The Tristan da Cunha archipelago in the South Atlantic also has an oceanic climate. This variant of an oceanic climate is found in parts of coastal Iceland, the Faroe Islands, parts of Scotland, northwestern coastal areas of Norway such as Lofoten and reaching to 70°N on some islands,[18] uplands near the coast of southwestern Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle, the far south of Chile and Argentina, and a few highland areas of Tasmania, and the Australian and Southern Alps. An oceanic climate, also known as a maritime climate, marine climate, marine west coast climate or temperate oceanic climate, is the Köppen classification of climate typical of west coasts in higher middle latitudes of continents, and generally features cool summers (relative to their latitude) and cool but not cold winters, with a relatively narrow annual temperature range and few extremes of temperature. Ãle Amsterdam and Ãle Saint-Paul, both part of the French Southern and Antarctic Lands, are located in the subtropics and have an oceanic climate (akin to Tristan da Cunha; see above).
and JavaScript. They are often found on or near the west coast of continents; hence another name for Cfb, i.e.
This work was supported by the Atlantic Climate Change Program of NOAA's Climate and Global Change Program and by the National Science Foundaiton.
In the autumn, winter, and early spring, when the polar jet stream is most active, the frequent passing of marine weather systems creates the frequent fog, cloudy skies, and light drizzle often associated with oceanic climates.
Despite the oceanic-like thermal regimes, these areas are generally classified as steppe or desert climates.
J. Clim.
Temperatures there remain relatively constant throughout the year and snowfall is seldom seen. However, conifers such as spruce, pine, and cedar are also common in few areas, and fruits such as apples, pears, and grapes can often be cultivated here. ADS
In the hottest month, the average temperature is below 22 °C (72 °F), and at least four months feature average temperatures higher than 10 °C (50 °F). Nature 388, 521–522 (1997). Areas with subpolar oceanic climates feature an oceanic climate but are usually located closer to polar regions, or at higher altitudes.
A climate type similar to this exists in the Northern Tablelands and Central Tablelands region of New South Wales in Australia, with more uniform rainfall distribution, and would have characteristics of the Cfa climate. An example of this is Bodø, Norway, which like nearby Harstad has moderately cold, snowy winters and mild to warm summers making this somewhat of a cool summer version of a four-season climate.
Temperate oceanic climates, also known as "marine mild winter" climates[12] or simply oceanic climates, are found either at middle latitudes or in equatorial areas at higher altitudes. Molinari, R. et al.
[8] The climate is found in Tasmania, southern half of Victoria and southeastern New South Wales (southwards from Wollongong). With decreasing distance to the Mediterranean Sea, the oceanic climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe.
Most of France (away from the Mediterranean), Belgium, the Netherlands, Germany, Norway, the north coast of Spain (Basque Country, north of Navarre[7], Galicia, Asturias and Cantabria), the western Azores off the coast of Portugal, the south of Kosovo and southern portions of Sweden, also have oceanic climates. Locations with oceanic climates tend to feature cloudy conditions with precipitation, though it can experience clear, sunny days.
While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa.
Hurrell, J. W. Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation.
This climate is found on the Asian mainland in mountainous areas of the tropics, such as the foothills of the Himalayas and south-west China. cd pub/nature/curry_etal. Mountain summits of Scotland, both the North Island, and the South Island of New Zealand, the Alaskan Panhandle, Vancouver Island of Canada, Tasmania, Tierra del Fuego, and Patagonia experience the subpolar variety, meaning that they have moderate to cool summers, and snowy winters. A mild maritime climate is in existence in New Zealand.
It occurs in a few areas of Australia, namely in the southeast, although average high temperatures during summers there tend to be higher and the summers drier than is typical of oceanic climates, with summer maxima sometimes exceeding 40 °C (104 °F). You could also do it yourself at any point in time.
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