Climate Of The Nordic Countries
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Climate Of The Nordic Countries
The climate of the Nordic countries is that of a region in Northern Europe that consists of Denmark, Finland, Iceland, Norway and Sweden and their associated territories, which include the Faroe Islands, Greenland and Åland. Stockholm, Sweden has on average the warmest summer of the Nordic capitals, with an average maximum temperature of in July; Copenhagen, Oslo and Helsinki have an average July maximum temperature of . Seasonal conditions Winter In Denmark, January temperatures average between and . Denmark's coldest month, however, is February, where the mean temperature is . The number of hours of sunlight per day does increase during the month of February for Denmark, where they get seven to eight hours a day. Iceland winters are generally mild considering how high its latitude is. The coastal lowlands of Iceland have average January temperatures of about , while the highlands of central Iceland generally stay below . The lowest winter temperatures in Iceland are usua ...
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Lapporten Winter
Lapporten (Swedish: "The Lapponian Gate") or Tjuonavagge (Northern Sami: ''Čuonjávággi'', "Goose Valley") is a U-shaped valley U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight s ... located just outside Abisko National Park in Lapland in northern Sweden, one of the most familiar natural sights of the mountains there. The valley is bounded to the southwest of the mountain Nissuntjårro (1,738 m) and in the northeast of Tjuonatjåkka (1,554 m). In the middle of the valley lies Lake Čuonjájávri, 950 metres above sea level. The terrain is easy to walk but has no marked trail. Lapporten is in the Nissuntjårro Natura 2000 site. A world record in highline was set by 4 Germans crossing the distance between the mountains on a slackline more than above ground. References Valley ...
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University Of Iceland
The University of Iceland ( is, Háskóli Íslands ) is a public research university in Reykjavík, Iceland and the country's oldest and largest institution of higher education. Founded in 1911, it has grown steadily from a small civil servants' school to a modern comprehensive university, providing instruction for about 14,000 students in twenty-five faculties. Teaching and research is conducted in social sciences, humanities, law, medicine, natural sciences, engineering and teacher education. It has a campus concentrated around ''Suðurgata'' street in central Reykjavík, with additional facilities located in nearby areas as well as in the countryside. History The University of Iceland was founded by the Alþingi on 17 June 1911, uniting three former post-secondary institutions: ''Prestaskólinn'', ''Læknaskólinn'' and ''Lagaskólinn'', which taught theology, medicine and law, respectively. The university originally had only faculties for these three fields, in addition to a fa ...
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Liverpool Land
Liverpool Land is a peninsula in eastern Greenland. Geography The peninsula is bounded by Scoresby Sund in the south, Carlsberg Fjord in the northwest, ''Kangerterajiva'' (Hurry Inlet) in the southwest, the Greenland Sea in the east, and Jameson Land in the west. It was named by William Scoresby, who thought that Hurry Inlet had a confluence with Carlsberg Fjord, separating Liverpool Land from Jameson Land. The fjord-rich peninsula is long from Kap Greville in the north to Uunarteq ( da, Kap Tobin) in the south, up to wide, and measures about in area. It is connected to Jameson Land over a length of . A large part of Liverpool Land is mountainous, the Didrik Pining Range and the Heywood Range are located in the peninsula. Warming Island is located approximately off the northeastern tip of Liverpool Land. Storefjord indents the peninsula from the east about , almost cutting it into two. The southern coast of Liverpool Land is the location of the town of Ittoqqortoormiit a ...
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Uunartoq Qeqertoq
Uunartoq Qeqertaq ( Greenlandic), ''Warming Island'' in English, is an island off the east central coast of Greenland, north of the Arctic Circle. It became recognised as an island only in September 2005, by US explorer Dennis Schmitt. It was attached to the mainland of Liverpool Land by glacial ice even in 2002, when the ice shelves began retreating rapidly in this area, so that by 2005 it was no longer attached to the mainland. Members of the scientific community believe this newly discovered island is a direct result of global warming. Controversy Patrick Michaels, a climatologist and prominent global warming denier, created a controversy over the history of Warming Island in a post on his website, World Climate Report, in which he argued that the island had been previously uncovered in the 1950s toward the end of a brief warm period in Greenland. Despite a general lack of suitably detailed maps, Michaels found a map published by Ernst Hofer, a photographer who did aerial ...
