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European Extratropical Cyclones European Extratropical Cyclones IMPLICATIONS FOR LOCAL INSURERS 0 European Extratropical Cyclones | TransRe White Paper by James Rohman | May 2014 ! 1 2 ! Introduction " 1" 2 This paper highlights the climatology, characteristics, history and climate change projections of European Extratropical Cyclones. " " January 2014" was the fourth warmest since record keeping began in 1880, yet it fell in the middle of the most extreme winter Europe (and the Northeast US) has experienced in 15 years. A nexus of storms brought high winds, heavy rainfall and severe snowstorms for almost five months, causing flooding and damage to life onshore and at sea. Such prodigious weather patterns indicate equally prodigious climate disturbances. Many of those storms formed as Extratropical Cyclone s (ETC). The first3 section of this paper discusses the large-scale climate 4 variations and indices that encourage and energize ETC development. Every year, roughly" 200 atmospheric disturbances form in the North 3 4" Atlantic. A handful of the disturbances, which develop as cold-core and 4 asymmetric cyclones, morph into organized storms and track east towards Europe. The second section summarizes the characteristics and dynamics " of these pandemonium-inducing windstorms. " On average, European ETCs create $1.2 billion of insured loss per year. In extreme years with multiple tail events, they can be the leading cause of global storm losses; in 1990 and 1999, they caused $18 billion and $14 billion of insured losses, respectively. The 2014 season is expected to exceed $5.5 billion in insured loss. Section three covers the finer points of the European ETC archival record. 5 6 ETCs that form in the North Atlantic are among nature’s most powerful cyclones on earth, deriving their energy from the interaction and difference between cold Arctic air masses and warm subtropical air masses. ETCs can 5" 6" produce storms with central low pressure as low as 916 mb, winds up 6 to 140 mph and wave heights over 100 feet. Given the recent record of IPCC reports and extreme weather, the final section offers predictions for ETC development" and tracking. " The disruption and loss to everyday life from extreme weather is calamitous. As the science of climatology continues to evolve, TransRe strives to inform the insurance industry of advancements in the field. Our efforts come with the hope that property damage, loss of life and societal interferences will diminish with greater knowledge of extreme natural Figurcatastrophes.e 1. An extratrop ical disturbance turns into an organized storm in the eastern North Atlantic. Over February 12-14, 2014, a series of storms struck the coastline of northern Europe, causing widespread flood and damage, resulting in approximate insured losses of $1.3B to residences, businesses and infrastructure. Fiigurre 1.. An exttrrattrropiicall diistturrbance tturrns iintto an orrganiized sttorrm iin tthe eastterrn Norrtth Atltlantitic.. Overr Febrruarry 12--14,, 2014,, a serriies off sttorrms sttrruck tthe coasttliline off norrttherrn Eurrope,, causiing wiidesprread flflood and damage,, rresultilting iin apprroxiimatte iinsurred llosses off $1..3B tto rresiidences,, busiinesses and iinffrrasttrructturre.. #! European Extratropical Cyclones | TransRe White Pape! r 3 European Extratropical Cyclones | TransRe White Paper 1 #! Eurropean Exttrrattrropiicall Cycllones || TrransRe Whitite Pape!! rr Executive Summary • Extratropical Cyclones (ETC) that form in the North Atlantic are, on average, the second most destructive insured natural catastrophe worldwide (after Atlantic hurricanes). • They can generate winds up to 140mph and waves over 100ft. • The wind-fields range from 120-1200 miles, with the spread of most damaging winds 50-150 miles from the storm center. • On average, 200 ETCs form each year. • They derive their energy from the horizontal temperature difference between warm, subtropical air masses and cold, polar air masses. • The two most consistent factors driving European ETCs are the Arctic Oscillation (AO) and North Atlantic Oscillation (NAO). • AO and NAO shape the jet stream, funnel ETCs into various parts of Europe. o Positive AO/NAO is associated with storms that have a west-southwest to east-northeast track across Europe. o Negative AO/NAO is linked to a more south-to-north track. o NAO positive (negative) years are associated with a 10- 15% increase (decrease) in losses during winter storm seasons. • AO/NAO variation is linked to the dynamics of the Madden-Julian Oscillation (MJO), a global tropical weather anomaly. • Climate projections indicate an increase in ETC wind gusts from the eastern North Atlantic Ocean into Northern and Central Europe. • Three futuristic climate simulations show ETC frequency is expected to increase over many parts of Europe, from Scandinavia to the Adriatic, due to climate change. • In addition to land based losses, ETCs will impact marine exposures. Post-Panamax containerships are more prone to a phenomenon known as ‘parametric rolling’ than smaller vessels due to hull shape. • TransRe is working to support insurers to better understand the causes and implications of European Extratropical Cyclones. 