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    PresenterPresenter

    Eric WarmathEric Warmath,, NDOTNDOT

    Using Remote Sensing and GIS toUsing Remote Sensing and GIS toImprove Runoff IndexImprove Runoff Index

    Determination for UrbanDetermination for UrbanHydrologic ModelingHydrologic Modeling

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    AcknowledgmentsAcknowledgmentsuu South Dakota State Univ. Brookings, SDSouth Dakota State Univ. Brookings, SD

    Ms. Pravara ThanapuraMs. Pravara Thanapura, Principal Investigator, and Research, Principal Investigator, and ResearchAssociate, Engineering Resource Center (ERC), Ph.D.Associate, Engineering Resource Center (ERC), Ph.D. SStudent in thetudent in the

    Geospatial Science and Engineering Program, andGeospatial Science and Engineering Program, and oowner of GeoTechwner of GeoTechConsulting, LLC.Consulting, LLC.

    Dr. Dennis HelderDr. Dennis Helder,, Director of Engineering Research, DepartmentDirector of Engineering Research, DepartmentHead,Head, Department of Electrical Engineering and Computer ScienceDepartment of Electrical Engineering and Computer Science **

    Mr. Kevin DalstedMr. Kevin Dalsted, Director, ERC, Director, ERC

    Dr. Suzette BurckhardDr. Suzette Burckhard, Hydrologist, College of Engineering, Hydrologist, College of Engineering** Dr. Dwight GalsterDr. Dwight Galster, Statistician, Department of Mathematics, Statistician, Department of Mathematics**

    Ms. Mary OMs. Mary ONeillNeill, Program Manager, Office of Remote Sensing, ERC, Program Manager, Office of Remote Sensing, ERC**

    uu City of Sioux Falls, SDCity of Sioux Falls, SD Steve Van AartsenSteve Van AartsenSteve Van AartsenSteve Van AartsenSteve Van AartsenSteve Van AartsenSteve Van AartsenSteve Van Aartsen, GIS Supervisor,, GIS Supervisor, Thanks for all the dataThanks for all the data!! Jeff DunnJeff Dunn, City Drainage Engineer, for reviews and information, City Drainage Engineer, for reviews and information

    Sam TrebilcockSam Trebilcock, Transportation Planner, for input and information, Transportation Planner, for input and information

    * Denotes coDenotes co--authorauthor

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    TopicsTopicsuu Presentation ObjectivePresentation Objective

    uu

    Research Contributions & DOT End User BenefitsResearch Contributions & DOT End User Benefitsuu Hydrologic Model BackgroundHydrologic Model Background

    uu Runoff Methods & Runoff Index for Urban Drainage DesignRunoff Methods & Runoff Index for Urban Drainage Designand Analysisand Analysis

    uu Composite Runoff Index Geographic Model for IndustryComposite Runoff Index Geographic Model for IndustryStandard Runoff Index CalculationsStandard Runoff Index Calculations

    uu Mapping Impervious Area and Open SpaceMapping Impervious Area and Open Space

    uu

    GIS SpatialGIS Spatial ModelingModelinguu ResultsResults

    uu ConclusionConclusionss

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    Presentation ObjectivesPresentation Objectivesuu Show the potential value of the research, in urbanShow the potential value of the research, in urban

    areas, for hydrologic engineers at DOTareas, for hydrologic engineers at DOTs nationally.s nationally.

    uu Briefly describe the 2 most common runoff methodsBriefly describe the 2 most common runoff methods

    and associated Runoff Indexand associated Runoff Index

    uu

    Describe the research:Describe the research: Integration of remote sensingIntegration of remote sensingand GIS for determining industry standard values ofand GIS for determining industry standard values of

    NRCS CN & C using the composite runoff indexNRCS CN & C using the composite runoff index

    geographic model developed by Thanapura in 2005geographic model developed by Thanapura in 2005--6.6.

