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Taigu District

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Taigu ( Chinese : 太谷 ; pinyin : Tàigǔ ) is a district of Shanxi province, China under the administration of Jinzhong City. It is administratively into three town-level entities ( Mingxing 明星镇, Hucun 胡村镇, and Fancun 范村镇), and six township-level entities ( Houcheng 侯城乡, Beiwang 北汪乡, Shuixiu 水秀乡, Yangyi 阳邑乡, Xiaobai 小白乡, and Rencun 任村乡). Taigu is linked to nearby Yuci in Jinzhong by rail via the Taigu Railway Stop.

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42-456: Taigu experiences a humid continental climate ( Köppen climate classification Dwa ). Spring is dry, with frequent dust storms , followed by early summer heat waves . Summer tends to be hot with most of the year's rainfall concentrated in July and August. Winter is long and cold, but dry and sunny. Downtown Taigu contains the local government institutions and buildings supporting the needs of

84-685: A Csa climate well inland to ensure hot summers and cold winters. They are generally found in the highly elevated areas of south-eastern Turkey ( Hakkâri ), north-western Iran, northern Iraq, parts of Central Asia , parts of the High Atlas mountain range in central Morocco and very small parts of the Intermountain West in the United States. This climate zone does not exist at all in the Southern Hemisphere, where

126-401: A component of traditional Chinese medicine with several various health benefits. 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

168-516: A marked reduction in wintry precipitation, which increases the chances of a wintertime drought ( w ). Snowfall occurs in all areas with a humid continental climate and in many such places is more common than rain during the height of winter. In places with sufficient wintertime precipitation, the snow cover is often deep. Most summer rainfall occurs during thunderstorms , and in North America and Asia an occasional tropical cyclone (or

210-474: A seat of a third order administration division. It lies southwest of Jinzhong and comprises nine administrative villages, eleven communities, with a total area of 22 square kilometres (8.5 sq mi). It has a total population of 60,500 people, of which 43,988 are urban dwellers. The language spoken by majority is Standard Manderin. The town is called "Mingxing" which means “Ming Star (Town)” or literally "Bright Star (Town)". There are numerous temples in

252-739: A subarctic climate. In the Southern Hemisphere , it exists in well-defined areas only in the Southern Alps of New Zealand , in the Snowy Mountains of Australia in Kiandra, New South Wales and the Andes Mountains of Argentina and Chile . Since climate regimes tend to be dominated by vegetation of one region with relatively homogenous ecology, those that project climate change remap their results in

294-526: A thermal profile, but because of semi-arid precipitation portions of it are grouped into the BSk category. In Europe , it is found in much of Central Europe : Germany (in the east and southeast part of the country), Austria (generally below 700 m (2,297 ft)), Poland , Czech Republic , Slovakia , Hungary (generally above 100 m (328 ft)), Croatia (mostly Slavonia region), in much of Eastern Europe : Ukraine (the whole country except

336-624: Is a site known as Cao's Courtyard Houses, a UNESCO World Heritage site tentative list of March 2008. The site occupies a total area of 10,600sq m (of which 6,384sq m are buildings), and contains Ming, Qing, and Republic of China era structures. 277 rooms are found in total across several multi-story buildings, halls, towers, and yards. The Cao Family Mansion is located just north of Beiwang . Additionally, Taigu also contains several halls, temples and structures of cultural significance. The Sanduo Hall in Beiwang has well-preserved stonework. Downtown

378-521: Is found in northern Kazakhstan , southern Siberia , parts of Mongolia , northern China , and highland elevations in the Koreas . Like its hot-summer counterpart, these climates are typically dry in the winter and bitterly cold due to the Siberian High (often with winter temperatures comparable to their nearby subarctic climates ), while summers are warm and long enough to avoid classification as

420-467: Is less extreme than the most inland hyper-continental variety. Using the Köppen climate classification , a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −3 °C [26.6 °F] and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). These temperatures were not arbitrary. In Europe,

