Köppen climate classification

The Köppen climate classification scheme divides climates into five main climate groups: A (tropical), B (arid), C (temperate), D (continental), and E (polar). The second letter indicates the seasonal precipitation type, while the third letter indicates the level of heat. Summers are defined as the six-month period that is warmer either from April to September or October to March, while winter is the six-month period that is cooler. • BWh = Hot desert climate • BWk = Cold desert climate • BSh = Hot semi-arid climate • BSk = Cold semi-arid climate Group C: Temperate climates , UK, has a temperate oceanic climate Temperate climates have the coldest month averaging between (or ) and and at least one month averaging above . For the distribution of precipitation in locations that both satisfy a dry summer (Cs) and a dry winter (Cw), a location is considered to have a wet summer (Cw) when more precipitation falls within the summer months than the winter months while a location is considered to have a dry summer (Cs) when more precipitation falls within the winter months. This additional criterion applies to locations that satisfies both Ds and Dw as well. • Cfa = Humid subtropical climate; coldest month averaging above (or ), at least one month's average temperature above , and at least four months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Cfb = Temperate oceanic climate or subtropical highland climate; coldest month averaging above (or ), all months with average temperatures below , and at least four months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Cfc = Subpolar oceanic climate; coldest month averaging above (or ) and 1–3 months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Cwa = Monsoon-influenced humid subtropical climate; coldest month averaging above (or ), at least one month's average temperature above , and at least four months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Cwb = Subtropical highland climate or Monsoon-influenced temperate oceanic climate; coldest month averaging above (or ), all months with average temperatures below , and at least four months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Cwc = Cold subtropical highland climate or Monsoon-influenced subpolar oceanic climate; coldest month averaging above (or ) and 1–3 months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Csa = Hot-summer Mediterranean climate; coldest month averaging above (or ), at least one month's average temperature above , and at least four months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . • Csb = Warm-summer Mediterranean climate; coldest month averaging above (or ), all months with average temperatures below , and at least four months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . • Csc = Cold-summer Mediterranean climate; coldest month averaging above (or ) and 1–3 months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . Group D: Continental climates in Alaska has a subarctic climate Continental climates have at least one month averaging below (or ) and at least one month averaging above . • Dfa = Hot-summer humid continental climate; coldest month averaging below (or ), at least one month's average temperature above , and at least four months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Dfb = Warm-summer humid continental climate; coldest month averaging below (or ), all months with average temperatures below , and at least four months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Dfc = Subarctic climate; coldest month averaging below (or ) and 1–3 months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Dfd = Extremely cold subarctic climate; coldest month averaging below and 1–3 months averaging above . No significant precipitation difference between seasons (neither the abovementioned set of conditions fulfilled). • Dwa = Monsoon-influenced hot-summer humid continental climate; coldest month averaging below (or ), at least one month's average temperature above , and at least four months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Dwb = Monsoon-influenced warm-summer humid continental climate; coldest month averaging below (or ), all months with average temperatures below , and at least four months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Dwc = Monsoon-influenced subarctic climate; coldest month averaging below (or ) and 1–3 months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Dwd = Monsoon-influenced extremely cold subarctic climate; coldest month averaging below and 1–3 months averaging above . At least ten times as much rain in the wettest month of summer as in the driest month of winter. • Dsa = Mediterranean-influenced hot-summer humid continental