14/18: LME FACTSHEET SERIES BEAUFORT SEA LME
tic LMEs Arc BEAUFORT SEA LME MAP 18 of Map
Canada LME
Amundsen Gulf
Victoria Island
Iceland Inuvik Region Central Arctic Ocean Baffin Island
14 1 ARCTIC LMEs
Large Marine Ecosystems (LMEs) are regions of ocean space PAME developed a working map delinea ng 17 Arc c Large of 200,000 km² or greater, that encompass coastal areas Marine Ecosystems (Arc c LME's) in the marine waters of the from river basins and estuaries to the outer margins of a Arc c and adjacent seas in 2006. In a consulta ve process con nental shelf or the seaward extent of a predominant including agencies of Arc c Council member states and other coastal current. LMEs are defined by ecological criteria, Arc c Council working groups, the Arc c LME map was including bathymetry, hydrography, produc vity, and revised during 2012. The revised boundaries of the 18 tropically linked popula ons. The LME concept for current LMEs were mapped by the Ecosystem Approach ecosystem-based management has 5-module approach Expert Group (EA-EG) in a report of the consulta ve process. focused on produc vity, fish and fisheries, pollu on and This is the working map of Arc c LMEs and used for ecosystem health, socioeconomics, and governance. descrip ve purposes in the work of the Arc c Council.
This factsheet is one of 18 in a series of the Arc c LMEs.
OVERVIEW: BEAUFORT SEA LME The Beaufort Sea LME consists of two main parts: the shallow shelves around the margins in the south and east adjacent to a deep basin with depths greater than 3 km. The shelves are separated from the deep Beaufort Sea basin by steep slopes which cons tute a third main Victoria Island topographic feature. The deepest parts are around Cape Bathurst 3.500m deep. Prominent Polynya Amundsen features are the Mackenzie Gulf delta river and estuary and the Cape Bathurst Polynya in the Amundsen Gulf. Map: The Beaufort Sea LME. Source: AMSAIIC Report Mackenzie River Mouth The Mackenzie River is the most sediment-rich river in the Arc c and transports annually about 130 million tons of sediments into the Beaufort Sea.
The Mackenzie and Amundsen Gulf region provides important breeding, feeding and migra on habitats for birds, as Ice begins to form in early to mid-October, ini ally in do areas in the Corona on and Queen Maud gulfs the nearshore zones and extends outward to expand south of Victoria Island. Three subpopula ons of and eventually establish the landfast ice zone, usually polar bears inhabit this LME: the southern and by November, generally extending out to 20m depth northern Beaufort and M’Clintock subpopula ons. growing to a 2m thick level. A mobile ice pack occupies the bulk of the Beaufort Sea region in The primary produc on is rela vely high due to winter. influence of nutrient-rich Pacific water, and zooplankton residing in the deeper offshore areas. As elsewhere in the Arc c, lack of light and nutrients There is probably a large migratory popula on of are the two main factors limi ng phytoplankton polar cod in the eastern Beaufort Sea, which is a growth in the Beaufort Sea. Phytoplankton are, along major summer feeding area for large numbers of with zooplankton, the base of marine food webs in bowheads and belugas from migratory popula ons the Beaufort LME, as most other marine ecosystems. wintering in the Bering Sea. 2
MARINE MAMMALS
Five species of marine mammals occur regularly in During summer, ringed seals are dispersed the Beaufort Sea: the bowhead whale, beluga whale, throughout open-water areas. Seasonal ringed seal, bearded seal, and polar bear. concentra ons of seals (related to food sources) are known in offshore waters of the Amundsen Gulf Bowhead and beluga whales region off the Tuktoyaktuk Peninsula and off Cape The recurrent polynya and ice-edge habitat make the Dalhousie in summer. In the Canadian Beaufort Sea, Cape Bathurst Polynya an important beluga, the bearded seal is most abundant over depths 25– bowhead whale, polar bear, and ringed seal feeding 50 m. During the summer open-water period, much ground. Beluga (around 40.000 individuals) and of the Canadian Beaufort is unsuitable for feeding bowhead whales (about 10.000 individuals) of the because the pack-ice habitat preferred by bearded large migratory Beaufort Sea and Bering-Chukchi- seals typically retreats north to waters deeper than Beaufort Sea popula ons, respec vely, use the those used by bearded seals. In most areas, numbers polynya area in the eastern Beaufort Sea as their are low, but bearded seals are rela vely common in main feeding ground in the early part of summer certain nearshore areas along southern Banks Island, (May–June). Cape Parry, and Herschel Island. The abundance of bearded seals is rela vely low (1200-3100 in the The Bering-Chukchi-Beaufort Sea stock of bowhead eastern Beaufort Sea). whales winters in the Bering Sea, and most of the stock summers in the Canadian Beaufort Sea and Polar bear Amundsen Gulf. The spring migra on across the Two subpopula ons of polar bears occur in the BS western Beaufort Sea occurs through offshore ice LME: the Northern Beaufort Sea (1000 individuals) leads, generally from mid April to mid June, and Southern Beaufort Sea (1500) subpopula ons. depending on ice condi ons. Most remain in During winter and spring, most polar bears are found offshore waters (>200 m deep) among the offshore on the sea ice, tending to concentrate along pressure pack ice in the central and eastern Beaufort Sea un l ice that parallels the coasts, and in the vicinity of floe late July to mid August, when they begin to move edges. gradually toward coastal and nearshore areas. In summer, when the pack ice retreats offshore, polar Generally, adults move into Amundsen Gulf into bears are found along the edge of the pack ice. water depths 50–200 m off Bathurst Peninsula, small During years with li le or no pack ice near the coast, (<10 m) sub adults move into coastal and nearshore polar bears are o en found along the coastline and waters at water depths 10–50 m along the Yukon on barrier islands. In late March and early April, coast, and large sub adults move into nearshore and females that have denned on land return with their shelf waters at water depths 20–200 m off the Yukon cubs to the sea ice to hunt seals. In early summer, coast, Mackenzie Delta, and Tuktoyaktuk Peninsula. they are rela vely concentrated in areas with irregular coastlines such as bays, par cularly those Ringed and bearded seals within which ice remains longer than in other areas. During the spring breeding and mol ng seasons, ringed seals are dispersed at low densi es in the ice Polar bears of the Southern Beaufort popula on throughout the southeastern Beaufort Sea. Prime move north with the retrea ng pack ice in summer breeding habitat are in areas with a high propor on and move south in the autumn as ice develops to of ice cover and moderate water depths of 50–75 m. areas where they can hunt ringed and also bearded Ringed seal pups are born in April, mostly on landfast seals. Bears of the northern popula on move north ice. with the retrea ng ice off western Banks Island and M’Clure Strait in summer and south and east into Amundsen Gulf when ice develops in fall.