Extreme Wind in the Asia Pacific:

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Extreme Wind in the Asia Pacific: A guessing game or an exact science? Megan Briggs April 2014

Agenda 01 02 03 04 05 Introduction to Extreme Winds Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 2 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

Agenda 01 02 03 04 05 Introduction to Extreme Winds Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 3 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

IEC standard 61400-1 Ed 3: Wind Turbine Class Site specific assessment : Turbulence Shear (0.2) Air density (1.225kg/m 3 ) Inflow angle (±8 ) V ref = reference 10 min wind speed average V ave = mean wind speed (weibull distribution) Where: V e50 = extreme wind (3-sec) with a recurrence of 50 years Where: Alstom Wind - 12/05/2014 P 4 Source: 61400-1 IEC:2005

Extreme Wind: How Three types of weather systems: Severe thunderstorm Supercell Mesoscale convective systems (Cyclonic) Extreme winds in Australia and NZ: Severe thunderstorm Warm moist air rises (updraft) Moist air cools & condenses into droplets (clouds) Droplets enlarge & fall (downdrafts) Downdrafts hit ground & spread strong horizontal winds Topographical speedups & channeling Alstom Wind - 12/05/2014 P 5

Extreme Winds in Cyclonic Regions Extreme winds highly influenced by the occurrence of cyclones and typhoons (TC) Circulating low pressure wind systems Clockwise Southern Hemisphere, counter clockwise Northern Hemisphere Condensation of water vapour supplied by warm sea surface (needs 26 C) Two wind speed peaks, one for each of the two passages of the eyewall Wind direction changes 180 Turbulence high between 15-25 m/s, however decreases above 30 m/s Source: NOAA Alstom Wind - 12/05/2014 P 6

Agenda 01 02 03 04 05 Introduction to Extreme Wind Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 7 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

Extreme Wind methodology IEC standard 61400-1 does not prescribe any preferred method for calculating V ref Most common: National Building Codes Gumbel Method of Independent Storms (MIS) or Peak Over Threshold (POT) Periodic Maxima Mesoscale virtual long term data: ie MERRA/ERA/CFSR Alstom Wind - 12/05/2014 P 8

Extreme Winds Gumbel Distribution Annual maxima fit to a gumbel distribution 50 years of data is ideal! At least 20 years for reliability! 10 years as a minimum! Pros Cons Safe to assume independence from extremes Requires at least 10-20 years of data! Source: Meteorol. Appl. 6, 119-132 (1999) We need to be able to extract more independent events from short term datasets Alstom Wind - 12/05/2014 P 9

Extreme Winds - MIS Lull threshold is defined Storm events are identified between lulls Maximum wind selected from each storm Pros More data points for gumbel distribution Cons Requires 7 years for reliability (Cook 1985) Decision needs to be made on lull threshold Cannot guarantee independence Methods are significantly influenced by the highest measured wind speed Neither sufficiently capture the Pacific typhoon climate Alstom Wind - 12/05/2014 P 10

Agenda 01 02 03 04 05 Introduction to Extreme Wind Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 11 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

Extreme Wind: Australia Example 7 years of data measurement MIS considered reliable At 89m (ECO122 hub height): Max meas. = 29.7 m/s V ref = 32.1 m/s V e50 = 45 m/s Class III What about the AS/NZS1170.2:2002 Wind Loading Standard Alstom Wind - 12/05/2014 P 12

AS/NZS1170.2:2002 Wind Loading Standard Multipliers: 1. Regional 3-sec gust wind speed 2. Wind direction and Shielding assume = 1 (conservative) 3. Terrain to structure height multiplier (shear) Based on Terrain Category (generally 1 or 2) Hub Height = 89m (ECO122) 4. Topographic speedup Alstom Wind - 12/05/2014 P 13

AS/NZS1170.2:2002 Wind Loading Standard Alstom Wind - 12/05/2014 P 14

AS/NZS1170.2:2002 Wind Loading Standard H 158 Lu 527 L2 759 L1 190 Clause (a) 0.05> 0.10 x 0 Alstom Wind - 12/05/2014 P 15

AS/NZS1170.2:2002 Wind Loading Standard Alstom Wind - 12/05/2014 P 16

AS/NZS1170.2:2002 Wind Loading Standard Compared with: V e50 Site near Wellington (Non-Cyclonic) = 45 m/s M d = 1 M z,cat = 1.23 M s = 1 M t = 1.2 V e50 Site near Cairns (Cyclonic) = 52 m/s M d = 0.95 M z,cat = 1.23 M s = 1 M t = 1.16 Alstom Wind - 12/05/2014 P 17

Agenda 01 02 03 04 05 Introduction to Extreme Wind Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 18 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

Typhoon Analysis: Southern Japan Typhoon MANI-YI 14 th July 2007 Passed 17km from project Typhoon air pressure: ~960 hpa Two wind speed maxima: 36 m/s & 30 m/s @ 60m 180 direction shift: 1 /min Alstom Wind - 12/05/2014 P 19 Source: KITAMOTO Asanobu @ National Institute of Informatics

Typhoon Climate Extreme Wind Analysis MIS with 4.5 years of data: Hub height (75m) V ref = 64.6m/s Max measured wind speed = 42.8 m/s MIS highly influenced by max wind speed METI (Japanese Trade & Industry Dept) requires wind turbines to be certified for V ref calculated by National Building Code Alstom Wind - 12/05/2014 P 20

