Oceanic climate

Last updated

Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found. Koppen World Map Cfb Cfc Cwb Cwc.png
Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found.

An oceanic climate, also known as a marine climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates, represented as Cwb or Cfb, and subpolar oceanic or cold subtropical highland climates, represented as Cfc or Cwc. Subtropical highland climates occur in some mountainous parts of the subtropics or tropics, some of which have monsoon influence, while their cold variants and subpolar oceanic climates occur near polar or tundra regions.

Contents

Precipitation

Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the regions, but are more common in subtropical highland climates where these air masses meet more frequently due to the influence of hotter weather in the subtropics or tropics, especially in monsoon-influenced climates. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. Most oceanic climate zones, however, experience at least one snowfall per year. Snowfall is more frequent and commonplace in the subpolar oceanic climates due to the colder weather in those locations.

Temperature

Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature. In the Köppen climate classification, oceanic climates have a mean temperature of 0 °C (32 °F) or higher (or −3 °C (27 °F) or higher) in the coldest month, compared to continental climates where the coldest month has a mean temperature of below 0 °C (32 °F) (or −3 °C (27 °F)) in the coldest month. Summers are warm but not hot, with the warmest month having a mean temperature below 22 °C (72 °F). Poleward of the latter is a subtype of it and is the subpolar oceanic climate (Köppen Cfc), [1] with long but relatively mild (for their latitude) winters and cool and short summers (average temperatures of at least 10 °C (50 °F) for one to three months). Examples of this climate include parts of coastal Iceland, the coast of Norway north of Bodø, the Scottish Highlands, the mountains of Vancouver Island, and Haida Gwaii in Canada, in the Northern Hemisphere and extreme southern Chile in the Southern Hemisphere (examples include Punta Arenas), the Tasmanian Central Highlands, and parts of New Zealand.

Cause

Oceanic climates are not necessarily found in coastal locations on the aforementioned parallels; however, in most cases oceanic climates parallel higher middle latitude oceans.[ clarification needed ] The polar jet stream, which moves in a west to east direction across the middle latitudes, advances low pressure systems, storms, and fronts. In coastal areas of the higher middle latitudes (45–60° latitude), the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the cool ocean adjacent to them. 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. They are typically found poleward of Mediterranean climates, except in Australia where they are poleward of both such climates and humid subtropical climates due to the shape of the continent. Only in Europe do they penetrate far inland, where they eventually transition into warm-summer humid continental climates; in other continents, they are blocked by a large mountain range or limited by nearby oceans.

The North Atlantic Gulf Stream, a tropical oceanic current that passes north of the Caribbean and up the East Coast of the United States to North Carolina, then heads east-northeast to the Grand Banks of Newfoundland, is thought to greatly modify the climate of northwest Europe. [2] As a result of the North Atlantic Current, west coast areas located in high latitudes like Ireland, the UK, and Norway have much milder winters (for their latitude) than would otherwise be the case. The lowland attributes of western Europe also help drive marine air masses into continental areas, enabling cities such as Dresden, Prague, and Vienna to have maritime climates in spite of being located well inland from the ocean.

Locations

Europe

Climate chart (explanation)
JFMAMJJASOND
 
 
67
 
 
6
1
 
 
55
 
 
7
1
 
 
52
 
 
10
3
 
 
40
 
 
14
5
 
 
54
 
 
18
9
 
 
65
 
 
20
11
 
 
82
 
 
23
14
 
 
99
 
 
22
13
 
 
84
 
 
19
11
 
 
87
 
 
15
8
 
 
85
 
 
10
5
 
 
82
 
 
7
2

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: Royal Netherlands Meteorological Institute [3]

Imperial conversion
JFMAMJJASOND
 
 
2.6
 
 
43
34
 
 
2.2
 
 
44
34
 
 
2
 
 
50
37
 
 
1.6
 
 
58
41
 
 
2.1
 
 
64
47
 
 
2.6
 
 
69
52
 
 
3.2
 
 
73
56
 
 
3.9
 
 
72
56
 
 
3.3
 
 
67
52
 
 
3.4
 
 
58
46
 
 
3.4
 
 
50
40
 
 
3.2
 
 
44
35

Average max. and min. temperatures in °F

Precipitation totals in inches

Oceanic climates in Europe occupy a large stretch of land, from Norway's Atlantic coast and the British Isles, southeast to some parts of Turkey.

