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Translating Scientific Advancement into Sustained Improvement of Tropical Cyclone Warnings – the Hong Kong Experience C.Y. Lam Hong Kong Observatory Hong Kong, China 28 March 2007
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Tropical Cyclone (TC) Warning System Maximising effectiveness of TC warning Design of warning system Coordination with emergency response units Forecast and warning operation Warning product presentation Communication and dissemination Post-event review Public education and outreach
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Factors determining the form of a warning system The built environment Expectations of the Society Warning System Meteorological ScienceCommunication
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Hazards associated with TCs High winds and flying debris Heavy Rain Flooding Landslip Storm surge
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Warnings Associated with TCs TC Signals Rainstorm Warning Flood Announcement Landslip Warning
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Translating science and technology into operational forecasting skills
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SWIRLS Short-range Warning of Intense Rainstorms in Localized Systems high resolution 0-3 hr QPF updated every 6 min prompting associated warnings operational since 1998 Dense raingauge network
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3 km TREC wind of a heavy rainstorm (>30mm/hr) 23 UTC 9 August 2002 3 km TREC wind of Typhoon Maria 31 August 2000 Asymmetric wind distribution (Stronger to the right, weaker to the left) SW’lies with embedded waves TREC (Tracking Radar Echoes by Correlation)
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Dynamic Z-R relation Z = aR b Searching radius radar reflectivity around 140 rain gauges
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Amber Rainstorm ( >30mm/hr ) Red Rainstorm ( >50mm/hr ) Black Rainstorm ( >70mm/hr ) Operational Mode Front-end display of SWIRLS
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Performance of SWIRLS rainstorm forecast POD = Probability of Detection FAR = False Alarm Rate
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SWIRLS Landslip Forecast If forecast >= 15 landslips -> issue Landslip Warning 21-hr actual rainfall from raingauges 3-hr SWIRLS rainfall forecast Starting 2000 Running 24-hr rainfall No. of reported landslides highly correlated
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Verification of SWIRLS Landslip Forecast Performance of SWIRLS landslip forecast POD81 % FAR26 % CSI63 % Average lead time (hr)1.5 Probability of Detection : POD = a / (a+b) *100 % False Alarm Rate : FAR = c / (a+c) *100 % Critical Success Index : CSI = a / (a+b+c) *100 % Forecast YesNo Observed Yesab NocNA SWIRLS forecast YesNo Observed Yes174 No6- Landslip warning threshold reached (2001-2006 data)
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ORSM (Operational Regional Spectral Model) Physical Initialization (PI) - using radar estimated rainfall to modify model relative humidity field and heating profile 20-km resolution 3-hourly update cycle forecasts up to 42 hours ahead
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SWIRLS and ORSM Combined Warning Panel
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Meso-scale NWP in support of Nowcasting Improving very-short-range QPF 0 – 6 hr Better grasp of growth/decay Nowcast High resolution NWP Extrapolation - effective in advective cases Coping with curved streamlines and intensity changes Rapidly updated very-short-range high-resolution QPF
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RAPIDS: 1-6 hours (Rainstorm Analysis and Prediction Integrated Data- processing System) NOWCASTING component – SWIRLS QPF by linear extrapolation of radar echoes NWP component – NHM QPF by non-hydrostatic numerical modelling
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SWIRLS – good intensity F/C NHM – good storm development F/C RAPIDS – the best F/C RAPIDS F/C + Radar observation NHM DMO F/C NHM F/C (rigid transformed) SWIRLS SLA F/C
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RAPIDS updated hourly (2 km resolution) Trial–operation since May 2005
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Ensemble TC track forecast JMA minimum mean sea-level pressure ECMWF minimum mean sea-level pressure NCEP minimum mean sea-level pressure 1.0 ° UKMO 850-hPa maximum relative vorticity HKO ensemble TC position forecast 1999 2002
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Verification of HKO TC position forecast Use of NWP Use of model ensemble forecast
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Skill of HKO TC position forecast Use of NWP Use of model ensemble forecast
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Objective guidance on TC intensity Model Output Statistics (MOS) model forecast intensity change vs observed intensity change
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Intensity forecast based on model regression with TC probabilistic categorization
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Intensity forecast based on climatology method Statistical dataset HKO’s 6-hourly best-track data of TCs within 0-45 N, 90-180 E from 1980 to 2002 Stratified by initial TC intensity category interaction type time change (T+12, T+24, T+48, T+72)
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Probability forecast of TC signal change Purpose : support TC-related decision making choice of “go” or “no go” risk assessment cost analysis Trial run with public transport sector starting from 2004
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Probability assessment Objective tools NWP technique - Track probability Statistical technique – Strong winds/Gales onset probability
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Probability assessment LOW (0 - 33 %) MEDIUM (34-66 %) HIGH (67-100 %) + Professional judgment
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Flooding due to Storm Surges ten tide gauges monitoring tide level "Sea, Lake, and Overland Surges from Hurricanes (SLOSH)" model to predict storm surge during the approach of TCs
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Storm Surge Advice If predicted storm surge + predicted astronomical tide > pre-defined threshold -> HKO issues storm surge advice in TC bulletins
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Advancement in science & technology -> sustained improvement in TC warning NMHS Numerical Weather Prediction Communication technology Human expertise Nowcasting techniques Meteorological observations Remote-sensing technology Improvement in products & services to meet evolving needs & expectations More accurate & reliable forecasts Improvement in effectiveness of warning system
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Thank you !
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