after spending 2 weeks in room 905:

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. 

 

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.

by Melissa T. Miller

The COVID-19 pandemic affected four SOCCOM (Southern Ocean Carbon and Climate Observations and Modeling) expeditions that were underway between December and April. The team was still able to safely deploy all of the planned autonomous floats, which add to a dataset crucial to understanding climate change.
The SOCCOM program relies on research cruises already going to the Southern Ocean in that hemisphere’s summer months. Planning can take place year-round, but the field season must be done when there is less ice, generally between October and April. The floats travel with the currents, moving up and down the water column to collect data with a suite of onboard sensors. Then they surface and transmit the data to researchers on land. 
Using ships of opportunity requires extensive cooperation and coordination even under normal circumstances. That all the floats were safely deployed under the ever-changing conditions of a global pandemic is a testament to the team’s planning but also to the flexibility and dedication of everyone involved, especially the scientists and crew members in the field.
Deployment of a SOCCOM float from R/V Mirai.
Dr. Lynne Talley, a professor at Scripps Institution of Oceanography (SIO), is the project lead of this international multidisciplinary program. “We have amazingly good relationships with the agencies who run these ships,” she says. “And the captains were amenable.”

When Wuhan, China went on lockdown on January 23, 2020, SIO technician Melissa Miller had been at sea for a month and was still two weeks from arriving in Singapore. Dr. Isa Rosso, an assistant project scientist at SIO, left port in Punta Arenas, Chile just a few days later on a two-month research cruise. Both expeditions were able to fulfill their science missions, including the deployment of SOCCOM floats, but traveling home from foreign ports was a serious concern.
The final two cruises of the season were scheduled for March, when the situation in the United States was becoming serious and changing by the hour. Dr. George Matsumoto of the Monterey Bay Aquarium Research Institute (MBARI) was in Fremantle to board an Australian ship. Channing Prend and Susan Becker, an SIO graduate student and staff member, respectively, traveled to Cape Town, South Africa for a NOAA GO-SHIP cruise. Neither cruise ended up fulfilling their larger science missions, but the SOCCOM floats were deployed. 
The experiences of SOCCOM’s sailing technicians vary depending on the timing, but also on the organization of the ship’s operators and the countries involved in their travel plans. In these unprecedented times, communication was crucial not only to the mission’s success but also to the physical and emotional health of the scientists.

Racing the Clock Aboard the Mirai

Melissa Miller left the U.S. in mid-December, a completely different time. She traveled care-free in Europe before heading to Mauritius, a small island in the Indian Ocean to meet the ship. A planned six-day vacation in the end port of Singapore seemed a long way off, but she was already looking forward to it. 
Miller oversaw deployments of eight SOCCOM floats from the Japanese research vessel (R/V) Mirai. She had no internet access, only an email account. English-language news updates were available a few times a week and steadily became dominated with updates about a new and unknown virus in China. Then came the news that it was spreading and that countries were closing their borders.
“I wouldn’t be surprised to find out that the people around me had been talking about the virus for weeks,” says Miller. “But I had no idea since I don’t understand much Japanese and wasn’t seeking out the news. My dad mentioned it in an email and that was the first I’d heard of it.”
Once in Singapore, scientists and crew who planned to return to the ship were required to wear a mask when they were outside. This included Miller when she was on deck to deal with the offload of samples and gear. The ship and crew were continuing to the ship’s home port in Japan. The other scientists all had flights out of Singapore within a day or two. 
“I kept the mask that the ship gave me and wore it as I disembarked through the cruise ship terminal,” says Miller. “I remember how weird it felt to wear one when not everyone was. It was my first experience with that conflict between paranoia and caution. Now it’s just part of every day life - what a difference a few months have made.”
In the days before her flight home, a few countries closed their borders to people coming from Singapore, which at the time had the highest infection rate outside of China. Miller worried that the United States would be next, in which case her flight home would be cancelled. 
Singapore implemented a rapid response plan, cancelling events that draw a crowd and installing cameras and sensors that take everyone’s temperature before they enter an enclosed space. Without the normal crowds of travelers coming from China, Miller played tourist in a practical ghost town. 
Though she stressed about new travel restrictions, none came and she flew home without incident on February 16. Miller diligently took her temperature every day for two weeks and made sure people knew she had just returned from Singapore in case they wanted to limit contact. But for the most part, she enjoyed a few weeks without worrying too much about the virus. 
“Since I had to be vigilant starting in early February, I feel like I’ve been dealing with the virus a month longer than everyone else I know,” says Miller. “I bought flour and yeast and hand sanitizer before they were out of stock. I stopped shaking hands at meetings. Other than that, I had a pretty normal re-entry period. I saw friends, went to a few bars and restaurants and for that I’m extremely grateful.” 
Within a few weeks, it was a different reality. Going to sea for the past ten years has given her a lot of experience in self-isolation, something everyone is learning to cope with now. Miller shared that insight in an article on Scientific American’s blog
You can also read Miller’s blog posts from the ship, which don’t mention the coronavirus, instead chronicling the deployments of SOCCOM floats and also the culinary and cultural experience of being on a foreign ship.

