Weathering the Storm. Steve Drews, Impact Forecasting & Paul Eaton, Aon Benfield Analytics Analytics Insights Conference July 22-24
|
|
- Allan Dean
- 6 years ago
- Views:
Transcription
1 Weathering the Storm Steve Drews, Impact Forecasting & Paul Eaton, Aon Benfield Analytics 2014 Analytics Insights Conference July 22-24
2 Agenda Section 1 Section 2 Section 3 IF s New Historical Severe Thunderstorm Model: STS RePlay Experience Analysis Enhanced Tornado Viewing Guide 2
3 Agenda Tracker Section 1 Section 2 Section 3 IF s New Historical Severe Thunderstorm Model: STS RePlay Experience Analysis Enhanced Tornado Viewing Guide 3
4 Why Not are enough the current emphasis severe thunderstorm stochastic on or a lack of recent catastrophe models so far off historical with their AAL hazard values???? data 4
5 Annual Severe Weather Frequency By Different Periods Average Annual SPC Reports: All Tornadoes Average Annual SPC Reports: All STS Perils 35,000 Reports / Year 28,642 29,638 30,000 26,931 25,000 20,000 15,000 11,271 10,000 5, Reports / Year 1,500 1,284 1,283 1, , Average Annual SPC Reports: All Hail Reports / Year 15,000 12,588 13,461 13,858 10,000 5,206 5,000 0 Average Annual SPC Reports: All Convective Wind Reports / Year 20,000 13,059 13,898 14,444 10,000 5,
6 Annual Severe Weather Frequency: Tornadoes The vast majority of tornado frequency increase stems from weaker (and not as easily detectable) tornadoes Note: 2013 lowest tornado total since
7 Annual Severe Weather Frequency: Hail The vast majority of hail frequency increase stems from smaller hail occurrences 7
8 Annual Severe Weather Frequency: Wind Both weaker AND stronger thunderstorm-produced winds continue to show frequency increases 8
9 What if there was a severe thunderstorm catastrophe model that would more accurately predict my AAL? Well, now there is 9
10 New IF ELEMENTS Severe Thunderstorm Tool: STS RePlay Based on recent historical data obtained from the Storm Prediction Center Contains last 10 years of severe thunderstorm activity Contains tornado, hail and convective wind occurrences Recent historic experience contains a richer catalog of activity based on better data capture using Doppler radar and other technological advancements ELEMENTS STS RePlay event set Can be used for a replay of a large catalog of historical daily outbreaks to better understand loss behavior A replay of historical event catalog against current exposures allows a recast to current loss expectations RePlay catalog can be used for obtaining a view of average yearly losses as an alternative to Average Annual Losses produced by stochastic models Note: the scenario set is not a replacement for stochastic models, but is an alternative recast view using actual historical experience 10
11 STS RePlay Source Data Source data: Storm Prediction Center Local Storm Reports (LSRs) Gathered from trained storm spotters, emergency managers, law enforcement, automated weather stations and Doppler Radar Three types of severe weather data gathered All tornadoes Hail 1 or greater Convectively-induced (thunderstorm-produced) winds of 58 mph or greater Reports characterize severe weather occurrences Date and time, location (lat/long), etc. Intensity, damage, etc. Data used Total of 260,610 LSRs analyzed and converted into ELEMENTS format after initial filtering (hail below 1, winds below 58 mph, reports with incomplete data) 11
12 STS RePlay Input Data Occurrence Counts Tornadoes: 13,764 (average 1,376/year) Hail: 125,924 (average 12,592/year) Wind: 120,922 (average 12,092/year) 12
13 STS RePlay Event Set Generation Hail and Wind Data usage within SPC LSR database files Start coordinates Hail Size Wind (knots) Directionality calculated as a random number due to the uncertainty of the direction (i.e. no end coordinates) Path Length and Path Width calculated as a random number based on average, lower bound, upper bound, and standard deviation values given within the ELEMENTS Severe Thunderstorm Model stochastic event set for each hail size bin (0-5) and wind intensity bin (0-3) Hail Size calculated using hail size provided by SPC and converted from inches to millimeters If hail size is less than 1 (25.4 mm), data is not used Wind intensity calculated using wind speed provided by SPC and assigned to Fujita Scale If wind intensity is less than 50 knots (58 mph) data is not used 13
14 Special Considerations For Wind and Hail SPC Reports Limited to point estimates No end coordinate reported in SPC data No data on swath shape (length, width) SOLUTION: Implement current inplace Impact Forecasting research on characterization of hail and wind swaths Multiple Hail Reports Multiple reports could represent portions of same event swath Overlapping swaths over-count losses SOLUTION: Bin events by report time (5 minute increment) and spatial proximity (0.6 mile increment) and treat similar reports as duplicates of the previous reports Single Hail Swath 14
15 STS RePlay Event Set Generation Tornadoes Data usage within SPC LSR database files Start and end coordinates Intensity (Fujita Scale/Enhanced Fujita Scale) Path Length (verification only) Path Width Directionality calculated by utilizing the start and end coordinates given by SPC data Path Length calculated by utilizing the start and end coordinates given by SPC data and converted into kilometers Output verified by SPC data values Path Width (maximum) taken directly from SPC data and converted into meters (given in yards) 15
