Information about Polynya

A polynya (US common spelling) or polynia (UK common spelling) (Russian: полынья; IPA: [pəlɨˈnʲja] ice hole) is any non-linear area of open water surrounded by sea ice. It is now used as geographical term for areas of sea in Arctic or Antarctic regions which remain unfrozen for much of the year.

The Polynia was the name for the sea believed to surround the North Pole.

Formation

Polynyas are formed through two main processes:
  • The first mechanism for polynya formation is thermodynamically driven, and occurs when the surface water temperature never reaches the freezing point. This may be due to a region of warm water upwelling, which reduces ice production and may stop it altogether. This type of polynya is called a Sensible Heat Polynya.
  • The second type of polynya is called a Latent Heat Polynya and is formed through the action of the wind or ocean currents which act to drive ice away from a fixed boundary, such as a coastline, fast ice, or an ice bridge. The polynya forms by initially the first year pack ice being driven away from the coast, which leaves an area of open water within which new ice is formed. This new ice is then also herded downwind toward the first year pack ice. When it reaches the pack ice the new ice is consolidated onto the first year pack ice. The latent heat polynya is the open water region between the coast and the first year ice pack.
Latent heat polynyas are regions of high ice production and therefore are possible sites of dense water production in both polar regions. The high ice production rates within these polynyas leads to a large amount of brine rejection into the surface waters. This salty water then sinks and mixes to possibly form new water masses. It is an open question as to whether the polynyas of the Arctic can produce enough dense water to form a major portion of the dense water required to drive the thermohaline circulation.

Some polynyas, such as the North Water Polynya in Canada, occur seasonally at the same time and place each year. Because animals can adapt their life strategies to this regularity, these types of polynyas are of special ecological research significance. In winter, marine mammals such as walruses, narwhals and belugas that do not migrate south, remain there. In spring, the thin or absent ice cover allows light in, through the surface layer as soon as the winter night ends, which triggers the early blooming of microalgae that are at the basis of the marine food chain. So, polynyas are suspected to be places where intense and early production of the planktonic herbivores ensure the transfer of solar energy (food chain) fixed by planktonic microalgae to Arctic cod, seals, whales, and polar bears.

Reference

The Polynia

A Russian word Полынья for a hole in the ice was adopted in the 19th century by polar explorers to describe navigable portions of the sea.[1] It was then rumoured that there was open sea around the North Pole, which was referred to as Polynia, or Kane’s Polynia. “The mystic Polynia, the open sea to the North of Siberia.”[2] The search for this Polar Sea is related to, and comparable with that for the North-West Passage.[3]

References

#^ Sherard Osborn, Peter Wells, A Petermann Proceedings of the Royal Geographical Society of London Vol 12 no 2 1867-1868 pages 92-113 On the Exploration of the North Polar Region
#^ Sherard Osborn Proceedings of the Royal Geographical Society of London, Vol. 16, No. 3. (1871 - 1872), pp. 227-241 On the Exploration of the North Polar Basin, with a Résumé of Recent Swedish, German and Austrian Attempts to Reach the Polar Circle from the Atlantic Ocean
#^  John K. Wright Geographical Review, Vol. 43, No. 3. (Jul., 1953), pp. 338-365 The Open Polar Sea

Other Uses

Reference

#^ F. A. McDiarmid The Geographical Journal, Vol. 62, No. 4. (Oct., 1923), pp. 293-302 Geographical Determinations of the Canadian Arctic Expedition

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Sea ice is formed from ocean water that freezes. Because the oceans consist of saltwater, this occurs at about -1.8 °C (28.8 °F).

