Instruct: Given a question, retrieve passages that answer the question.
Query: What are the main climate types?
The Köppen classification depends on average monthly values of temperature and precipitation. The most commonly used form of the Köppen classification has five primary types labeled A through E. These primary types are A) tropical, B) dry, C) mild mid-latitude, D) cold mid-latitude, and E) polar. The five primary classifications can be further divided into secondary classifications such as rainforest, monsoon, tropical savanna, humid subtropical, humid continental, oceanic climate, Mediterranean climate, desert, steppe, subarctic climate, tundra, and polar ice cap.
Moldjord or Moldjorda is the administrative centre of the municipality of Beiarn in Nordland county, Norway. The village is located along the Beiar River, about south of the river's mouth at the Beiar Fjord. The village is home to the Beiarn Church, the main church for the municipality. The village has about 150 residents (in 2016).
Climate type is dominated by the winter season, a long, bitterly cold period with short, clear days, relatively little precipitation mostly in the form of snow, and low humidity. The Köppen Climate Classification subtype for this climate is "Dfc" (Continental Subarctic Climate).
Northwest Argentina is predominantly dry, hot, and subtropical. Owing to its rugged topography, the region is climatically diverse, depending on the altitude, temperature, and distribution of precipitation. Consequently, vegetation differs within these different climate types. In general, the climate can be divided into two main types: a cold arid or semi-arid climate at the higher altitudes, and warmer subtropical climate in the eastern parts of the region. Under the Köppen climate classification, the region has 5 different climate types: semi–arid ("BS"), arid ("BW"), temperate climate without a dry season and with a dry season ("Cf" and "Cw" respectively), and an alpine climate at the highest altitudes.
The main difference between climate and everyday weather is best summarized by the popular phrase "Climate is what you expect, weather is what you get." Over historic time spans there are a number of static variables that determine climate, including: latitude, altitude, proportion of land to water, and proximity to oceans and mountains. Degree of vegetation coverage affects solar heat absorption, water retention, and rainfall on a regional level.
Barn design, overall, bears architectural, cultural and historical significance, as well as some anthropological and sociological significance. Barn design speaks to two distinct parameters in agricultural history, one being climate and the other being occupation. Different types of barns tell much about what inhabitants of the past cultivated and in what type of climate they did it in. In the United States climate allows regional barn variation to easily be divided along a north/south axis. Design divided along these lines speaks to how farmers responded to the severity of the winter. In the north, where cold, harsh winters are common, buildings were more extensive and spacious, to house animals, crops and vehicles. South and west, in the U.S., where the weather tends to be more mild, barn design focused on smaller more specialized structures such as tobacco barns. It is regional differences in North American climate that produced the major differences in northern and southern American barns.
Kosovo has on average 2,066 hours with sun per year or approximately 5.7 hours per day. The highest insolation value is in Pristina with 2.140 hours for 1 year, while Peć with the smallest insolation value of 1.958 hours, with 2.067 hours and Prizren with 2.099 hours. The maximum insolation in Kosovo occurs during July, while the lowest insolation occurs in December.
The climatic changes based on territories depend on various factors, such as: vegetation, humidity of the territory etc. Climate classifications are usually based on: wind exposure, mountain height and direction, climatic effects on vegetation and watercourses.
From all the climatic classifications made in Kosovo, the most accurate one is the one provided by W. Köppen. According to this classification, Kosovo is part of C and D types of climate. Kosovo’s hot average climate during summer months is under and the cold average is above . According to the thermal characteristics, amount of rainfall and their regime in low parts of Kosovo, we get two subtypes of climate:
The climatic subtype of the western part has soft winters and a big amount of rainfall. These characteristics are inherited by the Mediterranean mild climate. The climatic subtype of "Kosovo" has cold winters and lack of rainfall, characteristics inherited from the continental type of climate. Even though Kosovo has these climatic characteristics most of the time, there might be a major change in climate on certain years only. In 1992, Kosovo had a very hot and dry summer, which fits the B climatic type of Köppen. D-climatic type which is known for average temperatures of during cold months and during hot months can be found in high parts of Kosovo, such as Prokletije, the Šar Mountains and Kopaonik. This type of climate is known by the name "subalpine" and "alpine".
The highland of Has territory, on geographical basis has a climate of three main types such as: a) Continental climate with elements of Mediterrean Climate elements in the valley of the Drina and b) mountain climate which reigns in the hilly areas of Has. The Has part in which the impact of the Mediterranean climate is felt is characterized with hot and dry summers, with little precipitation. The average annual temperature reaches 11.4C. The month of January is the coldest month in this region where the average temperature is 0.4C - 0.9C, while higher temperatures meet during July and August with 22C and 22 C. Average amount of precipitation in Has ranges from 700 to 800 mm.
