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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Kittiwakes are abundant in the shelf waters of the assessment area (Fig.<br />
4.7.11) and many of these are non-breeding birds from populations breeding<br />
elsewhere in the North Atlantic (Lyngs 2003). Kittiwakes spend the winter in<br />
offshore parts of the North Atlantic, and at least some occur in the <strong>Davis</strong><br />
<strong>Strait</strong>, but very few were observed during the winter surveys in 1999<br />
(Merkel et al. 2002).<br />
Kittiwakes are most vulnerable to oil spills at breeding colonies where large<br />
numbers of birds often assemble on the sea surface. <strong>The</strong>re may also be concentrations<br />
at feeding areas, e.g. in the marginal ice in spring and early<br />
summer or at upwelling sites, but these are not predictable in time and<br />
space.<br />
Due to a substantial decrease in the breeding population (Labansen et al.<br />
2010), the kittiwake is listed as Vulnerable (VU) on the Greenland Red List<br />
(Boertmann 2007).<br />
Ivory gull, Pagophila eburnea<br />
Ivory gulls breeding in the northeast sector of the Arctic Atlantic (Northeast<br />
Greenland, Svalbard and the Russian Arctic) move south in autumn in the<br />
drift ice off East Greenland to winter quarters mainly in the marginal ice<br />
zone in the Labrador Sea and the <strong>Davis</strong> <strong>Strait</strong>, where they arrive in December<br />
(Orr & Parsons 1982, Gilg et al. 2010). This probably means that a large<br />
proportion of the northeast Atlantic population of the ivory gull moves<br />
through the assessment area in early December (Gilg et al. 2009, Gilg et al.<br />
2010). In years when the drift ice in winter moves into the assessment area<br />
from the west, ivory gulls will be present, but the fraction of the population<br />
is unknown. In spring, most of the gulls probably move the same way back<br />
through the assessment area; although it has been shown that they can migrate<br />
northwards in the <strong>Davis</strong> <strong>Strait</strong> and across the Greenland Ice Sheet to<br />
North East Greenland (O. Gilg pers. comm.). Observations from 2011 show<br />
that adult ivory gulls are present in Julianehåb Bugt as early as late-October<br />
(D. Boertmann, unpubl. data), a fact not revealed by the satellite-tracked<br />
birds. Ivory gulls can probably there<strong>for</strong>e also be present in the assessment<br />
area around this time or slightly later.<br />
<strong>The</strong> ivory gull is of high conservation concern (Gilg et al. 2009, Gilg et al.<br />
2010), being listed as near threatened (NT) on the international Red List<br />
(IUCN 2011), as vulnerable (VU) on both the Greenland and the Svalbard<br />
red lists (Boertmann 2007, Kålås et al. 2010), and as endangered by the<br />
Committee on the Status of Endangered Wildlife in Canada (COSEWIC).<br />
Iceland gull, Larus glaucoides<br />
This gull is the most abundant of the large gulls in the assessment area. Numerous<br />
breeding colonies are found there, on steep cliffs and small islands<br />
(Fig. 4.7.2).<br />
<strong>The</strong> assessment area is also an important winter habitat <strong>for</strong> this gull, and<br />
both local breeding birds and birds from northern areas assemble here<br />
(Lyngs 2003, Boertmann et al. 2006).<br />
Iceland gulls are most sensitive to oil spills at the breeding colonies. <strong>The</strong>se<br />
colonies, however, are generally small and the population is spread widely<br />
along the coasts and population sensitivity is there<strong>for</strong>e relatively low compared<br />
to other much more concentrated seabirds.