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    Location of the Arctic

    Artificially coloured topographical

    map of the Arctic region

    MODIS image of the Arctic

    From Wikipedia, the free encyclopedia

    The Arctic(/rktk/ or /rtk/) is a polar region located at the

    northernmost part of the Earth. The Arctic consists of the Arctic Ocean

    and parts of Canada, Russia, the United States (Alaska), Denmark

    (Greenland), Norway, Sweden, Finland, and Iceland. The Arctic region

    consists of a vast, ice-covered ocean, surrounded by treeless permafrost.The area can be defined as north of the Arctic Circle (66 33'N), the

    approximate limit of the midnight sun and the polar night. Alternatively,

    it can be defined as the region where the average temperature for the

    warmest month (July) is below 10 C (50 F); the northernmost tree line

    roughly follows the isotherm at the boundary of this region.[1][2]

    Socially and politically, the Arctic region includes the northern

    territories of the eight Arctic states, although by natural science

    definitions much of this territory is considered subarctic. The Arctic

    region is a unique area among Earth's ecosystems. The cultures in theregion and the Arctic indigenous peoples have adapted to its cold and

    extreme conditions. In recent years the extent of the sea ice has declined.[3][4]Life in the Arctic includes organisms living in the ice,[5]

    zooplankton and phytoplankton, fish and marine mammals, birds, land

    animals, plants and human societies.

    1 Etymology

    2 Climate

    3 Flora and fauna

    3.1 Plants

    3.2 Animals

    4 Natural resources

    5 Paleo-history

    6 Indigenous population

    7 International cooperation and politics

    7.1 Territorial claims

    7.2 Exploration

    7.3 Pollution

    7.4 Preservation

    8 Climate change

    9 Arctic waters

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    10 Arctic lands

    11 See also

    12 References

    13 Bibliography

    14 Further reading

    15 External links

    The word Arctic comes from the Greek (arktikos), "near the Bear, northern"[6]and that from the word

    (arktos), meaning bear.[7]The name refers either to the constellation Ursa Major, the "Great Bear",

    which is prominent in the northern portion of the celestial sphere, or to the constellation Ursa Minor, the "Little

    Bear", which contains Polaris, the Pole Star, also known as the North Star.[8]

    The Arctic's climate is characterized by cold winters and cool summers. Precipitation mostly comes in the form

    of snow. The Arctic's annual precipitation is low, with most of the area receiving less than 50 cm (20 in). High

    winds often stir up snow, creating the illusion of continuous snowfall. Average winter temperatures can be as

    low as 40 C (40 F), and the coldest recorded temperature is approximately 68 C (90 F). Coastal Arctic

    climates are moderated by oceanic influences, having generally warmer temperatures and heavier snowfalls

    than the colder and drier interior areas. The Arctic is affected by current global warming, leading to Arctic sea

    ice shrinkage and Arctic methane release.

    Due to the poleward migration of the planet's isotherms (about 35 mi (56 km) per decade during the past 30

    years as a consequence of global warming), the Arctic region (as defined by tree line and temperature) is

    currently shrinking.[9]Perhaps the most spectacular result of Arctic shrinkage is sea ice loss. There is a large

    variance in predictions of Arctic sea ice loss, with models showing near-complete to complete loss in

    September from 2040 to some time well beyond 2100. About half of the analyzed models show near-complete

    to complete sea ice loss in September by the year 2100.[3]

    Plants

    Arctic vegetation is composed of plants such as dwarf shrubs, graminoids, herbs, lichens and mosses, which all

    grow relatively close to the ground, forming tundra. As one moves northward, the amount of warmth available

    for plant growth decreases considerably. In the northernmost areas, plants are at their metabolic limits, and

    small differences in the total amount of summer warmth make large differences in the amount of energy

    available for maintenance, growth and reproduction. Colder summer temperatures cause the size, abundance,

    productivity and variety of plants to decrease. Trees cannot grow in the Arctic, but in its warmest parts, shrubs

    are common and can reach 2 m (6 ft 7 in) in height; sedges, mosses and lichens can form thick layers. In the

    coldest parts of the Arctic, much of the ground is bare; non-vascular plants such as lichens and mosses

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    Muskox

    Marine fossils in Canadian Arctic

    predominate, along with a few scattered grasses and forbs (like the arctic poppy).