climate; coldest month averaging below (or ), average temperature of the warmest month above and at least four months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . • Dsb = Mediterranean-influenced warm-summer humid continental climate; coldest month averaging below (or ), average temperature of the warmest month below and at least four months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . • Dsc = Mediterranean-influenced subarctic climate; coldest month averaging below (or ) and 1–3 months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . • Dsd = Mediterranean-influenced extremely cold subarctic climate; coldest month averaging below and 1–3 months averaging above . At least three times as much precipitation in the wettest month of winter as in the driest month of summer, and the driest month of summer receives less than . Group E: Polar and alpine climates Polar and alpine climates has every month of the year with an average temperature below . • ET = Tundra climate; average temperature of warmest month between and . • EF = Ice cap climate; eternal winter, with all 12 months of the year with average temperatures below . == Group A: Tropical/megathermal climates ==

Tropical climates are characterized by constant high temperatures (at sea level and low elevations); all 12 months of the year have average temperatures of 18 °C (64.4 °F) or higher; and generally high annual precipitation. They are subdivided as follows: Af: Tropical rainforest climate All 12 months have an average precipitation of at least . These climates usually occur within 10° latitude of the equator. This climate has no natural seasons in terms of thermal and moisture changes. Some of the places with this climate are indeed uniformly and monotonously wet throughout the year (e.g., the northwest Pacific coast of South and Central America, from Ecuador to Costa Rica; see, for instance, Andagoya, Colombia), but in many cases, the period of higher sun and longer days is distinctly wettest (as at Palembang, Indonesia) or the time of lower sun and shorter days may have more rain (as at Sitiawan, Malaysia). Among these places, some have a pure equatorial climate (Balikpapan, Kuala Lumpur, Kuching, Lae, Medan, Paramaribo, Pontianak, and Singapore) with the dominant ITCZ aerological mechanism and no cyclones or a subequatorial climate with occasional hurricanes (Davao, Ratnapura, Victoria). (The term aseasonal refers to the lack in the tropical zone of large differences in daylight hours and mean monthly (or daily) temperature throughout the year. Annual cyclic changes occur in the tropics, but not as predictably as those in the temperate zone, albeit unrelated to temperature, but to water availability whether as rain, mist, soil, or groundwater. Plant response (e.g., phenology), animal (feeding, migration, reproduction, etc.), and human activities (plant sowing, harvesting, hunting, fishing, etc.) are tuned to this 'seasonality'. Indeed, in tropical South America and Central America, the 'rainy season' (and the 'high water season') is called (Spanish) or (Portuguese), though it could occur in the Northern Hemisphere summer; likewise, the 'dry season (and 'low water season') is called or , and can occur in the Northern Hemisphere winter). Am: Tropical monsoon climate This type of climate results from the monsoon winds which change direction according to the seasons. This climate has a driest month (which nearly always occurs at or soon after the "winter" solstice for that side of the equator) with rainfall less than , but at least 100-\left (\frac{\mathrm{total\,annual\,precipitation\,(mm)}}{25} \right) of average monthly precipitation. This is the case in parts of Hawaii, northwestern Dominican Republic, Eastern Africa, southeast India and northeast Sri Lanka, and the Brazilian Northeastern Coast. In places that have this climate type, the dry season occurs during the time of high sun and longer days generally because of rain shadow effects. == Group B: Arid (desert and semi-arid) climates ==

distribution These climates are characterized by the amount of annual precipitation less than a threshold value that approximates the potential evapotranspiration. If the annual precipitation is less than 50% of this threshold, the classification is BW (arid: desert climate); if it is in the range of 50%–100% of the threshold, the classification is BS (semi-arid: steppe climate). A third letter can be included to indicate temperature. Here, h signifies low-latitude climate (average annual temperature above 18 °C) while k signified middle-latitude climate (average annual temperature below 18 °C). Desert areas situated along the west coasts of continents at tropical or near-tropical locations characterized by frequent fog and