The science party of R/V Mirai. SOCCOM technician Melissa Miller is in red.


Unexpected Endings on the Palmer

Dr. Isa Rosso is also a seasoned sea-going scientist. She has been Co-Chief Scientist on previous expeditions and knows the amount of planning that goes into every moment aboard a research cruise. And that interruptions to those plans are inevitable - weather delays, engine trouble, and shifting ice all have to be accommodated. But no one was prepared for just how much changed while the ship was in the Southern Ocean between January and March. 
The R/V Nathaniel B. Palmer is an icebreaker in the U.S. Antarctic Program’s fleet and has deployed SOCCOM floats on multiple occasions. This particular cruise was focused on Antarctica’s Thwaites Glacier and included programs to collect sediment cores and seawater samples as well as attach sensors to seals.
After a few weeks exploring Patagonia’s national parks, a vacation she wouldn't have been able to take if she'd planned it after the cruise instead of before, Rosso left port on the Palmer. The first six weeks of the expedition were relatively normal - if you consider rescuing a Norwegian fishing vessel and discovering a new island normal. Rosso settled in to life onboard as science operations went well and five SOCCOM floats were successfully deployed. 
As the virus continued to spread, Rosso, who is Italian, heard the news about her home country going on lockdown. Only being able to email friends and family and not be there to help was extremely difficult.
With the end of the cruise in sight, the uncertainty about the ship returning to port in Punta Arenas, Chile increased. It was decided that the ten British scientists onboard would be dropped off at the U.K.’s Antarctic base, Rothera, so that their travel arrangements would be taken care of. 
“That was pretty sad,” says Rosso. “After so long, you get so close to each other. You see your friends go into a Zodiac and then you see them waving and it breaks your heart. All of a sudden, the ship is silent. There’s this level of balance that has been disrupted.”
The Palmer was also diverted to evacuate people from a U.S. Antarctic station. The ship was supposed to pick personnel up later in the season, but the pandemic meant that no schedule guarantees could be made and the scientists weren't cleared to stay over winter. With only a few days notice, twelve scientists had to pack up their experiments and move onboard the ship, their Antarctic research plans cut short. 
“That was one of the weirdest things that could have happened,” says Rosso. “A couple of days [after the British scientists left] you have this bunch of new people. They are a group, they have their own dynamics. And for us, it was like ‘who are these people?’”
A gorgeous stretch of scenery as the Palmer transited through the Gerlache Strait helped Rosso withstand the unexpected departure of cruise friends. A few days later, the ship arrived back in Punta Arenas, which was itself on the verge of shutting down due to the virus. 

