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Transcript of KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2...
![Page 1: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/1.jpg)
KINEROS2and the AGWA
Modeling Framework
Darius J Semmens1, David C Goodrich2, Carl L Unkrich2,Roger E Smith3, David A Woolhiser3, and Scott N Miller4
1U.S. EPA Office of Research and Development, Las Vegas2USDA-ARS Southwest Watershed Research Center, Tucson, AZ
3USDA-ARS – Retired, Fort Collins, CO4Univ. of Wyoming, Department of Renewable Resources, Laramie
![Page 2: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/2.jpg)
Outline
• Background• Overview• Conceptual Model• Numerical Model• Sensitivity• AGWA GIS Interface• Conclusions
![Page 3: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/3.jpg)
Background • 1960’s - KINGEN• 1990 - KINEROS• 2002 – KINEROS2 • 2002 - AGWA – Coupling with
ArcView GIS• Still event based, but developing
continuous simulation w/ assimilated RS soil moisture
![Page 4: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/4.jpg)
Overview • Physically based• Event model (continuous coming)
• Time step = minutes• 1-D overland and channel flow • Erosion and sediment transport• Dynamic infiltration• Distributed rainfall• Flexible, distributed model elements• GIS interface – AGWA
![Page 5: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/5.jpg)
K2 Conceptual Model
• Overland flow• Urban overland• Channels • Detention structures (ponds)• Injection• Culverts
Model Elements:
![Page 6: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/6.jpg)
Conceptual Model - Structure• Watershed approximated by cascade of overland-flow
planes, channels, impoundments
![Page 7: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/7.jpg)
Conceptual Model – Overland Flow• Overland-flow planes can be split into multiple
components with different slopes, roughness, etc.• Adjacent planes need not have the same width
R a in fa l l
O ve rland F low
In f i l t ra t io nChannel Flow
Infiltration in Channe
![Page 8: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/8.jpg)
Conceptual Model – Overland Flow• Small scale spatial variability of infiltration
represented in distribution sense and parameterized for numerical efficiency
• Microtopography can be represented
![Page 9: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/9.jpg)
Conceptual Model – Urban Element• Urban element – various runoff – runon
combinations
![Page 10: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/10.jpg)
Conceptual Model - Infiltration• Dynamic infiltration in K2 - interacts with both rainfall
and runoff
![Page 11: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/11.jpg)
Conceptual Model - Infiltration• Infiltration with two-layer soil profile • Soil moisture re-distribution during storm hiatus
![Page 12: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/12.jpg)
Conceptual Model - Sediment• Multiple particle class size sediment routing (non-
interactive) • Entrainment by raindrop impact and hydraulic shear
![Page 13: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/13.jpg)
Conceptual Model - Channels• Compound channel routing with distinct main and
overbank channel infiltration
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Ephemeral StreamflowEvent of Aug. 27, 1982
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Conceptual Model - Culverts• Assumed to maintain free surface flow conditions at
all times
• No lateral inflow• Uses Darcy-Weisbach formula with kinematic
assumption so that
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Numerical Model• Rainfall
– Uniform or distributed
– Time, depth/intensity
– Linear interpolation
– Uniform on individual elements
– Radar (AGWA)
• Interception– Rainfall rate is reduced by the cover fraction until the
amount retained reaches a specified interception depth.
![Page 17: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/17.jpg)
Numerical Model - Infiltration• Infiltrability
– Parlange 3-Parameter model
– Green and Ampt (1911) and Smith and Parlange (1978) are included as the two limiting cases
– 3rd parameter, gamma, set to 0.85
– Infilitrability depth approximation – describes fc as a function of infiltrated depth, I, - eliminates the separate description of ponding time and the decay of f afterponding
f KI
G
c s
i
= +
−
11
γγexp∆θ
![Page 18: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/18.jpg)
Numerical Model - Infiltration• Infiltration
– Small scale spatial variability accommodated by introducing a coefficient of variability in Ks, CVK
– Assumes that KS is distributed log-normally
– Closely describes ensemble infiltration behavior
– f e * and r e * are infiltrability and rain rate scaled on the ensemble effective asymptotic KS value.
