'Climates and Climate Related Factors Essay\r'

' equatorial wet modes or wet equatorial humours argon usually found in atomic number 18as near the equator as the name states. These argonas include the Amazon, Congo, south-centraleast Asia and be sometimes found in the trade wind belts. The Koppen image for this character reference of humour is Af. This climate has the gnomishest temperature range in the world being in the midst of 2 and 3.6 degrees. These heavenss have on’t have a dry age because of the close proximity to the equator which covers 5-10 degrees. The stick out remains regular being warm and wet category nigh. equatorial wet climates see 60-100 inches of come down yearlyly and consume convective thunderstorms. This climate is known for being seasonless receivable to the physical structure in day to day weather.\r\nThe drive for thse unalterable weather patterns is mainly spatial relation. The analogue position allows cheerfulness coverage directly above creating uni play insolation . Also, the ITCZ acquires the year around humid, unstable air. These weather conditions create oxisol and latosol soils which atomic number 18 the least fertile; however, argon an apotheosis location for equatorial rain tones to emerge. Tropical rainforests and selva argon main office to animals much(prenominal) as birds, reptiles and insects. Those who run low in these causas of climates whitethorn use the weather to their advantage with agriculture, forestry, and with slash and skip cultivation.\r\nTropical savanna climates atomic number 18 found bring forward from the equator extending to 25°N and S analogue. The Koppen symbolic representation for this type of climate is Aw. Characteristics that make this climate distinctive is the alternation of a wet and dry season. Locations that have it off the Aw climate are Africa, S. America, and N. Australia. Winters in this climate are dry with trenchant skies and are associated with semitropic gameys. The summer s are wet with galore(postnominal) thunderstorms anf convectional rain of the ITCZ.\r\nThe tropical savanna sees an average of 35 to 70 inches of rain each year which for the well-nigh part comes from the summer season. The average annual tempeteature range is 5 to 15°. A surplus of the water supply comes during the summer. These weather conditions create a laterite soil type devising it an ideal location for grass orbits and tall grasses to thrive. These grasslands are stead to lions, gazelles and zebras. Those who live in these locations bear create ranches with animals or use the wildlife to their advantage for ecotourism.\r\nThe tropical monsoon climate is equivalent to the tropical savanna climate in the route they both have wet summers and dry winters. The Koppen symbol for this climate is Aw. This type of climate is found in areas such as southeast Asia, western Africa, north South America, the Phillipines, northeastern Australia, and some islands of the East In dies. It isn’t uncommon to see 30 inches of rain deep down dickens or three months in the summer.\r\nThe annual total rain in inches falls deep down 100 and 200. at that place is a surplus of rainwater in the summer and a deficit in the winter. The tropical monsoon climates are dominated by onshore winds and seasonal reversal of winds. Latosol soils, red or white-livereded in color, are found in the Aw climate allowing broadleaf forests with some grasses to grow. Birds, reptiles and insects title this climate lieu. Those who live in tropical monsoon climate can march on plantations, grow rice or sugarcane.\r\nThe tropical surrender climate, or Bwh, is found in wedlock Africa and southwestern Eurasia. Moist winds are kept out of this area by the Andes mountains. These locations are found 25-30 degrees N and S latitude. The tropical resign climate follow ups actually zealous summers and delicate winters. The annual temperature ranges 15 to 25°F with scar ce rainfall typi tendery less than 12 inches.\r\nClimatic controls that cause these weather patterns are settle down ocean currents that quiet any air that comes crosswise it and subsidence from semitropical highs. The forswear has aridosol soil which is fertile, hardly requires irrigation. Snakes, birds, reptiles and rabbits call the tropical desert climate home. Those who call the tropical desert home can create jobs by salt mining.\r\nThe steppe climate, or Bsh, is precise resembling to the tropical desert climate and surround the Bwh climates besides on the western side. They are found broadly speaking on the edges of the desert. Rainfall is somewhat greater than the tropical desert climate and temperatures are slightly moderated with white-hot summers and mild winters. The weather system is controlled by cool ocean currents and is affected by the rain overshadow of mountains. The steppe climate has short grasslands making it an ideal home to many reptiles, snakes, bi rds, and rabbits. Chestnut/ cook soils allow these grasses to grow. Those who call the steppe climate home whitethorn take up cattle ranching to earn an income.\r\nThe humid subtropic climate, represented as Cfa Cwa and Cwb, is located at 30 degrees latitude on eastern sides of the continents. many locations that experience this type of climate include North America, South America, and Eurasia. The summers at this latitude are warm and hot, duration the winters are mild to chilliness. During the summer, the average temperature ranges betwixt 75 and 80 degrees.\r\nThese climates receive convectional rain during the summer and cyclonic rain during the winter. Annual foolhardiness is abundant between 40 and 65 inches. The location of the humid subtropical climate plays a huge role on the climate. It is located in between and on up tilted side of subtropical high blackmail cells. There is gray/ embrown or yellow podsol soil in this climate allowing forest growth. Forests in addit ion bring along the forest animals such as deer, raccoons, and black bears. This also makes it an ideal agribusiness area.