Three main climatic zones can be separated, according to geographical situation and orographic conditions:Apart from these main types, other sub-types can be found, like the desertic climate in parts of southeastern Spain, like in coastal Almería. Humid continental, alpine and tundra climates in the Pyrenees and Sierra Nevada, and a typical subtropical climate in the Canary Islands, varying from humid subtropical climates to desertic climates in most of the islands, and a tropical hot semi-arid climate in coastal parts, such as Tenerife or Gran Canaria.The largest metropolitan areas, based on 2007 population, were:
Islander population:
The classification of climate from paleosols can be related using climatically sensitive features of soils that are sensitive to particular climatic variables, but even the best of these features lack precision. This is because soils are not as sensitive as meteorological instruments for recording climatic conditions. However, in a fairly broad category, climate can be interpreted from the sensitive features found in soils. One of the most large-scale influences regarding the classification of climate was created in 1918, then modified over two decades by the German meteorologist Vladimir Köppen (Trewartha 1982). He proposed there are five main climate groups (Köppen climate classification), each corresponding to the main types of terrestrial vegetation. Each climate type is designated by letters, with upper-case letters referring to the main climate groups and lower-case letters referring to subsidiary climatic features. (Retallack 2001)
In general, Argentina has four main climate types: warm, moderate, arid, and cold, all determined by the expanse across latitude, range in altitude, and relief features. The vast size, and wide range of altitudes, contribute to Argentina's diverse climate. Argentina possesses a wide variety of climatic regions ranging from subtropical in the north to subantarctic in the far south. Lying between those is the Pampas region, which features a mild and humid climate. Under the Köppen climate classification, Argentina has 11 different climate types: Humid Subtropical (Cfa, Cwa), moderate oceanic (Cfb), warm semi-arid (BSh), subtropical highland oceanic (Cwb), warm desert (BWh), cold semi–arid (BSk), cold desert (BWk), moderate Mediterranean (Csb), cold oceanic (Cfc), and tundra (ET). Consequently, there is a wide variety of biomes in the country, including subtropical rain forests, semi-arid and arid regions, temperate plains in the Pampas, and cold subantarctic in the south. However, despite the diversity of biomes, about two-thirds of Argentina is arid or semi-arid. Argentina is best divided into six distinct regions reflecting the climatic conditions of the country as a whole. From north to south, these regions are Northwest, Chaco, Northeast, Cuyo/Monte, Pampas, and Patagonia. Each climatic region has distinctive types of vegetation.
Due to its vast size and range of altitudes, Argentina possesses a wide variety of climatic regions, ranging from the hot subtropical region in the north to the cold subantarctic in the far south. Lying between those is the Pampas region, featuring a mild and humid climate. Many regions have different, often contrasting, microclimates. In general, Argentina has four main climate types: warm, moderate, arid, and cold in which the relief features, and the latitudinal extent of the country, determine the different varieties within the main climate types.
These criteria give particular importance to climate in the genesis of phenomena for which similar geological conditions can, in different climatic conditions, lead to totally different morphological evolution. As a consequence, in the description of a landslide, it can be interesting to understand in what type of climate the event occurred.
The difference between climate and weather is usefully summarized by the popular phrase "Climate is what you expect, weather is what you get."[12] Over historical time spans there are a number of nearly constant variables that determine climate, including latitude, altitude, proportion of land to water, and proximity to oceans and mountains. These change only over periods of millions of years due to processes such as plate tectonics. Other climate determinants are more dynamic: the thermohaline circulation of the ocean leads to a 5°C (9°F) warming of the northern Atlantic Ocean compared to other ocean basins.[13] Other ocean currents redistribute heat between land and water on a more regional scale. The density and type of vegetation coverage affects solar heat absorption,[14] water retention, and rainfall on a regional level. Alterations in the quantity of atmospheric greenhouse gases determines the amount of solar energy retained by the planet, leading to global warming or global cooling. The variables which determine climate are numerous and the interactions complex, but there is general agreement that the broad outlines are understood, at least insofar as the determinants of historical climate change are concerned.[15]
The geographic location of the Christmas tree nursery dictates what species of trees can be propagated. White and Scotch pines are relatively adaptable species of trees. Because many genetically different varieties are available, they can be grown in most of the temperate areas of the United States. True firs generally prefer a much cooler climate and are primarily grown in the northern United States with some varieties that only thrive in mountainous climates. Spruce prefer cool climates, but they will tolerate warmer conditions than most fir trees. Cypress generally prefer a warmer climate. For this reason, they are grown primarily in the south and southwestern United States. The Douglas fir is a fairly adaptable species and can be grown in much of the United States. In addition to the nursery’s location, the type and location of farms that purchase the seedlings or rooted cuttings also plays an important role in the type of tree that is propagated.
Northwest Argentina is predominantly dry and hot and classified as subtropical. Owing to its rugged topography, the region is climatically diverse, depending on the altitude, temperature and distribution of precipitation. Consequentially, the vegetation will differ at these different climate types. In general, the climate can be divided into 2 main types: a cold arid or semi-arid climate at the higher altitudes and warmer subtropical climate in the eastern parts of the region. Under the Köppen climate classification, the region has 5 different climate types which are semi–arid ("BS"), arid ("BW"), without a dry season and with a dry season ("Cf" and "CW" respectively) and an alpine climate at the highest altitudes.
