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After a long hiatus, the epic Ocean Race is back but this year, as well as dodging icebergs, cracking masts and suffering the occasional hull sandwich failure, the teams are gathering crucial data from places even research vessels rarely reach

Yvonne Gordon

Sat 25 Mar 2023 09.00 EDT

The Southern Ocean is not somewhere most people choose to spend an hour, let alone a month. Circling the icy continent of Antarctica, it is the planets wildest and most remote ocean. Point Nemo just to the north in the South Pacific is the farthest location from land on Earth, 1,670 miles (2,688km) away from the closest shore. The nearest humans are generally those in the International Space Station when it passes overhead.

But on 21 March, four sailing teams came through here part of a marathon race round the bottom of the Earth, from Cape Town in South Africa to Itaja in Brazil.

By the time these 18-metre (60ft) Imoca monohull sailing yachts neared Point Nemo, the five sailors on each boat had already been at sea for 23 days, with another two weeks to go before they reach port in early April. And this is just leg three, the longest portion of the even longer Ocean Race, a 32,000-nautical-mile dash around the world that started in January and finishes in July.

Competition is fierce and racing is close, even after three weeks at sea. Boat speeds on leg three so far have been up to 40.5 knots the equivalent of gale force winds and the vessels have, subject to ratification, broken the 24-hour distance record multiple times. The crews survive on freeze-dried food (rehydrated with hot water from a kettle theres no kitchen), and operate a four-hour alternating watch system. Nobody gets much sleep. The toilet is a bucket.

The dangers are unpredictable. Winds in the Southern Ocean can reach up to 70 knots and hitting an iceberg at speed would be catastrophic, so the boats have to steer clear of an ice exclusion zone around Antarctica. On 1 March, the Team Malizia crew discovered a crack at the top of the mast, requiring one of them to climb up 28 metres in rough seas to patch it over in the middle of the night. Guyot Environnement Team Europe had to abandon leg three completely after suffering a hull sandwich failure, spending three nervous days sailing 600 nautical miles back to Cape Town for repairs. The last time Team Holcim-PRBs skipper Kevin Escoffier raced here, his boat broke in half and sank and he was rescued from his life raft.

But while the Ocean Race is sometimes known as the toughest, and certainly the longest, professional sporting event in the world an event that began in 1973 as the Whitbread Round the World Race then became the Volvo OceanRace, and which attracts professional sailors of the highest level who join mixed crews every few years on sponsored teams to vie for an overall trophy (there is no cash prize) this year scientists have smelled an opportunity for them to benefit as well.

Because the boats visit the most remote part of the ocean, which even scientific vessels struggle to access, this year the crews will seed scientific instruments all around Antarctica, aiming to measure 15 different types of environmental data from ocean temperature and atmospheric indicators to concentrations of microplastic.

Information from the devices will help with everything from weather forecasting to insights into the climate emergency. The Southern Ocean is one of the planets largest carbon dioxide sinks, for example, but its inaccessibility has meant that there is relatively little CO2 data available.

The Southern Ocean is a very important driver of climate on a global scale [but] there is very little data, says Toste Tanhua, chemical oceanographer at Geomar Helmholtz Centre for Ocean Research in Kiel, Germany. Data from the sailing races in the Southern Ocean is very important for us to understand the uptake of carbon dioxide by the ocean.

Each boat is equipped with weather sensors on board that measure wind speed and direction, barometric pressure and air temperature. Each team will drop two surface drifter buoys provided by organisations such as Mto-France and the US National Oceanic and Atmospheric Administration, which capture data to help the World Meteorological Organization study ocean currents and forecast extreme weather events such as hurricanes.

A second type of buoy, the Argo profiler, deployed by Team Malizia in leg two, operates below the surface at depths of up to 2km, moving slowly with deep currents and transmitting information every 10 days. The data is used for climate analysis as well as for long-range weather forecasts.

Meanwhile, 11th Hour Racing Team and Team Malizia are using OceanPacks to take regular water samples to measure the levels of carbon dioxide, oxygen, salinity and temperature, to be analysed in Germany and fed to Socat, the Surface Ocean CO2 Atlas. Live dashboards give snapshots of the data as it is collected out at sea.

Tanhua says the fresh data reveals new patterns. For example, it shows how carbon dioxide varies over a year higher when the water warms up in summer, lower during a phytoplankton bloom. It also shows how the ocean takes carbon from the surface and transports it into the depths. In the Southern Ocean, you have three major frontal systems where water is either going down vertically (sinking) or coming up, Toste says. That has very different carbon levels. Eddies also transport carbon up and down. Scientists will now be able to observe these fronts and eddies up close, compare with satellite data and fill in the gaps.

The boats are also sampling trace elements such as iron, zinc, copper, cadmium, nickel and manganese, which are essential for the growth of plankton. Not only is plankton the base of the food chain, but phytoplankton are responsible for most of the transfer of CO2 from the atmosphere to the ocean.

This data is extremely important, says Dr Arne Bratki, environmental biogeochemist at the University of Lleida, Spain, who analyses the trace element results. It is important to know how much food is available for animals that will feed on phytoplankton eventually, and how much CO2 the phytoplankton is going to absorb from the atmosphere.

Bratki says that sampling such as this normally requires dedicated scientific voyages, on which places are limited and expensive. The Ocean Race is a way of testing investigations on non-scientific platforms at sea. We are paying attention to the design of the samplers what works and what does not, says Bratki. Its really exciting.

To add to the plankton study, Team Biotherm is working with the Tara Ocean Foundation to study ocean biodiversity, and the sailors have an automated onboard microscope to record images and provide insights into the diversity of phytoplankton species.

They are also studying oxygen. Dr Vronique Garon, senior scientist for Frances National Centre for Scientific Research at the Observatoire Midi-Pyrnes at the University of Toulouse, France, wants to better understand ocean deoxygenation, which is being caused by global heating.

Boats sail through remote parts of the world ocean where observations are really scarce, she says. Getting more oxygen data is invaluable to yield a better estimate of the ocean oxygen inventory and thus of the oceanic oxygen loss.

The more data we have, the more accurately we can understand the oceans capacity to cope with climate change and predict what will happen to the climate in future.

The 2017-18 race made headlines after samples taken near Point Nemo showed that even these remote waters are polluted with microplastics. This year, two teams, Holcim-PRB and Guyot Environnement, are again taking water samples to test for microplastics but can now also analyse them to determine their product source (for example, a bottle or plastic bag).

We still have a very poor understanding of the abundance and distribution of very small microplastics in the ocean, and its quite difficult to collect them, according to Dr Katsiaryna Pabortsava, a biogeochemist at the National Oceanography Centre in Southampton who is helping analyse the samples.

The Ocean Race will be delivering samples from places that otherwise wed have difficulty getting samples from, Pabortsava says. The other thing is the ease of collection of those samples. You dont need trained personnel, as you would have with research vessels. The hope is that this type of sampling could eventually be employed on other non-scientific ships, such as cruises or ferries.

The sailors benefit, too: in such a close and dangerous race (Team Holcim-PRB had a lead of 600 nautical miles at one stage, but light winds brought the pack together again and by 20 March just 5.1 nautical miles separated the four boats), every piece of information is vital.

Its a win-win situation, because six hours [after dropping the buoys], the sailors will download a new weather bulletin, using data from the buoys, says Martin Kramp, ship coordinator at OceanOPS, the monitoring, coordination and implementation support centre of the Global Ocean Observing System.

In such data-sparse areas as the Southern Ocean, [that] can make a significant difference the forecast will be much better.

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See original here:

The science of sailing: inside the race across the worlds most remote ocean - The Guardian