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Anton and I have just brought CTD cast number 45 to light. While we are once again shaking freshly tapped bottles with great enthusiasm, I think I can make out question marks in Jamileh’s expression as she smiles good morning to us. That’s what everyone here seems to be thinking: 45 CTD casts already? And many of them in the same place? Why all this? We should know the water once we’ve “measured” it, right? Well, somehow we do.

1: Map of Madeira with all CTD stations performed so far (red dots)

“Our” CTD, which biologists prefer to call a “water sampler”, is moved out of the side of the hangar, lowered and in the basic version measures Conductivity (salinity), Temperature and pressure (Depth) quasi continuously (at 24 Hz), ideally down to the seafloor. In addition, oxygen and fluorescence are measured, which makes it possible to estimate biological productivity (see previous blog entries by Nicole and Manfred). As an addition, water samples can be taken at various depths using the 24 Niskin bottles (Manfred is by far our best customer in this respect). For oceanographers, however, the continuous measurements of temperature and salinity are of crucial importance, as they allow us to see how stable the water is stratified, for example, or to deduce the origin of the water masses and geostrophic currents. This is important information that forms the framework conditions that strongly influence the local ecosystem. In order to achieve maximum precision in the physical measurements, I take water samples myself “only” to calibrate the oxygen and salinity sensors later, but not to analyze the suspicious living beings in it.

2: This is where we “winkler”: The oxygen content of water samples is determined by titration. The results are used to calibrate the measurement results of the CTD sensors, which often have an offset.

Most of the deployments to date have been close to shore at a depth of about 1500 meters. The following figure shows one of our precious deeper profiles down to a depth of almost 3300 meters. Here, the top 100 meters form the so-called “mixed layer”, in which all measured variables are well mixed by the wind. We observe that the depth of this surface layer varies, but is generally comparatively thick – as is typical for the winter months at these latitudes. At our first station, the mixed layer depth was even around 200m! Temperature (red), salt (blue), oxygen (yellow) and chlorophyll (green) draw practically vertical lines in the diagram. Interestingly, a maximum of chlorophyll often forms exactly at or below the surface layer, which serves as an indicator for the presence of phytoplankton (see Nicole’s and Manfred’s blog entry on “Micro-Creatures”). Although phytoplankton is basically autotrophic, i.e. dependent on sunlight, it can survive in this rather deep layer with very little sunlight. One reason for this is the increased nutrient content in deeper layers.

3: An exemplary CTD profile from February 23rd south of Madeira, to a depth of about 3300m. Contains fluorescence (green), oxygen (yellow), salinity (blue) and temperature (red))

In addition, the pycnocline directly below the mixed layer forms a strong physical barrier to vertical mixing and can practically “trap” organisms that cannot actively swim themselves. The pycnocline is the layer in which the density of the water increases very rapidly with depth (here due to the temperature gradient). These layers contain a wide range of temperature and salt contents and are also called Central Waters. To identify water masses, temperatures and salinities are plotted against each other in a so-called “T-S diagram” (as shown in Figure 4). In our example, you can clearly see that the water around Madeira consists largely of Eastern North Atlantic Central Water (ENACW). This water mass dominates the pycnocline in the large North Atlantic Gyre and is significantly more saline than in the South Atlantic (see Eastern South Atlantic Central Water). In our profile number 41 (Figure 3), however, something else catches the eye. At around 1100m, there is a nose with a significantly higher salinity, which does not seem to match the linear Central Water. The influence of the Mediterranean Water (MW) is noticeable here, which has a particularly high salt content due to the predominantly high evaporation and low precipitation in the Mediterranean region.

