Estimating present day extreme water level exceedance probabilities around the coastline of Australia: tropical cyclone-induced storm surges

The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water le...

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Published inClimate dynamics Vol. 42; no. 1-2; pp. 139 - 157
Main Authors Haigh, Ivan D., MacPherson, Leigh R., Mason, Matthew S., Wijeratne, E. M. S., Pattiaratchi, Charitha B., Crompton, Ryan P., George, Steve
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer Berlin Heidelberg 01.01.2014
Springer
Springer Nature B.V
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ISSN0930-7575
1432-0894
DOI10.1007/s00382-012-1653-0

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Abstract The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool ( www.sealevelrise.info ). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones.
AbstractList The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool ( www.sealevelrise.info ). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones.
The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones.
The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones.[PUBLICATION ABSTRACT]
The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones. Keywords Extreme water levels * Storm surges * Tides * Extra-tropical cyclones * Tropical cyclones * Hurricanes * Return levels * Return periods * Australia
Audience Academic
Author Wijeratne, E. M. S.
Pattiaratchi, Charitha B.
MacPherson, Leigh R.
Mason, Matthew S.
Crompton, Ryan P.
Haigh, Ivan D.
George, Steve
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  fullname: Wijeratne, E. M. S.
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  organization: Antarctic Climate and Ecosystems Cooperative Research Centre
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IsPeerReviewed true
IsScholarly true
Issue 1-2
Keywords Extra-tropical cyclones
Tropical cyclones
Storm surges
Hurricanes
Extreme water levels
Return levels
Australia
Tides
Return periods
Century 21st
Extreme event
Australasia
Forecast model
tides
coastal zone
hurricanes
Return period
Severe weather
Sea surge
Tropical cyclone
Risk assessment
Storm surge
Risk management
Natural hazards
sea level
Language English
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PublicationDate 2014-01-01
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  year: 2014
  text: 2014-01-01
  day: 01
PublicationDecade 2010
PublicationPlace Berlin/Heidelberg
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PublicationSubtitle Observational, Theoretical and Computational Research on the Climate System
PublicationTitle Climate dynamics
PublicationTitleAbbrev Clim Dyn
PublicationYear 2014
Publisher Springer Berlin Heidelberg
Springer
Springer Nature B.V
Publisher_xml – name: Springer Berlin Heidelberg
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– name: Springer Nature B.V
References McInnes KL, Macadam I, Hubbert GD, O’Grady JG (2011a) An assessment of current and future vulnerability to coastal inundation due to sea level extremes in Victoria, southeast Australia. Int J Clim. doi:10.1002/joc.3405
Harper BA, Holland GJ (1999) An updated parametric model of the tropical cyclone. In: 23rd conference on hurricanes and tropical meteorology, 893–896
Harper BA (ed) (2001) Queensland climate change and community vulnerability to tropical cyclones—ocean hazards assessment stage 1—review of technical requirements. Report prepared by Systems Engineering Australia Pty Ltd in association with James Cook University Marine Modelling Unit, Queensland Government, 375 pp, March 2001
McInnes KL, O’Grady JG, Hemer M, Macadam I, Abbs DJ, White CJ, Bennett JC, Corney SP, Holz GK, Grose MR, Gaynor SM, Bindoff NL (2011b) Climate future for Tasmania: Extreme tide and sea-level events. Technical Report, Antarctic Climate and Ecosystems Corporate Research Centre
