henderson, david james (2010) response of pierced fixed

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This file is part of the following reference: Henderson, David James (2010) Response of pierced fixed metal roof cladding to fluctuating wind loads. PhD thesis, James Cook University. Access to this file is available from: http://eprints.jcu.edu.au/12173

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This file is part of the following reference:

Henderson, David James (2010) Response of pierced fixed metal roof cladding to fluctuating wind loads.

PhD thesis, James Cook University.

Access to this file is available from:

http://eprints.jcu.edu.au/12173

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Page 169 of 207

Appendix A. Air-chamber trials

Figures show the cracking and deformation of cladding adjacent to the fixings at the completion of

the cyclic and simulated wind trials. For the cyclic trials the order is not chronological but is in

increasing magnitude of Pmin and then R. Note that the variation in colour of the cladding is due to

the varying light levels (e.g., flash, ambient light, or fluorescent lighting).

Trial S2 S3 S4 S5 Pmax

(kPa) R Ni

C45 ‐2.9  0.14  21030 

C29 ‐3.1  0.41  22796 

C44 ‐3.2  0.06  6830 

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C43 ‐3.4  0.13  4590 

C51 ‐3.46  0.04  2718 

C52 ‐3.47  0.01  1986 

C54 ‐3.47  0.01  1478 

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C49 ‐3.5  0.01  1810 

C50 ‐3.5  0.01  1980 

C27 ‐3.5  0.06  2702 

C55 ‐3.52  0.02  1626 

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C46 ‐3.54  0.07  2601 

C53 ‐3.55  0.02  1215 

C28 ‐3.6  0.08  3351 

C5

‐3.7  0.32  2910 

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C37 ‐3.75  0.13  2448 

C42 ‐3.8  0.01  900 

C30 ‐3.8  0.16  2507 

C32 ‐3.8  0.29  6922 

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C25 ‐3.85  0.00  808 

C34 ‐3.9  0.23  10030 

C31 ‐3.9  0.26  2370 

C17

‐4.1  0.02  632 

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C18 ‐4.1  0.03  1676 

C35 ‐4.1  0.24  2800 

C38

‐4.2  0  1009 

C39 ‐4.35  0  630 

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C12 ‐4.8  0.38  1491 

C13 ‐4.8  0.38  1845 

C14

‐4.8  0.38  2182 

C15

‐4.8  0.38  1890 

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C20 ‐4.95  0.42  1764 

C33 ‐5  0.40  1589 

C21 ‐5.05  0.42  2867 

C41 ‐5.06  0.45  2864 

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C40 ‐5.1  0.45  3960 

C19

‐5.1  0.49  7207 

W7

‐5.6  w  ‐ 

W1

‐6.7  w  ‐ 

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W4 ‐7.2  w  ‐ 

W5 ‐7.1  w  ‐ 

W2 ‐8.0  w  ‐ 

W3 ‐8.0  w  ‐ 

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Page 181 of 207

  ‐ W6 ‐8.3  w

Appendix B. Data for area of cladding screw study

Model dimensions and tap layouts used in the assessment of representative numbers of taps for the

tributary area of a cladding screw discussed in Chapter 5, are given in Figures B1 and B2. Table B1

presents the rainflow cycle counts for the 1, 2, 9 and 51 tap cases, as summarised in Chapter 5.

Figure B1: Dimensions (in full scale) of model showing location of the high density instrumented panel in the gable end corner (Ho and Surry 2000)

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Figure B2: Dimensions (in full scale) of the corner instrumented panel (Ho and Surry 2000) (Note: The dashed rectangle highlights the region of taps centred on tap 409)

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Table B1: Cycle counts for screw at tap 409 from rainflow analysis as discussed in Chapter 5

0.00 1.00 2.00 3.00 4.00 5.00 6.00 7.00 8.00 9.00 Range

1.00 2.00 3.00 4.00 5.00 6.00 7.00 8.00 9.00 10.00 total Mean (a) Area average 1 tap

