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47-404: Dobratsch has a subarctic climate ( Köppen Dfc ) bordering on tundra climate ( Köppen ET ). This Austrian location article is a stub . You can help Misplaced Pages by expanding it . This article about geological processes is a stub . You can help Misplaced Pages by expanding it . Subarctic climate The subarctic climate (also called subpolar climate , or boreal climate )

94-603: A 2012 survey, 26.2% of the population of Khabarovsk Krai adheres to the Russian Orthodox Church , 4% are unaffiliated generic Christians , 1% adhere to other Orthodox churches or are believers in Orthodox Christianity who do not belong to any church, while 1% are adherents of Islam . In addition, 28% of the population declared to be "spiritual but not religious", 23% are atheist , and 16.8% follow other religions or did not give an answer to

141-694: A chain of Russian Cossacks and peasants had been settled along the whole course of the river. In 1858, in the Treaty of Aigun , China recognized the Amur River downstream as far as the Ussuri River as the boundary between Russia and the Qing Empire, and granted Russia free access to the Pacific Ocean. The Sino-Russian border was later further delineated in the Treaty of Peking of 1860 when

188-619: A dry winter, are found in parts of East Asia, like China, where the Siberian High makes the winters colder than places like Scandinavia or Alaska interior but extremely dry (typically with around 5 millimeters (0.20 in) of rainfall equivalent per month), meaning that winter snow cover is very limited. The Dwc climate can be found in: In the Southern Hemisphere, small pockets of the Lesotho Highlands and

235-725: A number of peninsulas along the krai's extensive coast, the main ones being (north to south) the Lisyansky Peninsula , Nurki Peninsula , Tugurskiy Peninsula , and the Tokhareu Peninsula . The main islands of Khabarovsk Krai (north to south) are Malminskiye Island , the Shantar Islands , Menshikov Island , Reyneke Island (Sea of Okhotsk) , Chkalov Island , Baydukov Island , and the Chastye Islands . The island of Sakhalin (Russia's largest)

282-469: A subarctic climate, receives an average rain-equivalent of 101.91 inches (2,588.5 mm) of precipitation per year. Coastal areas of Khabarovsk Krai also have much higher precipitation in summer due to orographic influences (up to 175 millimetres (6.9 in) in July in some areas), whilst the mountainous Kamchatka peninsula and Sakhalin island are even wetter, since orographic moisture isn't confined to

329-430: Is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates . Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. Subarctic or boreal climates are

376-695: Is administered separately as Sakhalin Oblast , along with the Kuril Islands . The charts below detail climate averages from various locations in the krai. Khabarovsk is set near the Chinese border at a lower latitude far inland, while Komsomolsk-on-Amur being further downstream on the Amur river at a higher latitude. Sovetskaya Gavan and Okhotsk are coastal settlements in the deep south and far north, respectively. According to various Chinese and Korean records,

423-725: Is at the junction of the Amur River and the Trans-Siberian Railway . The region's mineral resources are relatively underdeveloped. Khabarovsk Krai contains large gold mining operations (Highland Gold, Polus Gold), a major but low-grade copper deposit being explored by IG Integro Group , and a world-class tin district which was a major contributor to the Soviet industrial complex and is currently being revitalised by Far Eastern Tin (Festivalnoye mine) and by Sable Tin Resources Archived March 13, 2017, at

470-471: Is because of the influence of the East Asian monsoon in summer and the bitterly cold Siberian High in winter. The second-largest city of Komsomolsk-on-Amur has even more violent temperature swings than Khabarovsk, with winter average lows below −30 °C (−22 °F), but in spite of this, avoiding being subarctic because of the significant heat in summer. The main mountain ranges in the region are

517-615: Is below freezing, all moisture in the soil and subsoil freezes solidly to depths of many feet. Summer warmth is insufficient to thaw more than a few surface feet, so permafrost prevails under most areas not near the southern boundary of this climate zone. Seasonal thaw penetrates from 2 to 14 ft (0.6 to 4.3 m), depending on latitude, aspect, and type of ground. Some northern areas with subarctic climates located near oceans (southern Alaska , northern Norway , Sakhalin Oblast and Kamchatka Oblast ), have milder winters and no permafrost, and are more suited for farming unless precipitation

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564-507: Is excessive. The frost-free season is very short, varying from about 45 to 100 days at most, and a freeze can occur anytime outside the summer months in many areas. The first D indicates continentality, with the coldest month below 0 °C (32 °F) (or −3 °C (27 °F)). The second letter denotes precipitation patterns: The third letter denotes temperature: Most subarctic climates have little precipitation, typically no more than 380 mm (15 in) over an entire year due to

