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Komoro, Nagano
is a city located in Nagano Prefecture, Japan. , the city had an estimated population of 42,489 in 18776 households, and a population density of 430 persons per km². Its total area is . Geography Komoro is located in eastern Nagano Prefecture. The Chikuma River flows thorough the southern and western part of the city. Some extinct volcanic mountains are located between Komoro and neighboring Tsumagoi. The highest point in Komoro is Mt. Kurofu ( ja). Its peak is above sea level. The lowest point is . The old city center is at about . There are many slopes, so Komoro is known as a "hilly city" (坂の町). Surrounding municipalities *Nagano Prefecture **Saku ** Tōmi **Miyota *Gunma Prefecture ** Tsumagoi Climate Komoro is far from the sea and surrounded by mountains, so the rainfall is lower and diurnal temperature range is greater than many locations in Japan, and average annual temperature of Komoro is relatively cool because of the high altitude. The city has a climate ...
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Cities Of Japan
A is a local administrative unit in Japan. Cities are ranked on the same level as and , with the difference that they are not a component of . Like other contemporary administrative units, they are defined by the Local Autonomy Law of 1947. City status Article 8 of the Local Autonomy Law sets the following conditions for a municipality to be designated as a city: *Population must generally be 50,000 or greater (原則として人口5万人以上) *At least 60% of households must be established in a central urban area (中心市街地の戸数が全戸数の6割以上) *At least 60% of households must be employed in commerce, industry or other urban occupations (商工業等の都市的業態に従事する世帯人口が全人口の6割以上) *Any other conditions set by prefectural ordinance must be satisfied (他に当該都道府県の条例で定める要件を満たしていること) The designation is approved by the prefectural governor and the Minister for Internal ...
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Saku, Nagano
is a city located in Nagano Prefecture, Japan. , the city had an estimated population of 99,131 in 41,522 households, and a population density of 230 persons per km². The total area of the city is . Geography Saku is located in east-central Nagano Prefecture in the Saku Basin of the upper reaches of the Shinano River. The city claims the distinction of containing the point furthest from the sea within Honshu island (actually this point lies within the former town of Usuda). Since the opening of Sakudaira Station on the Nagano Shinkansen, many people commute to Tokyo, which is one hour away. Surrounding municipalities *Nagano Prefecture ** Komoro, Chino, Tōmi ** Minamisaku District: Sakuho **Kitasaku District: Karuizawa, Miyota, Tateshina *Gunma Prefecture ** Kanra District: Shimonita, Nanmoku Climate The city has a climate characterized by characterized by hot and humid summers, and relatively mild winters (Köppen climate classification ''Dwa''). The average annu ...
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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, to the Tok ...
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Sengoku Period
The was a period in History of Japan, Japanese history of near-constant civil war and social upheaval from 1467 to 1615. The Sengoku period was initiated by the Ōnin War in 1467 which collapsed the Feudalism, feudal system of Japan under the Ashikaga shogunate. Various samurai warlords and Japanese clans, clans fought for control over Japan in the power vacuum, while the emerged to fight against samurai rule. The Nanban trade, arrival of Europeans in 1543 introduced the arquebus into Japanese warfare, and Japan ended its status as a Tributary system of China, tributary state of China in 1549. Oda Nobunaga dissolved the Ashikaga shogunate in 1573 and launched a war of political unification by force, including the Ishiyama Hongan-ji War, until his death in the Honnō-ji Incident in 1582. Nobunaga's successor Toyotomi Hideyoshi completed his campaign to unify Japan and consolidated his rule with numerous influential reforms. Hideyoshi launched the Japanese invasions of Korea (159 ...
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Muromachi Period
The is a division of Japanese history running from approximately 1336 to 1573. The period marks the governance of the Muromachi or Ashikaga shogunate (''Muromachi bakufu'' or ''Ashikaga bakufu''), which was officially established in 1338 by the first Muromachi ''shōgun'', Ashikaga Takauji, two years after the brief Kenmu Restoration (1333–1336) of imperial rule was brought to a close. The period ended in 1573 when the 15th and last shogun of this line, Ashikaga Yoshiaki, was driven out of the capital in Kyoto by Oda Nobunaga. From a cultural perspective, the period can be divided into the Kitayama and Higashiyama cultures (later 15th – early 16th centuries). The early years from 1336 to 1392 of the Muromachi period are known as the '' Nanboku-chō'' or Northern and Southern Court period. This period is marked by the continued resistance of the supporters of Emperor Go-Daigo, the emperor behind the Kenmu Restoration. The Sengoku period or Warring States period, which begi ...
