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Matsuyama, Ehime
270px, Matsuyama City Hall 270px, Ehime Prefectural Capital Building is the capital city of Ehime Prefecture, on the island of Shikoku, in Japan and is also Shikoku's largest city. , the city had an estimated population of 505,948 in 243,541 households and a population density of 1,200 persons per km2. The total area of the city is . Geography Matsuyama is located in central Ehime Prefecture, facing the Seto Inland Sea to the north, the mountains of the Takanawa Peninsula to the north and east, and the Saragamine Mountain Range, an extension of the Shikoku Mountains, to the south. It is located on the northeastern portion of the Dōgo Plain. The city also includes the Kutsuna Islands, an archipelago of 29 islands in the Seto Inland Sea. Neighbouring municipalities Ehime Prefecture * Imabari * Kumakōgen * Masaki * Tobe * Tōon Climate Matsuyama has a humid subtropical climate (Köppen climate classification ''Cfa''; Trewartha climate classification ''Cf'') with hot summe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Core Cities Of Japan
A is a class or category of cities of Japan, Japanese cities. It is a local administrative division created by the national government.Web-Japan.org"Local self-government", p. 3 retrieved 2012-11-28. Core cities are delegated many functions normally carried out by Prefectures of Japan, prefectural governments, but not as many as Cities designated by government ordinance of Japan, designated cities. To become a candidate for core city status, a city must have a population greater than 300,000 and an area greater than 100 square kilometers, although special exceptions may be made by order of the cabinet for cities with populations under 300,000 but over 200,000. After the abolition of Special cities of Japan, special city status on April 1, 2015, any city with a population above 200,000 may apply for core city status. Application for designation is made by a city with the approval of both the city and prefectural assemblies. History The term "core city" was created by the first c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shikoku Mountains
The Shikoku Mountains () are a mountain range that runs from east to west in the central part of the Shikoku in Japan. The length of the mountain range is about . The highest peak in the mountain range is Mount Ishizuchi. References {{coord missing, Japan Mountain ranges of Japan Geography of the Shikoku region ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shōtoku Taishi
Shōtoku may refer to: * Prince Shōtoku , also known as or , was a semi-legendary regent and a politician of the Asuka period in Japan who served under Empress Suiko. He was the son of Emperor Yōmei and his consort, Princess Anahobe no Hashihito, who was also Yōmei's younger half ... (574-622), a politician of the Asuka period * Empress Kōken, or Empress Shōtoku (718-770), the 48th imperial ruler of Japan * Shōtoku (era) (1711–1716), a Japanese era {{disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asuka Period
The was a period in the history of Japan lasting from 538 to 710, although its beginning could be said to overlap with the preceding Kofun period. The Yamato period, Yamato polity evolved greatly during the Asuka period, which is named after the Asuka, Yamato, Asuka region, about south of the modern city of Nara, Nara, Nara. The Asuka period is characterized by its significant Japanese art, artistic, social, and political transformations, having their origins in the late Kofun period. The introduction of Buddhism marked a change in Japanese society. The Asuka period is also distinguished by the change in the name of the country from to . Naming The term "Asuka period" was first used to describe a period in the history of Japanese fine-arts and architecture. It was proposed by fine-arts scholars and Okakura Kakuzō around 1900. Sekino dated the Asuka period as ending with the Taika Reform of 646. Okakura, however, saw it as ending with the transfer of the capital to the Heijō ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dōgo Onsen
is a hot spring in the city of Matsuyama, Ehime Prefecture on the island of Shikoku, Japan Japan is an island country in East Asia. Located in the Pacific Ocean off the northeast coast of the Asia, Asian mainland, it is bordered on the west by the Sea of Japan and extends from the Sea of Okhotsk in the north to the East China Sea .... History Dōgo Onsen is one of the oldest hot springs in Japan, with a history stretching back over 1000 years. The springs are mentioned in the Man'yōshū (written c. 759) and, according to legend, Prince Shōtoku (574–622) used to partake of the waters. Dōgo Onsen was the favorite retreat of writer Natsume Sōseki (1867–1916) when he was working near Matsuyama as a teacher in what was at the time rural Shikoku. In Soseki's loosely autobiographical novel '' Botchan'', the eponymous main character is a frequent visitor to the springs, the only place he likes in the area. Description Dōgo Onsen is famous for the Dōgo Onsen pub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iyo Province
