Copula Based Spatial Analysis of Drought Return Period in Southwest of Iran

Authors

  • Mohammadreza Kavianpour
    Affiliation

    Department of Civil Engineering, Khajeh Nasir al-Din Tusi University of Technology, Tehran 1969764499, Iran

  • Mohammadreza Seyedabadi
    Affiliation

    Department of Civil Engineering, Khajeh Nasir al-Din Tusi University of Technology, Tehran 1969764499, Iran

  • Saber Moazami
    Affiliation

    Water Resources Engineering Research Assistant, Western University, 1151 Richmond Street, London, Ontario N6A 3K7, Canada

  • Omid Aminoroayaie Yamini
    Affiliation

    Department of Civil Engineering, Khajeh Nasir al-Din Tusi University of Technology, Tehran 1969764499, Iran

https://doi.org/10.3311/PPci.16301

Abstract

In the past years, Khuzestan province which is located in the southwest of Iran has experienced severe droughts. Drought can be explained by its characteristics known as duration or severity. However, combination of the two features by probabilistic approach is appeared to be a well improved method to describe the phenomena. The aim of this study is to provide a more accurate statistical method of determining drought based on simultaneous analysis of two drought characteristics. Here, precipitation data from twenty stations were used to determine drought characteristics, by Standardized Precipitation Index (SPI). Joint probability function of two variables were built via copula functions. The drought return period was calculated in the form of two scenarios. The first scenario is, based on an assumption that drought is recognized by at least one of the two specific characteristics. Drought in the second scenario is distinguished by the two characteristics in a joint probabilistic form. According to research results, there was no significant difference between the north and south of Khuzestan in the study of single characteristics of drought. While analyzing two characteristics of the drought, the return period in the north was shorter than the south. The return period of droughts in the east was always shorter than in the west. The drought return period varies from 30 to 52 months and 50 to 87 months for the first and second scenarios, respectively.

Keywords:

drought, return period, Khuzestan, copula functions, standardized precipitation index, spatial analysis

Published Online

2020-08-05

How to Cite

Kavianpour, M., Seyedabadi, M., Moazami, S., Aminoroayaie Yamini, O. “Copula Based Spatial Analysis of Drought Return Period in Southwest of Iran”, Periodica Polytechnica Civil Engineering, 64(4), pp. 1051–1063, 2020. https://doi.org/10.3311/PPci.16301

Issue

Section

Research Article