ALLEY CATS: HOW EL NIÑO INFLUENCES TORNADO ALLEY AND THE THREAT OF CATASTROPHES

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ALLEY CATS: HOW EL NIÑO INFLUENCES TORNADO ALLEY AND THE THREAT OF CATASTROPHES Kevin Van Leer - Sr. Product Manager, Model Product Management National Tornado Summit - Tuesday, March 1 st, 2016 1

EL NIÑO/SOUTHERN OSCILLATION (ENSO) What is El Niño? A warming of the ocean surface, or above-average sea surface temperatures (SST), in the central and eastern tropical Pacific Ocean The low-level surface winds, which normally blow from east to west along the equator ( easterly winds ), instead weaken or, in some cases, start blowing the other direction (from west to east or westerly winds ). Maps by NOAA Climate.gov, based on data provided by NOAA 2

EL NIÑO SOUTHERN OSCILLATION (ENSO) 2015-2016 El Niño NOAA operationally defines El Niño, the warm phase of ENSO, as occurring when the Oceanic Niño Index (ONI) is greater than or equal to +0.5 C, typically for at least 5 consecutive overlapping 3-month periods ONI is based on the 3-month running mean SST anomaly in the Nino 3.4 region of the Pacific The most recent ONI value (Nov 2015 Jan 2016) is 2.3 C, which is considered a super El Niño The current El Niño is considered one of the strongest on record Images from the 15 Feb 2016 CPC ENSO Discussion 3

EL NIÑO S IMPACT ON ATLANTIC HURRICANES From RMS s 2015 Atlantic Hurricane Season Review Although predicted SST and sea-level pressure conditions did not materialize, 2015 was indeed a quiet season, as a result of the anticipated El Niño event, which is currently tied with 1997 as the strongest event on record. 16 14 1950-2014 Average 1995-2014 Average 2015 Season 14.8 12 10 11.2 11.0 8 6 4 2 0 7.6 6.2 4.0 3.6 2.7 2.0 Named Storms Hurricanes Major Hurricanes 4

COMPARING EL NIÑO RESEARCH HURRICANES Longer history of research tying El Niño to reduced Atlantic hurricanes Hurricanes are a larger scale phenomenon than tornadoes Increased wind shear across the Caribbean creates an unfavorable environment for hurricane development TORNADOES Recent research has identified a potential physical mechanism for El Niño s influence El Niño s influence is on a different scale than individual tornado development Focus is on El Niño s impact on ingredients for severe convective storm development CAPE (Convective Available Potential Energy) Directional Speed WIND SHEAR 5

LATEST RESEARCH 6

El Niño modifies the jet stream positioning over the continental U.S., which alters severe weather ingredients ALLEN, TIPPETT, AND SOBEL (2015) Tornado Index El Niño Influence La Niña Influence Identified lower tornado and hail activity in central U.S. during El Niño episodes Winter ENSO indices can be used to predict spring severe weather frequency Copyright 2016 Risk Management Solutions, Inc.. All Rights Reserved. March 1, 2016 Hailstorm Index Images from Climate.gov; Adapted from referenced Nature publications 7

RESEARCH SUMMARY Other References Cook and Shafer 2008 Lee et al 2013 Tippett et al 2014 Sparrow and Mercer 2015 Increased Winter Activity in the Southeast and East Research has related El Niño to winter tornado outbreaks (As was seen in December 2015 and last week!) Large scale atmospheric conditions favorable for tornado outbreaks, such as southwesterly wind shear, in the Southeast Reduced Spring Activity in the central Plains El Niño alters the jet stream position during the spring months, reducing favorable conditions for severe weather Fewer low pressure systems over the central Plains Less warm, moist air intrusion into central Plains from Gulf Copyright 2016 Risk Management Solutions, Inc.. All Rights Reserved. March 1, 2016 8