was a Provinces of Japan, province of Japan in the area of northwestern Shikoku.Louis-Frédéric, Nussbaum, Louis-Frédéric. (2005). "''Tosa''" in . Iyo bordered on Sanuki Province to the northeast, Awa Province (Tokushima), Awa to the east, and Tosa Province, Tosa to the south. Its abbreviated form name was . In terms of the Gokishichidō system, Iyo was one of the provinces of the Nankaidō circuit. Under the ''Engishiki'' classification system, Iyo was ranked as one of the "upper countries" (上国) in terms of importance, and one of the "far countries" (遠国) in terms of distance from the capital. The kokufu, provincial capital was located in what is now the city of Imabari, Ehime, Imabari, but its exact location is still unknown. The ''ichinomiya'' of the province is the Ōyamazumi Shrine located on the island of Ōmishima in what is now part of Imabari. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Japan Meteorological Agency
The Japan Meteorological Agency (JMA; ''気象庁, Kishō-chō'') is a division of the Ministry of Land, Infrastructure, Transport and Tourism dedicated to the Scientific, scientific observation and research of natural phenomena. Headquartered in Minato, Tokyo the government agency, agency collects data on meteorology, hydrology, seismology, volcanology, and other related fields. The JMA is responsible for collecting and disseminating weather data and Forecasting, forecasts to the public, as well as providing specialized information for aviation and Marine weather forecasting, marine sectors. Additionally, the JMA issues warnings for volcanic eruptions and is integral to the nationwide Earthquake Early Warning (Japan), Earthquake Early Warning (EEW) system. As one of the Regional Specialized Meteorological Centers designated by the World Meteorological Organization (WMO), the JMA also Forecasting, forecasts, Tropical cyclone naming, names, and distributes warnings for tropical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trewartha Climate Classification
The Trewartha climate classification (TCC), or the Köppen–Trewartha climate classification (KTC), is a climate classification system first published by American geographer Glenn Thomas Trewartha in 1966. It is a modified version of the Köppen–Geiger system, created to answer some of its deficiencies. The Trewartha system attempts to redefine the middle latitudes to be closer to vegetation zoning and genetic climate systems. Scheme Trewartha's modifications to the 1884 Köppen climate system sought to reclass the middle latitudes into three groups, according to how many months have a mean temperature of or higher: * ''C'' (subtropical)—8 or more months; * ''D'' (temperate)—4 to 7 months; * ''E'' ( boreal climate)—1 to 3 months. The tropical climates and polar climates remained the same as in the original Köppen climate classification. The "highland" climate is ambiguously defined. Newer users of KTC generally omit this option. Group A: Tropical climates This is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Subtropical Climate
A humid subtropical climate is a subtropical -temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia) or oceanic climates (in other continents). It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classific ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tōon, Ehime
270px, Aerial view of Tōon city center is a city located in Ehime Prefecture, Japan. , the city had an estimated population of 33,276 in 15571 households and a population density of 160 persons per km2. The total area of the city is . The city name may be romanized as 'Toon', 'Tôon', 'Tōon' or 'Tohon'. Geography Tōon is located in central Ehime Prefecture on the island of Shikoku. It is the only city in Ehime Prefecture that does not face the sea. Located at the top of the alluvial fan of Dogo Plain, Toon is bordered on the east by Matsuyama, and with Saijō through a pass called Sakurasanri, with Kumakōgen to the south, and Imabari to the north. The Shigenobu River and its tributaries flow through the city, forming a small alluvial fan. Neighbouring municipalities Ehime Prefecture * Imabari * Kumakōgen *Matsuyama * Saijō Climate Tōon has a humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light snowfall. The average annual ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tobe, Ehime
example of Tobe ceramics is a town located in Iyo District, Ehime Prefecture, Japan. , the town had an estimated population of 20,485 in 9385 households and a population density of 200 persons per km2. The total area of the town is . Geography Tobe is almost in the center of Ehime Prefecture, across the Shigenobu River south of Matsuyama City. There are many mountains in the south, and the northern portion of the town occupies the southern tip of the Matsuyama Plain. The entire Tobe area is located on gentle hills. Surrounding municipalities Ehime Prefecture * Iyo * Kumakōgen * Masaki * Matsuyama * Uchiko Climate Tobe has a humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light snowfall. The average annual temperature in Tobe is 14.3 °C. The average annual rainfall is 1777 mm with September as the wettest month. The temperatures are highest on average in January, at around 25.4 °C, and lowest in January ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
