There can be deaths, also, but only 5% of tornado deaths are caused by Weak Tornadoes. The next type is Strong Tornado. Significant Tornadoes (F2), which travel from 113 to 157 miles per hour and Severe Tornadoes (F3), which travel from 158 to 206 miles per hour, are classified as Strong Tornadoes. Theyusually last for about more than 20 minutes and can cause extensive damages: roofs of well-constructed buildings can be ripped off, trains can be overturned, and even large old trees can be uprooted and snapped. Not only properties and nature are damaged, but also human.
Initially, hurricanes are formed over warm water in the tropical oceans and develop best when far from the jet stream while tornadoes are formed over land and formed within storms that are often very close to the jet stream. Other than that, hurricanes can be up to several hundred miles wide while tornadoes are usually not more than a quarter of a mile. Besides that, hurricanes can last up to 3 weeks while tornadoes usually last not more than an hour. Likewise, the strength of the wind of hurricanes are usually 180 mph while the maximum strength of the wind of tornadoes can be up to 300 mph. Additionally, hurricanes occur in the Atlantic Ocean with an average of 10 tropical storms
Within the Loop Current there is warm water that extends fairly deeper than the water surrounding it. Hurricanes usually churn up slightly cooler water allowing for some weakening of the storm; however a hurricane moving over the Loop Current churns up warmer water that extends deeper into the ocean. Camille's extraordinary strength could be blamed in part due to the assumption that it tracked directly up the axis of the Loop Current. After landfall, Camille dropped torrential rains on the southern states with anywhere from 2 to 11 inches of rain. Camille eventually strengthened somewhat as it moved more inland bringing major destruction to the state of Virginia with damage to property and life.
Hurricanes and their impact on the environment The effect of hurricanes on the environment is catastrophic. The loss of life and damage to property and the environment has far reaching implications, for persons that survive these disasters. According to Remote Sensing Using Satellites,(n.d.)”A hurricane is an intense, rotating oceanic weather system that possesses maximum sustained winds exceeding 119km/hr (74 mph). It forms and intensifies over tropical oceanic regions”. Hurricanes normally develop in the Atlantic Ocean, Caribbean Sea, Gulf of Mexico and the North Pacific Ocean.
Tornadoes will occasionally softly "glow" due to lightning discharges in or near them. The sound of a tornado varies widely. It is actually a combination of many different sounds, usually created by rushing air and damage to ground structures. Most commonly, the sound of a tornado is described as a whooshing roar. The temperature is generally lower inside a tornado.
The position of the UK makes storm events an inevitable part of our climate. Located at latitude of 52 to 56 degrees north of the equator, low-pressure systems frequently dominate our weather as cold air from the poles meet warm moist air from the equator. In total, five different air masses compete for control of our weather creating turbulent and unstable air that results in storms. A storm can be defined as ‘a rainfall and wind event that produces more than 0.1 inches of precipitation and which is separated from the previous storm event by at least 72 hours of dry weather’. This essay will firstly discuss the extent to which the impacts of storms in the UK, such as ‘The Great Storm’ of October 1987 in Southern England and the recent St Jude’s storm in October 2013, are the result of physical and human influences, and then evaluate the effectiveness the responses to these storms.
Hurricanes and Tornadoes Hurricanes and tornadoes are the two most deadly storms which hit the United States every year. Often confused with each other hurricanes and tornadoes contribute to over 80 deaths a year. Hurricanes and tornadoes are similar and different in many ways. The experiences of living through a hurricane or tornado can be life changing. Both tornadoes and hurricanes destroy homes, businesses, and take people lives.
The climate is very bipolar though due to varying elevations and winds across the island. The east side of the island has the heaviest amount of rain which equals to about 3.5 meters a year. Not only does this side receive a great amount of rain it is also affected substantially more by the cyclones that wreak havoc on the tropical island. Rain clouds expel so much moisture to the east of the highest grounds the highlands in the central part of the island are much drier and cooler. The downside to the central highlands though are multiple thunderstorms that cause incredible damage due to lighting strikes.
The Effects of Hurricanes Hurricanes also known as Cyclones are amongst the strongest storms on earth, which have plagued man for centuries. Jay Barnes confirms this timeline, with this passage “They are called hurricanes in the Western Hemisphere, a term probably derived from ‘Hurukan,’ the name of the Mayan storm god, and other similar native Caribbean words translated as ‘evil spirit’ or ‘big wind’.” ( 6). Every year, in the summer season, these forces of nature begin to form themselves sometimes less numerous then the year before and sometimes in greater numbers witnessed in a decade. For future reference hurricanes are often named, not only to keep track of them but also people that have experienced them, tend to remember these storms by their name. They are born from tropic waters that affect quite a few across the world but in the Gulf of Mexico they tend to wreak particular havoc.
The heavy rainfall started falling at midday on the 16th August, and it was recorded that 5 inches fell in 8 hours. The storm was a remnant of the Hurricane Alex, which had carried over the Atlantic. The rain was cause due to warm air picking up moisture - due to residual heat from the Atlantic sea - travelled towards the South West Cornish coast as prevailing winds. Upon contact with the topographically vertical coast, these winds experienced a strong up-drafting force thus causing internal moisture to reach the atmosphere, and consequently cool as a string of storm clouds. With convergence and coalescence, enhanced moisture levels resulted in heavy rainfall on the afternoon of 16 August 2004.