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Shimizu, Shizuoka
is a town in Suntō District of Shizuoka Prefecture, Japan. , the town had an estimated population of 32,453 in 14058 households, and a population density of 3,700 persons per km2. The total area of the town was . Geography Shimizu is located at the northern end of Izu Peninsula. Both the Kakita River and the Kano River flow through the town. The area has a temperate maritime climate with hot, humid summers and mild, cool winters. Neighboring municipalities *Shizuoka Prefecture **Numazu ** Mishima **Nagaizumi Demographics Per Japanese census data, the population of Shimizu has been increasing over the past 70 years. Climate The city has a climate characterized by hot and humid summers, and relatively mild winters (Köppen climate classification ''Cfa''). The average annual temperature in Shimizu is 15.8 °C. The average annual rainfall is 1925 mm with September as the wettest month. The temperatures are highest on average in August, at around 26.6 °C ...
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Towns Of Japan
A town (町; ''chō'' or ''machi'') is a local administrative unit in Japan. It is a local public body along with prefecture (''ken'' or other equivalents), city (''shi''), and village (''mura''). Geographically, a town is contained within a district. Note that the same word (町; ''machi'' or ''chō'') is also used in names of smaller regions, usually a part of a ward in a city. This is a legacy of when smaller towns were formed on the outskirts of a city, only to eventually merge into it. Towns See also * Municipalities of Japan * Japanese addressing system The Japanese addressing system is used to identify a specific location in Japan. When written in Japanese characters, addresses start with the largest geographical entity and proceed to the most specific one. When written in Latin alphabet, Lati ... References {{reflist External links "Large_City_System_of_Japan";_graphic_shows_towns_compared_with_other_Japanese_city_types_at_p._1_[PDF_7_of_40/nowiki>">DF_7_of_ ...
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Population Density
Population density (in agriculture: Stock (other), standing stock or plant density) is a measurement of population per unit land area. It is mostly applied to humans, but sometimes to other living organisms too. It is a key geographical term.Matt RosenberPopulation Density Geography.about.com. March 2, 2011. Retrieved on December 10, 2011. In simple terms, population density refers to the number of people living in an area per square kilometre, or other unit of land area. Biological population densities Population density is population divided by total land area, sometimes including seas and oceans, as appropriate. Low densities may cause an extinction vortex and further reduce fertility. This is called the Allee effect after the scientist who identified it. Examples of the causes of reduced fertility in low population densities are * Increased problems with locating sexual mates * Increased inbreeding Human densities Population density is the number of people pe ...
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Meiji Period
The is an era of Japanese history that extended from October 23, 1868 to July 30, 1912. The Meiji era was the first half of the Empire of Japan, when the Japanese people moved from being an isolated feudal society at risk of colonization by Western powers to the new paradigm of a modern, industrialized nation state and emergent great power, influenced by Western scientific, technological, philosophical, political, legal, and aesthetic ideas. As a result of such wholesale adoption of radically different ideas, the changes to Japan were profound, and affected its social structure, internal politics, economy, military, and foreign relations. The period corresponded to the reign of Emperor Meiji. It was preceded by the Keiō era and was succeeded by the Taishō era, upon the accession of Emperor Taishō. The rapid modernization during the Meiji era was not without its opponents, as the rapid changes to society caused many disaffected traditionalists from the former samurai ...
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Edo Period
The or is the period between 1603 and 1867 in the history of Japan, when Japan was under the rule of the Tokugawa shogunate and the country's 300 regional '' daimyo''. Emerging from the chaos of the Sengoku period, the Edo period was characterized by economic growth, strict social order, isolationist foreign policies, a stable population, perpetual peace, and popular enjoyment of arts and culture. The period derives its name from Edo (now Tokyo), where on March 24, 1603, the shogunate was officially established by Tokugawa Ieyasu. The period came to an end with the Meiji Restoration and the Boshin War, which restored imperial rule to Japan. Consolidation of the shogunate The Edo period or Tokugawa period is the period between 1603 and 1867 in the history of Japan, when Japan was under the rule of the Tokugawa shogunate and the country's regional '' daimyo''. A revolution took place from the time of the Kamakura shogunate, which existed with the Tennō's court, t ...
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Tokugawa Shogunate
The Tokugawa shogunate (, Japanese 徳川幕府 ''Tokugawa bakufu''), also known as the , was the military government of Japan during the Edo period from 1603 to 1868. Nussbaum, Louis-Frédéric. (2005)"''Tokugawa-jidai''"in ''Japan Encyclopedia'', p. 978.Nussbaum"''Edo-jidai''"at p. 167. The Tokugawa shogunate was established by Tokugawa Ieyasu after victory at the Battle of Sekigahara, ending the civil wars of the Sengoku period following the collapse of the Ashikaga shogunate. Ieyasu became the ''shōgun,'' and the Tokugawa clan governed Japan from Edo Castle in the eastern city of Edo (Tokyo) along with the ''daimyō'' lords of the ''samurai'' class.Nussbaum"Tokugawa"at p. 976. The Tokugawa shogunate organized Japanese society under the strict Tokugawa class system and banned most foreigners under the isolationist policies of '' Sakoku'' to promote political stability. The Tokugawa shoguns governed Japan in a feudal system, with each ''daimyō'' administering a '' han'' ...
