Baffin Bay (Inuktitut: Saknirutiak Imanga; Greenlandic: Avannaata Imaa; French: Baie de Baffin),[a] located between Baffin Island and the west coast of Greenland, is a marginal sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea. The narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice and icebergs in the open areas. However, a polynya of about 80,000 km2 (31,000 sq mi), known as the North Water, opens in summer on the north near Smith Sound. Most of the aquatic life of the bay is concentrated near that region.
|Max. length||1,450 km (901 mi)|
|Max. width||110–650 km (68–404 mi)|
|Surface area||689,000 km2 (266,000 sq mi)|
|Average depth||861 m (2,825 ft)|
|Max. depth||2,136 m (7,008 ft)|
|Water volume||593,000 km3 (142,300 cu mi)|
On the East. The West Coast of Greenland.
On the South. The parallel of 70° North between Greenland and Baffin Land.
On the West. The Eastern limits of the North-West Passages [The East Coast of Ellesmere Island between C. Sheridan and Cape Norton Shaw ( ), thence across to Phillips Point (Coburg Island) through this Island to Marina Peninsula ( ) and across to Cape Fitz Roy (Devon Island) down the East Coast to Cape Sherard (Cape Osborn) ( ) and across to Cape Liverpool, Bylot Island ( ); down the East coast of this island to Cape Graham Moore, its southeastern point, and thence across to Cape Macculloch ( ) and down the East coast of Baffin Island to East Bluff, its Southeastern extremity, and thence the Eastern limit of Hudson Strait].— International Hydrographic Organization, Limits of Oceans and Seas, 3rd edition
The area of the bay has been inhabited since c. 500 BC. Around AD 1200, the initial Dorset settlers were replaced by the Thule (the later Inuit) peoples. Recent excavations also suggest that the Norse colonization of the Americas reached the shores of Baffin Bay sometime between the 10th and 14th centuries. The English explorer John Davis was the first recorded European to enter the bay, arriving in 1585. In 1612, a group of English merchants formed the "Company of Merchants of London, Discoverers of the North-West Passage". Their governor Thomas Smythe organized five expeditions to explore the northern coasts of Canada in search of a maritime passage to the Far East. Henry Hudson and Thomas Button's explored Hudson Bay, William Gibbons Labrador, and Robert Bylot Hudson Strait and the area which became known as Baffin's Bay after his pilot William Baffin. Aboard Discovery, Baffin charted the area and named Lancaster, Smith, and Jones Sounds after members of his company. By the completion of his 1616 voyage, Baffin held out no hope of an ice-free passage and the area remained unexplored for another two centuries. Over time, his account came to be doubted until it was confirmed by John Ross's 1818 voyage. More advanced scientific studies followed in 1928, in the 1930s and after World War II by Danish, American and Canadian expeditions.
Currently, there are a few Inuit settlements on the Canadian coast of the bay, including Arctic Bay (population 690), Pond Inlet (1,315) and Clyde River (820). Those settlements are accessed and supplied by air and annual sealifts. In 1975, a town was built at Nanisivik to support lead and zinc production at the Nanisivik Mine—the first Canadian mine in the Arctic. The mine was closed in 2002 due to declining resources and metal prices. Whereas the town still has a functional seaport and an airport, as of the 2006 census, it has an official population of zero.
Baffin Bay was the epicenter of a 7.3 magnitude earthquake in 1933. This is the largest known earthquake north of the Arctic Circle. It caused no damage because of its offshore location and the small number of the nearby onshore communities. The northwestern part of the bay remains one of the most seismically active regions in eastern Canada. Five earthquakes of magnitude 6 have occurred here since 1933. The latest strong earthquake occurred on 15 April 2010 and had the magnitude of 5.1.
Baffin Bay is an arm of the Atlantic Ocean bounded by the Baffin Island in the west, Greenland in the east, and Ellesmere Island in the north. It connects to the Atlantic through the Davis Strait, and to the Arctic through several narrow channels of Nares Strait. It is a northwestern extension of the North Atlantic and Labrador Sea. It can also be viewed as a long strait separating Baffin Island and Greenland.