0.00 -1.00 9 9 -1.00 -2.00 418 22 2 442 -2.00 -3.00 1920 193 51 10 2 2176 -3.00 -4.00 2640 343 129 72 29 18 2 3233 -4.00 -5.00 1349 192 59 22 10 7 11 5 1 1 1657 -5.00 -6.00 403 66 13 4 486 -6.00 -7.00 97 8 105 -7.00 -8.00 10 2 12 -8.00 -9.00 1 1 -9.00 -10.0 0 total 6847 826 254 108 41 25 13 5 1 1 8121 (b) Area average 2 taps – Numbers of cycles difference to 1 tap case (a) 0.00 -1.00 -1 -1 -1.00 -2.00 -56 -8 -1 -65 -2.00 -3.00 -201 -17 -6 -4 -2 -230 -3.00 -4.00 -46 -13 -4 -3 4 -6 -1 -69 -4.00 -5.00 97 5 1 4 1 4 3 2 1 0 118 -5.00 -6.00 104 6 6 -1 1 1 117 -6.00 -7.00 32 12 3 1 48 -7.00 -8.00 4 2 6 -8.00 -9.00 -1 -1 -9.00 -10.0 0 total -68 -13 -1 -3 4 -2 3 2 1 0 -77 99% 98% 100% 97% 110% 92% 123% 140% 200% 100% 99% (c) Area average 9 taps – Numbers of cycles difference to 1 tap case (a) 0.00 -1.00 -1 -1 -1.00 -2.00 -65 -8 -1 -74 -2.00 -3.00 -199 -23 -9 -4 -1 -236 -3.00 -4.00 -131 -6 4 -2 2 -7 -1 -141 -4.00 -5.00 45 -3 -2 1 2 6 1 1 1 0 51 -5.00 -6.00 57 5 6 -1 1 1 70 -6.00 -7.00 31 12 1 44 -7.00 -8.00 4 0 4 -8.00 -9.00 0 0 -9.00 -10.0 0 total -259 -23 -1 -6 4 0 0 1 1 0 -283 96% 97% 100% 94% 110% 100% 100% 120% 200% 100% 97% (d) Influence coefficients 51 taps – Numbers of cycles difference to 1 tap case 0.00 -1.00 -5 -5 -1.00 -2.00 -166 -10 -2 -178 -2.00 -3.00 -466 -64 -25 -8 -1 -564 -3.00 -4.00 -172 3 5 -4 -5 -10 -1 -184 -4.00 -5.00 251 19 2 15 4 11 -2 2 0 0 301 -5.00 -6.00 129 15 11 2 2 1 2 1 164 -6.00 -7.00 74 18 3 95 -7.00 -8.00 13 2 15 -8.00 -9.00 4 4 -9.00 -10.0 0 total -338 -17 -6 5 0 2 -1 2 1 0 -352 95% 98% 98% 105% 100% 108% 92% 140% 200% 100% 96%

Page 184 of 207

Appendix C. Pressure time series data

The AS/NZS1170.2:2002 and wind tunnel pressure coefficients for the various NIST building

configurations, discussed in Chapter 6, are presented in this Appendix.

C.1: Building 5-5 in open terrain

Table C1: AS/NZS1170.2:2002 Region C, Terrain Category 2

Cp,e Kl Design Pressure (external) (kPa)

Area A -0.9 2 -4.68 Area B -0.9 2 -4.68 Area C -0.3 1 -0.78 Area A -0.9 3 -7.02 (draft standard)

wall +0.7 1.25 +2.28

Figure C1: Minimum external and net peak pressure coefficients for Building 5-5 modelled in

Open terrain

Page 185 of 207

Figure C2: Mean and minimum peak pressure coefficients for Building 5-5 modelled in Open

terrain

Table C2: Wind tunnel (50 m/s mean at 10 m open terrain) qz = 1.5 kPa

Cp Pressure Wind tunnel / Design (kPa)

Area A ext -6.34 -7.70 1.65 (1.10 if KL of 3) Area A net -7.09 -8.61 1.35 (0.97 if KL of 3) Area B ext -4.39 -5.34 1.14 Area B net -5.35 -6.50 1.00 Area C ext -1.26 -1.53 1.96 Area C net -3.26 -3.96 1.52

wall +2.76 +3.35 1.47

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Figure C3: Pressure trace with GF 1.4 and a dominant opening occurring on long wall at 135

minutes

Table C3: Rainflow count for building 5-5 with dominant opening in long wall for half duration

