Oroshi Hocho Knives
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Oroshi Hocho Knives
is the Japanese term for a wind blowing strong down the slope of a mountain, occasionally as strong gusts of wind which can cause damage. ''Oroshi'' is a strong local wind across the Kanto Plain on the Pacific Ocean side of central Honshu. This term identifies a katabatic wind. Literary references The ''Oroshi'' wind is mentioned in Japanese poetry, including a poem which is included in the ''Hyakunin Isshu''.Mostow, Joshua S. (1996). Many versions of this poem which were published during the Edo period have ''yama-oroshi'' instead of ''yama-oroshi yo'', but the meaning is equivalent: the poet cries out to the wind; and he the cold down-draft to the heartless woman.Mostow, See also *Halny * Piteraq * Santa Ana winds * Williwaw Notes References * . (1969). , Vol. 20, No. 2, pp. 111–174, 126 Tokyo, Meteorological Research InstituteOCLC 1761858* Mostow, Joshua S., ed. (1996) ''Pictures of the Heart: The Hyakunin Isshu in Word and Image.''Honolulu: University of ...
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Kanto Plain
Kantō (Japanese) Kanto is a simplified spelling of , a Japanese word, only omitting the diacritics. In Japan Kantō may refer to: *Kantō Plain *Kantō region *Kantō-kai, organized crime group *Kanto (Pokémon), a geographical region in the ''Pokémon'' media franchise, named after the Japanese region of the same name Kantō is a festival held in Akita every year. *Akita Kanto (Japanese: 竿燈) In Northeast China or Manchuria Kantō may refer to the region of Jiandao (Japanese: 間島 ''Kantō'') in Manchuria, now known more commonly as Yanbian. Kantō (関東) is an alternate name for Northeast China or Manchuria used in the following: *Kwantung Army (Japanese: 関東軍 ''Kantōgun''), a unit of the Imperial Japanese Army *Kwantung Leased Territory (Japanese: 関東州 ''Kantōshū''), a Japanese possession in Northeastern China until the end of World War II Kanto (Italian) *Kanto (music) is a form of Italian theatre and opera popular in Turkey. *Kanto (comics), a ficti ...
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Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean
. '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc.
The centers of both the

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Honshu
, historically called , is the largest and most populous island of Japan. It is located south of Hokkaidō across the Tsugaru Strait, north of Shikoku across the Inland Sea, and northeast of Kyūshū across the Kanmon Straits. The island separates the Sea of Japan, which lies to its north and west, from the North Pacific Ocean to the south and east. It is the seventh-largest island in the world, and the second-most populous after the Indonesian island of Java. Honshu had a population of 104 million , constituting 81.3% of the entire population of Japan, and is mostly concentrated in the coastal areas and plains. Approximately 30% of the total population resides in the Greater Tokyo Area on the Kantō Plain. As the historical center of Japanese cultural and political power, the island includes several past Japanese capitals, including Kyōto, Nara and Kamakura. Much of the island's southern shore forms part of the Taiheiyō Belt, a megalopolis that spans several of the Japane ...
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Katabatic Wind
A katabatic wind (named from the Greek word κατάβασις ''katabasis'', meaning "descending") is a drainage wind, a wind that carries high-density air from a higher elevation down a slope under the force of gravity. Such winds are sometimes also called fall winds; the spelling catabatic winds is also used. Katabatic winds can rush down elevated slopes at hurricane speeds, but most are not that intense and many are 10 knots (18 km/h) or less. Not all downslope winds are katabatic. For instance, winds such as the föhn and chinook are rain shadow winds where air driven upslope on the windward side of a mountain range drops its moisture and descends leeward drier and warmer. Examples of true katabatic winds include the bora in the Adriatic, the Bohemian Wind or ''Böhmwind'' in the Ore Mountains, the Santa Ana in southern California, the piteraq winds of Greenland, and the oroshi in Japan. Another example is "the Barber", an enhanced katabatic wind that blows over t ...
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Hyakunin Isshu
is a classical Japanese anthology of one hundred Japanese ''waka'' by one hundred poets. ''Hyakunin isshu'' can be translated to "one hundred people, one poem ach; it can also refer to the card game of ''uta-garuta'', which uses a deck composed of cards based on the ''Hyakunin Isshu''. The most famous and standard version was compiled by Fujiwara no Teika (1162–1241) while he lived in the Ogura district of Kyoto. It is therefore also known as . Compilation One of Teika's diaries, the ''Meigetsuki'' (明月記), says that his son Tameie asked him to arrange one hundred poems for Tameie's father-in-law, Utsunomiya Yoritsuna, who was furnishing a residence near Mount Ogura; hence the full name of ''Ogura Hyakunin Isshu''. In order to decorate screens of the residence, Fujiwara no Teika produced the calligraphy poem sheets. Hishikawa Moronobu (1618–1694) provided woodblock portraits for each of the poets included in the anthology. Katsukawa Shunshō (1726–1793) designed ...
