The Davis Strait - DCE - Nationalt Center for Miljø og Energi
The Davis Strait - DCE - Nationalt Center for Miljø og Energi
The Davis Strait - DCE - Nationalt Center for Miljø og Energi
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have a negative impact on the energy uptake of the rorquals that are in West<br />
Greenland to feed be<strong>for</strong>e their southward migration. Given the extent of oil<br />
exploration in Greenland, there is a risk of cumulative effects if multiple<br />
surveys occur at the same time in adjacent areas. In this case marine mammals<br />
could be excluded from key habitats and unable to use alternative <strong>for</strong>aging<br />
grounds.<br />
<strong>The</strong> US National Marine Fisheries Service defines the radii about a seismic<br />
ship with received sound levels of 160 dB (re 1µPA) as the distance within<br />
which some cetaceans are likely to be subject to behavioural disturbance<br />
(NMFS 2005). Actual distances would depend on the source levels of the airgun<br />
array, the salinity and temperature layers of the water, and the depth of<br />
the observation. A few studies have observed lack of measurable behavioural<br />
changes by cetaceans exposed to the sound of seismic surveys taking place<br />
several kilometres away. For instance, Madsen et al. (2002) found no reaction<br />
of sperm whales to a distant seismic survey operating at tens of kilometres<br />
away. More recently, Dunn & Hernandez (2009) did not detect changes in<br />
the behaviour of blue whales that were at 15-90 km from operating airguns.<br />
<strong>The</strong> authors estimated that the whales experienced sounds of less than 145<br />
dB (re 1µPA) and concluded that, while their study supports the current US-<br />
NMFS guidelines, further studies with more detailed observations are warranted<br />
(Dunn & Hernandez 2009).<br />
An acoustic effect widely discussed in relation to whales and seismic surveys<br />
is the masking of communication and echolocation sounds. <strong>The</strong>re are,<br />
however, very few studies which document such effects (but see Castellote<br />
et al. 2010, Di Iorio & Clark 2010), mainly because the experimental setup is<br />
extremely challenging. Masking requires overlap in frequencies, overlap in<br />
time and sufficiently high sound pressures. <strong>The</strong> whales and seals in the assessment<br />
area use a wide range of frequencies (from < 10 Hz to > 100 kHz,<br />
Fig. 4.8.6), so the low frequency sounds of seismic surveys are likely to overlap<br />
in frequency with at least some of the sounds produced by these marine<br />
mammals.<br />
Masking is likely to occur as a result of the continuous noise from drilling<br />
and ship propellers, as documented <strong>for</strong> beluga whales and killer whales in<br />
Canada (Foote et al. 2004, Scheifele et al. 2005). Due to the low frequency of<br />
their phonation, baleen whales followed by seals would be the marine<br />
mammals most affected by auditory masking from seismic surveys (Gordon<br />
et al. 2003). It has furthermore been shown that blue whales increase their<br />
calling rate during seismic surveys, probably as a compensatory behaviour<br />
to the elevated ambient noise (Di Iorio & Clark 2010). Similarly, changes in<br />
the acoustic parameters of fin whale calls in the presence of airgun events<br />
indicate that fin whales also modify their acoustic behaviour to compensate<br />
<strong>for</strong> increased ambient noise (Castellote et al. 2010).<br />
Sperm whales showed diminished <strong>for</strong>aging ef<strong>for</strong>t during airgun emission,<br />
but it is not clear if this was due to masking of echolocation sounds or to behavioural<br />
responses of the whales or the prey (Miller et al. 2005).<br />
<strong>The</strong> most noise-vulnerable whale species in the assessment area belong to<br />
the baleen whales – minke, fin, blue and humpback whale – and the toothed<br />
whales – sperm whale and bottlenose whale (probably) – all of which all are<br />
present in the area during the ice free months when seismic surveys usually<br />
take place. At the time of writing this assessment we were not aware of any