c2vsim workshop 5 - c2vsim surface water representation
DESCRIPTION
The California Central Valley Groundwater-Surface Water Simulation Model (C2VSim) simulates the monthly response of the Central Valley’s groundwater and surface water flow system to historical stresses, and can also be used to simulate the response to projected future stresses. C2VSim contains monthly historical stream inflows, surface water diversions, precipitation, land use and crop acreages from October 1921 through September 2009. The model dynamically calculates crop water demands, allocates contributions from precipitation, soil moisture and surface water diversions, and calculates the groundwater pumpage required to meet the remaining demand.TRANSCRIPT
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The California Central Valley Groundwater-Surface Water
Simulation Model
Surface Water Processes
Charles Brush Modeling Support Branch, Bay-Delta Office
California Department of Water Resources, Sacramento, CA
CWEMF C2VSim Workshop January 23, 2013
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Outline
IWFM Surface Water Process
Stream Reach Budget
IWFM Small-Stream Watersheds Process
Small Watersheds Budget
C2VSim Results
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IWFM Surface Water Process
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Surface Water Process
Diversions
Inflow
Outflow
Runoff
Return Flows
Groundwater
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IWFM
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Stream Flow and Stream-Aquifer Interaction
• Assumption of zero storage at a stream node in computing stream flows; i.e. total inflow equals total outflow
• Fully coupled stream and groundwater conservation equations
• Simultaneous solution of stream and groundwater equations results in the computation of stream-aquifer interaction
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Stream Flow • Assumption of zero storage at a stream node
s soutsinQ Q Q 0− + =
Qs = stream flow, (L3/T) Qsin = inflows into stream (flow from upstream nodes, return
flow, rainfall runoff, tributary inflows, tile drain, lake outflow, bypass, user specified flows), (L3/T)
Qsout = outflows from stream (diversions, bypass flows, stream-aquifer interaction), (L3/T)
• Assumption requires simulation time step to be large enough for stream flow to travel from upstream to downstream in a single time step
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Stream-Groundwater Interaction
; ss s ssint b b s
KQ C max h ,h max h,h C LWd
= − =
stream surface
W
ds
h hb hs
datum
groundwater table
Qsint = stream-aquifer interaction, (L3/T) h = groundwater head, (L) hs = stream surface elevation, (L) hb = stream bottom elevation, (L) Ks = stream bed hydraulic
conductivity, (L/T) ds = stream bed thickness, (L) L = length of stream segment, (L) W = channel width, (L)
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Stream Diversions • Used to meet agricultural
and urban water demands
• User-specified fractions of diversion become recoverable (recharge to groundwater) and non-recoverable (evaporation) losses
• May be used to simulate spreading basins (100% recoverable and non-recoverable losses)
Stream
Groundwater
Recoverable Loss
Non-recoverable Loss
Delivery
Diversion
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Lake-Groundwater Interaction • One or more elements can be specified
as lake elements
• Lakes are fully coupled with groundwater
• Lake storage is a function of precipitation, evaporation, inflows, lake-aquifer interaction and lake outflow
lklkin lkout
S Q Q 0t∆
− + =∆
∆Slk = change in lake storage, (L3)
Qlkin = lake inflow (precipitation, inflows from streams and upstream lakes), (L3/T)
Qlkout = lake outflow (evaporation, lake spill, lake-aquifer interaction), (L3/T)
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Lake-Groundwater Interaction
( ) ( ) lklkint lk lk blk blk lk lk
lk
KQ C max h ,h max h,h ; C Ad
= − =
datum
hlk
hlkmax
lake surface
iblkh
ilkd
Qlkint = lake-aquifer interaction, (L3/T) h = groundwater head, (L) hlk = lake surface elevation, (L) hblk = lake bottom elevation, (L) Klk = lake bed hydraulic conductivity,
(L/T) dlk = lake bed thickness, (L) Alk = area of lake, (L)
• Lake outflow is computed when lake surface elevation exceeds maximum lake elevation
• Lake outflow can be directed to a stream node or a downstream lake
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Monthly at 38 locations
Inflows
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Inflows File
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Inflows File Sacramento River
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Monthly at 246 locations
Diversions
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Surface Water Diversions