Western Europe is almost exclusively oceanic between 45°N to 55°N; including most of France (away from the Mediterranean), nearly all of Belgium, the Netherlands, Austria, most of Luxembourg, most of Denmark, western Germany, northwestern Switzerland, south coast and western areas of Norway north to Skrova and extreme southern Sweden.

While most of Southern Europe is climatically Mediterranean, some parts of Southern Europe also have oceanic climates. However, these instances of the climate are highly variable, and often somewhat anomalous. The north coast of Spain, the western Azores off the coast of Portugal are too wet in summer to be Mediterranean, and too mild in summer to be humid subtropical, though they often have winter means above 9 °C (48 °F), unusual for European oceanic climates.

Another anomalous case can be found in northwestern Turkey, including northern Istanbul. These places are, in a strict air-mass sense, not oceanic: they are affected by southerlies directly from the Mediterranean, and polar intrusions from Siberia. [4] Yet their position near the Black Sea makes them too wet in summer to be Mediterranean, too mild during winter to be humid continental, and not hot enough in summer to be humid subtropical; therefore Köppen classifies them as oceanic. Despite their anomalous position, however, their temperatures, around 4–5 °C (39–41 °F) in winter and 20–22 °C (68–72 °F) in summer, are not wholly atypical for European oceanic climates.

Some Eastern European regions such as the north of Croatia and Serbia and some parts of the Czech Republic, also have oceanic climates; these are generally near the boundary for being humid continental.

The line between oceanic and continental climates in Europe runs in a generally north to south direction. For example, western Germany is more impacted by milder Atlantic air masses than eastern Germany. Thus, winters across Europe become colder to the east, and (in some locations) summers become hotter. The line between oceanic Europe and Mediterranean Europe normally runs west to east and is related to changes in precipitation patterns and differences to seasonal temperatures; although intrusions of polar air, remnants of marine air-masses, and higher summer precipitation can create oceanic climates in Eastern Europe and transcontinental regions as far south as 40°N.[ citation needed ]

The Americas

Climate chart (explanation)
JFMAMJJASOND
 
 
179
 
 
7
3
 
 
184
 
 
8
3
 
 
156
 
 
11
5
 
 
118
 
 
14
7
 
 
87
 
 
17
10
 
 
70
 
 
20
12
 
 
53
 
 
22
14
 
 
51
 
 
22
14
 
 
73
 
 
19
12
 
 
148
 
 
14
8
 
 
239
 
 
9
5
 
 
231
 
 
7
3

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: Environment Canada

Imperial conversion
JFMAMJJASOND
 
 
7
 
 
44
37
 
 
7.2
 
 
47
38
 
 
6.1
 
 
51
40
 
 
4.6
 
 
56
44
 
 
3.4
 
 
62
49
 
 
2.8
 
 
67
54
 
 
2.1
 
 
72
57
 
 
2
 
 
72
58
 
 
2.9
 
 
66
53
 
 
5.8
 
 
57
47
 
 
9.4
 
 
49
41
 
 
9.1
 
 
44
37

Average max. and min. temperatures in °F

Precipitation totals in inches

The oceanic climate exists in an arc spreading across the northwestern coast of North America from the Alaskan panhandle to northern Washington. In addition, some east coast areas such as Block Island, Cape Cod, Martha's Vineyard, and Nantucket have a similar climate. [5] An extensive area of oceanic climates distinguishes the coastal regions of southern Chile and extends into bordering Argentina.

Africa

The only noteworthy area of maritime climate at or near sea-level within Africa is in South Africa from Mossel Bay on the Western Cape coast to Plettenberg Bay (the Garden Route), with additional pockets of this climate inland of the Eastern Cape and KwaZulu-Natal coast. It is usually warm most of the year with no pronounced rainy season, but slightly more rain in autumn and spring. The Tristan da Cunha archipelago in the South Atlantic also has an oceanic climate.