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    BenefitsBenefitsuu Lead to an improved scheme for determining theLead to an improved scheme for determining the

    standard runoff index used in urban watershed runoffstandard runoff index used in urban watershed runoff

    assessment methodsassessment methods -- the NRCS curve number andthe NRCS curve number andrational methods.rational methods.

    uu Demonstrate a more precise, simpler, and efficientDemonstrate a more precise, simpler, and efficientapproach of calculating runoff index.approach of calculating runoff index.

    uu Allow repeatability and consistency of the results byAllow repeatability and consistency of the results byremoving human error factors while increasing speedremoving human error factors while increasing speedand potentially reducing costs of analysis andand potentially reducing costs of analysis and

    mapping for both methods.mapping for both methods.uu Lead to an improved scheme of urban imperviousLead to an improved scheme of urban impervious

    surface detectionsurface detection a key indicator of the effects ofa key indicator of the effects ofnonnon--point source pollution runoff and of future waterpoint source pollution runoff and of future water

    and ecosystem quality.and ecosystem quality.

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    DOT End User BenefitsDOT End User Benefitsuu Beneficial to engineers involved drainage analyses andBeneficial to engineers involved drainage analyses and

    designs in urban areas.designs in urban areas.

    uu

    Allow for identification of structures nearing designAllow for identification of structures nearing designcapacity and needing replacement due to the effects ofcapacity and needing replacement due to the effects ofincreased urbanization on a drainage basin.increased urbanization on a drainage basin.

    u Identify sites for potential property damage or loss of life.

    Table. Minor Structure Design Frequencies (Viessman and Lewis, 2003).

    Return period, Tr Frequency = 1/Tr

    0-400 ADT* 10 yr 0.10

    400-1700 ADT 10-25 yr 0.10-0.04

    1700-5000 ADT 25 yr 0.04

    5000+ ADT 50 yr 0.02

    Airfields 5 yr 0.20

    Railroads 25-50 yr 0.04-0.02

    Storm drainage 2-10 yr 0.50-0.10

    Levees 2-50 yr 0.50-0.02

    Drainage ditches 5-50 yr 0.20-0.02* ADT = average daily traffic

    Type of minor structure

    Highway crossroad drainage*

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    Why NDOT & SDSU ?Why NDOT & SDSU ?uu One of the conference discussions at GISOne of the conference discussions at GIS--T 2004 inT 2004 in

    Rapid City, SD, was getting more use out of imageryRapid City, SD, was getting more use out of imagery

    and remote sensing at DOTand remote sensing at DOTs.s.uu I met the principal investigator, was impressed withI met the principal investigator, was impressed with

    the research, and saw the potential benefits for NDOT.the research, and saw the potential benefits for NDOT.

    uu Since Nevada is the fastest growing state and urbanSince Nevada is the fastest growing state and urbandrainage problems sometimes occur, the research isdrainage problems sometimes occur, the research isvery relevant to NDOT issues .very relevant to NDOT issues .

    uu

    We have tentative plans to work in the Las Vegas areaWe have tentative plans to work in the Las Vegas areathis year as part of the study.this year as part of the study.

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    Hydrologic Models BackgroundHydrologic Models Backgrounduu There are 2 main hydrologic modeling methods used by theThere are 2 main hydrologic modeling methods used by the

    majority of practicing engineers. These models weremajority of practicing engineers. These models were

    developed for storm water calculation in engineering stormdeveloped for storm water calculation in engineering stormdrainage design and water resource planning and analysis.drainage design and water resource planning and analysis.

    1.1. Natural Resource Conservation Service (NRCS), NRCSNatural Resource Conservation Service (NRCS), NRCS--CNCN

    Method.Method.

    2.2. The Rational Method.The Rational Method.

    uu According to an EPA studyAccording to an EPA study ~86%~86%of private engineeringof private engineering

    firms, water boards, and other government entities arefirms, water boards, and other government entities areusing one or both methods in their hydraulic engineering.using one or both methods in their hydraulic engineering.

    uu NDOT and the City of Sioux Falls, SD use both.NDOT and the City of Sioux Falls, SD use both.

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    Runoff Curve Number MethodRunoff Curve Number Method

    uu The NRCS Runoff Curve Number (NRCSThe NRCS Runoff Curve Number (NRCS--CN)CN)

    method:method:

    Used to estimate runoff from storm rainfall.Used to estimate runoff from storm rainfall.

