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Otog Banner
Otog Banner
Otog Banner
(Mongolian: ᠣᠲᠣᠭ ᠬᠣᠰᠢᠭᠤ Ото қосиу Otoɣ qosiɣu; Chinese: 鄂托克旗; pinyin: Ètuōkè Qí) is a banner of southwestern Inner Mongolia, People's Republic of China. It is under the administration of Ordos City, and borders Otog Front Banner to the southwest and Uxin Banner
Uxin Banner
to the southeast. Geography and climate[edit] Otog Banner
Otog Banner
is located in the southwest of Inner Mongolia
Inner Mongolia
and the west of Ordos City's administration, with a latitude range of 38° 18' to 40° 11' N and a longitude range of 106° 41' to 108° 54', spanning 209 kilometres (130 mi) north to south and 188 kilometres (117 mi) west to east
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Xincheng District, Hohhot
Xincheng may refer to:Contents1 People 2 Places2.1 Mainland China 2.2 Taiwan3 Art forms 4 See alsoPeople[edit]Tuoba Xincheng (拓拔新成), brother of Emperor Wencheng of Northern Wei; held the title of Prince You of Yangping Xincheng, one of the daughters of Emperor Taizong of Tang
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Chinese Language
Legend:   Countries identified Chinese as a primary, administrative, or native language   Countries with more than 5,000,000 Chinese speakers   Countries with more than 1,000,000 Chinese speakers   Countries with more than 500,000 Chinese speakers   Countries with more than 100,000 Chinese speakers   Major Chinese-speaking settlementsThis article contains IPA phonetic symbols. Without proper rendering support, you may see question marks, boxes, or other symbols instead of Unicode
Unicode
characters
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Geographic Coordinate System
A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols.[n 1] The coordinates are often chosen such that one of the numbers represents a vertical position, and two or three of the numbers represent a horizontal position
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List Of Current And Former Capitals Of Subnational Entities Of China
This is a list of the current and former capitals of country subdivisions of China. The history of China
China
and its administrative divisions is long and convoluted; hence, this chart will cover only capitals after the completion of the Mongol conquest of China
China
in 1279, because the modern province (sheng 省) was first created during the Mongol Yuan dynasty. A selection of country subdivisions and their capitals before 1279 can be found in the article History of the political divisions of China. Years may not line up perfectly during periods of turmoil (e.g. at the end of each dynasty). The list includes current and former provinces, as well as other first-level units that have been used over the course of China's recent history, such as autonomous regions, military command zones during the Qing dynasty, and so forth. Unless otherwise specified, a given administrative unit can be assumed to be a province with its present name
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Autonomous Regions Of China
ProvincesAutonomous regions Special
Special
administrative regionsSub-provincial levelSub-provincial citiesSub-provincial autonomous prefecturesSub-provincial city districtsPrefectural level (2nd) Prefectural citiesAutonomous prefecturesLeaguesPrefectures (abolishing)Sub-prefectural-levelSub-prefectural citiesProvincial-controlled citiesProvincial-controlled countiesProvincial-controlled districtsCounty level (3rd) CountiesAutonomous countiesCou
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Precipitation
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity.[2] The main forms of precipitation include drizzle, rain, sleet, snow, graupel and hail. Precipitation
Precipitation
occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and "precipitates". Thus, fog and mist are not precipitation but suspensions, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation
Precipitation
forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud
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Köppen Climate Classification
Köppen climate classification
Köppen climate classification
is one of the most widely used climate classification systems. It was first published by Russian German climatologist Wladimir Köppen
Wladimir Köppen
in 1884,[2][3] with several later modifications by Köppen, notably in 1918 and 1936.[4][5] Later, German climatologist Rudolf Geiger (1954, 1961) collaborated with Köppen on changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system.[6][7] The Köppen climate classification
Köppen climate classification
system has been further modified, within the Trewartha climate classification
Trewartha climate classification
