a)(ft G
YDROLOGIC
MODELING
• INTRODUCTION
• HISTORY
• RECENT ADVANCES
• FUTURE OUTLOOK
INTRODUCTION
• DEFINITION OF HYDROLOGY
- What happens to the ram?
Occurrence, Movement, Distribution, and
Storage of Water Quantity and Quality
- Spatial, Temporal, and Frequency Domains
(or Characteristics)
- Quality of Water-Physical, Chemical and
Biological
- Spatial Scale-Watershed, Regional (Basin),
Continental, and Global
- Dynamic Interaction between Atmosphere,
Pedosphere, Lithosphere, and Hydrosphere-
Controlling Influences on Hydrology
APLICATION OF
HYDROLOGIC MODELS
• PLANNING, DESIGN,
DEVELOPMENT, OPERATION, AND
MANAGEMENT OF WATER
RESOURCES PROJECTS
• WATERSHED MANAGEMENT
• ENVIRONMENTAL PROTECTION
AND MANAGEMENT
• CLIMATE CHANGE
APPLICATION OF
HYDROLOGIC MODELS
0
SPECIFIC EXAMPLES
- Flood Protection Projects, Flood Warning
Systems, Reservoir Release Planning, Flood
Plain Management, etc.
Rehabilitation of Aging Dams
Water Supply Forecasting
- Irrigation Water Management
- Wetland Restoration
- Stream Restoration
- Water Table Management
- Drainage Systems Design
- Soil Conservation Practices
- Habitat Modeling
- Hydropower Development
- Consumptive Use and Water Allocation
HISTORICAL
PERSPECTIVE
0
THE BEGINNING YEARS:
DEVELOPMENT OF COMPONENT
MODELS
o Surface Runoff Modeling
• Rational Method (Mulvany, 1850;
Imbeau, 1892)
• Unit Hydrograph Method (Sherman,
1932)
• Overland Flow Analysis (Keulegan, 1944;
Izzard, 1944)
• Unit Hydrograph Theory (Nash, 1957;
Dooge, 1959)
o Subsurface Flow Modeling
Subsurface Flow Mechanism
(Lowdermilk, 1934; Hursh, 1936; Hursh
and Brater, 1944; Hoover and Hursh,
1944; Hursh, 1944; Roessel, 1950;
Hewlett, 1961; Nielsen et al., 1959;
Remson, et al., 1960)
HISTORICAL PERSPECTIVE
• Determination of Storm Runoff
Amount
SCS-CN Method (1956)
• Theory of Infiltration
Green-Ampt Model (1911)
Kostiakov Model (1932)
Horton Model (1933)
• Theory of Evaporation
Energy Method (Richardson,
1931; Cummings, 1935)
Combination Method (Penman,
1948)
HISTORICAL PERSPECTIVE
• Determination of Abstractions
- Interception (Horton, 1919)
- Detention and Depression Storage
(SCS9 1956)
o Base Flow
Darcy Equation (1854)
Hydraulic Conductivity Relation
(Fair and Hatch, 1933)
Well Response to Pumping (Theis,
1935)
Correlation between Ground Water
and Precipitation (Jacob, 1943, 1944)
HISTORICAL
PERSPECTIVE
o Reservoir Routing
Puis Method (USACOE, 1928)
Modified Puis Method (USBR, 1949)
o Channel Routing
Muskingum Method (McCarthy,
1934-35)
Modified Puis Method (USBR, 1949)
WATERSHED MODELS
• MODELS OF HYDROLOGIC CYCLE
• STANFORD WATERSHED MODEL (NOW
HSPF) (Crawford and Linsley, 1966)
• EXAMPLES OF MODELS
- HSPF-IV (Bicknell et al., 1993)
- USDA-HL Model (Holtan et al.,
1974)
- PRMS (Leavesley et al., 1983)
- NWS-RFS (Burnash et al., 1973)
- SSARR (Rockwood, 1982)
- SWMM (Metalf and Eddy et al.,
1971)
- HEC-HMS (U. S. Army Corps of
Engineers, 1999)
WATERSHED MODELS
KINEROS (Woolhiser et al, 1990)
- ANSWERS (Beasley et al., 1977)
- CREAMS (USDA, 1980)
- EPIC (Williams, 1995)
SWRRB (Williams, 1995)
SPUR (Carison et al., 1995)
AGNPS (Young et al., 1995)
- WATFLOOD (Kouwen et al., 1993)
- UBC (Quick, 1995)
- SHE (Abbott et al., 1986)
- TOPMODEL (Beven, 1995)
