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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70°N<br />
60°N<br />
50°N<br />
75°W<br />
120<br />
120°W<br />
105°W<br />
90°W 75°W 60°W 45°W 30°W<br />
60°W<br />
15°W<br />
0°<br />
Deployment sites<br />
Baffin Bay sub-pop.<br />
45°W<br />
70°N<br />
60°N<br />
Lancaster Sound sub-pop.<br />
Kane Basin sub-pop.<br />
<strong>Davis</strong> <strong>Strait</strong> sub-pop.<br />
Assessment area<br />
0 250 500 Km<br />
50°N<br />
70°N<br />
60°N<br />
50°N<br />
75°W<br />
120°W<br />
90°W 75°W 60°W 45°W 30°W<br />
A genetic study of polar bears (Paetkau et al. 1999) indicated significant differences<br />
between bears from the <strong>Davis</strong> <strong>Strait</strong> and neighbouring Baffin Bay.<br />
<strong>The</strong> <strong>Davis</strong> <strong>Strait</strong> subpopulation of polar bears range in the ‘seasonal-ice’<br />
ecoregion (Amstrup et al. 2007, 2008), with the ice-free period extending<br />
from approximately August through November. Annual ice cover in <strong>Davis</strong><br />
<strong>Strait</strong> is highly variable and ice breakup has become earlier since 1991<br />
(Stirling & Parkinson 2006).<br />
Satellite telemetry conducted in the period 1991-2001 showed that polar<br />
bears from the DS subpopulation range the offshore pack ice in the <strong>Davis</strong><br />
<strong>Strait</strong> (Mosbech et al. 2007). <strong>The</strong> movement of the bears instrumented with<br />
satellite-radios indicated an overall tendency to occur on the fast ice and in<br />
the shear zone between fast ice and pack ice along eastern Baffin Island.<br />
However, in December-June there is an overlap between the distribution of<br />
some polar bears from the <strong>Davis</strong> <strong>Strait</strong> subpopulation and the assessment<br />
area.<br />
<strong>The</strong> extent of the pack ice in the <strong>Davis</strong> <strong>Strait</strong> varies from year to year (see<br />
chapter 3). So does the position of the <strong>Davis</strong> <strong>Strait</strong> whelping patch of hooded<br />
seals, Cystophora cristata (Bowen et al. 1987). During the period 1974-1984,<br />
the location of this whelping patch where polar bears occur (F.O. Kapel, per-<br />
105°W<br />
60°W<br />
15°W<br />
0°<br />
Movement, all year<br />
<strong>Davis</strong> <strong>Strait</strong> sub-pop.<br />
Baffin Bay sub-pop.<br />
45°W<br />
70°N<br />
60°N<br />
Lancaster Sound sub-pop.<br />
Kane Basin sub-pop.<br />
Assessment area<br />
0 250 500 Km<br />
Figure 4.8.1. Left: Locations where adult female polar bears were instrumented with satellite transmitters (1991-1995) given by<br />
sub-population (<strong>Davis</strong> <strong>Strait</strong>, Baffin Bay, Lancaster Sound and Kane Basin). A total of 29 bears were instrumented in the <strong>Davis</strong><br />
<strong>Strait</strong> subpopulation (blue) and their movements tracked during 1991-2001. <strong>The</strong> identification and delineation of the various subpopulations<br />
based on hierarchal cluster analyses is described in Taylor et al. (2001). Unpublished data: Nunavut Wildlife Management<br />
Division, University of Saskatchewan, Canadian Wildlife Service, Greenland Institute of Natural Resources.<br />
Right: Track lines showing the overall movement during 1991-2001 of polar bears instrumented with satellite transmitters in the<br />
<strong>Davis</strong> <strong>Strait</strong>-Baffin region and adjacent areas. A certain degree of overlap between the different sub-populations is apparent.<br />
Unpublished data: Nunavut Wildlife Management Division, University of Saskatchewan, Canadian Wildlife Service, Greenland<br />
Institute of Natural Resources.<br />
50°N