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
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.