Asia and Oceania

Climate chart (explanation)
JFMAMJJASOND
 
 
37
 
 
23
12
 
 
41
 
 
22
12
 
 
41
 
 
20
10
 
 
55
 
 
18
7
 
 
56
 
 
15
5
 
 
61
 
 
12
2
 
 
57
 
 
11
1
 
 
51
 
 
13
3
 
 
36
 
 
15
4
 
 
49
 
 
17
6
 
 
41
 
 
19
8
 
 
52
 
 
21
11

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: CliFlo [6]

Imperial conversion
JFMAMJJASOND
 
 
1.5
 
 
73
53
 
 
1.6
 
 
72
53
 
 
1.6
 
 
69
49
 
 
2.2
 
 
64
44
 
 
2.2
 
 
58
40
 
 
2.4
 
 
53
35
 
 
2.2
 
 
53
34
 
 
2
 
 
55
37
 
 
1.4
 
 
59
39
 
 
1.9
 
 
62
42
 
 
1.6
 
 
67
46
 
 
2
 
 
70
51

Average max. and min. temperatures in °F

Precipitation totals in inches

The oceanic climate is prevalent in the more southerly parts of Oceania. A mild maritime climate is in existence in New Zealand. In Australia, the climate is found in Tasmania, southern half of Victoria and southeastern New South Wales (southwards from Wollongong).

Some parts of the northeastern coast of Honshu, such as Mutsu, Aomori in Japan, feature this climate, although it is rare in Asia due to the lack of a west coast in the middle latitudes. [7]

Indian Ocean

Île Amsterdam and Île 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).

Varieties

Marine west coast (Cfb)

Climate chart (explanation)
JFMAMJJASOND
 
 
108
 
 
9
4
 
 
84
 
 
9
4
 
 
78
 
 
11
5
 
 
67
 
 
13
6
 
 
64
 
 
16
9
 
 
57
 
 
18
11
 
 
62
 
 
20
13
 
 
67
 
 
20
13
 
 
74
 
 
18
12
 
 
113
 
 
15
9
 
 
113
 
 
12
6
 
 
119
 
 
10
5

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: Hong Kong Observatory

Imperial conversion
JFMAMJJASOND
 
 
4.3
 
 
48
39
 
 
3.3
 
 
48
38
 
 
3.1
 
 
51
41
 
 
2.6
 
 
55
43
 
 
2.5
 
 
60
48
 
 
2.2
 
 
64
52
 
 
2.4
 
 
68
56
 
 
2.6
 
 
68
56
 
 
2.9
 
 
65
53
 
 
4.4
 
 
59
49
 
 
4.4
 
 
53
44
 
 
4.7
 
 
49
40

Average max. and min. temperatures in °F

Precipitation totals in inches

Temperate oceanic climates, also known as "marine mild winter" climates [8] or simply oceanic climates, are found either at middle latitudes. They are often found on or near the west coast of continents; hence another name for Cfb, "marine west coast climates". In addition to moderate temperatures year-round, one of the characteristics is the absence of a dry season. Except for Europe, this type of climate is confined to narrow bands of territory, largely in mid or high latitudes, although it can appear in elevated areas of continental terrain in low latitudes, e.g. plateaus in the subtropics. [9] It exists in both hemispheres between 35° and 60°: at low altitudes between Mediterranean, humid continental, and subarctic climates. [10]

Western sea breezes ease temperatures and moderates the winter, especially if warm sea currents are present, and cause cloudy weather to predominate. Precipitation is constant, especially in colder months, when temperatures are warmer than elsewhere at comparable latitudes. This climate can occur farther inland if no mountain ranges are present or nearby. [11] As this climate causes sufficient moisture year-round without permitting deep snow cover, vegetation typically prospers in this climate. Deciduous trees are predominant in this climate region. 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.

