## Abstract Information on intensityโdurationโfrequency of rainfall is commonly required for a variety of hydrologic applications. In this study, trends are estimated for different durations of annual extreme rainfall using the regional average MannโKendall __S__ trend test. The method of Lโmoments
Detection of trends in hydrological extremes for Canadian watersheds
โ Scribed by Donald H. Burn; Mohammed Sharif; Kan Zhang
- Publisher
- John Wiley and Sons
- Year
- 2010
- Tongue
- English
- Weight
- 474 KB
- Volume
- 24
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.7625
No coin nor oath required. For personal study only.
โฆ Synopsis
Abstract
The potential impacts of climate change can alter the risk to critical infrastructure resulting from changes to the frequency and magnitude of extreme events. As well, the natural environment is affected by the hydrologic regime, and changes in high flows or low flows can have negative impacts on ecosystems. This article examines the detection of trends in extreme hydrological events, both high and low flow events, for streamflow gauging stations in Canada. The trend analysis involves the application of the MannโKendall nonโparametric test. A bootstrap resampling process has been used to determine the field significance of the trend results. A total of 68 gauging stations having a nominal record length of at least 50 years are analysed for two analysis periods of 50 and 40 years. The database of Canadian rivers investigated represents a diversity of hydrological conditions encompassing different extreme flow generating processes and reflects a national scale analysis of trends. The results reveal more trends than would be expected to occur by chance for most of the measures of extreme flow characteristics. Annual and spring maximum flows show decreasing trends in flow magnitude and decreasing trends in event timing (earlier events). Low flow magnitudes exhibit both decreasing and increasing trends. Copyright ยฉ 2010 John Wiley & Sons, Ltd.
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