16 Special Considerations For EF3+ Tornado SPC Reports Strong to violent tornadoes (EF3+) often long lived with complex track shape and varying intensity Example: Joplin, MO 5/22/2011 EF5 tornado SPC LSR data characterizes start and end coordinates and single intensity rating Example: Joplin EF5 as straight line between SPC start and end coordinates 490 EF3+ events in data set All 490 EF3+ events researched Majority didn t have detailed information 28 EF3+ tornado tracks modified Ad hoc research for event shape and intensity (NWS-sourced official track data) Re-parameterized events as necessary for proper representation within event set 16
17 Hazard Uncertainty Two mile tolerance for coordinate accuracy creates uncertainty in LSR event location Street-level addressing not available cross-street coordinate assignments most likely SOLUTION: Sample every LSR 25 times, adding position uncertainty 5% position uncertainty for tornadoes (more accurate reporting) 20% position uncertainty for hail and wind 6.5 million event set generated in ELEMENTS from 260,610 individual LSRs 17
18 STS RePlay Results Verification Comparison of Severe Convective Storm Models To Actual Client Historical AALs Client Client Size* IF STS RePlay to Actual Stochastic Model A to Actual Stochastic Model B to Actual Stochastic Model C to Actual A Large B Large C Small D Small E Large n/a F Large n/a Weighted Average * Large client actual loss approx. 10x small client actual losses 18
19 IF ELEMENTS STS RePlay Summary Designed only as an alternative AAL view using rich data due to technological improvements in data capture and an overall active severe convective weather period Contains historical SPC occurrences of tornadoes, hail and convective winds from active 10-year period Each severe weather occurrence is sampled 25 times to account for hazard position uncertainty Reports were analyzed spatially and temporally to eliminate duplicate reports Significant tornadoes were analyzed and modified (where information existed) to better represent the overall track and intensity fluctuations that EF3+ tornadoes often exhibit Over 6.5 million severe weather occurrences are contained within the STS RePlay event set Official Release: September 2014 (in coordination with new IF STS Stochastic Model) 19
20 Agenda Tracker Section 1 Section 2 Section 3 IF s New Historical Severe Thunderstorm Model: STS RePlay Experience Analysis Enhanced Tornado Viewing Guide 20
21 What if I Instant Have Need Want Want Don t noisy to a have realistic see quantifiable data Derrick experience credible that assessment makes Rose basis loss that fast for trend of experience selections my comparing break represents average through and because stochastic annual on-leveling my the current I ve loss entire model grown from very Mavericks underwriting severe output into new thunderstorms? difficult? to defense experience? regions? paradigm? again? 21
22 Severe Weather Experience Templates Superior Trend Diagnostics Daily Incurred Losses Log Scale 100,000 10,000 Loss Thousands 1, Trend: 8.2% 1 Jan-98 Jan-00 Jan-02 Jan-04 Jan-06 Jan-08 Jan-10 Jan-12 Date Daily Average Severity Log Scale Trend: 9.1% Trend: 0.0% 100,000 Daily Claim Counts Log Scale 10,000 10,000 Severity 1,000 Claims 1, Jan-98 Jan-00 Jan-02 Jan-04 Jan-06 Jan-08 Jan-10 Jan-12 Date Trend: 8.1% 10 1 Jan-98 Jan-00 Jan-02 Jan-04 Jan-06 Jan-08 Jan-10 Jan-12 Date Trend: 0.2% 22
23 Severe Weather Experience Templates Analysis Of Daily Loss Data Automated Aggregator of Events Per Occurrence XOL & Aggregate Structure Analysis Cat XOL Aggregate Optimization of Program Co-Part 5% Per Event Deductible 2,000,000 Limit 210,000,000 Deductible Type Standard Trended Retention 20,000,000 Per Event Limit 18,000,000 Selected Occ Ceded Max ceded through day n assuming an event ends on Max ceded Events, Gross Event Loss to Event Loss to Incurred AccidentDate DOY 96 Hour Total Regular XOL Loss Regular XOL Franchise XOL Ceded Loss Total Ceded day n through day n of Reinsurance Per Occ Layer Agg Layer 31, Jun , ,128,895 3,128, , Jun , ,128,895 3,128, , Jun , ,128,895 3,128, , Jun , ,128,895 3,128, , Jun , ,128,895 3,128, , Jun , ,128,895 3,128, , Jun , ,128,895 3,128, ,286, Jun ,522, ,522,215 7,522,215 5,522,215 5,522,215 8,651,110 8,651,110 7,522, ,522, , Jun ,457, ,457,260 7,457,260 5,457,260 5,457,260 8,586,156 8,651, , Jun ,491, ,491,894 7,491,894 5,491,894 5,491,894 8,620,789 8,651, , Jun ,521, ,521,013 7,521,013 5,521,013 5,521,013 8,649,908 8,651, , Jun , ,651,110 8,651, ,402, Jun ,593, ,758 2,593, , ,758 9,244,868 9,244,868 2,593, ,758 23, Jun ,549, ,545 2,549, , ,545 9,200,655 9,244, , Jun ,510, ,226 2,510, , ,226 9,161,336 9,244, , Jun ,503, ,044 2,503, , ,044 9,154,154 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, , Jun , ,244,868 9,244, IF RePlay Losses by day tracking Initial step to aggregate into 3 day step cumulative totals before and after an aggregate deductible Aggregation of daily losses via local optimization rule 23
24 Agenda Tracker Section 1 Section 2 Section 3 IF s New Historical Severe Thunderstorm Model: STS RePlay Experience Analysis Enhanced Tornado Viewing Guide 24
25 TVG Concentrations Are Tornado-Track Based TVG uses scenario or What if analysis Example: what if the Moore, OK tornado from 2013 hit other exposure concentrations St. Joseph Columbia Kansas City Sedalia St. Louis 2013 Moore, OK EF-5 Track Cape Girardeau Springfield Poplar Bluff 25