Range 0.9 1.7 2.6 3.4 4.3 5.2 6.0 6.9 7.7 8.6 Mean (kPa) 0.0 0.9 1.7 2.6 3.4 4.3 5.2 6.0 6.9 7.7 Total (a) External pressure cycles Building 5-5 orientation 25 GF=1.4 -0.9 0.0 32594 505 33099 -1.7 -0.9 24031 1404 297 52 25784 -2.6 -1.7 13231 1224 361 133 51 12 15012 -3.4 -2.6 5119 584 194 77 75 25 13 1 6088 -4.3 -3.4 1489 207 56 20 11 1 10 8 2 1 1805 -5.2 -4.3 397 52 16 4 1 1 471 -6.0 -5.2 65 6 3 74 -6.9 -6.0 10 1 1 12 -7.7 -6.9 4 4 -8.6 -7.7 0

total 79640 3983 928 286 138 39 23 9 2 1 82349 (b) Net pressure cycles Building 5-5 orientation 25 GF=1.4

-0.9 0.0 33722 1163 34885 -1.7 -0.9 19819 1348 427 108 21702 -2.6 -1.7 12857 1189 381 151 76 26 14680 -3.4 -2.6 6053 714 204 84 68 42 27 13 7205 -4.3 -3.4 2016 306 89 24 10 8 4 5 9 3 2474 -5.2 -4.3 619 104 26 6 5 1 1 762 -6.0 -5.2 178 29 7 2 216 -6.9 -6.0 15 3 1 1 20 -7.7 -6.9 4 4 -8.6 -7.7 4 4

total 75287 4856 1135 376 159 77 31 18 9 4 81952

Page 187 of 207

Figure C4: Pressure coefficients for building 5-5 with a dominant opening in gable end wall

Figure C5: Pressure trace based with GF = 1.4 and a dominant opening in gable end wall for

whole trace

Page 188 of 207

Table C4: Rainflow cycles for Building 5-5 orientation 25 with opening on gable end

Range 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 9.0 10.0 Mean (kPa) 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 9.0 total Design cyclone trace Building 5-5 orientation 25 GF=1.4 Gable Door -1.0 0.0 28040 493 28533 -2.0 -1.0 23853 1314 287 62 25516 -3.0 -2.0 14298 1351 397 128 68 10 16252 -4.0 -3.0 6965 893 298 134 82 51 23 4 8450 -5.0 -4.0 2527 385 119 40 25 20 17 14 2 4 3153 -6.0 -5.0 811 140 44 14 6 2 1 3 1021 -7.0 -6.0 220 34 18 4 276 -8.0 -7.0 44 10 2 1 57 -9.0 -8.0 9 1 10

-10.0 -9.0 4 4 total 76771 4620 1166 382 182 83 41 18 5 4 83272

C.2: Building 5-5 in suburban terrain

Table C5: AS/NZS1170.2:2002 Region C, Terrain Category 3

Cp,e Kl Design Pressure (external) (kPa)

Area A -0.9 2 -3.40 Area B -0.9 2 -3.40 Area C -0.3 1 -0.57 Area A -0.9 3 -5.10 (draft standard)

wall +0.7 1.25 +1.65

Table C6: Wind tunnel (36.3 m/s mean at 10 m suburban terrain) qz = 0.79 kPa

Cp Pressure Wind tunnel / Design (kPa)

Area A ext -9.52 -5.95 1.75 (1.16 if KL of 3) Area A net -10.40 -6.49 1.38 (1.01 if KL of 3) Area B ext -5.31 -3.31 0.97 Area B net -7.10 -4.43 0.94 Area C ext -1.82 -1.14 1.99 Area C net -5.39 -3.36 1.78

wall +4.86 +3.03 1.83

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Figure C6: Minimum and mean pressure coefficients for building 5-5 in suburban terrain