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Gokenin
A was initially a vassal of the shogunate of the Kamakura and the Muromachi periods.Iwanami Kōjien, "Gokenin" In exchange for protection and the right to become ''jitō'' (manor's lord), a ''gokenin'' had in times of peace the duty to protect the imperial court and Kamakura. In times of war, he had to fight with his forces under the shōgun’s flag. From the mid-13th century, the fact that ''gokenin'' were allowed to become ''de facto'' owners of the land they administered, coupled to the custom that all ''gokenin'' children could inherit, brought the parcelization of the land and a consequent weakening of the shogunate. The ''gokenin'' class ceased to be a significant force during the Muromachi period and was supplanted by the figure of the ''daimyō''. During the successive Edo period, the term finally came to indicate a direct vassal of the shōgun, below an , meaning that they did not have the right to an audience with the shōgun. Etymology The terms ''gokenin'' and ''ke ...
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Azuma Kagami
is a Japanese historical chronicle. The medieval text chronicles events of the Kamakura Shogunate from Minamoto no Yoritomo's rebellion against the Taira clan in Izokuni of 1180 to Munetaka Shinnō (the 6th shōgun) and his return to Kyoto in 1266.National Archives of JapanFeng, Wang The work is also called after the Later Hōjō family of Odawara (Kanagawa prefecture), in whose possession it used to be before it was donated to Tokugawa Ieyasu. It originally consisted of 52 chapters, but the 45th is lost. In spite of its many flaws, the document is considered the most important existing document concerning the Kamakura period. History The ''Azuma Kagami'' was compiled after 1266 under the directive of the Hōjō shikken (officially a regent to a shōgun, but the ''de facto'' ruler) and is a record in diary form of events occurring in Japan. Written in a Japanized version of classical Chinese known as , the massive work was incomprehensible to most Japanese until an edition w ...
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Kamakura Period
The is a period of Japanese history that marks the governance by the Kamakura shogunate, officially established in 1192 in Kamakura by the first ''shōgun'' Minamoto no Yoritomo after the conclusion of the Genpei War, which saw the struggle between the Taira and Minamoto clans. The period is known for the emergence of the samurai, the warrior caste, and for the establishment of feudalism in Japan. During the early Kamakura period, the shogunate continued warfare against the Northern Fujiwara which was only defeated in 1189. Then, the authority to the Kamakura rulers waned in the 1190s and power was transferred to the powerful Hōjō clan in the early 13th century with the head of the clan as regent (Shikken) under the shogun which became a powerless figurehead. The later Kamakura period saw the invasions of the Mongols in 1274 and again in 1281. To reduce the amount of chaos, the Hōjō rulers decided to decentralize power by allowing two imperial lines – Northern and Southern ...
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Tōsandō
is a Japanese geographical term. It means both an ancient division of the country and the main road running through it. It is part of the ''Gokishichidō'' system. It was situated along the central mountains of northern Honshu, specifically the Tōhoku region. This term also refers to a series of roads that connected the of each of the provinces that made up the region. The Tōsandō region encompasses eight ancient provinces. *Ōmi Province *Mino Province *Hida Province *Shinano Province *Kōzuke Province *Shimotsuke Province *Mutsu Province *Dewa Province After 711 AD, Tōsandō was understood to include the Musashi province. Nussbaum, Louis-Frédéric. (2005). "''Tōsandō''" in . See also * Comparison of past and present administrative divisions of Japan * Nakasendō (post-Sekigahara Tōsandō) * Sanriku, neighbouring region Notes References * Nussbaum, Louis-Frédéric and Käthe Roth. (2005) ''Japan encyclopedia.''Cambridge: Harvard University Press. OCLC 58053 ...
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Shinano Province
or is an old province of Japan that is now Nagano Prefecture. Shinano bordered on Echigo, Etchū, Hida, Kai, Kōzuke, Mikawa, Mino, Musashi, Suruga, and Tōtōmi Provinces. The ancient capital was located near modern-day Matsumoto, which became an important city of the province. The World War II–era Japanese aircraft carrier ''Shinano'' was named after this old province. Historical record In 713, the road that traverses Mino and Shinano provinces was widened to accommodate increasing numbers of travelers through the Kiso District of modern Nagano Prefecture. In the Sengoku period, Shinano Province was often split among fiefs and castle towns developed, including Komoro, Ina, and Ueda. Shinano was one of the major centers of Takeda Shingen's power during his wars with Uesugi Kenshin and others. Suwa taisha was designated as the chief Shinto shrine (''ichinomiya'') for the province.
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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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Diurnal Temperature Range
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 is an important factor in diurnal temperature variation: peak daily temperature generally occurs ''after'' noon, as air keeps net absorbing heat even after noon, and 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 to waist height. Incoming solar radiation exceeds outgoing heat energy for many hours afte ...
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