Sound scattering by hydrodynamic wakes of sea animals

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ICES Journal of Marine Science, 53: 377 381. 1996 Sound scattering by hydrodynamic wakes of sea animals Dmitry A. Selivanovsky and Alexander B. Ezersky Selivanovsky, D. A. and Ezersky, A. B. 1996. Sound scattering by hydrodynamic wakes of sea animals. ICES Journal of Marine Science, 53: 377 381.

1996 International Council for the Exploration of the Sea Key words: gas bubbles, phytoplankton, sonar, spectral characteristics of reverberation, turbulence, wake. D. A. Selivanovsky and A. B.

1 ICES Journal of Marine Science, 53: Sound scattering by hydrodynamic wakes of sea animals Dmitry A. Selivanovsky and Alexander B. Ezersky Selivanovsky, D. A. and Ezersky, A. B Sound scattering by hydrodynamic wakes of sea animals. ICES Journal of Marine Science, 53: It was observed that the hydrodynamic wake of sea animals such as squid or dolphin can have a considerably greater target strength than that of the animal itself International Council for the Exploration of the Sea Key words: gas bubbles, phytoplankton, sonar, spectral characteristics of reverberation, turbulence, wake. D. A. Selivanovsky and A. B. Ezersky: Institute of Applied Physics, RAS, 46 Ulyanov St, Nizhny Novgorod, 636 Russia. Correspondence to Selivanovsky [tel: , fax: ]. Introduction and methods Sonar observations were carried out using a fishhunting sonar at frequencies of 2 khz and 14 khz. The sonar emitted simultaneous tone-burst signals at frequencies of 1 and 4 ms duration. The widths of the coaxial beam patterns at the 3 db level were Figure 1. Flag-like echo traces associated with squid some distance from the ship. Axis of the beam at 15 below the horizontal. Night, Sea of Japan, October, drifting ship with an illumination system. Distance measured from the ship /96/ $18./ 1996 International Council for the Exploration of the Sea 16 Downloaded from on 21 December 217

378 D. A. Selivanovsky and A. B. Ezersky 5 1 15 2 25 3 5 1 15 2 25 3 Figure 2. Echo traces of the wakes of squid with axis of the beam at 23 below the horizontal.

2 378 D. A. Selivanovsky and A. B. Ezersky Figure 2. Echo traces of the wakes of squid with axis of the beam at 23 below the horizontal. Night, Sea of Japan, September, drifting ship with an illumination system. Results Observations on squid The first observations were of the wakes of the squid (Todarodes pacificus) swarming at the surface around a drifting ship. The echo trace of the wake of a squid resembled a flag or pennant strung out along a single axis or pole which represented the path of the squid (Nos 1, 2 in Figure 1, and 1, 2, 3 in Figure 2). The axis of the sonar beam was directed downwards at angles of ψ=15 (Fig. 1) and ψ=23 (Fig. 2) relative to the surface of the water. Thus, objects located at range x were situated at the depth H=x sinψ. The echo signals were recorded on magnetic tape and in the form of echograms: the elapsed time was plotted along the horizontal axis, and the distance from the ship was plotted along the vertical axis. The radial velocity was v 1 m s 1, and the target strength was TS 45 to 55 db, which is characteristic of squid with a mantle length of cm. The flag-like structure suggests that the echo signals are associated with reflections from the hydrodynamic wakes of the squid. This assumption is supported by the fact that the number of squid caught correlated well with the frequency of occurrence of the flags appearing on the echograms. The time dependence of the wake velocity relative to the water was determined from the Fourier spectra of the long tone-burst signals (τ=4 ms) using the Doppler technique. It was found that the mean velocity of the scattering zone fell considerably from v 2 ms 1 to v.1 m s 1, while the flags persisted (T<12 s). During this time, the target strength of the wake varied from TS 28 to 35 db. An important feature of the observed phenomenon, supporting our interpretation, was that the measured velocities of the squid and the scattering objects in the wakes were always in opposite directions. Observations on dolphins and fish The echoes associated with the sound reflections from the wakes of dolphins were recorded using a sonar with a horizontally orientated beam near the sea surface. The ship was drifting slowly during the measurements, and the sea was calm enough to avoid interfering signals scattered from the sea surface. The dashed lines in Figure 3 show the paths of two groups of dolphins, each of two to three individuals moving away from the ship at a speed of 4 6 m s 1 and easily followed visually when the animals appeared Downloaded from on 21 December 217

Sound scattering by hydrodynamic wakes of sea animals 379 2 3 4 5 at the surface. The target strength of the wake was found to be TS 12 to 18 db; the duration was T 1.5 min.