system in the middle 1960s (revised in 1980)
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Cold Desert Climate
The Desert
Desert
climate (in the Köppen climate classification
Köppen climate classification
BWh and BWk, sometimes also BWn), also known as an arid climate, is a climate in which precipitation is too low to sustain any vegetation at all, or at most a very scanty shrub,[citation needed] and does not meet the criteria to be classified as a polar climate. An area that features this climate usually experiences from 25 to 200 mm (7.87 inches) per year of precipitation[1] and in some years may experience no precipitation at all. Averages may be even less such as in Arica, Chile, where precipitation normals annually stand at around 1 mm per year
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Pinyin
Hanyu Pinyin
Hanyu Pinyin
Romanization
Romanization
(simplified Chinese: 汉语拼音; traditional Chinese: 漢語拼音), often abbreviated to pinyin, is the official romanization system for Standard Chinese
Standard Chinese
in mainland China
China
and to some extent in Taiwan. It is often used to teach Standard Mandarin Chinese, which is normally written using Chinese characters. The system includes four diacritics denoting tones. Pinyin
Pinyin
without tone marks is used to spell Chinese names and words in languages written with the Latin alphabet, and also in certain computer input methods to enter Chinese characters. The pinyin system was developed in the 1950s by many linguists, including Zhou Youguang,[1] based on earlier form romanizations of Chinese
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Monsoon
Monsoon
Monsoon
(/mɒnˈsuːn/) is traditionally defined as a seasonal reversing wind accompanied by corresponding changes in precipitation,[1] but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea.[2][3] Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is sometimes incorrectly used for locally heavy but short-term rains,[4] although these rains meet the dictionary definition of monsoon.[5] The major monsoon systems of the world consist of the West
West
African and Asia-Australian monsoons
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Mongolian Language
монгол хэл ᠮᠣᠩᠭᠣᠯ ᠬᠡᠯᠡPronunciation /mɔŋɢɔ̆ɮ xeɮ/Native to MongoliaRegion All of state Mongolia
Mongolia
and Inner Mongolia, parts of Liaoning, Jilin, Heilongjiang, Xinjiang
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Autonomous Regions Of The People's Republic Of China
In development or moral, political, and bioethical philosophy, autonomy[1] is the capacity to make an informed, un-coerced decision. Autonomous organizations or institutions are independent or self-governing. Autonomy can also be defined from human resource perspective and it means a level of discretion granted to an employee in his or her work.[2] In such cases, autonomy is known to bring some sense of job satisfaction among the employees. Autonomy is a term that is also widely used and in the field of medicine
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China Standard Time
The time in China
China
follows a single standard time offset of UTC+08:00 (eight hours ahead of Coordinated Universal Time), despite China spanning five geographical time zones. The official national standard time is called Beijing
Beijing
Time (Chinese: 北京时间) domestically [1] and China
China
Standard Time (CST) internationally.[2] Daylight saving time has not been observed since 1991.[3] The special administrative regions (SARs) maintain their own time authorities, with standards called Hong Kong Time
Hong Kong Time
(香港時間) and Macau
Macau
Standard Time (澳門標準時間)
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Time Zone
A time zone is a region of the globe that observes a uniform standard time for legal, commercial, and social purposes. Time
Time
zones tend to follow the boundaries of countries and their subdivisions because it is convenient for areas in close commercial or other communication to keep the same time. Most of the time zones on land are offset from Coordinated Universal Time
Time
(UTC) by a whole number of hours ( UTC−12
UTC−12
to UTC+14), but a few zones are offset by 30 or 45 minutes (e.g. Newfoundland Standard Time is UTC−03:30, Nepal
Nepal
Standard Time
Time
is UTC+05:45, and Indian Standard Time
Time
is UTC+05:30). Some higher latitude and temperate zone countries use daylight saving time for part of the year, typically by adjusting local clock time by an hour
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Prefecture-level City
ProvincesAutonomous regions Special
Special
administrative regionsSub-provincial levelSub-provincial citiesSub-provincial autonomous prefectures Sub-provincial city
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