    Well established in hydrologic engineering andWell established in hydrologic engineering and

    environmental impact analysis.environmental impact analysis.

    Widely used by practicing engineers andWidely used by practicing engineers and

    hydrologists nationally and internationally.hydrologists nationally and internationally.

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    Curve Number (CN)Curve Number (CN)

    Industry Standard TableIndustry Standard Tableuu CN is an runoffCN is an runoff

    index described inindex described in

    detail in the TRdetail in the TR--5555(NRCS 1986).(NRCS 1986).

    uu CN is a function of 3CN is a function of 3

    factors:factors:

    Hydrologic soilHydrologic soil

    groupgroup

    Cover complexCover complex

    (Land Cover /(Land Cover /Land Use)Land Use)

    Antecedent soilAntecedent soil

    moisturemoisture

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    Curve Number (CN)Curve Number (CN)uu Proposed runoff coefficients for the compositeProposed runoff coefficients for the composite

    runoff calculationrunoff calculation for urban land usefor urban land use

    recommended by McCuen in 2005recommended by McCuen in 2005

    (Thanapura, 2006).(Thanapura, 2006).

    Land Cover

    Character of Surface1: A B C D

    Impervious Areas 98 98 98 98

    Open Spaces - Good Condition 39 61 74 80

    Curve Number (CN) for

    SCS Hydrologic Soil Group

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    Rational MethodRational Method Developed by Mulvaney in 1851 and refinedDeveloped by Mulvaney in 1851 and refined

    by Kuichling and others in the late 19by Kuichling and others in the late 19ththccentury.entury.

    Is the preferred method for use in smallerIs the preferred method for use in smaller

    drainage basinsdrainage basins (

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    Runoff Coefficients (C)Runoff Coefficients (C)

    Industry Standard TableIndustry Standard Table

    uu C is a function of 3C is a function of 3factors:factors:

    Land coverLand cover(Impervious and(Impervious and

    Open space)Open space) Hydrologic SoilHydrologic Soil

    GroupGroup

    SlopeSlope

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    Runoff Coefficient (C)Runoff Coefficient (C)

    uu ProposedProposed rrunoffunoff ccoefficients for theoefficients for the ccompositeomposite rrunoffunoff

    ccalculation defined from thealculation defined from the rrunoffunoff ccoefficient, Coefficient, C

    rrecommended by the American Society of Civilecommended by the American Society of Civil

    Engineers (ASCE), the Water Pollution ControlEngineers (ASCE), the Water Pollution Control

    Federation (WPCF) in 1969, and McCuen in 2005Federation (WPCF) in 1969, and McCuen in 2005(Thanapura, 2006).(Thanapura, 2006).

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    Research ObjectiveResearch Objective

    The objective of this study was to demonstrateThe objective of this study was to demonstrate

    and evaluate Normalized Differenceand evaluate Normalized DifferenceVegetation Index (NDVI) data derived fromVegetation Index (NDVI) data derived from

    QuickBird (QB) high resolution satelliteQuickBird (QB) high resolution satellite

    imagery to mapimagery to map land coverland cover surfacesurface

    characteristics such as impervious area andcharacteristics such as impervious area and

    open space for runoff index numberopen space for runoff index numberdetermination in urban watersheds.determination in urban watersheds.

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    Study MethodStudy MethodComposite Runoff Index Spatial Model

    Digital Data & Pre-ProcessingData Merging and Integration

    QuickBird NDVI Imagery & GIS LayersDecision and Classification

    Image ClassificationUnsupervised ISODATA Algorithm & QuickBird NDVI

    Classification Output

    Accuracy AssessmentReference Data Ortho Photo

    Reports and GIS Data

    GIS Spatial ModelingThe Composite of Runoff Index CN & C calculations and comparisons

    Reject / Accept Hypothesis

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    Composite Runoff IndexComposite Runoff Index

    Geographic ModelGeographic Model

    In this study, the composite runoff index geographic model was applied todevelop a GIS spatial model for the composite runoff index calculation of boththe NRCS CN and C for the NRCS CN method and the rational method.

