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59-473: 54°38′13″N 5°40′39″W  /  54.63686°N 5.67759°W  / 54.63686; -5.67759 This article related to the geography of County Armagh , Northern Ireland is a stub . You can help Misplaced Pages by expanding it . This article about a specific United Kingdom geological feature is a stub . You can help Misplaced Pages by expanding it . County Armagh County Armagh ( Irish : Contae Ard Mhacha [ɑːɾˠd̪ˠ ˈwaxə] )

118-567: A Lieutenancy area – the county retains a lord lieutenant who acts as representative of the British Monarch in the county. Currently the county is covered for local government purposes by three district councils , namely Armagh, Banbridge and Craigavon Borough Council , approximately the western third of Newry, Mourne and Down Council and a part of Mid Ulster District Council , centred around Peatlands Park . Armagh ceased to serve as an electoral constituency in 1983 but remains

177-897: A few highland areas of Tasmania , and the Australian and Southern Alps . This type of climate is even found in very remote parts of the New Guinea Highlands . The classification used for this regime is Cfc. Temperatures above 30 °C (86 °F) and below −20 °C (−4 °F) are rare. In the most marine areas under this regime, temperatures above 20 °C (68 °F) are extreme weather events, even during summer. Small areas in Yunnan, Sichuan ; parts of Bolivia and Peru ; and parts of Mount Kilimanjaro in Tanzania have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This

236-407: A majority of the population from a Catholic background, according to the 2011 census . During the 17th and 18th centuries, County Armagh was a major center of guerrilla warfare , cattle raiding , and brigandage by local Rapparees ; including Count Redmond O'Hanlon , Cormacke Raver O'Murphy, and Séamus Mór Mac Murchaidh . The southern part of the county has been a stronghold of support for

295-514: A product and reflection of the cool ocean adjacent to them. In the autumn, winter, and early spring, when the polar jet stream is most active, the frequent passing of marine weather systems creates the frequent fog, cloudy skies, and light drizzle often associated with oceanic climates. They are typically found poleward of Mediterranean climates , except in Australia where they are poleward of both such climates and humid subtropical climates due to

354-595: A reading of 31.4 °C was registered at Armagh Observatory's weather station. Ancient Armagh was the territory of the Ulaid (also known as Voluntii, Ultonians, Ulidians, Ulstermen) before the fourth century AD. It was ruled by the Red Branch , whose capital was Emain Macha (or Navan Fort) near Armagh. The site, and subsequently the city, were named after the goddess Macha . The Red Branch play an important role in

413-561: A relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates , represented as Cwb or Cfb , and subpolar oceanic or cold subtropical highland climates , represented as Cfc or Cwc . Subtropical highland climates occur in some mountainous parts of

472-612: A result of their location, these regions tend to be on the cool end of oceanic climates, approaching polar regions . Snowfall tends to be more common here than in other oceanic climates. Subpolar oceanic climates are less prone to temperature extremes than subarctic climates or continental climates , featuring milder winters than these climates. Subpolar oceanic climates feature only one to three months of average monthly temperatures of at least 10 °C (50 °F). As with oceanic climates, none of its average monthly temperatures fall below -3.0 °C (26.6 °F) or 0 °C depending on

531-750: A strict air-mass sense, not oceanic: they are affected by southerlies directly from the Mediterranean, and polar intrusions from Siberia. Yet their position near the Black Sea makes them too wet in summer to be Mediterranean , too mild during winter to be humid continental , and not hot enough in summer to be humid subtropical ; therefore Köppen classifies them as oceanic. Despite their anomalous position, however, their temperatures, around 4–5 °C (39–41 °F) in winter and 20–22 °C (68–72 °F) in summer, are not wholly atypical for European oceanic climates. Some Eastern European regions such as

590-425: Is a climate variety, often grouped together with oceanic climates, which exists in some mountainous or elevated portions of the world in either the subtropics or tropics. Despite the latitude, the higher elevations of these regions mean that the climate shares characteristics with oceanic climates. Subtropical highland climates with uniform rainfall ( Cfb ) usually have rainfall spread relatively evenly throughout