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NASA
The National Aeronautics and Space Administration (NASA ) is an independent agency of the US federal government responsible for the civil space program, aeronautics research, and space research. NASA was established in 1958, succeeding the National Advisory Committee for Aeronautics (NACA), to give the U.S. space development effort a distinctly civilian orientation, emphasizing peaceful applications in space science. NASA has since led most American space exploration, including Project Mercury, Project Gemini, the 1968-1972 Apollo Moon landing missions, the Skylab space station, and the Space Shuttle. NASA supports the International Space Station and oversees the development of the Orion spacecraft and the Space Launch System for the crewed lunar Artemis program, Commercial Crew spacecraft, and the planned Lunar Gateway space station. The agency is also responsible for the Launch Services Program, which provides oversight of launch operations and countdown management f ...
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Greenland Ice Sheet
The Greenland ice sheet ( da, Grønlands indlandsis, kl, Sermersuaq) is a vast body of ice covering , roughly near 80% of the surface of Greenland. It is sometimes referred to as an ice cap, or under the term ''inland ice'', or its Danish equivalent, ''indlandsis''. An acronym, GIS, is frequently used in the scientific literature. It is the second largest ice body in the world, after the Antarctic ice sheet. The ice sheet is almost long in a north–south direction, and its greatest width is at a latitude of 77°N, near its northern margin. The average thickness is about and over at its thickest point. In addition to the large ice sheet, smaller ice caps (such as Maniitsoq and Flade Isblink) as well as glaciers, cover between around the periphery. The Greenland ice sheet is adversely affected by climate change. It is more vulnerable to climate change than the Antarctic ice sheet because of its position in the Arctic, where it is subject to the regional amplification o ...
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Jakobshavn Isbræ
Jakobshavn Glacier ( da, Jakobshavn Isbræ), also known as Ilulissat Glacier ( kl, Sermeq Kujalleq), is a large outlet glacier in West Greenland. It is located near the Greenlandic town of Ilulissat (colonial name in da, Jakobshavn) and ends at the sea in the Ilulissat Icefjord. Jakobshavn Glacier drains 6.5% of the Greenland ice sheet and produces around 10% of all Greenland icebergs. Some 35 billion tonnes of icebergs calve off and pass out of the fjord every year. Icebergs breaking from the glacier are often so large (up to 1 km in height) that they are too tall to float down the fjord and lie stuck on the bottom of its shallower areas, sometimes for years, until they are broken up by the force of the glacier and icebergs further up the fjord. Studied for over 250 years, the Jakobshavn Glacier has helped develop modern understanding of climate change and icecap glaciology. Ilulissat Icefjord ( kl, Ilulissat Kangerlua) was declared a UNESCO World Heritage Site in 2 ...
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Sea Level Rise
Globally, sea levels are rising due to human-caused climate change. Between 1901 and 2018, the globally averaged sea level rose by , or 1–2 mm per year on average.IPCC, 2019Summary for Policymakers InIPCC Special Report on the Ocean and Cryosphere in a Changing Climate .-O. Pörtner, D.C. Roberts, V. Masson-Delmotte, P. Zhai, M. Tignor, E. Poloczanska, K. Mintenbeck, A. Alegría, M.  Nicolai, A. Okem, J. Petzold, B. Rama, N.M. Weyer (eds.) Cambridge University Press, Cambridge, UK and New York, NY, USA. https://doi.org/10.1017/9781009157964.001. This rate is accelerating, with sea levels now rising by 3.7 mm per year. Climate scientists expect further acceleration during the 21st century. Climate change heats (and therefore expands) the ocean and melts land-based ice sheets and glaciers. Between 1993 and 2018, the thermal expansion of water contributed 42% to sea level rise; melting of temperate glaciers, 21%; Greenland, 15%; and Antarctica, 8%. Over the next 2 ...