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    Study AreaStudy Area

    The QB multi spectral image (4-3-2)The QB NDVI Image

    (Band 4 Band 3 / Band 4 + Band 3)

    This is ~2900 acres in the southwest portion of the City of Sioux Falls, SDrepresenting almost all potential land use types.

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    Digital DataDigital Datauu QuickBirdQuickBird

    uu ~8 ft (~2.4 m) [April 26, 2004]~8 ft (~2.4 m) [April 26, 2004]

    uu Blue, Green, Red, and NIR bandsBlue, Green, Red, and NIR bands

    uu OrthophotosOrthophotos

    uu 2 ft color (0.6 m)[April 23, 2004]2 ft color (0.6 m)[April 23, 2004]

    uu 0.5 ft color (0.15 m)[May 20, 2002]0.5 ft color (0.15 m)[May 20, 2002]

    uu QB NDVI (band4QB NDVI (band4--band3/band4+band3)band3/band4+band3)

    (created using Erdas Imagine 8.7)(created using Erdas Imagine 8.7)

    uu GIS LayersGIS Layers

    Parcel, hydro, and street layers.Parcel, hydro, and street layers.

    NRCS SSURGO (1:24K) soil dataNRCS SSURGO (1:24K) soil data

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    PrePre--ProcessingProcessing

    QB RegistrationQB Registration (2.39m/ 8ft)(2.39m/ 8ft)A Root Mean Square of 0.42m/1.38ft (0.69pixel)A Root Mean Square of 0.42m/1.38ft (0.69pixel)

    The QuickBird multi image (4-3-2)on the left with the 2004 Ortho-

    image (1-2-3) on the right.

    The QuickBird NDVI image on the leftwith the 2004 Ortho-image (1-2-3)

    on the right.

    The registered 2004 images displayed at same scale and location.

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    Classification ApproachClassification Approach

    Why High Resolution NDVI?Why High Resolution NDVI?uu Reduce heterogeneous spectralReduce heterogeneous spectral--radiometricradiometric

    characteristics within land use land covercharacteristics within land use land coversurfaces in the QB image.surfaces in the QB image.

    uu

    Normalize potential atmospheric effects withinNormalize potential atmospheric effects within

    the image.the image.

    uu Improve accuracy of mapping imperviousImprove accuracy of mapping impervious

    surface and open space as used in thesurface and open space as used in theproposed runoff index calculation.proposed runoff index calculation.

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    Classification ApproachClassification ApproachWhy Unsupervised Classification?Why Unsupervised Classification?

    uu To maximize control over the menu ofTo maximize control over the menu of

    informational classes.informational classes.uu Minimize human involvement and error whileMinimize human involvement and error while

    expediting the process.expediting the process.

    uu To maximize correlation between spectralTo maximize correlation between spectral

    homogeneous classes and the informationalhomogeneous classes and the informational

    categories (i.e., impervious area and opencategories (i.e., impervious area and openspace).space).

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    Classification ApproachClassification Approach

    QB multi spectral image (4-3-2) QB NDVI Image

    Orthophoto (1-2-3)

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    Sample DesignSample Design

    Random Sampling MethodRandom Sampling Methoduu The conservative sample size equation is expressedThe conservative sample size equation is expressed

    as follows (Congalton and Green, 1999):as follows (Congalton and Green, 1999):

    n = B/ 4bn = B/ 4b22

    Where: n =Where: n = the total samples of all classesthe total samples of all classes

    B = the upper (B = the upper (/k) x 100th percentile of the Chi/k) x 100th percentile of the Chi--

    squared distribution with 1 degree of freedom (squared distribution with 1 degree of freedom ())k = number of classesk = number of classes

    b = Significance level =b = Significance level = +/+/-- 5%5% accuracyaccuracy

    uu

    To ensure unbiased sample selection.To ensure unbiased sample selection.uu To provide a statistically sound assessment ofTo provide a statistically sound assessment of

    accuracy.accuracy.uu Over 500 points were used.Over 500 points were used.