649-687: Is a possible railway re-opening from Portadown railway station to Armagh railway station in the future. Government Minister for the Department for Regional Development , Danny Kennedy MLA indicates railway restoration plans of the line from Portadown to Armagh . Ulsterbus provides the most extensive public transport system within the county, including frequent bus transfers daily from most towns to Belfast. Northern Ireland Railways / Iarnród Éireann 's Enterprise service provides connections to Dublin in little over an hour and Belfast in little over forty minutes, several times daily. County Armagh

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708-463: Is below 18 °C (64 °F). Without their elevation, many of these regions would likely feature either humid subtropical or tropical climates. This type of climate exists in parts of east, south and southeastern Africa , interior southern Africa and elevated portions of eastern Africa as far north as Ethiopia and of western Africa (west region of Cameroon) up to the southwestern Angola highlands also share this climate type. It also exists in

767-571: Is climatically Mediterranean , some parts of Southern Europe also have oceanic climates. However, these instances of the climate are highly variable, and often somewhat anomalous. The north coast of Spain , the western Azores off the coast of Portugal are too wet in summer to be Mediterranean, and too mild in summer to be humid subtropical , though they often have winter means above 9 °C (48 °F), unusual for European oceanic climates. Another anomalous case can be found in northwestern Turkey, including northern Istanbul . These places are, in

826-617: Is found in parts of coastal Iceland , the Faroe Islands , upland/mountainous parts of Scotland and Northern England , northwestern coastal areas of Norway (most of Lofoten , Vesterålen , warmest part of Tromsø reaching to 71°N on some islands), uplands/highlands in western Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle , the southwest of Argentina and Chile , and

885-735: Is in South Africa from Mossel Bay on the Western Cape coast to Plettenberg Bay (the Garden Route ), with additional pockets of this climate inland of the Eastern Cape and KwaZulu-Natal coast. It is usually warm most of the year with no pronounced rainy season, but slightly more rain in autumn and spring. The Tristan da Cunha archipelago in the South Atlantic also has an oceanic climate. Although oceanic climate

944-452: Is more frequent and commonplace in the subpolar oceanic climates due to the colder weather in those locations. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature. In the Köppen climate classification , oceanic climates have a mean temperature of 0 °C (32 °F) or higher (or −3 °C (27 °F) or higher) in

1003-550: Is named after its county town , Armagh , which derives from the Irish Ard Mhacha , meaning "Macha's height". Macha was a sovereignty goddess in Irish mythology and is said to have been buried on a wooded hill around which the town of Armagh grew. County Armagh is colloquially known as the "Orchard County" because of its many apple orchards. The county covers an area of 1,327 km (512 sq mi), making it

1062-539: Is not infrequent in the months November to February. Snow rarely lies for longer than a few hours even in the elevated south-east of the county. Summers are mild and wet and although with sunshine often interspersed with showers, daylight lasts for almost 18 hours during high-summer. On 22 July 2021 the record for highest outside air temperature ever measured in Northern Ireland was set in Armagh City when

1121-521: Is one of the six counties of Northern Ireland and one of the traditional thirty-two counties of Ireland . It is located in the province of Ulster and adjoins the southern shore of Lough Neagh . It borders the Northern Irish counties of Tyrone to the west and Down to the east. The county borders Louth and Monaghan to the south and southwest, which are in the Republic of Ireland . It

1180-715: Is rare in Asia, subtropical highland climates and cold subtropical highland climates can be found in parts of Southwestern China , and the Himalayan regions of the northern Indian subcontinent . The oceanic climate is prevalent in the more southerly parts of Oceania . A mild maritime climate is in existence in New Zealand. In Australia, the climate is found in Tasmania , southern half of Victoria and southeastern New South Wales (southwards from Wollongong ). Some parts of

1239-682: Is traversed by the Ulster Canal and the Newry Canal which are not fully open to navigation. In association football, the NIFL Premiership , which operates as the top division, has one team in the county: Glenavon , with Portadown , Annagh United , Armagh City , Dollingstown , Loughgall and Lurgan Celtic competing in the NIFL Championship , which operates as levels two and three. The Armagh County Board of