The bay is less than 1,000 m (3,300 ft) deep near the coast, where the sea bottom is covered with gravel, crushed stone and sand. In the center, there is a deep pit called the Baffin Basin, reaching 2,136 m (7,008 ft) (see depth map), which is mostly covered in silt. Currents form a cyclonic circulation. On the eastern periphery, in summer, the West Greenland Current transports water from the Atlantic Ocean to the North. In its western part, the Baffin Island Current brings the Arctic waters to the south.
The climate is Arctic with frequent storms, especially in winter. Average January temperatures are −20 °C (−4 °F) in the south and −28 °C (−18 °F) on the north. In July, the average temperature is 7 °C (45 °F). The annual precipitation is 100–250 mm (3.9–9.8 in) on the Greenland side and about twice as much near Baffin Island.
The water temperature at the surface is below −1 °C (30 °F) in winter. In summer, it varies from 4–5 °C (39–41 °F) in the south-east to 0 °C (32 °F) and below at north-west. The salinity exceeds 34‰ (parts per thousand) in winter. In summer, it is 32‰ on the east and 30–31‰ on the west. Deep waters are formed as a result of mixing of Arctic and Atlantic waters; their temperature is about −0.5 °C (31.1 °F) and salinity is 34.5 ‰. In winter, 80% of the bay is covered with continuous ice, floating ice and fast ice. In some winters, the continuous ice stretches from shore to shore. The ice is most abundant in March and least in August–September. In summer, drifting ice remains in the central and western parts of the bay. Numerous icebergs are formed in this period and are brought, together with ice, to the Atlantic Ocean near Newfoundland.
The tides are semidiurnal, with an average height of 4 m (13 ft) and the maximum of 9 m (30 ft). Their speed varies between 1 and 3.7 km/h (0.62 and 2.30 mph) hour and the direction by as much as 180°. This variability results in the collision and crushing of fresh, old, and pack ice. Winds are predominantly north-western through the whole year. South-eastern and eastern winds are common in July and August.
Between May and July (sometimes April), a significant portion of navigable open water (polynya) forms at the extreme north of the bay, presumably due to the relatively warm Greenland Current. With an area of about 80,000 km2 (31,000 sq mi) in summer, it is the largest polynya of the Canadian Arctic and covers the Smith Sound between the Ellesmere Island and Greenland. This polynya has a stable position and existed for at least 9,000 years. It was first described in 1616 by William Baffin and was named North Water by whalers of the 18–19th centuries.
The North Water provides air to ice algae and zooplankton and is characterized by abundant fauna. Of about 20,000 beluga whales living in the Baffin Bay, some 15,000 are concentrated at the North Water. Other abundant animals of the region include walrus, narwhal, harp seal, bearded seal, ringed seal, bowhead whale, rorquals and polar bear. All aquatic mammals crucially depend on the availability of open water; they have very limited ability to maintain breathing holes in ice and are all vulnerable to attacks by the polar bear when breathing at the holes. The seals and walrus occupy areas of fast ice, which is essential for giving birth and raising the pups. Bearded seals feed near the bottom of the bay and therefore are restricted to the shallow waters. Ringed seal is the most common meal of the polar bear. It is also an occasional prey of the walrus and Arctic fox. Most large animals of the bay are being traditionally hunted, but the hunting has been restricted in the 20th century in order to preserve the wildlife population. For example, the quota for polar bears in the bay area is 105 per year.
There are about 400 plant and tree species on the bay shores, including birch, willow, alder and plants adapted to salty soils, as well as lyme grass, mosses, and lichens. These serve as food for caribou and rodents, such as lemming. Resident fish species include polar cod, Arctic flounder (Pleuronectidae, Liopsetta), four-horned sculpin and capelin, whereas cod, haddock, herring, halibut, and rattail migrate from the Atlantic. The birds are represented by the little auk, snowy owl, willow ptarmigan, rock ptarmigan, gyrfalcon, Arctic redpoll and guillemots. Most of them migrate to the south during the winter.
The US Geological Survey has estimated that at least 13% of the world's undiscovered oil deposits and 30% of the world's undiscovered gas pockets are located in the Arctic, with the seas around Greenland potentially holding large amounts of natural gas and lesser amounts of crude oil and natural-gas liquids. Accordingly, the Greenland authorities have offered a large number of off-shore concessions for potential hydrocarbon (oil and gas) extraction. The largest concession-areas are located in seas west of Greenland; primarily in Baffin Bay and the Davis Strait, but with several smaller concessions in the Greenland Sea in the east also.
