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- Siberian_High abstract "The Siberian High (also Siberian Anticyclone) is a massive collection of cold or very cold dry air that accumulates on the northeastern part of Eurasian terrain for the cold part of the year, roughly from September till April. Usually, it is centered around Lake Baikal. It reaches its greatest size and strength in the winter, when the air temperature near the center of the high-pressure cell or anticyclone is often lower than −40 °C (−40 °F). The sea-level pressure (atmospheric pressure) is often above 1,040 millibars (31 inHg). The Siberian High is the strongest semi-permanent high in the northern hemisphere and is responsible for both the lowest temperature in the Northern Hemisphere, of −67.8 °C (−90.0 °F) on 15 January 1885 at Verkhoyansk and the highest pressure, 1083.8 mbar (108.38 kPa, 32.01 inHg) at Agata, Krasnoyarsk Krai on 31 December 1968. The Siberian High is responsible both for severe winter cold and attendant dry conditions with little snow and few or no glaciers across Siberia, Mongolia and China. During the summer, the Siberian High is largely replaced by the Asiatic low.The Siberian High affects the weather patterns in most parts of the Northern Hemisphere: its influence extends as far west as the Po Valley in Italy and as far southeast as Malaysia, where it is a critical component of the northeast monsoon. Occasionally a strong Siberian High can bring unusually cold weather into the tropics as far southeast as the Philippines, or as far east from Russia as Eastern Canada (which happened several times over the course of the 2014 Winter) . It may block or reduce the size of low-pressure cells or cyclones and generate dry weather across much of the Asian landscape with the exception of regions such as Hokuriku and the Caspian Sea coast of Iran that receive orthographic rainfall from the winds it generates.Siberian air is generally colder than Arctic air, because unlike Arctic air which forms over the sea ice around the North Pole, Siberian air forms over the cold tundra of Siberia, which does not radiate heat the same way the ice of the Arctic does.".
- Siberian_High wikiPageID "1386236".
- Siberian_High wikiPageRevisionID "606794314".
- Siberian_High hasPhotoCollection Siberian_High.
- Siberian_High subject Category:Anticyclones.
- Siberian_High subject Category:Climate_change_in_Russia.
- Siberian_High subject Category:Climate_of_Asia.
- Siberian_High subject Category:Climate_of_Europe.
- Siberian_High subject Category:Climate_of_Russia.
- Siberian_High point "66.88333333333334 93.46666666666667".
- Siberian_High type Anticyclone114521021.
- Siberian_High type Anticyclones.
- Siberian_High type Atmosphere114520278.
- Siberian_High type AtmosphericPhenomenon111425580.
- Siberian_High type NaturalPhenomenon111408559.
- Siberian_High type Phenomenon100034213.
- Siberian_High type PhysicalEntity100001930.
- Siberian_High type PhysicalPhenomenon111419404.
- Siberian_High type Process100029677.
- Siberian_High type Weather111524662.
- Siberian_High type SpatialThing.
- Siberian_High comment "The Siberian High (also Siberian Anticyclone) is a massive collection of cold or very cold dry air that accumulates on the northeastern part of Eurasian terrain for the cold part of the year, roughly from September till April. Usually, it is centered around Lake Baikal. It reaches its greatest size and strength in the winter, when the air temperature near the center of the high-pressure cell or anticyclone is often lower than −40 °C (−40 °F).".
- Siberian_High label "Anticiclone russo-siberiano".
- Siberian_High label "Anticiclón de Siberia".
- Siberian_High label "Anticyclone de Sibérie".
- Siberian_High label "Siberian High".
- Siberian_High label "Sibirienhoch".
- Siberian_High label "Wyż syberyjski".
- Siberian_High label "Азиатский максимум".
- Siberian_High label "المرتفع السيبيري".
- Siberian_High label "シベリア高気圧".
- Siberian_High label "西伯利亞高壓".
- Siberian_High sameAs Sibirienhoch.
- Siberian_High sameAs Anticiclón_de_Siberia.
- Siberian_High sameAs Siberiako_goi_presio_gunea.
- Siberian_High sameAs Anticyclone_de_Sibérie.
- Siberian_High sameAs Anticiclone_russo-siberiano.
- Siberian_High sameAs シベリア高気圧.
- Siberian_High sameAs 시베리아_기단.
- Siberian_High sameAs Wyż_syberyjski.
- Siberian_High sameAs m.04yfwn.
- Siberian_High sameAs Q488578.
- Siberian_High sameAs Q488578.
- Siberian_High sameAs Siberian_High.
- Siberian_High lat "66.88333333333334".
- Siberian_High long "93.46666666666667".
- Siberian_High wasDerivedFrom Siberian_High?oldid=606794314.
- Siberian_High isPrimaryTopicOf Siberian_High.