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). The average temperature of the coldest month must not be colder than −3–0 °C (27–32 °F), or the climate will be classified as continental. [9] [12] The average temperature variations in the year are between 10–15 °C (50–59 °F), with average annual temperatures between 6–13 °C (43–55 °F). Rain values can vary from 50–500 cm (20–197 in), depending on whether mountains cause orographic precipitation. Frontal cyclones can be common in marine west coast regions, with some areas experiencing more than 150 rainy days annually, but strong storms are rare. [10]

Zennor, United Kingdom Zennor, from Zennor Hill - geograph.org.uk - 633.jpg
Zennor, United Kingdom

Cfb climates are predominant in most of Europe except the northeast, as global temperatures became warmer towards late 20th and early 21st century. They are the main climate type in New Zealand and the Australian states of Tasmania, Victoria, and southeastern New South Wales (starting from the Illawarra region). In North America, they are found mainly in Vancouver Island and neighbouring parts of British Columbia, as well as many coastal areas of southeast Alaska. There are pockets of Cfb in most South American countries, mostly in regions of southern Chile and Argentina, parts of the provinces of Chubut, Santa Cruz, and southeast Buenos Aires province in Argentina, the highest elevations of the Brazilian Highlands, and due to variations in rainfall and temperature patterns in some places of the Tropical Andes in Bolivia, Perú, Ecuador, Colombia and Venezuela. In Western Asia, the climate can be found on the Black Sea coast of northern Turkey and Georgia, often transitional to humid subtropical. While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa.

The climate subtype can also be found in Nantucket, Massachusetts (in the immediate west and northwest in transition for humid continental, the remainder of Cape Cod [13] ) [14] and northeastern Georgia both in the eastern United States. [15] It is also found in the highest portions of the Brazilian state of Bahia and Roraima (in transition or strongly influenced for Cwb), Cuyuni-Mazuruni in Guiana, Vinje, Sør-Trøndelag in 63.20 °N (Norway central coast), South Sudan (border with Uganda), Central Province of the Sri Lanka, the provinces of Bình Định and Quảng Ngãi in Vietnam, Sabah (northeastern Malaysia) and Baluchistan, Pakistan. Although there are more or less rare places associated with relatively isolated mountainous regions (e.g., North Oceania islands and China). [16]

Subtropical highland variety (Cfb, Cwb)

Climate chart (explanation)
JFMAMJJASOND
 
 
11
 
 
21
6
 
 
4.3
 
 
23
7
 
 
10
 
 
26
9
 
 
26
 
 
27
11
 
 
56
 
 
27
12
 
 
135
 
 
25
12
 
 
175
 
 
23
12
 
 
169
 
 
23
12
 
 
145
 
 
22
12
 
 
67
 
 
22
10
 
 
12
 
 
22
8
 
 
6
 
 
21
7

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: WMO

Imperial conversion
JFMAMJJASOND
 
 
0.4
 
 
70
42
 
 
0.2
 
 
73
45
 
 
0.4
 
 
78
49
 
 
1
 
 
80
51
 
 
2.2
 
 
80
53
 
 
5.3
 
 
76
54
 
 
6.9
 
 
73
53
 
 
6.7
 
 
74
53
 
 
5.7
 
 
72
53
 
 
2.6
 
 
72
50
 
 
0.5
 
 
71
46
 
 
0.2
 
 
69
44

Average max. and min. temperatures in °F

Precipitation totals in inches

Nuwara Eliya, Sri Lanka SL Nuwara Eliya asv2020-01 img12 racecourse.jpg
Nuwara Eliya, Sri Lanka

The subtropical highland climate is a climate variety often grouped together with oceanic climates which exists in some mountainous or elevated portions of the world in either the subtropics or tropics. Despite the latitude, the higher elevations of these regions mean that the climate shares characteristics with oceanic climates. [17] [18]

Subtropical highland climates with uniform rainfall (Cfb) [19] usually have rainfall spread relatively evenly throughout the year, similar to other oceanic climates but unlike these climates, they have a high diurnal temperature variation and low humidity, owing to their inland location and relatively high elevation. Subtropical highland climates with monsoon influence (Cwb), have distinctive wet summers and dry winters. [20]

In locations outside the tropics, other than the drying trend in the winter, subtropical highland climates tend to be essentially identical to an oceanic climate, with mild summers and noticeably cooler winters, plus, in some instances, some snowfall. In the tropics, a subtropical highland climate typically features mild weather year-round. Temperatures there remain relatively constant throughout the year and snowfall is seldom seen due to warmer winters than most oceanic climates.

