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Frequency (Hz)
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Figure 4. Comparing sound sources, where the order shows the relative sound pressure levels (dB) of the noise sources and the colour code allows
comparison of the levels between categories (orange being highest dB level to dark blue being lowest). The areas with hatching indicate the frequency
range with most energy. MFAS = Medium Frequency Active Sonar. LFAS = Low Frequency Active Sonar. ADD = Acoustic Deterrent Device
impulsive sound emitters of high relevance are explosions, airgun
arrays and navy sonar. Pile-driving could be regionally important,
for example in Northern Europe. The main and most important
amitter of continuous sound is commercial shipping. These sources
of anthropogenic sound are described in more detail below. For easy
reading, we avoid in most cases any reference to specific units such
as decibel levels and frequency. For frequency, ‘low’ refers to 1 Hz —
500 Hz, ‘mid’ means >500 Hz — 10 kHz and ‘high’ refers to >10 kHz
200 kHz (and more, see Figure 4; see Tasker et al., 2010). Concerning
decibel levels, ‘high’ and ‘low’ are always referred to as relative terms,
ie. in comparison to other sources. Due to the different physical
properties of impulsive vs continuous sounds, these comparisons
have to be viewed with caution.
Anthropogenic impulsive sounds
Explosions are caused by the use of explosives e.g. for the removal of
structures from the seabed, in military operations or when clearing
unexploded ordnance such as those deposited in the North Sea after
World War Il. Across all the impulsive sound sources, explosions
produce the highest peak levels of noise. This is why there is serious
risk of direct injury to marine organisms, which depends on the
weight of the charge and the depth of the detonation (Hildebrand,
2005; OSPAR Commission, 2009b).
Seismic surveys are conducted to map geological structures beneath
the seabed, both for the oil and gas industries and research purposes,
using arrays of airguns towed from seismic vessels. An airgun is a
compressed-air-filled cylinder and when the air is suddenly released,
it causes a transient high-pressure peak that can create a sound with
very high sound pressure levels (>230 dB re 1 WPa m). The sound is
reflected by the seabed and is detected, providing information about
the sub-sea properties. The main energy content is at low frequencies
{see Figure 4), with some mid- and high frequency content, although
the extent of the high frequency component is still uncertain (OSPAR
Commission, 2009b; Genesis Oil and Gas Consultants, 2011). Sub-
bottom profilers are also used to survey the seabed and are highly
directional sound sources. Sound levels can be relatively high
and there is a wide variety of profilers operating across a range of
frequencies (from low to high). Given their prevalent use in some
areas, more measurements are needed to fully characterize these
sources and assess their potential impact.
Much research has been done since 2008 on pile-driving, where piles
are driven into the seabed to provide foundation support for offshore
structures. This activity is undertaken in the construction of offshore
platforms, including those for wind farms. Pile-driving emits short
pulses of intense sound with a relatively high SPL in the low frequency
range but extending to higher frequencies as well. Propagated
sound levels depend on a number of factors including the maximum
energy rating of the hammers and the fact that the sound is not only
transferred into the water column but also to some extent into the
substrate (Bellmann et al, 2020; Jimenez-Arranz et al, 2020}.