Adams Island (Inuit: Tuujjuk) is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. The island is located in Baffin Bay off the northeastern coast of Baffin Island in the Canadian Arctic Archipelago. Nearby are Dexterity Island (northeast), Dexterity Fiord and Baffin Island (east), Tromso Fiord (south), Paterson Inlet (west), Bergesen Island (northwest), and Isbjorn Strait (north).Adams Island is irregularly shaped, its eastern and western sides split by the Ratcliffe Arm. Coastlines slope sharply while the interior mountains are over 800 m (2,600 ft) in height. The island comprises an area of 267 km2 (103 sq mi), measuring 30.55 kilometres (18.98 mi) in length and 18 kilometres (11 mi) to 22 kilometres (14 mi) in width.Another, much smaller, Adams Island is located off the northeastern tip of Baffin Island.Aulitivik Island
Aulitivik Island is an uninhabited island located in the Qikiqtaaluk Region of Nunavut, Canada. It is located in Baffin Bay's Isabella Bay by the Davis Strait. Situated north of Baffin Island's Henry Kater Peninsula, it is a member of the Canadian Arctic Archipelago. Aulitiving Island is 19.5 km (12.1 mi) to the east, with tiny Bearslide Island lying between them.Aulitiving Island
Aulitiving Island is an uninhabited island located in the Qikiqtaaluk Region of Nunavut, Canada. It is located in Baffin Bay's Isabella Bay by the Davis Strait. It is situated north of Baffin Island's Henry Kater Peninsula. Aulitivik Island is 19.5 km (12.1 mi) to the west, with tiny Bearslide Island lying between them.Baffin Bay (Texas)
Baffin Bay is a bay in South Texas, an inlet of the larger Laguna Madre. Located near the Gulf of Mexico, Baffin Bay forms part of the boundary between Kenedy County and Kleberg County.Baffin Island Current
Baffin Island Current (or Baffin Current) is an ocean current running south down the western side of Baffin Bay in the Arctic Ocean, along Baffin Island. Its sources are the West Greenland Current and outflow from the Arctic Ocean. Its speed is approximately 17 km (11 mi) per day.Bergesen Island
Bergesen Island is an uninhabited island located in the Qikiqtaaluk Region of Nunavut, Canada. It is located in Baffin Bay off the northeastern coast of Baffin Island. Adams Island is 22.3 km (13.9 mi) to the south, while Dexterity Island is 17.2 km (10.7 mi) to the east, across Isbjorn Strait. The Dymond Islands lie close to its southwest.Canadian Arctic Rift System
The Canadian Arctic Rift System is a major North American geological structure extending from the Labrador Sea in the southeast through Davis Strait, Baffin Bay and the Arctic Archipelago in the northwest. It consists of a series of interconnected rifts that formed during the Paleozoic, Mesozoic and Cenozoic eras. Extensional stresses along the entire length of the rift system have resulted in a variety of tectonic features, including grabens, half-grabens, basins and faults.
Development of the Canadian Arctic Rift System was accompanied by two plate tectonic episodes that originated on opposite sides of the North American Plate and were propagated toward each other. Both were strongly controlled by pre-existing structures, which either guided the propagating faults or impeded their growth. The rift system is now inactive except for minor adjustments that are indicated by occasional earthquakes in Baffin Bay and the Labrador Sea.Coburg Island
Coburg Island (Inuktitut: Nirjutiqavvik) is an uninhabited island in Qikiqtaaluk, Nunavut, Canada. It is one of the members of Queen Elizabeth Islands located in Baffin Bay's Lady Ann Strait. It is separated from Ellesmere Island by Glacier Strait; Devon Island is to the south.