Due to this high salt content, it manifests itself at greater depths, typically around 1100m to 1200m, despite the warm temperatures. However, we can also see in the T-S diagram that the Mediterranean water in the south of Madeira is already somewhat more mixed, i.e. less warm and saline than directly at the outflow of the Mediterranean. Even further down, which we can observe particularly well at our deeper CTD stations around 3000m, resides the famous North Atlantic Deep Water (NADW). This is formed by, for instance, deep convection in the North Atlantic and plays a central role in global thermohaline circulation and climate dynamics. Although constituting deep water, it is comparatively “young” and therefore rich in oxygen (we like to say “well ventilated”) and forms a contrast to the oxygen minimum, which we observe here around Madeira at around 800-900 meters. This minimum zone is formed by respiration of the sunken organic material, e.g. from the sunlight-dependent phytoplankton in the uppermost ~150 meters. Compared to the large known oxygen minimum zones in the subtropical eastern Atlantic and Pacific, however, there is still comparatively abundant oxygen.

4: The Temperature-Salinity diagram belonging to profile 41 in Figure 3. The letters indicate the typical temperature and salinity values of known water masses (see text).

Now, we know the profile of a single CTD station a little better. Basically, this one is actually fairly representative of the other 44, so the question of why Anton and I keep “driving CTDs” like madmen remains unanswered. However, if we take a closer look, we can see that the temperature and salinity profiles are not completely “smooth”. In fact, we discover small wavelike deviations. Measurement inaccuracies? No. It is internal waves that bring “life” to the profiles. Internal waves can occur in any stratified medium, i.e. fluids in which the density is not constant. There are two restoring forces that act on internal waves in the ocean: Gravity and the Coriolis force. The main drivers of internal waves are the tides (such as ebb and flow), closely followed by wind. We know that internal waves play a crucial role in energy transport in the ocean. Like ordinary surface waves, internal waves can also break. When they do, mixing takes place. This in turn can transport nutrients and thereby influence biological productivity. The interaction of internal waves with topography (i.e. islands such as Madeira) and currents is very complex and not yet fully understood. By using a large number of stations at different times (and tidal stages), we obtain a better spatial and temporal resolution of the internal wave field and improve our understanding. That’s also why we are fans of so-called “yo-yo CTDs”. Just like a real yo-yo, we move the CTD up and down several times in direct succession at one and the same location.

5: A “yo-yo CTD”. Like Figure 3, but six CTD profiles plotted on top of each other

In the figure above, we have plotted six directly consecutive profiles of a “CTD yo-yo” on top of each other. You can see that the profiles deviate more from each other at some depths and not at others (nodal points). The most impressive influence is exerted by internal waves on the mixed layer depth, which can vary by several tens of meters within minutes.

There is a particular thrill when the “Eddy hunt” is called for. That sounds more martial than it is meant to be. Eddies are oceanic vortices that reach a diameter of about 50 km around Madeira, interact with topography (islands) and internal waves and are known to have an impact on biodiversity. They develop over a period of days/weeks and are unfortunately hardly predictable. Therefore, we check satellite and model data for the region daily to identify a possible feature and, if possible, sample in situ with Merian. Strong eddies can generate a signal in sea level, surface temperatures and chlorophyll, recognizable via satellites. Our colleagues from the Oceanographic Institute of Madeira are helping us on site by providing the regional satellite and model data (see https://oomdata.arditi.pt/msm126/). Overall, it is impressive how well the collaboration on board and beyond works! One “eddy hunt” has already taken place on the night of February 13-14. However, the satellite signal was weak, and accordingly we were unable to detect a strong, coherent eddy In Situ with our shipboard ADCP (Acoustic Doppler Current Profiler, which measures ocean currents down to a depth of almost 1000m). (Side note: However, another exciting feature (presumably a strong internal wave) was identified in the surface layer, which we are now analyzing.)

6: Eddy hunt! The rough plan for a “spontaneous” survey of the potential eddy. There was a weak satellite signal for the one negative anomaly in the sea level (blue contours). The red line indicates the planned track and the purple triangles indicate the planned CTD stations.

In one of the following contributions, we want to prove to you that our beloved CTD is something very special in purely “objective” terms thanks to sophisticated tuning, including high-resolution camera systems. Then we’ll explain why Anton, although he’s not a physical oceanographer, also likes to drive “CTD yo-yos” and there will finally be photos of aquatic animals again!

Greetings from on board RV MARIA S. MERIAN,

Marco Schulz und Anton Theileis

A physical oceanographer alone among biologists

Ocean Acidification

Barnacles, buoys and boat engines: researching the effects of underwater sound in Malaysia

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Leonie (left) and Najwa (right) in front of the CEMACS jetty (© Izzat).

