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58-504: In the village of Bergkirchen, which belongs to Bad Oeynhausen, a wellspring sanctuary existed in pre-Christian (Saxon) times at the local crossing of the Wiehengebirge , which was replaced in the 9th century by a church. Today's church is a subsequent building. On the church and the downhill-situated Widukind spring plates explain this further. A few metres from the church a 13th-century timbered homestead can still be found. In 753 Pepin

116-749: A hill range in North Rhine-Westphalia and Lower Saxony in Germany . The hills run from west to east like a long finger away from the main upland area of the Lower Saxon Hills , beginning at the Weser River near Minden and terminating in the vicinity of Osnabrück . It is the northernmost of the German Central Upland ranges extending into the Northern Lowlands . Their highest hill is

174-464: A capacity of 6000 L/min and a total height of up to 40 m it is the world's highest carbonated thermal salt spring and de facto the town's landmark. Under Nazi Germany , Bad Oeynhausen hosted a synod of the Confessing Church , as well as the home congregation to Jakob Emil Karl Koch, a leading member. The World War II tank factory of the town was bombed on 30 March 1945. Post-war, the town hosted

232-873: 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

290-529: A height of 99 metre, but 2.5 km further west it reaches the level of the surrounding countryside. The waterways of the Mittelland Canal and Osnabrück Canal running away to the south appear to mark the end of the hill range, but west of these canals is the 82-metre-high Larberger Egge which forms the westernmost cornerstone of the Wiehen Hills, rising just 2  km northeast of the boundary with

348-509: 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

406-612: 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

464-738: 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

522-425: 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

580-463: 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

638-571: 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

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696-594: 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

754-704: 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

812-448: 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

870-695: 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

928-752: The Control Commission for Germany – British Element (CCG/BE) , the military government for the British Zone of Occupation and served as the British Army of the Rhine headquarters. The town was returned to local control in 1954 and spa activities resumed. In 1973, the seven surrounding municipalities Wulferdingsen, Volmerdingsen, Werste, Eidinghaisen, Dehme, Rehme and Lohe of the former "Amt Rehme" were merged with Bad Oeynhausen into one commune. The "State-owned Spa Bad Oeynhausen" ( German : Staatsbad ), property of

986-686: 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

1044-800: 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

1102-752: 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

1160-549: The Ruhr University Hospitals , is a world-leading institution for the treatment of cardiac, circulatory and metabolic diseases. Just outside the city lies the Klinik Bad Oexen , a rehabilitation center for cancer patients. Bad Oeynhausen is twinned with: Wiehengebirge The Wiehen Hills ( German : Wiehengebirge , pronounced [ˈviːənɡəˌbɪʁɡə] , also locally, just Wiehen ) are

1218-729: The province of Münster . To the north, the Wiehen descends to the North German Plain into a region known as the Lübbecke Loessland . On the banks of the Weser, opposite Porta Westfalica, lies the Wesergebirge , which is the eastern continuation of the Wiehen Hills. This ridge is of similar geological construction and runs as far as the area of Hessisch Oldendorf to the Süntel hills. Southeast of

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1276-425: 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

1334-893: 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

1392-575: The "Werre-Park". It gets its name from the nearby river Werre and was opened on 1 April 1998. ¹ census result There are a number of health treatment facilities in Bad Oeynhausen. The Maternus Rehabilitation Clinic deals with rehabilitation for orthopedic, degenerative, and neurological conditions. The Klinik am Korso deals with eating disorders. The Median Rehabilitation Clinic specializes on rehabilitation for Muslim patients. The Heart and Diabetes Center North Rhine-Westphalia , an institution of

1450-1012: The British Isles and Fennoscandinavia . 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 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

1508-475: The Heidbrink near Lübbecke with an altitude of 320 metres (1,050 ft). The Wiehen Hills lie within the districts of Osnabrück , Minden-Lübbecke and Herford . Their northern section runs in an east–west direction roughly from the territory of Bramsche (northwest of Osnabrück ) via Ostercappeln , Bad Essen , Preußisch Oldendorf and Rödinghausen , Lübbecke , Hüllhorst and Bad Oeynhausen as far as

1566-595: The Kurpark (spa garden), according to plans by Peter Joseph Lenné , and the Kurhaus (spa hotel) in 1908 (from 1980 to 2002 a Casino was located here; today called the Kaiserpalais, it hosts a Varieté, a noble restaurant and a discothèque) were constructed. At the beginning of the 20th century residential houses for the bourgeoisie were built around the spa garden. The extraordinary conglomeration of different architectural styles of

1624-576: The Short , according to the Royal Frankish Annals , stopped over ad locum qui dicitur Rimiae , so that Rehme is commonly accepted as the oldest part of town. The origin myth of Bad Oeynhausen relates that in 1745 a local farmer named Sültemeyer noticed that after his pigs had wallowed in nearby mud they had a salty crust on their backs and he decided to investigate the source. After public awareness of this finding, King Frederick II of Prussia ordered