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.
“I was looking from the portholes and saw a few people on the pier with masks and gloves and all of a sudden it hit me. All of a sudden it was a reality,” says Rosso.
The scientists had to depart on what they were told may be the last flight out of Punta Arenas. Rosso made sandwiches and filled leftover sample vials with hand sanitizer for the group to take with them. When they arrived at the airport, the airline told Rosso that she wouldn’t be allowed into the U.S. using her visa. But the scientists had been told when leaving the ship that they wouldn’t be allowed to return. Rosso was trapped in limbo.
Fortunately, the ship’s agents were able to assure the airline that the U.S. was letting visa holders in, but Rosso still worried about it through her next two connections - unable to relax until she was through customs and immigration in Miami. She arrived home on April 1 to a city already weeks in to stay at home orders. 
Adjusting to normal life after months at sea is always a challenge, and this time Rosso wasn’t able to follow her tried and true steps to acclimate.
“Usually I come back from a cruise and the first thing I do after I’m over the jet lag is go to the gym,” she says. “So even if I decide to stay home from work for a week to get adjusted, I have that routine. But not anymore - that was an extremely tough moment.”
The Palmer was recalled to the U.S., ending its season early. Thanks to the ship’s crew and technicians, the SOCCOM samples and equipment were able to ride the ship back and were transferred to SIO for storage until the analytical labs reopen to process them. Rosso, now working from home, is able to reflect positively on the experience, though it was stressful at the time.
“I think that in situations like this you really see how people are ready to help. That’s really cool, that’s really beautiful.”
To read Rosso's and other scientist’s insight from the Palmer, and see more pictures, check out the blog posts from the cruise

Rosso (far left) and the American scientists from Palmer in the Punta Arenas airport.


Cancellation of the Investigator

Dr. George Matsumoto was looking forward to his first expedition as a SOCCOM representative. He is an educator at MBARI and runs the popular Adopt A Float program that connects SOCCOM floats with classrooms around the world. On top of outreach projects, this time he was also in charge of deploying two floats and collecting seawater samples during a 12-day cruise. The science mission included training sessions onboard the Australian ship for students from around the country, with Matsumoto contributing lessons about SOCCOM floats and science communication.
Matsumoto left California on March 5, just before advice and restrictions began changing on a seemingly hourly basis. Joining R/V Investigator in Western Australia, he met up with the other scientists, educators, and students. While getting oriented, they were told that a few crew members were sick and had been tested for COVID-19. The ship had to remain in port until the results came back. Matsumoto, stressing about the delay, tried to keep busy.
“Facing an indefinite period at the dock, the trainers decided to take advantage of the time and continue with the training that we had planned and work with the students onboard,” says Matsumoto. “Day by day, we waited for results and did what we could to maintain our training schedule.”
It took four days to learn that the crew members all tested negative. By then, one of the scientists wasn’t feeling well and was sent off to get tested. Not able to continue delaying, the decision was made to cancel the cruise and get the ship back to its home port of Hobart, Tasmania. Though disappointed, Matsumoto was able to complete most of his planned training sessions before heading home on March 14. Though only nine days had passed, the virus and associated travel restrictions had intensified.
“The trip home was stressful as there were no PPE guidelines in place yet. I filled out a flyer about how I was feeling, but it was never collected. Once I got home, MBARI had closed which made the 14-day self-quarantine that I was going to undertake simple.”
The ship’s crew stepped up to deploy the two SOCCOM floats during the transit. Having an enthusiastic and helpful crew is always an asset. They have to accommodate changes and uncertainty and make sure everything is done safely on any normal expedition. This was an extreme case and they did an admirable job taking over when the scientists couldn’t be there.

Matsumoto (far right) and scientists aboard the Investigator. 

