Drought Characterisation of Syrdarya River Basin in Central Asia Using Reconnaissance Drought Index

A. Yegizbayeva, S. Ilyas, T. Berdimbetov
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引用次数: 1

Abstract

This study provides a comprehensive analysis of drought characteristics in Syrdarya River Basin (SRB) of Central Asia (CA) by using meteorological and environmental variables derived from reanalyzed information database. Drought Intensity and Frequency (DIF) curves were identified based on precipitation deficit and evapotranspiration rates by using Reconnaissance Drought Index (RDI). Climatic variables for the study period of 1985–2015 were derived from Climate Research Unit (CRU) database. The frequency and duration of events appearing from April to September of each year, and drought severity was calculated as the sum of an integral period from severe to the extreme range defined with RDI varied between −1.5 and −3, respectively. Several drought events, ranging between moderate, severe and extreme in past 30 years period, were revealed over the basin in this study. A significant decreasing trend at high elevations in contrast to obvious increasing trends at lower elevations of the river basin has been observed. The dynamic variations of drought events over the SRB indicates the variation patterns of climatic impacts on drought occurrences in the mountainous regions.
基于干旱指数的中亚锡尔达里亚河流域干旱特征
利用再分析数据库的气象和环境变量,对中亚锡尔达里亚河流域(SRB)干旱特征进行了综合分析。基于降水亏缺和蒸散速率,利用侦察干旱指数(RDI)识别干旱强度和干旱频率(DIF)曲线。1985-2015年研究期的气候变量来源于气候研究单位(CRU)数据库。每年4 - 9月的事件发生频率和持续时间以及干旱严重程度的计算分别为RDI定义的从严重到极端的积分周期之和,变化范围在- 1.5和- 3之间。该研究揭示了近30年来该流域发生的中度、重度和极端干旱事件。在高海拔地区有明显的减少趋势,而在低海拔地区则有明显的增加趋势。SRB干旱事件的动态变化反映了气候对山区干旱事件影响的变化模式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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