• Diversions and imports – “Diversions” means water taken from a
simulated river node, subject to availability – “Imports” generally means water taken from a
source that is not modeled • Reservoirs outside the model area serving canals • Reservoirs inside the model area that are not
modeled (for example Black Butte and Camanche) • Complex delivery systems (California Aqueduct)
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Surface Water Imports
• Friant-Kern Canal – Release water from Millerton Lake to canal – Deliveries to contractors along canal – Wasteway flows to river beds for delivery to
down-stream customers – Flows to Kern River
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Surface Water Imports
• Friant-Kern Canal deliveries simulated as: – Imports to individual subregions – Separate diversions for
• Agricultural • Urban • Refuges • Spreading (Aquifer Storage)
– Diversions to some districts via river channels • Inflow “FKC Wasteway Deliveries to Tule River” • Diversion from river
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Surface Water Exports & Imports
• California Aqueduct – Pump water from Delta to San Luis Reservoir
(outside model area) – Release water from San Luis Reservoir for use
inside model area – Release water from San Luis Reservoir for use
outside model area
• Simulated as exports and imports – Too complex to incorporate in a regional model
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Diversion Specification
Source River Node (0 = import) Allocation to losses and delivery Destination subregion Land use (23 = Ag, 22 = urban)
Diversion source and destination
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Diversion Specification Recharge area for recoverable losses
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• Flood control • Kings River bifurcation • ASR programs
Bypasses
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Bypass Specification Source and destination river nodes
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Bypass Specification Recharge area for recoverable losses
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River Parameters
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Lake Parameters
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Stream Reach Budget
Column Flow 08/31/2004 Process Upstream Inflow (+) IN 2,944 Downstream Outflow (-) OUT 781 Tributary Inflow (+) IN 0 SWS Tile Drain (+) IN 0 GW Runoff (+) IN 0 LS Return Flow (+) IN 2 LS Gain from Groundwater (+) +/- -1,593 GW Gain from Lake (+) +/- 0 Diversion (-) OUT 0 LS By-pass Flow (-) OUT 573 Discrepancy (=) 0.00 Diversion Shortage 0
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Lake Budget
Column Flow 08/31/2004 Process Beginning Storage (+) 63,418 Ending Storage (-) 51,052 Flow from Upstream Lake (+) IN 0 Flow from By-passes (+) IN 799 Precipitation (+) IN 0 Gain from Groundwater (+) +/- 1,939 GW Lake Evaporation (-) OUT 15,104 Lake Outflow (-) OUT 0 Discrepancy (=) 0.30 Lake Surface Elevation (FEET) 185
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Diversions & Imports
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Surface Water Destinations
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1922-1929 1960-1969
2000-2009
Surface Water Destinations
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Notes
IWFM Small Watersheds
Groundwater
Surface Water
Precipitation Evapotranspiration
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Small-Stream Watersheds
• Calculate monthly ungaged surface water inflows and groundwater inflows
• Areas and flow channels from CalWater watershed coverage
• Grouped with nearest boundary node • Resulted in 210 small-stream watersheds • Approximately 5% of surface water inflow
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Small-Stream Watersheds
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Small-Stream Watersheds
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Small-Stream Watersheds Eliminate the gaged watershed
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Small-Stream Watersheds These are the ungaged watersheds
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Small-Stream Watersheds Overland flow paths
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Small Watersheds
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Small Watershed Parameters
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Small Watershed Budget
Column Flow 08/31/2004 Process Total SW Outflow OUT 6,049 GW Base Outflow OUT 90,386 Base Flow + Surface Percolation OUT 90,456 Net Surface Outflow to Streams OUT 5,979
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Small-Watershed Inflows
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Small Watershed Inflows
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