delaware source water collaborative may 8, 2014
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The National Water Census * Part of the Initiative Overview of the Delaware River Basin Focus Area Study Jeffrey M Fischer [email protected] 609-771-3953. Delaware Source Water Collaborative May 8, 2014. - PowerPoint PPT PresentationTRANSCRIPT
The National Water Census * Part of the Initiative
Overview of the Delaware River Basin Focus Area Study
Jeffrey M Fischer
Delaware Source Water CollaborativeMay 8, 2014
Objective of the Water Census:
To place technical information and tools in the hands of stakeholders, allowing them to answer two primary questions about water availability:
Does the Nation have enough freshwater to meet both human and ecological needs?
Will this water be present to meet future needs?
Water Availability AnalysisThe process of determining the quantity and timing-characteristics of water, which is of sufficient quality, to meet human and ecological needs.
Technical InformationSocio-economic ConsiderationsLegal ConsiderationsRegulatory ConsiderationsPolitical Considerations
USGS only deals with the Technical Information!
Provide Enhanced Information On:StreamflowEvapotranspiration (ET)Ecological Flow NeedsGroundwaterWater Use and Consumption
Thermoelectric Power Irrigation Public Supply
Information available at:http://water.usgs.gov/watercensus
Daily ET from Satellite Data
Thermoelectric Consumptive Use
Information Delivery
A web application for delivering water availability information at scales that are relevant to the user
Select the area of interest.
Generate information on water accounting components.
Work with the online tool to construct your water budget.
Access trend information.
Example from French Creek
Beta version available on line in next few weekshttp://water.usgs.gov/watercensus
Focused Water Availability Assessments Testing grounds for the National Water Census
State, Local, RegionalStakeholder Involvement
Surface Water Trends, Precipitation, etc
Defined Technical Questions tobe Answered
Eco Flows
Water Use
Water Quality GroundwaterResources
Global Change
Delaware River Basin Focus Area Study
USGS Water CensusJeff Fischer, Susan Hutson, Jonathan Kennen, Kelly Maloney,
Marla Stuckey, Tanja Williamson, Ward Freeman, And many more
Study Started in 2012 and will conclude in 2015
Stakeholder Results – Areas of Study Water Use – Improved acquisition, management, and
integration of water-use and water-supply data. Robust Hydrologic Model – Evaluate growth of
population centers, effects of land-use change, and effects of climate variability and climate change on water resources
Ecological Water Needs – Development of ecological-flow science for main stem & tributaries. Evaluate flow alteration effects for ungaged tributaries. Improve decision support tool on main stem
Today’s talk focuses on Water Use and development of the Hydrologic Model.
Delaware River Basin Water Use
Temporal frameworkBase year 2010Multiple years as available
2005-2010 NJ and PA
Water-use transactionsWithdrawalsType of useReturn flows Interbasin transfersAquifer Storage and Recovery
Data Collection
Susan HutsonKristin LinseyRuss LudlowBetzaida ReyesJennifer Shourds
Delaware River Basin Water Use26,135 site-specific data records
single and multiple years 6,343 unique sites include 5 interbasin transfers
Areal estimates
Data Collection
Water Type Count PercentGroundwater 4,580 72
Surface water 1,001 16
Return flows 762 12
Livestock Irrigation Self-supplied Domestic
Total Water Use*7,000 Mgal/d
4,900 Mgal/d (70%) Thermoelectric Power Generation1,600 Mgal/d (23%) Public supply and Self-supplied domestic 290 Mgal/d (4%) Industrial, Commercial, and Mining 200 Mgal/d (3%) Irrigation, Livestock, and Aquaculture
Hydroelectric power is an “in stream" use and is not included in this calculation.*
92% Surface Water
8% Groundwater
Thermoelectric4,900 Mgal/d
>0 - 1010 - 100100 - 200200 - 300300 - 3100
0
Withdrawals,in Mgal/d
0%
100%
GW
SW
Fresh
Saline
40%
60%
Public Supply and Self-Supplied Domestic Withdrawals1,600 Mgal/d
Public supply withdrawals 1,500 Mgal/d
650 Mgal/d transferred out of basin
Self-supplied Domestic Withdrawals 120 Mgal/d
37%
63%
PS and DO Water Use
23%
77%
PS and DO Withdrawals
GWSW
Public SupplyPublic Supply Public Supply Public Supply Withdrawals Transfers Water Use
1 - 1010 - 100100 - 200200 - 300300 - 1000
0
Withdrawals,in Mgal/d
Determining Self-Supplied DomesticJack Monti and Jason Finkelstein
Domestic use data not collected by U.S Census since 1990. Developed current domestic use estimates from:• USGS National Water Use Information Program
• County use data every 5 years; 1985-2005• Estimates of total population served
• U.S. Census• Decadal data on population and housing units• Block groups and blocks were analyzed• 1990 census provided source of water information
per block group housing units
0 5000 10000 15000 200000
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Block GroupCut-off Limit100% Line95% Line
Population Density per Sq Mile
Pub
Supp
ly H
ouse
U
nits
%Pu
blic
Sup
ply
Hou
sing
Uni
ts (
perc
ent)
Statistical Determination of Domestic UseBuck County, PA Example
100 percent public supplyTop five % flip to public supply100 percent domestic self supply
Used population density 95th percent value to forecast/predict future years.
