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阳泉
Yangquan ( zh, s=阳泉 , t=陽泉 , p=Yángquán ) is a prefecture-level city in the east of Shanxi province, People's Republic of China, bordering Hebei province to the east. Known as "Rippling Spring" in ancient times, it lies on the eastern edge of the Loess Plateau and the western side of the Taihang Mountains. Yangquan occupies a total area of . According to the Seventh National Population Census of the People's Republic of China, 2020 census, Yangquan had a population of 1,318,505, of which 1,037,456 lived in the built-up (or metro) area consists of 3 urban districts plus Pingding County. Yangquan is a new industrial city in Shanxi province. It belongs to the warm temperate semi-humid continental monsoon climate zone. Yangquan City covers two counties and three districts. Administrative divisions Geography and climate Yangquan has a rather dry, monsoon-influenced humid continental climate /semi-arid climate (Köppen climate classification, Köppen ''Dwa/BSk''), with cold ...
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Shanxi
Shanxi; Chinese postal romanization, formerly romanised as Shansi is a Provinces of China, province in North China. Its capital and largest city of the province is Taiyuan, while its next most populated prefecture-level cities are Changzhi and Datong. Its one-character abbreviation is (), after the Jin (Chinese state), state of Jin that existed there during the Spring and Autumn period (). The name ''Shanxi'' means 'west of the mountains', a reference to its location west of the Taihang Mountains. Shanxi borders Hebei to the east, Henan to the south, Shaanxi to the west and Inner Mongolia to the north. Shanxi's terrain is characterised by a plateau bounded partly by mountain ranges. Shanxi's culture is largely dominated by the ethnic Han Chinese, Han majority, who make up over 99% of its population. Jin Chinese is considered by some linguists to be a distinct language from Mandarin and its geographical range covers most of Shanxi. Both Jin and Mandarin are spoken in Shanxi. ...
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Prefecture-level City
A prefecture-level city () or prefectural city is an administrative division of the China, People's Republic of China (PRC), ranking below a province of China, province and above a Counties of the People's Republic of China, county in China's administrative structure. Details During the Republican era, many of China's prefectural cities were designated as Counties of Taiwan, counties as the country's second level division below a province. From 1949 to 1983, the official term was a province-administrated city (Chinese: 省辖市). Prefectural level cities form the second level of the administrative structure (alongside prefecture of China, prefectures, Leagues of China, leagues and autonomous prefectures). Administrative chiefs (mayors) of prefectural level cities generally have the same rank as a division chief () of a national ministry. Since the 1980s, most former prefectures have been renamed into prefecture-level cities. A prefectural level city is a "city" () and "p ...
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Kuangqu, Yangquan
Kuangqu () is a district of Yangquan, Shanxi Shanxi; Chinese postal romanization, formerly romanised as Shansi is a Provinces of China, province in North China. Its capital and largest city of the province is Taiyuan, while its next most populated prefecture-level cities are Changzhi a ... province, China. As of 2002, it has a population of 220,000 residing in an area of . Referenceswww.xzqh.org County-level divisions of Shanxi Yangquan {{Shanxi-geo-stub ...
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Shijiazhuang
Shijiazhuang; Mandarin: ; formerly known as Shimen and romanized as Shihkiachwang is the capital and most populous city of China's Hebei Province. A prefecture-level city southwest of Beijing, it administers eight districts, three county-level cities and eleven counties, and is east of the Taihang Mountains, which extend over from north to south with an average elevation of . At the 2020 census, the city had a population of 11,235,086, with 6,230,709 in the built-up area comprising all urban districts except Jingxing District and Zhengding County, the twelfth largest in mainland China. Shijiazhuang experienced dramatic growth after the founding of the People's Republic of China in 1949. The population of the metropolitan area has more than quadrupled in thirty years as a result of industrialization and infrastructural developments. From 2008 to 2011, Shijiazhuang implemented a three-year plan, resulting in an increase of green areas and new buildings and roads. A railway ...
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Xinzhou
Xinzhou, ancient name Xiurong (), is a prefecture-level city occupying the north-central section of Shanxi Province in the People's Republic of China, bordering Hebei to the east, Shaanxi to the west, and Inner Mongolia to the northwest. As of 2022, the city has a permanent population of 2,655,563. Administrative divisions As of 2024, there are 14 county-level administrative divisions under jurisdiction of Xinzhou, including 1 district, 1 county-level city, and 12 counties. The details of those county-level administrative divisions are as follows: Climate Xinzhou has a continental, monsoon-influenced semi-arid climate (Köppen ''BSk''), with cold, very dry, and somewhat long winters, and warm, somewhat humid summers. The monthly 24-hour average temperature ranges from in January to in July, and the annual mean is . Typifying the influence of the East Asian Monsoon, close to three-fourths of the annual of precipitation occurs from June to September. Demographics Ac ...
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China Meteorological Administration
The China Meteorological Administration (CMA) is the national weather service of the People's Republic of China. The institution is located in Beijing. History The agency was originally established in December 1949 as the Central Military Commission Meteorological Bureau. It replaced the Central Weather Bureau formed in 1941. In 1994, the CMA was transformed from a subordinate governmental body into one of the public service agencies under the State Council.CMA.gov history
Meteorological bureaus are established in 31 provinces, autonomous regions and
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Diurnal Temperature Variation
In meteorology, diurnal temperature variation is the variation between a high air temperature and a low temperature that occurs during the same day. Temperature lag Temperature lag, also known as thermal inertia, is an important factor in diurnal temperature variation. Peak daily temperature generally occurs ''after'' noon, as air keeps absorbing net heat for a period of time from morning through noon and some time thereafter. Similarly, minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon is seasonal lag. As solar energy strikes the Earth's surface each morning, a shallow layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by from just above the ground t ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSh'' and ''BSk'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as they usually cannot support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): * ...
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Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons. The definition of this climate in terms of temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Although amount of snowfall is not a factor used in defining the humid continental climate, snow during the winter in this type of climate is almost a guarantee, either intermitte ...
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Monsoon
A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in Atmosphere of Earth, atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the Wet season, rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is also sometimes used to describe locally heavy but short-term rains. The major monsoon systems of the world consist of the Monsoon#Africa (West African and Southeast African), West African, Asian–Australian monsoon, Australian, the North American monsoon, North American, and South American monsoons. The term was first Glossary of the British Raj, used in English in British India and neighboring countries to refer to the big seasonal winds blowin ...
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Pinyin
Hanyu Pinyin, or simply pinyin, officially the Chinese Phonetic Alphabet, is the most common romanization system for Standard Chinese. ''Hanyu'' () literally means 'Han Chinese, Han language'—that is, the Chinese language—while ''pinyin'' literally means 'spelled sounds'. Pinyin is the official romanization system used in China, Singapore, Taiwan, and by the United Nations. Its use has become common when transliterating Standard Chinese mostly regardless of region, though it is less ubiquitous in Taiwan. It is used to teach Standard Chinese, normally written with Chinese characters, to students in mainland China and Singapore. Pinyin is also used by various Chinese input method, input methods on computers and to lexicographic ordering, categorize entries in some Chinese dictionaries. In pinyin, each Chinese syllable is spelled in terms of an optional initial (linguistics), initial and a final (linguistics), final, each of which is represented by one or more letters. Initi ...
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