ThunderJoin now to read essay ThunderThunderstorms occur throughout the world, even in the polar regions, with the greatest frequency in tropical rainforest areas, where they may occur nearly daily. Kampala and Tororo in Uganda have each been mentioned as the most thunderous places on Earth,[8] an accolade which has also been bestowed upon Bogor on Java, Indonesia or Singapore. Thunderstorms are associated with the various monsoon seasons around the globe, and they populate the rainbands of all tropical cyclones (typhoons, hurricanes, etc.) In temperate regions, they are most frequent in spring and summer, although they can occur along or ahead of cold fronts at any time of year. They may also occur within a cooler air mass following the passage of a cold front over a relatively warmer body of water. Thunderstorms are rare in polar regions due to cold surface temperatures.
The tropical rainforests of the Southern Indian Ocean, Central and South America, Western South Asia, Antarctica, New Guinea, and the Atlantic, as well as other tropical rainforests, have long been thought to possess a thunderstorm-like atmosphere that has been associated with the onset and progression of tropical cyclones.[9] An estimated 1.4 million people in central and southern Africa and more than 800,000 people in the Amazon region have used various environmental factors, such as wet soil, rainfall and wind patterns, to predict the onset and pattern of tropical cyclones.[5][5][10][11]
The annual thunderstorms occur from early October through early December in Australia, New Zealand and several Western countries.[12][13] The storm, named the Okeanos, was known to the authorities in Fiji, Indonesia and the Philippines in 2013, but it was subsequently banned in both Fiji and Hong Kong in the U.S., and was subsequently reintroduction into the Pacific.[4] Thunderstorms, if they are observed during the storm season, are a common occurrence in coastal areas and can occur during the period when tropical cyclones usually strike. These events are a consequence of a lack of water from the ocean during tropical cyclones, and an active weakening and weakening of rainforests along the tropical front during thunderstorms.[14]
In most temperate areas, where thunderstorms are most common in this location, as they are often associated with thunderstorms in the Southern Alps. Thunderstorms in the Alps do not occur in tropical cyclones much more often, as there is a relatively high rate of thunderstorms in these areas, with about 10 to 20 thunderstorms per minute.[15]
Thunderstorms cause the rainforest system to develop and produce the rain in rain forest areas during early morning hours, when the cold air has been deposited by an unusually cold wind (which is responsible for some of the rainfall during the monsoon). Within this initial period of weather, moisture is stored within the rainfowl and it absorbs and protects the air between the cold front and the cooler part of the region.[16][17] Thunderstorms are often associated with the onset of other storm-like climatic events, such as hurricanes, cyclones (such as Hurricane Irene in the Pacific), and droughts; while thunderstorms can occur over much of the Northern Hemisphere, with occasional occurrence in Europe.
In northern and central Central America, where lightning is a major concern, this term is used to refer to a storm that brings hail in the middle of the morning, resulting in a thunderstorm in the vicinity of a tree that is often torn off by falling trees and is a powerful “wind-like, thunder” instrument. Rainforest fire infestations are common in these regions (see Category 2), primarily in southeastern Peru, the Amazon, and south-east Asia and the Middle East.
Storms, also sometimes referred to as droughts, are rare and extremely deadly as a result of atmospheric warming, or by a combination of the effects of more heat, less rainfall, and changes in the earth’s atmosphere, usually at the direction of wind speed. In tropical rain forest areas, storm-like cyclones of up to 20 feet can occur, along with massive thunderstorms in those areas, with temperatures as low as 150F (38C) in the Northern Hemisphere in May, as predicted by the National Snow and Ice Data Center, which reports a total of 18 different major precipitation storms, including 2 inches (3.6 cm) of rain, from May 6 through May 30.
In central and eastern tropical rain forest areas, however, hail, droughts, mudstorms, and tropical cyclones are common. In addition, thunderstorms caused by droughts usually result from a combination of thunderstorm or drought conditions, which causes increased precipitation that also occurs over a shorter time period.[5] In some parts of northeastern North America, such as Texas and Oklahoma, thunderstorms also create extreme humidity in places, and severe flooding in urban areas that are likely to result in power outages.
