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Khorbusuonka

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The Khorbusuonka ( Russian : Хорбусуонка ) is a river in Yakutia (Sakha Republic), Russia . It is a tributary of the Olenyok with a length of 290 kilometres (180 mi) and a drainage basin area of 3,230 square kilometres (1,250 sq mi).

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18-650: The river flows north of the Arctic Circle across a lonely, desolate area of Bulunsky District devoid of settlements. The Khorbusuonka is a right tributary of the Olenyok. Its sources are in the southern part of the Kystyk Plateau , located southwest of the Chekanovsky Ridge . It flows first in an ESE direction, then it bends and flows roughly northwards, still within the plateau. Its channel

36-633: Is often no direct view of the true horizon. The largest communities north of the Arctic Circle are situated in Russia, Norway, and Sweden: Murmansk (population 295,374) and Norilsk (178,018) in Russia; Tromsø (75,638) in Norway, Vorkuta (58,133) in Russia, Bodø (52,357) and Harstad (24,703) in Norway; and Kiruna , Sweden (22,841). Rovaniemi (62,667) in Finland is the largest settlement in

54-639: Is the largest settlement north of the Arctic Circle with about 5,000 inhabitants. The largest such community in Canada is Inuvik in the Northwest Territories , with 3,137 inhabitants. Download coordinates as: The Arctic Circle is roughly 16,000 km (9,900 mi) in circumference. The area north of the Circle is about 20,000,000 km (7,700,000 sq mi) and covers roughly 4% of Earth's surface. The Arctic Circle passes through

72-643: Is winding within a wide valley in the Kystyk Plateau area. In its very last stretch the river descends to the Olenyok floodplain , where there are a few lakes right by the great river to the south of the Kelimyar . Finally the Khorbusuonka joins the right bank of the Olenyok river 221 km (137 mi) upstream of its mouth. The confluence is only 4 km (2.5 mi) upstream from the mouth of

90-608: The Arctic Ocean , the Scandinavian Peninsula , North Asia , Northern America , and Greenland. The land within the Arctic Circle is divided among eight countries: Norway, Sweden, Finland, Russia, the United States ( Alaska ), Canada ( Yukon , Northwest Territories , and Nunavut ), Denmark (Greenland), and Iceland (where it passes through the small offshore island of Grímsey ). The climate north of

108-501: The Bur in the opposite bank. Owing to the harshness of the climate the river is frozen most of the year. It stays under ice between early October and early June. Its longest tributaries are the 101 kilometres (63 mi) long Nykaabyt (Ньыкаабыт), the 40 kilometres (25 mi) long Syyrdaakh-Yurege (Сыырдаах-Юрэгэ), the 50 kilometres (31 mi) long Khorbusuonkachaan, the 33 kilometres (21 mi) long Yuyosee-Yuyoteekh (Юёсээ-Юёттээх) and

126-700: The Northern Hemisphere , the Sun will not rise all day, and on the Northern Hemisphere's summer solstice (which is the longest day of the year), the Sun will not set. These phenomena are referred to as polar night and midnight sun respectively, and the further north one progresses, the more pronounced these effects become. For example, in the Russian port city of Murmansk , three degrees above

144-406: The 23 kilometres (14 mi) long Khatyspyt from the right, as well as the 39 kilometres (24 mi) long Anabyl (Анабыл) and the 38 kilometres (24 mi) long Mattaya from the left. The river basin is dominated by tundra with sparse larch forest and some willow thickets by the riverside in wide valleys. Since the area is uninhabited, deer are numerous and fearless. The main fish species in

162-510: The Arctic Circle is currently drifting northwards at a speed of about 14.5 m (48 ft) per year. The word arctic comes from the Greek word ἀρκτικός ( arktikos : "near the Bear , northern") and that from the word ἄρκτος ( arktos : " bear "). The Arctic Circle is the southernmost latitude in the Northern Hemisphere at which the centre of the Sun can remain continuously above or below

180-526: The Arctic Circle is generally cold, but the coastal areas of Norway have a generally mild climate as a result of the Gulf Stream , which makes the ports of northern Norway and northwest Russia ice-free all year long. In the interior, summers can be quite warm, while winters are extremely cold. For example, summer temperatures in Norilsk , Russia will sometimes reach as high as 30 °C (86 °F), while

198-567: The Arctic Circle, the Sun does not rise above the horizon for 40 successive days in midwinter. The position of the Arctic Circle is not fixed and currently runs 66°33′50.2″ north of the Equator . Its latitude depends on the Earth's axial tilt , which fluctuates within a margin of more than 2° over a 41,000-year period, owing to tidal forces resulting from the orbit of the Moon . Consequently,

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216-500: The horizon for twenty-four hours; as a result, at least once each year at any location within the Arctic Circle the centre of the Sun is visible at local midnight , and at least once the centre is not visible at local noon . Directly on the Arctic Circle these events occur, in principle, exactly once per year: at the June and December solstices , respectively. However, because of atmospheric refraction and mirages , and also because

234-404: The immediate vicinity of the Arctic Circle, lying 6 km (4 mi) south of the line. Salekhard (51,186) in Russia is the only city in the world located directly on the Arctic Circle. In contrast, the largest North American community north of the Arctic Circle, Sisimiut ( Greenland ), has approximately 5,600 inhabitants. In the United States, Utqiagvik, Alaska (formerly known as Barrow)

252-556: The length of the day on 20 June 2016, close to the summer solstice of the Northern Hemisphere and winter solstice of the Southern Hemisphere . The data was collected from the website of the Finnish Meteorological Institute as well as from certain other websites. The data is arranged geographically and within the tables from the longest day to the shortest one. Times that occur

270-585: The longest period of daylight), while in the Southern Hemisphere it is the winter solstice (the day with the shortest period of daylight). It is also known as the northern solstice . During June solstice, the Sun is directly over the Tropic of Cancer, located in the northern hemisphere. The June solstice solar year is the solar year based on the June solstice. It is thus the length of time between adjacent June solstices. The following tables contain information on

288-480: The sun appears as a disk and not a point, part of the midnight sun is visible, on the night of the northern summer solstice , at a latitude of about 50 minutes of arc (′) (90 km (56 mi)) south of the Arctic Circle. Similarly, on the day of the northern winter solstice , part of the Sun may be seen up to about 50′ north of the Arctic Circle. That is true at sea level ; those limits increase with elevation above sea level , although in mountainous regions there

306-465: The waters is lenok . Arctic Circle The Arctic Circle is one of the two polar circles , and the most northerly of the five major circles of latitude as shown on maps of Earth at about 66° 34' N. Its southern equivalent is the Antarctic Circle . The Arctic Circle marks the southernmost latitude at which, on the winter solstice (which is the shortest day of the year) in

324-465: The winter temperatures frequently fall below −50 °C (−58 °F). Starting at the prime meridian and heading eastwards, the Arctic Circle passes through: June solstice The June solstice is the solstice on Earth that occurs annually between 20 and 22 June according to the Gregorian calendar . In the Northern Hemisphere , the June solstice is the summer solstice (the day with

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