- IHDM (Calver and Wood, 1995)
- SHETRAN (Ewen et al., 2000)
MI
WATERSHED MODELS
- WBNM (Boyd et al., 1979)
- RORB (Laurenson and Mein, 1995)
- THALES (Grayson et al., 1995)
LASCAM (Sivapalan et al., 1996)
- Tank Model (Sugawara, 1975)
- Xinanjiang Model (Zhao et al., 1980)
- HBV Model (Bergstrom, 1976)
- ARNO Model (Todini, 1988)
- TOPIKAPI Model (Todini, 1995)
- HYDROTEL (Fortin et al., 2001)
CLASSIFICATION OF
WATERSHED MODELS
0
CRITERIA FOR CLASSIFICATION
- Process Description
- Dynamics and Simplification
Time Scale
- Space Scale
- Method of Solution
- Land Use
- Model Use
- Model Complexity
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1
MODEL CONSTRUCTION
• MODEL ARCHITECTURE AND
STRUCTURE
• WATERSHED REPRESENTATION
• HYDROLOGIC PROCESS
- Precipitation
- Storage Abstractions
- Evaporation and Evapotranspiration
- Infiltration
Soil Moisture Accounting
- Runoff Production
Snowmelt Runoff
- Surface Runoff Routing
- Channel Flow Routing
- Interflow
- Groundwater Flow
- Stream-Aquifer Interaction
- Water Quality
MODEL CONSTRUCTION
• MODEL CALIBRATION
• GOODNESS-.OF-TEST
• MODEL VALIDATION
• MODEL ERROR ANALYSIS
• MODEL RELIABILITY
RECENT ADVANCES
o
HYDROLOGIC PATA NEEDS
- Hydrometeorologic
- Topographic
- Geomorphologic
- Pedologic
- Land Use
Lithologic
Hydraulic
HYDROLOGIC PATA ACQUISITION
- Remote Sensing
- Satellite Technology
Radar Technology
- Digital Terrain and Elevation Modeis
- Chemical Tracers
o
PATA PROCESSING AND MANAGEMENT
- Geographical Information Systems (GIS)
- Pata Base Management Systems (DBMS)
RAINFALL VARIABILITY
• STORM MOVEMENT
• SPATIAL VARIABILITY
• TEMPORAL VARIABILITY
• RAINFALL FIELD
DESCRIPTION
• RAINFALL FORECASTING
VARIABILITY IN
WATERSHED
CHARACTERISTICS
0
SPATIAL VARIABILITY OF
HYDRAULIC ROUGHNESS
- Effect 011 Runoff Dynamics and Hydrograph
- Formation of Shocks
SPATIAL VARIABILITY OF
INFILTRATION
- Hydraulic Conductivity
Steady Infiltration
- Mean Infiltration
Effect on Runoff Hydrograph
SCALING AND
VARIABILITY
• SPATIAL SCALING
- Spatial Heterogeneity in Watershed
Characteristics
- Spatial Variability in Processes
• PHYSICAL SPATIAL SIZE
- Representative Elementary Area
- Hydrologic Response Units
- Computational Grid Size
• TEMPORAL SCALING
- Time Interval of Observations
- Computational Grid Size
- Temporal Variability of Processes
LIN NG HYDROLOGIC
MODELS
• GEOCHEMISTRY
• ENVIRONMENTAL BIOLOGY
• METEOROLOGY
• CLIMATOLOGY
• OCEANOGRAPHY
• SOCIAL SCIENCES
• ECONOMICS
• DECISION MAKING
MODEL CALIBRATION
9
PARAMETER ESTIMATION
ALGORITHM
Obj ective Function
Optimization Algorithm
- Termination Criteria
- Calibration Data
• HANDLING DATA ERRORS
• DETERMINATION OF DATA
NEEDS-QUANTITY AND
INFORMATION-RICHNESS
REPRESENTATION OF
UNCERTAINTY OF CALIBRATED
MODEL
• ARTIFICIAL NEURAL NETWORKS
FUTURE OUTLOOK
• INCREASING SOCIETAL DEMAND
FOR MODELS
• INCREASING EMPHASIS ON
LINKING MODELS TO
ENVIRONMENTAL AND ECO-
SYSTEMS
• EMPHASIS ON USER-
FRIENDLINE SS
• INC ORPORATION OF
INFORMATION TECHNOLOGy,
COMPUTER-BASED DESIGN,
ARTIFICIAL INTELLIGENCE, AND
SPACE TECHNOLOGY
• MODEL UNCERTAINTY AND
RELIABILITY
• MODEL COMPETITIVENESS

Hydrologic modeling

  • 1.
    a)(ft G YDROLOGIC MODELING • INTRODUCTION •HISTORY • RECENT ADVANCES • FUTURE OUTLOOK
  • 2.
