A synthetic seep generator for calibrating gas bubble echo sounding data is deployed into New Zealand’s Bay of Plenty.
A synthetic seep generator, used to calibrate echo sounding data from naturally emitted gas bubbles, is deployed into New Zealand’s Bay of Plenty. A recent study of bubble streams emitted from hydrothermal vents beneath the bay’s surface has provided a foundation for developing methodologies to identify and characterize gases (including greenhouse gases) emitted from the ocean floor using solely their acoustic response. Credit: Tom Weber, University of New Hampshire

In July 2018, our research group set sail for the Calypso hydrothermal vent field in New Zealand’s Bay of Plenty aboard the New Zealand flagship R/V Tangaroa. The voyage was dubbed Quantitative Ocean-Column Imaging (QUOI). Our mission: Find bubbles—lots of them—and record everything they told us about themselves.

The vent field (Figure 1) did not disappoint: It emitted diffuse streams of carbon dioxide and discrete seeps of methane. Our ship’s echo sounders sent out acoustic waves, and we recorded the echoes that these bubbles generated in response. The ways that these echoes varied, depending on the depth of the bubbles and the angles and frequencies of the incoming acoustic waves, provided a wealth of information.

We wondered whether we could use acoustics to fingerprint bubbles in the ocean.

The world’s oceans are full of bubbles. They come from natural sources like dissolving organic matter and gases seeping from great depths below the seafloor and from human sources like leaky oil and natural gas wells and pipelines. Many of these bubbles rise to the surface and release greenhouse gases like carbon dioxide (CO2) and methane (CH4) into the atmosphere.

Some research expeditions have collected preliminary information on bubble streams that they discovered by chance while using echo sounders to map the morphology of the seafloor or search for fish aggregates and even using seismic equipment for subseafloor investigations. Our group wanted to dive deeper into the information that ocean bubbles provide. We wondered whether we could use acoustics to fingerprint bubbles in the ocean.

Map showing the location of the Bay of Plenty off the northern coast of New Zealand
Fig. 1. The Quantitative Ocean-Column Imaging (QUOI) mission visited the Calypso hydrothermal vent field off the northern coast of New Zealand in the Bay of Plenty. The black and white inset shows a wider view of northern New Zealand, with the area of the larger figure outlined by the black box.

Gathering Clues from Bubbles

Many scientific, industrial, and environmental enterprises make use of the ability to detect, characterize, and quantify bubbles generated from liquid or gaseous features in the ocean, but observations enabling us to measure the volume or identify the types of gases that are released from the seafloor are scarce. Such observations are important as inputs into global carbon cycle models, in helping monitor deep-sea wells and pipelines for potential gas leaks, and in mitigating the associated environmental and economic risks.

Modern echo sounders have been able to image bubble streams in the ocean and trace their movement and behavior as they rise through the water column. To date, analysis of such acoustic data has been largely restricted to localizing and mapping sources of bubbles on the seafloor [e.g., Skarke et al., 2014]. Although there has been some recent progress, it has been more difficult to use echo sounders to quantify and characterize bubble streams (numbers of bubbles, geometry, and composition) and, ultimately, the associated volumetric and mass flow of gas [e.g., Greinert and Nützel, 2004; Weber et al., 2014; Veloso et al., 2015; Weidner et al., 2019].

Differentiating between gas types such as CH4 and CO2, the two most common greenhouse gases released at the seafloor, solely from their acoustic response remains a major challenge. Recent advances in echo sounders, including in our ability to calibrate and use them over a wide range of frequencies and to visualize and analyze their data, have provided a technological arsenal that we can bring to bear on this challenge.

Map of the Calypso hydrothermal vent field indicating sites where researchers deployed acoustic devices
Fig. 2. The QUOI voyage deployed a variety of acoustic devices over the Calypso hydrothermal vent site to study acoustic flares associated with gas bubbles. Red stars indicate very active flares of interest (FOI). Crossed circles indicate failed sampling stations. Brown dots show where sediment samples were collected to ground truth data on seafloor backscatter associated with the flares.

The 3-week QUOI voyage on board R/V Tangaroa used this arsenal to generate a unique data set over the Calypso hydrothermal vent field (Figure 2). The voyage benefited from a 3-year Catalyst: Seeding project, funded by the Royal Society of New Zealand. The project, which launched in April 2017, established a consortium of experts in marine geology, geophysics, and acoustics from seven countries. The data set is now enabling the team to advance the research looking at multidimensional acoustical analysis of the water column, a kind of marine acoustic forensics analysis.

How Do You Characterize a Bubble?

One of the most remarkable of the numerous gas seepages over the New Zealand continental shelf is the Calypso hydrothermal vent field [Stoffers et al., 1999]. Vents emit large bubble streams that can show up on ships’ sonars as gas flares (also called gas plumes). Yet many previous surveys only serendipitously imaged the seeps. These images enable qualitative observations, but gas bubble streams cannot be characterized with conventional oceanographic surveys, which provide only partial physical information on individual bubbles.

Synthetic image of the Calypso hydrothermal vent field showing sites where streams of gas bubbles rise from the seafloor
A synthetic image of the Calypso hydrothermal vent field showing sites where streams of gas bubbles rise from the seafloor. Credit: Erin Heffron

Our project enables us to move beyond locating and defining the shape of the flares to assess the bubble size distribution, differentiate between CH4 and CO2 gases (both of which are known to be released at the Calypso vents), and eventually develop rapid, cost-effective methods of estimating the bubbles’ greenhouse gas flux through the water column.

