Fig. 4: Projected GWS trends under different climate scenarios on the TP.
From: The slowdown of increasing groundwater storage in response to climate warming in the Tibetan Plateau
Bars represent projected GWS trends in the near (2019–2040) and far future (2079–2100) under three SSP scenarios. Projections were derived from a deep learning approach using bias-corrected climate projections from CMIP6 model outputs.