Elsewhere in Nunavut, there is also a tiny Saxe-Coburg Island, lying in Davis Strait, south of Leopold Island, itself east of Baffin Island's Cape Mercy (Cumberland Peninsula).Davis Strait
Davis Strait (French: Détroit de Davis) is a northern arm of the Labrador Sea. It lies between mid-western Greenland and Nunavut, Canada's Baffin Island. To the north is Baffin Bay. The strait was named for the English explorer John Davis (1550–1605), who explored the area while seeking a Northwest Passage. By the 1650s it was used for whale hunting.Devon Island
Devon Island (Inuit: Tatlurutit) is an island in Canada and the largest uninhabited island on Earth. It is located in Baffin Bay, Qikiqtaaluk Region, Nunavut, Canada. It is one of the larger members of the Canadian Arctic Archipelago, the second-largest of the Queen Elizabeth Islands, Canada's sixth-largest island, and the 27th-largest island in the world. It comprises 55,247 km2 (21,331 sq mi) (slightly smaller than Croatia) of Precambrian gneiss and Paleozoic siltstones and shales. The highest point is the Devon Ice Cap at 1,920 m (6,300 ft) which is part of the Arctic Cordillera. Devon Island contains several small mountain ranges, such as the Treuter Mountains, Haddington Range and the Cunningham Mountains. The notable similarity of its surface to that of Mars has attracted interest from scientists.Dexterity Island
Dexterity Island is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. It is located in Baffin Bay off the northeastern coast of Baffin Island. Adams Island is 19.3 km (12.0 mi) to the south, while Bergesen Island is 17.2 km (10.7 mi) to the west, across Isbjorn Strait.Hoved Island
Hoved Island is part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. The island is located between the Svendsen and Bjorne peninsulas, and within the Baumann Fiord of Ellesmere Island, considered part of the Queen Elizabeth Islands, in the Canadian Arctic Archipelago. It comprises an area of 158 km2 (61 sq mi).Hoved Island was first charted and named (hoved, Norwegian for "main") by the second Norwegian expedition of the Fram (1898—1902) under Capt. Otto Sverdrup.Nova Zembla Island
Nova Zembla Island ("New Land") is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. It is located across the mouth of Coutts Inlet in Baffin Bay off the northeastern coast of Baffin Island. Round Island is 7.4 km (4.6 mi) to the southeast.The island was visited in 1875 by a Swedish expedition led by Adolf Erik Nordenskiöld and sponsored by the businessman Oscar Dickson.Philpots Island
Philpots Island is a member of the Queen Elizabeth Islands and the Canadian Arctic Archipelago in the territory of Nunavut. It is the largest of Devon Island's offshore islands, located at Devon's eastern end. It lies in Baffin Bay, with Hyde Inlet to the north, and the Parry Channel to the south.
Philpots Island is home to northern fulmars, glaucous gulls, and ivory gullsQeqertarsuaq Island (Nasaussap Saqqaa)
Qeqertarsuaq Island is an island of Greenland. It is located in Baffin Bay in the Ussing Icefjord (Nasaussap Saqqaa) area of the Upernavik Archipelago.Round Island (Nunavut)
Round Island is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. It is located across the mouth of Coutts Inlet in Baffin Bay off the northeastern coast of Baffin Island. Nova Zembla Island is 7.4 km (4.6 mi) to the northwest.Another, smaller Nunavut Round Island is located in Cross Bay, at the land end of Chesterfield Inlet.Scott Island (Nunavut)
Scott Island is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. It is located in Baffin Bay, off the eastern coast of Baffin Island, in the middle of Scott Inlet, north of the confluence of Clark Fiord and Gibbs Fiord which embrace Sillem Island.
Another, much smaller Scott Island lies off the southwest coast of Baffin Island, near the mouth of Keltie Inlet.Sillem Island
Sillem Island is an uninhabited island in the Qikiqtaaluk Region of Nunavut, Canada. It is the second largest (after Bylot Island) of the several hundred islands and islets that are located in Baffin Bay, immediately off the northern coast of Baffin Island. It is defined by Clark and Gibbs Fiords, which join at its northern end to form Scott Inlet. Further north lies Scott Island.Upernavik Archipelago
Upernavik Archipelago is a vast coastal archipelago in the Avannaata municipality in northwestern Greenland, off the shores of northeastern Baffin Bay. The archipelago extends from the northwestern coast of Sigguup Nunaa peninsula in the south at approximately 71°50′N 56°00′W to the southern end of Melville Bay (Greenlandic: Qimusseriarsuaq) in the north at approximately 74°50′N 57°30′W.
Marginal seas of the Atlantic Ocean