462-565: Is less seasonally uniform in the west. The western states of the western United States (namely Montana , Wyoming , parts of southern Idaho , most of Lincoln County in Eastern Washington , parts of Colorado , parts of Utah , isolated parts of northern New Mexico , western Nebraska , and parts of western North and South Dakota ) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with

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504-724: Is linked to nearby Yuci in Jinzhong by rail via the Taigu Railway Station. However, residents traveling longer distances sometimes prefer simply to take the approximately one-hour drive to the provincial capital of Taiyuan where they can directly take high and low speed trains to Beijing and other major cities. There are three railway stations in Taigu District: The most famous tourist attractions in Taigu are examples of Shanxi Courtyard Houses . One of

546-724: Is noted during the autumn of deciduous forests. In the poleward direction, these climates transition into subarctic climates featuring short summers (and usually very cold winters) allowing only conifer trees. Moving equatorword, the hot-summer continental climates grade into humid subtropical climates (chiefly in North America and Asia) while the warm-summer continental climates grade into oceanic climates (chiefly in Europe), both of which have milder winters where average temperatures stay above 0°C (or -3°C). Some continental climates with lower precipitation (chiefly in Central Asia and

588-964: Is the Drum Tower. Just to the west of downtown Taigu in Mingxing one can visit the picturesque Northern Song dynasty Wubian Temple and White Tower Chinese pagoda (also known as the Boundless Pagoda). Also located in Taigu are the Ming dynasty Dacheng Hall of the Temple of Confucius, and Song dynasty Anchan Temple. Guanghua Temple in Baicheng Village is another common visitor attraction, as well as Jingxin Temple near Dongyangyi Village and Zhengsheng Temple in Fancun . The traditional foods of northern China are common in Taigu, including

630-701: Is to be found in northern China including Manchuria and parts of North China , south-east Russia , and over much of the Korean Peninsula ; it has the Köppen classification Dwa . Much of central Asia , northwestern China , and southern Mongolia has a thermal regime similar to that of the Dfa climate type, but these regions receive so little precipitation that they are more often classified as steppes ( BSk ) or deserts ( BWk ). Dsa climates are rare; they are generally restricted to elevated areas adjacent to mid-latitude Mediterranean climate regions with

672-698: The Black Sea coast), Belarus , Russia (mostly central part of European Russia ), south and central parts of the Nordic countries not bathed by the Atlantic Ocean or North Sea : Sweden (historical regions of Svealand and Götaland ), Denmark , Finland (south end, including the three largest cities ), Norway (most populated area), all Baltic States : Estonia , Latvia , Lithuania and also in parts of: Romania (generally above 100 m (328 ft)), Bosnia and Herzegovina , Turkey and in

714-482: The Cairngorm Mountains of Scotland , (generally above 100 m (328 ft)). It has little warming or precipitation effects from the northern Atlantic. The cool summer subtype is marked by mild summers, long cold winters and less precipitation than the hot summer subtype; however, short periods of extreme heat are not uncommon. Northern Japan has a similar climate. In Asia, this climate type

756-484: The Dfa climate type is present near the Black Sea in southern Ukraine , the Southern Federal District of Russia , southern Moldova , Serbia , parts of southern Romania , and Bulgaria , but tends to be drier and can be even semi-arid in these places. In East Asia, this climate exhibits a monsoonal tendency with much higher precipitation in summer than in winter, and due to the effects of

798-538: The Korean Peninsula , parts of Eastern Europe , parts of southern Ontario , much of the American Midwest , and the Northeast US , the climate combines hotter summer maxima and greater humidity (similar to those found in adjacent humid subtropical climates ) and moderately cold winters and more intermittent snow cover (averaging somewhat below freezing, too cold for a more temperate classification), and

840-563: The Nationalist government in the 1930s and 1940s, the compound contains examples of traditional courtyard-style living arrangements, temples, areas set aside for young women to separate them from young men, as well as a small exhibit detailing the life of Kung. The site is located in central Taigu just northwest of the Pangzhuang Reservoir off of 319 Sheng Dao road. Another example of Shanxi Courtyard Houses found in Taigu