    Animals

    Herbivores on the tundra include the Arctic hare, lemming, muskox, and

    caribou. They are preyed on by the Snowy owl, Arctic fox and wolf. The

    polar bear is also a predator, though it prefers to hunt for marine life

    from the ice. There are also many birds and marine species endemic tothe colder regions. Other land animals include wolverines, ermines, and

    Arctic ground squirrels. Marine mammals include seals, walrus, and

    several species of cetaceanbaleen whales and also narwhals, killer

    whales and belugas.

    The Arctic includes sizable natural resources (oil, gas, minerals, fresh water, fish and if the subarctic is

    included, forest) to which modern technology and the economic opening up of Russia have given significant

    new opportunities. The interest of the tourism industry is also on the increase.

    The Arctic is one of the last and most extensive continuous wilderness areas in the world, and its significance in

    preserving biodiversity and genotypes is considerable. The increasing presence of humans fragments vital

    habitats. The Arctic is particularly susceptible to the abrasion of groundcover and to the disturbance of the rare

    reproduction places of the animals that are characteristic to the region. The Arctic also holds 1/5 of the Earth's

    water supply.

    During the Cretaceous, the Arctic still had seasonal snows, though only

    a light dusting and not enough to permanently hinder plant growth.

    Animals such as Chasmosaurus,Hypacrosaurus, Troodon, and

    Edmontosaurusmay have all migrated north to take advantage of the

    summer growing season, and migrated south to warmer climes when the

    winter came. A similar situation may also have been found amongst

    dinosaurs that lived in Antarctic regions, such asMuttaburrasaurusof

    Australia.

    The earliest inhabitants of North America's central and eastern Arctic are referred to as the Arctic small tooltradition (AST) and existed c. 2500 BC. AST consisted of several Paleo-Eskimo cultures, including the

    Independence cultures and Pre-Dorset culture.[10][11]The Dorset culture (Inuktitut: Tuniitor Tunit) refers to the

    next inhabitants of central and eastern Arctic. The Dorset culture evolved because of technological and

    economic changes during the period of 1050550 BC. With the exception of the Quebec/Labrador peninsula,

    the Dorset culture vanished around 1500 AD.[12]Supported by genetic testing, evidence shows that Dorset

    culture, known as the Sadlermiut, survived in Aivilik, Southampton and Coats Islands, until the beginning of

    the 20th century.[13]

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    Polar bears on the sea ice of the

    Arctic Ocean, near the North Pole.

    USSHonolulupictured.

    Dorset/Thule culture transition dates around the 9th10th centuries. Scientists theorize that there may have been

    cross-contact of the two cultures with sharing of technology, such as fashioning harpoon heads, or the Thule

    may have found Dorset remnants and adapted their ways with the predecessor culture.[14]Others believe the

    Thule displaced the Dorset. By 1300, the Inuit, present-day Arctic inhabitants and descendants of Thule culture,

    had settled in west Greenland, and moved into east Greenland over the following century. Over time, the Inuit

    have migrated throughout the Arctic regions of Canada, Greenland, Russia and the United States.[15]

    Other Circumpolar North indigenous peoples include the Buryat, Chukchi, Evenks, Inupiat, Khanty, Koryaks,Nenets, Sami, Yukaghir, and Yupik, who still refer to themselves as Eskimo which means "snowshoe netters",

    not "raw meat eaters" as it is sometimes mistakenly translated.[16]

    The eight Arctic nations (Canada, Denmark (Greenland & The Faroe

    Islands), Finland, Iceland, Norway, Sweden, Russia, and USA) are all

    members of the Arctic Council, as are organizations representing six

    indigenous populations. The Council operates on consensus basis,

    mostly dealing with environmental treaties and not addressing boundaryor resource disputes.

    Though Arctic policy priorities differ, every Arctic nation is concerned

    about sovereignty/defense, resource development, shipping routes, and

    environmental protection. Much work remains on regulatory agreements

    regarding shipping, tourism, and resource development in Arctic waters.

    Research in the Arctic has long been a collaborative international effort,

    evidenced perhaps most notably by the International Polar Year. The

    International Arctic Science Committee, hundreds of scientists and specialists of the Arctic Council, and the

    Barents Euro-Arctic Council are more examples of collaborative international Arctic research.

    Territorial claims

    No country owns the geographic North Pole or the region of the Arctic Ocean surrounding it. The surrounding

    Arctic states that border the Arctic Ocean Canada, Denmark (via Greenland), Iceland, Norway, Russia, and

    the United States are limited to a 200 nautical miles (370 km; 230 mi) economic zone around their coasts.

