Continental climate in the context of "Kyrgyzstan"

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⭐ Core Definition: Continental climate

Continental climates often have a significant annual variation in temperature (warm to hot summers and cold winters). They tend to occur in central and eastern parts of the three northern-tier continents (North America and Eurasia), typically in the middle latitudes (40 to 55 or 60 degrees north), often within large landmasses, where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans.

Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, northern Mongolia, most of Korea, central Afghanistan, parts of Kazakhstan and Kyrgyzstan, eastern and southeastern Europe, much of the Russian Federation south of the Arctic Circle, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate.

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Continental climate in the context of Europe

Europe is a continent located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south, and Asia to the east. Europe shares the landmass of Eurasia with Asia, and of Afro-Eurasia with both Africa and Asia. Europe is commonly considered to be separated from Asia by the watershed of the Ural Mountains, the Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea, and the Turkish straits.

Europe covers approx. 10,186,000 square kilometres (3,933,000 sq mi), or 2% of Earth's surface (6.8% of Earth's land area), making it the second-smallest continent (using the seven-continent model). Politically, Europe is divided into about fifty sovereign states, of which Russia is the largest and most populous, spanning 39% of the continent and comprising 15% of its population. Europe had a total population of about 745 million (about 10% of the world population) in 2021; the third-largest after Asia and Africa. The European climate is affected by warm Atlantic currents, such as the Gulf Stream, which produce a temperate climate, tempering winters and summers, on much of the continent. Further from the sea, seasonal differences are more noticeable producing more continental climates.

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Continental climate in the context of Kosovo

Kosovo, officially the Republic of Kosovo, is a landlocked country in Southeast Europe with partial diplomatic recognition. It is bordered by Albania to the southwest, Montenegro to the west, Serbia to the north and east, and North Macedonia to the southeast. It covers an area of 10,887 km (4,203 sq mi) and has a population of nearly 1.6 million, of whom the vast majority (approximately 92 per cent) are ethnic Albanians. Kosovo has a varied terrain, with high plains along with rolling hills and mountains, some of which have an altitude over 2,500 m (8,200 ft). Its climate is mainly continental with some Mediterranean and Alpine influences. Kosovo's capital and most populous city is Pristina; other major cities and urban areas include Prizren, Ferizaj, Gjilan, and Peja.

Kosovo formed the core territory of the Dardani, an Illyrian people, attested in classical sources from the 4th century BCE. The Dardani established the Kingdom of Dardania, with its political and cultural center likely located near present-day Lipjan (ancient Ulpiana). The kingdom was incorporated into the Roman Empire in the 1st century BCE; later, in the 3rd century CE, it was transformed into a separate Roman province. During the Byzantine period, the region was eventually organised as part of the Theme of Dardania and remained under imperial control, facing Slavic migrations in the 6th and 7th centuries CE. Control shifted between the Byzantines and the First Bulgarian Empire. In the 13th century, Kosovo became integral to the Serbian medieval state and the establishment of the Serbian Patriarchate. Ottoman expansion in the Balkans in the late 14th and 15th centuries led to the decline and fall of the Serbian Empire; the Battle of Kosovo of 1389, in which a Serbian-led coalition of various ethnicities fought against the Ottoman Empire, is considered one of the defining moments.

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Continental climate in the context of Shkodër

Shkodër (/ˈʃkdər/ SHKOH-dər, Albanian: [ˈʃkɔdəɾ]; Albanian definite form: Shkodra; historically known as Scodra or Scutari) is the fifth-most-populous city of Albania and the seat of Shkodër County and Shkodër Municipality. Shkodër has been continuously inhabited since the Early Bronze Age (c. 2250–2000 BC), and has roughly 2,200 years of recorded history. The city sprawls across the Plain of Mbishkodra between the southern part of Lake Shkodër and the foothills of the Albanian Alps on the banks of the Buna, Drin and Kir rivers. Due to its proximity to the Adriatic Sea, Shkodër is affected by a seasonal Mediterranean climate with continental influences.

An urban settlement called Skodra was founded by the Illyrian tribe of Labeatae in the 4th century BCE. It became the capital of the Illyrian kingdom under the Ardiaei and Labeatae and was one of the most important cities of the Balkans in ancient times. It has historically developed on a 130 m (430 ft) hill strategically located in the outflow of Lake Shkodër into the Buna. The Romans annexed the city after the third Illyrian War in 168 BC, when the Illyrian king Gentius was defeated by the Roman force of Anicius Gallus. In the 3rd century AD, Shkodër became the capital of Praevalitana, due to the administrative reform of the Roman Emperor Diocletian. With the spread of Christianity in the 4th century AD, the Archdiocese of Scodra was founded and was assumed in 535 by Byzantine Emperor Justinian I.

