温和な、温帯の、(ウイルス)ンペレート

関: temperate zone、warm

WordNet

not extreme in behavior; "temperate in his habits"; "a temperate response to an insult"; "temperate in his eating and drinking"
(of weather or climate) free from extremes; mild; or characteristic of such weather or climate; "a temperate region"; "the temperate zones"; "temperate plants"
uncomfortable because of possible danger or trouble; "made things warm for the bookies"
get warm or warmer; "The soup warmed slowly on the stove" (同)warm_up
make warm or warmer; "The blanket will warm you"
(color) inducing the impression of warmth; used especially of reds and oranges and yellows; "warm reds and yellows and orange"
characterized by liveliness or excitement or disagreement; "a warm debate"
having or producing a comfortable and agreeable degree of heat or imparting or maintaining heat; "a warm body"; "a warm room"; "a warm climate"; "a warm coat"
of a seeker; near to the object sought; "youre getting warm"; "hot on the trail"
psychologically warm; friendly and responsive; "a warm greeting"; "a warm personality"; "warm support"
the colder parts of temperate waters
a rain forest in a temperate area
pigment mixed with water-soluble glutinous materials such as size and egg yolk (同)poster_paint, poster color, poster colour

PrepTutorEJDIC

(行動が)『節度のある』,節制のある / (土地・気候などが)『温和な』,温暖な
(気候が適度に)『暖かい』,温暖な / (飲み物などが適度に)『暖かい』,(衣服・場所などが)暖かく感じられる,(人が)暖まった,ほてる / 『心の暖かい』,思いやりのある;心からの,愛情のこもった / 熱した,激した,興奮した / (色が)暖かい,暖色(赤または黄を含む色)の / (獲物の遺臭・通った跡が)新しい,生々しい / 《話》(当て物ゲームなどで目的物に)近い,もう少しの / 『…‘を'暖める』,暖かくする《+up+名,+名+up》 / 〈人・心〉‘を'興奮させる,活気づける;〈人・心〉‘を'暖かい気持ちにする《+up+名,+名+up》 / 『暖まる』,暖かくなる《+up》 / 熱心になる,活気づく,興奮する《+up》 / (人・物に)優しくなる,好意を持つ《+to(toward)+名》 / 《a~》暖まること / 《the~》暖かい場所
テンペラ画[法](壁画などに水性絵の具を卵黄などで溶いて用いた画法) / テンペラ絵の具

Wikipedia preview

出典(authority):フリー百科事典『ウィキペディア（Wikipedia）』「2014/10/01 02:04:34」(JST)

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The different geographical zones

In geography, temperate or tepid latitudes of the globe lie between the tropics and the polar regions.^[1] The changes in these regions between summer and winter are generally relatively moderate, rather than extreme hot or cold.

However, in certain areas, such as Asia and central North America, the variations between summer and winter can be extreme because these areas are far away from the sea, causing them to have a continental climate. In regions traditionally considered tropical, localities at high altitudes (e.g. parts of the Andes) may have a temperate climate.

Zones and climate

The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arctic Circle (approximately 66.5° north latitude). The south temperate zone extends from the Tropic of Capricorn (approximately 23.5° south latitude) to the Antarctic Circle (at approximately 66.5° south latitude).^[2]^[3] The cooler parts of the temperate zone may be referred to as 'subtemperate'.

Temperate climate also broadly includes subtropical climate variants: subtropical semidesert/desert, humid subtropical, oceanic subtropical and Mediterranean climate. However, typically temperate climate is one of the world's four climate zones (besides the polar, subtropical, and tropical zones).

The maritime climate is affected by the oceans, which help to sustain somewhat stable temperatures throughout the year. In temperate zones the prevailing winds are from the west, thus the western edge of temperate continents most commonly experience this maritime climate. Such regions include Western Europe, and western North America at latitudes between 40° and 60° north (65°N in Europe).

Continental, semi-arid and arid are usually situated inland, with warmer summers and colder winters. Heat loss and reception are aided by extensive land mass. In North America, the Rocky Mountains act as a climate barrier to the maritime air blowing from the west, creating a semi-arid and continental climate to the east.^[4]^[5]^[6] In Europe, the maritime climate is able to stabilize inland temperature, because the major mountain range – the Alps – is oriented east-west (the area east of the long Scandinavian mountain range is an exception).