Sailing Home on the Brown

The GO-SHIP cruise A13.5 was overshadowed by the coronavirus from start to finish. The plan was to board the NOAA research vessel Ronald H. Brown on March 19 and spend 45 days at sea, ending in the Cape Verde islands off the northwestern coast of Africa. Despite the timing, SOCCOM representative Channing Prend was excited to be heading out on his first research cruise. Susan Becker, who has participated on many SOCCOM cruises, was also onboard.
Prend prepares to deploy a SOCCOM float from the Brown.
Though there were relatively few cases of the virus, the busy port city of Cape Town, South Africa began to shut down operations while the ship was being loaded. Ten of the twenty seven scientists who were supposed to be onboard weren’t able to travel due to university and agency restrictions. The rest scrambled to make a plan so that the science mission could still be accomplished - it would mean more work for everyone but people were ready to step up. 
The plans changed every day, and eventually NOAA recalled the ship to the port of Norfolk, Virginia. At first, the scientists were told they could still do an adjusted schedule, getting some of the intended projects done. A day later, that changed and they were directed to head straight to the U.S. But first, the ship had to stay within a four day’s radius of Cape Town for a week in case anyone onboard got sick.
“Given that everyone on board was healthy, I would have rather stayed at sea and completed the full transect before steaming home,” says Prend. “It was undoubtedly safer on the ship than it is here [at home in San Diego], so I wasn't in a big rush to get back.”  
The bulk of the science mission had to be scrapped, but the decision was made to prioritize the SOCCOM floats. Talley had to change the locations of deployments based on the ship’s restrictions, taking into account ocean currents and depths. Usually she has weeks to make the calculations, but this time she had to come up with an entirely new plan overnight. The team rallied and deployed six SOCCOM floats and collected water samples.
Then came a three-week transit across the Atlantic Ocean, including an equator crossing. Surface water samples were taken while underway, keeping the scientists busy and on shifts to run analyses. Making the most of time aboard the ship was all the scientists could do. They got daily updates about the virus along with the crew. 
Plans for the ship’s arrival and everyone’s travel home from Norfolk continued to change throughout the journey. Becker and Prend had to fly across the U.S., returning home over a month in to San Diego’s stay at home orders, which began only a few days after they left in March.
“It seems that everyone is trying to make the best of this unprecedented situation,” says Prend. “That didn't really come through when we were at sea and all we saw were sensationalized news stories. My impression now that I'm back is that people are adaptable and resilient.”
Prend’s blog posts, unlike those from earlier cruises, are full of mentions of the coronavirus. He also did a wonderful job of explaining the scientific impacts of the SOCCOM float program. Prend wrote an article for the SIO website about resilience in the face of the pandemic.


What’s Next?

Shipments usually start going out in September for the upcoming SOCCOM season, and the team is already hard at work planning. But there are many factors involved and much more uncertainty than usual as every institution determines reopening procedures. Ship schedules are in flux as cancelled cruises jockey for a spot later in the year. SOCCOM relies on already-planned expeditions and Talley hopes that the strong relationships she’s cultivated in the community will lead to a successful season.
Another factor is float production. Many of the sensors have to be ordered from Seabird Scientific, which has been closed for months and may have a backlog once they reopen. The floats are built and tested at MBARI and the University of Washington, both of which have been closed since March. Months of work in those labs has gone undone and the short Southern Ocean season, dictated by ice coverage, can’t be delayed.
“Everyone is expecting a big impact,” says a pragmatic Talley. “The next season is all up in the air. We’re just going to see what we can do. Whatever floats we can scrape together, we’ll deploy.”
International cooperation and multidisciplinary teams are necessary for all scientific pursuits, but it’s going to take a redoubling of those efforts to secure a safe and successful season. The SOCCOM team is prepared to put in the work.

Wednesday, March 25, 2020

Musings from the R/V Ron Brown (March-April 2020)

The R/V Ron Brown left port in Cape Town on March 21, 2020 and is heading back to
the United States. Most recent posts will be at the top.


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April 14, 2020

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.
The view from the fantail of the R/V Ron Brown
I’m sitting at that same picnic table now, as I write this, enjoying the late afternoon sun. The ocean extends to the edges of the horizon in every direction. I have (somewhat surprisingly) not gotten tired of this view. The seascapes have been varied, ranging from the heaving washed out gray waves of a storm, to gentle blue ripples that scatter morning light. On breezy days like today, I often find myself watching the wind blow across the sea surface and imagining the waves that are being generated beneath it, which mix the upper ocean. Or trying to visualize the complex topography on the seafloor, and how the deep currents are navigating it.