HardyTAMcConochieJDMasonLBModeling tropical cyclone wave population of the Great Barrier ReefJ Waterway Port Coastal Ocean Eng2003129104113
Seneviratne SI, Nicholls N, Easterling D, Goodess CM, Kanae S, Kossin J, Luo Y, Marengo J, McInnes K, Rahimi M, Reichstein M, Sorteberg A, Vera C, Zhang X (2012) Changes in climate extremes and their impacts on the natural physical environment. In: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. Editors: Field CB, Barros V, Stocker TF, Qin D, Dokken DJ, Ebi KL, Mastrandrea MD, Mach KJ, Plattner GK, Allen SK, Tignor M, Midgley PM. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge University Press, Cambridge, UK, and New York, NY, USA, pp 109–230
NichollsRJMarinovaNLoweJABrownSVellingaPde GusmaoDHinkelJTolRSJSea-level rise and its possible impacts given a ‘beyond 4°C world’ in the twenty-first centuryPhilos Trans R Soc A Math Phys Eng Sci2011369193416118110.1098/rsta.2010.0291
PughDTChanging sea levels: effects of tides, weather and climate2004Cambridge, United KingdomCambridge University Press280 pp
GeorgiouPNDavenportAGVickeryBJDesign wind speeds in regions dominated by tropical cyclonesJ Wind Eng Ind Aerodyn19831313915210.1016/0167-6105(83)90136-8
HolmesJDWind loading of structures2001LondonSpon Press10.4324/9780203301647356 pp
EgbertGDErofeevaSEfficient inverse modeling of barotropic ocean tidesJ Atmos Ocean Technol200219218320410.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2
HarperBHardyTMasonLFryarRDevelopments in storm tide modelling and risk assessment in the Australian regionNat Hazards20095122523810.1007/s11069-009-9382-3
WoodworthPLBlackmanDLEvidence for systematic changes in extreme high waters since the mid-1970sJ Clim20041761190119710.1175/1520-0442(2004)017<1190:EFSCIE>2.0.CO;2
KistlerRKalnayECollinsWSahaSWhiteGWoollenJChelliahMEbisuzakiWKanamitsuMKouskyVDoolHJenneRFiorinoMThe NCEP-NCAR 50-year Reanalysis: monthly Means CD ROM and documentationBull Am Meteorol Soc200182224726710.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2
SimiuEScanlanRHWind effects on structures19862New YorkWiley-Interscience
HollandGJOn the quality of the Australian tropical cyclone data baseAust Meteorol Mag198129169181
HollandGJAn analytic model of the wind and pressure profiles in hurricanesMon Weather Rev19801081212121810.1175/1520-0493(1980)108<1212:AAMOTW>2.0.CO;2
KaplanJDeMariaMA simple empirical model for predicting the decay of tropical cyclone winds after landfallJ Appl Meteorol1995342499251210.1175/1520-0450(1995)034<2499:ASEMFP>2.0.CO;2
JevrejevaSMooreJCGrinstedAHow will sea level respond to changes in natural and anthropogenic forcings by 2100?Geophys Res Lett2010377L0770310.1029/2010GL042947
Haigh ID, Pattiaratchi C (2010) 21st century changes in extreme sea levels around Western Australia. In: Proceedings of the 17th National Australian Meteorological & Oceanographic Society Conference, Canberra, Australia
Haigh ID, Wijeratne EMS, MacPherson LR, Pattiaratchi CB, George S (2013) Estimating present day extreme total water level exceedance probabilities around the coastline of Australia: tides, extra-tropical storm surges and mean sea level. Clim Dyn. doi:10.1007/s00382-012-1652-1
KepertJThe dynamics of boundary layer jets within the tropical cyclone core. Part 1: linear TheoryJ Atmos Sci2001582469248410.1175/1520-0469(2001)058<2469:TDOBLJ>2.0.CO;2
VermeerMRahmstorfSGlobal sea level linked to global temperatureProc Natl Acad Sci20091062152710.1073/pnas.0907765106
McInnesKLWalshKJEHubbertGDBeerTImpact of sea-level rise and storm surges on a coastal communityNat Hazards200330218720710.1023/A:1026118417752
HortonRHerweijerCRosenzweigCLiuJGornitzVRuaneACSea level rise projections for current generation CGCMs based on the semi-empirical methodGeophys Res Lett2008352L0271510.1029/2007GL032486