The vast majority of the world's human population resides in temperate zones (if defined as comprising the subtropics as well), especially in the northern hemisphere because of its greater mass of land.^[7]

References

^ Education Scotland. "Weather & climate Change Climates around the world". educationscotland.gov.uk.
^ McColl, R. W. (2005). Encyclopedia of World Geography, Volume 1. (Facts on File Library of World Geography). New York: Facts on File. p. 919. ISBN 0-816-05786-9.
^ "Solar Illumination: Seasonal and Diurnal Patterns". Encyclopedia.com. Retrieved October 4, 2012.
^ "Köppen Climate Classification: The Temperate Climate". The International Sustainability Council - Audubon. 2008. Retrieved July 6, 2014. "...the north-south aligned Rocky Mountains act as a climate barrier to the mild maritime air blowing from the west."
^ "Climate of Switzerland". Swiss University. Retrieved October 4, 2012. "The Alps act as a climate barrier: Southern Switzerland, which is mainly influenced by the Mediterranean Sea, is characterized by a much milder climate than Northern Switzerland."
^ Brinch, Brian (2007-11-01). "How mountains influence rainfall patterns". USA Today (Tysons Corner, Virginia: Gannett). ISSN 0734-7456. Retrieved October 4, 2012. "As air ascends mountains, such as the Washington Cascades, it is forced to rise. The rising air cools, condenses, and drops rain on locations situated on the windward slopes, like Seattle. When the air descends the back side of the mountain toward Spokane, it is compressed, warming and drying it out. This sinking, dry air produces a rain shadow, or area in the lee of a mountain with less rain and cloudcover."
^ Cohen, Joel E.; Christopher Small (November 24, 1998). "Hypsographic demography: The distribution of human population by altitude". Proceedings of the National Academy of Sciences of the United States of America, Vol. 95. Washington, D.C.: The Academy. pp. 14009–14014. Retrieved September 19, 2012.

UpToDate Contents

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English Journal

Distribution and evolutionary dynamics of Stowaway Miniature Inverted repeat Transposable Elements (MITEs) in grasses.

Minaya M, Pimentel M, Mason-Gamer R, Catalan P.SourceDepartmento de Ciencias Agrarias y del Medio Natural, Escuela Politécnica Superior Huesca, Universidad Zaragoza, Ctra. Cuarte km 1, 22071 Huesca, Spain. Electronic address: miguel.minay@gmail.com.
Molecular phylogenetics and evolution.Mol Phylogenet Evol.2013 Jul;68(1):106-18. doi: 10.1016/j.ympev.2013.03.005. Epub 2013 Mar 16.
The occurrence of Stowaway MITEs and their potential footprints in the grasses was assessed within an explicit phylogenetic framework. An organismal tree was used to analyze the distribution and evolutionary dynamics of these elements and their potential excision footprints in the fourth intron of t
PMID 23511216

Pigment production by a new thermotolerant microalga Coelastrella sp. F50.

Hu CW, Chuang LT, Yu PC, Chen CN.SourceInstitute of Marine Biology, National Sun Yat-sen University, Kaohsiung 804, Taiwan.
Food chemistry.Food Chem.2013 Jun 15;138(4):2071-8. doi: 10.1016/j.foodchem.2012.11.133. Epub 2012 Dec 27.
Microalgae are good crops to produce natural pigments because of their high growth rates. Tropical zones are better locations than temperate areas for microalgal cultivation because they have longer duration of daylight and more stable temperatures throughout the year, but the high temperatures pose
PMID 23497860

Reproductive Parameters of Female Macaca mulatta tcheliensis in the Temperate Forest of Mount Taihangshan, Jiyuan, China.

Tian JD, Wang ZL, Lu JQ, Wang BS, Chen JR.SourceInstitute of Biodiversity and Ecology, Zhengzhou University, Zhengzhou, China.
American journal of primatology.Am J Primatol.2013 Jun;75(6):605-12. doi: 10.1002/ajp.22147. Epub 2013 Mar 22.
The remaining population of Macaca mulatta tcheliensis, approximately 3,000 individuals, is currently confined to the southern region of Mount Taihangshan, northern China. Using data collected from February 2003 to November 2012, we examined female reproductive characteristics in a seasonally food s
PMID 23526654

Mobilome and genetic modification of bifidobacteria.

Guglielmetti S, Mayo B, Álvarez-Martín P.SourceDipartimento di Scienze e Tecnologie Alimentari e Microbiologiche, Sezione di Microbiologia Industriale, Università degli studi di Milano, Via Celoria 2, 20133 Milan, Italy.
Beneficial microbes.Benef Microbes.2013 Jun 1;4(2):143-66. doi: 10.3920/BM2012.0031.
Until recently, proper development of molecular studies in Bifidobacterium species has been hampered by growth difficulties, because of their exigent nutritive requirements, oxygen sensitivity and lack of efficient genetic tools. These studies, however, are critical to uncover the cross-talk between
PMID 23271067

Japanese Journal

Homegardens of the Cao Lan, a Tai-Speaking Ethnic Minority in Vietnam's Northern Mountains

