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Funäsdalen
Funäsdalen is a village located in Härjedalen Municipality, Jämtland County, Sweden with 890 inhabitants in 2010. Funäsdalen is situated in western Härjedalen near the Norwegian border. Funäsdalen is the site of Härjedalens Fjällmuseum which provides exhibits relating to mountain farming and Sami culture. Funäsdalen has long been a gathering place for Sámi people. The museum buildings were designed by architect Jörgen Grönvik. Inside the museum there is a permanent exhibition of work by sculptor Emil Näsvall (1908-1965). Adjacent to the museum is Fornminnesparken. This open-air museum provides a display of historic buildings dating from the 16th century to the 19th century. Funäsdalen Church (''Funäsdalens kyrka'') was built between 1926 and 1928 after drawings by the architects Curt Björklund (1895-1958) and Martin Westerberg (1892-1963). The building has a frame of brick. The altarpiece is attributed to the 17th century Dutch artist Henricus Noêll. The chur ...
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Funäsdalen Church
Funäsdalen is a village located in Härjedalen Municipality, Jämtland County, Sweden with 890 inhabitants in 2010. Funäsdalen is situated in western Härjedalen near the Norwegian border. Funäsdalen is the site of Härjedalens Fjällmuseum which provides exhibits relating to mountain farming and Sami culture. Funäsdalen has long been a gathering place for Sámi people. The museum buildings were designed by architect Jörgen Grönvik. Inside the museum there is a permanent exhibition of work by sculptor Emil Näsvall (1908-1965). Adjacent to the museum is Fornminnesparken. This open-air museum provides a display of historic buildings dating from the 16th century to the 19th century. Funäsdalen Church (''Funäsdalens kyrka'') was built between 1926 and 1928 after drawings by the architects Curt Björklund (1895-1958) and Martin Westerberg (1892-1963). The building has a frame of brick. The altarpiece is attributed to the 17th century Dutch artist Henricus Noêll. The churc ...
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Funäsfjällen
Funäsfjällen is an alpine ski area in Sweden. Funäsfjällen consists of the resorts Funäsdalen, Ramundberget, Tänndalen, Bruksvallarna, Ljusnedal, Messlingen (Mittådalen), Tännäs and Fjällnäs. Alpine skiing There are five resorts with alpine skiing: Funäsdalsberget, Ramundberget, Tänndalen (with Tänndalsvallen), Tännäskröket and Kappruet. Cross-country skiing Nordic Ski Center, one of the largest cross-country skiing systems in the world (300 km groomed trails, 450 km marked trails), is situated in Funäsfjällen. In Bruksvallarna there are also groomed trails with snowmaking Snowmaking is the production of snow by forcing water and pressurized air through a "snow gun", also known as a "snow cannon". Snowmaking is mainly used at ski resorts to supplement natural snow. This allows ski resorts to improve the reliabilit .... References *''The information in this article is based on that in its Swedish equivalent''. External links F ...
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Härjedalen Municipality
Härjedalen Municipality (, , no, Herjedalen kommune) is a municipality in Jämtland County in northern Sweden. Its seat is located in Sveg. The municipality roughly, but not exactly, corresponds with the traditional province Härjedalen. The municipality was created in 1974 and is one of two in Sweden with the name of a province (Gotland Municipality is the other). It consists of nine original local government entities (as of 1863). Geography With a total area of , it is Sweden's fifth largest. However, it is largely wilderness, and the municipality is sparsely inhabited. For comparison, the municipality covers as much territory as Uppsala County and Stockholm County combined, but those two counties have over 2,000,000 inhabitants. Localities There are eight localities (or urban areas) in Härjedalen Municipality: The municipal seat in bold Riksdag This table lists the national results since the 1972 Swedish municipality reform. The results of the Sweden Democrats ...
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Härjedalen
Härjedalen (; no, Herjådalen or ) is a historical province (''landskap'') in the centre of Sweden. It borders the Norwegian county of Trøndelag as well as the provinces of Dalarna, Hälsingland, Medelpad, and Jämtland. The province originally belonged to Norway, but was ceded to Sweden in the Treaty of Brömsebro, 1645. The province forms the bulk of Härjedalen Municipality, of which the village of Sveg is the seat. Etymology The name ''Härjedalen'', from Old West Norse , literally means the "Valley of the Härje river". A Latinized transliteration is Herdalia, although that name is hardly encountered in the English language today. More prominent are derivations such as ''Herjedalen'' or ''Haerjedalen''. The more prosaic explanation of the name says that the word ''her'' or ''har'' just means "mound of stones" and refers to stones in the river . History Jämtland and Härjedalen were provinces of Denmark-Norway until the mid-17th century. After the Treaty o ...
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Country
A country is a distinct part of the world, such as a state, nation, or other political entity. It may be a sovereign state or make up one part of a larger state. For example, the country of Japan is an independent, sovereign state, while the country of Wales is a component of a multi-part sovereign state, the United Kingdom. A country may be a historically sovereign area (such as Korea), a currently sovereign territory with a unified government (such as Senegal), or a non-sovereign geographic region associated with certain distinct political, ethnic, or cultural characteristics (such as the Basque Country). The definition and usage of the word "country" is flexible and has changed over time. '' The Economist'' wrote in 2010 that "any attempt to find a clear definition of a country soon runs into a thicket of exceptions and anomalies." Most sovereign states, but not all countries, are members of the United Nations. The largest country by area is Russia, while the ...