26 Accumulations By Census Statistical Area Metropolitan Micropolitan Rural Joplin, MO 2011 Historical Tornado Track Fayetteville Springdale Rogers, Conditional Kansas City, MO KS St. Joseph, MO KS Cape Girardeau Jackson, MO IL Springfield, MO AR MO Percentile TIV No. Events TIV No. Events TIV No. Events TIV No. Events TIV No. Events Max 39,466, ,366, ,297, ,878, ,048, % 17,585, ,453, ,470, ,553, ,348, % 5,412,883 1,191 7,266, ,639, ,988, ,483, % 3,771,730 2,381 3,195, ,609, ,723,276 1,617 2,267,785 1, % 1,475,490 Conditional 5, ,917 1,584 Kansas 512,595 1,237 City, MO KS 1,415,083 4, ,076 2,886 MEAN 2,466,163 2,836,071 2,137,388 2,872,752 1,582,815 Total Events 11,908 3,168 2,474 8,086 5,772 Metropolitan Percentile TIV No. Events Joplin, MO 2011 Historical Tornado Track Max 39,466, % 17,585, Conditional Poplar Bluff, MO Sedalia, MO Sikeston, MO Paragould, AR Hannibal, MO Percentile TIV No. Events TIV No. Events TIV No. Events TIV No. Events TIV No. Events Max 63,045, ,566, ,808, ,479, ,629, % 50,838, ,498, ,377,070 27,025, ,423, % 12,989, ,920, ,320, ,414, ,066, % 5,412,883 1, % 5,914, ,409, ,991, ,442, ,360, % 1,541, ,268, ,499, , , MEAN 4,923,481 3,920,615 3,515,049 2,743,152 1,351, % 3,771,730 2,381 Total Events 1,988 1,804 1,192 1,226 1, % Joplin, MO 2011 Historical Tornado 1,475,490 Track 5,954 MEAN 2,466,163 Conditional Macon, MO Anabel, MO Bertrand, MO Matthews, MO Bevier, MO Percentile TIV No. Events TIV No. Events TIV No. Events TIV No. Events TIV No. Events Max 42,836, ,361, ,734, ,353, ,226, % 42,046, ,361, ,734, ,614, ,226,224 1 Total Events 11, % 23,580, ,649, ,275, ,482, ,643, % 9,327, ,150, ,446, ,986, ,326, % 2,887, ,319, ,635, , ,186, MEAN 6,871,468 4,355,448 7,894,294 2,514,532 5,466,836 Total Events
27 Tornado Viewing Guide Top Accumulations Loss Scenarios Conditional Sikeston, MO Poplar Bluff, MO Sedalia, MO Lebanon, MO Kennett, MO Percentile TIV No. Events TIV No. Events TIV No. Events TIV No. Events TIV No. Events Max 70,566, ,802, ,827, ,964, ,750, % 59,718, ,327, ,565, ,725, ,633, % 28,595, ,891, ,989, ,740, ,024, % 19,031, ,505, ,558, ,858, ,517, % 8,337, ,080,895 1,082 3,506, ,674,278 1,015 3,058, MEAN 12,255,941 10,235,657 8,144,893 15,490,019 6,411,309 Total Events 1,196 2,164 1,810 2,030 1,422 US $ in Ones Mayflower, AR 2014 Historical Tornado Track Sikeston, MO Conditional Loss Potential Inside Track Percentile TIV Low Intensity (20%) High Intensity (50%) Max 70,566,784 14,113,357 35,283, % 59,718,096 11,943,619 29,859, % 28,595,964 5,719,193 14,297, % 19,031,244 3,806,249 9,515, % 8,337,714 1,667,543 4,168,857 MEAN 12,255,941 2,451,188 6,127,971 Total Events 1,196 US $ in Ones Mayflower, AR 2014 Historical Tornado Track 27
28 Major (EF4 to EF5) Tornado Days Per Century A Tornado Day is any day in which you see at least one EF4+ tornado within 80km 28
29 TVG Loss Ranges Using Historical EF4 & EF5 Event Frequency Exceedance Probabilities Modeled Other Wind Loss Potential Inside Track RMS AIR TIV Low Intensity High Intensity RiskLink Touchstone Return Period 100% 20% 50% Return Period v13.1 v1.5 1,000 58,500 11,700 29,250 1,000 46,842 45, ,008 9,402 23, ,035 39, ,813 7,363 18, ,864 30, ,456 5,091 12, ,335 20, ,656 3,731 9, ,786 16, ,830 2,566 6, ,237 12,338 Annualized Loss from EF4s and EF5s in TVG 675 1,687 Annual avg 21,658 22,996 Std dev 5,316 7,543 US $ in Thousands Assumptions: Tornado frequency uses NOAA Storm Prediction Center data TVG event frequency by smoothed historical average of EF4+ tornadoes is SPC data using 80km Gaussian filter US $ in Thousands Excess of 1,000 Year Return Period Excess of 100 Year Return Period Memphis Memphis Other Denver Denver Monroe Clovis Tulsa Monroe Other Tulsa Clovis 29
30 TVG Loss Ranges Using Historical EF4 & EF5 Event Frequency Exceedance Probabilities 2013 Other Wind Change RMS AIR TIV Loss TIV Loss 2011 RiskLink Touchstone Return Period 100% 50% 100% 50% to 2013 Return Period v13.1 v1.5 1,000 17,191 8,596 15,423 7,712-10% 1,000 12,575 13, ,590 7,295 13,045 6,523-11% ,318 10, ,360 5,680 10,042 5,021-12% 250 8,379 8, ,825 3,912 6,792 3,396-13% 100 6,274 6, ,888 2,944 4,996 2,498-15% 50 4,941 4, ,306 2,153 3,664 1,832-15% 25 3,821 3,417 AAL from EF4s and EF5s in TVG % Annual avg 6,585 3,351 US $ in Thousands Std dev 1,435 1,667 Assumptions: Tornado frequency uses NOAA Storm Prediction Center data US $ in Thousands TVG event frequency by smoothed historical average of EF4+ tornadoes is SPC data using 80km Gaussian filter Key Metropolitan Risks 2011 Key Metropolitan Risks 2013 Excess of 100 Year RP Excess of 1,000 Year RP Excess of 100 Year RP Excess of 1,000 Year RP Other Louisville Cincinnati Other Louisville Cincinnati Cincinnati Cleveland Cleveland Louisville Cincinnati Cleveland Cleveland Louisville 30
31 TVG Historical Tornado Shapes Moore, OK Tornado Joplin, MO Tornado Date: May 22, 2011 Rating: EF 5 Date: Rating: Mayflower, AR Tornado May 20, 2013 Date: EF 5 Rating: April 27, 2014 EF 4 Est. Max. Wind: 200+ mph Est. Max. Wind: 210 mph Est. Max. Wind: Path Length: 22.1 Miles Path Length: 17 Miles Path Length: 41.3 Miles Path Width: 0.75 Mile Path Width: 1.3 Miles Path Width: 0.75 Miles Fatalities 162 Fatalities 24 Fatalities mph 16
32 What if you could run every EF4 and EF5 tornado? 32
33 Stop Light Exposure Management 33
34 Paul s Everyone s Favorite Quotable Statistician Essentially, all models are wrong, but some are useful George E. P. Box 34