Areas with this climate feature monthly averages below 22 °C (72 °F) but above −3 °C (27 °F) (or 0 °C (32 °F) using American standards). At least one month's average temperature is below 18 °C (64 °F). Without their elevation, many of these regions would likely feature either humid subtropical or tropical climates.

This type of climate exists in parts of east, south and southeastern Africa, interior southern Africa and elevated portions of eastern Africa as far north as Ethiopia and of western Africa (west region of Cameroon) up to the southwestern Angola highlands also share this climate type. It also exists in the exposed areas of the High Atlas, some mountainous areas across southern Europe, mountainous sections of North America, including parts of the southern Appalachians and the Central America Volcanic Arc. In South America, it can be found mainly in temperate mountainous areas in the Tropical Andes, Venezuelan Coastal Range, the highest elevations of Serra do Mar in Southeastern Brazil, and tepuis of the Guiana Shield. Most of Yunnan and mountainous areas across Southeast Asia, parts of the Himalayas, parts of Sri Lanka, and parts of the Hawaiian Islands of Maui and Hawaii. In the Caribbean, only the peaks in the highest mountain ranges have this climate (including the Blue Mountains in Jamaica and Cerro Maravilla in Puerto Rico), with only Hispaniola's Cordillera Central and Chaîne de la Selle having significant urban settlements under this climate zone, such as cities like Kenscoff in Haiti and Constanza in the Dominican Republic.

Subpolar oceanic and cold subtropical highland varieties (Cfc, Cwc)

Climate chart (explanation)
JFMAMJJASOND
 
 
42
 
 
14
7
 
 
31
 
 
14
7
 
 
38
 
 
12
5
 
 
40
 
 
10
3
 
 
41
 
 
7
1
 
 
27
 
 
4
1
 
 
29
 
 
4
1
 
 
30
 
 
5
0
 
 
27
 
 
8
1
 
 
27
 
 
10
3
 
 
30
 
 
12
5
 
 
33
 
 
14
6

Average max. and min. temperatures in °C

Precipitation totals in mm

Source: Dirección Meteorológica de Chile [21]

Imperial conversion
JFMAMJJASOND
 
 
1.6
 
 
58
44
 
 
1.2
 
 
57
44
 
 
1.5
 
 
54
41
 
 
1.6
 
 
49
38
 
 
1.6
 
 
44
34
 
 
1.1
 
 
39
30
 
 
1.1
 
 
39
30
 
 
1.2
 
 
41
32
 
 
1
 
 
46
34
 
 
1.1
 
 
50
37
 
 
1.2
 
 
54
40
 
 
1.3
 
 
56
43

Average max. and min. temperatures in °F

Precipitation totals in inches

Areas with subpolar oceanic climates feature an oceanic climate but are usually located closer to polar regions, with long but relatively mild winters and short, cool summers. As a result of their location, these regions tend to be on the cool end of oceanic climates, approaching to polar regions. Snowfall tends to be more common here than in other oceanic climates. Subpolar oceanic climates are less prone to temperature extremes than subarctic climates or continental climates, featuring milder winters than these climates. Subpolar oceanic climates feature only one to three months of average monthly temperatures that are at least 10 °C (50 °F). As with oceanic climates, none of its average monthly temperatures fall below -3.0 °C (26.6 °F) or 0 °C depending on the isotherm used. Typically, these areas in the warmest month experience daytime maximum temperatures below 17 °C (63 °F), while the coldest month features highs slightly above freezing and lows near or just below freezing while keeping the average warm enough. It typically carries a Cfc designation, though very small areas in Argentina and Chile have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). [22]

This variant of an oceanic climate is found in parts of coastal Iceland, the Faroe Islands, upland/mountainous parts of Scotland and Northern England, northwestern coastal areas of Norway (most of Lofoten, Vesterålen, warmest part of Tromsø reaching to 71°N on some islands), [23] uplands/highlands in western Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle, the southwest of Argentina and Chile, and a few highland areas of Tasmania, and the Australian and Southern Alps. [24] This type of climate is even found in very remote parts of the New Guinea Highlands. The classification used for this regime is Cfc. [1] In the most marine of those areas affected by this regime, temperatures above 20 °C (68 °F) are extreme weather events, even in the midst of summer. Temperatures above 30 °C (86 °F) have been recorded on rare occasions in some areas of this climate, and in winter temperatures down to −20 °C (−4 °F) have seldom been recorded in some areas.

