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The Davis Strait - DCE - Nationalt Center for Miljø og Energi

The Davis Strait - DCE - Nationalt Center for Miljø og Energi

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type or timing of vocalisations. In addition, there may be indirect effects associated<br />

with altered prey availability (Gordon et al. 2003).<br />

<strong>The</strong>re is strong evidence <strong>for</strong> behavioural effects on marine mammals from<br />

seismic surveys (Compton et al. 2008). Mortality has not been documented,<br />

but there is a potential <strong>for</strong> physical damage, primarily auditory damage.<br />

Under experimental conditions temporary elevations in hearing threshold<br />

(TTS) have been observed (Richardson et al. 1995, Anon 2005). In the USA a<br />

sound pressure level of 180 dB re 1µPA) (rms) or higher is believed to provoke<br />

TTS or PTS and is adopted by the US National Marine Fisheries Service<br />

as a mitigation standard to protect whales (NMFS 2003, Miller et al. 2005).<br />

Displacement is a behavioural response, and there are many documented<br />

cases of displacement from feeding grounds or migratory routes of marine<br />

mammals exposed to seismic sounds. <strong>The</strong> extent of displacement varies between<br />

species and also between individuals within the same species. For example,<br />

a study in Australia showed that migrating humpback whales generally<br />

avoided seismic sound sources at distances of 4-8 km but occasionally<br />

came closer. In the Beau<strong>for</strong>t Sea autumn-migrating bowhead whales avoid<br />

areas where the noise from exploratory drilling and seismic surveys exceeds<br />

117–135 dB and they may avoid the seismic source by distances of up to 35<br />

km (Reeves et al. 1984, Richardson et al. 1986, Ljungblad et al. 1988, Brewer<br />

et al. 1993, Hall et al. 1994, NMFS 2002, Gordon et al. 2003); although a Canadian<br />

study showed somewhat shorter distances (Lee et al. 2005). White<br />

whales avoided seismic operations in Arctic Canada by 10-20 km (Lee et al.<br />

2005). Stone & Tasker (2006) showed a significant reduction in marine<br />

mammal sightings during seismic surveys in the UK during periods of<br />

shooting compared with non-shooting periods. In the Mediterranean, bearings<br />

of singing fin whales estimated with passive acoustic monitoring indicated<br />

that whales moved away from the airgun source and out of the area<br />

<strong>for</strong> a time period that extended well beyond the duration of the airgun activity<br />

(Castellote et al. 2010). In contrast, minke whales have been observed as<br />

close as 100 m to operating airgun arrays (AU unpublished), which is potentially<br />

close enough to sustain physical damage.<br />

<strong>The</strong> ecol<strong>og</strong>ical significance of displacement effects is generally unknown. If<br />

alternative areas are available the impact probably will be low and the temporary<br />

character of seismic surveys will allow displaced animals to return<br />

after the surveys.<br />

In West Greenland waters satellite-tracked humpback whales utilised extensive<br />

areas and moved between widely spaced feeding grounds, presumably<br />

searching <strong>for</strong> their preferred prey (krill, sandeel and capelin) as prey availability<br />

shifted through the season (Heide-Jørgensen & Laidre 2007). <strong>The</strong> ability<br />

of humpback whales to find prey in different locations may suggest that<br />

they would have access to alternative <strong>for</strong>aging areas if they were displaced<br />

from one area by a seismic activity. However, even though many areas can<br />

be used, a few key zones seem to be especially important. <strong>The</strong> satellitetracked<br />

humpback whales favoured a zone on the shelf within the assessment<br />

area with high concentrations of sandeel (Heide-Jørgensen & Laidre<br />

2007). Similarly, a modelling study based on cetacean and prey surveys<br />

showed that rorquals (fin, sei, blue, minke and humpback whale) and krill<br />

aggregate in three high density areas on the West Greenland banks (Laidre<br />

et al. 2010). One of these important feeding areas covers the northern part of<br />

the assessment area. Displacement from major feeding areas can there<strong>for</strong>e<br />

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