Figure C7: Minimum external and net peak pressure coefficients for building 5-5 in suburban

terrain

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Figure C8: Pressure trace with GF=1.7 and a dominant opening occurring on long wall at 135

minutes

Table C7: External and net rainflow cycle count for building 505

EXT Range 0.6 1.2 1.7 2.3 2.9 3.5 4.1 4.6 5.2 5.8 Mean (kPa) 0.0 0.6 1.2 1.7 2.3 2.9 3.5 4.1 4.6 5.2 total (a) External pressure cycles Building 5-5 orientation 25 -0.6 0.0 33318 847 34165 -1.2 -0.6 13756 1106 492 121 15475 -1.7 -1.2 4275 453 214 114 103 34 5193 -2.3 -1.7 1253 149 58 35 23 18 23 12 1571 -2.9 -2.3 366 53 21 4 4 3 1 1 3 456 -3.5 -2.9 88 11 3 1 103 -4.1 -3.5 19 2 21 -4.6 -4.1 3 2 5 -5.2 -4.6 0 -5.8 -5.2 1 1

total 53079 2623 788 275 130 55 23 13 1 3 56990 (b) Net pressure cycles Building 5-5 orientation 25 NET Range 0.6 1.3 1.9 2.6 3.2 3.9 4.5 5.2 5.8 6.5 Mean (kPa) 0.0 0.6 1.3 1.9 2.6 3.2 3.9 4.5 5.2 5.8 -0.6 0.0 29901 770 30671 -1.3 -0.6 13556 1157 507 141 15361 -1.9 -1.3 4344 442 213 116 112 46 5273 -2.6 -1.9 1336 158 53 26 20 14 23 14 1644 -3.2 -2.6 346 42 10 7 1 1 4 2 413 -3.9 -3.2 106 17 3 4 130 -4.5 -3.9 22 5 27 -5.2 -4.5 4 4 -5.8 -5.2 0 -6.5 -5.8 1 1

total 49616 2591 786 294 132 61 24 14 4 2 53524

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C.3: Building 5-14 in open terrain

Building eaves height of 5 m with a 14° pitch roof (6.43m mid roof height)

Table C8: AS/NZS1170.2:2002 Pressures for building 5-14 Region C, Terrain Category 2

Cp,e Kl Design Pressure (external) (kPa)

Area A -0.9 2 -4.83 Area B -0.5 2 -2.68

Area C/D -0.5 2 -2.68 Area A -0.9 3 -7.24 (draft standard)

wall +0.7 1.25 +2.35

Table C9: Peak pressures from Wind tunnel (50 m/s mean at 10 m open terrain) qz = 1.5 kPa

Cp Pressure Wind tunnel / Design (kPa)

Area A ext -5.44 -6.61 1.37 (0.91 if KL of 3) Area A net -6.57 -7.99 1.19 (0.88 if KL of 3) Area B ext -2.31 -2.81 1.05 Area B net -4.00 -4.86 1.07 Area C ext -1.77 -2.15 0.80 Area C net -3.65 -4.44 0.97 Area D ext -3.04 -3.69 1.38 Area D net -4.80 -5.83 1.28

Wall +2.85 +3.47 1.47

Figure C9: Minimum external and net peak pressure coefficients for building 5-14 in open

terrain

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Figure C10: Minimum and mean pressure coefficients for building 5-14 in open terrain

C.4: Building 5-14 in suburban terrain

Building eaves height of 5 m with a 14° pitch roof (6.43m mid roof height)

Table C10: Pressures from AS/NZS1170.2:2002 Region C, Terrain Category 3

Cp,e Kl Design Pressure (external) (kPa)

Area A -0.9 2 -3.53 Area B -0.5 2 -1.96

Area C/D -0.5 2 -1.96 Area A -0.9 3 -5.29 (draft standard)

wall +0.7 1.25 +1.71

Table C11: Peak pressures from wind tunnel time series (36.3 m/s mean at 10 m suburban

terrain)

Cp Pressure Wind tunnel / Design (kPa)