35 Biographies Steve Drews, Associate Director & Lead Meteorologist Steve Drews is Associate Director and Lead Meteorologist for Impact Forecasting. He currently heads the development of model customization for Impact Forecasting s catastrophe modeling suite, ELEMENTS. Over his 12 years with Aon, Steve has provided expert analysis on hurricane and tornado damage and has been a featured speaker at client, meteorological and government presentations about coastal urbanization, global climate change, tropical cyclone frequency, and severe convective weather frequency as well as provided scientific testimony on behalf of insurance and reinsurance companies in legal matters. Paul Eaton, FCAS, Director Paul Eaton has worked in the Aon Benfield Analytics Chicago office for seven years. Paul s current role focuses on catastrophe management including risk adjusted pricing and capacity allocation. Paul dabbled in telephony consulting, home improvement sales, and even driving an ambulance prior to joining Aon Benfield. 35
36 Contacts Steve Drews Associate Director & Lead Meteorologist Impact Forecasting Paul Eaton, FCAS Director Aon Benfield Analytics
37 Legal disclaimer: Impact Forecasting LLC The results listed in this report are based on engineering / scientific analysis and data, information provided by the client, and mathematical and empirical models. The accuracy of the results depends on the uncertainty associated with each of these areas. In particular, as with any model, actual losses may differ from the results of simulations It is only possible to provide plausible results based on complete and accurate information provided by the client and other reputable data sources. Furthermore, this information may only be used for the business application specified by Impact Forecasting, LLC and for no other purpose. It may not be used to support development of or calibration of a product or service offering that competes with Impact Forecasting, LLC. The information in this report may not be used as a part of or as a source for any insurance rate filing documentation. THIS INFORMATION IS PROVIDED "AS IS" AND IMPACT FORECASTING, LLC HAS NOT MADE AND DOES NOT MAKE ANY WARRANTY OF ANY KIND WHATSOEVER, EXPRESSED OR IMPLIED, WITH RESPECT TO THIS REPORT; AND ALL WARRANTIES INCLUDING WARRANTIES OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE ARE HEREBY DISCLAIMED BY IMPACT FORECASTING, LLC. IMPACT FORECASTING, LLC WILL NOT BE LIABLE TO ANYONE WITH RESPECT TO ANY DAMAGES, LOSS OR CLAIM WHATSOEVER, NO MATTER HOW OCCASIONED, IN CONNECTION WITH THE PREPARATION OR USE OF THIS REPORT. 37
The AIR Severe Thunderstorm Model for the United States
The AIR Severe Thunderstorm Model for the United States In 2011, six severe thunderstorms generated insured losses of over USD 1 billion each. Total losses from 24 separate outbreaks that year exceeded
More informationCS-11 Tornado/Hail: To Model or Not To Model
CS-11 Tornado/Hail: To Model or Not To Model CAS Seminar on Reinsurance- June 5, 2012 George Davis 2012 AIR WORLDWIDE CAS Seminar on Reinsurance 1 Antitrust Notice The Casualty Actuarial Society is committed
More informationTHE AIR SEVERE THUNDERSTORM MODEL FOR AUSTRALIA
THE AIR SEVERE THUNDERSTORM MODEL FOR AUSTRALIA In Australia, severe thunderstorms occur more frequently and cost more annually than any other atmospheric peril. The industry s first comprehensive severe
More informationUNDERSTANDING RECENT TRENDS IN U.S. THUNDERSTORM LOSSES
Photo: FEMA UNDERSTANDING RECENT TRENDS IN U.S. THUNDERSTORM LOSSES Mark C. Bove, CPCU Senior Research Meteorologist Munich Re America CAS Special Interest Seminar 30 September 2013 Agenda Trends in U.S.
More informationImpact Based Warning Tornado - Infrastructure
National Weather Service Impact Based Warning Tornado - Infrastructure Jim Kramper Warning Coordination Meteorologist St. Louis, MO NOAA s National Weather Service 2011 was a devastating year for tornado
More informationThe AIR Crop Hail Model for Canada
The AIR Crop Hail Model for Canada In 2016, the Canadian Prairie Provinces experienced one of the most active and longest hail seasons in at least 25 years. The number of hailstorms more than doubled the
More informationPRICING TORNADOES: USING CAT MODELS FOR GRANULAR RISK UNDERWRITING
PRICING TORNADOES: USING CAT MODELS FOR GRANULAR RISK UNDERWRITING Kevin Van Leer, Product Manager Americas Climate National Tornado Summit Oklahoma City, OK February 24, 2015 PURPOSE OF RMS Tool for the
More information2/27/2015. Perils. Risk. Loss PRICING TORNADOES: USING CAT MODELS FOR GRANULAR RISK UNDERWRITING WHY MODEL TORNADO RISK? FIRST, YOU HAVE TO ANSWER:
PURPOSE OF RMS Tool for the Insurance Industry to help with: PRICING TORNADOES: USING CAT MODELS FOR GRANULAR RISK UNDERWRITING Kevin Van Leer, Product Manager Americas Climate National Summit Oklahoma
More informationHow Detailed Weather Data and Geospatial Tools Can Be Used to Increase Net Income
How Detailed Weather Data and Geospatial Tools Can Be Used to Increase Net Income Session 475 Tuesday, June 10 10:30 11:30 am IASA 86 TH ANNUAL EDUCATIONAL CONFERENCE & BUSINESS SHOW How Detailed Weather
More informationNational Weather Service
National Weather Service Performance and Challenges Warning Systems Kenneth E. Graham Meteorologist-in-Charge New Orleans Busy 2008 Number of Tornadoes Number of Tornado Fatalities *Preliminary So Far
More informationComplete Weather Intelligence for Public Safety from DTN
Complete Weather Intelligence for Public Safety from DTN September 2017 White Paper www.dtn.com / 1.800.610.0777 From flooding to tornados to severe winter storms, the threats to public safety from weather-related
More informationClaim: Global warming is causing more and stronger tornadoes REBUTTAL
