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United States
The U.S. Hurricane model incorporates unique and innovative techniques for developing and validating hurricane models that have lead the state-of-the-art in modeling. The model is the first to fully represent the physical processes of hurricanes that impact the United States, simulating realistic behavior throughout a hurricane's life cycle. RMS has addressed the challenges of modeling the unique features of the United States coastlines through a combination of innovative modeling methodologies, insightful interpretations of historical and meteorological information, and extensive high resolution geophysical data. Furthermore, through its relationships with the leading property insurers in the U.S., RMS has accessed the wealth of knowledge embedded in claims files for numerous hurricanes to validate its models. Model Highlights
Geographic Scope The RMS® U.S. Hurricane Model covers the entire U.S. Eastern Seaboard, Gulf Coast, and Hawaii. Specifically, the states included in the model are: Alabama, Connecticut, Delaware, District of Columbia, Florida, Georgia, Hawaii, Louisiana, Maine, Maryland, Massachusetts, Mississippi, New Hampshire, New Jersey, New York, North Carolina, Pennsylvania, Rhode Island, South Carolina, Texas, Vermont, Virginia, and West Virginia. Exposure Data Resolution The Hurricane model supports analyses at each of the following levels of geographic resolution: Latitude/Longitude, Street Address, ZIP Code, City, and County.
Earthquakes can occur throughout the United States, as demonstrated by historical records and geological research. As such the RMS Earthquake Model covers all 50 United States, including high-risk regions such as California and the New Madrid Seismic Zone. In 2003 the western U.S. earthquake model was updated with source modeling representing the latest research, high resolution geotechnical data, and underwriting capabilities using the most advanced approach available for modeling building damage. Model Highlights Included in 2003 Western U.S. Update
Geographic Scope The U.S. Earthquake model is discretized into 11 distinct regions which are comprised of individual states or groups of states. Each region reflects the unique characteristics of seismic hazard in different parts of the U.S. The regions are Alaska, California, Great Basin, Hawaii, Midwest, Central U.S., Northeast U.S., Northern Rockies, Southeast U.S., Southern Rockies, and Pacific Northwest. Exposure Data Resolution The RMS Earthquake model supports analyses at each of the following levels of geographic resolution: Latitude/Longitude, Street Address, ZIP Code, City, and County.
Winter storms in the U.S. are complex, extra-tropical weather systems that can produce various types and combinations of damage from the perils of snow, ice, freezing temperatures, and extra-tropical winds. The combination and intensity of the winter storm perils at a particular location are governed by the location of the storm origin, the region impacted, and the large-scale weather pattern. Winter storms that impact the U.S. can be generally characterized as follows:
Winter Storm Risk Winter storm losses are a key component of the total natural catastrophe risk in the U.S. contributing an estimated 10% of the overall average annual loss in the U.S. Winter storms are the key driver of risk to regions such as the Pacific Northwest and the northeast U.S. Several historical winter storms have highlighted the potential winter storm risk across the U.S. with events such as the 1962 Pacific Northwest Windstorm, the 1983 Freeze Outbreak, and the 1993 Superstorm, which was arguably the costliest winter storm to impact the U.S. with insured loss estimates of $US1.75 billion at the time of the event. From March 12-14, 1993, a powerful extra-tropical storm descended upon the eastern half of the United States, causing widespread damage from the Gulf Coast to Maine. The storm spawned tornadoes in Florida, caused record snowfalls across the Appalachian Mountains and Mid-Atlantic states, hurricane-force wind speeds along the coast, and extremely low temperatures throughout the region. Model Highlights
Geographic Scope
Exposure Data Resolution
The unique geography of the United States contributes to the highest annual frequency of severe convective storm occurrence in the world. The risk associated with severe convective storms—destructive storms including thunderstorms, tornadoes, and hailstorms—results in average annual insured losses of approximately $11 billion in the U.S., comparable to insured losses from hurricanes and about three times that of insured losses from earthquakes. Since 1994 the RMS® U.S. Severe Convective Storm Model (formerly the Tornado/Hail Model), has been utilized by the insurance and reinsurance industry to evaluate and transfer risk associated with these types of severe convective storms. The model considers risk from tornadoes, hailstorms, damaging straight-line winds, and lightning for the contiguous 48 states. The U.S. is located within the mid-latitudes (35-65° N), a region where strong horizontal variations in temperature accompanied by large vertical variations in wind speed create a volatile mix of ingredients for storm formation. Two primary mechanisms spawn severe local storms. The first, common throughout the Central Plains, the Midwest, and much of the South, occurs when abundant moisture originating from the Gulf of Mexico meets cool, dry air from the north along boundaries such as cold fronts. Severe storms develop along these boundaries with highest frequency during the spring and summer months. A second type of storm formation is more common on the eastern slopes of the Rocky Mountains and in the southern Plains, where warm, dry air originating in the higher elevations descends atop moist air at the surface. Storm initiation occurs as the moist air is forced upward through the mass of dry air, particularly in areas of rapidly increasing elevation. Tornadoes, hail, and straight-line winds have been observed in each of the contiguous 48 states and can occur at any time of year, most frequently from March to September. The annual frequency of tornadoes, hail, and straight-line winds is highest in the Central Plains, Midwest, and southern U.S. Risk decreases gradually to the north and east and there is a sharp decrease in risk in the western U.S. Some recent notable hail and tornado events are summarized below.
*Values are for property damage only. Source:
Property Claims Services Model Highlights
Geographic Scope The U.S. Severe Convective Storm Model covers the 48 contiguous states, comprising all areas of the United States with significant tornado, hail, and straight-line wind risk. Exposure Data Resolution Exposure data may be entered at county, ZIP Code, street address, or latitude/longitude level of resolution. Model analysis is performed based on a variable resolution grid, with greatest resolution in metropolitan areas with high exposure to severe convective storm hazard. |
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