611-676: Is found in the following areas: Further north and east in Siberia, continentality increases so much that winters can be exceptionally severe, averaging below −38 °C (−36 °F), even though the hottest month still averages more than 10 °C (50 °F). This creates Dfd climates, which are mostly found in the Sakha Republic : In the Southern Hemisphere , the Dfc climate is found only in small, isolated pockets in

658-594: Is the fundamental law of the krai. The Legislative Duma of Khabarovsk Krai is the regional standing legislative (representative) body. The Legislative Duma exercises its authority by passing laws, resolutions, and other legal acts and by supervising the implementation and observance of the laws and other legal acts passed by it. The highest executive body is the Krai Government, which includes territorial executive bodies, such as district administrations, committees, and commissions that facilitate development and run

705-585: Is the most industrialized territory of the Far East of Russia, producing 30% of the total industrial products in the Far Eastern Economic Region. The machine construction industry consists primarily of a highly developed military–industrial complex of large-scale aircraft- and shipbuilding enterprises. The Komsomolsk-on-Amur Aircraft Production Association is currently among the krai's most successful enterprises, and for years has been

752-1127: The Bureya Range , the Badzhal Range (highest point 2,221 metres (7,287 ft) high, the Gora Ulun ), the Yam-Alin , the Dusse-Alin , the Sikhote-Alin , the Dzhugdzhur Mountains , the Kondyor Massif , as well as a small section of the Suntar-Khayata Range , the Yudoma-Maya Highlands , and the Sette-Daban in the western border regions. The highest point is 2,933 metres (9,623 ft) high, Berill Mountain . There are

799-627: The Drakensberg Mountains have a Dwc classification. Khabarovsk Krai Khabarovsk Krai ( Russian : Хабаровский край , romanized :  Khabarovskiy kray , IPA: [xɐˈbarəfskʲɪj kraj] ) is a federal subject (a krai ) of Russia . It is located in the Russian Far East and is administratively part of the Far Eastern Federal District . The administrative centre of

846-781: The Pacific Ocean , resulting in increased precipitation, especially during the winter months. This climate zone supports the presence of temperate rainforests, mostly on highest areas of the Valdivian rainforest in Chile and the subantarctic forest in Argentina. Climates classified as Dsc or Dsd , with a dry summer, are rare, occurring in very small areas at high elevation around the Mediterranean Basin , Iran , Kyrgyzstan , Tajikistan , Alaska and other parts of

893-570: The Pacific Ocean . Khabarovsk Krai is bordered by Magadan Oblast to the north; Amur Oblast , Jewish Autonomous Oblast , and the Sakha Republic to the west; Primorsky Krai to the south; and Sakhalin Oblast to the east. The population consists of mostly ethnic Russians , but indigenous people of the area are numerous, such as the Tungusic peoples ( Evenks , Negidals , Ulchs , Nanai , Oroch , Udege ), Amur Nivkhs , and Ainu . Khabarovsk Krai shares its borders with Magadan Oblast in

940-713: The Snowy Mountains of Australia , the Southern Alps of New Zealand , and the Lesotho Highlands . In South America , this climate occurs on the western slope of the central Andes in Chile and Argentina , where climatic conditions are notably more humid compared to the eastern slope. The presence of the Andes mountain range contributes to a wetter climate on the western slope by capturing moisture from

987-609: The USSR's collapse when the Jewish Autonomous Oblast was separated from its jurisdiction and made into a direct federal subject of Russia. On 24 April 1996, Khabarovsk signed a power-sharing agreement with the federal government, granting it autonomy. This agreement would be abolished on 12 August 2002. During the Soviet period, the high authority in the oblast was shared between three persons: The first secretary of

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1034-600: The Uda River and the Greater Khingan mountain range (i.e. most of Lower Amuria) was left undemarcated and the Sino-Russian border was allowed to fluctuate. Later in the nineteenth century, Nikolay Muravyov conducted an aggressive policy with China by claiming that the lower reaches of the Amur River belonged to Russia . In 1852, a Russian military expedition under Muravyov explored the Amur, and by 1857,

1081-828: The Ussuri Territory (the Maritime Territory ), which was previously a joint possession, became Russian. Khabarovsk Krai was established on 20 October 1938, when the Far Eastern Krai was split into the Khabarovsk and Primorsky Krais . Kamchatka Oblast , which was originally subordinated to the Far Eastern Krai, fell under the Jurisdiction of Khabarovsk Krai, along with its two National Okrugs, Chukotka and Koryak . In 1947,