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1298-766: Is traversed by two major highways – the M1 linking Belfast to Dungannon crosses the north of the county whilst the A1/N1 from Belfast to Dublin runs in the far south east. Other major roads in the county include the A3 and A29 . Armagh once had a well-developed railway network with connections to, among others, Armagh City, Culloville , Goraghwood , Markethill , Vernersbridge , Tynan (see History of rail transport in Ireland ) but today only Newry (Bessbrook) , Portadown , Poyntzpass , Scarva , and Lurgan are served by rail. There

1357-629: The Gaelic Athletic Association or Armagh GAA organises Gaelic games in the county. 54°21′00″N 6°39′17″W  /  54.3499°N 6.6546°W  / 54.3499; -6.6546 Oceanic climate An oceanic climate , also known as a marine climate or maritime climate , is the temperate climate sub-type in Köppen classification represented as Cfb , typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with

1416-705: The Grand Banks of Newfoundland , is thought to greatly modify the climate of northwest Europe. As a result of the North Atlantic Current , west coast areas located in high latitudes like Ireland, the UK, and Norway have much milder winters (for their latitude) than would otherwise be the case. The lowland attributes of western Europe also help drive marine air masses into continental areas, enabling cities such as Dresden , Prague , and Vienna to have maritime climates in spite of being located well inland from

1475-846: The Guiana Shield , The highest elevations of the Brazilian Highlands , and due to variations in rainfall and temperature patterns in some places of the Tropical Andes in Bolivia, Perú, Ecuador, Colombia and Venezuela. Most of Yunnan and mountainous areas across Southeast Asia , parts of the Himalayas , parts of Sri Lanka , and parts of the Hawaiian Islands of Maui and Hawaii . In the Caribbean , only

1534-749: The IRA , earning it the nickname "Bandit Country". South Armagh is predominantly nationalist , with much of the population being opposed to any form of British presence, especially that of a military nature. The most prominent opposition to British rule was the Provisional IRA South Armagh Brigade . On 10 March 2009, the CIRA claimed responsibility for the fatal shooting of a PSNI officer in Craigavon , County Armagh—the first police fatality in Northern Ireland since 1998. The officer

1593-793: The Northern Hemisphere include parts of coastal Iceland , the coast of Norway north of Bodø , the Scottish Highlands , the mountains of Vancouver Island , and Haida Gwaii in Canada . In the Southern Hemisphere examples include extreme southern Chile and Argentina (such as Punta Arenas and Ushuaia ), the Tasmanian Central Highlands , and parts of New Zealand . Oceanic climates are not necessarily found in coastal locations on

1652-714: The Ulster Cycle , as well as the Cattle Raid of Cooley . However, they were eventually driven out of the area by the Three Collas, who invaded in the 4th century and held power until the 12th. The Clan Colla ruled the area known as Airghialla or Oriel for these 800 years. The chief Irish clans of the county were descendants of the Collas, the O'Hanlons and Mac Cana , and the Uí Néill , the O'Neills of Fews. Armagh

1711-425: The subtropics or tropics , some of which have monsoon influence, while their cold variants and subpolar oceanic climates occur near polar or tundra regions. 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

1770-893: The subtropics . It exists in both hemispheres between 35° and 60°: at low altitudes between Mediterranean , humid continental , and subarctic climates. Western sea breezes ease temperatures and moderates the winter, especially if warm sea currents are present, and cause cloudy weather to predominate. Precipitation is constant, especially in colder months, when temperatures are warmer than elsewhere at comparable latitudes. This climate can occur farther inland if no mountain ranges are present or nearby. As this climate causes sufficient moisture year-round without permitting deep snow cover, vegetation typically prospers in this climate. Deciduous trees are predominant in this climate region. However, conifers such as spruce , pine , and cedar are also common in few areas, and fruits such as apples , pears , and grapes can often be cultivated here. In