– Has the effect of creating a gradual evolution of runoff rather than it commencing at the time of ponding
( ) ( )f rr
e re ee I
c c
ee
* **
/
*( ) ,*= + − +−
−
>
−
1 1 11
1 1
1
γγ
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Numerical Model – Overland Flow
• One-dimensional flow process in which a simple power relation relates flux to the unit-area storage
• Used in conjunction with the equation of continuity:
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Numerical Model – Overland Flow• Boundary conditions
– Flow = 0 if upper boundary is a flow divide
– Equivalence of discharge between the upstream and downstream elements otherwise
• Roughness relationships– Manning
– Chezy
![Page 21: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/21.jpg)
Numerical Model – Channel Flow• Kinematic approximation again
• Continuity equation for a channel with lateral inflow is
• Compound channels– Flows routed separately
– Explicit assumption of no energy transfer
– Implicit assumption of uniform water-surface elevation
![Page 22: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/22.jpg)
Numerical Model – Channel Flow• Base flow – user-specified constant base flow
added at a fractional rate at each computational node along the channel
• Channel infiltration – Optional
– At low flow an empirical expression is used to estimate an "effective wetted perimeter" for use in infiltration calculations, until a threshold depth reached
![Page 23: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/23.jpg)
Numerical Model – Sediment• Optional rain-splash and hydraulic erosion
computed for computed for upland, channel, and pond elements
• General mass-balance equation
• Net erosion, e, is a sum of splash-erosion rate ases and hydraulic-erosion rate as eh,
• Splash erosion computed by Meyer and Wischmeier (1969) only when flow > 0
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Numerical Model – Sediment• Hydraulic erosion/deposition modeled as a kinetic-
transfer process
• Transport capacity, Cm, computed by modified version of Engelund and Hansen (1967)
• Transfer-rate coefficient, cg, – Deposition – set by particle settling velocity (Fair and
Geyer, 1954) divided by the hydraulic depth, h
– Erosion – limited for cohesive soils by vs/h
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Numerical Solution
• Four-point implicit finite difference method
• Solutions obtained by Newton's method (Newton-Raphson technique)
• Unconditionally stable, but accuracy for routing is highly dependent on the size of x and t values used– New version will set x and t for optimal solution
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K2 SENSITIVITY • Relative ranking of most sensitive
inputs and parameters
– Rainfall Inputs (particularly in arid and semi-arid areas)
– Saturated Hydraulic Conductivity– Hydraulic Roughness
• All a function of watershed geometric complexity
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CSA: 2.5% (6.9 km2)44 watershed elements29 channel elements
CSA: 20% (55 km2)8 watershed elements5 channel elements
CSA: 5% (13.8 km2)23 watershed elements15 channel elements
CSA: 10% (27.5 km2)11 watershed elements7 channel elements
0 5 10 km
N
the influence of CSA on watershed complexitySensitivity to Geometric Complexity
![Page 28: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/28.jpg)
Darius Semmens, Bill KepnerDarius Semmens, Bill KepnerUS US –– EPA EPA
Landscape Ecology BranchLandscape Ecology BranchLas Vegas, NVLas Vegas, NV
David Goodrich, Mariano Hernandez, David Goodrich, Mariano Hernandez, Ian Burns, Averill Ian Burns, Averill CateCate, , Soren Soren ScottScott
USDA USDA –– Agricultural Research ServiceAgricultural Research ServiceSouthwest Watershed Research CenterSouthwest Watershed Research Center
Tucson, AZTucson, AZ
GISGIS--BASED HYDROLOGIC MODELING:BASED HYDROLOGIC MODELING:THE AUTOMATED GEOSPATIAL THE AUTOMATED GEOSPATIAL
WATERSHED ASSESSMENT TOOLWATERSHED ASSESSMENT TOOL
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Project Background & Acknowledgements• Long-Term Research Project
– Landscape Ecology Branch – 6 years
• Interdisciplinary– Watershed management– Landscape ecology– Atmospheric modeling– Remote sensing– GIS
• Multi-Agency– USDA – ARS– US – EPA– University of Arizona– University of Wyoming– USGS
• Student Support– 2 Post-Doc– 2 PhD– 2 Masters
USDA-ARSDavid GoodrichMariano HernandezAverill CateIan BurnsCasey TifftSoren Scott
US-EPABill KepnerDarius SemmensDan HeggemBruce JonesDon Ebert
University of ArizonaPhil Guertin
University of WyomingScott Miller
![Page 30: KINEROS2 - University of Arizonaweb.sahra.arizona.edu/unesco/shortcourses/Semmens_Darius.pdfKINEROS2 and the AGWA ... • Uses Darcy-Weisbach formula with kinematic assumption so that.](https://reader031.fdocuments.us/reader031/viewer/2022030510/5ab9a2637f8b9ac10d8e7e41/html5/thumbnails/30.jpg)
• PC-based GIS tool for watershed modeling– KINEROS & SWAT (modular)
• Investigate the impacts of land-use/cover change on runoff, erosion, and water quality at multiple scales
• Compare and visualize results• Targeted for use by research
scientists and management specialists
• Analyses can be integrated with those from other GIS-based tools & data
• Widely applicable
Automated Geospatial Watershed Assessment (AGWA) Tool
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• Used with US-EPA Analytical Tool Interface for Landscape Assessment (ATtILA)
• Simple, direct method for model parameterization
• Provide accurate, repeatable results
• Require basic, attainable GIS data– DEM– Soil data (FAO soil map)– Land-use/cover data (easily adapted to local data)
• Useful for scenario development, alternative futures simulation work.