882-591: The Canadian Prairie Provinces and below 40°N in the high Appalachians . In Europe, this subtype reaches its most northerly latitude in Bodø at the 67°N . High-altitude locations such as Flagstaff, Arizona , Aspen, Colorado and Los Alamos, New Mexico in the western United States exhibit local Dfb climates. The south-central and southwestern Prairie Provinces also fits the Dfb criteria from

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924-547: The Western United States) grade into semi-arid climates with similar temperatures but low precipitation. A hot summer version of a continental climate features an average temperature of at least 22 °C (71.6 °F) in its warmest month. Since these regimes are restricted to the Northern Hemisphere, the warmest month is usually July or August. High temperatures during the warmest month tend to be in

966-466: The broad preference for noodles over rice. Taigu itself is also known for several special kinds of food. Taigu Cake is well known in Shanxi and sometimes attributed as kind of Taiyuan food. This is a soft, sweet and moist kind of small baked cake made with a cake blank, sesame, and a sweet red bean filling, all topped with large amounts of sugar. Guilingji wine is produced locally and very popular as

1008-459: The classification symbol defines seasonal rainfall as follows: while the third letter denotes the extent of summer heat: Within North America, moisture within this climate regime is supplied by the Great Lakes , Gulf of Mexico and adjacent western subtropical Atlantic . Precipitation is relatively well distributed year-round in many areas with this climate ( f ), while others may see

1050-425: The continents either do not penetrate low enough in latitude or taper too much to have any place that gets the combination of snowy winters and hot summers. Marine influences are very strong around 40°S and such preclude Dfa , Dwa , and Dsa climates from existing in the southern hemisphere. Also known as hemiboreal climate , areas featuring this subtype of the continental climate have an average temperature in

1092-542: The district. Significant buildings include the Taigu People's Government Building, Taigu People's Court Building, and Taigu People's Procuratorate Building. While economic activity in the Taigu area is primarily agricultural, major non-agricultural industries in Taigu include production of malleable cast iron, cast steel, insulator fittings, radiator piping, and other small industrial components. Notable academic institutions include: Shanxi Agricultural University , on

1134-401: The form of climate regimes as an alternative way to explain expected changes. For a more comprehensive list, see Continental climate#List of locations with a continental climate . Mingxing, Shanxi Mingxing ( Chinese : 明星 ; pinyin : Míngxīng ) (formerly Taigu or Taiku ) is a town and township-level division and seat of Taigu County , Shanxi , China . It is

1176-776: The former site of the Ming Hsien schools established by the Oberlin Shansi Memorial Association , founded in 1907, and located on the eastern side of downtown Taigu, is one of the few remaining Chinese agricultural universities situated in a farming area, and Taigu Normal University . Taigu Senior High School is also regarded as one of the best in the region. The school includes boarding facilities for students attending from areas outside commuting range. The Shanxi Taigu Middle School , in eastern downtown Taigu, Taigu No. 2 Middle School , in northern downtown, and Taigu No. 3 Middle School , located in

1218-651: The freezing mark (too cold for such a classification). More extreme and inland humid continental climates, sometimes known as "hyper-continental" climates, are found in northeast China , southern Siberia , Mongolia , Kazakhstan , most of the southern interior of Canada , and the Upper Midwest , where temperatures in the winter resemble those of adjacent subarctic climates (with long, drier, generally very cold winters) but have longer and generally warmer summers (in occasional cases, hot summers). A more moderate variety, found in places like Honshu , east-central China,

1260-526: The high 20s to low 30s °C (80s °F), while average January afternoon temperatures are near or well below freezing. Frost-free periods typically last 4 to 7 months in this climate regime. Within North America , this climate includes portions of the central and eastern United States from east of 100°W to south of about the 44°N to the Atlantic . Precipitation increases further eastward in this zone and

