Climates and Climate Related Factors Essay

Tropical wet climes or wet equatorial climes argon usually institute in argonas near the equator as the name states. These atomic number 18as involve the Amazon, Congo, mhoeast Asia and are nightimes launch in the patronage wind belts. The Koppen symbol for this type of humor is Af. This humour has the smallest temperature consort in the world being amongst 2 and 3.6 degrees. These areas dont have a dry season beca utilize of the close proximity to the equator which covers 5-10 degrees. The conditions remains constant being warm and wet year around. Tropical wet humors see 60-100 inches of rain annually and experience convective thunderstorms. This clime is known for being seasonless due to the consistency in daytime to day live on.The reason for thse constant weather patterns is mainly location. The latitude position al embarrasseds sun coverage directly in a higher place cralimentation uniform insolation. Also, the ITCZ get tos the year around humid, unstable air. These weather conditions create oxisol and latosol dents which are the least fruitful however, are an ideal location for tropical rainforests to emerge. Tropical rainforests and selva are al-Qaida to animals such as birds, reptiles and insects. Those who populate in these types of climates whitethorn use the weather to their advantage with agriculture, forestry, and with slash and burn cultivation.Tropical savannah climates are put in further from the equator extending to 25N and S latitude. The Koppen symbol for this type of climate is Aw. Characteristics that make this climate distinctive is the alternation of a wet and dry season. Locations that experience the Aw climate are Africa, S. America, and N. Australia. Winters in this climate are dry with clear skies and are associated with subtropical highs. The summers are wet with many thunderstorms anf convectional rain of the ITCZ.The tropical savanna sees an second-rate of 35 to 70 inches of rain annually which broad ly speaking 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 make it an ideal location for grasslands and tall grasses to thrive. These grasslands are home to lions, gazelles and zebras. Those who live in these locations stand create ranches with animals or use the wildlife to their advantage for ecotourism.The tropical monsoon climate is similar to the tropical savanna climate in the way they both have wet summers and dry overwinters. The Koppen symbol for this climate is Aw. This type of climate is found in areas such as southeast Asia, western Africa, northeastern South America, the Phillipines, northeastern Australia, and some islands of the East Indies. It isnt uncommon to see 30 inches of rain within two or threesome months in the summer.The annual total rain in inches falls within 100 and 200. There is a surplus of rainfall in the summ er and a deficit in the winter. The tropical monsoon climates are henpecked by offshore winds and seasonal reversal of winds. Latosol soils, red or yellow in color, are found in the Aw climate allowing deciduous forests with some grasses to grow. Birds, reptiles and insects bitch this climate home. Those who live in tropical monsoon climate can build plantations, grow rice or sugarcane.The tropical give up climate, or Bwh, is found in north-central 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 desert climate experiences very sizzling summers and loco winters. The annual temperature ranges 15 to 25F with scarce rainfall typically less than 12 inches.Climatic controls that cause these weather patterns are composed maritime currents that cool any air that comes across it and subsidence from subtropical highs. The desert has aridosol soil which is fertile, but r equires 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.The steppe climate, or Bsh, is very similar to the tropical desert climate and surround the Bwh climates except on the western side. They are found mostly on the edges of the desert. Rainfall is clean greater than the tropical desert climate and temperatures are slightly moderated with hot summers and mild winters. The weather corpse is controlled by cool ocean currents and is affected by the rain shadow of mountains. The steppe climate has short grasslands making it an ideal home to many reptiles, snakes, birds, and rabbits. Chestnut/brown soils allow these grasses to grow. Those who call the steppe climate home may take up cattle ranching to earn an income.The humid subtropical climate, represented as Cfa Cwa and Cwb, is hardened at 30 degrees latitude on eastern sides of the continents. slightly locations that ex perience this type of climate include northern America, South America, and Eurasia. The summers at this latitude are warm and hot, while the winters are mild to cold. During the summer, the average temperature ranges among 75 and 80 degrees.These climates receive convectional rain during the summer and cyclonic rain during the winter. Annual hastiness is abundant between 40 and 65 inches. The location of the humid subtropical climate tactical manoeuvres a huge role on the climate. It is located in between and on up tilted side of subtropical high pressure cells. There is gray/brown or yellow podsol soil in this climate allowing forest growth. Forests also bring along the forest animals such as deer, raccoons, and black bears. This also makes it an ideal farming area.The 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. Some locations that experience this type of climate include Southern Europe, Central Chile, and the South tip of Africa. Summers in these locations are hot and dry with wet, mild winters. Average annual precipitation ranges from 15 to 25 inches. Rainfall in the Mediterranean is cyclonic. A orotund amount of the precipitation falls in the winter and summers are mostly rainless. These weather patterns are controlled by the subtropical high pressure cells.There is a deficit of rain in the summer and a surplus in the winter. The soils in these C climates can be very fertile if irrigated. The soil is a chestnut/brown pedical which is very dry with an abundance of calcium. Chaparrals thrive in this type of climate. They take on a brown/yellow color in the summer and become green in the winter. push-down list lions, bears, deer, coyotes, gofers and birds call this climate home. These areas are utilise for agriculture with irrigation in the winter.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 within this climate are Western and Central Europe, the Western side of North America, and parvenue Zealand. For this latitude, these areas experience very mild winters as tumefy as mild summers.Westerly winds adjacent to the ocean are the reason for the mild summer and winters. It is wet year around due to oceanic invite 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 trees to grow. Deer, bears, birds and other forest animals call this climate home. These forests may be used people for lumbering to gain a profit on the lands.The mid-latitude desert and steppe climates are also very similar. First, the mid-latitude desert climate, or Bwk, can be found nonadjacent from the ocean and surrounded by mountains. Some of these locations include centra l Eurasia, North American and southern South America. The Bwk region receives most of its precipitation during the summer when warming is occurring.This warming also causes the ice to melt and create more of a water supply. The winter is dominated by severely 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.The mid-latitude steppe climate, or Bsk, isnt much different from the desert climate. Its 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 temp erature 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.Moving raze 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 only between 20-40 inches. Westerly winds and storms, especially in the winter play a key role in 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 mixed forest, deciduous and evergreen. There is a large variety or mammals and birds. The humid continental climate is ideal for farming.50 to 70 degrees North and South latitude is the Continental Subarctic climat e, 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 resolve takes place until the summer.Cyclonic storms alternate with prominent anticylonic conditions. The annual precipitation is 5-20 inches. Also, continentality is also a key grammatical constituent in the reason for the cold winters and hot summers. The absolute annual temperature variation has sometimes been as salient 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. Many people use these locations for forestry.The finis two climates are Tundra and the Icecap which are both cold climates. The Tundra, or ET climate, is located pole guard of the margins and occupies small coastal areas in the Antarctic. The warmest month will only reach 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. Polar bears and some birds can tolerate the coldness of the ET climate and many people use these animals for fur trapping.The 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 message of the tundra, temperatures dont exceed 32 degrees F. There is a sparse amount of precipitation in this climate with only less than 5 in ches all in the form of snow. The cause for these freezing temperatures is mostly the latitude location. Also, the distance from sources of heat cause cold temperatures. There is no soil type here, with no vegetation and no economic activity.