Objectives of the AGWA tool
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(SWAT)• Daily time step• Distributed: empirical and physically-based model• Hydrology, sediment, nutrient, and pesticide yields• Larger watersheds (> 1,000 km2)• Similar effort used by BASINS
71
7373
Soil and Water Assessment Tool
7173
pseudo-channel 71
channel 73
Abstract Routing Representation
to next channel
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Watershed Discretization(model elements) ++
LandCover
Soils
Rain (Observed or
Design Storm)
Results
Run model and import results
Intersect model elements with
Watershed Delineation using Digital Elevation
Model (DEM)
Sediment yield (t/ha)Sediment discharge (kg/s)
Water yield (mm)Channel Scour (mm)
Transmission loss (mm)Peak flow (m3/s or mm/hr)
Channel Disch. (m3/day)Sediment yield (kg)
Percolation (mm)Runoff (mm or m3)
ET (mm)Plane Infiltration (mm)
Precipitation (mm)Channel Infiltration (m3/km)
SWAT OutputsKINEROS Outputs
AGWA Conceptual Design: Inputs and Outputs
Output results that can be displayed in AGWA
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AGWA ArcView Interface
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PROCESS
runoff, sediment hydrographtime
runo
ff
STATSGONALC, MRLCUSGS 7.5' DEM
Conceptual Design of AGWA
Build Model Input Files
Derive Secondary Parameterslook-up tables
Characterize Model Elementsf (land cover, topography, soils)
Discretize Watershedf (topography)
View Model Resultslink model to GIS
Build GIS Database
PRODUCTS
ContributingSource Area
Gravelly loam SoilKs = 9.8 mm/hrG = 127 mmPor. = 0.453
inte
nsity
time
10-year, 30-minute event
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Texture Ksat Suction Porosity Smax CV Sand Silt Clay Dist KffClay 0.6 407.0 0.475 0.81 0.50 27 23 50 0.16 0.34Fractured Bedrock 0.6 407.0 0.475 0.81 0.50 27 23 50 0.16 0.05Clay Loam 2.3 259.0 0.464 0.84 0.94 32 34 34 0.24 0.39Sandy Clay Loam 4.3 263.0 0.398 0.83 0.60 59 11 30 0.40 0.36Silt 6.8 203.0 0.501 0.97 0.50 23 61 16 0.23 0.49Loam 13.0 108.0 0.463 0.94 0.40 42 39 19 0.25 0.42Sandy Loam 26.0 127.0 0.453 0.91 1.90 65 23 12 0.38 0.32Gravel 210.0 46.0 0.437 0.95 0.69 27 23 50 0.16 0.15
KINEROS2 Parameter EstimationParameters based on soil texture (STATSGO, SSURGO, FAO)
Parameters based on land-cover classification (e.g. NLCD)
Land Cover Type Interception (mm/hr) Canopy (%) Manning's nForest 1.15 30 0.070Oak Woodland 1.15 20 0.040Mesquite Woodland 1.15 20 0.040Grassland 2.0 25 0.050Desertscrub 3.0 10 0.055Riparian 1.15 70 0.060Agriculture 0.75 50 0.040Urba n 0.0 0.0 0.010
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AZ061
Component 1
20%
Component 2
45% Component 3
35%
9 inches
Layer 1
Layer 2
Layer 3
2
2
5
Layers for component 3
Components for MUID AZ061
Intersection of model element with soils map
AGWA Soil Weighting (KINEROS2)• Area and depth weighting of soil parameters
• Area weighting of averaged MUID values for each watershed element
AZ076
AZ067
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Parameter Manipulation (optional)
Ksat
Can manually change parameters for each channel and plane element
Stream channel attributes
Upland plane attributes Ksat
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Automated tracking of simulation inputs
Calculate and view differences between
model runs
Multiple simulation runs for a given watershed
Color-ramping of results for each element to show spatial variability
Visualization of Results
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Spatial and Temporal Scaling of Results
High urban growth1973-1997
Upper San PedroRiver Basin
#
#
ARIZONA
SONORA
Phoenix
Tucson
<<WY >>WY
Water yield change between 1973 and 1997
SWAT Results
Sierra Vista Subwatershed
KINEROS Results
N
ForestOak WoodlandMesquite DesertscrubGrasslandUrban1997 Land Cover
