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hydrology-expert

Expert-level hydrology covering the water cycle, surface water hydrology, groundwater, watershed analysis, flood hydrology, water quality, and water resource management.

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Hydrology Expert

Before Starting

  1. Surface water or groundwater?
  2. Flood, drought, or water quality focus?
  3. Research or engineering application?

Core Expertise Areas

Water Cycle

Precipitation: rain, snow, hail — measured by rain gauges and radar. Evapotranspiration: evaporation plus plant transpiration, largest water loss. Infiltration: water entry into soil — controlled by soil type, moisture, vegetation. Runoff: surface flow to streams — generated when precipitation exceeds infiltration. Groundwater recharge: infiltrated water reaching saturated zone.

Surface Water

Streamflow: discharge Q = A x V, measured at gauging stations. Rating curve: relationship between stage and discharge at a gauging site. Hydrograph: streamflow vs time response to precipitation event. Unit hydrograph: 1 cm of effective rainfall over watershed in unit time. Base flow: groundwater contribution to streamflow during dry periods.

Groundwater

Aquifer types: unconfined (water table), confined (artesian), perched. Darcy law: Q = -KA dh/dl, K is hydraulic conductivity. Hydraulic head: elevation head plus pressure head. Theis equation: drawdown around pumping well in confined aquifer. Groundwater flow equation: combines Darcy law and continuity.

Flood Hydrology

Return period: 100-year flood has 1% chance of exceedance in any year. Frequency analysis: fit probability distribution to annual maximum flows. Flood routing: tracking flood wave through channel or reservoir. Rational method: Q = CiA for small watersheds, C is runoff coefficient.

Best Practices

  • Always perform quality control on streamflow records
  • Use multiple methods for evapotranspiration estimation
  • Account for land use change effects on hydrology
  • Consider climate change projections in water resource planning

Common Pitfalls

PitfallFix
Confusing return period with probability100-year flood does not mean once per century
Ignoring baseflow separationStormflow and baseflow behave differently
Applying Darcy law to turbulent flowCheck Reynolds number for flow regime
Assuming stationarity in frequency analysisClimate change may shift flood frequency

Related Skills

  • geology-expert
  • meteorology-expert
  • oceanography-expert

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