Area A ext -7.19 -4.48 1.27 (0.85 if KL of 3) Area A net -8.43 -5.25 1.07 (0.79 if KL of 3) Area B ext -3.83 -2.39 1.22 Area B net -6.40 -3.99 1.20 Area C ext -2.47 -1.54 0.79 Area C net -5.62 -3.50 1.05 Area D ext -4.42 -2.76 1.41 Area D net -7.24 -4.52 1.36

Wall +4.24 +2.65 1.55

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Figure C11: Minimum external and net peak pressure coefficients for building 5-14 in suburban

terrain

Figure C12: Minimum and mean pressure coefficients for building 5-14 in suburban terrain

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Table C12: Rainflow cycle count for Building 5-14 in suburban terrain

NET Range 0.5 0.9 1.4 1.8 2.3 2.7 3.2 3.6 4.1 4.5 Mean (kPa) 0.0 0.5 0.9 1.4 1.8 2.3 2.7 3.2 3.6 4.1 total suburb Roof area D - building 5-14 orient 75 dominant opening in long wall -0.5 0.0 24143 312 24455 -0.9 -0.5 27177 1363 306 73 28919 -1.4 -0.9 11789 1162 305 140 79 25 13500 -1.8 -1.4 3541 478 126 53 26 23 21 6 4274 -2.3 -1.8 937 175 42 18 6 2 3 2 8 4 1197 -2.7 -2.3 285 55 18 4 362 -3.2 -2.7 50 9 0 1 1 61 -3.6 -3.2 9 4 1 14 -4.1 -3.6 1 1 2 -4.5 -4.1 0

total 67932 3559 798 289 112 50 24 8 8 4 72784

Figure C13: Roof area B on building 5-14 orientation 75 modelled in rough terrain

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Figure C14: Roof area D on building 5-14 orientation 75 modelled in rough terrain

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Appendix D. Generated pressure traces based on

actual cyclone events

D.1 Cyclone Tracy D.1.1 Darwin

TC Tracy impacted the city of Darwin on 25 December 1974. The cyclone had a small diameter but

was a very intense slow moving system which produced maximum wind gust velocities in the range of

65 to 70 m/s. The cyclone passed directly over Darwin on an E-SE track as shown in Figure D.1. The

slow forward speed of the cyclone in relation to the circulation speed resulted in wind speeds being of

similar magnitude around the eye. In addition to the high wind speed a contributing factor to the

damage was the long duration of these high speeds.

Figure D.1: Track of TC Tracy (Walker 1975)

In summary the report by Walker (1975) indicated that traditional housing performed extremely

poorly, particularly those built leading up to TC Tracy, in the northern suburbs. Overall between 50

and 60% of houses were damaged beyond repair, and in some of the northern suburbs the damage was

nearly 100%.

As discussed in Chapter 2, a major factor in the extreme damage was the loss of roof cladding which

led to:

A significant loss of strength in many houses, leading to collapse

The production of a large amount of wind borne debris causing further damage to buildings

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D.1.2 Wind speed and direction

Cyclone Tracy was a seminal event in the reassessment of Australian wind loading design standards

and the development of engineered wind resistant construction for housing (Walker 2009). However

the official wind speed recording instrument, the Dines anemometer failed during the event. The Dines

anemometer was located in the path of Cyclone Tracy, with its trace, shown in Figure D.2 (Walker

1975). Walker (1975) provides estimates of wind speeds in the range of 60 to 70 m/s referenced to 10

m height, based on engineering assessments of failed structures across the Darwin area. The damage to

houses in Darwin varied depending on the location and type of construction. Typically, houses fared

much worse than engineered buildings. The “Report on Cyclone Tracy – Effect on buildings – Dec

1974” (Walker 1975) assessed patterns of damage in terms of the wind field, topography and the

variation of building strength, construction type and materials used. The report summarises a damage

survey of about 7000 houses. Appendices in volumes II and III detail the performance of engineered

structures including industrial type sheds and commercial buildings.

Figure D.2: Anemometer trace for Cyclone Tracy (Walker 1975)

The detailed post disaster damage surveys (Leicester and Reardon 1976; Walker 1975) including the

estimate of wind speeds have not only been used in setting Australian design and testing standards,

and building regulations, but also for validation data for vulnerability models for use in disaster

mitigation studies and insurance loss models (Henderson and Ginger 2007).