2015 SEVERE WEATHER SEASON 9

2015 INSURED LOSSES From an insured loss perspective, 2015 was a normal year Billions $30 PCS Trended Loss (2015) 1990-2015 mean 2000-2015 mean 2008-2015 mean $25 Only 2 events with insured losses greater than $1B $20 $15 Many events dominated by flash flood losses, instead of hail, wind, and tornado $10 $5 $- 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015 Data retrieved from Property Claims Service (PCS) and Trended to 2015 Copyright 2016 Risk Management Solutions, Inc.. All Rights Reserved. March 1, 2016 10

2015 TORNADO COUNTS Tornado counts below the 25th percentile Slow start season (March and April) Significant events in May, November, and December Copyright 2016 Risk Management Solutions, Inc.. All Rights Reserved. March 1, 2016 11

2015 TORNADO WATCH COUNTS Marked decrease in Tornado Watches in Tornado Alley and Southeast U.S. Reflects decreased tornado activity in these areas Pattern matches well with those identified in research Copyright 2016 Risk Management Solutions, Inc.. All Rights Reserved. March 1, 2016 12

2015-2016 WINTER SEVERE WEATHER Evergreen, VA 24 Feb 2016 Clarksdale, MS 23 Dec 2015 Increased Winter activity in the Southeast and East aligns well with published research findings Photo: Jason Smith Rowlett, TX 26 Dec 2015 Photo: AFP/Getty Images Photo: NWS Forth Worth 13

WHY SHOULD ENSO BE REPRESENTED IN CAT MODELS? 14

WHY SHOULD ENSO BE REPRESENTED IN CAT MODELS? A granular seasonal view on severe weather patterns could inform the insurance industry of increased or decreased risk geographically Severe Convective Storm Risk Observed patterns during this El Niño event compare well with the recent research Reduced Spring activity in the central Plains Increased Winter activity in the Southeast and East These patterns could be reflected in a special stochastic event set for use in El Niño or La Niña periods generated using an ingredients-based approach This type of approach is already used in CAT models to generate severe convective storm event sets 15

SUMMARY The current El Niño episode is one of the strongest on record The 2015 season saw decreased tornado activity over the central U.S., though insured losses were still near average The 2015/2016 winter has been marked by significant severe weather events Recent research has identified links between El Niño and decreases in severe weather activity over the central U.S., as well as an increase in activity during winter months The ingredients-based approach to severe storm event set generation in CAT models may present a future opportunity for incorporating seasonal views of severe storm frequency Many questions remain regarding the impacts of ENSO on severe convective storm activity, though recent research is showing great promise. 16

ABOUT RMS RMS is the world s leading provider of products, services, and expertise for the quantification and management of catastrophe risk. More than 400 leading insurers, reinsurers, trading companies, and other financial institutions rely on RMS models to quantify, manage, and transfer risk. As an established provider of risk modeling to companies across all market segments, RMS provides solutions that can be trusted as reliable benchmarks for strategic pricing, risk management, and risk transfer decisions. 2016 Risk Management Solutions, Inc. RMS and the RMS logo are registered trademarks of Risk Management Solutions,Inc. All other trademarks are property of their respective owners. Copyright 2016 2015 Risk Management Solutions, Inc. All Rights Reserved. March 1, 2016 17

REFERENCES Allen J. T., Tippett, M. K. & Sobel, A. H. Influence of the El Nino/Southern Oscillation on tornado and hail frequency in the United States. Nature Geoscience. 8, 278-283 (2015). Cook, A. R. & Shafer, J. T. The relation of El Nino-Souther Oscillation (ENSO) to winter tornado outbreaks. Mon. Weath. Rev. 136, 3121-3137 (2008). Lee, S-K., Atlas, R., Enfield, D. B., Wang, C. & Liu, H. Is there an optimal ENSO pattern that enhances large-scale atmospheric processes conducive to major torando outbreaks in the U.S.? J. Clim. 26, 1626-1642 (2013). Sparrow, K. H. & Mercer, A. E. Predictability of U.S. tornado outbreak seasons using ENSO and northern hemisphere geopotential height variability. Geosci. Frontiers, 7, 21-31 (2015). Tippett, M. K., Sobel, A. H., Camargo, S. J. & Allen, J. T. An empirical relation between U.S. tornado activity and monthly environmental parameters. J. Clim. 27, 2983-2999 (2014). 18