1829-1049: The 2021 Census, County Armagh recorded a population of 194,394. It is one of four counties in Northern Ireland with a Catholic majority, with 58% of the population coming from a Catholic community background. Around 10% of the population was born outside the United Kingdom and Ireland, mainly immigrants from the European Union and concentrated in the Craigavon urban area ( Lurgan , Portadown and Craigavon ). (population of 18,000 or more and under 75,000 at 2001 Census) (population of 10,000 or more and under 18,000 at 2001 Census) (population of 4,500 or more and under 10,000 at 2001 Census) (population of 2,250 or more and under 4,500 at 2001 Census) (population of 1,000 or more and under 2,250 at 2001 Census) (population of fewer than 1,000 at 2001 Census) Baronies Parishes Townlands County Armagh

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1888-424: The aforementioned parallels; however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream , which moves in a west to east direction across the middle latitudes, advances low pressure systems, storms, and fronts. In coastal areas of the higher middle latitudes (45–60° latitude), the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are

1947-455: The capital of the Ulaid kings (who give their name to Ulster ) and is believed to be the high place from which the county takes its name. From its highest point at Slieve Gullion , in the south of the county, Armagh's land falls away from its rugged south with Carrigatuke, Lislea and Camlough mountains, to rolling drumlin country in the middle and west of the county and finally flatlands in

2006-617: The city of Newry , notable towns in the county include Lurgan , Portadown and Craigavon . The name Armagh derives from the Irish Ard Macha , meaning Macha's height / Macha's high place . Macha is a mythological figure who is mentioned in The Book of the Taking of Ireland . Macha is also said to have been responsible for the construction of the hill site of Emain Macha (now Navan Fort near Armagh City ) to serve as

2065-570: The coldest month, compared to continental climates where the coldest month has a mean temperature of below 0 °C (32 °F) (or −3 °C (27 °F)) in the coldest month. Summers are warm but not hot, with the warmest month having a mean temperature below 22 °C (72 °F). Poleward of the latter is a subtype of it, the subpolar oceanic climate (Köppen Cfc ), with long but relatively mild (for their latitude) winters, and cool and short summers with average temperatures of at least 10 °C (50 °F) for one to three months. Examples in

2124-712: The core of the Newry and Armagh constituency represented at Westminster and the Newry and Armagh constituency represented in the Northern Ireland Assembly . County Armagh also remains as a district for legal and property purposes; however, its baronies no longer have any administrative use. The -XZ suffix is currently used on vehicle registration plates for vehicles registered in County Armagh. Other suffixes have been -IB and -LZ. These marks are followed by up to four numbers, e.g., JLZ 6789 As of

2183-571: The county's northern boundary. There are also a number of uninhabited islands in the county's section of Lough Neagh: Coney Island Flat, Croaghan Flat, Padian, Phil Roe's Flat and the Shallow Flat. Despite lying in the east of Ireland, Armagh enjoys an oceanic climate strongly influenced by the Gulf Stream with damp mild winters, and temperate, wet summers. Overall temperatures rarely drop below freezing during daylight hours, though frost

2242-551: The east, and (in some locations) summers become hotter. The line between oceanic Europe and Mediterranean Europe normally runs west to east and is related to changes in precipitation patterns and differences to seasonal temperatures; although intrusions of polar air, remnants of marine air-masses, and higher summer precipitation can create oceanic climates in Eastern Europe and transcontinental regions as far south as 40°N. The oceanic climate exists in an arc spreading across

2301-635: The exposed areas of the High Atlas , some mountainous areas across southern Europe , mountainous sections of North America , including parts of the southern Appalachians and the Central America Volcanic Arc . In South America , it can be found mainly in temperate mountainous areas in the Tropical Andes , Venezuelan Coastal Range , the highest elevations of Serra do Mar in Southeastern Brazil , and tepuis of

