In cold regions, where snowmelt dominates the local hydrological processes, Irannezhad et al.  and Vincent et al.  show high recharge to aquifers from glacial meltwater, while Nygren et al.  report a decrease in groundwater recharge due to a shift in main recharge period from spring  to winter . In Finland, a sustained reduction  of long- term snow accumulation combined with early snowmelt has reduced spring recharge  .
IPCC
Climate Change 2022: Impacts, Adaptation and Vulnerability
IPCC Report