Summer and fall movements of narwhals (Monodon monoceros) from northeastern Baffin Island towards northern Davis Strait

Citation
R. Dietz et al., Summer and fall movements of narwhals (Monodon monoceros) from northeastern Baffin Island towards northern Davis Strait, ARCTIC, 54(3), 2001, pp. 244-261
Citations number
42
Categorie Soggetti
Multidisciplinary
Journal title
ARCTIC
ISSN journal
00040843 → ACNP
Volume
54
Issue
3
Year of publication
2001
Pages
244 - 261
Database
ISI
SICI code
0004-0843(200109)54:3<244:SAFMON>2.0.ZU;2-M
Abstract
Ten narwhals (Monodon monoceros) were instrumented with satellite-linked ra dio transmitters in Tremblay Sound in August 1997 (N = 5) and August 1998 ( N = 5). All whales stayed in the waters around Bylot Island until the end o f September. On the basis of these animals and others tagged previously (to tal N = 24), it is believed that the Bylot Island summering population has limited or no contact with other summering populations in Canada or Greenla nd. Four whales were monitored during their southward movement along the ea st coast of Baffin Island. Three of them travelled close to the shore, visi ting several fjords and bays, during September and October. The fourth whal e started the southward migration at the same time as the other three, but it returned to the area east of Pond Inlet and made two trips northeast of Bylot Island. It headed south on 21 October 1998. South of Royal Society Fi ord, it travelled offshore along the continental slope (1000 to 1500 m), pr obably because of ice formation in inshore areas. This narwhal and another male tagged in 1997 moved east toward the northern parts of the Davis Strai t, reaching an area midway between Canada and Greenland in early November. Their winter movements were monitored until 30 January. The same wintering area in northern Davis Strait was previously documented for two male narwha ls tracked from Melville Bay, NW Greenland, in 1993 and 1994. The whales sh owed a preference for deep areas, including deep fjords and the continental slope, where depths ranged between 500 and 1500 m. Even deeper areas, wher e maximum daily dives exceeded 1000 m, were also visited occasionally.