2 European Extratropical Cyclones | TransRe White Paper 2 Introduction Introduction This paper highlights the climatology, characteristics, history and Thisclimate paper changehighlights projections the clima oftology, European characteristics, Extratropical history Cyclones. and climate change projections of European Extratropical Cyclones. January 2014 was the fourth warmest since record keeping began in 1880, Januaryyet it 2014fell in wathes middlethe fourth of the warmest most extreme since record winter keeping Europe began (and the in 1880, Northeast yet US)it fell h inas the experienced middle of thein 15 most years. extreme A nexus winter of storms Europe brought (and the high Northeast winds, US)heavy has experienced rainfall and insevere 15 years. snowstorms A nexus for of almoststorms fivebrought months, high causing winds, heavyflooding rainfall and and damage severe tosnowstorms life onshore for and almost at sea. five months, causing flooding and damage to life onshore and at sea. Such prodigious weather patterns indicate equally prodigious climate Suchdisturbances. prodigious weather Many of patterns those storms indicate formed equally as prodigious Extratropical climate Cyclone s disturbances.(ETC). The Many first section of those of thisstorms paper formed discusses as Extratropical the large-scale Cyclone climates (ETC)variations. The first and section indices of thatthis encouragepaper discusses and energize the large ETC-scale development. climate variations and indices that encourage and energize ETC development. Every year, roughly 200 atmospheric disturbances form in the North EveryAtlantic. year, roughlyA handful 200 of theatmospheric disturbances disturbance, which develops form as in cold the-core North and Atlantic.asymmetric A handful cyclones, of the morphdisturbances into organized, which develop storms andas cold track-core east and towards asymmetricEurope. Thecyclones, second morph section into summarizes organized storms the characteristics and track east and towards dynamics Europe.of these The pandemonium second section-inducing summarizes windstorms the characteristics. and dynamics of these pandemonium-inducing windstorms. On average, European ETCs create $1.2 billion of insured loss per year. On Iaverage,n extreme European years with ETCs multiple create tail events, $1.2 billion they canof insured be the leading loss per cause year of. In extremeglobal storm years losses; with multiple in 1990 tail and events, 1999, they they can caused be the $18 leading billion causeand $14 of globalbillion storm of insuredlosses; lossesin 1990, respectively.and 1999, they The caused 2014 season$18 billion is expectedand $14 to billionexceed of insured $5.5 billionlosses, inrespectively. insured loss. The Section 2014 season three covers is expected the finer to points of exceedthe European $5.5 billion ETC in archivalinsured record loss. .Section three covers the finer points of the European ETC archival record. ETCs that form in the North Atlantic are among nature’s most powerful ETCscyclones that form on inearth the, Northderiving Atlantic their energyare among from nature’s the interaction most powerful and difference cyclonesbetween on earthcold Arctic, deriving air masses their energy and wfromarm thesubtropical interaction air andmasses. difference ETCs can betweenproduce cold storms Arctic air with masses central and low warm pressure subtropical as low air asmasses. 916 mb, ETC windss can up produceto 140 storms mph and with wave central heights low pressureover 100 feet.as low Given as 916 the mb,recent winds record up of to 140IPCC mph reports and andwave extreme heights weather, over 100 the feet. final Given section the offers recent predictions record of for IPCCETC reports development and extreme and trackingweather,. the final section offers predictions for ETC development and tracking. The disruption and loss to everyday life from extreme weather is Thecalamitous. disruption andAs the loss science to everyday of climatology life from continues extreme to weather evolve, TransReis calamitous.strives to Asinform the thescience insurance of climatology industry ofcontinues advancements to evolve, in theTransRe field. Our strivesefforts to inform come withthe insurance the hope thatindustr propertyy of advancements damage, loss in of the life field. and societalOur
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