Selamat Datang and welcome to the hot and sweaty country of Malaysia! Ever since we, Leonie and Najwa, have arrived in Penang, the northwestern island of Malaysia, in April this year, it has been a constant 30 degrees with an average humidity of 70%. However, it feels both hotter and more humid than that. Unfortunately, the weather will not change much during our stay as Malaysia lies very close to the equator (at latitude 5°N). Thus, it has no seasons, but a nearly constant temperature and day/night rhythm of 12 hours.

Beginning to adapt

The sun is just peaking above the sea when I (Leonie) have to leave my house. The bus leaves (more or less) always at the perfect time to watch the sun slowly rise over the ocean. I use the 30 min bus ride, which costs me about 2 Ringitt (or ~20 cent), to wake up and prepare for the day ahead at the Centre for Marine and Coastal Studies (CEMACS). During the bus ride beaches, restaurants, cafés and small towns pass by in the window. Especially, one secluded beach and its beach house, which is for sale, make the bus ride go by fast – thanks to daydreaming about living there. When I arrives at 8 am at the entrance to the National park, in which the institute is located, Najwa is already waiting for me. She only needs a 5 minute car ride to get there from home, since she found an apartment close by. Now we just have to wait for the boat to take us to the institute within the national park. Technically, a 40 min hike through the park would also do the trick, but both of us are not ready for such a sporty activity at 8 in the morning and a daily boat ride is so much more fun anyways.

CEMACS lies in the heart of the Taman Negara Pulau Pinang, the national park of the island of Penang in northwestern Malaysia. Because of that, it’s quite a way to the big city of Georgetown and thus sources of noise, disturbances and pollution are far away. This is especially important for this year’s GAME project as we aim to find out whether underwater soundscapes influence the formation of hard-bottom communities.

Leonie taking a nap on the beach during lunch break (left, © Najwa).
The sunset by the institute (right, © Leonie).

We are trying to find answers to this question in the warm and salty ocean right in front of the gates of CEMACS. For that we deploy large metal frames that carry settlement panels into the sea. Two of those frames will additionally be equipped with an underwater speaker with which we can playback – in principle – any kind of sound we like (trust me, it was tested and it was a good day). To distinguish between the experiments that the two of us will conduct, we will use different soundscapes. One will focus on anthropogenic noise, i.e. the sound that is emitted by either a fishing or a container vessel. The noise will be played back at random times during the day, but will accumulate to a total of 30 minutes every hour. The other team member will focus on a natural soundscape that will be recorded at a healthy underwater location close by. The settlement panels will be retrieved regularly in order to find out how and if the playbacks are affecting the composition of the establishing hard-bottom communities.

The set-up of our ambient frame without (left) and with the dummy speaker (right, ©Leonie).

Sounds easy enough, yea? Technically it is, but the nature can be treacherous around here. Jellyfish, like the Ribbon Jellyfish (Chrysaora chinensis), are daily visitors and as pretty as they are, as much does it hurt to get stung by them. After some painful incidents, we now wear full body coverage whenever we are in the water to minimize the skin contact. One person, who stands on land, is always watching the water surface to give a warning in case one of us comes too close to one of the jellies. It’s important to always have someone watching, since we don’t see a lot when we are in the water ourselves. The visibility can be so poor that you cannot even see your hand in front of you. Which is why we struggle to detect the up to 50 cm long tentacles that can sting us. The jellies drift with the currents and like to hang around the jetty, where our frames are deployed.

Leonie and Najwa successfully retrieving all the HydroMoths (hydrophones) (top left, ©Izzat). Buoys that mark the position of one experimental frame near the jetty on a calm day (top right, ©Leonie). Najwa and Leonie attaching PVC settlement panels to the frames in the water (bottom left/right, ©Izzat).

