Now showing items 1-2 of 2
The evolution of root-zone moisture capacities after deforestation: a step towards hydrological predictions under change?
The core component of many hydrological systems, the moisture storage capacity available to vegetation, is impossible to observe directly at the catchment scale and is typically treated as a calibration parameter or obtained ...
Streamflow response to increasing precipitation extremes altered by forest management
(Amer Geophysical Union, 2016-04-28)