1682-898: The Wiehen Hills are the Lippe Uplands , to the south the Ravensberg Hills , to the southwest in the area of the Tecklenburg Land are the northern foothills of the Teutoburg Forest , and to the northwest are the hills of the Gehn and the Ankum Heights , the Damme Hills and the Stemweder Berg . North of the northwestern tip of the Wiehen liest the great bog of the Großes Moor . The hills of

1740-433: The Wiehen range from west to east are: Height of the highest hill in bold; heights in metres (m) above Normalhöhennull (NHN) According to folklore, regionally conscious residents around the hills usually admit grudgingly that the Wiehen Hills are not particularly high. In the same breath, they may assert, often with a raised index finger and an odd emphasis on the word gebirge ("hill/mountain range"), that they are

1798-424: 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

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1856-465: The area is used for agriculture: This applies to the entire district of Minden-Lübbecke , where the majority of the land is used for agriculture. Bad Oeynhausen consists of 8 districts: The climate in Bad Oeynhausen is controlled by the Oceanic Climate . The values are based on the ones from Herford (Temperature) and the ones in Bad Oeynhausen (Precipitation) Bad Oeynhausen built a mall called

1914-570: 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

1972-491: The community, which now was called "Neusalzwerk near Rehme". In 1848 King Frederick William IV of Prussia renamed it to "Royal Bath (German: Bad) Oeynhausen", and this name was retained after receiving its own town charter in 1860. The opening of the Cologne - Minden railway line in 1847 connected the city with railroad network. The growth of spa activities and the town's development continued into World War II. Among other things

2030-522: The construction of a saltworks, which was named "Royal Saline Neusalzwerk". Today's Sültemeyer Fountain (colloquial: Pig-Fountain), in the city centre, is a reminder of the city's beginning. After 1830, mining captain Carl Baron of Oeynhausen (1795–1865) oversaw drilling in today's spa garden area in search of salt deposits, but instead found a thermal salt spring in 1845. Quickly the healing abilities of this spring were discovered and first baths were built in

2088-544: 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

2146-608: 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

2204-817: 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

2262-755: 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

2320-556: 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

2378-531: 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

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2436-792: 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

2494-644: 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

2552-571: The northern foothills of Deister and Bückeberge extend farther north than the eastern Wiehen range. However, it is also true that the highest part of the Wiehen Hills at Lübbecke has the most northerly hill over 300 metres in Germany. The Heidbrink, at almost 320 metres high, is also the northernmost "three-hundred" on the European continent between the central Ural Mountains and the Atlantic , i.e. excluding

2610-498: The northernmost hill range in Germany and the one closest to the sea. Whether this assertion is true is in fact a matter of definition. It clearly ignores the morainic ridges further north and closer to the sea, as well as other true uplands such as the Stemweder Berg or the Rehburg Hills . Of course, these hills are much lower and do not reach the 200-metre contour line. Of the higher, say up to 300-metre-high (980 ft) uplands,

2668-611: 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

2726-743: 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

2784-547: 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

2842-421: 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

2900-419: 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

2958-411: The ridge. Whilst the eastern end of the hill chain is clearly defined by the Porta Westfalica gorge and the hill of Wittekindsberg , this is not so simple for its western extremity. To the west the Wiehen descends gradually, transitioning from a hilly ridge into a chain of hillocks and then descending almost imperceptibly into the plain . South of Bramsche the ridge rises again at the Penter Egge to

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3016-436: 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

3074-403: The spa garden's buildings and the surrounding mansions bestowed Bad Oeynhausen the unofficial title "Museum for the Architecture of the 19th Century". One of the most famous buildings, the "Farne-Villa" was replaced by a new building in 1969. In the first half of the 20th century additional thermal salt springs were drilled. Among these the Jordansprudel , drilled in 1926, is best known and with

3132-410: The state of North Rhine-Westphalia , was municipalised in 2004. Bad Oeynhausen is located on the left bank of the Weser river. It has the world's most highly carbonated thermal saltwater fountain, the Jordansprudel . On calm days the fountain gets up to 40 metres high. The water of the spring is believed to have many medicinal qualities, giving rise to a number of health spas. A large percentage of

3190-417: The towns of Minden and Porta Westfalica on the Porta Westfalica gorge and River Weser . They also graze Bohmte and Hille to the north. South of the Wiehen Hills lie Osnabrück , Bissendorf , Melle , Kirchlengern , Bünde , Löhne and Bad Oeynhausen . The Wiehen Hills form the northwestern boundary of the Lower Saxon Hills to which they belong geographically, together with the Westphalian part of

3248-448: 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

3306-414: 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

3364-571: 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

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