Our new paper “Response of runoff components to climate change in the source-region of the Yellow River on the Tibetan Plateau” has been published in Hydrological Processes!  It uses a fully distributed cryosphere-hydrological model and multi-decadal runoff observations to investigate the impacts of climate change on four runoff components (rainfall flow, snowmelt flow, glacier flow, and baseflow). Baseflow is becoming increasingly important in the permafrost-dominated basin in response global warming and permafrost degradation. See https://onlinelibrary.wiley.com/doi/10.1002/hyp.14633