Cardone VJ, Cox AT, Greenwood JA, Thompson EF (1994) Upgrade of tropical cyclone surface wind field model. Miscellaneous Paper, CERC-94-14, prepared for U.S. Army Corps of Engineers (101 pp)
McInnesKLMacadamIHubbertGDO'GradyJDA modelling approach for estimating the frequency of sea level extremes and the impact of climate change in southeast AustraliaNat Hazards2009511153710.1007/s11069-009-9383-2
PawlowiczRBeardsleyBLentzSClassical tidal harmonic analysis including error estimates in MATLAB using T_TIDEComput Geosci200228892993710.1016/S0098-3004(02)00013-4
LoweJAWoodworthPLKnutsonTMcDonaldREMcInnesKWothKVon StorchHWolfJSwailVBernierNGulevSHorsburghKUnnikrishnanASHunterJWeisseRChurchJAWoodworthPLAarupTWilsonSPast and future changes in extreme water levels and wavesUnderstanding sea-level rise and variability2010OxfordWiley-Blackwell
McConochieJDHardyTAMasonLBModelling tropical cyclone over-water wind and pressure fieldsOcean Eng2004311757178210.1016/j.oceaneng.2004.03.009
Danish Hydraulic Institute (2013) Mike 21 & Mike 3 flow model FM. Hydrodynamic and transport module scientific documentation. http://www.dhisoftware.com/Download/DocumentsAndTools/~/media/Microsite_MIKEbyDHI/Publications/PDF/Short%20descriptions/MIKE213_FM_HD_Short_Description.ashx
NottJHayneMHow high was the storm surge from tropical cyclone MahinaAust J Emerg Manag2000151113
HaighIDNichollsRJWellsNCRising sea levels in the english channel 1900–2100Proc ICE Marit Eng20111642819210.1680/maen.2011.164.2.81
Meehl GA, Stocker TF, Collins WD, Friedlingstein P, Gaye AT, Gregory JM, Kitoh A, Knutti R, Murphy JM, Noda A, Raper SCB, Watterson IG, Weaver AJ, Zhao ZC (2007) Global climate projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: The physical science basis. Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 747–845
Colberg F, McInnes KL (2012) The impact of storminess changes on extreme sea levels over southern Australia. JGR-Oceans, doi:10.1029/2012JC007919.
EliotMPattiaratchiCRemote forcing of water levels by tropical cyclones in southwest AustraliaCont Shelf Res201030141549156110.1016/j.csr.2010.06.002
McConochie JD, Mason LB, Hardy TA (1999) A Coral Sea cyclone wind model intended for wave modelling. In: Proceedings of 14th conference on coastal and ocean engineering, IEAust, Perth, pp 413–418
Hunter J (2011) A simple technique for estimating an allowance for uncertain sea-level rise. Clim Change. doi:10.1007/s10584-011-0332-1
UhlhornEWBlackPGFranklinJLGoodberletMCarswellJGoldsteinASHurricane surface wind measurements from an operational stepped frequency microwave radiometerMon Weather Rev20071353070308510.1175/MWR3454.1
ColesSAn introduction to statistical modelling of extreme values2001BerlinSpringer10.1007/978-1-4471-3675-0207 pp
MenéndezMWoodworthPLChanges in extreme high water levels based on a quasi-global tide-gauge datasetJ Geophys Res2010115C10C1001110.1029/2009JC005997
Bindoff NL, Willebrand J, Artale V, Cazenave A, Gregory J, Gulev S, Hanawa K, Le Quéré C, Levitus S, Nojiri Y, Shum CK, Talley LD, Unnikrishnan A (2007) Observations: Oceanic climate change and sea level. In: Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 385–432
JamesMKMasonLBSynthetic tropical cyclone databaseJ Waterw Port Coastal Ocean Eng2005131418119210.1061/(ASCE)0733-950X(2005)131:4(181)
RahmstorfSA semi-empirical approach to projecting future sea-level riseScience2007315581036837010.1126/science.1135456
ChurchJAGregoryJMWhiteNJPlattenSMMitrovicaJXUnderstanding and projecting sea level changeOceanography (J Oceanogr Soc)201124213014310.5670/oceanog.2011.33
HunterJEstimating sea-level extremes under conditions of uncertain sea-level riseClim Change201099333135010.1007/s10584-009-9671-6
HorsburghKLWilsonCTide-surge interaction and its role in the distribution of surge residuals in the North SeaJ Geophys Res2007112CO800310.1029/2006JC004033
