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11/23/2009 10:40:45 AM
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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 />I <br />I <br />1 <br /> <br />nonnal range of observations must be extrapolated to the <br />range of interest in this Book. <br /> <br />(c) Design flood characteristics <br /> <br />In many cases, the flood hydrograph is required as well <br />as the peak discharge and in some cases may be more <br />important For the design of a dam spillway or a detention <br />basin, floods calculated from a range of design rainfall <br />durations should be routed through the storage for a variety <br />of combinations of spillway and gate configurations, <br />operating procedures and dam crest heights to determine <br />the optimum design. Different durations of design rainfalls <br />may be critical for different configurations and combinations <br />of conditions, which should all confonn with the <br />recommendations of ANCOLD (1998). The complete <br />hydrograph of the design flood is also required for flood <br />studies where flow profiles in natural or constructed <br />channels are to be calculated by unsteady flow prDcedures. <br /> <br />I <br />I <br /> <br />1 <br /> <br />(eI) Special circumstances <br /> <br />The recommendatiDns in this section apply only to the <br />direct estimation of floods from design rainfalls, without the <br />consideration of other factors. However, there may be <br />some cases where some other set of circumstances may <br />be critical for design. One example is dams with very large <br />storages where it is necessary to take explicit account of <br />initial storage level or rainfall sequences over very long <br />durations. The assessment of consequences on <br />communities downstream of a storage may require <br />consideration of concurrent floods in adjacent catchments. <br />Also, a series of dams along a given stream requires <br />special consideration, as failure of an upstream dam could <br />impose more severe conditions on a downstream dam than <br />its nonnal design flood. It is the responsibility of the <br />designer to consider all circumstances that are critical for <br />design. A number of issues related to these and other <br />design considerations are discussed in Section 5. <br /> <br />I <br />I <br />I <br />1 <br />1 <br /> <br />4.2 Losses and Rainfall Excess <br /> <br />I <br /> <br />4.2.1 General Considerations <br /> <br />A loss model is needed to partition the design rainfall <br />input into rainfall excess (runoff) and loss. General <br />guidance on loss mDdelling is provided in Book II Section 3, <br />and the following discussion focuses mainly on those <br />aspects that are related to the estimation of Large to <br />Extreme floods. <br /> <br />I <br />I <br /> <br />(a) Importance of design losses - Large to <br />Extreme events <br /> <br />Like temporal patterns of storm rainfan, design losses <br />are highly variable and can have an appreciable impact on <br />both the peak and volume of the resulting flood. A given <br />rainfall occurring on a dry watershed produces a <br />significantly smaller flood than the same rainfall occurring <br />on a wet watershed. For more frequent events, loss may be <br />the most important factor. Joint probability approaches <br />(Weinmann et aI., 1998) are better able to deal with the <br />high variability of design losses as, in contrast to the design <br />event approach, they IIse a probability diStribution of loss <br />values, rather than a single representative value. However, <br />the importance of losses diminishes with decreasing AEP, <br />and for Extreme events it is Iikety that losses are of lesser <br />importance than temporal patterns. For the estimation of <br />Large to Extreme floods, the use of single-valued <br />fejlr<i5enlatille *siglllosses is lhos generaVy ade~ta. <br /> <br />For extreme rains and floods, a much greater proportion <br />of a catchment may become saturated during the event <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />---.,.. ...-...,......-.. -. --';3-'- -....-...-. .---- <br /> <br />than is the case for most floods in the observed range. <br />Also, during extreme rainfalls, vegetation may be stripped <br />from the catchment, thus resulting in an increase in the <br />speed and volume of the overland flow component of runoff <br />(Kemp and Daniell. 1997). Any evidence considered <br />relevant to the changed behaviour of the catchment under <br />extreme rainfall conditions should be considered when <br />estimating the resulting design flODds. <br /> <br />(b) Losses associated with design storms and <br />design bursts <br /> <br />(i) Design storms versus design bursts <br /> <br />When considering the adoption of design losses it is <br />necessary to understand the distinction between design <br />bursts of rainfall, and design stonns. A schematic diagram <br />illustrating the difference between the two concepts is <br />shown in Figure 7. Design bursts are generally preceded by <br />SDme lower intensity rainfall (pre-burst rainfall), they do not <br />represent complete storms. The selection of design loss <br />values must take into consideration the manner in which <br />the design information was derived, and whether the losses <br />are to be applied to design storms or design bursts. <br /> <br />(Ii) Initial losses for design storms and design <br />bursts <br /> <br />In the context of the above distinction between design <br />storms and design bursts, it is clear that generally the burst <br />initial loss is less than the storm initial loss, as the pre-burst <br />rainfall within a complete storm tends to satisfy part of the <br />initial loss requirement The difference between IL. and IL. <br />increases with decreasing burst duration. <br /> <br />Intrinsically the initial loss concept relates to complete <br />storms, as the catchment saturation process depends on <br />the total rainfall from the beginning of the stonn event (and <br />pre-storm rainfall). Initial loss values from calibration to <br />historic events are also based on the analysis of complete <br />storms. However, as the design rainfall and temporal <br />pattern information presented in Section 3 generally relates <br />to design bursts, derived loss values are not directly <br />compatible with the design rainfall data. There are two <br />basic options' for overcoming this incompatibility: <br /> <br />. transform the design rainfall burst into complete design <br />storms, then apply storm initial losses (in this <br />transfonnation a constant ratio between burst rainfall <br />and storm rainfall is assumed, regardless of event <br />frequency). <br /> <br />. use design rainfall bursts with burst initial losses, I.e. <br />use initial loss values that have been adjusted for the <br />occurrence of pre-burst rainfall. <br /> <br />This distinction between the storm and burst initial loss <br />concepts has important implications for the manner In <br />which design inputs are combined (e.g. see Hill et aI., <br />1998) and specific recommendations for both concepts are <br />provided below. <br /> <br />(ill) Continuing tosses for design storms and <br />design bursts <br /> <br />For the continuing loss rate or the proportional loss <br />fraction, there is no systematic difference between the loss <br />values associated with design storms or design bursts, aOO <br />the two are treated as equivalent <br /> <br />(c) Variation of loss values with event <br />magnitude <br /> <br />The discosslon in (b) above makes it clear that stofm <br />initial loss (IL.) and burst initial loss (14) are expected to <br />show a variation with event magnitude. The two types of <br />
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