Example for Sussex County, Delaware
1990 Population of P.S. block groups (pink): 53,521
1990 Water-use Program P.S. population : 54,430
2000 Water-use Program P.S. population : 78,420
Predicted population for P.S. blocks in 2000 (light and dark purple): 83,819
Basin-Wide Decadal Predictions1990 2000 2010
Basin-Wide Results
Delaware River Basin Block Group Populations*
Year Total Public SupplyDomestic Self-
Supply Undetermined1990 7,590,442 6,313,877 1,276,565 2000 8,061,808 6,544,054 1,517,754 2010 8,579,716 6,929,628 1,649,175 913
*Population totals not fully apportioned to Delaware River Basin extent (Total includes parts of counties not fully in basin)
15%
85%
Industrial, Commercial,and Mining 290 Mgal/d Industrial
240 Mgal/d
Commercial 34 Mgal/d
Mining 18 Mgal/d 47%53%
23%
77%
GWSW 1 - 1010 - 100100 - 200200 - 300300 - 1031
0Withdrawals,in Mgal/d
Industrial,Commercial,& Mining
Agriculture200 Mgal/d*Irrigation 170 Mgal/d
Livestock 9.2 Mgal/d
Aquaculture 18 Mgal/d
56%44%
91%
9%
61%39%
GWSW 1 - 1010 - 100100 - 200200 - 300300 - 1031
0Withdrawals,in Mgal/d
Agriculture
* 60 percent of total was reported values
Rasterizing Estimated Livestock & Irrigation Data
Combined: 2010 USDA Crop Data Layer-CDL 2010 USGS county livestock or irrigation use dataAnd distributed by land use over county
Water Use Data Compilation & Dissemination
USGS SIR Report 2014 Web-portal data delivery
8-digit subbasin
data and methods
12-digit subbasin
data
426 subbasins
13 subbasins
Report out by end of calendar yearWeb tool available in 2015
Estimating Streamflow
Tool for predicting flow at ungaged basins based on correlation with historic flow at gaged sites – Marla Stuckey
Hydrologic model to evaluate how water stressors such as population growth, land-use change, and climate change affect the availability of water resources – Tanja Williamson
Both models are used in current evaluations and future predictions of ecological flow needs – Jonathan Kennen
WATER Hydrologic ModelWater Availability Tool for Environmental Resources (WATER) Used as a decision support tool to evaluate how water
stressors such as population growth, land-use change, and climate change affect the availability of water resources.
Model encompasses the whole non-tidal Delaware River Basin.
Validated using precipitation, water-use, streamflow, and other information for the time period 2001 to 2011.
Simulations of future streamflow and water-availability conditions centered on 2030 and 2060 will incorporate projected changes in water use, land use, and climate in the watershed.
Tanja N. Williamson, Jeremiah Lant, Elizabeth Nystrom, Scott Hoffman, and Hugh Nelson
WATER Hydrologic Modelbased on TOPMODEL
TOPography-based hydrological MODEL Developed by Beven and Kirkby, 1979 “Physically-based watershed model that
simulates the variable-source-area concept of streamflow generation.” (Wolock, 1993)
Three fundamental assumptions steady-state recharge to the groundwater hydraulic gradient of the water table ≈ the surface
slope transmissivity profile decreases exponentially
with depthBeven, K.J. and M.J. Kirkby. 1979. A physically based, variable contributing area model of basin hydrology. Hydrological Sciences Bulletin, v. 24, pp. 43-69. Wolock, David M. 1993. Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL. USGS WRI 93-4124.