Claim: Global warming is causing more and stronger tornadoes REBUTTAL Tornadoes are failing to follow global warming predictions. Strong tornadoes have seen a drop in frequency since the 1950s. The years
More informationReal-Time Loss Estimates for Severe Thunderstorm Damage: The Event of April 27-28, 2002
AIR Special Report July 2002 Real-Time Loss Estimates for Severe Thunderstorm Damage: The Event of April 27-28, 2002 Technical Document_LPSR_0207 I. Overview On April 27-28, 2002, a frontal system generated
More informationThe AIR Severe Thunderstorm Model for Europe
The AIR Severe Thunderstorm Model for Europe In 2013 Andreas was the costliest severe thunderstorm outbreak to ever strike Europe and it still is. If Andreas were to recur today, it would cause about EUR
More informationMeasuring Hail and Wind Ground-Truth to Facilitate Rapid Response
Measuring Hail and Wind Ground-Truth to Facilitate Rapid Response Alex Kubicek CEO and Co founder Understory Weather alex.kubicek@understoryweather.com Overview Introduction to Understory Understory technology
More informationWe Had No Warning An Overview of Available Forecast Products Before and During Severe Weather Events
We Had No Warning An Overview of Available Forecast Products Before and During Severe Weather Events Two main sources for severe weather info NOAA/NWS Storm Prediction Center (SPC) Convective Outlooks
More informationEnhancing Weather Information with Probability Forecasts. An Information Statement of the American Meteorological Society
Enhancing Weather Information with Probability Forecasts An Information Statement of the American Meteorological Society (Adopted by AMS Council on 12 May 2008) Bull. Amer. Meteor. Soc., 89 Summary This
More informationTornado Hazard Risk Analysis: A Report for Rutherford County Emergency Management Agency
Tornado Hazard Risk Analysis: A Report for Rutherford County Emergency Management Agency by Middle Tennessee State University Faculty Lisa Bloomer, Curtis Church, James Henry, Ahmad Khansari, Tom Nolan,
More informationUS/Global Natural Catastrophe Update
US/Global Natural Catastrophe Update NAIC's CIPR Symposium on Implications of Increasing Catastrophe Volatility on Insurers Carl Hedde, SVP, Head of Risk Accumulation Munich Reinsurance America, Inc. Source:
More informationSITE-SPECIFIC HAIL ANALYSIS
SITE-SPECIFIC HAIL ANALYSIS PREPARED FOR: Beneficial Insurance Attn: Jeff Marker June 22, 2010 Case Reference: Burke #2307IY PROJECT INFORMATION Report Completion Date: June 22, 2010 Prepared for: Beneficial
More informationSAMPLE. SITE SPECIFIC WEATHER ANALYSIS Wind Report. Robinson, Smith & Walsh. John Smith. July 1, 2017 REFERENCE: 1 Maple Street, Houston, TX 77034
SAMPLE SITE SPECIFIC WEATHER ANALYSIS Wind Report PREPARED FOR: Robinson, Smith & Walsh John Smith July 1, 2017 REFERENCE: JACK HIGGINS / 4151559-01 1 Maple Street, Houston, TX 77034 CompuWeather Sample
More informationBuilding A Weather-Ready Nation
Building A Weather-Ready Nation Steve Runnels National Weather Service Springfield, MO` Photo Credit: Tim Marshall 122 National Weather Service Offices NWS Offices Service Missouri and Warning Coordination
More informationNatural Catastrophes: Is this the New Norm and other often asked Questions
27/04/12 Natural Catastrophes: Is this the New Norm and other often asked Questions and inadequate reinsurance Sean Devlin CAS Spring Meeting May 23, 12 2 Question 1 First a quick Look back at 11 January
More informationLab 21. Forecasting Extreme Weather: When and Under What Atmospheric Conditions Are Tornadoes Likely to Develop in the Oklahoma City Area?
Forecasting Extreme Weather When and Under What Atmospheric Conditions Are Tornadoes Likely to Develop in the Oklahoma City Area? Lab Handout Lab 21. Forecasting Extreme Weather: When and Under What Atmospheric
More informationSAMPLE. SITE SPECIFIC WEATHER ANALYSIS Rainfall Report. Bevins Engineering, Inc. Susan M. Benedict. July 1, 2017 REFERENCE:
SAMPLE SITE SPECIFIC WEATHER ANALYSIS Rainfall Report PREPARED FOR: Bevins Engineering, Inc. Susan M. Benedict July 1, 2017 REFERENCE: DUBOWSKI RESIDENCE / FILE# 11511033 1500 Water Street, Pensacola,
More informationThe Climate of Payne County
The Climate of Payne County Payne County is part of the Central Great Plains in the west, encompassing some of the best agricultural land in Oklahoma. Payne County is also part of the Crosstimbers in the
More informationSuperstorm Sandy What Risk Managers and Underwriters Learned
Superstorm Sandy What Risk Managers and Underwriters Learned Gary Ladman Vice President, Property Underwriting AEGIS Insurance Services, Inc. Superstorm Sandy Change in the Weather Recent years appears
More informationUnited States Multi-Hazard Early Warning System
United States Multi-Hazard Early Warning System Saving Lives Through Partnership Lynn Maximuk National Weather Service Director, Central Region Kansas City, Missouri America s s Weather Enterprise: Protecting
More informationFLOOD/SCS EVENT, APRIL 28 MAY 4
REPORT DATE: May 4, 2017 EVENT DATE: April 28-May 4, 2017 FLOOD/SCS EVENT, APRIL 28 MAY 4 Event Summary General Significant Flood Outlook. SOURCE: National Weather Service. A significant severe thunderstorm
More informationCoCoRaHS. Community Collaborative Rain, Hail, & Snow Network. Ashley Wolf Meteorologist NWS Green Bay Northeast Wisconsin CoCoRaHS Coordinator
CoCoRaHS Community Collaborative Rain, Hail, & Snow Network Ashley Wolf Meteorologist NWS Green Bay Northeast Wisconsin CoCoRaHS Coordinator What is CoCoRaHS Who, What, Where and Whys of CoCoRaHS What?