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Minamoto No Toshiyori
was an important and innovative Japanese poet, who compiled the ''Gosen Wakashū''. He was the son of Minamoto no Tsunenobu (1016–1097); holder of the second rank in court and of the position of Grand Counsellor). Shunrai was favored by Emperor Go-Sanjo and to a lesser degree Emperor Shirakawa; in no small part for political reasons. At this time, the Fujiwara family dominated the country, and its branch, the Rokujō family, similarly dominated the court poetry scene; by favoring their rivals, the Emperors could thus strike back. Although Shunrai was passed over to compile the ''Goshūi Wakashū''. Shunrai's angry polemical ''Nan Goshūi'' ("Errors in the ''Goshūishū''") appears to have somehow convinced Shirakawa to have Shunrai compile the next imperial anthology, the ''Kin'yō Wakashū''. This anthology, when completed, embroiled Shunrai in dispute, and his ''Gosen Wakashū'' was especially criticized with various uncomplimentary nicknames; Brower and Miner mention that ...
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Hanabusa Futen, The Wind Deity
Hanabusa (written: or ) is a Japanese surname. Notable people with the surname include: *Colleen Hanabusa Colleen Wakako Hanabusa ( ja, 花房 若子; born May 4, 1951) is an American lawyer and politician who served as the U.S. representative for from 2011 to 2015 and again from 2016 to 2019. A member of the Democratic Party, she ran for her party ... (born 1951), American politician *, Japanese painter, calligrapher, and haiku poet *, son and pupil of Hanabusa Itchō *, Japanese samurai *, Japanese photographer *, Japanese film director *, Japanese manga artist *, Japanese politician and diplomat *, Japanese actress {{surname Japanese-language surnames ...
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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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Halny
Halny is a foehn wind that blows in southern Poland and in Slovakia in the Tatra Mountains of the Carpathians. The most turbulent halny blows in Podhale region of southern Poland, coming from the south, down the slopes of the Tatra Mountains; in Slovakia, on the other side of the mountains, it comes from the north. Halny is a warm windstorm that blows through the valleys. It is often disastrous; ripping off roofs, causing avalanches and, according to some people, can have some influence on mental states. Most halny occur in October and November, sometimes in February and March, rarely in other months. In May 1968 a destructive halny known as ''Wind of the Century'' where winds reportedly reached 288 km/h, destroyed large areas of forestry in southern Poland. See also *Oroshi References Notes #{{note, a A note attempting to provide the English comprehension of ''halny'', which lacks a one-word translation: ''Halny'' is a singular masculine noun in Polish (plural: ''halne'') when ...
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Piteraq
A piteraq is a cold katabatic wind which originates on the Greenlandic icecap and sweeps down the east coast. The word "piteraq" means "that which attacks you" in the local language.Danish Meteorological InstituteThe Observed Climate of Greenland, 1958–99 p. 96 Piteraqs are most common in the autumn and winter. Wind speeds typically reach 50 to 80 m/s (180–288 km/h; 111–178 mph). The Greenland ice sheet cools the air directly above it. Colder air is denser and it sinks, forming a separate layer of cold air in between warmer air. A piteraq is triggered by low pressure systems off the east coast of Greenland. Piteraqs do not only affect coastal towns, but also large areas of sea to the east of Greenland. On February 6, 1970 at about 6:00 PM, the community of Tasiilaq was hit by the worst documented piteraq ever in Greenland (estimated at 90 m/s — about 325 km/h or 200 mph) (Stronger than a category five Atlantic hurricane) causing severe damage.''ibid.'', p ...
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Santa Ana Winds
The Santa Ana winds (sometimes devil winds) "Scholars who have looked into the name's origins generally agree that it derives from Santa Ana Canyon, the portal where the Santa Ana River -- as well as a congested Riverside (CA-91) Freeway -- leaves Riverside County and enters Orange County. When the Santa Anas blow, winds can reach exceptional speeds in this narrow gap between the Puente Hills and Santa Ana Mountains." are strong, extremely dry downslope winds that originate inland and affect coastal Southern California and northern Baja California. They originate from cool, dry high-pressure air masses in the Great Basin. Santa Ana winds are known for the hot, dry weather that they bring in autumn (often the hottest of the year), but they can also arise at other times of the year. They often bring the lowest relative humidities of the year to coastal Southern California, and “beautifully clear skies.” These low humidities, combined with the warm, compressionally-heated air ...
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