low clouds, although these places rank among the driest on earth in terms of actual precipitation received, can be labeled BWn with the n denoting a climate characterized by frequent fog. BW: Arid climates The desert climate or arid climate (BW) is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of Earth's land area, hot deserts are the second-most common type of climate on Earth after the Polar climate. There are two variations of a desert climate: a hot desert climate (BWh), and a cold desert climate (BWk). To delineate "hot desert climates" from "cold desert climates", a mean annual temperature of is used as an isotherm so that a location with a BW type climate with the appropriate temperature above this isotherm is classified as "hot arid subtype" (BWh), and a location with the appropriate temperature below the isotherm is classified as "cold arid subtype" (BWk). Most desert/arid climates receive between of rainfall annually, although some of the most consistently hot areas of Central Australia, the Sahel and Guajira Peninsula can be, due to extreme potential evapotranspiration, classed as arid with the annual rainfall as high as . BWh: Hot deserts Hot desert climates (BWh) are typically found under the subtropical ridge in the lower middle latitudes or the subtropics, often between 20° and 33° north and south latitudes. In these locations, stable descending air and high pressure aloft clear clouds and create hot, arid conditions with intense sunshine. Hot desert climates are found across vast areas of North Africa, West Asia, northwestern parts of the Indian subcontinent, southwestern Africa, interior Australia, the Southwestern United States, northern Mexico, the coast of Peru and Chile, parts of the Brazilian sertão and the southeastern coast of Spain. This makes hot deserts present in every continent except Antarctica. At the time of high sun (summer), scorching, desiccating heat prevails. Hot-month average temperatures are normally between , and midday readings of are common. BWk: Cold deserts , at elevation Cold desert climates (BWk) usually feature hot (or warm in a few instances), dry summers, though summers are not typically as hot as hot desert climates. Unlike hot desert climates, cold desert climates tend to feature cold, dry winters. Snow tends to be rare in regions with this climate. The Gobi Desert in northern China and Mongolia is one example of a cold desert. Though hot in the summer, it shares the freezing winters of the rest of Inner Asia. Summers in South America's Atacama Desert are mild, with only slight temperature variations between seasons. Cold desert climates are typically found at higher altitudes than hot desert climates and are usually drier than hot desert climates. Cold desert climates are typically located in temperate zones in the 30s and 40s latitudes, usually in the leeward rain shadow of high mountains, restricting precipitation from the westerly winds. BS: Semi-arid (steppe) climates A semi-arid 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. BSh: Hot semi-arid Hot semi-arid climates (type "BSh") tend to be located from the high teens to mid-30s latitudes of the tropics and subtropics, typically in proximity to regions with a tropical savanna climate or a humid subtropical climate. These climates tend to have hot, or sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts. BSk: Cold semi-arid Cold semi-arid climates (type "BSk") tend to be located in elevated portions of temperate zones generally from the mid-30s to low 50s latitudes, typically bordering a humid continental climate or a Mediterranean climate. They are also typically found in continental interiors some distance from large bodies of water. Cold semi-arid climates usually feature warm to hot dry summers, though their summers are typically not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold and possibly freezing winters. These areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. == Group C: Temperate/mesothermal climates ==

distribution In the Köppen climate system, temperate climates are defined as having an average temperature above (or , as noted previously) in their coldest month but below . The average temperature of roughly coincides with the equatorward limit of frozen ground and snow cover lasting for a month or more. The second letter indicates the precipitation pattern—w indicates dry winters (driest winter month average precipitation less than one-tenth wettest summer month average precipitation). s indicates at least three times as much rain in the wettest month of winter as in the driest month of summer. f means significant precipitation in all seasons (neither above-mentioned set of conditions fulfilled). These climates are in the polar front