Concentrated urbanization
Using SWAT and KINEROS for integrated watershed assessmentLand cover change analysis and impact on hydrologic response
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Urbanization Effects (KINEROS2)
Pre-urbanization
1973 Land cover
Post-urbanization
1997 Land cover
• Results from pre- and post-urbanization simulations using the 10-year, 1-hour design storm event
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0 4 8 12 16 200
4
8
12
16
20
1:1 line
observed runoff depth (mm)
sim
ulat
ed ru
noff
dept
h (m
m)
KINEROS - Simulated runoff depth(distributed and uniform rainfall)
Rainfall Input
uniform PPT
distributed PPT
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Land-Cover Modification ToolAllows users to build management scenariosLocation of land-cover alterations specified by either drawing a polygon on
the display, or specifying a polygon map
Types of Land-Cover Changes:• Change entire user-defined area to new land cover • Change one land-cover type to another in user-defined area • Change land-cover type within user-supplied polygon map • Create a random land-cover pattern
• e.g. to simulate burn pattern, change to 64% barren, 31% desert scrub, and 5% mesquite woodland
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Alternative Futures: Base-Change Scenarios1. CONSTRAINED – Assumes population increase less than 2020 forecast
(78,500). Development in existing areas, e.g. 90% urban.
2. PLANS – Assumes population increase as forecast for 2020 (95,000). Development in mostly existing areas, e.g. 80% urban and 15% suburban.
3. OPEN – Assumes population increase more than 2020 forecast (111,500).Most constraints on land development removed. Development occurs mostly into rural areas (60%) and less in existing urban areas (15%).
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Percent Change in Runoff under Future Scenarios
• Relative change for each scenario can be mapped for each model output
• Highlights spatial variability in response to different scenarios
• One component of planning efforts
(Derived from using future land covers
and AGWA)
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Plans
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Limitations of GIS - Model Linkage• Model Parameters are based on look-up tables
- need for local calibration for accuracy- FIELD WORK!
• Subdivision of the watershed is based on topography- prefer it be based on intersection of soil, lc, topography
• No sub-pixel variability in source (GIS) data- condition, temporal (seasonal, annual) variability- MRLC created over multi-year data capture
• No model-element variability in model input- averaging due to upscaling
Most useful for relative assessment unless calibrated
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AGWA Support & Distribution• Fact Sheets, Product Announcement, Brochures• Documentation and User Manual• Quality Assurance Report
Research PlanCode Structure (Avenue Scripts, Dialogs, System Calls)EPA and USDA/ARS companion WebsitesJournal Publications (Hernandez et al. 2000, Miller et al. 2002a, Miller et al. 2002b, Kepner et al., 2004)Training: Las Vegas (2001); Reston (2002); Tucson (2003); San Diego (2004)
• AGWA Web Siteshttp://www.epa.gov/nerlesd1/land-sci/agwa/index.htmhttp://www.tucson.ars.ag.gov/agwa
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CONCLUSIONS• KINEROS2 – Evolved from a research model to
one gaining wider applicability
• Physically based, distributed, event model
• Most sensitive to rainfall input and Ks, but model geometric complexity also significant
• GIS interface, AGWA, is key to developing complex spatial organization and parameter inputs
• AGWA facilitates calibration, change analyses, and planning work through scenario development