1302-439: The humid continental climate covers a much larger area than the hot subtype. In North America, the climate zone covers from about 42°N to 50°N latitude mostly east of 100°W , including parts of Southern Ontario , the southern half of Quebec , The Maritimes , and Newfoundland , as well as the northern United States from eastern North Dakota east to Maine . However, it can be found as far north as 54°N , and further west in

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1344-582: The larger ocean area at that latitude, smaller land mass, and the consequent greater maritime moderation. In the Northern Hemisphere, some of the humid continental climates, typically in around Hokkaido , Sakhalin Island , northeastern mainland Europe , Scandinavia , Nova Scotia , and Newfoundland are closer to the sea and heavily maritime-influenced and comparable to oceanic climates , with relatively cool summers, significant year-round precipitation (including high amounts of snow) and winters being just below

1386-422: 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 intermittently throughout the winter months near the poleward or coastal margins, or persistently throughout

1428-492: The most known is Kong Family Compound, also known as the Former Kong Xiangxi Residence (designated as a Key Cultural Relic of Shanxi Province). This site is a well-preserved example of mid-Qing dynasty architecture typical of wealthy Chinese families during the period. Most recently occupied by H. H. Kung (transliterated by pinyin as "Kong Xiangxi"), a wealthy Chinese banker and politician active in

1470-467: 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 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition,

1512-537: The remnants thereof). Though humidity levels are often high in locations with humid continental climates, the "humid" designation means that the climate is not dry enough to be classified as semi-arid or arid . By definition, forests thrive within this climate. Biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous or evergreen forests, coniferous forests, and coniferous swamps. Within wetter areas, maple , spruce , pine , fir , and oak can be found. Fall foliage

1554-674: The southern portion of downtown, are also of locally significant size. Taigu also contains several vocational-track educational institutions, including the Shanxi Theater Career College , as well as the Shanxi Traffic Senior Vestibule School , both in downtown Taigu. Taigu is the site of People's Hospital No. 2, a large hospital serving the region. Downtown Taigu is served by many taxis for hire, as well as approximately six bus lines, designated T01 through T06. In addition, Taigu

1596-585: The steppe ( BSk ) climates. In the eastern and Midwestern United States, Pennsylvania , Ohio , Illinois , Indiana , southern New York , most of Connecticut and Rhode Island , and eastern Massachusetts fall into the hot-summer humid continental climate. In Canada, this climate type exists only over portions of Southern Ontario . In the Eastern Hemisphere, this climate regime is found within interior Eurasia and east-central Asia. Within Europe,

1638-488: The strong Siberian High much colder winter temperatures than similar latitudes around the world, however with lower snowfall, the exception being western Japan with its heavy snowfall. Tōhoku , between Tokyo and Hokkaidō and Western coast of Japan also has a climate with Köppen classification Dfa , but is wetter even than that part of North America with this climate type. A variant which has dry winters and hence relatively lower snowfall with monsoonal type summer rainfall

1680-435: The warmest month below 22 °C (72 °F). Summer high temperatures in this zone typically average between 21–28 °C (70–82 °F) during the daytime and the average temperatures in the coldest month are generally well or far below the −3 °C (27 °F) (or 0 °C (32.0 °F)) isotherm. Frost-free periods typically last 3–5 months. Heat spells lasting over a week are rare. The warm summer version of

1722-430: The winter months elsewhere in the climate zone. Humid continental climates are generally found between latitudes 40° N and 60° N , within the central and northeastern portions of North America , Europe , and Asia . Occasionally, they can also be found at higher elevations above other more temperate climate types. They are rare in the Southern Hemisphere , limited to isolated high altitude locations, due to

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1764-455: The −3 °C (27 °F) average temperature isotherm (line of equal temperature) was near the southern extent of winter snowpack . In the United States, it is more common to use the 0 °C [32.0 °F] isotherm instead. The 10 °C (50 °F) average temperature was found to be roughly the minimum temperature necessary for tree reproduction and growth. Wide temperature ranges are common within this climate zone. Second letter in

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