But even on the land, it’s not entirely safe. Since CEMACS is in the middle of the national park, it is not uncommon to see animals around the institute. The cats and even the lizards are rather cute to look at but the monkeys and the mosquitos? A nightmare! Before the morning boat even leaves at 08:10 both of us already have 5 mosquito bites, a constant buzzing in the ear and are always itchy. Want to have your lunch by the water on the beach? Think twice because monkeys can and will steal your food. Even the laboratory is not safe and has to be locked up monkey-proof.

A ribbon jellyfish (left) and our technical equipment box locked to keep it safe from the monkeys (right, ©Leonie).

When we are not blasting ABBA or LinkinPark while setting-up our experiment or trying not to get stung by jellyfish during maintenance work in the water, we can actually enjoy Georgetown. The city is about 1 hour by bus from our living quarters and offers the exact opposite of CEMACS. It is loud, full, bright and brimming with life (humans, not animals). Due to its rich mix of Malay, Chinese, Indian and indigenous cultures clashing together, you can find every kind of food downtown. From delicious savoury food over sticky fruits and drinks to sweet desserts. You can find these tasty items all over the island often in hawker stalls or cute restaurants. Of course, you can also go shopping wonderfully (much to the dismay of Leonie and her limited baggage weight for the flight back home) or just walk around the town and get swept up by the street murals, salty breeze and picturesque buildings.

A traditional dish – Roti Kari, very tasty! (top left). The bottom left and right picture show Love Lane and Umbrella Lane within downtown Georgetown, which are popular for going out and shopping (©Leonie).

Do we have to restart?

The deployment of our frames went smoothly, attaching and retrieving the HydroMoths (i.e. hydrophones) went smoothly, and the preparation for the sampling week went smoothly. Probably, everything went a bit too smooth in hindsight, because when the sampling week arrived, nothing went smoothly.

We seemingly lost our entire control frame (i.e. frame without sound playbacks).

During our daily boat ride towards CEMACS we have normally perfect view to see the white buoys of our control frame floating in the distance. Except on that Tuesday. The weather was a bit rough over the weekend and it was still windy and wavy, so we tried to argue that the glare of the sun plus the waves are messing with our eyesight. Surely, we would see it once we get out there to take off and analyse our panels. But when our boat reached the exact coordinates, at which we deployed the frame, there was nothing. No buoy. No rope. No frame. No hint whatsoever. Immediately, we got into the water and were searching the area with the help of two colleagues. But still, we found nothing. The visibility was not in our favour and Najwa got stung by a jelly, what didn’t make the situation better.

After we had to realize that the possibilities were high that our frame got either stolen by someone or it got washed away during the storms, we accepted defeat. Over the next couple of days, we were analysing the panels from the frame with sound playback (aka speaker frame) and discussed options with our supervisors. Upon agreement we started one more search and rescue mission. This time we were dragging an anchor across the seabed for quite some time. Clammy hands, shallow breath and elevated heartbeat. Everyone on the boat was on edge after 30 min of searching. Our colleague held up his hand. The boat stopped. He got something. To everybody’s surprise he pulled up our control frame!! It was completely covered with barnacles, so that the frames and panels were barely distinguishable but we got it back. It obviously became to heavy for the buouys that we attached to it and sank to the seafloor. Immediately, we got to work: Pulling the frame onto the boat, cutting off each panel to inspect it in the lab and cleaning the frame (which was equally stinky, disgusting and difficult).

Finding the ambient frame and pulling it out of the water (top left, ©Najwa). Najwa is cleaning the barnacles off of the frame (top right, ©Leonie). Our ambient frame on the boat after we pulled it out (bottom left) and the cleaned-up frame shortly before we deployed it again (bottom right, ©Leonie).

Now the hard work began: analysing the panels. We first weighed and photographed them to estimate the biomass and the degree of coverage on them. Then each and every panel needed to be inspected through a stereomicroscope to identify as many organisms as possible. Most of the panels were covered with barnacles, to be precise it was Amphibalanus amphritite. But apart from that we also found some worms that built themselves tubes on our panels (probably individuals from the family Sepulidae and Spionidae) and were thus sessile too, some bryozoans, colourful tunicates and a lot of small shrimps, crabs and flatworms that were roaming around. Just within four weeks, the sad-looking grey PVC panels have become a location for the smaller animals of the ocean to settle and start their lives.

