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A dimensionless ratio quantifying stream competence or a stream flow's capacity to mobilize bed particles of a given size
The depth below which the total annual groundwater flux is a sufficiently small fraction of the annual watershed hydrologic budget that its exclusion from watershed numerical models has a negligible i...
Water electrical conductivity that increases as solutes concentrate during pond drying
The fraction of water that was originally withdrawn from a source for irrigation and is subsequently removed from availability owing to evaporation, transpiration, or incorporation into crops
Metric defined as d-excess = δ²H - 8·δ¹⁸O, indicative of non-equilibrium conditions during evaporation and sublimation processes