Recently, in developing storm surge models for warning and hazard mitigation studies, SEA modelled

the wind field, path and hypothesised rapidly changing parameters of Cyclone Tracy to achieve a good

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match with the recorded tidal surge levels in the harbour, and also the anemometer and barometer

records (Harper 2010; SEA 2005; SEA 2006). The SEA cyclone model is based on the Holland radial

profile but with imposed inflow angles and forward speed asymmetry (Harper and Holland 1999). The

analytical model can be run at any desired resolution, with estimates of wind speed and direction

typically calculated for 10 minute intervals. A sample of graphical output is given in given in Figure

D.3, showing the narrow eye and wind gust vector pattern (550 m resolution) about 30 minutes after

the peak winds at the airport were recorded (Harper 2009).

Figure D.3: Wind swath of SEA modelled Cyclone Tracy

Although Harper (2010) adapted the cyclone wind field model to generate the observed wave impacts,

measured surge heights, and official barometers and anemometer, no calibration of the model’s

overland wind fields were made against the wind field estimates derived from the damage surveys.

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While Harper contends that the failed Dines instrument probably did measure the peak wind at that

location, the modelling indicates that higher winds may have occurred closer to the coast.

A comparison of the estimated wind speeds, impacting the suburbs of Darwin, between the model and

survey is given in Table D.1. The modelled peak wind speeds are in general in close agreement with

the reported wind speeds from the Cyclone Tracy report (Walker, 1975). The two notable

discrepancies of nearly 5 m/s at East Point and Winnellie may be due to the aggregated banding of

wind speed data presented in the Cyclone Tracy report.

Table D.1: Modelled and reported peak gust wind speeds

SEA supplied data Report on Cyclone Tracy (Walker, 1975) Suburb/Location V3 Theta (ref to 10m height open terrain) m/s Degrees m/s Passage of eye Darwin AMO Dines 64.1 35 65 - 70 Eye TIWI 62.1 357 65 - 70 NAKARA 63.8 10 65 - 70 WANGURI 61.3 8 65 - 70 ALAWA 65.6 11 65 - 70 Eye RAPID CREEK 69.0 13 65 - 70 Eye WAGAMAN 62.3 8 65 - 70 NIGHTCLIFF 70.8 4 65 - 70 Eye JINGILI 65.5 16 65 - 70 Eye MOIL 63.1 20 65 - 70 Eye ANULA 61.3 23 65 - 70 Eye MILLNER 67.6 16 65 - 70 Eye COCONUT GROVE 70.1 30 65 - 70 Eye EAST POINT 74.9 30 65 - 70 Eye LUDMILLA 69.3 38 65 - 70 Eye THE NARROWS 65.0 46 65 - 70 Eye FANNIE BAY 70.3 45 65 - 70 Eye WINNELLIE 60.2 47 65 - 70 Eye PARAP 67.7 57 65 - 70 Eye THE GARDENS 67.0 62 60 - 65 STUART PARK 63.9 68 60 - 65 LARRAKEYAH 66.2 74 60 - 65 DARWIN CITY 61.2 35 60 - 65

D.1.3 Simulated pressure trace

Estimates of gust wind speed from the SEA model (referenced to 10 m height in open terrain) and

direction are plotted in Figure D.4 and Figure D.5, respectively, for the locales of Alawa and

Winnellie and for the location where the Dines anemometer was at the Darwin airport. It should be

noted that the SEA wind field model applies a gust factor of approximately 1.4 for the peak mean to

gust winds in the locales of interest.

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Alawa and Winnellie were chosen based on wind speed, change in wind direction and available

descriptions of building damage. The model wind trace for Alawa shows the eye wall skirting the

locale as opposed to the eye passing over Winnellie and the Dines anemometer. Therefore the wind

speed trace for Alawa does not rapidly drop to and rise from near zero, but neither does it have a rapid

change in wind direction to that of Winnellie or the Dines.

To compare with the “design” cyclone trace, a five hour section of the SEA modelled trace was used

approximately centred about the passage of the eye and with the mean wind speeds at the start and end

to be near to 30 m/s. The selected traces are enclosed by the box in Figure D.4 and Figure D.5.

