A westward moving tropical wave reached the Caribbean Sea in late May and gradually organized over the next few days. Around 00:00 UTC on June 3, a tropical depression developed about 265 miles (425 km) east of Belize City, Belize. The depression initial moved northwestward, before recurving to the north. The depression entered the Gulf of Mexico and strengthened into Tropical Storm Allison by 12:00 UTC. Despite unfavorable upper-level winds, the storm intensified into a hurricane about 24 hours later. Allison then peaked with maximum sustained winds of 75 mph (120 km/h) and a minimum barometric pressure of 987 mbar (29.1 inHg). Increasing wind shear weakened it to a tropical storm early on June 5. At 14:00 UTC, Allison made landfall near Alligator Point, Florida, with winds of 70 mph (110 km/h). After briefly emerging over Apalachee Bay, Allison struck near St. Marks with winds of 65 mph (100 m/h). Early on June 6, Allison weakened to a tropical depression, shortly before becoming extratropical. The remnants continued northeastward and later struck Newfoundland before dissipating near Greenland on June 11.[14] While brushing Cuba, Allison produced wind …show more content…
During the next week, the wave improved on satellite imagery and developed into a tropical depression about 420 mi (680 km) east-northeast of Guadeloupe on July 12. The depression quickly strengthened into Tropical Storm Chantal. Initially, Chantal threatened the Bahamas, and the Government of the Bahamas issued a tropical storm watches and warnings, which were in effect for southeast and central islands as well as the Turks and Caicos Islands. However, Chantal re-curved to the north and did not directly affect the Bahamas. After the cyclone turned northward, it threatened Bermuda, which prompted a tropical storm watch for the island on July 16, which was canceled on July 18 as the storm passed well northwest of the
The development of the storm was initiated by an apparent tropical wave that had given way of the African Coast around August 5th. The cloud pattern of the storm slightly resembled that of an inverted “V” began traveling westward, then northward, across the Atlantic Ocean and was recognized as a tropical disturbance 4 days later, August 9th. The following 5 days or so the storm continued to travel showing no sign of circulation. On August 14th the United States Air Force sent a reconnaissance aircraft into the storm for surveillance, with a growing concern. What was about to be Tropical storm Camille was still south of Cuba with expectation to become much more potent. At the point of infiltration by the aircraft the planes barometer revealed a 999 millibar pressure center with 55 mile an hour surface winds. At this point the disturbance was inaugurated to be a “tropical storm.” As the intensification process ensued, and the squall shifted northwestward at a slow speed of 9 miles per hour, but gained a great amount of force in...
It is truly one of hurricane lore’s greatest storms. Such greatness had innocuous and humble beginnings. Like all hurricanes that have existed, is existing, and will exist, the hurricane originated within the waters of the world and from the winds of the world. The temperate waters of the eastern North Atlantic Ocean gave rise to the storm upon August 31, 1900. Its birthplace is roughly 400 miles west of Africa’s Cape Verde Islands (Longshore).
Most of the destructions from the events of August 29th 2005, when Katrina Hit the City Of New Orleans, were not only caused by the storm itself; but also, by failure of the engineering of the levee system protecting the entire infrastructure of the city. The years of poor decision making and avoidance of the levee system led to one of the most catastrophic events in the history of the United States. Throughout our research, we have identified three key players in charge of the levee system design, construction and maintenance. These three organizations are the Unites States Corps of Engineers, the New Orleans Levee District and the Louisiana Department of Transportation. The consequences of the hurricane showed the organizations negligence in the design, construction and maintenance of the protective walls. Later independent sresearch showed that more than 50 levees and food walls failed during the passage of the hurricane. This failure caused the flooding of most of New Orleans and all of ST. Bernard Parish. The Unites States Corps of Engineers had been in charge of the of the levee system and flood walls construction since the 1936 flood act. According to the law, the Louisiana Department of Transportation is in charge to inspect the overall design and engineering practices implemented in the construction of the system. Once the levee systems were finished, they were handed over to the New Orleans Levee District for regular maintenance and periodically inspections. The uncoordinated actions of these three agencies resulted in the complete failure of a system that was supposed to protect the people of New Orleans. The evidence is clear that this catastrophic event did not happened by chance. The uncoordinated response of these...
Andrew began as a tropical depression in the Atlantic almost a week before hitting South Florida. The next day, which was August 17th , it was the first tropical storm of the season. It was moving with amazing quickness and strength in a west and northwest dire...
Leading up to the hurricane, many scientists expected the storm to dissipate over the ocean and cause little to no harm (Rappaport). The scientists were relying on faulty equipment that said that due to slow air speed and l...
When Hurricane Darby blew through the Hawaiian Islands in late July 2016, it left behind a lot of damage due to flooding and winds on Oahu.
