鄱阳湖流域极端降水时空分布和非平稳性特征

全球变暖背景下的极端天气气候事件显著增加。本研究基于PreWhitening Mann-Kendall(PWMK)、极点对称模态分解法和广义可加模型,利用鄱阳湖流域1959—2019年16个国家级气象站点的逐日降水数据,从极端降水的强度、频率和持续性3个维度系统检测和分析流域极端降水的时空分布和非平稳性特征。结果表明: 研究期间,鄱阳湖流域极端降水强度和频率呈显著增加趋势,持续性呈下降趋势,极端降水整体表现出强度大、频率高、持续时间短的特点;极端降水存在明显的汛期和非汛期时间分异规律,汛期极端降水集中在流域北部和中部,而非汛期多集中于中部,子流域中信江流域降水量增加趋势最显著,达到2.10 mm·a^-1;汛期极端降水的持续时间越长,强度和范围越小,非汛期极端降水则相反;鄱阳湖流域的极端降水强度和频率以平稳性特征为主,持续性表现出非平稳性特征。随着鄱阳湖流域极端降水量的不断增加,其可能引发的灾害风险将进一步增大。

Temporal-spatial and non-stationarity characteristics of extreme precipitation in the Poyang Lake Basin,China

Extreme weather/climate events increased significantly because of global warming. Based on daily records from 16 meteorological stations in the Poyang Lake Basin (PLB) from 1959 to 2019, we comprehensively investigated the temporal-spatial and non-stationarity characteristics of extreme precipitation from three dimensions (intensity, frequency and duration) using PreWhite-ning Mann-Kendall (PWMK), extreme-point symmetric mode decomposition method (ESMD) and the generalized additive models for location, scale and shape (GAMLSS). The results showed that the intensity and frequency of extreme precipitation increased significantly in the PLB, while the duration of extreme precipitation decreased from 1959 to 2019. The extreme precipitation had features of high intensity, high frequency, and short duration in the PLB. There was a clear distinction between flood season and non-flood season for extreme precipitation. Extreme precipitation was concentrated in the northern and central PLB during the flood season and in the central PLB during the non-flood season. The increasing trend of extreme precipitation amount was 2.10 mm·a^-1 in the Xinjiang basin, which had the largest increment over the PLB. In the flood season, the extreme precipitation had longer duration but weaker intensity and smaller range, contrasting with the status during the non-flood season. The intensity and frequency of extreme precipitation showed stationarity characteristics in the PLB. However, the duration of extreme precipitation showed non-stationarity characteristics. With the continuous increase of extreme precipitation amount, the risk of related disasters would increase.