Active model cells from the Eastern Snake Plain Aquifer Model version 2.2, showing the fraction of impact of an aquifer stress applied in a cell that is predicted to accrue to each reach at steady-state. Snake River reaches include Ashton to Rexburg (A_R), Heise to Menan (H_M), Menan to Shelley (M_S), near Blackfoot to Neeley (nB_N), Neeley to Minidoka (N_M), Kimberly to Buhl (Kim_Buhl), Buhl to Lower Salmon Falls (LSF_KH), and Lower Salmon Falls to King Hill (LSF_KH). Responses at combined reaches are summed for near Blackfoot to Minidoka (NB_Min), all reaches above Minidoka (abvMilner), and all reaches below Kimberly (blwMilner). Attributes beginning with SP are the response in drain cells between Kimberly and King Hill that is predicted to emerge as surficial springs. Attributes beginning with BF are the response in river cells between Kimberly and King Hill that is predicted to emerge as obscured flow to the Snake River. See model documentation for additional information.

Sukow, J., 2021, Model calibration report, Eastern Snake Plain Aquifer Model Version 2.2, Idaho Department of Water Resources, 226 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/ModelCalibrationRpt/.

Sukow, J., 2021, Predictive uncertainty analysis, Eastern Snake Plain Aquifer Model version 2.2, Idaho Department of Water Resources, 208 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/UncertaintyRpt/.

Sukow, J., 2021, Comparison of superposition model with fully-populated model for Eastern Snake Plain Aquifer Model version 2.2, 14 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/.

Sukow, J., 2021, Comparison of Eastern Snake Plain Aquifer Model version 2.2 with version 2.1 via the curtailment scenario, Idaho Department of Water Resources, 64 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/.

Active model cells from the Eastern Snake Plain Aquifer Model version 2.2, showing the fraction of impact of an aquifer stress applied in a cell that is predicted to accrue to each reach at steady-state. Snake River reaches include Ashton to Rexburg (A_R), Heise to Menan (H_M), Menan to Shelley (M_S), near Blackfoot to Neeley (nB_N), Neeley to Minidoka (N_M), Kimberly to Buhl (Kim_Buhl), Buhl to Lower Salmon Falls (LSF_KH), and Lower Salmon Falls to King Hill (LSF_KH). Responses at combined reaches are summed for near Blackfoot to Minidoka (NB_Min), all reaches above Minidoka (abvMilner), and all reaches below Kimberly (blwMilner). Attributes beginning with SP are the response in drain cells between Kimberly and King Hill that is predicted to emerge as surficial springs. Attributes beginning with BF are the response in river cells between Kimberly and King Hill that is predicted to emerge as obscured flow to the Snake River. See model documentation for additional information.

Sukow, J., 2021, Model calibration report, Eastern Snake Plain Aquifer Model Version 2.2, Idaho Department of Water Resources, 226 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/ModelCalibrationRpt/.

Sukow, J., 2021, Predictive uncertainty analysis, Eastern Snake Plain Aquifer Model version 2.2, Idaho Department of Water Resources, 208 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/UncertaintyRpt/.

Sukow, J., 2021, Comparison of superposition model with fully-populated model for Eastern Snake Plain Aquifer Model version 2.2, 14 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/.

Sukow, J., 2021, Comparison of Eastern Snake Plain Aquifer Model version 2.2 with version 2.1 via the curtailment scenario, Idaho Department of Water Resources, 64 p., https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/.