flushing
flushing C‐Q patterns
flushing behavior
Increasing concentrations with discharge, with positive b values indicating enrichment behavior
green water
grey water
gridded meteorological forcing
Spatially and temporally distributed weather data products that provide precipitation, temperature, and other meteorological variables on regular grids for model input
groundwater CO2 inputs
CO2 delivered to streams through groundwater discharge
hillslope-riparian gradient
Spatial gradient from hillslope to riparian zone representing changes in hydrology, geochemistry, and proximity to stream
hydrograph extremes
Peaks and troughs in groundwater level time series representing maximum and minimum water levels
hydrologic processes
Water movement and chemistry dynamics that maintain fen ecosystems and support specialized plant communities
hydrological conditions
Water-related environmental factors including humidity, rainfall, snow cover, and soil moisture that affect disease transmission and host physiology
infiltration capacity
The maximum rate at which water can enter soil under specified conditions
instream flow protection
inter-seasonal storage
Water storage transfer between seasons, particularly winter snow storage contributing to summer flows
interception rates
interflow
Lateral movement of snowmelt downgradient through soil zone toward topographic convergent zones to form streams
inverse storage effect
More young water released from storage during wet periods than during dry periods
isothermal snowpack
Snowpack condition when snow temperature is uniform at 0°C and entering net seasonal melting cycle
kinematic wave equation
kinetic fractionation
lateral flow
lumped parameter models
Models that describe the relationship between environmental tracer concentrations and residence time distributions using convolution integrals
magnitude
melt timing
mixed-modern water
mixing model prediction bias
modern residence times
mountain pass formation
Creation of low elevation corridors through mountain ridges by water erosion
nonlinear hydrologic response
Hydrologic system responses where combined effects of multiple perturbations differ from the sum of individual effects
oxbow deposits
Diffusion-limited organic-rich deposits that result from river meanders with fine-grained nature producing near-zero rate of water flow
pore volume
Volume of void space in a column, used to normalize flow-through time in column experiments
post-depositional fluid flow
Movement of fluids through porous rocks after initial sediment deposition that can alter magnetic mineralogy and create secondary magnetic fabrics
prior appropriation
pulse flow
push-pull test
Single-well tracer test involving injection of tracer solution followed by extraction to evaluate aquifer transport and reaction processes
quantitative precipitation estimate
Estimates of precipitation amount derived from radar and other observational data
re-inundation
river networks
road drainage structures
Infrastructure components like culverts, ditches, and berms that manage water flow along roads
sap velocity
Rate of water movement through tree xylem measured using thermal dissipation methods
seasonal streamflow variation
Variations in water quality concentrations due to observed seasonal streamflow fluctuations, with smaller concentrations noted through the 1980-81 period for sampling sites downstream from mine draina...
sediment integrator concept
The concept that sediments act as integrators providing information that complements analyzed trace metal concentrations in water samples collected at or near the same stream site, representing compos...
severity
shear velocity
shortage declaration
snow heterogeneity
Spatial fragmentation of snow cover, referring to patchiness conditions
snow-covered area mapping
Remote sensing technique to identify and quantify spatial extent of snow cover using satellite imagery
soil thickness
Depth of mobile regolith layer from land surface to bedrock contact, controlling water, carbon, and nutrient dynamics
soil-plant-atmosphere-continuum
Water potential gradient system where water potential values are highest in soil, lowest in atmosphere, and intermediate in the plant, driving water movement upward
