{ "Introduction": { "Background": { "text": "The Arctic Ocean is the smallest of the world's five oceans (after the Pacific Ocean, Atlantic Ocean, Indian Ocean, and the Southern Ocean). The Northwest Passage (US and Canada) and Northern Sea Route (Norway and Russia) are two important seasonal waterways. In recent years the polar ice pack has receded in the summer allowing for increased navigation and raising the possibility of future sovereignty and shipping disputes among the six countries bordering the Arctic Ocean (Canada, Denmark (Greenland), Iceland, Norway, Russia, US)." } }, "Geography": { "Location": { "text": "body of water between Europe, Asia, and North America, mostly north of the Arctic Circle" }, "Geographic coordinates": { "text": "90 00 N, 0 00 E" }, "Map references": { "text": "Arctic Region" }, "Area": { "total": { "text": "15.558 million sq km" }, "note": "note: includes Barents Sea, Beaufort Sea, Chukchi Sea, East Siberian Sea, Greenland Sea, Kara Sea, Laptev Sea, Northwest Passage, Norwegian Sea, and other tributary water bodies" }, "Area - comparative": { "text": "slightly less than 1.5 times the size of the US" }, "Coastline": { "text": "45,389 km" }, "Climate": { "text": "polar climate characterized by persistent cold and relatively narrow annual temperature range; winters characterized by continuous darkness, cold and stable weather conditions, and clear skies; summers characterized by continuous daylight, damp and foggy weather, and weak cyclones with rain or snow" }, "Terrain": { "text": "
central surface covered by a perennial drifting polar icepack that, on average, is about 3 m thick, although pressure ridges may be three times that thickness; the icepack is surrounded by open seas during the summer, but more than doubles in size during the winter and extends to the encircling landmasses; the ocean floor is about 50% continental shelf (highest percentage of any ocean) with the remainder a central basin interrupted by three submarine ridges (Alpha Cordillera, Nansen Cordillera, and Lomonosov Ridge)
major surface currents: two major, slow-moving, wind-driven currents (drift streams) dominate: a clockwise drift pattern in the Beaufort Gyre in the western part of the Arctic Ocean and a nearly straight line Transpolar Drift Stream that moves eastward across the ocean from the New Siberian Islands (Russia) to the Fram Strait (between Greenland and Svalbard); sea ice that lies close to the center of the gyre can complete a 360 degree circle in about 2 years, while ice on the gyre periphery will complete the same circle in about 7-8 years; sea ice in the Transpolar Drift crosses the ocean in about 3 years
" }, "Elevation": { "highest point": { "text": "sea level" }, "lowest point": { "text": "Molloy Deep -5,577 m" }, "mean depth": { "text": "-1,205 m" }, "ocean zones": { "text": "Composed of water and in a fluid state, the oceans are delimited differently than the solid continents. Oceans are divided into three zones based on depth and light level. Although some sea creatures depend on light to live, others can do without it. Sunlight entering the water may travel about 1,000 m into the oceans under the right conditions, but there is rarely any significant light beyond 200 m.record summer melting of sea ice in the Arctic has renewed interest in maritime shipping lanes and sea floor exploration
Canada-US: dispute how to divide the Beaufort Sea and the status of the Northwest Passage but continue to work cooperatively to survey the Arctic continental shelf
Canada-Denmark (Greenland)-Norway: have made submissions to the UN Commission on the Limits of the Continental shelf (CLCS)
Norway-Russia: signed a comprehensive maritime boundary agreement in 2010; Russia has augmented its 2001 CLCS submission