Small areas in Yunnan, Sichuan; parts of Bolivia and Peru; and parts of Mount Kilimanjaro in Tanzania have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). [22] This is the cold variant of the monsoon-influenced subtropical highland climate. El Alto, Bolivia, is one of the few confirmed towns that features this variation of the subtropical highland climate.

Examples

^1 According to the Trewartha climate classification the climate is considered humid subtropical (Cf) since at least eight months are greater than 10 °C (50 ″C).

Africa

Asia

Europe

North America

Oceania

South America

Southern Indian Ocean

See also

Related Research Articles

<span class="mw-page-title-main">Subarctic climate</span> Climate characterised by long, usually very cold winters, and short, cool summers

The subarctic climate is a continental climate with long, cold winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd.

<span class="mw-page-title-main">Temperate climate</span> Main climate class

In geography, the temperate climates of Earth occur in the middle latitudes, which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation differences.

<span class="mw-page-title-main">Continental climate</span> Köppen climate category

Continental climates often have a significant annual variation in temperature. They tend to occur in central and eastern parts of the three northern-tier continents, typically in the middle latitudes, often within large landmasses, where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, much of Russia south of the arctic circle, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate.

<span class="mw-page-title-main">Mediterranean climate</span> Type of climate

A Mediterranean climate, also called a dry summer climate, described by Köppen as Cs, is a temperate climate type that occurs in the lower mid-latitudes. Such climates typically have dry summers and wet winters, with summer conditions ranging from warm to hot and winter conditions typically being mild to cool. These weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location.

<span class="mw-page-title-main">Subtropics</span> Geographic and climate zone

The subtropical zones or subtropics are geographical and climate zones to the north and south of the tropics. Geographically part of the temperate zones of both hemispheres, they cover the middle latitudes from 23°26′10.1″ (or 23.43615°) to approximately 35° north and south. The horse latitudes lie within this range.

<span class="mw-page-title-main">Köppen climate classification</span> Climate classification system

The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, German climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system in 1954 and 1961, which is thus sometimes called the Köppen–Geiger climate classification.

<span class="mw-page-title-main">Semi-arid climate</span> Climate with precipitation below potential evapotranspiration

A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes.

<span class="mw-page-title-main">Humid continental climate</span> Category in the Köppen climate classification system

A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot summers, and cold and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons. The definition of this climate in terms of temperature is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid. The cooler Dfb, Dwb, and Dsb subtypes are also known as hemiboreal climates. Although amount of snowfall is not a factor used in defining the humid continental climate, snow during the winter in this type of climate is almost a guarantee, either intermittently throughout the winter months near the poleward or coastal margins, or persistently throughout the winter months elsewhere in the climate zone.

<span class="mw-page-title-main">Geography of New South Wales</span> Overview of the geography of New South Wales

New South Wales is Australia's most populous state, located in the east coast of the continent. It is in the southern hemisphere between latitudes 28 and 38 degrees south of the equator and longitudes 141 and 154 degrees east of the Universal Prime Meridian. The state is in the warm temperate climatic zone.

<span class="mw-page-title-main">Geography of Ontario</span>

Ontario is located in East/Central Canada. It is Canada's second largest province by land area. Its physical features vary greatly from the Mixedwood Plains in the southeast to the boreal forests and tundra in the north. Ontario borders Manitoba to the west, Hudson Bay and James Bay to the north, Quebec to the east, and the Great Lakes and the United States to the south. The province is named for Great Lake Ontario, an adaptation of the Iroquois word Onitariio, meaning "beautiful lake", or Kanadario, variously translated as "beautiful water". There are approximately 250,000 lakes and over 100,000 kilometres (62,000 mi) of rivers in the province.