1128-643: The Wayback Machine , which is developing the Sable Tin Deposit (Sobolinoye) , a large high-grade deposit, 25 km from Solnechny town. Population : 1,292,944 ( 2021 Census ) ; 1,343,869 ( 2010 Census ) ; 1,436,570 ( 2002 Census ) ; 1,824,506 ( 1989 Soviet census ) . Vital statistics for 2022: Total fertility rate (2022): 1.50 children per woman Life expectancy (2021): Total — 67.85 years (male — 62.91, female — 72.94) According to

1175-601: The northwestern United States ( Eastern Washington , Eastern Oregon , Southern Idaho , California's Eastern Sierra ), the Russian Far East , Akureyri, Iceland , Seneca, Oregon , and Atlin, British Columbia . Turkey and Afghanistan are exceptions; Dsc climates are common in Northeast Anatolia , in the Taurus and Köroğlu Mountains , and the Central Afghan highlands . In the Southern Hemisphere,

1222-416: The subpolar oceanic climate , as the sea is approached where winter temperatures average near or above freezing despite maintaining the short, cool summers. In China and Mongolia, as one moves southwestwards or towards lower elevations, temperatures increase but precipitation is so low that the subarctic climate grades into a cold semi-arid climate . The Dfc climate, by far the most common subarctic type,

1269-823: The Dsc climate is present in South America as a subarctic climate influenced by Mediterranean characteristics, often considered a high-altitude variant of the Mediterranean climate. It is located on the eastern slopes of the central Argentine Andes and in some sections on the Chilean side. While there are no major settlements exhibiting this climate, several localities in the vicinity experience it, such as San Carlos de Bariloche , Villa La Angostura , San Martín de los Andes , Balmaceda , Punta de Vacas , and Termas del Flaco . Climates classified as Dwc or Dwd , with

1316-540: The Khabarovsk CPSU Committee (who, in reality, had the biggest authority), the chairman of the oblast Soviet (legislative power), and the Chairman of the oblast Executive Committee (executive power). Since 1991, CPSU lost all the power, and the head of the Oblast administration, and eventually the governor, was appointed/elected alongside elected regional parliament . The Charter of Khabarovsk Krai

1363-581: The banks of the Amur. The resistance of the Chinese, however, obliged the Cossacks to quit their forts, and by the Treaty of Nerchinsk (1689), Russia abandoned its advance into the basin of the river. Although the Russians were thus deprived of the right to navigate the Amur River, the territorial claim over the lower courses of the river was not settled in the Treaty of Nerchinsk of 1689. The area between

1410-605: The day to day matters of the province. The Krai Administration supports the activities of the Governor , who is the highest official and acts as guarantor of the observance of the Charter in accordance with the Constitution of Russia . On 9 July 2020, the governor of the region, Sergei Furgal , was arrested and flown to Moscow. The 2020 Khabarovsk Krai protests began on 11 July 2020, in support of Furgal. Khabarovsk Krai

1457-490: The krai is the city of Khabarovsk , which is home to roughly half of the krai's population and the largest city in the Russian Far East (just ahead of Vladivostok ). Khabarovsk Krai is the fourth-largest federal subject by area, and had a population of 1,343,869 as of 2010. Being dominated by the Siberian High winter cold, the continental climates of the krai see extreme freezing for an area adjacent to

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1504-437: The largest taxpayer of the territory. Other major industries include timber-working and fishing , along with metallurgy in the main cities. Komsomolsk-on-Amur is the iron and steel centre of the Far East; a pipeline from northern Sakhalin supplies the petroleum-refining industry in the city of Khabarovsk . In the Amur basin, there is also some cultivation of wheat and soybeans . The administrative centre , Khabarovsk,

1551-406: The long summer days at such latitudes do permit some agriculture. In some areas, ice has scoured rock surfaces bare, entirely stripping off the overburden. Elsewhere, rock basins have been formed and stream courses dammed, creating countless lakes. Should one go northward or even toward a polar sea, one finds that the warmest month has an average temperature of less than 10 °C (50 °F), and

1598-423: The long winters and make use of the short summers. Trees are mostly limited to conifers , as few broadleaved trees are able to survive the very low temperatures in winter. This type of forest is also known as taiga , a term which is sometimes applied to the climate found therein as well. Even though the diversity may be low, the area and numbers are high, and the taiga (boreal) forest is the largest forest biome on

1645-425: The low temperatures and evapotranspiration . Away from the coasts, precipitation occurs mostly in the summer months, while in coastal areas with subarctic climates the heaviest precipitation is usually during the autumn months when the relative warmth of sea vis-à-vis land is greatest. Low precipitation, by the standards of more temperate regions with longer summers and warmer winters, is typically sufficient in view of

