scholarly journals Seals of the Pack Ice

Oryx ◽  
1955 ◽  
Vol 3 (2) ◽  
pp. 75-88
Author(s):  
Harry R. Lillie

Around the seas of the far northern Atlantic coming under the influence of Arctic conditions lives, frequently on the wander, one of the most delightful of creatures, the harp seal or saddleback, Phoca groenlandica. Large communities migrate in the Newfoundland, Labrador, Baffin Land, Greenland sector; others through the area of Jan Mayen Island towards Spitzbergen. Gregarious for much of the time, they share their world of ice with the occasional bearded seal and ringed seal, walrus, and polar bear. The White Sea in northern European Russia is a great harp seal nursery, for an eastern community in the area of the Barents Sea.

2006 ◽  
Vol 63 (1) ◽  
pp. 95-104 ◽  
Author(s):  
Tore Haug ◽  
Garry B. Stenson ◽  
Peter J. Corkeron ◽  
Kjell T. Nilssen

Abstract From 14 March to 6 April 2002 aerial surveys were carried out in the Greenland Sea pack ice (referred to as the “West Ice”), to assess the pup production of the Greenland Sea population of harp seals, Pagophilus groenlandicus. One fixed-wing twin-engined aircraft was used for reconnaissance flights and photographic strip transect surveys of the whelping patches once they had been located and identified. A helicopter assisted in the reconnaissance flights, and was used subsequently to fly visual strip transect surveys over the whelping patches. The helicopter was also used to collect data for estimating the distribution of births over time. Three harp seal breeding patches (A, B, and C) were located and surveyed either visually or photographically. Results from the staging flights suggest that the majority of harp seal females in the Greenland Sea whelped between 16 and 21 March. The calculated temporal distribution of births were used to correct the estimates obtained for Patch B. No correction was considered necessary for Patch A. No staging was performed in Patch C; the estimate obtained for this patch may, therefore, be slightly negatively biased. The total estimate of pup production, including the visual survey of Patch A, both visual and photographic surveys of Patch B, and photographic survey of Patch C, was 98 500 (s.e. = 16 800), giving a coefficient of variation of 17.9% for the survey. Adding the obtained Greenland Sea pup production estimate to recent estimates obtained using similar methods in the Northwest Atlantic (in 1999) and in the Barents Sea/White Sea (in 2002), it appears that the entire North Atlantic harp seal pup production, as determined at the turn of the century, is at least 1.4 million animals per year.


2004 ◽  
Vol 23 (1) ◽  
pp. 43-50 ◽  
Author(s):  
Stig Falk-Petersen ◽  
Tore Haug ◽  
Kjell T. Nilssen ◽  
Anette Wold ◽  
Trine M. Dahl

ARCTIC ◽  
2019 ◽  
Vol 72 (2) ◽  
pp. 197-202 ◽  
Author(s):  
Thomas G. Smith ◽  
Ian Stirling

Harp seals (Pagophilus groenlandicus) that breed in February and March in the White Sea migrate to open water around Svalbard and Franz Josef Land in the Barents Sea, feeding pelagically while following the receding ice edge northward to the edge of the polar pack. Although harp seals are present throughout the area during the summer, they are primarily pelagic and do not appear to be extensively preyed upon by polar bears (Ursus maritimus). However, occasionally, large numbers of harp seals may haul out and rest on the pack ice or feed in the water below the ice and surface to breathe between the floes. When approached by a polar bear while on the ice, harp seals do not exhibit the instant flight response characteristic of the polar bear’s primary prey species, ringed (Pusa hispida) and bearded seals (Erignathus barbatus). In this situation, polar bears may make multiple kills without either consuming their own prey or scavenging seals killed by other bears. This behavior appears not to frighten other nearby harp seals, whether hauled out on the ice or in the water below the floes. These unusual concentrations of harp seals hauled out on sea ice may be related to the distribution and abundance of fish or other epontic prey. Their lack of an escape response to predators on the surface of the sea ice is probably a result of briefly hauling out in large numbers in spring while whelping on the sea ice in areas where the consequences of potential polar bear predation are insignificant. The rare events of harp seal mortality from bears killing them on the surface of pack ice during the summer do not appear to have a significant impact at the population level of either species.


2004 ◽  
Vol 23 (1) ◽  
pp. 43-50 ◽  
Author(s):  
Stig Falk-Petersen ◽  
Tore Haug ◽  
Kjell T. Nilssen ◽  
Anette Wold ◽  
Trine M. Dahl

2019 ◽  
Vol 12 (9-10) ◽  
pp. 38-48
Author(s):  
V. I. Batuev ◽  
I. L. Kalyuzhny

The development of the European North of Russia, where flat and high-hummocky bog complexes are spread, requires information on the processes of formation of their hydrological regime and freezing of this territory. For the first time, based on observational data, for the period from 1993 to 2013, characteristics of the hydrological regime and freezing of hummocky bogs in Northern European Russia are presented, the case study of the Lovozerskoye bog. The observations were carried out in accordance with the unified methods, approved for the specialized network of Roshydromet bog stations. The regularities of the formation of the hydrological regime of hummocky bogs have been revealed: bog water level drops dramatically from the beginning of freezing to the end of March, rises during snow melt period, slightly drops in summer and rises in autumn. The main feature of hummocky bogs is permafrost, which determines their specific structure. It has been discovered that gravitation snowmelt and liquid precipitation waters relatively quickly run down the hummocks over the frozen layer into hollows between them. Levels of bog waters on the hummocks are absent for a longer period of time. In spring, the amplitude of water level rise in swamplands is on average 60–80 cm. Air temperature and insulation properties of snow are the main factors that influence the bog freezing. Hummocks freeze out as deep as 63–65 cm, which corresponds to the depth of their seasonal thawing in the warm period of the year, and adjoin the permafrost. The greatest depth of freezing of the swamplands is 82 – 87 cm, with an average of 68 cm. The frozen layer at swamplands thaws out from both its upper and bottom sides. The melting of the frozen layer at hummocks occurs only from the bog surface with an average intensity of 0,51 cm/day.


Author(s):  
Svtelana B. Selyanina ◽  
◽  
Marina V. Trufanova ◽  
Svtelana A. Zabelina ◽  
Mikhail V. Bogdanov ◽  
...  

1999 ◽  
Vol 48 (1) ◽  
pp. 59-72 ◽  
Author(s):  
J Wolkers ◽  
I.C Burkow ◽  
M Monshouwer ◽  
C Lydersen ◽  
S Dahle ◽  
...  

2007 ◽  
Vol 415 (1) ◽  
pp. 711-713 ◽  
Author(s):  
E. N. Borisenko ◽  
V. I. Velichkin ◽  
T. A. Vorob’eva ◽  
A. V. Evseev ◽  
A. Yu. Miroshnikov

1995 ◽  
Vol 14 (3) ◽  
pp. 335-338
Author(s):  
Erling Sverre Nordøy
Keyword(s):  

Boreas ◽  
1999 ◽  
Vol 28 (1) ◽  
pp. 23-45 ◽  
Author(s):  
VALERY I. ASTAKHOV ◽  
JOHN INGE SVENDSEN ◽  
ALEXEI MATIOUCHKOV ◽  
JAN MANGERUD ◽  
OLGA MASLENIKOVA ◽  
...  

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