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This Special Issue comprises 11 papers that outline the advances in research on various aspects of climate change impacts on hydrologic extremes, including both drivers (temperature, precipitation, and snow) and effects (peak flow, low flow, and water temperature). These studies cover a broad range of topics on hydrological extremes, including hydro-climatic controls, trends, homogeneity, nonstationarity, compound events and associated uncertainties, for both historical and future climates.

regional flood frequency analysis --- flood-related attribute --- region of influence --- flood region revision process --- Canadian annual maximum flow --- extreme precipitation --- LARS-WG --- CMIP5 --- spatiotemporal changes --- climate change --- climatic controls --- multiple linear regression --- permafrost region --- streamflow extremes --- trend analysis --- variable importance analysis --- extreme events --- hydrology --- concurrent --- Colorado River basin --- heatwaves --- drought --- flooding --- low flows --- multi-purpose reservoir --- functional volume --- uncertainties --- Monte Carlo method --- hydrological extremes --- simulation-optimization model --- optimal storage volume --- simulation model --- retention volume --- transformation of flood discharges --- CMIP6 --- extreme --- SWAT --- flood --- IHA --- global warming --- Malaysia --- Kelantan --- peak flows --- predictor --- predictand --- snow water equivalent --- annual maximum flow --- western Canada --- uncertainty --- riverine flooding --- coastal flooding --- compound flooding --- projected IDF curves --- design storm --- Stephenville Crossing --- snow --- trends --- Yakima River basin --- cascade reservoirs --- design flood --- nonstationary conditions --- equivalent reliability --- most likely regional composition --- dependence structure --- glacier ablation --- North Cascade Range --- salmon --- glacier mass balance --- heat wave --- n/a