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.
The blog author just before the final SOCCOM float deployment several weeks ago.
Thank you all for listening to my thoughts and reflections over the past few weeks. Being at sea during a global pandemic has been a strange and memorable experience. I hope that amidst all the uncertainty in the world, you’ve learned a bit about the SOCCOM floats and why the data they are collecting is so important. As I said in my first post, we need science now more than ever. Stay safe everyone!

- Channing


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April 11, 2020

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.
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.
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


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April 8, 2020

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.
Schematic of the global carbon cycle showing both land
and ocean sinks (NASA Earth Observatory)
To illustrate how the SOCCOM float array can lead to new insights about the oxygen cycle, I’ll summarize some results from a recent paper led by University of Hawaii professor Seth Bushinsky. Seth’s study used float measurements to calculate air-sea oxygen fluxes, which revealed that the Southern Ocean is a larger oxygen sink than was thought based on sparse ship data. Most of this previously undetected ocean oxygen uptake occurred in winter in the regions closer to the pole (south of the about 60°S), where sea ice cover is common. It is extremely difficult to access these icy regions, particularly in winter, so this discovery relied on the SOCCOM floats’ ability to sample year-round and in hard-to-reach areas.

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.
Map showing location of SOCCOM float profiles (left) compared to all previously
available data collected by ships (right) (Bushinsky et al., 2017)
And that is the power of oxygen! This key element supporting life on our planet also provides important constraints on the carbon cycle due to the coupling of CO2 and O2 via photosynthesis (as well as respiration and combustion). SOCCOM floats equipped with oxygen sensors can help us refine estimates of air-sea oxygen fluxes, and in doing so, better understand the relative importance of ocean and land carbon sinks. Since ocean uptake of carbon and oxygen are independent, however, other methods must be used to calculate air-sea CO2 fluxes directly. But I’ll talk more about that in the next post.

- Channing


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April 5, 2020

Last time, we talked about phytoplankton, microscopic algae that form the base of marine food webs and absorb carbon dioxide (CO2) from the atmosphere through photosynthesis. I previously referred to “forests” of phytoplankton in the ocean, but there are also “deserts”, expansive regions of sea with very little life. Why do phytoplankton thrive in certain places but not in others? Like plants, they need sunlight to grow. But they also require certain nutrients, including nitrate, phosphate, and iron, which they convert into proteins, fats, and carbohydrates. These nutrients are just like the ones contained in plant fertilizer that you might use in your garden, and without them, phytoplankton cannot survive. Therefore, measuring nutrient concentrations in seawater, for example by using the nitrate sensor on the SOCCOM floats, can help determine what controls patterns of biological productivity in the ocean.

Microscope image of diatoms, a major phytoplankton group
in the Southern Ocean (Wikimedia Commons
).

I mentioned before that phytoplankton sequester carbon in sediments when they die and sink to the seafloor. But that is not the fate of all phytoplankton, many get eaten by krill, copepods, and other organisms higher up on the food chain. In fact, only a fraction of the carbon produced by phytoplankton during photosynthesis gets stored in the ocean abyss where it is effectively removed from the atmosphere. To diagnose the impact of biological productivity on atmospheric CO2 levels, we need to know the amount of carbon that actually gets exported to the deep ocean. Since this is difficult to measure, scientists can estimate it using a number of different techniques, one of which relies on changes in nitrate. In a recent paper led by Monterey Bay Aquarium Research Institute scientist Ken Johnson, this method was applied to the nitrate measurements from the SOCCOM floats in order to quantify the biological contribution to Southern Ocean carbon uptake.

