ArcGIS REST Services Directory Login
Home > services > Modeling > Espa22SteadyStateResponseFunction (FeatureServer) API Reference
JSON | SOAP

Modeling/Espa22SteadyStateResponseFunction (FeatureServer)

View In: ArcGIS JavaScript   ArcGIS Online Map Viewer

Service Description: <div style='text-align:Left;'><div><div><p style='margin:0 0 11 48;'><span><span>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.</span></span></p><p style='margin:0 0 11 48;'><span><span>Sukow, J., 2021, Model calibration report, Eastern Snake Plain Aquifer Model Version 2.2, Idaho Department of Water Resources, 226 p., </span></span><a href='https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/ModelCalibrationRpt/'><span><span>https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/ModelCalibrationRpt/</span></span></a><span><span>. </span></span></p><p style='margin:0 0 11 48;'><span><span>Sukow, J., 2021, Predictive uncertainty analysis, Eastern Snake Plain Aquifer Model version 2.2, Idaho Department of Water Resources, 208 p., </span></span><a href='https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/UncertaintyRpt/'><span><span>https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/UncertaintyRpt/</span></span></a><span><span>.</span></span></p><p style='margin:0 0 11 48;'><span><span>Sukow, J., 2021, Comparison of superposition model with fully-populated model for Eastern Snake Plain Aquifer Model version 2.2, 14 p., </span></span><a href='https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/'><span><span>https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/</span></span></a><span><span>.</span></span></p><p style='margin:0 0 11 48;'><span><span>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., </span></span><a href='https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/'><span><span>https://research.idwr.idaho.gov/files/projects/espam/browse/ESPAM22_Reports/Scenarios/</span></span></a><span><span>.</span></span></p><p><span /></p></div></div></div>

All Layers and Tables

Has Versioned Data: false

MaxRecordCount: 2000

Supported Query Formats: JSON

Supports Query Data Elements: true

Layers: Description: 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/.

Service Item Id: 7f98c49476194ea6b8e82eacbc531585

Copyright Text: Idaho Department of Water Resources

Spatial Reference: 102605  (8826)  LatestVCSWkid(0)


Initial Extent: Full Extent: Units: esriMeters

Document Info: Enable Z Defaults: false

Supports ApplyEdits With Global Ids: false

Support True Curves : true

Only Allow TrueCurve Updates By TrueCurveClients : true

Supports Return Service Edits Option : true

Supports Dynamic Layers: false

Child Resources:   Info   Query Data Elements   Relationships

Supported Operations:   Query   Query Contingent Values   QueryDomains   Append   Extract Changes   Get Estimates