Wind Damage >> Tropical Hurricane Hugo Storm Damage

Hurricane Hugo in 1989 was the most powerful Tropical Hurricane Hugo Storm Damage and rainstorm to hit the United States since 1969 when Camille hit the Gulf Coast. Hugo was disastrous and caused extensive residential wind damage, widespread lifeline annihilation, and massive timber devastation in South Carolina. The rainstorm flow from Hurricane Hugo was, at 20 feet, the highest to hit the East Coast this period.

  1. Hugo produced $1 billion in Tropical Hurricane Hugo Storm Damage for each of the six hours it moved through South Carolina. Hugo started as a tropical storm on September 10, 1989, 12 days before coming across the South Carolina coast. With wind speeds of up to 160 mph, Hugo was classed as a category 5 hurricane. Soon before midnight on September 22, Hugo, now a category 4 rainstorm with continued winds diminished to 135 mph, came across the South Carolina coast just north of Charleston. Hugo's most powerful Tropical Hurricane Hugo Storm Damage now were limited to the Bulls Bay area 25 miles northeast of Charleston.
  2. Winds there gusted up to 144 mph. Hurricane winds covered 100 miles northeast, and 50 miles south. A rainstorm tide of nearly 20 feet flooded the coast as far north as Myrtle Beach. The eye of Hugo passed just east of Columbia, South Carolina, 100 miles inshore, at 3:00 a.m. with winds of 109 mph. By sunrise Hugo, now a tropical rainstorm, had reached Charlotte, North Carolina, with Tropical Hurricane Hugo Storm Damage still gusting to 87 mph. South Carolina suffered extensively damage, but little loss of life. Thirteen of the 49 deaths ascribed to Hugo were in South Carolina.
  3. The low death toll was a outcome of timely warnings and clearings. One interesting feature of the wind damage caused by Hugo was the volume of wind damage to trees. There were many regions where the Tropical Hurricane Hugo Storm Damage caused considerable damage to trees, while wind damage to houses was small. The main cause for this was that the main tree in the area is pine; pine trees tower 30-40 feet above the earth, where the wind speeds are greater than at ground level. The pine trees served as a wind block that kept the wind from damaging many buildings. Instead, houses were damaged by broken trees and branches.
  4. In general, more buildings seemed to have profited rather than suffered from the Tropical Hurricane Hugo Storm Damage trees. Hurricane Andrew was the most damaging natural disaster in U.S. history in relationship to property loss. Andrew started as a tropical rainstorm on August 17, 1992. By August 22, Andrew was a negligible category 1 hurricane, 800 miles east of Miami. Andrew increased quickly, and less than a day later was a powerful category 4 rainstorm with winds of 135 mph. That very same afternoon, winds intensified to 150 mph, Andrew's highest sustained winds, and near category 5 in power.
  5. Andrew was now 330 miles east of Miami, and hurricane warnings went up from Vero Beach, Florida, south to the Keys. On August 24, Andrew hit Florida with continued winds of 145 mph.Tropical Hurricane Hugo Storm Damage to Florida farming alone was over $1 billion. One hundred seventeen-thousand homes were wind damaged or demolished and 90% of all homes in Dade County had major roof damage. Only 41 deaths were credited to Andrew, thanks to mass departures prior to Andrew making landfall.Though the rainstorm created a high rainstorm flow and high winds, water damage was limited to a small part of the coastal floodplain.
  6. Consequently, the flood damage from Andrew, not like many rainstorms of its size, was small. Wind damage was customary, though. Andrew caused considerable wind damage to both residential houses and commercial edifices in southern Dade County, Florida.Andrew was a powerful Tropical Hurricane Hugo Storm Damage but compact rainstorm. Major Tropical Hurricane Hugo Storm Damage to buildings was restricted to an area bordered by Homestead to the south, Coral Gables on the north, the Everglades on the west, and Biscayne Bay on the east. Yet again, rainstorm water damage from Andrew was negligible when matched to Hugo.
  7. Rainstorm flow higher than 10 feet covered about 10 miles north of Andrew's landfall, though the same flow elevation covered 100 miles north of landfall for Hurricane Hugo. Though Andrew created high winds and a high rainstorm flow, the results of the rainstorm Tropical Hurricane Hugo Storm Damage and wave achievement were limited to a small area of the coastal floodplain.Flood damage was negligible for a rainstorm as big as Andrew, although landfall happened at high tide. The highest rainstorm flow observed was 16.9 feet at Cutler Ridge, about 20 miles south of Miami.
  8. The flow lessened off quickly, and was only five feet at the north end of Miami Beach. Coastal flooding was restricted to a few spots in Key Biscayne, and a few canal-front cities along the coast off Cutler Ridge. No considerable beach Tropical Hurricane Hugo Storm Damage was credited to Hurricane Andrew. This might have been the cause of the compactness of the rainstorm and the overall speed at which it moved inland.Hurricane Iniki was one of the most violent and devastating rainstorms to hit Hawaii in recent history. Iniki's central barometric pressure of 938 mb was the lowest ever logged in a central Pacific hurricane.
  9. A small and compact rainstorm like Andrew, Iniki started as a tropical rainstorm on September 7, 1992, and turn into a hurricane a day later. Iniki followed a Tropical Hurricane Hugo Storm Damage trail that traditionally had carried hurricanes south of the Hawaiian Islands, but a low pressure depression turned the rainstorm northward and into the island of Kauai on September 11. By the time Iniki occurred over the north shore of the island and back out to sea two hours later, over 90% of all edifices on the island had been wind damaged, ranging from minor Tropical Hurricane Hugo Storm Damage to complete destruction.
  10. Iniki produced $3 billion in Tropical Hurricane Hugo Storm Damage in two hours. Over 14,000 homes were wind damaged or demolished. Wind damage was most unyielding on the north, south, and east ends of the island. In spite of the prevalent wind damage, only three deaths were credited to the rainstorm, thanks to sufficient warning and withdrawal.Hawaii is a mountainous state, not like Florida and coastal South Carolina. This complicated topography produced extremely complex wind-flow designs that resulted in high restricted wind speeds, which worsened the destruction in certain areas. According to experts, one 227 mph gust was recorded over one of the higher mountain ridges.
  11. Topological wind intensification caused heavy Tropical Hurricane Hugo Storm Damage to houses erected along the island's cliffs in parts such as Princeville on the north shore of the island.Iniki created a considerable rainstorm flow and consistent wind damage. The geology of the Hawaiian Islands provided to one unusual result, Tropical Hurricane Hugo Storm Damage to houses from wave-borne suspended volcanic rock.Coastal flooding was sizeable along the southern beach from Kekaha to Poipu beach. Still-water flood advancements varied from 10.5 to 12.5 feet above mean lower low water (mllw) at Kekaha to 12.5 to over 20 feet above mllw along Poipu Beach.

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