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首页> 外文期刊>Journal of Hydrology >Detection and attribution of non-stationarity in intensity and frequency of daily and 4-h extreme rainfall of Hyderabad, India
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Detection and attribution of non-stationarity in intensity and frequency of daily and 4-h extreme rainfall of Hyderabad, India

机译:印度海得拉巴每日降雨和4小时极端降雨的强度和频率非平稳性的检测和归因

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摘要

The high intensity rainfall has a significant contribution in urban area flooding and understanding this high intensity rainfall over urban areas may help us to reduce the damage caused by urban floods. In this study, the changes in Hyderabad city daily and sub-daily (4-h) extreme rainfall are analyzed using various climate change detection indices. Our analysis indicates that there is increasing trend in intensity and frequency of Hyderabad city daily extreme rainfall. In addition, increasing trend in intensity and frequency of monsoon months' (June-August) 1 a.m. to 4 a.m., 5 p.m. to 8 p.m. and 9 p.m. to 12 a.m. and non-monsoon months' 5 p.m. to 8 p.m. extreme rainfall is also observed. Based on recent theoretical development in the Extreme Value Theory (EVT), the changes in extreme rainfall of Hyderabad city are further attributed through modelling the non-stationarity (trend) present in the extreme rainfall intensity and frequency. The extreme rainfall intensity is modelled with peaks-over-threshold (POT) based Generalized Pareto Distribution (GPD) and frequency is modelled using inhomogeneous Poisson distribution. The trend is incorporated as covariate in the scale parameter (a) of the GPD and the rate parameter (2) of the Poisson distribution. In this study, four physical processes, i.e. Urbanization, El Nino-Southern Oscillation (ENSO) cycle, local temperature changes, and global warming are used as covariates. Further, the combinations of these covariates are also considered for modelling the non-stationarity.
机译:高强度降雨在市区洪水中发挥了重要作用,了解这种高强度降雨在市区范围内可能有助于我们减少城市洪水造成的破坏。在这项研究中,使用各种气候变化检测指标分析了海得拉巴市每日和次日(4-h)极端降雨的变化。我们的分析表明,海得拉巴城市每日极端降雨的强度和频率呈上升趋势。此外,季风月份(6月至8月)的凌晨1点至凌晨4点,下午5点,强度和频率呈上升趋势。到晚上8点晚上9点到凌晨12点和非季风月份的下午5点到晚上8点还观察到极端降雨。根据极值理论(EVT)的最新理论发展,通过对极端降雨强度和频率中存在的非平稳性(趋势)进行建模,进一步归纳了海得拉巴市极端降雨的变化。极端降雨强度使用基于峰值阈值(POT)的广义帕累托分布(GPD)进行建模,频率使用不均匀的Poisson分布进行建模。该趋势作为协变量并入GPD的比例参数(a)和泊松分布的速率参数(2)。在这项研究中,将四个物理过程(即城市化,厄尔尼诺-南方涛动(ENSO)周期,局部温度变化和全球变暖)用作协变量。此外,还考虑将这些协变量的组合用于建模非平稳性。

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