More informationTHE FUTURE OF U.S. WEATHER CATASTROPHES
Source: NASA THE FUTURE OF U.S. WEATHER CATASTROPHES Mark C. Bove, CPCU, ARe Senior Research Meteorologist Munich Reinsurance America, Inc. AIMU Marine Insurance Day 2 October 2015 Agenda Natural Catastrophes
More informationThe AIR Bushfire Model for Australia
The AIR Bushfire Model for Australia In February 2009, amid tripledigit temperatures and drought conditions, fires broke out just north of Melbourne, Australia. Propelled by high winds, as many as 400
More informationThe Climate of Seminole County
The Climate of Seminole County Seminole County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationThe Climate of Grady County
The Climate of Grady County Grady County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 33 inches in northern
More informationThe Climate of Marshall County
The Climate of Marshall County Marshall County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeastern Oklahoma. Average
More informationThe Climate of Bryan County
The Climate of Bryan County Bryan County is part of the Crosstimbers throughout most of the county. The extreme eastern portions of Bryan County are part of the Cypress Swamp and Forest. Average annual
More information15.3A TORNADO VISUALIZATION AND DOPPLER RADAR ANALYSIS PROJECT. Thomas Dolan * Independent Geographer, Rocklin, CA
15.3A TORNADO VISUALIZATION AND DOPPLER RADAR ANALYSIS PROJECT Thomas Dolan * Independent Geographer, Rocklin, CA 1. INTRODUCTION Tornadoes play a significant role in the weather of the United States and
More informationStatistical Work and Predictability of Tornados. Misha Shvartsman Department of Mathematics University of St. Thomas
Statistical Work and Predictability of Tornados Misha Shvartsman Department of Mathematics University of St. Thomas Statistical Work and Predictability of Tornados Tornado (violently rotating column of
More informationCharles Kuster Leadville, CO. Personal Overview
Charles Kuster Leadville, CO Personal Overview Personal Overview Charles Kuster Leadville, CO OU to study meteorology Charles Kuster Leadville, CO Personal Overview OU to study meteorology Graduated in
More informationCURRENT AND FUTURE TROPICAL CYCLONE RISK IN THE SOUTH PACIFIC
CURRENT AND FUTURE TROPICAL CYCLONE RISK IN THE SOUTH PACIFIC COUNTRY RISK PROFILE: SAMOA JUNE 2013 Samoa has been affected by devastating cyclones on multiple occasions, e.g. tropical cyclones Ofa and
More informationThe Climate of Kiowa County
The Climate of Kiowa County Kiowa County is part of the Central Great Plains, encompassing some of the best agricultural land in Oklahoma. Average annual precipitation ranges from about 24 inches in northwestern
More informationA pragmatic view of rates and clustering
North Building Atlantic the Chaucer Hurricane Brand A pragmatic view of rates and clustering North Atlantic Hurricane What we re going to talk about 1. Introduction; some assumptions and a basic view of
More informationGC Briefing. Weather Sentinel Hurricane Florence. Status at 5 PM EDT (21 UTC) Today (NHC) Discussion. September 13, 2018
GC Briefing September 13, 2018 Weather Sentinel Hurricane Florence Tropical storm conditions have been reported for areas of North Carolina and will continue to spread inland to the west and south. Hurricane
More informationNOAA s National Weather Service. National Weather Service
NOAA s National Weather Service Serving the Nation s Environmental Forecasting Needs Lynn Maximuk Regional Director National Weather Service Central Region Headquarters Kansas City, Missouri America s
More informationAt the Midpoint of the 2008
At the Midpoint of the 2008 Atlantic Hurricane Season Editor s note: It has been an anxious couple of weeks for those with financial interests in either on- or offshore assets in the Gulf of Mexico and
More information3/5/2013 UNCERTAINTY IN HURRICANE FREQUENCY: HOW MODELERS APPROACH THE PROBLEM PROBLEM STATEMENT
UNCERTAINTY IN HURRICANE FREQUENCY: HOW MODELERS APPROACH THE PROBLEM Matthew Nielsen Director, Product Management PROBLEM STATEMENT Hurricane Frequency Isn t Stable Over Time Are historical average frequencies
More informationThe Climate of Texas County
The Climate of Texas County Texas County is part of the Western High Plains in the north and west and the Southwestern Tablelands in the east. The Western High Plains are characterized by abundant cropland
More informationThe Climate of Haskell County
The Climate of Haskell County Haskell County is part of the Hardwood Forest. The Hardwood Forest is characterized by its irregular landscape and the largest lake in Oklahoma, Lake Eufaula. Average annual
More informationKentucky Weather Hazards: What is Your Risk?
Kentucky Weather Hazards: What is Your Risk? Stuart A. Foster State Climatologist for Kentucky 2010 Kentucky Weather Conference Bowling Green, Kentucky January 16, 2010 Perspectives on Kentucky s Climate
More informationKCC White Paper: The 100 Year Hurricane. Could it happen this year? Are insurers prepared? KAREN CLARK & COMPANY. June 2014
KAREN CLARK & COMPANY KCC White Paper: The 100 Year Hurricane Could it happen this year? Are insurers prepared? June 2014 Copyright 2014 Karen Clark & Company The 100 Year Hurricane Page 1 2 COPLEY PLACE
More informationEVALUATION AND VERIFICATION OF PUBLIC WEATHER SERVICES. Pablo Santos Meteorologist In Charge National Weather Service Miami, FL
EVALUATION AND VERIFICATION OF PUBLIC WEATHER SERVICES Pablo Santos Meteorologist In Charge National Weather Service Miami, FL WHAT IS THE MAIN DIFFERENCE BETWEEN A GOVERNMENT WEATHER SERVICE FORECAST
More informationTornadoes. tornado: a violently rotating column of air
Tornadoes tornado: a violently rotating column of air Tornadoes What is the typical size of a tornado? What are typical wind speeds for a tornado? Five-stage life cycle of a tornado Dust Swirl Stage Tornado
More informationMiami-Dade County Overview
Miami-Dade County Overview 2,000 square miles World s busiest cruise port 2.6 million residents Second busiest US airport for international travelers Gateway to the Caribbean and Latin America Natural
More informationCommunicating uncertainty from short-term to seasonal forecasting
Communicating uncertainty from short-term to seasonal forecasting MAYBE NO YES Jay Trobec KELO-TV Sioux Falls, South Dakota USA TV weather in the US Most TV weather presenters have university degrees and
More informationCASA WX DFW URBAN DEMONSTRATION NETWORK
CASA WX DFW URBAN DEMONSTRATION NETWORK Goals Background on Regional CASA WX Project Explain the capabilities, structure of the Radar Network Present the CASA WX DFW Test Bed will be rolled out Describe
More informationExtremes Seminar: Tornadoes
Dec. 01, 2014 Outline Introduction 1 Introduction 2 3 4 Introduction 101: What is a tornado? According to the Glossary of Meteorology (AMS 2000), a tornado is a violently rotating column of air, pendant
More informationMET Lecture 29 Tornadoes IV
MET 4300 Lecture 29 Tornadoes IV Outline Definition, life cycle, & climatology of tornadoes Tornado formation within supercells Tornado formation within nonsupercell thunderstorms Fujita scale Tornado
More informationThe Climate of Pontotoc County
The Climate of Pontotoc County Pontotoc County is part of the Crosstimbers. This region is a transition region from the Central Great Plains to the more irregular terrain of southeast Oklahoma. Average
More informationThe Climate of Murray County
The Climate of Murray County Murray County is part of the Crosstimbers. This region is a transition between prairies and the mountains of southeastern Oklahoma. Average annual precipitation ranges from
More informationAdvanced Spotter Training Welcome! Lesson 1: Introduction and Why Spotters are Important
Advanced Spotter Training 2009 Welcome! Lesson 1: Introduction and Why Spotters are Important Introduction This course is intended to advance the basic training given by the National Weather Service (NWS).