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    Classification SchemeClassification Scheme

    Labels Rules

    Land Use / Land CoverCharacter of Surface:

    Impervious Areas If land area has < 25% covered with areas characterized by

    vegetative open spaces then Impervious Area (1)

    If land area > or = 75% characterized by impervious surfaces(e.g., asphalt, concrete, and buildings.) then Impervious Area (1)

    If land area > or = 75% covered by bare land (e.g., bare rock,

    gravel, silt, clay, dirt, and sand or any other earthen materials.)then Impervious Area (1)

    Open Spaces Else if land area < 25% covered with areas characterized by impervious surfacesthen Open Space (2)

    If land area > 75% covered with vegetation naturally existing or planted

    (e.g., grass, plants, trees (leaf-on /leaf-off), forest, shrub, and scrub.)then Open Space (2)

    Else Impervious Area (1)

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    Accuracy AssessmentAccuracy Assessment

    Map C ass Name

    ID

    11 Impervious area 1-40 1270.98 43.72 258 216 210 81.40 97.22 0.9429

    Open space 41-100 1635.81 56.28 244 286 238 97.54 83.22 0.6734

    12 Impervious area 1-45 1392.27 47.90 258 241 229 88.76 95.02 0.8976Open space 46-100 1514.53 52.10 244 261 232 95.08 88.89 0.7838

    13 Impervious area 1-50 1526.54 52.52 258 261 247 95.74 94.64 0.8896

    Open space 51-100 1380.25 47.48 244 241 230 94.26 95.44 0.9112

    14 Impervious area 1-55 1677.57 57.71 258 285 250 96.90 87.72 0.7473

    Open space 56-100 1229.22 42.29 244 217 209 85.66 96.31 0.9283

    15 Impervious area 1-60 1842.09 63.37 258 306 251 97.29 82.03 0.6302

    Open space 61-100 1064.70 36.63 244 196 189 77.46 96.43 0.9305

    Overall Classification Accuracy = 87.65 % Overall Kappa Statistics = 0.7515

    Overall Classification Accuracy = 95.02 % Overall Kappa Statistics = 0.9003

    Overall Classification Accuracy = 91.43 % Overall Kappa Statistics = 0.828

    Overall Classification Accuracy = 89.24 % Overall Kappa Statistics = 0.7857

    Overall Classification Accuracy = 91.83 % Overall Kappa Statistics = 0.8368

    Accuracy Assessment - Unsupervised Thematic Map#1(100 spectral clusters)Labeling

    Criteria*

    Areas

    (Acres)Areas (%)

    Reference

    Totals

    Classified

    Totals

    Number

    Correct

    Producers

    Accuracy

    Users

    Accuracy

    Kappa

    Statistics

    > Comparing the maps generated using five different labeling criteriashowed slight differences in overall accuracy results, with accuracy

    improvement increasing toward the mid DNs of the unsupervisedQB NDVI. No major difference was found between 8 and 16 bit imagery.

    > This pattern of change in classification accuracy showed thepotential correlations between increasing and decreasing of the DN

    values and amounts of open space and impervious area.

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    Accuracy AssessmentAccuracy Assessment

    QB NDVI Thematic MapQB NDVI Thematic Map

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    Geographic ModelingGeographic Modelinguu ArcView 3.3 geoprocessing was used to generateArcView 3.3 geoprocessing was used to generate

    new polygons showing the relationship betweennew polygons showing the relationship between

    impervious area, open space, hydrologic soil groups,impervious area, open space, hydrologic soil groups,and slopeand slope with the index valuewith the index valuess (NRCS CN or C).(NRCS CN or C).

    uu The composite runoff index spatial model was usedThe composite runoff index spatial model was used

    to develop spatial modeling for the runoff indexto develop spatial modeling for the runoff indexcalculation in the study area.calculation in the study area.

    uu The results were compared toThe results were compared to industry standardindustry standard

    values of NRCS CN and Cvalues of NRCS CN and C in order to validate thein order to validate theutility of the QB NDVI image.utility of the QB NDVI image.