<span class="mw-page-title-main">Beulah, Colorado</span> Unincorporated community in Pueblo County, Colorado, United States

Beulah is an unincorporated community and a post office located within the Beulah Valley census-designated place in Pueblo County, Colorado, United States. The Beulah Post Office has the ZIP code 81023. Beulah is a part of the Beulah Valley CDP. Beulah lies along State Highway 78 about 21 miles southwest of Pueblo, in the foothills of the Wet Mountains.

<span class="mw-page-title-main">Climate of Alaska</span> Overview of the climate of the U.S. state of Alaska

The climate of Alaska is determined by average temperatures and precipitation received statewide over many years. The extratropical storm track runs along the Aleutian Island chain, across the Alaska Peninsula, and along the coastal area of the Gulf of Alaska which exposes these parts of the state to a large majority of the storms crossing the North Pacific. The climate in Juneau and the southeast panhandle is a mid-latitude oceanic climate, in the southern sections and a subarctic oceanic climate in the northern parts. The climate in Southcentral Alaska is a subarctic climate due to its short, cool summers. The climate of the interior of Alaska is best described as extreme and is the best example of a true subarctic climate, as the highest and lowest recorded temperatures in Alaska have both occurred in the interior. The climate in the extreme north of Alaska is an Arctic climate with long, cold winters, and cool summers where snow is possible year-round.

<span class="mw-page-title-main">Climate of Japan</span> Overview of the Climate of Japan

Most regions of Japan, such as Honshu, Shikoku, and Kyushu, belong to the temperate zone with humid subtropical climate characterized by four distinct seasons. However, its climate varies from cool humid continental climate in the north such as northern Hokkaido, to warm tropical rainforest climate in the south such as the Yaeyama Islands and Minami-Tori-shima.

<span class="mw-page-title-main">Climate of Russia</span> Characteristics of the climate of Russia

The climate of Russia is formed under the influence of several determining factors. The enormous size of the country and the remoteness of many areas from the sea result in the dominance of the continental climate, which is prevalent in European and Asian Russia except for the tundra and the extreme southwest. Mountains in the south obstructing the flow of warm air masses from the Indian Ocean and the plain of the west and north makes the country open to Arctic and Atlantic influences.

<span class="mw-page-title-main">Climate of Mexico</span> Overview of the climate of Mexico

The climate of Mexico is very varied. The Tropic of Cancer effectively divides the country into temperate and tropical zones. Land that is north of the twenty-fourth parallel experiences lower temperatures during the winter months. South of the twenty-fourth parallel, temperatures are fairly consistent all year round and vary solely as a function of elevation. The north of the country usually receives less precipitation than the south.

<span class="mw-page-title-main">Humid subtropical climate</span> Transitional climatic zone

A humid subtropical climate is a temperate climate type characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents, generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental or oceanic climates. It is also known as warm temperate climate in some climate classifications.

<span class="mw-page-title-main">Climate of Turkey</span> Overview of the climate of Turkey

Turkey's climate is varied and generally temperate, with the regions bordering the Mediterranean and Black Sea heavily affected by the coasts, and the interior being drier and more continental.

<span class="mw-page-title-main">Climate of Spain</span> Overview of the climate of Spain

The climate of Spain is highly diverse and varies considerably across the country's various regions. Spain is the most climatically diverse country in Europe with 14 different Köppen climates.

<span class="mw-page-title-main">Humid temperate climate</span> Climate sub-type

The humid temperate climate is a temperate climate sub-type mainly located at mid latitudes. It is characterized by humidity and rain throughout the year from oceanic influence. Although the term humid temperate climate is not used in the Köppen climate classification, this climate type may fall under the Cf classification, which indicates a temperate climate without a dry season.

<span class="mw-page-title-main">Subhumid temperate climate</span>

The subhumid temperate climate also called monsoon temperate climate, is a temperate climate sub-type with monsoon influence, that is a climate with dry winter and wet summer. Although the terms subhumid temperate climate and monsoon temperate climate are not officially used in the Köppen climate classification, climates of this type may fall under the Cw classification for dry winters. In most cases it may be present as highland climate.

