Groundwater storage changes are estimated with hydro-geodesy in the Tibetan Plateau.
Groundwater increases in the Three Rivers Source Region of the eastern Plateau.
Groundwater increases in the central Qiangtang Nature Reserve, Upper Indus basin.
Groundwater increases in the Aksu River basin south to the central Tien Shan.
Groundwater decreases along Afghanistan, Pakistan, North India and Bangladesh.