Through the path of history, there have been several major events that influenced thousands of lives and were significant in forming the world today. One of the largest and deadliest events that occurred in history was a disaster not anybody could control or be held accountable for. This was Hurricane Katrina. On the early Monday morning of August 29th, 2005, a Category 5 rating Hurricane Katrina struck the Gulf Coast of the United States with winds up to 175 miles per hour and a storm surge of 20 feet high. Hurricane Katrina was one of the greatest and most destructive natural disasters recorded to make landfall in the United States. The natural causes of the hurricane, poorly structured levees, disaster inside the Superdome, and the
The first few reasons this hurricane was so awful are a few weather conditions. It was raining for four days before it started so there was a lot of high waters. The whole thing got up to 500 miles wide. The flooding got up to 12 to 17 feet and the high 30 to 50 feet waves don’t help the flooding whatsoever.
Dr. Isaac M. Cline was the chief of the U.S. weather Bureau's Galveston station located on the 3rd floor of the Levy Building which can still be found on the corner of Market and 23rd. Cline had begun tracking the storm from the Cape Verde Basin off the western coast of Africa. On August 31, this storm entered the Caribbean and began to increase in size. The hurricane passed just north of Cuba, and on Thursday, September 6, entered the Gulf of Mexico. The projected course would have the storm make landfall well east of Galveston, but on Friday Dr. Cline became worried.
Hurricane Katrina began its formation above the tropical oceans of the Bahamas. As it traveled to Florida, Katrina became classified as a tropical storm, and then a category one hurricane. With its southwestern path, Hurricane Katrina raged to the east portion of...
Hurricane Betsy developed east of the Windward Islands. This means that Betsy occurred in the Atlantic Basin, which includes the North Atlantic Ocean, the Gulf of Mexico, and the Caribbean Sea. Many hurricanes form in this area since it is near the equator and warm water, which is a requirement to form a hurricane is always available. In fact, hurricanes or tropical cyclones can only form if they meet four conditions. First, the temperature of ocean waters must be 82 degrees F or warmer in order. Moreover, low air pressure is needed. Furthermore, you need tropical winds located near the equator. Lastly, you need moist ocean air. The most important part is the warm air since it serves as energy for the storm. The air then rises into the low pressure are and cold air replaces it; this is what then produces what is called a disturbance, which is an area of heavy rainfall, thunder clouds and powerful winds. From here a hurricane can only get stronger and its wind speed is measured and depending on how powerful the storm is it is then assigned into one of five categories.
Hurricanes form over the ocean. Easterly waves, what hurricanes develop from, are long, narrow regions of low pressure which occur in ocean winds called trade winds. At first, these easterly waves can grow into something called, a tropical depression. A tropical depression occurs when winds are up to 31 mph. Then tropical depressions can be upgraded into a tropical storm if the winds reach speeds of 74 mph or less. Then finally a the storm can be bumped up into a hurricane if the winds reach 75 mph.
Every year many natural disasters happen around the world. In New Orleans, and several other states, a devastating hurricane struck. High speed winds and major flooding caused many people to lose their homes and even their lives. Many people have heard of hurricane Katrina, but not everybody knows what caused it and the affect it had on the United States.
That eye would break the record for lowest recorded pressure for an Atlantic hurricane that did not reach category 5, at 919 millibars, until Hurricane Opal in 1995 (National Weather Service). When winds, rain, and debris faded to quiet, my father, along with my grandma and most of the neighborhood, decided to walk outside and look around. It did not last long- thirty years later, he estimates about 15 minutes at most. It was eerie and unsettling, as he described it: “The lighting was all wrong- it was like a scene from a horror movie. I was waiting for the guy in the mask to pop out.” They could see the debris that had been thrown around, and the storms in the distance. Soon enough, the winds started to pick back up, and everyone hurried back
Hurricanes occur all over the world, at different times, but commonly through June first and late November. However in late August 2005 a catastrophic hurricane struck. This was Hurricane Katrina. With winds traveling over one hundred miles per hour making it a category five on the Saffir- Simpson Hurricane Scale it was said to have cause billions of dollars’ worth of damage. Hurricane Katrina flooded nearly forty thousand homes, and killed at least two thousand people (“Hurricane”). An average category five hurricane has enough energy to power street lamps for more than twenty seven thousand hours (Williams 58). Knowing about Hurricane Katrina, and the devastation of the city in New Orleans would be beneficial. Also, general information on hurricanes can help civilians and people of higher authority better understand and prepare for damage that could once hit their town and community. Because experts know the general information on these storms they can help explain to the public why and how Hurricane Katrina and other hurricanes occur. Hopefully, in the future civilians will know and use this information to their advantage against hurricanes.