State Key Joint Laboratory of Environmental Simulation and Pollution Control, China-Canada Center for Energy, Environment and Ecology Research, UR-BNU, School of Environment, Beijing Normal University, Beijing 100875, China; Sino-Canada Resources and Environmental Research Academy, North China Electric Power University, Beijing 102206, China.
State Key Joint Laboratory of Environmental Simulation and Pollution Control, China-Canada Center for Energy, Environment and Ecology Research, UR-BNU, School of Environment, Beijing Normal University, Beijing 100875, China; Faculty of Engineering and Applied Science, University of Regina, Regina, Saskatchewan S4S 0A2, Canada.
J Contam Hydrol. 2021 Dec;243:103887. doi: 10.1016/j.jconhyd.2021.103887. Epub 2021 Sep 3.
Future changes in drought events are critical for risk assessment and associated policymaking. In this study, the future changes in meteorological droughts in Henan Province, China are explored. Random forests downscaling model is first constructed based on ERA5 reanalysis data and meteorological observations. The model is validated using evaluation indices such as R and RMSE, and is shown to be able to capture the relationship between large-scale predictors and monthly precipitation. The validated random forests downscaling model is driven by multiple global climate models (GCMs) from the Phase 6 of the Coupled Model Intercomparison Project (CMIP6) under three emission scenarios for projecting three future drought characteristics (duration, frequency, and intensity). Results show that drought frequency decreases in most areas of Henan while drought duration and intensity increase in various degrees. Some differences are also observed among different emission scenarios, especially under SSP2-4.5, where the magnitudes of changes in drought duration and intensity are lower relative to other scenarios. The decrease in drought frequency in most areas is found to be caused by increases in monthly mean precipitation in this study. Changes in drought duration and intensity are related to a combination of increases in precipitation mean and variability.
未来干旱事件的变化对风险评估和相关政策制定至关重要。本研究探讨了中国河南省气象干旱的未来变化。首先基于 ERA5 再分析数据和气象观测构建了随机森林降尺度模型。该模型使用 R 和 RMSE 等评估指标进行验证,表明能够捕捉到大尺度预测因子与月降水量之间的关系。验证后的随机森林降尺度模型由耦合模式比较计划第六阶段(CMIP6)的多个全球气候模式(GCM)驱动,在三种排放情景下预测未来三种干旱特征(持续时间、频率和强度)。结果表明,河南大部分地区的干旱频率下降,而干旱持续时间和强度不同程度增加。不同排放情景之间也存在一些差异,特别是在 SSP2-4.5 情景下,干旱持续时间和强度的变化幅度相对其他情景较低。本研究发现,大部分地区干旱频率的降低是由于月平均降水量的增加所致。干旱持续时间和强度的变化与降水均值和变率的增加有关。