3 Sound scattering by hydrodynamic wakes of sea animals at the surface. The target strength of the wake was found to be TS 12 to 18 db; the duration was T 1.5 min. Echoes associated with the wakes of fish (presumably Thunnus thynnus) were observed under similar conditions, and are illustrated in Figure 4 (No. 1). Discussion Figure 3. Echo traces of the wakes of dolphins, recorded by day. The axis of the beam was horizontal. What is the structure of the hydrodynamic wakes responsible for such backscattering? We suggest that wakes consist of vortices which are uniform in temperature and density and that the vortices are generated by the undulations of the fins or tails of dolphins or by water expelled from the mantle of squid. Such wakes cannot be observed by echolocation, since the vortices scatter predominantly in the forward direction and the backscattered echo is negligible (Tatarskii, 1967). The temperature and density fluctuations of the liquid in the wake would have to be much greater than is generally observed in the ocean in order to match the 16 measured target strength. Furthermore, we do not know of any mechanisms which might cause such large fluctuations in the wakes of marine animals. A more likely hypothesis is that the scattering of ultrasound by the wake is attributable to gas bubbles, perhaps predominantly those near resonance. The duration of the echo signals in the form of flags in this case is determined by the time the gas bubbles take to rise from a depth of several metres. The ascent rate of bubbles of the size resonant at 2 khz near the water surface is about 7 cm s 1. Consequently, the wake for resonant bubbles should vanish after about 1 s, but turbulence could make the ascent time noticeably longer. The gas-bubble concentrations indicated by the measured target strength in the volume occupied by the wake were in the range 5 23 m 3, which is the same order as the concentration of gas bubbles in a ship s wake. The target strength was much lower in the case of the wakes of squid. We found that the average target strength corresponded to several bubbles resonant at 2 khz and giving echoes in phase. The observation of squid wakes in regions where the horizontal currents at depths of 4 m have a layered structure (see for example Fig. 2) showed that the wake-generating scatterers drifted upwards, since the flags bend when crossing the boundary between layers with different current velocities. This is additional evidence for the hypothesis that the wakes of squid contain gas bubbles. The formation of vortex rings in a medium when liquid is injected through an orifice for a short time is a well-known phenomenon. The vortex rings are formed over a wide range of orifice shape and injection times. When the Reynolds number is sufficiently large, and after enough time for the motion to become stable, the velocity of these vortex rings in water obeys the law V=V (4α tv /R ) 3/4. Here R and V are, respectively, the initial radius and velocity of the vortex, and α is a dimensionless coefficient determined by the conditions under which the vortex ring is formed (e.g. the Reynolds number). The relationship d(logv)/ d(logt)=.75 is generally applicable here (Lavrent ev and Shabat, 1977). This hypothesis of the gas bubble as the cause of scattering of sound in the wakes of marine animals is supported by the observed time dependence of the vortex rings velocity. We note that the gas bubbles, which are a passive impurity, move on the average together with the ring. The mean slope d(logv)/d(logt) for the duration of the squid measurements (2 8 s) is close to the expected.75 given by the above law. A large-scale vortex is clearly not formed in the wake at time t<2 s, while the velocity of the vortex becomes small (V=1 cm/s) at time t>8 s. The dominant forces controlling the bubbles are the buoyancy, not the centripetal forces that confine the bubbles in the vortex. Downloaded from on 21 December 217

38 D. A. Selivanovsky and A. B. Ezersky 1 2 3 4 5 6 1 2 3 4 5 Figure 4.

4 38 D. A. Selivanovsky and A. B. Ezersky Figure 4. Echogram of wakes of fish (Thunnus thynnus) by day. The axis of the beam was horizontal Figure 5. Echograms from wakes of squid some distance from a drifting ship. Evening, Sea of Japan. Beam horizontal. Downloaded from on 21 December 217

5 Sound scattering by hydrodynamic wakes of sea animals 381 The question arises as to how gas bubbles form in the hydrodynamic wake of squids and fishes, and what is the mechanism of their formation? Gas bubbles are known to form in a liquid through cavitation when the pressure drops. For cavitation to occur at a depth of 1 m in a liquid flow, we estimate the velocity at which the pressure reduces to zero would be about 2 m s 1. This velocity is possible, in principle, if the squid expels half of its own weight in water through a siphon of radius.3.6 cm. Alternatively, it is possible that the gas bubbles in the jets of water expelled by squid come from phytoplankton cells that contain gas cavities. Finally, we show another echogram (Fig. 5) where reverberation in the surface layers of the sea is mainly determined by the effects of the wakes of the squid. References Lavrent ev, M. A. and Shabat, B. V Problems of hydrodynamics and their mathematical models. Moscow, Nauka. 44 pp. (In Russian.) Tatarskii, V. I Wave propagation in a turbulent atmosphere. Moscow, Nauka. 657 pp. (In Russian.) Downloaded from on 21 December 217

Measured broadband reverberation characteristics in Deep Ocean. [E.Mail: ]

Measured broadband reverberation characteristics in Deep Ocean Baiju M Nair, M Padmanabham and M P Ajaikumar Naval Physical and Oceanographic Laboratory, Kochi-682 021, India [E.Mail: ] Received ; revised