region in winter, and thus have moderate temperatures and changeable, rainy weather. Summers are hot and dry, due to the domination of the subtropical high-pressure systems, except in the immediate coastal areas, where summers are milder due to the nearby presence of cold ocean currents that may bring fog but prevent rain. Csb: Warm-summer Mediterranean climates Dry-summer climates sometimes extend to additional areas where the warmest month average temperatures do not reach , most often in the 40s latitudes. These climates are classified as Csb. Csc: Cold-summer Mediterranean climates Cold summer Mediterranean climates (Csc) exist in high-elevation areas adjacent to coastal Csb climate areas, where the strong maritime influence prevents the average winter monthly temperature from dropping below . This climate is rare and is predominantly found in climate fringes and isolated areas of the Cascades and Andes Mountains, as the dry-summer climate extends further poleward in the Americas than elsewhere. Rare instances of this climate can be found in some coastal locations in the North Atlantic, central Tasmania, and at high altitudes in Hawaii. Cfa: Humid subtropical climates , China These climates usually occur on the eastern coasts and eastern sides of continents, usually in the high 20s and 30s latitudes. Unlike the dry summer Mediterranean climates, humid subtropical climates have a warm and wet flow from the tropics that creates warm and moist conditions in the summer months. As such, summer (not winter as is the case in Mediterranean climates) is often the wettest season. The flow out of the subtropical highs and the summer monsoon creates a southerly flow from the tropics that brings warm and moist air to the lower east sides of continents. This flow is often what brings the frequent and strong but short-lived summer thundershowers so typical of the more southerly subtropical climates like the southeast United States, southern China, and Japan. Cfb: Oceanic climates Marine west coast climate Cfb climates usually occur in the higher middle latitudes on the western sides of continents; they are typically situated immediately poleward of the Mediterranean climates in the 40s and 50s latitudes. However, in southeast Australia, southeast South America, and extreme southern Africa this climate is found immediately poleward of temperate climates, on places near the coast and at a somewhat lower latitude. In western Europe, this climate occurs in coastal areas up to 68°N in Norway. These climates are dominated all year round by the polar front, leading to changeable, often overcast weather. Summers are mild due to cool ocean currents. Winters are milder than other climates in similar latitudes, but usually very cloudy, and frequently wet. Cfb climates are also encountered at high elevations in certain subtropical and tropical areas, where the climate would be that of a subtropical/tropical rainforest if not for the altitude. These climates are called "highlands". Subtropical highland climate with uniform rainfall Subtropical highland climates with uniform rainfall (Cfb) are a type of oceanic climate mainly found in the highlands of Australia, such as in or around the Great Dividing Range in the north of the state of New South Wales, and also sparsely in other continents, such as in South America, among others. Unlike a typical Cwb climate, they tend to have rainfall spread evenly throughout the year. They have characteristics of both the Cfb and Cfa climates, but unlike these climates, they have a high diurnal temperature variation and low humidity, owing to their inland location and relatively high elevation. Cfc: Subpolar oceanic climate Subpolar oceanic climates (Cfc) occur poleward of or at higher elevations than the maritime temperate climates and are mostly confined either to narrow coastal strips on the western poleward margins of the continents, or, especially in the Northern Hemisphere, to islands off such coasts. They occur in both hemispheres, generally in the high 50s and 60s latitudes in the Northern Hemisphere and the 50s latitudes in the Southern Hemisphere. Cw: Dry-winter subtropical climates Cwa: Dry-winter humid subtropical climate Cwa is a monsoonal influenced version of the humid subtropical climate, having the classic dry winter–wet summer pattern associated with tropical monsoonal climates. They are found at similar latitudes as the Cfa climates, except in regions where monsoons are more prevalent. These regions are in the Southern Cone of South America, the Gangetic Plain of South Asia, southeastern Africa, parts of East Asia and Mexico, and Northern Vietnam of Southeast Asia. Cwb: Dry-winter subtropical highland climate Dry-winter subtropical highland climate (Cwb) is a type of climate mainly found in highlands inside the tropics of Central America, South America, Africa, and South and Southeast Asia or areas in the subtropics. Winters are noticeable and dry, and summers can be very rainy. In the tropics, the monsoon is provoked by the tropical air masses and the dry winters by subtropical high pressure. Cwc: Dry-winter cold subtropical highland climate Dry-winter cold subtropical highland climates (Cwc) exist in high-elevation areas adjacent to Cwb climates. This climate is rare and is found mainly in isolated locations mostly in the Andes in Bolivia and Peru, as well as in sparse mountain locations in Southeast Asia. == Group D: Continental/microthermal climates ==