A juvenile crab found on our panels in between the barnacles (top left), some Ascidiacea on the panels (bottom left) and the barnacle Amphibalanus sp. next to some bryozoans (right, ©Leonie).

Before we deployed the frame again, we attached a total of 13 buoys and have now a little buoy party in the water which never fails to make us giggle. They are supposed to prevent the frame from sinking again.

Leonie deploying the ambient frame after the first sampling event with the newly added buoys (©Haziq).

The natural soundscape dilemma

Now that Leonies experiment is running (more or less smoothly) it is time to concentrate on the preparation for Najwas experiment which will focus on the natural soundscape.

At first, CEMACS and Penang seemed like the perfect place to begin collecting natural soundscape recordings. We believed it would provide a healthy, natural, and undisturbed underwater acoustic environment. However, despite being located in the national park with little human activity per se, Penang is one of Malaysia’s busiest coastal regions. The constant movement of ferries, fishing boats, tourist vessels, and commercial shipping creates a persistent layer of anthropogenic noise beneath the water. Instead of capturing the quiet rhythms of marine life, many of the recordings that we made were dominated by human activity. It became clear that Penang was not the ideal location for getting an undisturbed soundscape on tape. But where can we find that?

The search led us to Langkawi, an archipelago of 99 islands located just 100 km north of Penang near the border with Thailand. Renowned for its clear waters, rich marine biodiversity, and relatively low levels of coastal development in certain areas, Langkawi offered a far more promising environment for natural underwater acoustic recordings.

Within Langkawi, our attention turned to Pulau Anak Datai, a small island situated off the northwestern coast of the main Langkawi Island. It’s surrounded by coral reefs, rocky shorelines, and lush tropical rainforest. Compared to many of the more popular tourist destinations in Langkawi, Pulau Anak Datai experiences considerably less boat traffic, allowing its underwater environment to retain a more natural acoustic character. These conditions make it an ideal site for our needs.

With the study site finally selected, the next challenge was deploying the HydroMoths.

Concrete blocks with metal poles (left). Najwa on the way to Anak Datai Island together with Izzat (left) and Mr Suhardi (right, ©Najwa).

The recordings were scheduled over five consecutive days, with two HydroMoths deployed simultaneously to maximize the number of sites we could survey. To secure the HydroMoths underwater, we brought along two concrete blocks fitted with metal poles from CEMACS. These were previously used by another GAME team, and at the time, they seemed like the perfect solution. The concrete blocks were heavy, stable, and, most importantly, gave us peace of mind. We were worried about the HydroMoths moving with waves and currents, creating unwanted handling noise in the recordings. We were also concerned about the possibility of losing the devices whether due to storms, strong currents, or even someone discovering and taking them. But due to the seabed at Pulau Anak Datai being covered in rocks, corals and just life, it was difficult to position the blocks securely. The handling became a struggle, above and underwater.

No, we needed to adapt. Field work has a funny way of destroying the illusion of a thought through plan and pointing out every little flaw. We thought the original plan was fool proof. Turns out, it was not.

Giant clamps, soft corals, anemones and clown fish that we found in Anak Datai Island during the HydroMoth deployment for natural sound recording (©Najwa).

After surveying the area more closely and brainstorming some ideas, we purchased ~100 cm long metal poles, which we would simply hammer down into the ground between the corals. We then could attach the HydroMoths onto them. Fool proof, for real.

The new setup was lighter, easier to transport, quicker to deploy, and required only a fraction of the energy needed for the concrete blocks. What initially felt like a major setback showed us that flexibility and adaptability are the most important qualities during field work. And keeping a cool head, which can be the most difficult part.

Najwa is now owner of hours on end of the natural underwater soundscape in Langkawi. In order to actually use it as a playback, though, she has to listen, filter, crop and edit the recordings.

A HydroMoth attached to metal pole that was anchored in a concrete block (top left). Hydromoth attached to a 100 cm metal pole (top right). Najwa inserting a metal pole with a HydroMoth for recording (bottom left). Najwa with two HydroMoths on the last day of a natural sound recording trip in Langkawi (bottom right, ©Najwa).

