How Much Do We Have Left? Coming to Terms With the Colorado River Water Availability Study Annual Colorado Water Workshop July 21, 2010 Ben Harding – AMEC Earth and Environmental Erin Wilson – Leonard Rice Engineers
Colorado Decision Support System - Overview Water Management System Developed by CWCB and Division of Water Resources Goal is to provide data/tools to assist in making informed decisions regarding historic and future use of water future Legislative Authorization Initial CRDSS Development (Gunnison, Yampa, Colorado, San Juan, Dolores) RGDSS Development (Rio Grande) CRDSS (Enhancements and Extension) Maintenance & Updates, Arkansas? SPDSS Development (South Platte, North Platte)
Colorado Decision Support System HydroBase Data Management Interfaces Consumptive Use Model “StateCU” Surface Water Model “StateMod” User/Operator/ Administrator Input Results for Decision Makers GIS Coverages
Consumptive Use Model StateCU Surface Water Model StateMod Results for Decision Makers Alternate Temperature Physical and Legal Water Availability Alternate CIR Alternate Hydrology Alternate Precipitation Estimating Water Availability
Findings - Temperature Map shows Average of the Five 2040 Projections All Five Projections show Temperature Increases Increases basin-wide by 3.3 to 3.7 deg F Lower elevations show largest increase Increase occurs each month of the year
Findings - Temperature
Findings - Winter Precipitation (Nov-Mar) Map shows Average of Five Projections Increases basin-wide by 6 to 13 percent Increases more in the northern part of the basin Increases more at higher elevations Shifts from snow to rain in the shoulder months
Findings - Summer Precipitation (Apr-Oct) Decreases basin-wide by 4 to 10 percent Wet projections show more precipitation in some summer months than dry projections Decreases more in the southern part of the basin Decreases less at higher elevations
Findings - Precipitation
Findings - Crop Irrigation Requirement Map shows Average of Five Projections Increases basin-wide 2.6 to 6.7 in/yr for pasture grass Basin-wide CIR is 20% greater than historical Growing season increases basin-wide by 15 to 22 days Increases more at lower elevations
Findings - Crop Irrigation Requirement
StateMod Model Components
16 Inflow Hydrology – Natural Flows Historical Natural Flows Estimated by Removing the Effects of Man from Gaged Flows Diversions Reservoir Contents Return Flows Climate Projected Natural Flows
17 Physical Systems Diversion Structures –Location on the River –Headgate and Canal Capacities –Return Flow Locations Reservoirs –Location on River or Off-Channel –Location of Carrier Ditches –Storage Volume, Outlet Capacities, Account Size, Area/Capacity Tables Instream Flow Reaches –Beginning/Ending of Reach
18 Water Demands Irrigation Demands – Full Irrigation Water Requirements from StateCU (Historical, Based on Climate Projections) Municipal and Industrial Demands – Current Use Levels Trans-basin Demands – Current Diversions Reservoir “Demands” – Reservoir Capacities or Operational Targets
19 Water Demands CWCB Instream Flow Demands based on Water Rights Reservoir and Trans-basin Bypass Requirements based on Operational Agreements Endangered Species Flow Demands based on Flow Targets
20 Administrative Conditions Water Rights (Direct, Storage, Instream Flow) Reservoir and Carrier Operations Policies and Agreements (Such as Minimum Bypasses, Fish Flows, etc) Potential Colorado River Compact Obligations NOT Included in Phase I Conditional Rights without Current Demands NOT included in Phase I
21 Model Operations 1.Based on Natural Inflow and Return Flows from Previous Time Steps 2.Identifies Most Senior Water Right 3.Estimates Diversion =min (Demand, Water Right, Headgate Capacity, Available Flow) 4.Adjusts Downstream Flows to Reflect Senior Diversions and Immediate Return Flows 5.Future Returns are Calculated 6.Repeated for Next Junior Water Right
Sequence of Results: Uncompahgre River at Delta and Gunnison River Basin
Natural Flow
Modeled Streamflow
Water Availability
Modeled Consumptive Use
Modeled Reservoir Storage
Result Summary: West-Slope Basins
Water Availability
Modeled Consumptive Use
Modeled Reservoir Storage
Water Availability
Modeled Consumptive Use
Modeled Reservoir Storage
Water Availability
41PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Water Availability
42PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Modeled Consumptive Use
43PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Modeled Reservoir Storage
44PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Modeled Reservoir Storage
Result Summary – Natural Flow 45PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Annual flow increases in some possible futures and decreases in others Annual flow generally increases in parts of the Yampa River basin and at higher elevation watersheds Annual flow generally decreases in southwestern watersheds and at lower elevations Shifts toward earlier peak runoff Flow decreases in late summer and early fall
Result Summary – Modeled Streamflow 46PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Annual modeled streamflow decreases basin-wide, except in the Yampa River basin, and higher elevation locations in the Upper Colorado River basin Modeled Flow increases in April and May and decreases in later summer and fall months
Result Summary – Water Available to Meet Future Demands Result Summary – Water Available to Meet Future Demands 47PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Higher elevations generally have less annual flow available to meet future demands, as a percent of modeled streamflow Available flow generally increases in April and May, corresponding to the shift in natural flow hydrographs
Result Summary – Modeled Consumptive Use 48PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Increases in Yampa, White, Upper Colorado, and Gunnison basins by 4 to 18 % Decreases in the San Juan and Dolores basins by 8 %
Result Summary – Use of Reservoirs 49PRELIMINARY RESULTS – UNDER REVIEWColorado River Water Availability Study – Phase I Reservoirs show increased use Pool levels fluctuate more than historical Shifts in Runoff Increases the Value and Need for Storage