O’GradyJGMcInnesKLExtreme wind waves and their relationship to storm surges in northeastern Bass StraitAust Meteorol Oceanogr J201060265275
GrinstedAMooreJCJevrejevaSReconstructing sea level from paleo and projected temperatures 200–2100 adClim Dyn201034446147210.1007/s00382-008-0507-2
VickeryPJSkerljPFTwisdaleLASimulation of hurricane risk in the U.S. using empirical track modelJ Struct Eng20001261012221237
HarperBAStroudSAMcCormackMWestSA review of historical tropical cyclone intensity in northwestern Australia and implications for climate change trend analysisAust Meteorol Mag200857121141
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References_xml – reference: McInnes KL, Macadam I, Hubbert GD, O’Grady JG (2011a) An assessment of current and future vulnerability to coastal inundation due to sea level extremes in Victoria, southeast Australia. Int J Clim. doi:10.1002/joc.3405
– reference: JamesMKMasonLBSynthetic tropical cyclone databaseJ Waterw Port Coastal Ocean Eng2005131418119210.1061/(ASCE)0733-950X(2005)131:4(181)
– reference: HorsburghKLWilsonCTide-surge interaction and its role in the distribution of surge residuals in the North SeaJ Geophys Res2007112CO800310.1029/2006JC004033
– reference: ColesSAn introduction to statistical modelling of extreme values2001BerlinSpringer10.1007/978-1-4471-3675-0207 pp
– reference: GeorgiouPNDavenportAGVickeryBJDesign wind speeds in regions dominated by tropical cyclonesJ Wind Eng Ind Aerodyn19831313915210.1016/0167-6105(83)90136-8
– reference: HollandGJAn analytic model of the wind and pressure profiles in hurricanesMon Weather Rev19801081212121810.1175/1520-0493(1980)108<1212:AAMOTW>2.0.CO;2
– reference: PughDTChanging sea levels: effects of tides, weather and climate2004Cambridge, United KingdomCambridge University Press280 pp
– reference: HarperBHardyTMasonLFryarRDevelopments in storm tide modelling and risk assessment in the Australian regionNat Hazards20095122523810.1007/s11069-009-9382-3
– reference: SimiuEScanlanRHWind effects on structures19862New YorkWiley-Interscience
– reference: VickeryPJSkerljPFTwisdaleLASimulation of hurricane risk in the U.S. using empirical track modelJ Struct Eng20001261012221237
– reference: McConochieJDHardyTAMasonLBModelling tropical cyclone over-water wind and pressure fieldsOcean Eng2004311757178210.1016/j.oceaneng.2004.03.009
– reference: KistlerRKalnayECollinsWSahaSWhiteGWoollenJChelliahMEbisuzakiWKanamitsuMKouskyVDoolHJenneRFiorinoMThe NCEP-NCAR 50-year Reanalysis: monthly Means CD ROM and documentationBull Am Meteorol Soc200182224726710.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2
– reference: NottJHayneMHow high was the storm surge from tropical cyclone MahinaAust J Emerg Manag2000151113
– reference: NichollsRJMarinovaNLoweJABrownSVellingaPde GusmaoDHinkelJTolRSJSea-level rise and its possible impacts given a ‘beyond 4°C world’ in the twenty-first centuryPhilos Trans R Soc A Math Phys Eng Sci2011369193416118110.1098/rsta.2010.0291
– reference: ChurchJAGregoryJMWhiteNJPlattenSMMitrovicaJXUnderstanding and projecting sea level changeOceanography (J Oceanogr Soc)201124213014310.5670/oceanog.2011.33
– reference: EgbertGDErofeevaSEfficient inverse modeling of barotropic ocean tidesJ Atmos Ocean Technol200219218320410.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2
– reference: HortonRHerweijerCRosenzweigCLiuJGornitzVRuaneACSea level rise projections for current generation CGCMs based on the semi-empirical methodGeophys Res Lett2008352L0271510.1029/2007GL032486
– reference: Bindoff NL, Willebrand J, Artale V, Cazenave A, Gregory J, Gulev S, Hanawa K, Le Quéré C, Levitus S, Nojiri Y, Shum CK, Talley LD, Unnikrishnan A (2007) Observations: Oceanic climate change and sea level. In: Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 385–432
– reference: Harper BA, Holland GJ (1999) An updated parametric model of the tropical cyclone. In: 23rd conference on hurricanes and tropical meteorology, 893–896
