Knowledge graph centered on Elevation-stratified mountain watershed hydrological modeling with 76 nodes and 152 connections. Top connected: Convergence across biomes to a common rain-use eff, climate change, elevational gradients, snowpack persistence, groundwater storage dynamics.
Hydrological modeling approach that stratifies mountain watersheds by elevation zones to quantify water budget components and assess climate change impacts on streamflow and groundwater storage.
Synthesized from method descriptions across 11 papers using this protocol.
Steps below were extracted from the most recent peer-reviewed implementation of this protocol in the corpus — Controls from above and below: Snow, soil, and steepness drive diverging trends of subsurface water and streamflow dynamics (2025), Hydrological Processes. The protocol was originally introduced by Convergence across biomes to a common rain-use efficiency (2004), Nature. Implementations in other papers (listed below) may differ.