各种气候带英文说法

沿海气候 coastal climate
高地气候 highland climate
海洋气候 marine climate
森林气候 forest climate
温带气候 temperate climate
湿润气候 humid climate
温带草原气候 temperate grassy climate
山地气候 mountain climate
冬季季风气候 winter monsoon climate
季风气候 monsoon climate
亚热带气候 sub-tropical climate
高原气候 plateau climate
海滨气候 littoral climate
极地气候 polar climate
热带气候 tropical climate
温带沙漠气候 temperate desert climate
温带干燥气候 temperate arid climate
热带季风气候 tropical monsson climate
大陆气候 continental climate
沙漠气候 desert climate
An oceanic climate, also called marine west coast climate, European climate, maritime climate and Cascadian climate for K?ppen climate classification Cfb and subtropical highland for K?ppen Cfb or Cwb, is a type of climate typically found along the west coasts at the middle latitudes of some of the world's continents. This climate generally features warm, but not hot summers and cool, but not cold winters, with a narrow annual temperature range. It typically lacks a dry season, as precipitation is more evenly dispersed through the year. It is the predominant climate type across much of Europe, coastal northwestern North America, portions of southern South America and small areas of Africa, southeast Australia, New Zealand, as well as isolated locations elsewhere.
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Between October and May, Seattle is mostly or partly cloudy six out of every seven days[5]
Precipitation is both adequate and reliable throughout the year in oceanic climates, except in certain tropical highland areas, which would have tropical or humid subtropical climates (with a dry season in winter) if not for the high altitude making them cooler (Koppen Cwb). Under some variations of the Koeppen classification system, parts of the Pacific Northwest and south-central Chile are sometimes considered as having a Mediterranean climate (Koppen "Csb") due to a drying trend in the summer. However despite the "Csb" designation, these areas are generally considered oceanic as opposed to "Mediterranean".
Contents
[hide] 1 Properties 1.1 Precipitation
1.2 Temperature
2 Locations
3 Varieties 3.1 Subtropical highland variety (Cwb)
3.2 Subpolar variety (Cfc)
亚热带季风气候: Subtropical monsoon climate
温带大陆性湿润气候:Humid temperate continental climate
亚热带湿润气候:Subtropical humid climate
温带大陆性气候:Temperate continental climate
Similar climates in thermal range are also found in tropical highlands even at considerable distance from any coastline. Generally, they fall into K?ppen climate classification Cfb or Cwb.[3][4] The narrow range of temperatures results from the slight thermal range of temperatures between seasons characteristic of tropical lowlands. Altitudes are high enough that some places have at least one month cooler than 18 °C (64 °F) and do not qualify for grouping in the true tropical climates. This variation of the oceanic climate is termed “subtropical highland climate”. Unlike the norm in true oceanic climates, subtropical highland climates may have a marked winter drought. Agricultural potential in both oceanic climates and subtropical highland climates is similar.
In most areas with an oceanic climate, for the majority of the year precipitation comes in the form of rain. However during the winter, despite its C classification, the majority of areas with this climate see some snowfall annually. Outside of Australia, South Africa and tropical highland locations, most areas with an oceanic climate experiences at least one snowstorm per year. In the poleward locations of the oceanic climate zone (“subpolar oceanic climates”, described in greater detail below), snowfall is more frequent and commonplace.
3.3 Dry summers
4 See also
5 References
6 External links
[edit] Properties
Climates near the ocean generally have warm (but not hot) summers, and cool (but not cold) winters. They are characterized by a narrower annual range of temperatures than are encountered in other places at a comparable latitude, and generally do not have the extremely dry summers of Mediterranean climates.[1] Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents.[2]
For the influence of oceanic/maritime climates on viticulture, see maritime climate (wine).