    Upon ratification of the United Nations Convention on the Law of the Sea, a country has ten years to make

    claims to an extended continental shelf beyond its 200 nautical mile zone.[17]Due to this, Norway (which

    ratified the convention in 1996),[18]

    Russia (ratified in 1997),[18]

    Canada (ratified in 2003)[18]

    and Denmark(ratified in 2004)[18]launched projects to establish claims that certain sectors of the Arctic seabed should

    belong to their territories.

    On August 2, 2007, two Russian bathyscaphes, MIR-1 and MIR-2, for the first time in history descended to the

    Arctic seabed beneath the North Pole and placed there a Russian flag made of rust-proof titanium alloy. The

    mission was a scientific expedition, but the flag-placing during Arktika 2007, raised concerns of a race for

    control of the Arctic's vast petroleum resources.[19]

    Foreign ministers and other officials representing Canada, Denmark, Norway, Russia, and the United States met

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    Long-range pollution pathways to the

    Arctic

    in Ilulissat, Greenland on May 28, 2008 at the Arctic Ocean Conference and announced the Ilulissat

    Declaration,[20][21]blocking any "new comprehensive international legal regime to govern the Arctic Ocean,"

    and pledging "the orderly settlement of any possible overlapping claims."[22]

    As of 2012, Denmark is claiming the continental shelf between Greenland and the North Pole.[23]The Russian

    Federation is claiming a large swath of seabed along the Lomonosov Ridge but confined to its sector of the

    Arctic.

    Exploration

    Since 1937, the whole Arctic region has been extensively explored by Soviet and Russian manned drifting ice

    stations. Between 1937 and 1991, 88 international polar crews established and occupied scientific settlements

    on the drift ice and were carried thousands of kilometers by the ice flow.[24]

    Pollution

    The Arctic is comparatively clean, although there are certain

    ecologically difficult localized pollution problems that present a seriousthreat to people's health living around these pollution sources. Due to the

    prevailing worldwide sea and air currents, the Arctic area is the fallout

    region for long-range transport pollutants, and in some places the

    concentrations exceed the levels of densely populated urban areas. An

    example of this is the phenomenon of Arctic haze, which is commonly

    blamed on long-range pollutants. Another example is with the

    bioaccumulation of PCB's (polychlorinated biphenyls) in Arctic wildlife

    and people.

    Preservation

    There have been many proposals to preserve the Arctic over the years. Most recently a group of stars at the Rio

    Earth Summit, on June 21, 2012, proposed protecting the Arctic, similar to the Antarctic protection. The initial

    focus of the campaign will be a UN resolution creating a global sanctuary around the pole, and a ban on oil

    drilling and unsustainable fishing in the Arctic.[25]

    The Arctic is especially vulnerable to the effects of global warming, as has become apparent in the melting sea

    ice in recent years. Climate models predict much greater warming in the Arctic than the global average,[28]

    resulting in significant international attention to the region. In particular, there are concerns that Arctic

    shrinkage, a consequence of melting glaciers and other ice in Greenland, could soon contribute to a substantial

    rise in sea levels worldwide.[29]The climate models on which the IPCC report Nr.4 is based give a range of

    predictions of Arctic sea ice loss, showing near-complete to complete loss in September anywhere from 2040 to

    some time well beyond 2100. About half of the analyzed models show near-complete to complete sea ice loss in

    September by the year 2100.[3]More recently, the Catlin Arctic Survey concluded that summer ice loss would

    occur around 2029.[30][31]

    It has been apparent though since 2007, that those models grossly underestimate sea

    ice loss.[32]

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    Arctic sea ice coverage as of 2007

    compared to 2005 and compared to

    19792000 average

    The development of Arctic sea ice

    area as measured with satellites.[26]

    The development of Arctic sea ice

    volume as estimated by measurement

    corrected numerical simulation shows

    probability of total sea ice loss insummer for the near future.

    [27]

    As can be seen in the two plot at the right, since about 1995 to 2000, all

    three size numbers of the Arctic sea ice shield (extent, area and volume)

    are decreasing in an accelerated way. This downward movement is

    modulated by statistical variations, which lead to considerable media

    attention, when a new record has been reached.

