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Viana Do Castelo, Portugal
Viana do Castelo () is a municipality and seat of the district of Viana do Castelo in the Norte Region of Portugal. The population in 2011 was 88,725, in an area of 319.02 km². The urbanized area of the municipality, comprising the city, has a population of approximately 36,148 inhabitants, although the extended densely populated region reaches surrounding municipalities like Caminha and Ponte de Lima with a population above 150,000 inhabitants. It is located on the Portuguese Way path, an alternative path of the Camino de Santiago, and at the mouth of the Lima river. History Human settlement in the region of Viana began during the Mesolithic era, from discoveries and archaeological excavations. Even around the Roman occupation the area was settled along the Mount of Santa Luzia. The settlement of ''Viana da Foz do Lima'', which it was called when King Afonso III of Portugal issued a foral (''charter'') on 18 July 1258, was a formalization of the 1253 ''Viana'' that the ...
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Norte Region, Portugal
The North Region ( pt, Região do Norte ) or Northern Portugal is the most populous region in Portugal, ahead of Lisbon, and the third most extensive by area. The region has 3,576,205 inhabitants according to the 2017 census, and its area is with a density of 173 inhabitants per square kilometre. It is one of five regions of Mainland Portugal ( NUTS II subdivisions). Its main population center is the urban area of Porto, with about one million inhabitants; it includes a larger political metropolitan region with 1.8 million, and an urban-metropolitan agglomeration with 2.99 million inhabitants, including Porto and neighboring cities, such as Braga, Guimarães and Póvoa de Varzim. The Commission of Regional Coordination of the North (CCDR-N) is the agency that coordinates environmental policies, land-use planning, cities and the overall development of this region, supporting local governments and associations. Northern Portugal is a culturally varied region. It is a land of dense ...
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Maria II Of Portugal
, image = Queen Maria II by John Simpson.jpg , caption = Portrait by John Simpson, 1835 , succession = Queen of Portugal , reign = , predecessor = Pedro IV , successor = Miguel I , reg-type = Regents , regent = Infanta Isabel Maria Infante Miguel , reign1 = 26 May 1834 – , coronation1 = 20 September 1834 , cor-type1 = Acclamation , predecessor1 = Miguel I , successor1 = Pedro V , reg-type1 = Co-monarch , regent1 = Fernando II , regent2 = Pedro IV , spouse = , issue = , issue-link = #Marriages and issue , house = Braganza , father = Pedro I of Brazil and IV of Portugal , mother = Maria Leopoldina of Austria , birth_date = , birth_place = São Cristóvão, Rio de Janeiro, Brazil , death_date = , death_place = Necessidades, Lisbon, Portugal , burial_date = 19 November 1853 , burial_place = Pantheon of the House of Braganza , religion = Roman Catholicism ...
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Continental Portugal
Continental Portugal ( pt, Portugal continental, ) or mainland Portugal comprises the bulk of the Portuguese Republic, namely that part on the Iberian Peninsula and so in Continental Europe, having approximately 95% of the total population and 96.6% of the country's land. Mainland Portugal is therefore commonly called by residents of the Portuguese archipelagos of the Azores and Madeira the continent ( pt, o continente) in all respects including minor elements of combined governance from Lisbon, the country's capital. Before 1975, when the Portuguese territory also stretched to several now-independent states in Africa, the designation ''metropolis'' ( pt, metrópole) was also used. Context The designation ''mainland Portugal'' is used to differentiate the continental territory of Portugal from its insular territory. The latter comprises the archipelagos of Madeira and Azores in the Atlantic Ocean. The Azores and Madeira are also commonly referred to as the autonomous region ...
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Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. ...
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Thornthwaite Climate Classification
The Thornthwaite climate classification is a climate classification system created by American climatologist Charles Warren Thornthwaite in 1931 and modified in 1948. 1931 classification Precipitation effectiveness Thornthwaite initially divided climates based on five characteristic vegetations: Rainforest, forest, grassland, steppe and desert. One of the main factors for the local vegetation is precipitation, but most importantly, precipitation effectiveness, according to Thornthwaite. Thornthwaite based the effectiveness of precipitation on an index (the P/E index), which is the sum of the 12 monthly P/E ratios. The monthly P/E ratio can be calculated using the formula: P/E \text = \frac Temperature efficiency Similarly to precipitation effectiveness, Thornthwaite also developed a T/E index to represent thermal efficiency. Featuring six climate provinces: Tropical, mesothermal, microthermal, taiga, tundra and frost. The T-E index is the sum of the 12 monthly T-E ra ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Warm-summer Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 4 ...
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Darque
Darque is a civil parish In England, a civil parish is a type of administrative parish used for local government. It is a territorial designation which is the lowest tier of local government below districts and counties, or their combined form, the unitary authorit ... in the municipality of Viana do Castelo, Portugal. The population in 2011 was 7,817,Instituto Nacional de Estatística (INE)
Census 2011 results according to the 2013 administrative division of Portugal
in an area of 9.01 km2.


References

Freguesias of Viana do Castelo {{VianadoCastelo-geo-stub ...
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Chafé
Chafé is a civil parish in the municipality of Viana do Castelo, Portugal. The population in 2011 was 2,841,Instituto Nacional de Estatística (INE)
Census 2011 results according to the 2013 administrative division of Portugal
in an area of 7.85 km2. It is located near the coast, 7 km south of Viana do Castelo, Portugal, 59 km north of

Barroselas E Carvoeiro
Barroselas e Carvoeiro is a civil parish in the municipality of Viana do Castelo, Portugal. It was formed in 2013 by the merger of the former parishes Barroselas Barroselas is a former civil parish in the municipality of Viana do Castelo, Portugal. In 2013, the parish merged into the new parish Barroselas e Carvoeiro. On the 2001 census, Barroselas had a total population of 3,799. The total area is 7.47&n ... and Carvoeiro. The population in 2011 was 5,031,Instituto Nacional de Estatística (INE)
Census 2011 results according to the 2013 administrative division of Portugal
in an area of 18.68 km².


References

{{authority control
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Areosa
Areosa is a civil parish located in the municipality (''concelho'') of Viana do Castelo, in northern Portugal The North Region ( pt, Região do Norte ) or Northern Portugal is the most populous region in Portugal, ahead of Lisbon Region, Lisbon, and the third most extensive by area. The region has 3,576,205 inhabitants according to the 2017 census, and its .... The population in 2011 was 4,853,Instituto Nacional de Estatística (INE)
Census 2011 results according to the 2013 administrative division of Portugal
in an area of 14.11 km².


References

{{authority control Freguesias of Viana do Castelo ...
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