How do you get from nitrate to carbon storage? This method relies on the strong seasonality in phytoplankton growth, which peaks in spring and summer (just like flowers and other land plants across much of the US). For each float, Ken calculated the decrease in nitrate in the sunlit upper ocean over the course of a growing season, and then assumed that those changes were due to consumption by phytoplankton. The amount of nitrate utilized can then be converted to the amount of carbon produced by phytoplankton using the known ratio between nitrogen and carbon in their cells. In other words, based on the elemental composition of phytoplankton, we can infer the total annual carbon export to the deep ocean at a given location just by knowing the change in the near-surface nutrient inventory.

This innovative method requires year-round sampling of nitrate, which was scarce in the Southern Ocean before SOCCOM floats existed. The results from the full float dataset show that carbon sequestration by phytoplankton varies spatially, and is highest between 40° and 50°S. This is consistent with past studies, which required decades of data due to limited wintertime measurements. The SOCCOM floats now enable us, for the first time, to resolve this key process annually in locations around the Southern Ocean.
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).

And that is the power of nitrate! This essential nutrient supporting all marine life can also help quantify carbon export to the deep sea associated with biological productivity. Taking advantage of the unprecedented spatial and temporal coverage provided by the SOCCOM float array, through studies like Ken’s, can lead to new insights about the impact of phytoplankton photosynthesis on atmospheric CO2 concentrations. This, in turn, improves models of the global climate system. Furthermore, this information can be combined with other parameters measured by the floats, such as oxygen, to provide even further constraints on the carbon cycle. But I’ll talk more about that in the next post.

- Channing

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April 2, 2020

It is well known that expansive rainforests like the Amazon absorb carbon dioxide (CO2) from the atmosphere through photosynthesis. Similarly, the ocean has “forests” of microscopic algae called phytoplankton that take up atmospheric CO2 just like trees and other land plants. When these organisms die and sink to the seafloor, the carbon in their cells gets stored in deep-sea sediments. Therefore, determining the distribution of phytoplankton in the ocean can provide important constraints on the global carbon cycle.

Like flowers and other land plants, phytoplankton go through periods of rapid growth in spring called blooms. Blooms occur as a result of higher light levels and enhanced stratification, which increases the available nutrient concentrations near the surface where phytoplankton grow. Large green patches of ocean, marking regions with abundant phytoplankton, are even visible from space, and change the way the surrounding seawater reflects and absorbs sunlight. Scientists can exploit this fact to estimate phytoplankton biomass from optical measurements taken by satellites or by the bio-optical sensors on the SOCCOM floats.

To illustrate the importance of bio-optical data, as well as the science made possible by the SOCCOM float array, I’ll summarize some results from a recent paper that I led as part of my PhD thesis at Scripps Institution of Oceanography. In this study, we examined the drivers of the Scotia Sea phytoplankton bloom, which is the earliest and largest spring bloom in the open Southern Ocean. This can be seen from maps of satellite chlorophyll, a proxy for phytoplankton biomass calculated from optical measurements, which show high values in the Scotia Sea (outlined in red) while the rest of the Southern Ocean remains low.
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.

Although long-term satellite data clearly indicate that the bloom occurs in the same location around the same time each year, it’s difficult to know why since the satellites only measure surface properties and do not provide information about the physical processes that regulate phytoplankton growth. Therefore, SOCCOM floats, which simultaneously record physical and biological data throughout the upper 2000 meters of the water column, were essential in discovering what initiates and sustains the Scotia Sea bloom. Two floats, which captured the 2016 and 2017 bloom cycles in this region, revealed a close link between biological productivity and seafloor topography. The highest chlorophyll values were measured when the floats were trapped in a recirculating eddy that formed over an undersea mountain called Pine Bank. This is due to enhanced mixing when the current flows over the seamount, which supplies essential nutrients (in this case iron) from great depths to the sunlit upper ocean where phytoplankton can grow.
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.

Although this result is specific to the local topography in the Scotia Sea, several other phytoplankton blooms in the Southern Ocean are located close to topographic features, suggesting that this process may be important in other regions as well. Since phytoplankton abundance varies considerably in space and time, understanding what controls bloom location, timing, and magnitude, through studies like this, is necessary to model Southern Ocean food webs and biological effects on atmospheric CO2 levels.