Pijika Timsuksai,Nguyen Dinh Tien,Rambo A. Terry
Southeast Asian Studies 4(2), 365-383, 2015-08-27
… This structure is very different from the temperate type gardens of the Kinh in Vietnam with whom the Cao Lan share a common environment and are in frequent contact. …
NAID 110009929995

<Articles>Homegardens of the Cao Lan, a Tai-Speaking Ethnic Minority in Vietnam's Northern Mountains

Timsuksai Pijika,Tien Nguyen Dinh,Rambo A. Terry
Southeast Asian Studies 4(2), 365-383, 2015-08
… This structure is very different from the temperate type gardens of the Kinh in Vietnam with whom the Cao Lan share a common environment and are in frequent contact. …
NAID 120005649341

Mortality risk attributable to high and low ambient temperature: a multicountry observational study

Gasparrini Antonio,Guo Yuming,Hashizume Masahiro,Lavigne Eric,Zanobetti Antonella,Schwartz Joel,Tobias Aurelio,Tong Shilu,Rocklöv Joacim,Forsberg Bertil,Leone Michela,De Sario Manuela,Bell Michelle L,Guo Yue-Liang Leon,Wu Chang-fu,Kan Haidong,Yi Seung-Muk,de Sousa Zanotti Stagliorio Coelho Micheline,Saldiva Paulo Hilario Nascimento,Honda Yasushi,Kim Ho,Armstrong Ben
The Lancet 386(9991), 369-375, 2015-07-25
… The temperature percentile of minimum mortality varied from roughly the 60th percentile in tropical areas to about the 80-90th percentile in temperate regions. …
NAID 120005625364

Differences in hydrophyte life forms induce spatial heterogeneity of CH_4 production and its carbon isotopic signature in a temperate bog peatland

Itoh Masayuki,Shimamura Tetsuya,Ohte Nobuhito,Takemon Yasuhiro
Journal of Geophysical Research: Biogeosciences 120(6), 2015-07-14
To clarify the effect of differences in hydrophyte life forms on methane (CH_4) production and its carbon stable isotopic signature (δ_13C-CH_4), we analyzed CH4 and carbon dioxide (CO_2) concentratio …
NAID 120005624347

Related Pictures

★リンクテーブル★

リンク元	「温和」「warm」「温帯」「テンペレート」
拡張検索	「temperate phage」

「温和」

　　[★]

英: warm、temperate
関: 温帯、テンペレート、温かい、温める

「warm」

　　[★]

温かい、温和な、温める

関: temperate

「温帯」

　　[★]

英: temperate zone、temperate
関: 温和、テンペレート

「テンペレート」

　　[★]

英: temperate
関: 温和、温帯

「temperate phage」

　　[★]

英: temperate phage
同: 穏和なファージ、溶原性ファージ lysogenic phage
関: 形質導入、ラムダファージ

[1] Education Scotland. "Weather & climate Change Climates around the world". educationscotland.gov.uk.

[2] McColl, R. W. (2005). Encyclopedia of World Geography, Volume 1. (Facts on File Library of World Geography). New York: Facts on File. p. 919. ISBN 0-816-05786-9.

[3] "Solar Illumination: Seasonal and Diurnal Patterns". Encyclopedia.com. Retrieved October 4, 2012.

[4] "Köppen Climate Classification: The Temperate Climate". The International Sustainability Council - Audubon. 2008. Retrieved July 6, 2014. "...the north-south aligned Rocky Mountains act as a climate barrier to the mild maritime air blowing from the west."

[5] "Climate of Switzerland". Swiss University. Retrieved October 4, 2012. "The Alps act as a climate barrier: Southern Switzerland, which is mainly influenced by the Mediterranean Sea, is characterized by a much milder climate than Northern Switzerland."

[6] Brinch, Brian (2007-11-01). "How mountains influence rainfall patterns". USA Today (Tysons Corner, Virginia: Gannett). ISSN 0734-7456. Retrieved October 4, 2012. "As air ascends mountains, such as the Washington Cascades, it is forced to rise. The rising air cools, condenses, and drops rain on locations situated on the windward slopes, like Seattle. When the air descends the back side of the mountain toward Spokane, it is compressed, warming and drying it out. This sinking, dry air produces a rain shadow, or area in the lee of a mountain with less rain and cloudcover."

[7] Cohen, Joel E.; Christopher Small (November 24, 1998). "Hypsographic demography: The distribution of human population by altitude". Proceedings of the National Academy of Sciences of the United States of America, Vol. 95. Washington, D.C.: The Academy. pp. 14009–14014. Retrieved September 19, 2012.

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temperate