2360-817: The hottest month, the average temperature is below 22 °C (72 °F), and at least four months feature average temperatures higher than 10 °C (50 °F). The average temperature of the coldest month must not be colder than −3–0 °C (27–32 °F), or the climate will be classified as continental. The average temperature variations in the year are between 10–15 °C (50–59 °F), with average annual temperatures between 6–13 °C (43–55 °F). Rain values can vary from 50–500 cm (20–197 in), depending on whether mountains cause orographic precipitation . Frontal cyclones can be common in marine west coast regions, with some areas experiencing more than 150 rainy days annually, but strong storms are rare. Cfb climates are predominant in most of Europe except

2419-765: The immediate west and northwest in transition for humid continental , the remainder of Cape Cod ) and northeastern Georgia both in the eastern United States . It is also found in the highest portions of the Brazilian state of Bahia and Roraima (in transition or strongly influenced for Cwb ), Brønnøy Municipality in Nordland at 65.28 °N ( Norway north-central coast), the provinces of Sabah (northeastern Malaysia ), and Baluchistan , Pakistan . Although there are more or less rare places associated with relatively isolated mountainous regions (e.g., North Oceania islands and China ). The subtropical highland climate

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2478-561: The isotherm used. Typically, these areas in the warmest month experience daytime maximum temperatures below 17 °C (63 °F), while the coldest month features highs slightly above freezing and lows near or just below freezing while keeping the average warm enough. It typically carries a Cfc designation, though very small areas in Argentina and Chile have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This variant of an oceanic climate

2537-542: The north of Croatia and Serbia and some parts of the Czech Republic , also have oceanic climates; these are generally near the boundary for being humid continental . The line between oceanic and continental climates in Europe runs in a generally north to south direction. For example, western Germany is more impacted by milder Atlantic air masses than eastern Germany. Thus, winters across Europe become colder to

2596-426: The north where rolling flats and small hills reach sea level at Lough Neagh . County Armagh's boundary with Louth is marked by the rugged Ring of Gullion rising in the south of the county whilst much of its boundary with counties Monaghan and Down goes unnoticed with seamless continuance of drumlins and small lakes. The River Blackwater marks the border with County Tyrone and Lough Neagh otherwise marks out

2655-818: The northeast, as global temperatures became warmer towards late 20th and early 21st century. They are the main climate type in New Zealand and the Australian states of Tasmania , Victoria , and southeastern New South Wales (starting from the Illawarra region). In North America, they are found mainly in Vancouver Island and neighbouring parts of British Columbia , as well as many coastal areas of southeast Alaska . There are pockets of this iteration of Cfb climates in South American countries, mostly in regions of southern Chile and Argentina, parts of

2714-655: The northeastern coast of Honshu , such as Mutsu, Aomori in Japan, feature this climate, which is rare in Asia due to the lack of a west coast in the middle latitudes. Île Amsterdam and Île Saint-Paul , both part of the French Southern and Antarctic Lands , are located in the subtropics and have an oceanic climate (akin to Tristan da Cunha; see above). Temperate oceanic climates, also known as "marine mild winter" climates or simply oceanic climates, are found either at middle latitudes . They are often found on or near

2773-620: The northwestern coast of North America from the Alaskan panhandle to northern Washington . In addition, some east coast areas such as Block Island , Cape Cod , Martha's Vineyard , and Nantucket have a similar climate. And in the highlands of Central and South America with the variant Cfb. An extensive area of oceanic climates distinguishes the coastal regions of southern Chile and extends into bordering Argentina . The only noteworthy area of maritime climate at or near sea-level within Africa

2832-763: The ocean. Oceanic climates in Europe occupy a large stretch of land, from Norway 's Atlantic coast, Ireland and the United Kingdom and southeast to some parts of Turkey . Western Europe is almost exclusively oceanic between 45°N to 54.913°N; including most of France (away from the Mediterranean), nearly all of Belgium , the Netherlands , Austria , most of Luxembourg , most of Denmark , western Germany , northwestern Switzerland , south coast and western areas of Norway north to Skrova and extreme southern Sweden . While most of Southern Europe