And that is the power of bio-optical data! The information about phytoplankton biomass inferred from these measurements, combined with the physical parameters recorded by the floats, helped introduce a new conceptual framework for a bloom system that scientists had known about for decades. This highlights one of the unique aspects of the SOCCOM data: its' ability to relate changes in biogeochemical properties directly to their physical drivers. These results also demonstrate, as we saw in the previous post, how just a few floats in the right place at the right time can lead to new dynamical understanding of phenomena observed by satellites. In the remaining posts, we’ll see how the entire float dataset taken together can be leveraged to uncover new insights about global biogeochemical cycles.

- Channing

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March 30, 2020

This is the first post in a series about the different sensors on the SOCCOM floats and some of the recent scientific advancements that have been made using these data. We’re starting off with Conductivity Temperature Depth (CTD) sensors, which measure the temperature, salinity, and pressure (approximately equivalent to depth) of the water. These are the fundamental physical parameters in the ocean because they determine the density of seawater. Colder water is denser since the water molecules contract together at lower temperatures. Higher salinity water is denser since there is more stuff (salt) packed into it. Under high pressure (i.e. deeper) water gets compressed and thus denser. Changes in the temperature or salinity of seawater lead to gradients in density, which drive the currents in the deep ocean.

To illustrate the importance of temperature and salinity, as well as the science made possible by the SOCCOM float array, I’ll summarize some results from a recent paper led by University of Washington graduate student Ethan Campbell. Ethan’s study looked at the formation of polynyas, large holes in the winter sea ice, which formed over an undersea mountain called Maud Rise in 2016 and 2017. These were the largest such events to occur in the region since the 1970s (the holes in the ice were nearly the size of the state of South Carolina!), and scientists were stumped as to what caused the polynyas’ reappearance.
Satellite image of the 2017 polynya at Maud Rise (NASA Earth Observatory)

Collecting data within a polynya is extremely hard due to the remoteness of the formation regions and harsh weather. Therefore, SOCCOM floats provide an important source of information in ice-covered areas that are difficult to access by ship. In these icy locations, fresh water overlies warm, salty water. The cold surface water creates a barrier that prevents the ice from melting. During the polynya years, observations collected by SOCCOM floats show that the surface waters over Maud Rise were saltier and thus denser than usual. As a result, the density difference between the surface and deep ocean was small, allowing the water column to mix more readily. This led to an anomalously large heat transfer to the surface that melted the ice. Particularly strong storms during the polynya years also helped upwell warm water, establishing a feedback loop that prevented ice from re-forming and sustained the hole in the ice.
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)

Although the polynya formation is a local process, it could have large impacts on the climate system. For example, deep waters over Maud Rise are enriched in carbon (because they haven’t been in contact with the atmosphere for hundreds of years or more). This sequestered carbon can be released back into the atmosphere when the water gets drawn up by the polynya. By acting as a direct conduit between the surface and deep ocean, these holes in the ice can alter the exchange of properties at the air-sea interface. Therefore, accurately describing the dynamics of these systems, through studies like Ethan’s, is critical to improving future climate predictions.

And that is the power of temperature and salinity! These key ocean properties, measured by a few strategically placed SOCCOM floats, helped solve a decades-long puzzle about the drivers of open-ocean polynya events. Furthermore, the physical processes recorded by the floats can be linked to changes in ocean biogeochemistry using the properties measured by the other sensors. But I’ll talk more about that in future posts.

