In summary, radiative forcing by GHG and aerosols drives changes in ET and precipitation at global and regional scales, and the associated warming shifts the balance between frozen and liquid water . Rising CO2 concentrations also affect the water cycle via plant physiological responses affecting transpiration, including via reduced stomatal opening and increased leaf area . Land cover changes and urbanisation affect both the climate and land hydrology by altering the exchanges of energy and moisture between the atmosphere and surface  and changing the permeability of the land surface. Direct human interventions in river systems and groundwater systems are non- climatic drivers with substantial impacts on the water cycle  and have the potential to change as part of societal responses to climate change .
IPCC
Climate Change 2022: Impacts, Adaptation and Vulnerability
IPCC Report