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Swedish Meteorological And Hydrological Institute
The Swedish Meteorological and Hydrological Institute ( sv, Sveriges meteorologiska och hydrologiska institut, abbreviated SMHI) is a Government agency in Sweden and operates under the Ministry of the Environment. SMHI has expertise within the areas of meteorology, hydrology and oceanography, and has extensive service and business operations within these areas. History In 1873, ''Statens Meteorologiska Centralanstalt'' was founded, an autonomous part of the Royal Swedish Academy of Sciences, but the first meteorological observations began on July 1, 1874. It was not until 1880 that the first forecasts were issued. The latter will be broadcast on Stockholm radio from 19 February 1924.. In 1908, the Hydrographic Office (''Hydrografiska byrån'', HB) was created. Its task is to scientifically map Sweden's freshwater and collaborate with the weather service in taking certain weather observations such as precipitation and snow cover. In 1919, the two services merged and became t ...
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Ljusnedal
Ljusnedal () is a village and parish in Härjedalen Municipality in Jämtland County, Sweden. Ljusnedal Church (''Ljusnedals kyrka'') is a wooden church built in 1796. The interior is characterized by renovation conducted during 1902. The altarpiece is painted by the artist Sven Linnborg (1857-1932). The church is associated with the Tännäs-Ljusnedal parish in the Diocese of Härnösand The Diocese of Härnösand ( sv, Härnösands stift) is a division in the Church of Sweden in Västernorrland County. The Cathedral is located at Trädgårdsgatan in Härnösand. History The diocese was established in 1647. In 1904, the diocese o .... Climate References Populated places in Härjedalen Municipality Härjedalen {{Jämtland-geo-stub ...
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Røros
Røros ( sma, Plaassja, ) is a municipality in Trøndelag county, Norway. The administrative centre of the municipality is the town of Røros. Some of the villages in Røros include Brekken, Glåmos, Feragen, Galåa, and Hitterdalen. The mining town of Røros (the administrative centre of the municipality) is sometimes called ''Bergstaden'' which means "mountain town" due to its historical notoriety for copper mining. It is one of two towns in Norway that were historically designated "mining towns", along with the "silver-town" of Kongsberg. The modern-day inhabitants of Røros still work and live in the characteristic 17th and 18th century buildings which led to its designation as a UNESCO World Heritage Site in 1980. Røros has about 80 wooden houses, most of them standing around courtyards. Many retain their dark pitch-log facades, giving the town a medieval appearance. The municipality is the 39th largest by area out of the 356 municipalities in Norway. Røros is the 1 ...
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Frost
Frost is a thin layer of ice on a solid surface, which forms from water vapor in an above- freezing atmosphere coming in contact with a solid surface whose temperature is below freezing, and resulting in a phase change from water vapor (a gas) to ice (a solid) as the water vapor reaches the freezing point. In temperate climates, it most commonly appears on surfaces near the ground as fragile white crystals; in cold climates, it occurs in a greater variety of forms. The propagation of crystal formation occurs by the process of nucleation. The ice crystals of frost form as the result of fractal process development. The depth of frost crystals varies depending on the amount of time they have been accumulating, and the concentration of the water vapor (humidity). Frost crystals may be invisible (black), clear ( translucent), or white; if a mass of frost crystals scatters light in all directions, the coating of frost appears white. Types of frost include crystalline frost ( ...
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Inversion (meteorology)
In meteorology, an inversion is a deviation from the normal change of an atmospheric property with altitude. It almost always refers to an inversion of the air temperature lapse rate, in which case it is called a temperature inversion. Normally, air temperature decreases with an increase in altitude, but during an inversion warmer air is held above cooler air. An inversion traps air pollution, such as smog, close to the ground. An inversion can also suppress convection by acting as a "cap". If this cap is broken for any of several reasons, convection of any moisture present can then erupt into violent thunderstorms. Temperature inversion can notoriously result in freezing rain in cold climates. Normal atmospheric conditions Usually, within the lower atmosphere (the troposphere) the air near the surface of the Earth is warmer than the air above it, largely because the atmosphere is heated from below as solar radiation warms the Earth's surface, which in turn then warms ...
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Storlien
Storlien is a village and ski resort located in Åre municipality in Jämtland, Sweden, two kilometres from the Swedish-Norwegian border. The primary bases of the settlement are tourism and outdoor life – alpine skiing, snowmobiling, cross-country skiing, hunting, fishing and hiking. During the 2000s, retail sales to customers from Norway become important, and most of the tourists in Storlien are Norwegians. The Swedish royal family has a house in Storlien, where they usually celebrate Easter and the New Year. There was also previously a sanitarium. Storlien was formerly the centre of winter activities for , now , an organisation that promotes outdoor leisure, and played a major role in developing downhill skiing in Sweden. Storlien has, among other services, a hotel called ('Storlien Mountain Lodge') and a holiday village called . A large part of the village is owned by the Lars Nilsson estate, a real estate agent. The hotel was formerly the largest in the country. ...
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Diurnal Temperature Variation
In meteorology, diurnal temperature variation is the variation between a high air temperature and a low temperature that occurs during the same day. Temperature lag Temperature lag is an important factor in diurnal temperature variation: peak daily temperature generally occurs ''after'' noon, as air keeps net absorbing heat even after noon, and similarly minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon is seasonal lag. As solar energy strikes the Earth's surface each morning, a shallow layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by from just above the ground to waist height. Incoming solar radiation exceeds outgoing heat energy for many hours af ...
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