16/18: LME FACTSHEET SERIES
CANADIAN EASTERN ARCTIC - WEST GREENLAND LME
tic LMEs Arc CANADIAN EASTERN ARCTIC - WEST GREENLAND LME MAP 18 of Canada Central Map Arctic Ocean Hudson Bay LME
Greenland
Iceland
Iceland
16 1 ARCTIC LMEs
Large Marine Ecosystems (LMEs) are defined as regions of work of the Arc c Council in developing and promo ng the ocean space of 200,000 km² or greater, that encompass Ecosystem Approach to management of the Arc c marine coastal areas from river basins and estuaries to the outer environment. margins of a con nental shelf or the seaward extent of a predominant coastal current. LMEs are defined by ecological Joint EA Expert group criteria, including bathymetry, hydrography, produc vity, and PAME established an Ecosystem Approach to Management tropically linked popula ons. PAME developed a map expert group in 2011 with the par cipa on of other Arc c delinea ng 17 Arc c Large Marine Ecosystems (Arc c LME's) Council working groups (AMAP, CAFF and SDWG). This joint in the marine waters of the Arc c and adjacent seas in 2006. Ecosystem Approach Expert Group (EA-EG) has developed a In a consulta ve process including agencies of Arc c Council framework for EA implementa on where the first step is member states and other Arc c Council working groups, the iden fica on of the ecosystem to be managed. Iden fying Arc c LME map was revised in 2012 to include 18 Arc c the Arc c LMEs represents this first step. LMEs. This is the current map of Arc c LMEs used in the
This factsheet is one of 18 in a series of the Arc c LMEs.
OVERVIEW: CANADIAN EASTERN ARCTIC - WEST GREENLAND LME
The Canadian Eastern Arc c – West Greenland LME includes Baffin Bay - a large, elongated basin with a maximum depth of >2300 m, Davis Strait, the south-western shelf of Greenland, and the northern part of the Labrador shelf. Baffin Bay’s very large north-south extent, con guity 1.1: North Water Polynya to the North Atlan c Ocean, mul ple 1.3: Eastern Jones Sound linkages to the Arc c Ocean, and 1.4: Northern Baffin Bay direct contact with Greenland’s vast 2.1: Baffin Island coastline terrestrial ice masses make this LME 2.2: Baffin Bay shelf break a par cularly dynamic and sensi ve 3.1: Ha on Basin-Labrador Arc c regime. Sea-Davis Strait 3.2: Cumberland Sound Its deep and coastal shelf waters 4.1: Southern Baffin Bay are, with the excep on of the North Water Polynya and, in most years, its south-eastern areas off southern Greenland, fully ice-covered between January and April. The region’s numerous icebergs, calved chiefly at the glaciers of West Greenland, are an equally dominant feature of the Map: The Canadian Eastern Arc c – West Greenland LME. Source: AMSAIIC Report marine environment whose movements are determined largely by a combina on of sea ice condi ons and the The hydrography is characterized by circula on of region’s strong cyclonic (an -clockwise) system of Atlan c water through Baffin Bay and Lancaster currents in the upper water column. Sound, and flow of Pacific water from the Arc c Ocean through passages in the Canadian archipelago It is also one of the largest Arc c LMEs, 1,4 million and Nares Strait. The Pacific water is nutrient-rich km2. and is one factor why the primary produc on is rela vely high in this LME.