More informationA COMPREHENSIVE 5-YEAR SEVERE STORM ENVIRONMENT CLIMATOLOGY FOR THE CONTINENTAL UNITED STATES 3. RESULTS
16A.4 A COMPREHENSIVE 5-YEAR SEVERE STORM ENVIRONMENT CLIMATOLOGY FOR THE CONTINENTAL UNITED STATES Russell S. Schneider 1 and Andrew R. Dean 1,2 1 DOC/NOAA/NWS/NCEP Storm Prediction Center 2 OU-NOAA Cooperative
More informationImpacts of Frequency Contagion on Pricing of Catastrophe Excess of Loss Reinsurance for Australian Natural Perils
Impacts of Frequency Contagion on Pricing of Catastrophe Excess of Loss Reinsurance for Australian Natural Perils Dr Will Gardner This presentation has been prepared for the 2016 General Insurance Seminar.
More informationWeather can change quickly...are you on top of the changes?
Weather Access Bob Glancy NOAA National Weather Service, Boulder, CO Near Cedar Point, CO May 9, 2004 Weather can change quickly...are you on top of the changes? National Weather Service Local offices:
More informationThe Politics of Tornadoes The Impacts of Sudden Storm Events on People
The Politics of Tornadoes The Impacts of Sudden Storm Events on People Today s Discussion Brief Review Student Presentation When the Sky Kills Impacts of Tornadoes Questions & Discussion Next Class Brief
More informationThe AIR Tropical Cyclone Model for India
The AIR Tropical Cyclone Model for India Tropical cyclones have caused millions, and even billions, of dollars in damage in India. The growing number of properties on the coast, together with growing insurance
More informationWeather in Saskatchewan. John Paul Cragg Warning Preparedness Meteorologist Environment and Climate Change Canada
Weather in Saskatchewan John Paul Cragg Warning Preparedness Meteorologist Environment and Climate Change Canada The Climate of Saskatchewan -35 Average January Low Temperature -30-25 -20-15 -10-5 0 5
More informationTornadoes Student Activity Book
Tornadoes Student Activity Book I. Introduction Have you ever seen a tornado? Hopefully, it was in a video on television. Each year as many as 1000 tornadoes may occur in the United States. Their destruction
More informationHazardous Weather and Flooding Preparedness. Hazardous Weather and Flooding Preparedness
Hazardous Weather and Flooding Preparedness 1 A Cooperative Effort 2 Administrative Information Emergency exits and procedures Location of restrooms Mobile devices Procedure for questions Course materials
More information2/27/2015. Big questions. What can we say about causes? Bottom line. Severe Thunderstorms, Tornadoes, and Climate Change: What We Do and Don t Know
Severe Thunderstorms, Tornadoes, and Climate Change: What We Do and Don t Know Big questions How and why are weather hazards distributed? Are things changing in time and will they? HAROLD BROOKS NOAA/NSSL
More informationModelling the impact of climate change and weather related events. Seong Woh Choo Head of R&D and Chief Underwriting Officer
Modelling the impact of climate change and weather related events Seong Woh Choo Head of R&D and Chief Underwriting Officer 1 1 Introduction Risk to community and insurers Climatic cycles/change affecting
More informationIntroduction to Weather Analytics & User Guide to ProWxAlerts. August 2017 Prepared for:
Introduction to Weather Analytics & User Guide to ProWxAlerts August 2017 Prepared for: Weather Analytics is a leading data and analytics company based in Washington, DC and Dover, New Hampshire that offers
More informationTROPICAL CYCLONE TORNADOES
TROPICAL CYCLONE TORNADOES 2018 GOVERNOR S HURRICANE CONFERENCE TUESDAY, MAY 15, 2018 WILL ULRICH NWS FORECAST OFFICE MELBOURNE WHERE ARE THE TORNADOES? WHERE ARE THE TORNADOES? C B A WEST MELBOURNE, FL
More informationWeather Analysis and Forecasting
Weather Analysis and Forecasting An Information Statement of the American Meteorological Society (Adopted by AMS Council on 25 March 2015) Bull. Amer. Meteor. Soc., 88 This Information Statement describes
More informationRunning Head: HAZARD MITIGATION PLAN OUTLINE FOR MISSISSIPPI 1
Running Head: HAZARD MITIGATION PLAN OUTLINE FOR MISSISSIPPI 1 Hazard Mitigation Plan Outline for Mississippi Name: Institution: HAZARD MITIGATION PLAN OUTLINE FOR MISSISSIPPI 2 Hazard Mitigation Plan
More informationEastern Shore Weather and Climate. Bill Sammler Warning Coordination Meteorologist National Weather Service Wakefield, VA
Eastern Shore Weather and Climate Bill Sammler Warning Coordination Meteorologist National Weather Service Wakefield, VA About The NWS The National Weather Service is: A Federal Government Agency Part
More informationA Preliminary Severe Winter Storms Climatology for Missouri from
A Preliminary Severe Winter Storms Climatology for Missouri from 1960-2010 K.L. Crandall and P.S Market University of Missouri Department of Soil, Environmental and Atmospheric Sciences Introduction The
More informationTHE CHANGING CLIMATE OF CATASTROPHE RISK UNDERWRITING
Source: NPS THE CHANGING CLIMATE OF CATASTROPHE RISK UNDERWRITING Mark C. Bove, CPCU, ARe Senior Research Meteorologist Munich Reinsurance America, Inc. Midwest / Western Regional Farm Bureau Underwriting
More informationNational Weather Service
National Weather Service Integrated Warning Team Workshops: NWS Warnings and Outdoor Warning Sirens Tim Halbach Warning Coordination Meteorologist Milwaukee NWS Integrated Warning Team NWS State Officials
More informationExposure Disaggregation: Introduction. By Alissa Le Mon
Exposure Disaggregation: Building Better Loss Estimates 10.2010 Editor s note: In this article, Alissa Le Mon, an analyst in AIR s exposures group, discusses how AIR s innovative disaggregation techniques
More informationTornadoes in America: The Oklahoma Disaster in Context