- Channing

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March 27, 2020 

Our final floats have been deployed! These were Floaty McFloatface, named by the Monterey Bay Aquarium in homage to the infamous Boaty McBoatface, and Sylvia Whirl, named by the Scripps Polar Center in honor of the legendary oceanographer Sylvia Earle and in reference to the Southern Ocean’s active eddy field.
Floaty McFloatface ready to join the fleet of SOCCOM floats collecting data
in the Southern Ocean. - photo by Channing Prend

Shortly after being deployed, the floats will sink down to 1000 meters depth (that’s more than half a mile below the surface!) where they’ll live for the next few years, drifting with the ocean currents. Every 10 days they will go down to 2000 meters and then rise up to the surface, collecting data as they go (which they will send back to us via satellite). Floaty McFloatface and Sylvia Whirl are the newest additions to a fleet of more than 150 SOCCOM floats measuring the physical, chemical, and biological properties of the Southern Ocean.
The blog author enjoying sunrise over the Atlantic before deploying Sylvia Whirl
(photo by Susan Becker)

In a series of posts, I’ll talk about the different sensors on the floats, what they measure, and some of the scientific breakthroughs that have already been made using this data. So stay tuned! In the meantime, I hope everyone back on land is staying safe and adjusting to the changes to daily life. I’m thinking of you all from the middle of the Atlantic Ocean!

- Channing

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March 26, 2020

It’s been a busy few days. Because of the ship’s orders to return to the US, all of our float deployments are occurring within the span of 3 days. Knight Drifter from Buckingham Brown and Nichols School and See Turtles from Winston Campus Elementary have both taken the plunge into the cold Southern Ocean waters.

The floats were deployed into calm seas. We have left behind the sea birds and dolphins near the coast. Here it seems desolate, empty. But we are only seeing the surface. Thousands of meters below us is an even more foreign world, where strong currents traverse undersea mountain ranges, and internal waves the size of skyscrapers break and mix the waters close to the seafloor. These are the forces that Knight Drifter and See Turtles will reckon with as they drift around collecting data.

The blog author standing proudly with Knight Drifter just before deployment. photo by Molly Martin.

See Turtles ready to begin its journey around the Southern Ocean. Photo by Channing Prend>

Now that the floats have been deployed, where will they go? This turns out to be a difficult question to answer since the ocean is immense, chaotic, and constantly in motion. Honestly, we don’t know exactly where the floats will travel; they are at the mercy of the waves and currents now. But we can predict where they are likely to go based on our knowledge of ocean circulation and statistics from floats that moved through this region in the past. Ultimately, only time will tell where the currents carry Knight Drifter and See Turtles. I’m excited to see where they end up though, because this information will help us determine the pathways by which the ocean transports heat, nutrients, and carbon around the world.


- Channing 

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March 24, 2020

When I left home several weeks ago, I couldn’t have imagined the magnitude of the global pandemic that I would soon watch unfold from port in Cape Town and from the deck of the R/V Ron Brown. With all the uncertainty in the world right now, our ship has understandably been recalled to the US. Before heading home, we’ll be taking a slight detour to deploy six SOCCOM floats, the only portion of our initial science plan that will see completion.

There have been numerous times when I’ve wondered whether it’s appropriate to be conducting fieldwork under these circumstances. It seems frivolous to worry about float deployments given the challenges facing those back on land, and I feel guilty for being somewhat sheltered from the barrage of news (by the ship’s limited bandwidth). But I have come to think that now, more than ever, our society needs science and science-based policy. The data collected by these floats will provide new insights about the ocean and climate, and in doing so, ultimately contribute to a better world. When viewed through this lens, our science mission takes on a whole new urgency. And on a personal level, I am grateful for the sense of purpose that this has afforded me amidst all the turmoil.
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

So today, a team of scientists worked together to deploy two SOCCOM floats: the Bobcat’s Be-bopping Bobber from Louisa County Middle School and Gloria’s Gulper from the Monterey Bay Aquarium Research Institute. It was not easy. We were battling large waves and high winds. Our boat was bobbing up and down in the swell like a toy sailboat, completely dwarfed by the immensity and sheer power of the ocean. Once the floats were in the water, we quickly lost sight of them. The storm seemed to have blurred the boundary between sea and sky. But as we sailed on to our next station, I had the distinct feeling that we’d done something important, not in spite of everything going on in the world right now, but because of it.

- Channing Prend

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