Figure D.6 shows the five hour portion and the “design” cyclone trace mean wind speed and

corresponding wind direction.

Figure D.4: Gust wind speed at 10 m height

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Figure D.5: Wind direction, Theta (North is zero and clockwise is positive)

Figure D.6: SEA modelled and “design” mean wind speed and Wind direction

The obvious differences are the amount and rate of change in wind speed and direction for the

Cyclone Tracy modelled traces compared to the “design” cyclone. The greater angle change is

because Cyclone Tracy had a smaller radius to maximum winds than the parameters chosen for the

“design” cyclone. The larger mean wind speeds occur earlier and drop off quicker than the “design”

trace. A less obvious difference is that for the first hour of the Cyclone Tracy traces the wind direction

has minimal change. This is over the same period when the wind speeds are rapidly increasing leading

to the possibility that some building elements may be subjected to a higher level of accumulated

damage than the “design” trace.

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As per Section 6.4 the building orientation was aligned such that the maximum winds occurred in the

direction with the peak Cpe for the area A at the gable end, with a dominant opening occurring 60

minutes into the trace, that is ‘building orientation 25’. The calculated pressure traces for the Alawa

and Winnellie locations are shown in Figure D.7 and Figure D.8, respectively.

Figure D.7: Pressure trace for bo1 in Alawa

Figure D.8: Pressure trace for bo1 in Winnellie

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The pressure traces drop off markedly at approximately 140 minutes and stay low. This is due in part

to the lower wind speed but more to the cladding area A now being on the downwind part of the roof

and therefore not subjected to the large suction pressures associated with the windward edge.

To compare accumulated damage a rainflow analysis was carried out for a cladding fastener tributary

area A. The rainflow counts are given in Table D.2. The damage index (DI) values for the generated

pressure traces for Building 5-5 orientation 25 with a dominant opening was 0.29 for the Alawa trace

and 0.14 for the Winnellie trace.

The large peak pressures of the Alawa trace along with the DI of 0.29, show that 900 mm span

corrugated cladding when fixed at alternate crests would have suffered severe cracking with possible

failure. (It is interesting to note that an often quoted reason for the Darwin building authorities not

allowing the TR440 test criteria to be used in Darwin was that they believed that TR440 was allowing

cladding spans and fixings to be used in Darwin when similar spans had failed during Cyclone Tracy.)

Damage inspections of cladding and building systems were conducted by Beck (1975). Beck detailed

failure and loss of cladding to the gable end regions of low roof pitch housing in the Alawa suburb.

The cladding was fixed typically at every second crest at the ends of cladding lengths, but used a

wider screw spacing of every third or fourth crest for fixings to intermediate battens. Increasing the

spacing of the screws leads to a DI in excess of 1.0 for a Building 5-5 geometry.

Beck (1975) detailed cladding failures in the first few sheets at the gable ends of low roof pitch metal

clad industrial sheds in the Winnellie suburb. The cladding was fixed with only the three screws at

intermediate purlins as was the practice. Beck noted relatively undamaged sheds near either side of a

damaged shed. Halpern Glick Pty Ltd (1975) described the good performance of cladding on sheds

with substantial ridge ventilators. They note however, that the cladding was fixed at alternate crests at

all purlins, and was 0.60 mm thick. The ridge ventilators would greatly reduce any sudden positive

pressure arising from a windward dominant opening. The generated wind trace with building 5-5 for

the external pressure only scenario for Winnellie resulted in the DI of 0.07. This suggests survival of

the 0.42 mm thick G550 cladding in the highly loaded gable region of a building 5-5 geometry, but

that crack initiation might have occurred.

