3D DBSCAN detection and parameter sensitivity of the 2022 Yangtze river summertime heatwave and drought

极端气候事件的精准识别是机理分析的重要前提.本研究借助无监督机器学习中经典的DBSCAN密度聚类算法,发展了在三维(经度-纬度-时间)空间内进行目标事件识别和参数敏感性分析的研究方案.在2022年长江全域高温伏秋旱事件识别中的应用表明,本次天气尺度极端热浪和季节尺度重旱事件的产生发展,空间传播模式不同.天气尺度热浪信号自6月底从北太平洋向西南方向延伸,直至8月中旬覆盖长江全域;季节重旱信号于7月中旬从孟加拉湾陆面区域向东北向延伸,直至9月中旬覆盖长江全域.同时,本研究中亦进行了相关参数敏感性的详细分析,对算法应用,结果理解亦有帮助.

Spatially and temporally accurate event detection is a precondition for exploring the mechanisms of climate extremes.To achieve this,a classical unsupervised machine learning method,the DBSCAN(Density-Based Spatial Clustering of Applications with Noise)clustering algorithm,was employed in the present study.Furthermore,the authors developed a 3D(longitude–latitude–time)DBSCAN-based workflow for event detection of targeted climate extremes and associated analysis of parameter sensitivity.The authors applied this 3D DBSCAN-based workflow in the detection of the 2022 summertime Yangtze extreme heatwave and drought based on the ERA5 reanalysis dataset.The heatwave and drought were found to have different development and migration patterns.Synoptic-scale heatwave extremes appeared over the northern Pacific Ocean at the end of June,extended southwestwards,and covered almost the entire Yangtze River Basin in mid-August.By contrast,a seasonal-scale drought occurred in mid-July over the continental area adjacent to the Bay of Bengal,moved northeastwards,and occupied the entire Yangtze River Basin in mid-September.Event detection can provide new insight into climate mechanisms while considering patterns of occurrence,development,and migration.In addition,the authors also performed a detailed parameter sensitivity analysis for better understanding of the algorithm application and result uncertainties.