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Last modified
11/23/2009 10:40:45 AM
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10/4/2006 10:23:01 PM
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Title
Australian Rainfall and Runoff 1998, Revision of Book VI - Estimation of Large to Extreme Floods
Date
11/28/1998
Prepared By
Rory Nathan, Sinclair Knight Merz
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />UKAI-I U <br /> <br />tsOOK VI- tstlmatlon or Large to txtreme I"'I000S <br /> <br />I <br /> <br />I <br /> <br />Table 2 Summary of procedures to derive Design Rainfalls. <br /> <br /> <br />I <br /> <br />I <br />I <br /> <br />The credible limit of <br />extrapolation generally <br />ranges from 1 in 1 00 to <br />1 in 5000 AEP <br /> <br />Use of design <br />estimates based on <br />regional pooling of data <br />(Section 3.3.2) <br /> <br />Extrapolation of IFD <br />data to 1 in 500 AEP <br />(Section 3.3.1) where <br />no regional data exists <br />(applies only to a <br />limited range of <br />situations) <br /> <br />All rainfall depths are <br />for design bursts <br /> <br />For information on <br />seasonal estimates see <br />Section 3,7 <br /> <br />Generalised IFD <br />information (Section <br />3.2); spatial <br />variation in depths <br />may need to be <br />accounted for <br />(Section 3.10b) <br /> <br />, <br />I <br /> <br />Not appiicable <br /> <br />I <br /> <br />Interpolation to areal PMP <br />estimate based on either: <br /> <br />shape factors <br />(Section 3.6.1) <br /> <br />2 paramo parabolic <br />function (Section 3.6.2) <br /> <br />extrapolation from long <br />to short duration storms <br />(Seclion 3.6.3) <br /> <br />See Section 3.2(b) for <br />discussion on areal <br />reduction factors <br /> <br />Derived from point design rainfalls by application <br />of areal reduction factors (ARFs), selected as a <br />function of storm area, duration, and AEP (design <br />ARFs based on regional data may not be <br />available for all regions in Australia). <br /> <br />I <br /> <br />See Table 6 for <br />summary of <br />interpolation <br />procedures (applied to <br />areal rainfalls) <br /> <br />I <br /> <br />See Figure 2 for areas <br />covered by different <br />generalised methods <br />Genera/ised methods <br />yield areal PMP depths <br />AEP of PMP based <br />solely on catchment <br />area, Section 3.5 <br /> <br />GSDM for short <br />durations and small <br />areas (Section 3-4.2) <br /> <br />GSAM for SE Aust <br />region (Section 3.4.3) <br /> <br />GTSM for tropical <br />region (Section 3-4-4) <br /> <br />I <br /> <br />Not applicable <br /> <br />I <br /> <br />- GSDM pattems for all <br />short durations <br /> <br />- GTSM patterns for long <br />durations in tropical <br />areas <br /> <br />Unsmoothed GSAM for <br />long durations in SE <br />Aust <br /> <br />Both GSDM and <br />unsmoothed GSAM for <br />intennediate durations <br />In SE Aust <br /> <br />GSDM patterns for all <br />short durations <br /> <br />GTSM pattems for all <br />durations in tropical <br />areas <br /> <br />GSAM for long <br />durations in SE Aust. <br /> <br />Both GSDM and GSAM <br />for intermediate <br />durations in SE Aust. <br /> <br />GSDM patterns for all <br />short durations <br />GTSM pattems for all <br />durations in tropical <br />areas <br />GSAM for long <br />durations in SE Aust. <br />Both GSOM and GSAM <br />patterns for <br />intermediate durations <br />in SE Aust <br /> <br />I <br /> <br />Unsmoothed <br />GSAM patterns <br />for long durations <br />in SE Aust. <br /> <br />Generalised <br />patterns (Book II, <br />Section 2) for all <br />other cases <br /> <br />Sae Table 8 for <br />summary of tempora' <br />pattern selection <br />Pre-burst temporal <br />patterns may be used <br />in conjunction with <br />storm losses (Section <br />3.9. Ie) <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />See Section 3.10(b) for <br />discussion on need for <br />incorporation of spatia' <br />trend <br />See Table 9 for <br />summary of spatial <br />pattern selection <br /> <br />Use either GSDM, GSAM, <br />or GTSM patterns, <br />depending on location and <br />duration <br /> <br />Uniformly distributed <br />(unless clear <br />evidence for spatial <br />trend) <br /> <br />1 <br /> <br />I <br /> <br />I <br />
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