Exploring the Air Where Ocean Meets Atmosphere


Imagine standing on a beach, breathing in the fresh, salty air. Have you ever wondered what makes coastal air feel so special? The answer lies in marine aerosols—tiny particles from the ocean that influence sunlight and clouds, playing an important role in shaping our climate.

As part of my PhD research at Southern Cross University, I recently conducted a field trip to Heron Island. This research is part of the Cooling and Shading initiative in the Reef Restoration and Adaptation Program, which is funded by the Australian Government’s Reef Trust and the Great Barrier Reef Foundation, and led by Associate Professor Daniel Harrison of Southern Cross University

The Reef Restoration and Adaptation Program is a partnership focused on helping the Great Barrier Reef resist, adapt, and recover from the impacts of climate change. These efforts aim to protect the reef and buy time while we work as a global community to reduce CO2 emissions.

Heron Island is located in the southern Great Barrier Reef, about 80 km off Australia’s east coast (Figure 1). We respectfully acknowledge the Gooreng Gooreng, Gurang, Bailai, and Taribelang Bunda peoples as the Traditional Custodians of this Sea Country.

Map of Heron Island, Great Barrier Reef, showing flight sampling areas and measurements.
Figure 1. Heron Island is a coral cay in the Capricorn group, southern Great Barrier Reef, Australia (-23.439°S, 151.908°E). Sampling flights were conducted over four areas: near the island, the lagoon, the reef crest, and open water. Flights were timed for high or low tide. Measurements included air temperature, relative humidity, and atmospheric pressure, along with aerosol sizing and counting from 5.5 m to 105.5 m above the beach in 5 m intervals.
Map by Christian Eckert (Southern Cross University) (Source: Esri)

Discovering the Secrets of Coastal Air Using Drones

Marine aerosols form when the wind creates whitecaps on breaking waves, tearing tiny droplets from the wave crests (Andreae et al., 1985; Lewis & Schwartz, 2004). These aerosols are carried into the atmosphere by wind, which determines their movement both vertically and horizontally (Goroch et al., 1980; Lewis & Schwartz, 2004). Other factors like temperature, and humidity near the ocean surface also play a key role in how these aerosols behave.

However, studying marine aerosols in the critical first 100 m above the ocean surface has been challenging. Land and ship-based instruments can’t reach high enough, while planes fly too high to capture the details. That’s where drones come in.

Multirotor drones offer a game-changing solution. These drones are flexible, mobile, and able to hover precisely at different altitudes. They’re also emission-free, making them ideal for research in remote and environmentally sensitive areas (Burgués & Marco, 2020).

How We Used a Drone to Study Marine Aerosols

Our research used the Matrice 600 drone as a platform to carry specialized instruments. Underneath the drone, we attached a box containing a miniaturized Optical Particle Counter (mOPC) and a battery to power the equipment. The mOPC is capable of measuring aerosol sizes ranging from 160 nanometers to 3,000 nanometers.

To measure wind speed and direction, we integrated a TriSonica™ Mini 3D Ultrasonic Wind Sensor approximately 50 cm above the drone mounted to a carbon fibre tube. Placing it above the drone helped reduce interference from the drone's propellers. This sensor was connected to a Beaglebone Black development platform housed in a custom-designed, 3D-printed casing (Figure 2).

WindMaster 3D mounted on a drone with LI-550 TriSonica® Mini Wind and Weather Sensor.
Figure 2. The WindMaster 3D was equipped with quick-release mounts for installation on the drone. The LI-550 TriSonica® Mini Wind and Weather Sensor was mounted on a custom base plate and a carbon fibre tube to position the sensor above all other instrumentation, minimizing interference from the drone’s propeller downwash (A). A custom-made housing provided external access to a microSD card for data storage and included fans for ventilation. All inlets were fitted with filter material to protect sensitive components from the salty marine air (B).
Image by Adrian Doss (A), and Kim Monteforte (B) (both Southern Cross University)

Our Fieldwork on Heron Island

We completed about 80 successful sampling flights across four different locations: open water, the reef crest, the lagoon, and close to the island at either low or high tide. Each flight followed a precise strategy to ensure accurate data collection.

  • Hovering for Accuracy: Each flight began with the drone facing true north, hovering for 15 sec at 5-metre above its starting point. This step minimized the need for adjustments in wind speed and direction measurements caused by drone movements.
  • Ascending in Steps: After the initial hover, the drone ascended vertically in 5-metre intervals, hovering for 15 sec at each level until it reached a final altitude of 105-metres.

This systematic approach allowed us to gather consistent data on aerosols and wind conditions at various altitudes (Figure 3).

Drone take-off from the beach at Shark Bay, Heron Island.
Figure 3. Take-off from the beach on the eastern tip of Heron Island at Shark Bay. The vertical sampling missions were pre-programmed and automated, while take-off and landing were performed manually.
Image by Brendan Kelaher (Southern Cross University)

What Happens Next?

Now that we’ve returned from Heron Island, the next step is to analyze the data. We’ll investigate how aerosol size distributions vary and how meteorological conditions influence their behavior.

One exciting part of this research is comparing the real-world measurements with computer models of marine aerosol entrainment. By doing so, we hope to improve our understanding of how these tiny particles affect climate processes like solar radiation and cloud formation.

References

Andreae, M. O., Ferek, R. J., Bermond, F., Byrd, K. P., Engstrom, R. T., Hardin, S., Houmere, P. D., LeMarrec, F., Raemdonck, H., & Chatfield, R. B. (1985). Dimethyl sulfide in the marine atmosphere. Journal of Geophysical Research. D. Atmospheres, 90(D7), 12891-12900. https://doi.org/10.1029/JD090iD07p12891

Burgués, J., & Marco, S. (2020). Environmental chemical sensing using small drones: A review. Science of The Total Environment, 748, 141172. https://doi.org/10.1016/j.scitotenv.2020.141172

Goroch, A., Burk, S., & Davidson, K. L. (1980). Stability effects on aerosol size and height distributions. Tellus, 32(3), 245-250.

Lewis, E. R., & Schwartz, S. E. (2004). Sea salt aerosol production: mechanisms, methods, measurements, and models (Vol. 152). American Geophysical Union. https://doi.org/10.1029/GM152


Christian Eckert is a PhD candidate at Southern Cross University, focusing on atmospheric marine boundary layer dynamics as part of the Reef Restoration and Adaptation Program. His supervisors are Associate Professor Daniel Harrison and Professor Brendan Kelaher; both of Southern Cross University. Christian holds a Master's in Geomatics and a Bachelor's in Applied Geodesy and Geoinformatics from the Munich University of Applied Sciences. His professional experience includes working as a cadastral surveyor and for the Federal State of Schleswig-Holstein. Additionally, he is skilled in fine woodworking and holds a CASA Remote Pilot Licence.