\r\nThe Mediterranean or sometimes referred to as the Dry- summer sub-tropial climate, is known as Csa or Csb. These C climates are located 35 degrees North and South latitude. close to locations that experience this type of climate include southerly Europe, Central Chile, and the South tip of Africa. Summers in these locations are hot and dry with wet, mild winters. Average annual hurry ranges from 15 to 25 inches. Rainfall in the Mediterranean is cyclonic. A large amount of the precipitation falls in the winter and summers are in general rainless. These weather patterns are controlled by the subtropical high pressure cells.\r\nThere is a deficit of rain in the summer and a surplus in the winter. The soils in these C climates can be very(prenominal) fertile if irrigated. The soil is a chestnut/brown pedical which is very dry with an abundance of calcium. Ch aparrals thrive in this type of climate. They take on a brown/yellow color in the summer and bugger off green in the winter. Mountain lions, bears, deer, coyotes, gofers and birds call this climate home. These areas are utilize for agriculture with irrigation in the winter.\r\n moving further from the equator at 40-60 degrees North and South latitude is the West Coast Marine climate. The koppen symbols for this type of climate are Cfc and Cfb. Some major locations in spite of appearance this climate are westward and Central Europe, the Western side of North America, and New Zealand. For this latitude, these areas experience very mild winters as well as mild summers.\r\nWesterly winds adjacent to the ocean are the source for the mild summer and winters. It is wet year around due to oceanic influence with an annual rainfall between 30 and 50 inches received mostly in the winter. Podsol or spotosol is the soil type this climate allowing needle leaf forests with some deciduous tree s to grow. Deer, bears, birds and other forest animals call this climate home. These forests may be used people for lumbering to meet a profit on the lands.\r\nThe mid-latitude desert and steppe climates are also very similar. First, the mid-latitude desert climate, or Bwk, can be found distant from the ocean and meet by mountains. Some of these locations include central Eurasia, North American and southern South America. The Bwk region receives most of its precipitation during the summer when warming is occurring.\r\nThis warming also causes the ice to melt and create more of a water supply. The winter is dominated by bad low temperatures and anticyclonic conditions. These low temperatures create a much lower annual temperature range than the subtropical desert climate. The most fertile soil in the world is found in the mid-latitude climate allowing grasslands to grow. These grasslands are home to grass eating animals and the lands are used for animals to graze.\r\nThe mid-latit ude steppe climate, or Bsk, isn’t much different from the desert climate. It’s mainly used as a transition between desert and humid climates. Some areas that experience these climates are in found in the interior southwest of the United States such as Colorado. The temperatures in the Bsk climate are similar to the desert climate; however, have more precipitation and lesser temperature extremes. These climates are similar in the way that they are both grassland oriented, home to grass eating animals, and the land is used for animals to graze.\r\nMoving even farther from the equator, between 35 and 55 degrees North and South latitude, is the humid Continental climate, or Dfa, Dfb, Dwa, and Dwb. Eurasia and North America are a couple locations that have this type of climate. They experience long, very cold winters and hot summers. Precipitation is not high ranging moreover between 20-40 inches. Westerly winds and storms, specially in the winter play a primaeval role i n the weather conditions. The average winter month temperature is usually between 10 and 25 degrees F. Gray-brown podsols are found in the humid Continental climate as well as prairie grasses and intricate forest, deciduous and evergreen. There is a large diversity or mammals and birds. The humid continental climate is ideal for farming.\r\n50 to 70 degrees North and South latitude is the Continental Subarctic climate, or Dfc, Dwd, Dfd, and Dwc. Locations that experience this climate are Western Alaska across Canada, Eurasia, and Scandanavia. There are extremely cold winter conditions in these D climates with a light amount of snow that falls during the winter; however, little melting takes place until the summer.\r\ncyclonic storms alternate with prominent anticylonic conditions. The annual precipitation is 5-20 inches. Also, continentality is also a key factor in the reason for the cold winters and hot summers. The absolute annual temperature var. has sometimes been as dramati c as -90 degrees F to 98 degrees F. Podsolization occurs here making the soil cold and wet. This is an area where evergreen trees will thrive and be a home to animals such as deer, birds, bears and elk. galore(postnominal) people use these locations for forestry.\r\nThe last two climates are Tundra and the Icecap which are both cold climates. The Tundra, or ET climate, is located pole ward of the margins and occupies small coastal areas in the Antarctic. The warmest month will only choke up to 32 degrees F making it extremely difficult for plant life other than small bushes and grasses to grow. The ET climate experiences long, cold winters and cool summers. Most of the precipitation falls during the summer, but is less than 10 inches annually that falls mostly in the form of snow. There is a low evaporation level due to the low temperatures. Tundra soil is found in these climates. cold bears and some birds can tolerate the coldness of the ET climate and many people use these anim als for fur trapping.\r\nThe last climate is the Icecap or EF climate. Antarctica and Greenland are two locations that experience these freezing weather conditions. 50 degrees F is the average temperature of the warmest month found on the very edge of the Tundra. More towards the center of the tundra, temperatures don’t exceed 32 degrees F. There is a slender amount of precipitation in this climate with only less than 5 inches all in the form of snow. The cause for these freezing temperatures is mostly the latitude location. Also, the standoffishness from sources of heat cause cold temperatures. There is no soil type here, with no vegetation and no economic activity.\r\n'