– reference: Meehl GA, Stocker TF, Collins WD, Friedlingstein P, Gaye AT, Gregory JM, Kitoh A, Knutti R, Murphy JM, Noda A, Raper SCB, Watterson IG, Weaver AJ, Zhao ZC (2007) Global climate projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: The physical science basis. Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 747–845
– reference: VermeerMRahmstorfSGlobal sea level linked to global temperatureProc Natl Acad Sci20091062152710.1073/pnas.0907765106
– reference: O’GradyJGMcInnesKLExtreme wind waves and their relationship to storm surges in northeastern Bass StraitAust Meteorol Oceanogr J201060265275
– reference: HaighIDNichollsRJWellsNCRising sea levels in the english channel 1900–2100Proc ICE Marit Eng20111642819210.1680/maen.2011.164.2.81
– reference: HolmesJDWind loading of structures2001LondonSpon Press10.4324/9780203301647356 pp
– reference: KaplanJDeMariaMA simple empirical model for predicting the decay of tropical cyclone winds after landfallJ Appl Meteorol1995342499251210.1175/1520-0450(1995)034<2499:ASEMFP>2.0.CO;2
– reference: Harper BA (ed) (2001) Queensland climate change and community vulnerability to tropical cyclones—ocean hazards assessment stage 1—review of technical requirements. Report prepared by Systems Engineering Australia Pty Ltd in association with James Cook University Marine Modelling Unit, Queensland Government, 375 pp, March 2001
– reference: RahmstorfSA semi-empirical approach to projecting future sea-level riseScience2007315581036837010.1126/science.1135456
– reference: McInnesKLMacadamIHubbertGDO'GradyJDA modelling approach for estimating the frequency of sea level extremes and the impact of climate change in southeast AustraliaNat Hazards2009511153710.1007/s11069-009-9383-2
– reference: Cardone VJ, Cox AT, Greenwood JA, Thompson EF (1994) Upgrade of tropical cyclone surface wind field model. Miscellaneous Paper, CERC-94-14, prepared for U.S. Army Corps of Engineers (101 pp)
– reference: WoodworthPLBlackmanDLEvidence for systematic changes in extreme high waters since the mid-1970sJ Clim20041761190119710.1175/1520-0442(2004)017<1190:EFSCIE>2.0.CO;2
– reference: Danish Hydraulic Institute (2013) Mike 21 & Mike 3 flow model FM. Hydrodynamic and transport module scientific documentation. http://www.dhisoftware.com/Download/DocumentsAndTools/~/media/Microsite_MIKEbyDHI/Publications/PDF/Short%20descriptions/MIKE213_FM_HD_Short_Description.ashx
– reference: Haigh ID, Pattiaratchi C (2010) 21st century changes in extreme sea levels around Western Australia. In: Proceedings of the 17th National Australian Meteorological & Oceanographic Society Conference, Canberra, Australia
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Snippet The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events,...
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SubjectTerms Annual variations
Australia
climate
Climatology
coasts
continental shelf
Continental shelves
Cyclones
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
engineering
Engineering and environment geology. Geothermics
engineers
Environment
Environmental aspects
Exact sciences and technology
External geophysics
Fluid mechanics
Geophysics/Geodesy
Hurricanes
Hydrodynamics
Hydrofoil boats
Internet
land use
Land use planning
managers
Meteorology
Natural hazards: prediction, damages, etc
Oceanography
Physics of the oceans
planning
researchers
risk
Sea level
Storm surges
Storms
Surface waves, tides and sea level. Seiches
Tidal analysis
Tidal waves
tides
Tropical cyclones
United States
wastes
Water levels
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Title Estimating present day extreme water level exceedance probabilities around the coastline of Australia: tropical cyclone-induced storm surges
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