Extreme Wind Analysis: 2010 Japanese Building Code Alstom Wind - 12/05/2014 P 21

Extreme Wind Analysis: 2010 Japanese Building Code Alstom Wind - 12/05/2014 P 22

Extreme Wind Analysis: 2010 Japanese Building Code However this assumes an air density of 1.225kg/m 3 Average site density is 1.16 kg/m 3 during a typhoons it would be significantly lower The Dvorak method and Boyle s law calculates site typhoon air density as 1.02 kg/m 3 therefore Dynamic pressure equivalent Vref is 55.5 m/s Why is this important? Dynamic pressure is what drives component loading Alstom Wind - 12/05/2014 P 23

Typhoon analysis: South Korea Typhoon TEMBIN, Aug 30 th 2012 Passed 27km from project Typhoon air pressure: ~985 hpa Two wind speed maxima: 28 m/s & 21.5 m/s @ 60m 180 direction shift: 1 /min Source: KITAMOTO Asanobu @ National Institute of Informatics Alstom Wind - 12/05/2014 P 24

Extreme Wind Atlas South Korea Extreme Wind Atlas derived from the Japanese Meteorological Agency (JMA) typhoon tracks Estimates V e50 (m/s) at 10m a.s.l Therefore for the site indicated V e50 = 45 m/s Extrapolating to hub height (assuming typhoon shear 0.11) V e50 = 56 m/s @ 1.225kg/m 3 Dynamic pressure equivalent: V e50 = 53 m/s @ 1.09 kg/m 3 Class II Alstom Wind - 12/05/2014 P 25 Source: RIS-R-1544 Extreme Winds in the Western North Pacific: Soren Ott 2006

Agenda 01 02 03 04 05 Introduction to Extreme Wind Conventional Methods Extreme Winds in Aus/NZ Extreme Winds in Northern Pacific Turbine Loads & Alstom solutions Alstom Wind - 12/05/2014 P 26 ALSTOM 2013. ALSTOM All rights reserved. 2013. Information All rights reserved. contained in Information this document contained is indicative in only. this No document representation is indicative or warranty only. is given No or representation should be relied on or that warranty it is complete is given or correct should be relied on or will apply to that any particular it is complete project. or This correct will depend or will on apply the technical to any and particular commercial project. circumstances. This will It is depend provided without on the liability technical and is and subject commercial to change without circumstances. notice. Reproduction, It is provided without use or disclosure liability to third and parties, is subject without express to change written without authority, notice. is strictly Reproduction, prohibited. use or disclosure to third parties, without express written authority, is strictly prohibited.

IEC Load Conditions in Extreme Winds IEC standard 61400-1 Design Load Cases (DLC) Normal design situations Fault design situations Transportation, installation and maintenance design situations Fatigue loads evaluate fatigue strength Ultimate loads evaluate max-strength, fatigue failure and blade tip deflection DLC 6: Parked or Idling Turbine 6.1: Extreme Wind Speed condition (EWS) 6.2: EWS combined with loss of grid 6.3: EWS combined with yaw misalignment Alstom Wind - 12/05/2014 P 27

Turbine operation in Typhoons Extreme Wind speed alone is not the cause of WT failure Considering that blade tip velocity is ~72 m/s During extreme conditions WT is parked & not subjected to dynamic component loads Failure usually occurs due to cascading faults: Loss of electrical network Loss of turbine control system Yaw error/misalignment Blade pitch misalignment WT Ultimate loads may be exceeded Alstom Wind - 12/05/2014 P 28 Damaged Wind Turbines from Typhoon Maemi, Japan 2003

ECO100 Platform customisation for Typhoon Climate Yaw backup Active yaw breaks Redundant UPS pitch control Seismic + Typhoon towers Advanced lightning protection ALSTOM PURE TORQUE Hamada 48 MW [29 x ECO 74] UNDER CONSTRUCTION Satomi 10 MW [6 x ECO 74] Operational since 2006 Kawazu 16.7MW [10 x ECO 74] Operational in 2015 Higashi Izu II 18.37 MW [11 x ECO 74] Operational in 2015 Alstom Wind - 12/05/2014 P 29

Yaw Backup & Active Yaw Brake During typhoon (10min average >30m/s) + grid loss WT switches to TYPHOON MODE Yaw System UPS allows: 180º yawing to downwind position Re-orientate WT 15º every 15min for at least 6hrs Active yaw brakes: 6 hydraulic brakes & 4 yaw motors Engage after every yaw alignment No loading on yaw gear Alstom Wind - 12/05/2014 P 30

Pitch Control System Pitch-based aerodynamic braking system Default pitch at full feather (86º) x3 independent pitch system (redundancy) UPS for control system During grid loss (typhoon): Control system connected to the UPS Blades are returned to default pitch Alstom Wind - 12/05/2014 P 31 Landes de Couesme

Summary Calculating extreme wind is essential for certifying a turbine for the 20 year project lifetime How do you calculate it? Commonly used classic methods (Gumbel, MIS) National Building Codes OTHER?? Typhoon tracks How do you combat it? Innovation (yaw backup, UPS) Determination Alstom Wind - 12/05/2014 P 32

Thank you for your attention! www.alstom.com