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Continental climate in the context of Romania

Romania is a country located at the crossroads of Central, Eastern and Southeast Europe. It borders Ukraine to the north and east, Hungary to the west, Serbia to the southwest, Bulgaria to the south, Moldova to the east, and the Black Sea to the southeast. It has a mainly continental climate, and an area of 238,397 km (92,046 sq mi) with a population of 19 million people. Romania is the twelfth-largest country in Europe and the sixth-most populous member state of the European Union. Europe's second-longest river, the Danube, empties into the Danube Delta in the southeast of the country. The Carpathian Mountains cross Romania from the north to the southwest and include Moldoveanu Peak, at an altitude of 2,544 m (8,346 ft). Bucharest is the country's capital, largest urban area, and financial centre. Other major urban areas include Cluj-Napoca, Timișoara, Iași, Constanța and Brașov.

Settlement in the territory of modern Romania began in the Lower Paleolithic, later becoming the Dacian Kingdom before Roman conquest and Romanisation. The modern Romanian state was formed in 1859 with the unification of Moldavia and Wallachia under Alexandru Ioan Cuza, becoming the Kingdom of Romania in 1881 under Carol I of Romania. Romania gained independence from the Ottoman Empire in 1877, formalised by the Treaty of Berlin. After World War I, Transylvania, Banat, Bukovina, and Bessarabia joined the Old Kingdom, forming Greater Romania, which reached its largest territorial extent. In 1940, under Axis pressure, Romania lost territories to Hungary, Bulgaria, and the Soviet Union. Following the 1944 Romanian coup d'état, Romania switched sides to join the Allies. After World War II, it regained Northern Transylvania through the Paris Peace Treaties. Under Soviet occupation, King Michael I was forced to abdicate, and Romania became a socialist republic and Warsaw Pact member. After the uniquely violent Romanian revolution in December 1989, Romania began a transition to liberal democracy and a market economy.

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Continental climate in the context of Slovenia

Slovenia, officially the Republic of Slovenia, is a country in Central Europe. Formed in 1991, Slovenia borders Italy to the west, Austria to the north, Hungary to the northeast, and Croatia to the south and southeast; its southwestern boundary consists of a 46.6 km coastline on the Adriatic Sea. Slovenia is mostly mountainous and forested, covers 20,271 square kilometres (7,827 sq mi), and has a population of approximately 2.1 million people. Slovene is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. Ljubljana, the capital and largest city of Slovenia, is geographically situated near the centre of the country. Other larger urban centers include Maribor, Ptuj, Kranj, Celje, and Koper.

Slovenia's territory has been part of many different states, including the Byzantine Empire, the Carolingian Empire, the Holy Roman Empire, the Kingdom of Hungary, the Republic of Venice, the Illyrian Provinces of Napoleon's First French Empire and the Habsburg Empire. The Kingdom of Serbs, Croats, and Slovenes was formed in December 1918; in 1929, the Kingdom became known as Yugoslavia. In 1946, after World War II, Slovenia was established as one of six republics that made up the socialist federation of Yugoslavia. In June 1991, Slovenia declared independence from Yugoslavia and became an independent sovereign state.

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Continental climate in the context of New Brunswick

New Brunswick is a province of Canada, bordering Quebec to the north, Nova Scotia to the east, the Gulf of Saint Lawrence to the northeast, the Bay of Fundy to the southeast, and the U.S. state of Maine to the west. It is part of Eastern Canada and is one of the three Maritime provinces and one of the four Atlantic provinces. The province is about 83% forested and its northern half is occupied by the Appalachians. The province's climate is continental with snowy winters and temperate summers. The province has a surface area of 72,908 km (28,150 sq mi) and 775,610 inhabitants (2021 census).

Approximately half of the population lives in urban areas, predominantly in Moncton, Saint John and Fredericton. In 1969, New Brunswick passed the Official Languages Act which began recognizing French as an official language, along with English. New Brunswickers have the right to receive provincial government services in the official language of their choice. About two thirds of the population are English speaking and one third is French speaking. New Brunswick is home to most of the cultural region of Acadia and most Acadians. New Brunswick's variety of French is called Acadian French. There are seven regional accents.