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Retreat Of The Helheim Glacier, Greenland
Retreat or re-treat may refer to: Common uses * Retreat (spiritual), a time taken to reflect or meditate * Retreat (survivalism), a place of refuge for survivalists Military *Retreat (bugle call), a military signal for the end of day, known as "Sunset" in some countries *Retreat (military), a withdrawal of military forces Places Australia * Retreat, Tasmania, a locality in Australia Great Britain *Retreat, County Antrim, a small village in Northern Ireland * The Retreat, the London home of English textile designer, artist, writer and socialist William Morris, who renamed it Kelmscott House South Africa *Retreat, Cape Town United States * Retreat, Indiana * Retreat, Louisiana *Retreat (Port Tobacco, Maryland) * Retreat, New Jersey * Retreat, Texas *Retreat, Wisconsin Arts, entertainment, and media Films * ''Retreat'' (2011 film), a film starring Cillian Murphy, Jamie Bell, and Thandiwe Newton * ''Retreat'' (2013 film), a short film featuring Sophie Stone * ''The Retreat' ...
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Glacial Motion
Glacial motion is the motion of glaciers, which can be likened to rivers of ice. It has played an important role in sculpting many landscapes. Most lakes in the world occupy basins scoured out by glaciers. Glacial motion can be fast (up to , observed on Jakobshavn Isbræ in Greenland) or slow ( on small glaciers or in the center of ice sheets), but is typically around . Processes of motion Glacier motion occurs from four processes, all driven by gravity: basal sliding, glacial quakes generating fractional movements of large sections of ice, bed deformation, and internal deformation. * In the case of basal sliding, the entire glacier slides over its bed. This type of motion is enhanced if the bed is soft sediment, if the glacier bed is thawed and if meltwater is prevalent. * Bed deformation is thus usually limited to areas of sliding. Seasonal melt ponding and penetrating under glaciers shows seasonal acceleration and deceleration of ice flows affecting whole icesheets. * Some gl ...
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Midnight Sun
The midnight sun is a natural phenomenon that occurs in the summer months in places north of the Arctic Circle or south of the Antarctic Circle, when the Sun remains visible at the local midnight. When the midnight sun is seen in the Arctic, the Sun appears to move from left to right, but in Antarctica the equivalent apparent motion is from right to left. This occurs at latitudes from 65°44' to 90° north or south, and does not stop exactly at the Arctic Circle or the Antarctic Circle, due to refraction. The opposite phenomenon, polar night, occurs in winter, when the Sun stays below the horizon throughout the day. Details Around the summer solstice (approximately 21 June in the Northern Hemisphere and 21 December in the Southern Hemisphere), in certain areas the Sun does not set below the horizon within a 24-hour period. Geography Because there are no permanent human settlements south of the Antarctic Circle, apart from research stations, the countries and territo ...
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Trondheim
Trondheim ( , , ; sma, Tråante), historically Kaupangen, Nidaros and Trondhjem (), is a city and municipality in Trøndelag county, Norway. As of 2020, it had a population of 205,332, was the third most populous municipality in Norway, and was the fourth largest urban area. Trondheim lies on the south shore of Trondheim Fjord at the mouth of the River Nidelva. Among the major technology-oriented institutions headquartered in Trondheim are the Norwegian University of Science and Technology (NTNU), the Foundation for Scientific and Industrial Research (SINTEF), and St. Olavs University Hospital. The settlement was founded in 997 as a trading post, and it served as the capital of Norway during the Viking Age until 1217. From 1152 to 1537, the city was the seat of the Catholic Archdiocese of Nidaros; it then became, and has remained, the seat of the Lutheran Diocese of Nidaros, and the site of the Nidaros Cathedral. It was incorporated in 1838. The current municipalit ...
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