Sea ice may be contrasted with icebergs, which are chunks of ice shelves or glaciers that calve into the ocean.
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Arctic is the region around the Earth's North Pole, opposite the Antarctic region around the South Pole. In the northern hemisphere, the Arctic includes the Arctic Ocean (which overlies the North Pole) and parts of Canada, Greenland (a territory of Denmark), Russia, the United
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North Pole, also known as the Geographic North Pole or Terrestrial North Pole, is, subject to the caveats explained below, defined as the point in the northern hemisphere where the Earth's axis of rotation meets the Earth's surface.
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Freezing point can refer to several things:
  • For the chemistry term, see Melting point.
  • For the news journal in the People's Republic of China, see Freezing Point.
  • For the 1966 Japanese film, see Freezing Point (1966 film).

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Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water.
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ocean current is any more or less continuous, directed movement of ocean water that flows in one of the Earth's oceans. Ocean Currents are rivers of hot or cold water within the ocean.
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coast is defined as the part of the land adjoining or near the ocean. A coastline is properly a line on a map indicating the disposition of a coast, but the word is often used to refer to the coast itself.
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Sea ice is formed from ocean water that freezes. Because the oceans consist of saltwater, this occurs at about -1.8 °C (28.8 °F).

Sea ice may be contrasted with icebergs, which are chunks of ice shelves or glaciers that calve into the ocean.
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Ice roads or ice bridges are frozen structures formed over bays, inlets, rivers or lake surfaces. An ice bridge is a structure which is typically formed during glaciation, and may be related to a significant migration of prehistoric peoples.
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Drift ice consists of sea ice that floats on the surface of the water in cold regions, as opposed to fast ice, which is attached ("fastened") to a shore. Usually drift ice is carried along by winds and sea currents, hence its name, "drift ice".
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polar regions are the areas of the globe surrounding the poles also known as frigid zones. The North Pole and South Pole being the centers, these regions are dominated by the polar ice caps, resting respectively on the Arctic Ocean and the continent of Antarctica.
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water mass is an identifiable body of water which has physical properties distinct from surrounding water. Properties include temperature, salinity, chemical - isotopic ratios, and other physical quantities.
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Arctic is the region around the Earth's North Pole, opposite the Antarctic region around the South Pole. In the northern hemisphere, the Arctic includes the Arctic Ocean (which overlies the North Pole) and parts of Canada, Greenland (a territory of Denmark), Russia, the United
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thermohaline circulation (THC) is the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water.
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marine mammal is a mammal that is primarily ocean-dwelling or depends on the ocean for its food. Mammals originally evolved on land, but later marine mammals evolved to live back in the ocean.
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Odobenidae
Allen, 1880

Genus: Odobenus
Brisson, 1762

Species: O.
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Monodon

Species: M. monoceros

Binomial name
Monodon monoceros
Linnaeus, 1758

Narwhal range (in blue)

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Delphinapterus

Species: D. leucas

Binomial name
Delphinapterus leucas
(Pallas, 1776)

Beluga range

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Microalgae are a type of photosynthetic protist. While the mechanism of photosynthesis in microalgae is similar to that of true plants, they are generally more efficient converters of solar energy because of their simple cellular structure.
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Food chains, food webs and/or food networks describe the feeding relationships between species in an ecological community. They graphically represent the transfer of material and energy from one species to another within an ecosystem.
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Arctogadus

Species: A. glacialis

Binomial name
Arctogadus glacialis
Peters, 1872

The Arctic cod (Arctogadus glacialis
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Pinnipeds ("fin-feet", lit. "winged feet") are marine mammals belonging to the former biological suborder Pinnipedia (sometimes now a superfamily) of the order Carnivora. The pinnipeds now fall within the suborder Caniformia and comprise the families Odobenidae (walruses),
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whale can refer to all cetaceans, to just the larger ones, or only to members of particular families within the order Cetacea. The last definition is the one followed here. Whales are those cetaceans which are neither dolphins (i.e.
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North Pole, also known as the Geographic North Pole or Terrestrial North Pole, is, subject to the caveats explained below, defined as the point in the northern hemisphere where the Earth's axis of rotation meets the Earth's surface.
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The Northwest Passage is a sea route through the Arctic Ocean, along the northern coast of North America via the waterways amidst the Canadian Arctic Archipelago, connecting the Atlantic and Pacific Oceans.
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