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    CN Results and ComparisonCN Results and Comparison

    ReferenceThe City of Sioux Falls s Standard CN:The City of Sioux Falls, 2005. The Citys design standards, Chapter 11. Drainage improvements, Sioux Falls,South Dakota. Available athttp://www.siouxfalls.org/upload/documents/publicworks/designstandards/ch11.pdf .

    Keyword: U30011. Accessed onFebruary 3, 2006.

    Table. The Runoff Curve Number (CN) Results and Comparisons.

    GIS GIS Vector Layer Descriptions Industry Standard Values of NRCS CN

    ID Activity Code and Description CN (avg.) Impervious (%) (McCuen, 2005)

    Hydrologic Soil Group B 5 10 100 Impervious (%)

    1 11 Single family - Residential 1/8 acre (0.13 acres or 506 sq.m) 80 50 85 45 50 70 40

    2 11 Single family - Residential 1/4 acre (0.25 acres 1012 sq.m) 76 41 75 45 50 70 40

    3 11 Single family - Residential 1/3 acre (0.33 acres 1348 sq.m) 74 35 72 45 50 70 40

    4 11 Single family - Residential 1/2 acre (0.5 acres 2023 sq.m) 74 34 70 45 50 70 40

    5 11 Single family - Residential 1 acre (4047 sq.m) 68 29 68 40 45 65 30

    6 11 Single family - Residential 2 acres (8094 sq.m) 76 31 65 40 45 65 30

    7 31 Banks and Financial Institutions 92 82 92 88 90 93 95

    8 33 Other offices 90 73 92 88 90 93 95

    9 64 Warehousing, Distribution, and Wholesale 76 81 88 80 80 85 80

    Total (avg.) 78 51 79 57.33 61.11 75.67 54.44

    by StormFrequency, Years and Impervious Areas (%)

    The Standard CN of Sioux Falls in 2005GIS Model CN Results

    CN results compared to published values: NRCS/McCuen and City of Sioux Falls

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    C Results and ComparisonC Results and Comparison

    C results compared to the industry standard published values of C

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    ConclusionsConclusionsuu The composite runoff index geographic model (Thanapura 2005/6)The composite runoff index geographic model (Thanapura 2005/6)

    demonstrated that mapping techniques using high spatial resolutidemonstrated that mapping techniques using high spatial resolution satelliteon satelliteimagery, and GIS spatial modeling were successful in determiningimagery, and GIS spatial modeling were successful in determining a morea moreprecise, spatially representative runoff index (CN or C) in urbaprecise, spatially representative runoff index (CN or C) in urban watersheds.n watersheds.

    uu Mapping impervious area and open space, using QuickBird NDVI satMapping impervious area and open space, using QuickBird NDVI satelliteelliteimagery generated with traditional unsupervised classification uimagery generated with traditional unsupervised classification using thesing theISODATA algorithm, is a more precise, simpler, consistent, and eISODATA algorithm, is a more precise, simpler, consistent, and efficient datafficient dataextraction approach. This is reflected in the fact that overallextraction approach. This is reflected in the fact that overall accuracy for theaccuracy for theQB NDVI thematic map produced wasQB NDVI thematic map produced was 9595%.%.

    uu The finer resolution image and the mapping approach used in thisThe finer resolution image and the mapping approach used in this studystudyallowed for better discrimination in land cover/land use and morallowed for better discrimination in land cover/land use and more accuratee accuratespatially representative runoff index estimation compare to prevspatially representative runoff index estimation compare to previous studiesious studiesthat utilized medium resolution remotely sensed data ( Bondelidthat utilized medium resolution remotely sensed data ( Bondelid et al., 1981;et al., 1981;Singh, 1982; Slonecker et al., 2001).Singh, 1982; Slonecker et al., 2001).

    uu Previous studies using medium resolution data demonstrated a sigPrevious studies using medium resolution data demonstrated a significantnificanttime savings in the ability to produce land cover but with accurtime savings in the ability to produce land cover but with accuracies only inacies only inthethe 7070--8080% range. That was not sufficient for urban areas.% range. That was not sufficient for urban areas.

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