4.7 Article

What does I30 tell us? An assessment using high-resolution rainfall event data from two Australian locations

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CATENA
卷 180, 期 -, 页码 320-332

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ELSEVIER
DOI: 10.1016/j.catena.2019.05.011

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I-50; EI30; Rainfall intensity; Rainfall event; Millaa Millaa; Fowlers Gap

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The maximum depth of rainfall in any 30-minute period-I-30-has been used as an index of erosive rainfall events for more than half a century, and is a key component of the R factor in the Universal Soil Loss Equation (USLE) and its derivatives. Other indices are in common use, including I-5, I-10, and I-15. However, there has been little study of the ability of I-30 to capture the erosive nature of a rainfall event in regions beyond the foundation experimental work in the USA. This paper examines several apparently neglected issues: how reliance on fixed clock-periods might diminish the efficacy of the various indices of short-interval intensity; how well a single 30 minute period is able to reflect the intensity-duration properties of long enclosing rainfall events, and hence, whether the influence of event duration should be evaluated in applications of I-30 and related indices. Results from two Australian sites with high-resolution rainfall records show that within the enclosing rainfall events, actual intensities corresponding to the I-30 value (which is an equivalent intensity or 'rainfall rate', calculated from rainfall depth in 30 min) commonly occur for both less and > 30 min. Often the I-30 interval within a rainfall event excludes the most intense periods of rain, and in long events the index reflects 1% of the event duration. The I-30 intensity can occur for total durations of 1-3 h in the events studied, or for just a few minutes. An alternative class of indices is proposed, in which fixed clock-periods are not used, and instead, the duration of rainfall within an event that exceeds a nominated intensity is recorded as an index of intensity. This has a number of advantages, including the ability to work with events shorter than 30 min, which are frequently intense but which cannot yield an I-30 index that is strictly comparable to those of longer events. Illustrative results for this new index are presented.

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