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COHYST2010 Groundwater Model: Phase II Summary. April 15 th -16 th Lincoln, NE Nebraska Department of Natural Resources. COHYST 2010: Groundwater Model Objectives. Simulate groundwater system response to changes in pumping, recharge Measured through water levels, baseflows
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COHYST2010 Groundwater Model:Phase II Summary April 15th-16th Lincoln, NE Nebraska Department of Natural Resources
COHYST 2010: Groundwater Model Objectives • Simulate groundwater system response to changes in pumping, recharge • Measured through water levels, baseflows • Couple with CROPSIM & STELLA models to build integrated water budget
COHYST 2010: Groundwater Model Context † Average 1985-2005, from COHYST 2010 Phase I water budget report FINAL Phase I Water Budget CalendarYr3252012.doc
COHYST 2010: Groundwater Model Fundamental Approach • Single layer • ½ mi x ½ mi grid cells • Transient – 255 Stress periods (Oct-84 to Dec-2005) • Vadose zone not considered
COHYST 2010: Groundwater Model Fundamental Approach Platte & tribs simulated with variable stage, routing, and integrated in-stream budget (STR) Bounding basins included
COHYST 2010: Groundwater Model Fundamental Approach • Pumping + Recharge from CROPSIM • Annual pattern same, magnitude varies • Monthly stress periods • Initial condition (uncertain) estimated from: • mapped water levels • STR elevations • point observations
COHYST 2010: Groundwater Model Fundamental Approach • Functional goals: • Low mass balance (solver) error • Manageable run time • Robust – avoid instabilities under changed stresses • Level of calibration commensurate with purposes
COHYST 2010: Groundwater Model Fundamental Approach:Calibration • Baseflow targets – uncertain in managed system • Reach-by-reach • Semi-quantitative match{annual, seasonal} • Head targets – some uncertainty • Quantitative history match: • absolute elevations • relative differences
COHYST 2010: Groundwater Model Fundamental Approach:Calibration • Inputs: • Aquifer properties, boundary condition assignments,pumping, recharge, Platte surface flows, “observed” data for history matching • Manipulations: • Adjust properties, assignments within reasoned hydrologic constraints to better match observed history • Outputs: • Water levels, baseflows, regional water budget terms
COHYST 2010: Groundwater Model: Structure Stream Package
COHYST 2010: Groundwater Model: Structure General Head Boundaries
COHYST 2010: Groundwater Model: Structure Drain, River Boundaries
COHYST 2010: Groundwater Model: Structure • Evapotranspiration (EVT) • riparian, shallow GW • Head dependent: defined everywhere, active only where water level near “surface” • Elevation assignments: • Extinction depth: 1*stddev(DEM) • Max elevation: DEM maximum
COHYST 2010: Groundwater Model: Structure • Evapotranspiration (EVT)
Final Zoned Hydraulic Conductivity • Hydraulic conductivity spatial distribution
COHYST 2010: Groundwater Model: Structure • Recharge (RCH) & Pumping (WEL) • From CROPSIM Outputs
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching • Head & baseflow residuals, statistics • Time series comparison (qualitative) • Trend differences • Internal budget reasonable? • Purpose: • GW budget makes sense within integrated budget? • Model suitable for, capable of assessing impact of change in GW on contributions to streams? • Robust enough to accommodate widely variable input stresses?
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching: GW Budget
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching: Head Residuals
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching: Head Residuals
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching: Head Residuals
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Calibration/history-matching: Baseflow Residuals, Qualitative comparisons
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: Baseflows
Quantitative/ Qualitative Comparisons
Simulated Baseflow (blue) Baseflow Target (dark grey) Daily Gage flow (light grey)
Logarithmic Scale Simulated Baseflow (blue) Baseflow Target (dark grey) Daily Gage flow (light grey)
Comparison of Simulated Total Flows (STELLA and MODFLOW) Simulated baseflow & daily measured gage flow for reference
Logarithmic Scale Comparison of Simulated Total Flows (STELLA and MODFLOW) Simulated baseflow & daily measured gage flow for reference
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary: OutbasinBaseflows
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary: OutbasinBaseflows
COHYST 2010 - Groundwater Model Final Run (22a_17_21) Summary • Evaluation criteria: • Purpose: • Scenario robustness • tested in Nov/Dec 2012, throughout process • Able to translate GW to SW (or baseflow) • Depletions testing – in progress • Hydrologic connection/Cycle Well/[28/40 or 10/50] – in progress • Integrated budget – addressed by Duane
COHYST 2010 - Phase II Groundwater ModelSuccesses & Limitations • Water levels: • overall good agreement between measured and simulated heads, especially in area of interest • Trends/changes match reasonably well • Seasonal and multi-year variation captured • Congruence between modeled & observed groundwater flow system
COHYST 2010 - Phase II Groundwater ModelSuccesses & Limitations • Baseflows: • Can simulate seasonal, multiyear variability • Generally match magnitude of gains on a reach-by-reach basis within uncertainty of targets • Demonstrate dynamic interchange of SW/GW • Congruence between modeled & observed interaction of groundwater & surface water • *Lower Platte reaches?