Every obstacle from searching for a truly natural soundscape to redesigning our deployment method became a lesson that no classroom could have taught. In the midst of our experiment, we are still learning to adapt, be patient with ourselves and stay curious about the processes and solutions that fieldwork demand. The ocean rarely follows our plans, but perhaps that is exactly what makes studying it so rewarding. Jumpa lagi! (See y’all!)

Barnacles, buoys and boat engines: researching the effects of underwater sound in Malaysia

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Ocean Acidification

The jellyfish we see are only half the story

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When moon jellyfish gather in large numbers, the bloom is impossible to ignore. Hundreds or thousands of medusae can suddenly fill a bay or fjord. Because this swimming stage is so visible, it is often the focus of monitoring and research. But the familiar jellyfish is only one chapter in a much more complex life cycle. Before entering the open water, moon jellyfish can spend years as tiny polyps attached to rocks, algae or other hard surfaces on the seafloor. These polyps reproduce asexually and release young jellyfish when conditions are suitable. Our new study in Trondheimsfjorden, Norway, shows why this hidden stage deserves much more attention. The central finding is that the stage that moves the least may be the stage that gives a jellyfish population its greatest stability.

Image courtesy: https://sciencedigest.org/facts-about-jellyfish/

One animal two worlds

Moon jellyfish (Aurelia aurita) alternate between two contrasting habitats. Polyps remain attached to the seabed and can persist locally for years. Medusae live in the water column for a much shorter time and can be transported by currents across the fjord.

This creates an ecological puzzle. If medusae can travel widely, should populations throughout a fjord become genetically well mixed? Or can local structure survive because the stationary polyp stage retains diversity in particular places? Our new study in Trondheimsfjorden, Norway, shows that these hidden polyps may be crucial for maintaining genetic diversity. We combined field observations, genetic analyses of 572 samples and a model of movement through fjord currents. We found 70 genetic variants—and a striking difference between life stages.Polyps consistently held high genetic diversity. Medusae varied much more between places and years and were sometimes dominated by only a few variants. The polyps therefore appear to act like a biological seed bank: many possibilities remain stored out of sight, while each year’s conditions determine which ones emerge.

Currents alone could not explain the genetic patterns: the model predicted more mixing than was observed among medusae. Transport is therefore only part of the story. Local retention, temperature, food, survival and reproductive timing can filter which variants reach the visible stage.

This matters because jellyfish blooms affect food webs, fisheries, tourism and coastal infrastructure. Better forecasts will require more than counting medusae or following currents. We must also monitor polyp habitats and understand what controls transitions between life stages.

The wider lesson is simple: to understand the connectivity and resilience of marine organisms, we cannot study only the most visible, or most mobile part of their lives.

Paper: Majaneva, S., Ellingsen, I., Javidpour, J. and Aberle, N. (2026). Benthic life stages retain fjord-scale population structure despite pelagic dispersal. Frontiers in Marine Science, 13:1895768. https://doi.org/10.3389/fmars.2026.1895768

The jellyfish we see are only half the story

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Ocean Acidification

What are Tire Wear Particles?

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What do you think about when you hear the words “microplastic pollution?” Your mind may immediately go to imagery of colorful fragmented plastics broken off from bottles, buckets and other items we use in our everyday lives. Or, perhaps, you imagine a pile of microplastic fibers—the tiny, squiggly, spaghetti-shaped plastics that shed from our synthetic clothing. You may be surprised to hear there is another major source of microplastic pollution that’s hiding in plain sight, quite literally under our feet, that might change how you think about microplastics: tire particles.

We all know tires wear down over time—that’s why we have to replace them on our cars roughly every 60,000 miles or so. Every time a vehicle accelerates, brakes or simply drives down the road, the friction between its tires and the pavement creates tiny fragments of rubber, known as tire wear particles.

Driving a car or even riding in a bus is a bit like dragging an eraser across the planet, except the crumbs are microplastics. Toxic microplastics.