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Table D.2: Rainflow cycle counts for generated traces for Alawa and Winnellie Range 0.9 1.8 2.8 3.7 4.6 5.5 6.4 7.4 8.3 9.2 Mean (kPa) 0.0 0.9 1.8 2.8 3.7 4.6 5.5 6.4 7.4 8.3 total (a) Alawa Building 5-5 orient 25 (opening in long wall at 60 minutes) -0.9 0.0 49236 116 49352 -1.8 -0.9 12134 545 97 11 12787 -2.8 -1.8 6278 518 166 71 29 4 7066 -3.7 -2.8 2436 272 72 25 26 22 6 7 2866 -4.6 -3.7 668 102 18 3 3 2 3 3 802 -5.5 -4.6 179 28 8 0 3 218 -6.4 -5.5 56 14 1 1 72 -7.4 -6.4 13 3 17 -8.3 -7.4 1 1 -9.2 -8.3 4 4

total 71005 1598 362 112 61 26 8 7 3 3 73185 Range 0.8 1.5 2.3 3.1 3.8 4.6 5.4 6.1 6.9 7.7 Mean (kPa) 0.0 0.8 1.5 2.3 3.1 3.8 4.6 5.4 6.1 6.9 total (b) Winnellie Building 5-5 orient 25 (opening in long wall at 60 minutes) -0.8 0.0 46340 203 46543 -1.5 -0.8 9132 512 135 29 9808 -2.3 -1.5 5157 440 131 51 26 12 5817 -3.1 -2.3 2139 236 75 32 23 16 11 7 2539 -3.8 -3.1 651 93 11 3 2 2 1 5 4 772 -4.6 -3.8 217 42 12 0 2 273 -5.4 -4.6 66 14 4 1 85 -6.1 -5.4 18 2 1 21 -6.9 -6.1 6 6 -7.7 -6.9 4 4

total 63730 1542 368 117 53 28 13 8 5 4 65868 Range 0.7 1.4 2.0 2.7 3.4 4.1 4.8 5.4 6.1 6.8 Mean (kPa) 0.0 0.7 1.4 2.0 2.7 3.4 4.1 4.8 5.4 6.1 total (c) Winnellie Building 5-5 orient 25 (no dominant opening) -0.7 0.0 37852 15 37867 -1.4 -0.7 10708 404 59 5 11176 -2.0 -1.4 6779 550 152 38 8 1 7528 -2.7 -2.0 3024 346 108 41 33 20 5 3577 -3.4 -2.7 940 147 37 12 9 5 6 8 2 2 1168 -4.1 -3.4 257 41 9 3 1 2 313 -4.8 -4.1 93 17 6 5 121 -5.4 -4.8 21 3 24 -6.1 -5.4 8 1 9 -6.8 -6.1 3 3

total 59685 1524 371 104 50 26 12 8 4 2 61786

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D.2 Cyclone Vance

In 1999, Cyclone Vance hit Exmouth in Western Australia, with wind speeds up to 70m/s, similar to

those estimated from Cyclone Tracy. The maximum winds from Cyclone Vance did not pass over

Exmouth, as its track was to the east of the town. Section 6.1 details the track and wind speed record

of the cyclone.

The 10 minute mean wind speeds at 10 m height, recorded by the Learmonth automatic weather

station (AWS) three cup anemometer, and direction are plotted in Figure D.9. Learmonth is the

aerodrome servicing the town of Exmouth, with the locations shown in Figure 6.2. The form of the

mean wind speed varying with time and the change in wind direction is similar to the “design” cyclone

parameters proposed by Jancauskas et al. (1994) with both cyclones having a wide diameter as

opposed to Cyclone Tracy.

Figure D.9: Mean wind speed and direction from AWS for Learmonth

A generated pressure trace based on the AWS wind speeds and direction for building 5-5 orientation

25 geometry with a dominant opening in the long wall, is shown in Figure D.10. The peak pressure

was -6.7 kPa, with a corresponding DI of 0.21. Detailed damage investigations of light gauge metal

cladding observed minimal sign of fatigue failure of cladding (Reardon et al. 1999). The lack of

fatigue damage was attributed in part to the fast forward motion of the cyclone (short duration) but

more to the fact that Exmouth is located in cyclonic Region D, with a corresponding ULS VR,500 of 85

m/s. Correspondingly, cyclone washers were used in the installation of cladding to increase the design

capacity.

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Figure D.10: Generated trace for Cyclone Vance based on Building 5-5 orientation 25, with opening on long wall at 200 minutes