2891-842: The peaks in the highest mountain ranges have this climate (including the Blue Mountains in Jamaica and Cerro Maravilla in Puerto Rico ), with only Hispaniola 's Cordillera Central and Chaîne de la Selle having significant urban settlements under this climate zone, such as cities like Kenscoff in Haiti and Constanza in the Dominican Republic . Areas with subpolar oceanic climates feature an oceanic climate but are usually located closer to polar regions, with long but relatively mild winters and short, cool summers. As

2950-421: The provinces of Chubut , Santa Cruz , and southeast Buenos Aires province in Argentina. In Western Asia , the climate can be found on the Black Sea coast of northern Turkey and Georgia , often transitional to humid subtropical . While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa . The climate subtype can also be found in Nantucket , Massachusetts (in

3009-419: The regions, but are more common in subtropical highland climates where these air masses meet more frequently due to the influence of hotter weather in the subtropics or tropics, especially in monsoon-influenced climates. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. Most oceanic climate zones, however, experience at least one snowfall per year. Snowfall

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3068-436: The shape of the continent. Only in Europe do they penetrate far inland, where they eventually transition into warm-summer humid continental climates ; in other continents, they are blocked by a large mountain range or limited by nearby oceans. The North Atlantic Gulf Stream , a tropical oceanic current that passes north of the Caribbean and up the East Coast of the United States to North Carolina , then heads east-northeast to

3127-418: The smallest of Northern Ireland's six counties by size and the sixth-smallest county on the island of Ireland. With a population of 194,394 as of the 2021 census , it is the fourth-most populous county in both Northern Ireland and Ulster. It is the 10th most populous of Ireland's 32 traditional counties, as well as the fifth-most densely populated. In addition to the city of Armagh and the western portion of

3186-448: The tropics, a subtropical highland climate typically features mild weather year-round. Temperatures there remain relatively constant throughout the year and snowfall is seldom seen due to warmer winters than most oceanic climates. Areas with this climate feature monthly averages below 22 °C (72 °F) but above either 0 °C (32 °F) or −3 °C (27 °F) depending on isotherm used. At least one month's average temperature

3245-414: The west coast of continents; hence another name for Cfb, "marine west coast climates". In addition to moderate temperatures year-round, one of the characteristics is the absence of a dry season. Except for Europe , this type of climate is confined to narrow bands of territory, largely in mid or high latitudes, although it can appear in elevated areas of continental terrain in low latitudes, e.g. plateaus in

3304-571: The year, similar to other oceanic climates, but unlike these climates, they have a high diurnal temperature variation and low humidity, owing to their inland location and relatively high elevation. Subtropical highland climates with monsoon influence ( Cwb ) have distinctive wet summers and dry winters . In locations outside the tropics, other than the drying trend in the winter, subtropical highland climates tend to be essentially identical to an oceanic climate, with mild summers and noticeably cooler winters, plus, in some instances, some snowfall. In

3363-491: Was divided into several baronies: Armagh was held by the O'Rogans, Lower Fews was held by O'Neill of the Fews, and Upper Fews were under governance of the O'Larkins, who were later displaced by the MacCanns. Oneilland East was the territory of the O'Garveys, who were also displaced by the MacCanns. Oneilland West, like Oneilland East, was once O'Neill territory, until it was then held by the MacCanns, who were Lords of Clanbrassil. Upper and Lower Orior were O'Hanlon territory. Tiranny

3422-506: Was fatally shot by a sniper as he and a colleague investigated "suspicious activity" at a house nearby when a window was smashed by youths causing the occupant to phone the police. The PSNI officers responded to the emergency call, giving a CIRA sniper the chance to shoot and kill officer Stephen Carroll. The county was administered by Armagh County Council from 1899 until the abolition of county councils in Northern Ireland in 1973. County Armagh remains officially used for purposes such as

3481-415: Was ruled by Ronaghan. Miscellaneous tracts of land were ruled by O'Kelaghan. The area around the base of Slieve Gullion near Newry also became home to a large number of the Clan McGuinness as they were dispossessed of hereditary lands held in the County Down . St. Patrick is considered the first bishop of the Diocese of Armagh. County Armagh is presently one of four counties of Northern Ireland to have

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