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Long-term Rainfall Analysis towards Detection of Meteorological Drought over Kozhikode District of Kerala

机译:长期降雨对检测分析在科泽科德地区气象干旱喀拉拉邦

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This study was carried out with the objective of identifying the trends in season, annual rainfall and occurrence of drought events using different statistical methods for the period of 110 years for Kozhikode district of Kerala, India. The results showed that the average annual rainfall of Kozhikode is 3177 mm with the standard deviation of 551.7 mm. The coefficient of variation confirmed that annual rainfall has very low inter annual variability, but the seasonal variability is high. Trend analysis results revealed that the rainfall is decreasing in Southwest Monsoon, Northeast Monsoon and Winter Season while increasing trend was observed in Summer Season. To understand the variation due to climate change, the time scales were divided into two (viz., 1902-1956 and 1957-2012), and trend analysis were carried out. The results showed that the Southwest Monsoon indicated a decreasing trend in both time scales; however substantial decreasing trend was observed for the recent decade i.e. 1957-2012 indicating the climatic variability. Precipitation Concentration Index (PCI) analysis showed that, among the 110 years, 57 years are coming under the classification of strong irregularity in the rainfall (PCI > 20) and the remaining years falls under the class of irregular precipitation with the PCI value 15-20. Drought indices were characterized using Rainfall Anomaly Index, Departure Analysis of Rainfall, Deciles, and Standardized Precipitation Index and the occurrence of drought events were identified. The wavelet analysis clearly showed noticeable change in the rainfall pattern after 1950 and indicating the impact of climate change. Findings from such studies are useful tools for policy makers to devise strategic management plans to overcome droughts and mitigate their effects on the activities in different sectors of the Kerala State.
机译:本研究的目标识别趋势季节,年降雨量并使用不同的干旱事件的发生统计方法的110年科泽科德地区的喀拉拉邦,印度。结果表明,平均年降雨量科泽科德是3177毫米的标准551.7毫米的偏差。证实,年降雨量有很变化低国际年度变化,但季节性可变性很高。显示,降雨减少西南季风、东北季风和冬季观察季节而增加的趋势夏天的季节。气候变化、时间尺度被分成两个(即1902 - 1956和1957 - 2012年),和趋势进行了分析。西南季风表示减少趋势在这两个时间尺度;最近观察下降趋势十年即1957 - 2012年的气候指示可变性。(PCI)的分析显示,在110年,57年的分类下强烈的不规则的降雨(PCI > 20)剩下的几年属于的类不规则的降水与PCI值15 - 20。干旱指数的概念是使用降雨特征异常指数,离职分析降雨,十分位数,标准化降水指数和确定了干旱事件的发生。小波分析清楚地显示明显1950年和后降雨模式的变化说明气候变化的影响。从这些研究都是有用的工具的政策制造商设计战略管理计划克服干旱和减轻其影响在喀拉拉邦的不同领域的活动状态。

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