The intensity of a bubble’s acoustic signal—and whether it generates an echo on a ship’s sonar screen—is related to the bubble’s acoustic scattering cross section, which quantifies the ability of a bubble to reflect the acoustic energy of an incoming acoustic wave back to the echo sounder. This physical (measurable) parameter depends on the geometry, resonance frequency, and damping properties of the bubbles, as well as on the nominal frequency and incident angle of the incoming wave [Clay and Medwin, 1977].

The need to understand how these physical parameters influence acoustic measurements highlights specific requirements for quantitative description of water column gas bubbles. These requirements include calibration of the acoustic devices used to study the bubbles [Ladroit et al., 2018], multifrequency measurements of the backscatter strength of individual bubbles within a plume [Le Gonidec et al., 2002] and how the frequency response of a bubble changes with the ensonification angle (the angle between the sonar beam and the vertical at the point where the beam reaches the bubble), and visual observations for ground truthing. We carried out all of these experiments in 180-meter water depths during the QUOI voyage.

The design of the QUOI voyage included very large overlaps of the sounder seafloor footprints, with up to 95% overlay of adjacent swaths (Figure 3). This enabled us to generate high-resolution images of both the seafloor and the water column, as well as full ensonification of bubbles—immersing them in sound waves with incidence angles from the vertical to a grazing angle of 60°. We were thus able to observe bubble flares from a range of incidence angles. We conducted a robust and complete calibration of all systems at the start of the survey to enable cross correlation between the multiple echo sounder systems. The swath echograms revealed the presence of multiple acoustic flares, and the map of the sum of all echoes within the water column projected on the seafloor highlighted the importance of both the geometry and intensity of the flares and the spatial distribution of the vents on the seafloor (Figure 4).

Sketch of the QUOI acquisition protocol over a bubble seep
Fig. 3. Sketch of the QUOI acquisition protocol over a bubble seep to assess the frequency and angular dependency of the bubble backscatter strength using multibeam and single-beam echo sounders simultaneously in the range of 18–200 kilohertz. The image demonstrates the high swath overlap on the seafloor.
Swath echograms recorded by a multibeam echo sounder over a gray scale map of the seafloor reflectivity
Fig. 4. Swath echograms recorded by a multibeam echo sounder (illustrated in the inset) over a gray scale map of the seafloor reflectivity (backscatter). The elongated red patches on the seafloor correspond to the vertical echo integration of water column backscatter data: They highlight positions and extensions of flares on the seafloor (processed using the SonarScope software by Institut Français de Recherche pour l’Exploration de la Mer (Ifremer)).

Our Technological Arsenal

Fully characterizing the bubbles required us to explore different echo sounder deployment methods and data acquisition procedures. We used multiple synchronous echo sounders to assess the backscatter strength of targets at different frequencies:

  • EM302 and EM2040 multibeam echo sounders collected echo amplitudes athwart and along track simultaneously at 30 and 200 kilohertz.
  • An EK60 vertical echo sounder operated simultaneously at 18, 38, 70, 120, and 200 kilohertz.
  • A wideband EK80 transducer mounted on a rotatable system emitted pulses in the frequency range of 84–270 kilohertz at different incidence angles.

The voyage deployed three technologically and scientifically innovative systems.

The voyage deployed three technologically and scientifically innovative systems. A mobile unit with a split-beam echo sounder that operates at 38 or 120 kilohertz was deployed directly on the seafloor to ensonify bubble streams horizontally. This generated contrasting images from a different point of view—sideways rather than top down. For 5 days, an autonomous hydrophone placed in the center of a large flare field recorded bubble sounds. We also deployed a synthetic seep generator (or bubble maker) on the seafloor to establish a control data set for many of the bubble parameters. The seep generator creates bubbles with known properties and at known rates and sizes. It allows us to develop an empirical model to which data from natural sites can be compared and to develop a quantitative approach to estimate bubble flux rates.

We collected sediment and water samples for ground truthing of the acoustic signals across the entire Bay of Plenty survey site (Figure 2, brown dots). Video transits allowed us to directly observe most of the active vents identified from high-amplitude echo integration of water column acoustic data (Figure 5, large red spot).

Example of a vertical echo integration in the Calypso hydrothermal vent field. The red patches identify active vent fields
Fig. 5. Example of a vertical echo integration in the Calypso hydrothermal vent field. The red patches identify active vent fields.

This original, diverse, and multifaceted oceanographic survey has provided us with a data set from which we can develop robust water column surveying methodologies. We anticipate that this will lead to new protocols in identifying, quantifying, and classifying gas bubble streams in the ocean water masses. The QUOI experiments will advance understanding of active geological systems and the relationship the seabed has with the atmosphere.


This project is funded by the Royal Society of New Zealand Catalyst: Seeding fund. The QUOI voyage on board R/V Tangaroa was funded by the National Institute of Water and Atmospheric Research. V.L. was supported by the Marine Biodiversity Hub through funding from the Australian government’s National Environmental Science Program.


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Author Information

Geoffroy Lamarche (geoffroy.lamarche@niwa.co.nz), National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand; also at University of Auckland, New Zealand; Yves Le Gonidec, Centre national de la recherche scientifique University of Rennes 1, France; Vanessa Lucieer, Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia; Yoann Ladroit, NIWA, Wellington, New Zealand; Tom Weber, University of New Hampshire, Durham; Arnaud Gaillot, Institut Français de Recherche pour l’Exploration de la Mer (Ifremer), Brest, France; Erin Heffron, University of New Hampshire, Durham; and Sally Watson and Arne Pallentin, NIWA, Wellington, New Zealand


Lamarche, G.,Le Gonidec, Y.,Lucieer, V.,Ladroit, Y.,Weber, T.,Gaillot, A.,Heffron, E.,Watson, S., and Pallentin, A. (2019), Gas bubble forensics team surveils the New Zealand ocean, Eos, 100, https://doi.org/10.1029/2019EO133649. Published on 26 September 2019.

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