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PDF | 2 MB - Australian Building Codes Board

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In the absence of other comparable tower measurements in tropical cyclones,<br />

hurricanes and typhoons, profiles of M z, Cat based on the NW Cape measurements<br />

were incorporated into the 1989 edition of the <strong>Australian</strong> Standard on Wind Actions<br />

(AS1170.2-1989) for both Regions C and D, and the gust profile was continued<br />

without modification in the 2002 edition.<br />

Figure 4.1 shows the average maximum gust profiles derived from the 10-minute<br />

mean windspeeds and gust factors obtained for the four recorded cyclones at NW<br />

Cape. The profile in the Standard is assumed to increase monotonically up to 100m<br />

and above that height takes a constant value of 1.40 for all Terrain Categories. The<br />

Standard is conservative with respect to the averaged measurements above 100 m.<br />

However, these profiles need reviewing in the light of the more recent dropwindsonde<br />

measurements in U.S. hurricanes described in the following section.<br />

Mz cat comparisons<br />

500<br />

Height (m)<br />

400<br />

300<br />

200<br />

100<br />

0<br />

0.0 0.5 1.0 1.5<br />

Mz,Cat1<br />

Avg. measured -<br />

NW Cape<br />

AS/NZS1170.2<br />

Figure 4.1 Comparison of average measured maximum gust profiles for four<br />

cyclones (1973-7) at North-west Cape and M z,Cat 1 from AS/NZS1170.2:2002<br />

4.3 Dropwindsonde measurements<br />

The dropwindsonde (Figure 4.2) is a probe containing sensors and a GPS satellite<br />

receiver that enables profiles of various atmospheric variables, including wind speed,<br />

to be monitored as it falls after being dropped from an aircraft.<br />

Since 1997 the National Oceanic and Atmospheric Administration (NOAA) and the<br />

U.S. Air Force have been deploying GPS-based dropwindsondes into hurricanes in the<br />

Atlantic and eastern North Pacific oceans. These have generated vertical profiles of<br />

wind and thermodynamic parameters from flight level (typically about 3000 metres)<br />

down to sea level. It should be noted that dropwindsondes are not normally deployed<br />

over land.<br />

The development of the dropwindsonde has been described by Hock and Franklin<br />

(1999). Detailed analyses of wind profiles from 1997-1999 have been described by<br />

Franklin et al (2003); the main purpose was to obtain a ratio between surface (10<br />

22

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