In many places in northern and central North America, thunderstorms may be seen on the ground outside the homes of some residents or nearby property owners, or they may also occur as part of a direct response effect of rainfall, such as a heavy rain which may be associated with a hurricane or an ongoing lightning strike.[15] In some sections of Alaska and North America, where meteorological conditions may not be favorable, thunderstorms may be reported as being a result of lightning, but this does not mean that the effects of lightning tend to be limited by the area, as in southern Florida or Florida which experienced more rain in 2013.[18]
In some areas of southeastern North America, during the winter months of July and August, thunderstorms can occur as a result of tornadoes or droughts that are caused by a hurricane,[19] or even as rain from a tornado.
In certain parts of the United States, thunderstorms are known to be due to hail and thunderstorm activity, and sometimes in areas where a power line is suspended. In rural areas where thunderstorms are known
In northern and central Central America, where lightning is a major concern, this term is used to refer to a storm that brings hail in the middle of the morning, resulting in a thunderstorm in the vicinity of a tree that is often torn off by falling trees and is a powerful “wind-like, thunder” instrument. Rainforest fire infestations are common in these regions (see Category 2), primarily in southeastern Peru, the Amazon, and south-east Asia and the Middle East.
Storms, also sometimes referred to as droughts, are rare and extremely deadly as a result of atmospheric warming, or by a combination of the effects of more heat, less rainfall, and changes in the earth’s atmosphere, usually at the direction of wind speed. In tropical rain forest areas, storm-like cyclones of up to 20 feet can occur, along with massive thunderstorms in those areas, with temperatures as low as 150F (38C) in the Northern Hemisphere in May, as predicted by the National Snow and Ice Data Center, which reports a total of 18 different major precipitation storms, including 2 inches (3.6 cm) of rain, from May 6 through May 30.
In central and eastern tropical rain forest areas, however, hail, droughts, mudstorms, and tropical cyclones are common. In addition, thunderstorms caused by droughts usually result from a combination of thunderstorm or drought conditions, which causes increased precipitation that also occurs over a shorter time period.[5] In some parts of northeastern North America, such as Texas and Oklahoma, thunderstorms also create extreme humidity in places, and severe flooding in urban areas that are likely to result in power outages.
In many places in northern and central North America, thunderstorms may be seen on the ground outside the homes of some residents or nearby property owners, or they may also occur as part of a direct response effect of rainfall, such as a heavy rain which may be associated with a hurricane or an ongoing lightning strike.[15] In some sections of Alaska and North America, where meteorological conditions may not be favorable, thunderstorms may be reported as being a result of lightning, but this does not mean that the effects of lightning tend to be limited by the area, as in southern Florida or Florida which experienced more rain in 2013.[18]
In some areas of southeastern North America, during the winter months of July and August, thunderstorms can occur as a result of tornadoes or droughts that are caused by a hurricane,[19] or even as rain from a tornado.
In certain parts of the United States, thunderstorms are known to be due to hail and thunderstorm activity, and sometimes in areas where a power line is suspended. In rural areas where thunderstorms are known
History
The formation of the tropics during the time of the Pleistocene and Neogene was primarily a major process by which temperate and tropical regions first emerged. Although the climate changed, the earliest known recorded record indicates that the tropics expanded around about two billion years ago,[18] with early hominid dinosaurs in North America, and during Asia’s second and fourth centuries BC, Homo sapiens expanded northward and began to live in the Americas[19] and Australasia.[20][21] However, early hominid species continued to survive as part of the global community, and by that time most regions had become flooded during the period. These hominid populations eventually dispersed to the subarctic,[22] possibly migrating westward from a single island in the north-eastern half of the world to what appears to be Central America (probably North America) as far south as Brazil (possibly Australia).[23] Around this time, Homo sapiens began migrating to the Amazon Ocean, which formed a new core zone around the present day South
The most powerful and dangerous severe thunderstorms also occur over the USA, particularly in the Midwest and the southern states. These storms can produce very large hail and powerful tornadoes. Thunderstorms are relatively uncommon along much of