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Tenryō
The Tokugawa shogunate (, Japanese 徳川幕府 ''Tokugawa bakufu''), also known as the , was the military government of Japan during the Edo period from 1603 to 1868. Nussbaum, Louis-Frédéric. (2005)"''Tokugawa-jidai''"in ''Japan Encyclopedia'', p. 978.Nussbaum"''Edo-jidai''"at p. 167. The Tokugawa shogunate was established by Tokugawa Ieyasu after victory at the Battle of Sekigahara, ending the civil wars of the Sengoku period following the collapse of the Ashikaga shogunate. Ieyasu became the ''shōgun,'' and the Tokugawa clan governed Japan from Edo Castle in the eastern city of Edo (Tokyo) along with the ''daimyō'' lords of the ''samurai'' class.Nussbaum"Tokugawa"at p. 976. The Tokugawa shogunate organized Japanese society under the strict Tokugawa class system and banned most foreigners under the isolationist policies of ''Sakoku'' to promote political stability. The Tokugawa shoguns governed Japan in a feudal system, with each ''daimyō'' administering a '' han'' (feud ...
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Suruga Province
was an old province in the area that is today the central part of Shizuoka Prefecture. Suruga bordered on Izu, Kai, Sagami, Shinano, and Tōtōmi provinces; and was bordered by the Pacific Ocean through Suruga Bay to the south. Its abbreviated form name was . History Early period Suruga was one of the original provinces of Japan established in the Nara period under the Taihō Code. The original capital of the province was located in what is now Numazu, which also had the ''Kokubun-ji'' and the Ichinomiya ( Mishima Taisha) of the province. Under the '' Engishiki'' classification system, Suruga was ranked as a "major country" (上国), and was governed by a '' Kuni no miyatsuko'' and under the ''ritsuryō'' system was classed as a "middle country" (中国) In a 680 AD cadastral reform, the districts forming Izu Province were administratively separated from Suruga, and the provincial capital was relocated to the right bank of the Abe River in what is now Shizuoka City. ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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'' indi ...
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Nagaizumi, Shizuoka
270px, Nagaizumi Town Hall is a town located in Suntō District, Shizuoka Prefecture, Japan. , the town had an estimated population of 43,568 in 18154 households and a population density of 1,600 persons per km². The total area of the town was . Geography Nagaizumi is located in east-central Shizuoka Prefecture, south of Mount Fuji, and north of Izu Peninsula. The area has a temperate maritime climate with hot, humid summers and mild, cool winters. Neighboring municipalities *Shizuoka Prefecture ** Mishima **Numazu **Susono **Fuji ** Shimizu Demographics Per Japanese census data, the population of Nagaizumi has been increasing rapidly over the past 60 years. Climate The city has a climate characterized by hot and humid summers, and relatively mild winters (Köppen climate classification ''Cfa''). The average annual temperature in Nagaizumi is 14.1 °C. The average annual rainfall is 1945 mm with September as the wettest month. The temperatures are highest on av ...
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Mishima, Shizuoka
Mishima City Hall is a city located in eastern Shizuoka Prefecture, Japan. , the city had an estimated population of 109,803 in 49,323 households, and a population density of 1800 persons per km². The total area of the city is . Geography Mishima is located in far eastern Shizuoka Prefecture, at the northern end of Izu Peninsula and in the foothills of Mount Fuji. Surrounding municipalities *Shizuoka Prefecture **Numazu **Susono ** Kannami ** Shimizu ** Nagaizumi *Kanagawa Prefecture **Hakone Demographics Per Japanese census data, the population of Mishima has remained stable over the past 25 years. Climate Mishima has a humid subtropical climate (Köppen climate classification ''Cfa'') with hot summers and cool winters. Precipitation is significant throughout the year, but is heaviest from June to September. The average annual temperature in Mishima is . The average annual rainfall is with September as the wettest month. The temperatures are highest on average in Augu ...
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Numazu, Shizuoka
is a city located in eastern Shizuoka Prefecture, Japan. , the city had an estimated population of 189,486 in 91,986 households, and a population density of 1,014 persons per km2. The total area of the city is . Geography Numazu is at the northwestern end of the Izu Peninsula, which is a leisure destination known for its numerous hot springs. Mount Fuji, Japan's tallest mountain, may also be seen from Numazu on clear days. Numazu is located west of Tokyo and is on the Tōkaidō Main Line, the main railway line from Osaka to Tokyo. Warmed by the Kuroshio Current, the area enjoys a warm maritime climate with hot, humid summers and mild, cool winters. The Kano River runs through the middle of the city. Mount Ashitaka (1188 meters) is the highest point in the city Neighboring municipalities Shizuoka Prefecture * Mishima *Fuji * Izu * Izunokuni * Shimizu * Nagaizumi * Kannami Demographics Per Japanese census data, the population of Numazu has been in slow decline over the past 30 ...
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Maritime Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. ...
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