    Concerning melting records, 2012 was a productive year, thus

    corroborating the tendency of the past decade. This may have been

    furthered by a strong summer storm cyclone, a rare event in the Arctic,which spread the already very thin ice and caused mixing of the cold

    surface waters with deeper warmer water layers. According to the

    University of Bremen, in September 2011 the Arctic ice cap was smaller

    than ever recorded (the satellite measurements started in the 1970s).[33][34]Arctic ice is declining in area and thinning. Arctic temperatures

    have risen more than twice as fast as the global average over the past

    half century. The speed of change has shocked scientists. If current

    trends continue, a largely ice-free Arctic in the summer is likely within

    30 years up to 40 years earlier than was anticipated by the IPCC

    Fourth Assessment Report.[35]

    As the volume of sea ice until recently could not be measured by remote

    sensing as easy as its extent, numerical models have been made to

    estimate the ice thickness field between known points, which then is

    summed up to yield ice volume. The resulting volume over time reveals

    a much stronger loss of ice than ice extent studies suggest.[27]

    The current Arctic shrinkage is leading to fears of Arctic methane

    release.[36]Release of methane stored in permafrost could cause abrupt

    and severe global warming,[37]

    as methane is a potent greenhouse gas.On millennial time-scales, decomposition of methane hydrates in the

    Arctic seabed could also amplify global warming. Previous methane

    release events have been linked to the great dying, a mass extinction

    event at the boundary of the Permian and Triassic, and the Paleocene

    Eocene Thermal Maximum, in which temperatures abruptly increased.

    Apart from concerns regarding the detrimental effects of warming in the

    Arctic, some potential opportunities have gained attention. The melting

    of the ice is making the Northwest Passage, the shipping routes through

    the northernmost latitudes, more navigable, raising the possibility that

    the Arctic region will become a prime trade route.[38]In addition, it is

    believed that the Arctic seabed may contain substantial oil fields which

    may become accessible if the ice covering them melts.[39]These factors

    have led to recent international debates as to which nations can claim sovereignty or ownership over the waters

    of the Arctic.[40][41][42][43]

    The National Oceanic and Atmospheric Administration's Arctic Report Card[44]presents annually updated,

    peer-reviewed information on recent observations of environmental conditions in the Arctic relative to historical

    records.

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    Eidsfjord in Vesterlen, Norway is250 km (160 mi) inside the Arctic

    Circle, but the comparatively

    temperate Norwegian sea gives a

    mean annual temperature of 4 C

    (39 F) and a three-month summer

    above 10C.[45]

    Arctic Ocean

    Baffin Bay

    Beaufort Sea

    Barents Sea

    Bering Sea

    Bering Strait

    Chukchi Sea

    Davis Strait

    Denmark Strait

    East Siberian

    Sea

    Greenland Sea

    Hudson Bay

    Kara Sea

    Laptev Sea

    Nares Strait

    Norwegian Sea

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    Geographic Designation National Affiliation Designation

    Alaska United States State

    Aleutian Islands United States Alaskan Archipelago

    Arkhangelsk Oblast Russia Federal subject

    Canadian Arctic Archipelago Canada Canadian Archipelago

    Diomede Island (Big) Russia Island

    Diomede Island (Little) United States Island

    Finnmark Norway County

    Franz Josef Land Russia Federal subject archipelago

    Greenland Denmark Autonomous country

    Grmsey Iceland Island

    Jan Mayen Norway Island

    Lapland Finland Region

    Lapland Sweden Province

    New Siberian Islands Russia Archipelago

    Nordland Norway County

    Norrbotten Sweden Province

    Northwest Territories Canada Territory

    Novaya Zemlya Russia Federal subject archipelago

    Nunavik Canada Northern part of Quebec

    Nunavut Canada Territory

    Russian Arctic islands Russia Islands

    Spmi Norway, Sweden, Finland, Russia Fennoscandia region

    Sakha Republic Russia Federal subject

    Severnaya Zemlya Russia Federal subject archipelago

    Siberia Russia Region

    Svalbard Norway Governor of Svalbard archipelago

    Troms Norway County

    Yukon Canada Territory

    Wrangel Island Russia Zapovednik (nature reserve)

    Poverty in the Arctic

    List of countries by northernmost point

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    Energy Studies, August 2007

    GLOBIO Human Impact maps (http://www.globio.info/region/polar/#arctic)Report on human impacts on

    the Arctic

    Krupnik, Igor, Michael A. Lang, and Scott E. Miller, eds. Smithsonian at the Poles: Contributions to

    International Polar Year Science.(http://www.sil.si.edu/smithsoniancontributions/proceedings

    /sc_RecordSingle.cfm?series=IPY&toplevel=1) Washington, D.C.: Smithsonian Institution Scholarly

    Press, 2009.

    Kpyl, Juha & Mikkola, Harri: The Global Arctic: The Growing Arctic Interests of Russia, China, the

    United States and the European Union (http://www.fiia.fi/en/publication/347/the_global_arctic/) FIIA

    Briefing Paper 133, August 2013, The Finnish Institute of International Affairs (http://www.fiia.fi/en/).

