Original source · versioned page text
Bushfire Hazard Assessment
Very large file: it may take a few minutes
The original of this document is very large (32.2 MB). Opening the original or downloading it may take a few minutes. Please be patient and don't click again. The page text is quick to read. If you are on mobile data, it is best to wait until you are on Wi-Fi.
Bushfire Hazard Assessment 14 Serenity Close, Noosa Heads 6.1.2 LANDSCAPE SLOPE Landscape slope was created from a 25m resolution digital terrain model (DTM) by calculating the maximum slope (in degrees) from the central pixel in a group of 9 x 9 cells to the eight (8) adjoining cells in that group. Maximum landscape slope within the site assessment area varied from one (1) and eleven (11) degrees (Refer to Map 8). 6.1.3 FIRE WEATHER SEVERITY In addition to vegetation fuel loads and slope, fire behaviour and intensity is influenced by a range of weather variables such as wind speed, relative humidity, temperature and atmospheric conditions, as well preceding drought conditions7. These variables are summarised as an index value which can be used by proxy to estimate and predict fire behaviour: Fire Weather Severity (FWS). The McArthur Forest Fire Danger Index (FFDI) (McArthur 1967) is the most widely used proxy of fire weather severity in Australia and is used for both bushfire hazard assessment, emergency management and in regulations such as in AS 3959:2018 Construction of buildings in bushfire-prone areas. Unlike AS 3959:2018, which adopts a single FFDI for all of Queensland (40), fire weather conditions vary spatially according to temperature, wind, relative humidity and precipitation. Although FWS is equivalent to the Forest Fire Danger Index (FFDI) defined in AS 3959:2018; spatially explicit FWS values for Queensland have been calibrated by Leonard et al. (2014) based on a gridded prediction of the FFDI from long term spatial weather products produced by the Australian Bureau of Meteorology. Adopted FWS values reflect a 1:20 year or 5% annual exceedance probability (AEP) weather event. Climate change projections suggest that the likelihood, intensity and extent of bushfires are likely to increase, together with longer, hotter and drier fire seasons (Bureau of Meteorology 2019). The gridded fire weather severity values for Queensland have been adjusted to reflect the expected climate in 2050 using the Intergovernmental Panel on Climate Change A1FI climate scenario8 (Queensland Fire and Emergency Services 2019). The fire weather severity used for the purpose of calculating fireline intensity was based on 1 in 20-year weather conditions (i.e. 5% annual exceedance probability) to reflect the severity of fires and events suited to mitigation through land use planning in Queensland and was based on advice from the Queensland Fire and Emergency Services. An FFDI of 48 was adopted based on the 5% AEP event as per Leonard et al. (2014) (Refer to Map 9). 7 Days since last rainfall. 8 The SRES A1FI scenario is most similar to the current RCP 8.5 scenario. 17 | 38
See the original
The page text is free to read. Viewing or downloading an original file needs an account.
Log in to see the originalLog in to download the original file
Very large file: the download may take a few minutes. If you are on mobile data, it is best to wait until you are on Wi-Fi.
Searchable page text hides email addresses. Original files are unchanged and may show email addresses.