1692-539: The north; with the Sakha Republic and Amur Oblast in the west; with the Jewish Autonomous Oblast , China ( Heilongjiang ), and Primorsky Krai in the south; and is limited by the Sea of Okhotsk in the east. In terms of area, it is the fourth-largest federal subject within Russia. Major islands include the Shantar Islands . Taiga and tundra in the north, swampy forest in the central depression, and deciduous forest in

1739-596: The northern part of Sakhalin was removed from the Krai to join the southern part and form Sakhalin Oblast . In 1948, parts of its southwestern territories were removed from the Krai to form Amur Oblast . In 1953, Magadan Oblast was established from the northern parts of the Krai and was given jurisdiction over Chukotka National Okrug, which was originally under the jurisdiction of Kamchatka oblast. In 1956, Kamchatka Oblast became its own region and took Koryak National Okrug with it. The Krai took its modern form in 1991, just before

1786-460: The planet, with most of the forests located in Russia and Canada . The process by which plants become acclimated to cold temperatures is called hardening . Agricultural potential is generally poor, due to the natural infertility of soils and the prevalence of swamps and lakes left by departing ice sheets , and short growing seasons prohibit all but the hardiest of crops. Despite the short season,

1833-487: The question. There are the following institutions of higher education in Khabarovsk Krai. The city was a host to the 1981 Bandy World Championship as well as to the 2015 Bandy World Championship . For the 2015 games, twenty-one teams originally were expected, which would have been four more than the record-making seventeen from the 2014 tournament , but eventually, only sixteen teams came. The A Division of

1880-468: The sea near the mid-latitudes, but also warm summers in the interior. The southern region lies mostly in the basin of the lower Amur River , with the mouth of the river located at Nikolaevsk-on-Amur draining into the Strait of Tartary , which separates Khabarovsk Krai from the island of Sakhalin . The north occupies a vast mountainous area along the coastline of the Sea of Okhotsk , a marginal sea of

1927-447: The source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification Dfc , Dwc , Dsc , Dfd , Dwd and Dsd . This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below −50 °C (−58 °F) and in summer, the temperature may exceed 26 °C (79 °F). However,

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1974-703: The south are the natural vegetation in the area. The main rivers are the Amur , Amgun , Uda , and Tugur , among others. There are also lakes such as Bokon , Bolon , Chukchagir , Evoron , Kizi , Khummi , Orel , and Udyl , among others. Khabarovsk Krai has a severely continental climate with its northern areas being subarctic with stronger maritime summer moderation in the north. In its southerly areas, especially inland, annual swings are extremely strong, with Khabarovsk itself having hot, wet, and humid summers which rapidly transform into severely cold and long winters, where temperatures hardly ever go above freezing. This

2021-727: The southern part of Khabarovsk Krai was originally occupied by one of the five semi-nomadic Shiwei , the Bo Shiwei tribes, and the Black Water Mohe tribes living, respectively, on the west and the east of the Bureya and the Lesser Khingan ranges. In 1643, Vassili Poyarkov 's boats descended the Amur , returning to Yakutsk by the Sea of Okhotsk and the Aldan River , and in 1649–1650, Yerofey Khabarov occupied

2068-403: The subarctic climate grades into a tundra climate not at all suitable for trees. Southward, this climate grades into the humid continental climates with longer summers (and usually less-severe winters) allowing broadleaf trees ; in a few locations close to a temperate sea (as in northern Norway and southern Alaska ), this climate can grade into a short-summer version of an oceanic climate ,

2115-420: The summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least 10 °C (50 °F) to fall into this category of climate, and the coldest month should average below 0 °C (32 °F) (or −3 °C (27 °F)). Record low temperatures can approach −70 °C (−94 °F). With 5–7 consecutive months when the average temperature

2162-428: The very low evapotranspiration to allow a water-logged terrain in many areas of subarctic climate and to permit snow cover during winter, which is generally persistent for an extended period. A notable exception to this pattern is that subarctic climates occurring at high elevations in otherwise temperate regions have extremely high precipitation due to orographic lift . Mount Washington , with temperatures typical of

2209-519: The warmer months and creates large glaciers in Kamchatka. Labrador , in eastern Canada, is similarly wet throughout the year due to the semi-permanent Icelandic Low and can receive up to 1,300 millimetres (51 in) of rainfall equivalent per year, creating a snow cover of up to 1.5 metres (59 in) that does not melt until June. Vegetation in regions with subarctic climates is generally of low diversity, as only hardy tree species can survive

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