基于SPEI指数的丹寨县干旱气候特征及气象因子分析
Analysis of Drought Climate Characteristics and Meteorological Factors in Danzhai County Based on SPEI Index
DOI: 10.12677/CCRL.2023.125095, PDF,   
作者: 盛升旺*, 皮义均:丹寨县气象局,贵州 丹寨;马洪燕:岑巩县气象局,贵州 岑巩;蒋松林:剑河县气象局,贵州 剑河;杨胜忠#:黔东南州气象局,贵州 凯里
关键词: SPEI干旱气候特征气象因子SPEI Drought Climate Characteristics Meteorological Factors
摘要: 基于1960~2022年丹寨县国家气象观测站逐月气象数据,通过计算月、季、年时间尺度的标准化降水蒸散指数(SPEI)的序列变化情况,采用M-K突变检验和相关分析法分析了丹寨县月、季、年时间尺度的干旱演变特征和各类气象因子与SPEI的相关性。结果表明:1) 1960~2022年丹寨县月、季、年SPEI值均有年代际的变化,总体向湿润化方向发展。2) 春旱事件发生频率最高,秋旱次之,春、秋季节主要以轻到中旱为主,重旱高发期主要在夏季和冬季。季节变化气候特征中,秋季向干旱趋势发展,春、夏、冬三个季节为向湿润趋势发展。3) 年尺度及季尺度降水量与SPEI相关性最强,季节尺度的气象因子对SPEI的影响更明显。
Abstract: Based on monthly meteorological data from the National Meteorological Observatory of Danzhai County from 1960 to 2022, the time series changes of standardized precipitation evapotranspiration index (SPEI) at monthly, seasonal, and annual scales were calculated. The M-K mutation test and correlation analysis were used to analyze the drought evolution characteristics at monthly, seasonal, and annual time scales in Danzhai County, as well as the correlation between various meteorological factors and SPEI. The results show that: 1) From 1960 to 2022, the monthly, quarterly, and annual SPEI values in Danzhai County showed interdecadal changes, and generally developed towards humidification. 2) The frequency of spring drought events is the highest, followed by autumn drought. The spring and autumn seasons are mainly characterized by mild to moderate drought, and the high incidence period of severe drought is mainly in summer and winter. In the climate characteristics of seasonal changes, autumn tends to develop towards drought, while spring, summer, and winter tend to develop towards wetness. 3) Annual and seasonal precipitation have the strongest correlation with SPEI, with seasonal meteorological factors having a more significant impact on SPEI.
文章引用:盛升旺, 马洪燕, 蒋松林, 皮义均, 杨胜忠. 基于SPEI指数的丹寨县干旱气候特征及气象因子分析[J]. 气候变化研究快报, 2023, 12(5): 925-932. https://doi.org/10.12677/CCRL.2023.125095

参考文献

[1] GB/T 20481-2017. 气象干旱等级[S]. 北京: 中国标准出版社, 2017.
[2] 张敏, 黄晓荣, 任文辉. 基于SPEI指数的金沙江流域气象干旱时空特征分析[J]. 中国农村水利水电, 2022(1): 95-101.
[3] 杨庆, 李明星, 郑子彦, 等. 7种气象干旱指数的中国区域适应性[J]. 中国科学, 2017, 47(3): 337-353.
[4] 张景扬, 卢远, 李嘉力, 等. 基于SPEI的广西干旱时空变化特征分析[J]. 云南地理环境研究, 2015, 27(6): 15-24.
[5] 熊光洁, 王式功, 李崇银, 等. 三种干旱指数对西南地区适用性分析[J]. 高原气象, 2014, 33(3): 686-697.
[6] 薛华柱, 李阳阳, 董国涛. 基于SPEI指数分析河西走廊气象干旱时空变化特征[J]. 中国农业气象, 2022, 43(11): 923-934.
[7] 王玉雪, 李波, 王槿妍, 等. 基于Mann-Kendall检验法的北运河流域降水和径流变化趋势分析[J]. 北京水务, 2022, 5(1): 24-28.
[8] 齐斐, 张春强, 刘霞, 等. 基于M-K检验和地统计分析的沂蒙山区降雨侵蚀力时空变化趋势研究[J]. 水土保持通报, 2021, 41(5): 146-53.
[9] 曹永强, 李可欣, 任博, 等. 基于SPEI的辽宁省气象干旱特征及驱动因素分析[J]. 水利水电科技进展, 2022, 42(5): 28-36.