Atlantic hurricane seasons have a long history of creating devasting storm damage causing significant financial impacts. Between 100 and 200 kilometers from the eye, the winds are fast enough to qualify as tropical storm force. Researchers applied a dataset of normalized hurricane damage, looking at historical hurricane damage and adjusting that data to determine how much damage might occur today given changes in population, inflation and wealth. Based on the proposed pressure scale, Sandy would have been a Category 4 hurricane.Sandy's enormous size – more than 850 miles in diameter – drove a catastrophic storm surge into New York and New Jersey.Superstorm Sandy caused $65 billion in damage in the mid-Atlantic and in the Northeast, currently the The study also found that the relationship between wind speeds at landfall and damage weakens as you move farther north along the U.S. East Coast, while the relationship between minimum pressure and damage remains strong. In 2009, the NHC made moves to eliminate pressure and storm surge ranges from the categories, transforming it into a pure wind scale, called the Saffir–Simpson Hurricane Wind Scale (Experimental) [SSHWS]. This is likely because hurricanes typically grow in size as they gain latitude, meaning pressures are usually lower for hurricanes at a higher latitude for storms with similar wind speeds (i.e., a Category 1 hurricane (using the current SSHWS) off the coast of the Northeast will generally have a lower pressure than one in the Caribbean).The authors of the study state, "While no scale will ever perfectly account for the totality of storm risk to life and property (e.g., inland flooding), any improvements to better explain and warn the potential hurricane impacts to an increasingly vulnerable coastal and inland population is, in our view, a worthwhile endeavor.
A hurricane with wind speed 35 m/s is acting on a 10 m 2 wall. Hurricanes Harvey, Irma, Maria, Florence, and Michael combined to incur more than $345 billion (USD) in economic damage during 2017 and 2018. The Tropical Meteorology Project team at Colorado State University, along with colleagues at NOAA, North Carolina State University, Aon and UCAR set out to analyze existing data to assess what may be a more accurate factor in predicting hurricane strength and damage post-landfall. While pressure and wind speed are strongly correlated, pressure is more of an integrated quantity that assesses the “strength” of the storm, as opposed to just the maximum wind speed at any point in the storm’s circulation. This was the third-lowest pressure for a landfalling Category 2 since 1900.The best example of a SSHWS failure (along with its giant communication failures) was Hurricane Sandy, better known as Superstorm Sandy. Consequently, the maximum winds can be somewhat weaker, but these hurricanes often have low minimum sea level pressure (MSLP) and present the likelihood of significant damage upon landfall. Or - from the table above the wind load per square metre is 735 N/m 2. Hurricane storm characteristics that inflict damage are not isolated to just the maximum wind speed.
In general, damage rises by about a factor of four with every category increase.However, hurricanes with large wind fields can produce storm-surge heights that are much higher than is average for a given category, as was the case with Category 2 Hurricane Ike in 2008.Conversely, very compact hurricanes – even if extremely strong windwise and with very low central pressures, as was the case with Hurricane Charley in 2004 – can produce surges substantially lower than what was included in the original scale.This scale does not account for how much rainfall or how many tornadoes a hurricane will produce, either.Tropical storms can create more damage than Category 5 hurricanes in some cases – Tropical Storm Allison in 2001, for example.Smaller changes to the scale regarding translations to knots were made in 2012.The SSHWS has been tweaked since its inception, and conceivably will be changed in the future, perhaps with pressure in mind once again.We recognize our responsibility to use data and technology for good. Sea-level pressure, however, is more directly related to all threats in a hurricane's arsenal. Air pressure inside a hurricane measures the storm’s intensity. The lower the pressure, the stronger the storm.
Air pressure inside a hurricane measures the storm’s intensity. This scale estimates potential property damage. Superstorm Sandy was extremely large when it made landfall in New Jersey in late October 2012. For instance for a central pressure of 920 mb I've observed it's possible to have both 145 mph and 170 mph wind speed for two different storms. While Sandy became post-tropical just before making landfall, its category using MSLP immediately before landfall indicated a much more powerful hurricane than would have been anticipated by its Vmax. A larger storm is also more likely to bring damaging hazards to larger population centers.Two examples of failures by the current SSHWS are Hurricane Ike in 2008 and Superstorm Sandy in 2012.Hurricane Ike was a Category 2 on the SSHWS but had a pressure of 950 millibars when it arrived on the Texas coast. Over 1,500 fatalities occurred in Louisiana from Katrina due to storm surge and associated failure of the levees. If Ike had been classified using pressure, it would have been a Category 3 hurricane, elevating Ike to major (Category 3+) hurricane status and giving residents additional cause to take preparedness actions. Sandy caused over $65 billion in damage, making it the third costliest U.S. hurricane on record – trailing only Katrina (2005) and Harvey (2017).Ironshore distinguishes itself in the industry by closely aligning our claim professionals with members of the underwriting, actuarial and finance teams.
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