Tornadoes in America: The Oklahoma Disaster in Context This briefing is excerpted from the article written by Alexis C. Madrigal as a backgrounder for understanding the storm that hit Moore, Oklahoma on
More informationSAMPLE. SITE SPECIFIC WEATHER ANALYSIS Wind Report. Robinson, Smith & Walsh. John Smith REFERENCE:
SAMPLE SITE SPECIFIC WEATHER ANALYSIS Wind Report PREPARED FOR: Robinson, Smith & Walsh John Smith REFERENCE: JACK HIGGINS / 4151559-01 CompuWeather Sample Report Please note that this report contains
More informationAN ANALYSIS OF THE TORNADO COOL SEASON
AN ANALYSIS OF THE 27-28 TORNADO COOL SEASON Madison Burnett National Weather Center Research Experience for Undergraduates Norman, OK University of Missouri Columbia, MO Greg Carbin Storm Prediction Center
More informationThe Joplin Tornado: Lessons Learned from the NIST Investigation
February 4, 2014 AMS Annual Meeting The Joplin Tornado: Lessons Learned from the NIST Investigation Franklin T. Lombardo, NIST Erica Kuligowski, NIST Marc Levitan, NIST Long Phan, NIST David Jorgensen,
More informationSOUTHERN CLIMATE MONITOR
SOUTHERN CLIMATE MONITOR MARCH 2011 VOLUME 1, ISSUE 3 IN THIS ISSUE: Page 2 to 4 Severe Thunderstorm Climatology in the SCIPP Region Page 4 Drought Update Page 5 Southern U.S. Precipitation Summary for
More informationTHE IMPACT OF WEATHER
The United States is the most severe weather prone country in the world. Each year, people in this country cope with an average of 10,000 thunderstorms, 5,000 floods, 1,200 tornadoes and two landfalling
More informationCore Curriculum Supplement
Core Curriculum Supplement Academic Unit / Office EAS Catalog Year of Implementation 2018-2019 Course (Prefix / Number) GEOL / 1370 Core Proposal Request Add to Core Curriculum Course Title Natural Disasters
More informationTORNADOES. DISPLAY VISUAL A Tornado Is... Tornadoes can: Rip trees apart. Destroy buildings. Uproot structures and objects.
TORNADOES Introduce tornadoes by explaining what a tornado is. DISPLAY VISUAL A Tornado Is... A powerful, circular windstorm that may be accompanied by winds in excess of 250 miles per hour. Tell the participants
More informationThe AIR Hurricane Model for Offshore Assets
The AIR Hurricane Model for Offshore Assets The combined insured losses to offshore assets caused by hurricanes in 2004 and 2005 alone were estimated at the time to be about USD 16 billion. Today, the
More informationHow Wind Technologies Work. WHITE PAPER 4 April 2017
How Wind Technologies Work WHITE PAPER 4 April 2017 ii Table of Contents Introduction... 1 The Challenge... 1 Purpose... 1 Limited Data Sources... 2 Using Point Measurements for Wind Verification... 2
More informationCurrent Details from the National Hurricane Center (NHC)
Current Watches/Warnings A Hurricane Warning is in effect from Surf City, North Carolina to the North Carolina/Virginia border; Pamlico Sound; Eastern Albemarle Sound A Hurricane Watch is in effect from
More informationSummary of 2006 Atlantic Tropical Cyclone Season and Verification of Authors Seasonal Forecasts
Summary of 2006 Atlantic Tropical Cyclone Season and Verification of Authors Seasonal Forecasts Issued: 22nd January 2007 by Professor Mark Saunders and Dr Adam Lea Benfield Hazard Research Centre, UCL
More informationThe Joplin Tornado: Lessons Learned from the NIST Investigation
February 4, 2014 AMS Annual Meeting The Joplin Tornado: Lessons Learned from the NIST Investigation Franklin T. Lombardo, NIST/RPI Erica Kuligowski, NIST Marc Levitan, NIST Long Phan, NIST David Jorgensen,
More informationNW Pacific and Japan Landfalling Typhoons in 2000
NW Pacific and Japan Landfalling Typhoons in 2000 Pre-Season Forecast Issued 26th May, 2000 Produced under contract for TSUNAMI in collaboration with the UK Met. Office by Drs Paul Rockett, Mark Saunders
More information2004 Hurricane Season: Climate Overview and Lessons Learned
2004 Hurricane Season: Climate Overview and Lessons Learned Mark Saunders, PhD (Presenter: Milan Simic,, PhD, Benfield) Lead Scientist, Tropical Storm Risk Benfield Hazard Research Centre University College
More informationTHE CRUCIAL ROLE OF TORNADO WATCHES IN THE ISSUANCE OF WARNINGS FOR SIGNIFICANT TORNADOS
THE CRUCIAL ROLE OF TORNADO WATCHES IN THE ISSUANCE OF WARNINGS FOR SIGNIFICANT TORNADOS John E. Hales, Jr. National Severe Storms Forecast Center Kansas City, Missouri Abstract The tornado warning is
More informationAre Tornadoes Getting Stronger?
Are Getting Stronger? Department of Geography, Florida State University Thomas Jagger, Ian Elsner Categorical Scale for Tornado Intensity The EF damage scale to rate tornado intensity is categorical. An
More informationIBM Insights for Weather
Service Description IBM Insights for Weather This Service Description describes the Cloud Service IBM provides to Client. Client means the company and its authorized users and recipients of the Cloud Service.
More information(Severe) Thunderstorms and Climate HAROLD BROOKS NOAA/NSSL
(Severe) Thunderstorms and Climate HAROLD BROOKS NOAA/NSSL HAROLD.BROOKS@NOAA.GOV Big questions How and why are weather hazards distributed? Are things changing in time and will they? Begin with thunderstorm
More informationTornadoes. Tornadoes COMMUNITY EMERGENCY RESPONSE TEAM TORNADOES
Tornadoes Tornadoes Tell the participants that tornadoes are powerful, circular windstorms that may be accompanied by winds in excess of 200 miles per hour. Tornadoes typically develop during severe thunderstorms
More informationDate of Storm Storm Duration * Intensity Max Size Storm Speed Storm Direction : " 40 MPH ENE
HailStrike 4011 W Plano Pkwy Suite #105 Plano, TX 75093 support@hailstrike.com Property Owner Information Report No. 17696 Property Information To order additional OneSite reports, visit our website at
More information