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Continental climate in the context of Sivas Province

Sivas Province (Turkish: Sivas ili) is a province of Turkey. It is located in the eastern part of the Central Anatolia region of Turkey. Its area is 28,164 km (the second largest province after Konya), and its population is 634,924 (2022). Its adjacent provinces are Yozgat to the west, Kayseri to the southwest, Kahramanmaraş to the south, Malatya to the southeast, Erzincan to the east, Giresun to the northeast, and Ordu to the north. Its capital is Sivas.

Most of Sivas Province has the typical continental climate of the Central Anatolian Region, in which summer months are hot and dry, while winter months are cold and snowy. However, the northern part of the province shows some features of the oceanic/humid subtropical Black Sea climate, while the eastern portion has influences of the Eastern Anatolian highland climate. This province is noted for its thermal springs.

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Continental climate in the context of Bosnia and Herzegovina

Bosnia and Herzegovina, often referred to as Bosnia-Herzegovina or short as Bosnia, is a country in Southeast Europe. Situated on the Balkan Peninsula, it borders Serbia to the east, Montenegro to the southeast, and Croatia to the north and southwest, with a 20-kilometre-long (12-mile) coast on the Adriatic Sea in the south. Bosnia has a moderate continental climate with hot summers and cold, snowy winters. Its geography is largely mountainous, particularly in the central and eastern regions, which are dominated by the Dinaric Alps. Herzegovina, the smaller, southern region, has a Mediterranean climate and is mostly mountainous. Sarajevo is the capital and the largest city.

The area has been inhabited since at least the Upper Palaeolithic, with permanent human settlement traced to the Neolithic cultures of Butmir, Kakanj, and Vučedol. After the arrival of the first Indo-Europeans, the area was populated by several Illyrian and Celtic civilisations. Most of modern Bosnia was incorporated into the Roman province of Dalmatia by the mid-first century BCE. The ancestors of the modern South Slavic peoples arrived between the sixth and ninth centuries. In the 12th century, the Banate of Bosnia was established as the first independent Bosnian polity. It gradually evolved and expanded into the Kingdom of Bosnia, which became the most powerful state in the western Balkans by the 14th century. The Ottoman Empire annexed the region in 1463 and introduced Islam. From the late 19th century until World War I, the country was annexed into the Austro-Hungarian monarchy. In the interwar period, Bosnia and Herzegovina was part of the Kingdom of Yugoslavia. After World War II, it was granted full republic status in the newly formed Socialist Federal Republic of Yugoslavia. In 1992, following the breakup of Yugoslavia, the republic proclaimed independence. This was followed by the Bosnian War, which lasted until late 1995 and ended with the signing of the Dayton Agreement.

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Continental climate in the context of Prizren

Prizren (Albanian definite form: Prizreni, pronounced [pɾizˈɾɛni]; Serbian Cyrillic: Призрен) is the second most populous city and municipality of Kosovo and seat of the eponymous municipality and district. It is located on the banks of the Prizren River between the foothills of the Sharr Mountains in southern Kosovo. Prizren experiences a continental climate with some mediterranean influences.

Prizren is constitutionally designated as the historical capital of the country. Archaeological excavations in Prizren Fortress indicate that its fortress area has seen habitation and use since the Bronze Age. Prizren has been traditionally identified with the settlement of Theranda in Roman Dardania, although other locations have been suggested in recent research. In late antiquity it was part of the defensive fortification system in western Dardania and the fort was reconstructed in the era of eastern Roman Emperor Justinian. Byzantine rule in the region ended definitively in 1219-20 as the Serbian Nemanjić dynasty took control of the fort and the town. Prizren served as the capital of the Serbian Empire under the reign of Stefan Dušan, as it bloomed to become an important center of trade and commerce during Dušan's reign. From 1371, a series of regional feudal rulers controlled Prizren, including the Mrnjavčević family, the Balšić noble family, the Branković dynasty, as well as the prominent House of Kastrioti. Ottoman Turks captured Prizren from Serbian Despotate in 1455 and almost immediately served as the capital of Sanjak of Prizren in the Ottoman Empire. While standing as an important administrative city for the Ottomans, Prizren became an important political center of the Albanian Renaissance during the late 19th century.

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