WordNet
- psychologically cool and unenthusiastic; unfriendly or unresponsive or showing dislike; "relations were cool and polite"; "a cool reception"; "cool to the idea of higher taxes"
- loose heat; "The air cooled considerably after the thunderstorm" (同)chill, cool down
- make cool or cooler; "Chill the food" (同)chill, cool down
- lose intensity; "His enthusiasm cooled considerably" (同)cool_off, cool down
- the quality of being at a refreshingly low temperature; "the cool of early morning"
- marked by calm self-control (especially in trying circumstances); unemotional; "play it cool"; "keep cool"; "stayed coolheaded in the crisis"; "the most nerveless winner in the history of the tournament" (同)coolheaded, nerveless
- (color) inducing the impression of coolness; used especially of greens and blues and violets; "cool greens and blues and violets"
- (used of a number or sum) without exaggeration or qualification; "a cool million bucks"
- fashionable and attractive at the time; often skilled or socially adept; "hes a cool dude"; "thats cool"; "Marys dress is really cool"; "its not cool to arrive at a party too early"
- neither warm nor very cold; giving relief from heat; "a cool autumn day"; "a cool room"; "cool summer dresses"; "cool drinks"; "a cool breeze"
- 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"
- speak softly or lovingly; "The mother who held her baby was cooing softly"
- the sound made by a pigeon
- cry softly, as of pigeons
- pigment mixed with water-soluble glutinous materials such as size and egg yolk (同)poster_paint, poster color, poster colour
- the process of becoming cooler; a falling temperature (同)chilling, temperature reduction
PrepTutorEJDIC
- 『涼しい』,ひんやりとする / 冷たい,(熱いものが)さめた / 『冷静な』沈着な・(態度・感情などが)『冷淡な』,冷ややかな・平気な,ずうずうしい・《話》(金額・数量などを強調して)掛け値なしの,正味の・《俗》《今はまれ》すぐれた・冷たい色の,寒色の・…'を'『冷やす』,涼しくする,さます・〈情熱・興奮・怒りなど〉'を'+『静める』,落ち着かせる・〈物・空間などが〉冷える,涼しくなる・〈興奮・怒りなどが〉さめる,収まる・涼しさ,涼しい時(場所) ・冷静さ
- (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
- クークー(キトの鳴き声,赤ちゃんの泣き声など) / 〈ハトが〉クークー鳴く / 〈恋人が〉むつ言(ごと)を言う / 〈恋人などが〉'を'やさそくささやく
- 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)』「2015/05/18 11:08:06」(JST)
[Wiki en表示]
The different geographical zones
World map with temperate zones highlighted in green
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Precipitation |
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- Snow grains
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- Air pollution
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- Meteorology
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Weather portal |
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In geography, temperate or tepid latitudes of Earth lie between the tropics and the polar regions.[1] The temperatures in these regions are generally relatively moderate, rather than extremely hot or cold, and the changes between summer and winter are also usually moderate.
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 Temperate climate zone is normally divided into two types of climates:
1)Temperate Continental climates (which include arid climates within the Temperate zone), are normally located between 35 or 40 and 55 north latitude on the eastern side or interior of the large landmasses in Asia, Europe, and North America (no Temperate Continental climates occur in the southern Hemisphere). In this climate zone, summers are warm (to hot in some areas), and winters often long, cold, and snowy (in the more humid sectors). [4][5][6]
2)Temperate Oceanic Climates are normally located between 45 and 58 north latitude on the west sides or west coastal areas of the large landmasses in Asia, Europe, North America, extreme South America, and South Island, New Zealand. In this climate zone, summers are cool, and winters are cool, but not cold, and there is little frozen precipitation at lower elevations. Located in the higher latitudes on the windward sides of landmass, some oceanic climates can have much cloudy and overcast skies.
The vast majority of the world's human population resides in temperate zones, especially in the northern hemisphere because of its greater mass of land.[7]
See also
- Geographical zone
- Middle latitudes
- Habitat (ecology)
- Polar circle
- Subtropics
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.
Seasons
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Temperate seasons |
- Spring
- Summer
- Autumn
- Winter
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Tropical climate seasons |
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Specific |
- Fog season
- Hurricane season
- Monsoon season
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Climate types under the Köppen climate classification
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Class A |
- Tropical rainforest (Af)
- Tropical monsoon (Am)
- Tropical savanna (Aw, As)
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Class B |
- Desert (BWh, BWk)
- Semi-arid (BSh, BSk)
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Class C |
- Humid subtropical (Cfa, Cwa)
- Oceanic (Cfb, Cwb, Cfc, Cwc)
- Mediterranean (Csa, Csb)
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Class D |
- Humid continental (Dfa, Dwa, Dfb, Dwb, Dsa, Dsb)
- Subarctic (Dfc, Dwc, Dfd, Dwd, Dsc, Dsd)
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Class E |
- Tundra (ET)
- Ice cap (EF)
- Alpine (ET, EF)
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UpToDate Contents
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English Journal
- Role of host and environment in mediating reduced gastrointestinal nematode infections in sheep due to intensive rotational grazing.