Direct
Infiltration
Precipitation
EvaporationET
Sub-surface flowSaturatedAreas or
ImpermeableSurface
Wat
er B
udge
t
Over-land flow
Qout
TOPMODEL topographic wetness index
High values of TWI High potential for saturationLow values of TWI Low potential for saturation
Grid cells with the same TWI are hydrologically similar
Calculations need not be performed on every single grid cell.
slopeareangcontributiupslope
TWItan
ln
Soil CharacteristicsSSURGO Variables Calculated “m” Hydraulic conductivity (moderately
high or higher) Field Capacity Available Water Capacity Porosity Thickness
And…..
Scaling Parameter “m” computed from processed SSURGO data
m = readily drained soil porosity/rate of decrease with depth
Conductivity Multiplier
Scaling Parameter
mporosity field capacity
f
depthsoilmultipliertyconductivi
fln
Low-K High-K
sat
sat
WATER – A decision support tool
1-Ja
n11
-Jan
21-Ja
n31
-Jan
10-F
eb20
-Feb
2-M
ar12
-Mar
22-M
ar1-
Apr
11-A
pr21
-Apr
1-M
ay11
-May
21-M
ay31
-May
10-Ju
n20
-Jun
30-Ju
n05
101520253035404550 0
5101520253035404550
2003
Dis
char
ge (
mm
)Precipitation (m
m)
Precipitation Record or Forecast
Simulated Hydrograph
Changed climate Water availability
Validated Model
Current conditions
Current ConditionGaged Streams
Flow at ungaged sites
Land management and
water allocation decisions
Landscape Characterization
Scenarios Potential Uses
Landscape change
Resolution of Spatial Layers
Precipitation Record
WATER-TopModel
0
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
2.03
2.42
2.82
3.22
3.62
4.01
4.41
4.81
5.21
5.60
6.00
6.40
6.79
7.19
7.59
7.99
8.38
8.78
9.18
9.58
9.97
10.3
7
10.7
7
11.1
7
11.5
6
11.9
6
12.3
6
12.7
5
13.1
5
13.5
5
CTI
Frac
tion
of W
ater
shed Histogram
of TWI
Ksat
TWI
NLCD
Incorporate Water-Use Data
Seasonal Contribution to Annual Total
Withdrawals Returns/Discharges Transfers
426 basins
12.48 km2
to270.06 km2
Permit Number
P
erce
nt o
f 201
0 To
tal
Representative Values Long-term Median Seasonal
Data distributed over HUC 12 Basins. This will protect privacy information
Model Validation
Minimally impacted basins 1.5 to 675 km2 (0.6 to 261 mi2)
Comparison of streamflow estimates USGS streamflow data
Evaluate potential bias in water budget Snowpack PET
Sites will also be valuable for evaluating future land use change scenarios.
Reservoir Management System
Initial work focusing on basin areas upstream of reservoirs. Ultimately: WATER will export long-term
record of flow in OASIS format
Use OASIS for points downstream of reservoirs
Non-OASIS users will use lake delay
Snowpack Simulation – Upper BasinFl
ow
Sno
w
Simulation of EvapotranspirationPotential Evapotranspiration (PET) – Hamon (1963)
Simulated Actual Evapotranspiration (AET) – limited by soil-moisture availability
For Future Hydrologic Predictions WATER Model Needs Projections of Changes in:
Water Use
Climate
Land Use (subject of next talk)
Future: Global Circulation Models (GCM)
3736 basins10 km2
Coupled Model Intercomparison Project CMIP5GCMs Previously used in the basin
NCAR CCSM GFDL ESM2G, NOAA GISS-E2-H, NASA CGCM4-CanES
Change factor (delta) approach
Target time periods 2030 2060
Representative Concentration Pathways RCP4.5 RCP8.5
ModeledArea
GCMArea
6 – 10 Cells100 – 200 km2
RCP scenario conditions
At Conclusion of the Delaware Study Database of water withdrawal, use, and return flow
information for watersheds Tool to estimate daily streamflow from 1960 to 2010
for ungaged streams Hydrologic model of the non-tidal portions of the
watershed tributaries Flow and aquatic assemblage response relations for
tributaries An updated Decision Support System for sections of
the main-stem Delaware
Jeff Fischer [email protected] 609-771-3953