01.09.2013 Views

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!