Abstract

Intense monsoonal rain is one of the major triggering factors of floods and mass movements in Nepal that needs to be better understood in order to reduce human and economic losses and improve infrastructure planning and design. This phenomena is better understood through intensity-duration-frequency (IDF) relationships, which is a statistical method derived from historical rainfall data. In Nepal, the use of IDF for disaster management and project design is very limited. This study explored the rainfall variability and possibility to establish IDF relationships in data-scarce situations, such as in the Central-Western hills of Nepal, one of the highest rainfall zones of the country (~4500 mm annually), which was chosen for this study. Homogeneous daily rainfall series of 8 stations, available from the government’s meteorological department, were analyzed by grouping them into hydrological years. The monsoonal daily rainfall was disaggregated to hourly synthetic series in a stochastic environment. Utilizing the historical statistical characteristics of rainfall, a disaggregation model was parameterized and implemented in HyetosMinute, software that disaggregates daily rainfall to finer time resolution. With the help of recorded daily and disaggregated hourly rainfall, reference IDF scenarios were developed adopting the Gumbel frequency factor. A mathematical model [i = a(T)/b(d)] was parameterized to model the station-specific IDF utilizing the best-fitted probability distribution function (PDF) and evaluated utilizing the reference IDF. The test statistics revealed optimal adjustment of empirical IDF parameters, required for a better statistical fit of the data. The model was calibrated, adjusting the parameters by minimizing standard error of prediction; accordingly a station-specific empirical IDF model was developed. To regionalize the IDF for ungauged locations, regional frequency analysis (RFA) based on L-moments was implemented. The heterogeneous region was divided into two homogeneous sub-regions; accordingly, regional L-moment ratios and growth curves were evaluated. Utilizing the reasonably acceptable distribution function, the regional growth curve was developed. Together with the hourly mean (extreme) precipitation and other dynamic parameters, regional empirical IDF models were developed. The adopted approach to derive station-specific and regional empirical IDF models was statistically significant and useful for obtaining extreme rainfall intensities at the given station and ungauged locations. The analysis revealed that the region contains two distinct meteorological sub-regions highly variable in rain volume and intensity.

Highlights

  • We focused on available on available daily monsoonal rainfall series to parameterize the model adopting a global optimization daily monsoonal rainfall series to parameterize the model adopting a global optimization algorithm

  • The main objective was to establish monsoonal IDF relationship; we focused on the monsoonal rainfall series and the probability distribution function (PDF) parameters

  • The evaluation of the historical daily rainfall series from the available 11 stations led to the exclusion of three stations (Chapakot, Nr. 810; Lamachaur, Nr. 818 and Ghandruk, Nr. 821) from further analysis as these data passed the threshold of inhomogeneity or contained more than five percent of missing values

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Summary

Introduction

While critical to maintaining ecosystem services and supporting livelihoods, is a triggering factor that needs to be understood and managed in order to reduce impacts due to flooding and mass movements and erosion. Reducing and managing climate-induced disaster-risk (e.g., damage due to floods and landslides) relies on knowledge of the frequency and intensity of rainfall events [11]. Extreme precipitation-induced pluvial flood and shallow landslide disaster management requires the establishment of intensity-duration-frequency (IDF) relationships of extreme events in order to formulate better design guidelines for the development of infrastructure so as to reduce impacts due to disaster-risk, and save lives, property and ecosystems [12]

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