Dr. Britta Baechler
Director, Ocean Plastics Research, as quoted in Eos magazine

Tires are made from a complex mix of natural and synthetic rubber along with a range of additives, fillers and chemical compounds—some of which, like the preservative 6PPD, have been shown to be highly toxic to coho salmon when they break down into derivative product 6PPD-Q in the environment—even in tiny concentrations.

Some studies have shown that a single vehicle’s tires can emit more than two trillion particles per mile driven—and that the average person generates nearly two pounds of tire particles per year! Once these particles are shed from tires, they don’t just disappear. Some are small and light enough to become airborne, drifting away from roadways as dust. Others settle on road surfaces, where they accumulate until the next heavy rain washes them into storm drains and from there, into streams, rivers and eventually the ocean.

That’s why tire wear particles are now considered one of the top sources of microplastics to the environment. In fact, until recent developments in analytical methods, scientists weren’t reliably able to detect tire wear particles in microplastic counts—thus, these pesky microplastics may have been evading our detection for years.

Why green infrastructure may be one of our best near-term solutions

Unlike some sources of plastic pollution, we can’t simply stop driving overnight. Reformulating tire rubber to be less toxic or shed less material, while promising, will take time to develop, test and scale across the global vehicle fleet. So, what can we do about tire wear particle pollution right now?

This is where green infrastructure comes in. Green infrastructure refers to engineered natural systems (things like bioswales, rain gardens, roadside buffers and permeable pavement) that are designed to slow down, filter and treat stormwater before it reaches rivers, lakes and coastlines. Instead of routing runoff directly into storm drains and out to sea, green infrastructure gives contaminated water a chance to percolate through soil, plants and other natural filtration media, which helps trap microplastics, including tire wear particles, preventing them moving further downstream.

Early research on green infrastructure has been promising, showing that these systems are quite effective at capturing microplastics and other contaminants carried in road runoff. But there’s a critical piece we still don’t fully understand: What would it take to scale up green infrastructure across an entire city, and how much of a dent would that actually make in long-term tire wear particle pollution?

Our research on green infrastructure capture of tire wear particles

Funded by the Tire Industry Project, our plastics science and policy teams at Ocean Conservancy have partnered with the University of Toronto on a new study evaluating the costs and benefits of scaling up green infrastructure at the city level specifically to capture tire wear particles.

If you happen to be driving on the roadways of Portland, Oregon, you may spot our scientists crouched over, precariously scooping dirt with spoons from a sample area on the roadside. Don’t be alarmed—that’s just us doing science! Feel free to give us a wave.

Ocean Conservancy is currently working to:

  • Quantify the scale of pollution: Collect road dust samples from 30 cities globally to measure both total microplastic and tire wear particle concentrations and determine how different variables (population density, road size, rainfall) might influence those values.
  • Assess feasibility: Determine what it would take realistically—logistically, financially and spatially—to scale up green infrastructure across an entire city.
  • Model positive impacts: Estimate how much city-scale green infrastructure could reduce tire wear particle pollution entering aquatic ecosystems.
  • Compare across cities: Understand how well these solutions might translate across different urban contexts, focusing on Portland, Oregon; Toronto, Canada; and London, England as case-study cities.
  • Make our findings accessible: Produce a public-facing toolkit to help city planners, engineers and advocates guide real-world implementation of infrastructure that captures tire-wire particles. 

By pairing rigorous science with practical guidance, we hope to help cities move from asking “Could this work?” to confidently building solutions that we know can be effective.

Give today and make a difference!
We are on the front lines of ocean protection, investing in research, leadership and advocacy that advances evidence-based solutions that work.

How can I help?

Tire wear particle pollution can feel like an overwhelming problem. After all, it’s tied to transportation, which most of us rely on every day. But that’s exactly why research like this matters: It gives us a real, near-term path forward that doesn’t require waiting for the entire global transportation system to change first.

You can help by staying engaged with Ocean Conservancy as we continue to dig into solutions for the plastic pollution crisis—one roadway, one storm drain and one city at a time. Together, we can keep working toward a world and ocean free of plastic pollution, forever and for everyone.

The post What are Tire Wear Particles? appeared first on Ocean Conservancy.

What are Tire Wear Particles?

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