The relationship between fire, vegetation, and climate create what is known as a fire regime. Within a fire regime, fire ecologists study the relationship between diverse ecosystems and fire; not only how fire affects vegetation, but also how vegetation affects the behavior of fire. The study of neighboring vegetation types that may be highly flammable and less flammable has provided insight into how these vegetation types can exist side by side, and are maintained by the presence or absence of fire events. Ecologists have studied these boundaries between different vegetation types, such as a closed canopy forest and a grassland, and hypothesized how climate, and soil fertility create these boundaries in vegetation types. Research in the field of pyrogeography shows how fire also plays an important role in the maintenance of dominant vegetation types, and how different vegetation types with distinct relationships to fire can exist side by side in the same climate conditions. These relationships can be described in conceptual models called fire-vegetation feedbacks, and alternative stable states.
In general, Argentina has four main climate types: warm, moderate, arid, and cold, all determined by the expanse across latitude, range in altitude, and relief features. The vast size, and wide range of altitudes, contribute to Argentina's diverse climate. Argentina possesses a wide variety of climatic regions ranging from subtropical in the north to subantarctic in the far south. Lying between those is the Pampas region, which features a mild and humid climate. Under the Köppen climate classification, Argentina has 11 different climate types: Humid Subtropical (Cfa, Cwa), moderate oceanic (Cfb), warm semi-arid (BSh), subtropical highland oceanic (Cwb), warm desert (BWh), cold semi–arid (BSk), cold desert (BWk), moderate Mediterranean (Csb), cold oceanic (Cfc), and tundra (ET). Consequently, there is a wide variety of biomes in the country, including subtropical rain forests, semi-arid and arid regions, temperate plains in the Pampas, and cold subantarctic in the south. However, despite the diversity of biomes, about two-thirds of Argentina is arid or semi-arid. Argentina is best divided into six distinct regions reflecting the climatic conditions of the country as a whole. From north to south, these regions are Northwest, Chaco, Northeast, Cuyo/Monte, Pampas, and Patagonia. Each climatic region has distinctive types of vegetation.
The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are "A" (tropical), "B" (dry), "C" (temperate), "D" (continental), and "E" (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the "E" group are assigned a seasonal precipitation subgroup (the second letter). For example, "Af" indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the "A" group, indicated by the third letter for climates in "B", "C", and "D", and the second letter for climates in "E". For example, "Cfb" indicates an oceanic climate with warm summers as indicated by the ending "b". Climates are classified based on specific criteria unique to each climate type.
Apart from these main types, other sub-types can be found, like the alpine climate in areas with very high altitude, the humid subtropical climate in areas of northeastern Spain and the continental climates ("Dfc", "Dfb" / "Dsc", "Dsb") in the Pyrenees as well as parts of the Cantabrian Range, the Central System, Sierra Nevada and the Iberian System, and a typical desert climate ("BWk", "BWh") in the zone of Almería, Murcia and eastern Canary Islands. Low-lying areas of the Canary Islands average above during their coldest month, thus having a tropical climate.
There are three main climates in the state. The lowlands are hot with temperatures rising as high as 44C in the summer in places such as the municipality of Pisaflores. Temperate regions can have hot days but often the temperature is moderated by cooler winds and clouds. Cold climates dominate the highest altitudes where freezing temperatures at night are not uncommon. Rainfall varies widely from as low as 250mm per year to as high as 2,800mm per year. The main indicator of climate type is altitude.
Khasan has a four-season humid continental climate typical of Primorsky Krai. Due to its sheltered and southerly location, it contains lesser seasonal swings than northerly inland areas. As typical of this area of the world the East Asian monsoon in summer and the Siberian High in winter are the main drivers of the local climate, resulting in wet and humid and also warm to hot summers. August temperatures are around in terms of mean temperatures, bordering on a hot-summer subtype of the climate type (Köppen climate classification "Dwa)." This is followed by cold and dry winters.
Climate type is characterized by extremely variable temperature conditions. The Köppen Climate Classification sub-type for this climate is "Bsh" (Mid-Latitude Steppe and Desert Climate).
The east-central Brazilian plateau has a humid and warm tropical climate. The northern and eastern parts of the Argentine pampas have a humid subtropical climate with dry winters and humid summers of the Chinese type, while the western and eastern ranges have a subtropical climate of the dinaric type. At the highest points of the Andean region, climates are colder than the ones occurring at the highest point of the Norwegian fjords. In the Andean plateaus, the warm climate prevails, although it is tempered by the altitude, while in the coastal strip, there is an equatorial climate of the Guinean type. From this point until the north of the Chilean coast appear, successively, Mediterranean oceanic climate, temperate of the Breton type and, already in Tierra del Fuego, cold climate of the Siberian type.
The Köppen climate classification scheme divides climates into five main climate groups: "A" (tropical), "B" (dry), "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 6 month period that is warmer either from April–September and/or October–March while winter is the 6 month period that is cooler.
Armenia's different varieties of climates depend on the absolute height of the land. They vary from the dry subtropical to the mountain tundra climate. The following six basic types can be distinguished. Another type of climate is the dry continental type. It prevails along the middle reaches of the Arax up to an elevation of 1,300 m. It differs from the dry subtropical climate by its cold winters.