    Arctic Report Card (http://www.arctic.noaa.gov)

    International Arctic Research Center (http://www.iarc.uaf.edu)

    Arctic Theme Page (http://www.arctic.noaa.gov) Comprehensive Arctic Resource from NOAA.

    WWF International Arctic Programme (http://www.panda.org/arctic) Arctic environment and

    conservation information

    Bering Sea Climate and Ecosystem (http://www.beringclimate.noaa.gov) Current state of the Bering Sea

    Climate and Ecosystem. Comprehensive resource on the Bering Sea with viewable oceanographic,

    atmospheric, climatic, biological and fisheries data with ecosystem relevance, recent trends, essays on

    key Bering Sea issues, maps, photos, animals and more. From NOAA.

    Toxoplasma gondii in the Subarctic and Arctic (http://www.actavetscand.com/content/pdf/1751-0147-52-

    S1-S7.pdf)

    Protecting U.S. Sovereignty: Coast Guard Operations in the Arctic: Hearing before the Subcommittee on

    Coast Guard and Maritime Transportation of the Committee on Transportation and Infrastructure, House

    of Representatives, One Hundred Twelfth Congress, First Session, December 1, 2011 (http://purl.fdlp.gov

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    /GPO/gpo23245)

    Maps

    Arctic Environmental Atlas (http://maps.grida.no/arctic) Circum-Arctic interactive map, with multiple

    layers of information

    Interactive Satellite Map (http://www.arctic.io/observations/) with daily update (true color/infrared)

    Media

    The Emerging Arctic (http://www.cfr.org/arctic/emerging-arctic/p32620#!/) An Infoguide from the

    Council on Foreign Relations

    "Global Security, Climate Change, and the Arctic" (http://acdis.illinois.edu/newsarchive/newsitem-

    VideoGlobalSecurityClimateChangeandtheArctic.html) streaming video of November 2009 symposium

    at the University of Illinois

    Implications of an Ice-Free Arctic for Global Security (http://acdis.illinois.edu/newsarchive/newsitem-

    ImplicationsofanIceFreeArcticforGlobalSecurity.html) November 2009 radio interview with Professor

    Klaus Dodds (Royal Holloway, University of London)

    The Canadian Museum of Civilization The Story of the Canadian Arctic Expedition of 19131918

    (http://www.civilization.ca/cmc/exhibitions/hist/cae/indexe.shtml)

    UNEP/GRID-Arendal Maps and Graphics library (http://maps.grida.no/go/searchRegion/regionid

    /geoarctic) Information resources from the UN Environment programme

    Arctic Institute of North America Digital Library (http://contentdm.ucalgary.ca

    /cdm4/browse.php?CISOROOT=/aina3) Over 8000 photographs dating from the late 19th century

    through the 20th century.

    euroarctic.com (http://www.euroarctic.com/) News service from the Barents region provided by

    Norwegian Broadcasting Corp (NRK), Swedish Radio (SR) and STBC Murman.

    arcticfocus.com (http://www.arcticfocus.com/) Independent News service covering Arctic region with

    daily updates on environment, Arctic disputes and business

    Vital Arctic Graphics (http://www.vitalgraphics.net/arctic.cfm) Overview and case studies of the Arctic

    environment and the Arctic Indigenous Peoples.

    Arctic and Taiga Canadian Atlas (http://www.canadiangeographic.ca/atlas/themes.aspx?id=artic&

    lang=En)

    Scientific Facts on Arctic Climate Change (http://www.greenfacts.org/en/arctic-climate-change

    /index.htm)

    PolarTREC (http://www.polartrec.com) PolarTREC-Teachers and Researchers Exploring and

    Collaborating

    Arctic Change (http://www.arctic.noaa.gov/detect/):Information on the present state of Arctic ecosystems

    and climate, presented in historical context (from NOAA, updated regularly)

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    Monthly Sea Ice Outlook (http://www.arcus.org/search/seaiceoutlook/)

    UN Environment Programme Key Polar Centre at UNEP/GRID-Arendal (http://polar.grida.no/)

    Arctic Geobotanical Atlas, University of Alaska Fairbanks (http://www.arcticatlas.org)

    Polar Discovery (http://polardiscovery.whoi.edu/)

    Arctic Transform (http://www.arctic-transform.eu/) Transatlantic Policy Options for Supporting

    Adaptation in the Marine Arctic

    ArcticStat Circumpolar Database (http://www.arcticstat.org/)

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    Categories: Arctic Polar regions of the Earth

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