References

  1. 1 2 Tom L. McKnight & Darrel Hess (2000). Climate Zones and Types: The Köppen System. Physical Geography: A Landscape Appreciation. Prentice Hall. pp.  226–235. ISBN   978-0-13-020263-5.
  2. Briney, Amanda (22 January 2020). "The Gulf Stream". ThoughtCo. Retrieved 1 June 2015.
  3. "Klimaattabel Schiphol, langjarige gemiddelden, tijdvak 1991–2020" (in Dutch). Royal Netherlands Meteorological Institute . Retrieved 30 March 2022.
  4. "Klimatoloji-2" (PDF).
  5. M. C. Peel; B. L. Finlayson & T. A. McMahon (11 October 2007). "Updated world map of the Köppen-Geiger climate classification" (PDF). Hydrology and Earth System Sciences. 11 (5): 1638–1643. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . Retrieved 30 January 2011.
  6. "CliFlo – National Climate Database". NIWA. Archived from the original on 27 November 2015. Retrieved 23 June 2015.
  7. "Winter in Japan - a Complete Guide to Wintertime in Japan | Compathy Magazine". Compathy Magazine (コンパシーマガジン). 18 September 2016. Retrieved 8 August 2020.
  8. Michael Pidwirny, 2017, Appendix 3: Köppen Climate Classification: Single appendix from the eBook Understanding Physical Geography. Kelowna BC, Canada; Our Planet Earth Publishing, pp. 8, 24.
  9. 1 2 "Temperate oceanic climate". www.mindat.org. Retrieved 11 October 2018.
  10. 1 2 "marine west coast climate | Characteristics & Facts". Encyclopedia Britannica. Retrieved 11 October 2018.
  11. "Marine West Coast Climate". www.earthonlinemedia.com. Retrieved 11 October 2018.
  12. "Hot Continental Division". www.fs.fed.us. Retrieved 11 October 2018.
  13. "Mean Temperature US in January - 30 yrs (normals)".
  14. "Massachusetts Koppen Climate".
  15. "Georgia US Koppen Climate".
  16. "World Maps of Köppen-Geiger climate classification". koeppen-geiger.vu-wien.ac.at. Retrieved 16 October 2018.
  17. Pacheco-Torgal, Fernando; Goran-Granqvist, Claes (30 January 2023). Adapting the Built Environment for Climate Change. Elsevier. p. 187. ISBN   9780323953375 . Retrieved 11 June 2023.
  18. Herminingrum, Sri; Hum, M (November 2021). Fisheries and Marine Science. Media Nusa Creative (MNC Publishing). p. 17. ISBN   9786024620998 . Retrieved 11 June 2023.
  19. Khan, Ansar; Niyogi, Dev; Fiorito, Francesco; Akbari, Hashem; Mithun, Sk (15 June 2022). Global Urban Heat Island Mitigation. Elsevier Science. p. 253. ISBN   9780323897945 . Retrieved 21 June 2023.
  20. "Mindat.org". www.mindat.org. Retrieved 11 June 2023.
  21. "Estadistica Climatologica Tomo III (pg 512–537)" (PDF) (in Spanish). Dirección General de Aeronáutica Civil. March 2001. Archived from the original (PDF) on 17 April 2012. Retrieved 15 January 2013.
  22. 1 2 Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (11 October 2007). "Updated world map of the Köppen-Geiger climate classification" (PDF). Hydrology and Earth System Sciences. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007 . S2CID   9654551 . Retrieved 5 December 2022.
  23. "Weather statistics for Hasvik (Finnmark)".
  24. Tapper, Andrew; Tapper, Nigel (1996). Gray, Kathleen (ed.). The weather and climate of Australia and New Zealand (First ed.). Melbourne, Australia: Oxford University Press. p. 300. ISBN   978-0-19-553393-4.
  25. "World Meteorological Organization Climate Normals for 1991-2020 — Trevico". National Oceanic and Atmospheric Administration. Retrieved 3 February 2024.