distribution These climates have an average temperature above in their warmest months, and the coldest month average below (or , as noted previously). These usually occur in the interiors of continents and on their upper east coasts, normally north of 40°N. In the Southern Hemisphere, group D climates are extremely rare due to the smaller land masses in the middle latitudes and the almost complete absence of land at 40–60°S, existing only in some highland locations. Dfa/Dwa/Dsa: Hot summer humid continental climates , Japan, has a humid continental climate (Dfa) Dfa climates usually occur in the high 30s and low 40s latitudes, with a qualifying average temperature in the warmest month of greater than . In Europe, these climates tend to be much drier than in North America. Dsa exists at higher elevations adjacent to areas with hot summer Mediterranean (Csa) climates. == Group E: Polar climates ==

distribution In the Köppen climate system, polar climates are defined as the warmest temperature of any month being below . Polar climates are further divided into two types, tundra climates and icecap climates: ET: Tundra climate Tundra climate (ET): warmest month has an average temperature between and . These climates occur on the northern edges of the North American and Eurasian land masses (generally north of 70 °N although they may be found farther south depending on local conditions), and on nearby islands. ET climates are also found on some islands near the Antarctic Convergence, and at high elevations outside the polar regions, above the tree line. EF: Ice cap climate , Antarctica Ice cap climate (EF): this climate is dominant in Antarctica, inner Greenland, and summits of many high mountains, even at lower latitudes. Monthly average temperatures never exceed . == Ecological significance ==

Biomass The Köppen climate classification is based on the empirical relationship between climate and vegetation. This classification provides an efficient way to describe climatic conditions defined by temperature and precipitation and their seasonality with a single metric. Because climatic conditions identified by the Köppen classification are ecologically relevant, it has been widely used to map the geographic distribution of long-term climate and associated ecosystem conditions. Climate change Over recent years, there has been an increasing interest in using the classification to identify changes in climate and potential changes in vegetation over time. In 2015, a Nanjing University paper published in Scientific Reports analyzing climate classifications found that between 1950 and 2010, approximately 5.7% of all land area worldwide had moved from wetter and colder classifications to drier and hotter classifications. The authors also found that the change "cannot be explained as natural variations but are driven by anthropogenic factors". A 2018 study provides detailed maps for present and future Köppen-Geiger climate classification maps at 1-km resolution. == Other Köppen climate maps ==

All maps use the ≥ definition for the temperate-continental border. File:Koppen-Geiger_Map_v2_North_America_1991–2020.svg|North America File:Koppen-Geiger_Map_v2_Europe_1991–2020.svg|Europe File:Koppen-Geiger_Map_v2_RUS_1991–2020.svg|Russia File:Koppen-Geiger_Map_v2_Central_Asia_1991–2020.svg|Central Asia File:Koppen-Geiger_Map_v2_Eastern_Asia_1991–2020.svg|East Asia File:Koppen-Geiger_Map_v2_South_America_1991–2020.svg|South America File:Koppen-Geiger_Map_v2_Africa_1991–2020.svg|Africa File:Koppen-Geiger_Map_v2_Western_Asia_1991–2020.svg|Western Asia File:Koppen-Geiger_Map_v2_Southern_Asia_1991–2020.svg|South Asia File:Koppen-Geiger_Map_v2_Southeastern_Asia_1991–2020.svg|Southeast Asia File:Koppen-Geiger_Map_v2_Melanesia_1991–2020.svg|Melanesia/Oceania File:Koppen-Geiger_Map_v2_AUS_1991–2020.svg|Australia File:Koppen-Geiger_Map_v2_NZL_1991–2020.svg|New Zealand File:Koppen-Geiger_Map_v2_World_1991–2020.svg|World (1991–2020) File:Koppen-Geiger_Map_v2_World_2071–2099_SSP245.svg|World (2071–2099, SSP245) == See also ==