- Colvin AF, Walkden-Brown SW, Knox MR.SourceAnimal Science, School of Environmental and Rural Science, University of New England, Armidale, NSW, 2351, Australia.
- Veterinary parasitology.Vet Parasitol.2012 Mar 23;184(2-4):180-92. Epub 2011 Aug 25.
- We have previously reported marked reductions in faecal worm egg counts (WECs) and drenching frequency in sheep on an intensive rotational grazing system (IRG) in a cool temperate environment with summer-dominant rainfall. These experiments were designed to determine the role of the host and environ
- PMID 21924833
- Comparative Effect of Low Temperature on Virulence and Twitching Motility of Ralstonia solanacearum Strains Present in Florida.
- Bocsanczy AM, Achenbach UC, Mangravita-Novo A, Yuen JM, Norman DJ.AbstractABSTRACT Ralstonia solanacearum causes bacterial wilt on a wide range of plant hosts. Most strains of R. solanacearum are nonpathogenic below 20°C; however, Race 3 Biovar 2 (R3B2) strains are classified as quarantine pathogens because of their ability to infect crops, cause disease, and survive in temperate climates. We have identified race 1 biovar 1 Phylotype IIB Sequevar 4 strains present in Florida which were able to infect and produce wilt symptoms on potato and tomato at 18°C. Moreover they infected tomato plants at rates similar to strains belonging to R3B2. We determined that strains naturally nonpathogenic at 18°C were able to multiply, move in planta, and cause partial wilt when inoculated directly into the stem, suggesting that low temperature affects virulence of strains differently at early stages of infection. Bacterial growth in vitro was delayed at low temperatures, however it was not attenuated. Twitching motility observed on growing colonies was attenuated in nonpathogenic strains at 18°C, while not affected in the cool virulent ones. Using pilQ as a marker to evaluate the relative expression of the twitching activity of R. solanacearum strains, we confirmed that cool virulent strains maintained a similar level of pilQ expression at both temperatures, while in nonpathogenic strains pilQ was downregulated at 18°C.
- Phytopathology.Phytopathology.2012 Feb;102(2):185-94.
- ABSTRACT Ralstonia solanacearum causes bacterial wilt on a wide range of plant hosts. Most strains of R. solanacearum are nonpathogenic below 20°C; however, Race 3 Biovar 2 (R3B2) strains are classified as quarantine pathogens because of their ability to infect crops, cause disease, and survive i
- PMID 21936660
Japanese Journal
- Deposition and decomposition of cattle dung and its impact on soil properties and plant growth in a cool-temperate pasture
- Yoshitake Shinpei,Soutome Hiromi,Koizumi Hiroshi
- Ecological research 29(4), 673-684, 2014-07
- NAID 40020134928
- 林床におけるイワガラミとツルアジサイの直立茎形成場所と光環境
- 加藤 正吾,森戸 寛,花岡 創,小見山 章
- 森林立地 56(1), 49-54, 2014-06-25
- 付着根型つる植物2種(イワガラミ,ツルアジサイ)は登攀する際に樹幹表面という同じ資源を利用する。冷温帯の常緑針葉樹人工林下に0.45m×18mの調査プロットをもうけ, 2種の直立茎の形成場所の環境条件(光環境,土壌水分環境)による差異を明らかにすることを目的とした。林床において,イワガラミの分布は幅広い光環境に分布したが,ツルアジサイの分布はより明るい光環境に分布が偏っていた。付着根型つる植物2種 …
- NAID 110009839147
- Comparison of the diversity, composition, and host recurrence of xylariaceous endophytes in subtropical, cool temperate, and subboreal regions in Japan
- Ikeda Anzu,Matsuoka Shunsuke,Masuya Hayato [他]
- Population Ecology 56(2), 289-300, 2014-04
- NAID 40020048422
Related Links
- Welcome! We’ve recently moved… The Cool Temperate Nursery is now situated on Newtons Lane, Cossall, Notts, NG16 2YH. Its about 100 metres from the junction with the A6096, on the left and next to the private drive to Welltro ...
- tem·per·ate (tĕm′pər-ĭt, tĕm′prĭt) adj. 1. a. Of or occurring in the Temperate Zone: temperate regions; temperate species. b. Characterized by moderate temperatures, weather, or climate; neither hot nor cold. 2. a. Moderate in ...
Related Pictures
★リンクテーブル★
[★]
- 英
- cool temperate
- 関
- 冷温帯
[★]
- 英
- cool temperate
- 関
- 冷温
[★]
- 関
- chill、cold、cooling
[★]
- 関
- temperate zone、warm
[★]
- 関
- chill、cool