    INTRODUCTION • DEFINITION OFHYDROLOGY - What happens to the ram? Occurrence, Movement, Distribution, and Storage of Water Quantity and Quality - Spatial, Temporal, and Frequency Domains (or Characteristics) - Quality of Water-Physical, Chemical and Biological - Spatial Scale-Watershed, Regional (Basin), Continental, and Global - Dynamic Interaction between Atmosphere, Pedosphere, Lithosphere, and Hydrosphere- Controlling Influences on Hydrology
  • 3.
    APLICATION OF HYDROLOGIC MODELS •PLANNING, DESIGN, DEVELOPMENT, OPERATION, AND MANAGEMENT OF WATER RESOURCES PROJECTS • WATERSHED MANAGEMENT • ENVIRONMENTAL PROTECTION AND MANAGEMENT • CLIMATE CHANGE
  • 4.
    APPLICATION OF HYDROLOGIC MODELS 0 SPECIFICEXAMPLES - Flood Protection Projects, Flood Warning Systems, Reservoir Release Planning, Flood Plain Management, etc. Rehabilitation of Aging Dams Water Supply Forecasting - Irrigation Water Management - Wetland Restoration - Stream Restoration - Water Table Management - Drainage Systems Design - Soil Conservation Practices - Habitat Modeling - Hydropower Development - Consumptive Use and Water Allocation
  • 5.
    HISTORICAL PERSPECTIVE 0 THE BEGINNING YEARS: DEVELOPMENTOF COMPONENT MODELS o Surface Runoff Modeling • Rational Method (Mulvany, 1850; Imbeau, 1892) • Unit Hydrograph Method (Sherman, 1932) • Overland Flow Analysis (Keulegan, 1944; Izzard, 1944) • Unit Hydrograph Theory (Nash, 1957; Dooge, 1959) o Subsurface Flow Modeling Subsurface Flow Mechanism (Lowdermilk, 1934; Hursh, 1936; Hursh and Brater, 1944; Hoover and Hursh, 1944; Hursh, 1944; Roessel, 1950; Hewlett, 1961; Nielsen et al., 1959; Remson, et al., 1960)
  • 6.
    HISTORICAL PERSPECTIVE • Determinationof Storm Runoff Amount SCS-CN Method (1956) • Theory of Infiltration Green-Ampt Model (1911) Kostiakov Model (1932) Horton Model (1933) • Theory of Evaporation Energy Method (Richardson, 1931; Cummings, 1935) Combination Method (Penman, 1948)
  • 7.
    HISTORICAL PERSPECTIVE • Determinationof Abstractions - Interception (Horton, 1919) - Detention and Depression Storage (SCS9 1956) o Base Flow Darcy Equation (1854) Hydraulic Conductivity Relation (Fair and Hatch, 1933) Well Response to Pumping (Theis, 1935) Correlation between Ground Water and Precipitation (Jacob, 1943, 1944)
  • 8.
    HISTORICAL PERSPECTIVE o Reservoir Routing PuisMethod (USACOE, 1928) Modified Puis Method (USBR, 1949) o Channel Routing Muskingum Method (McCarthy, 1934-35) Modified Puis Method (USBR, 1949)
  • 9.
    WATERSHED MODELS • MODELSOF HYDROLOGIC CYCLE • STANFORD WATERSHED MODEL (NOW HSPF) (Crawford and Linsley, 1966) • EXAMPLES OF MODELS - HSPF-IV (Bicknell et al., 1993) - USDA-HL Model (Holtan et al., 1974) - PRMS (Leavesley et al., 1983) - NWS-RFS (Burnash et al., 1973) - SSARR (Rockwood, 1982) - SWMM (Metalf and Eddy et al., 1971) - HEC-HMS (U. S. Army Corps of Engineers, 1999)
  • 10.
    WATERSHED MODELS KINEROS (Woolhiseret al, 1990) - ANSWERS (Beasley et al., 1977) - CREAMS (USDA, 1980) - EPIC (Williams, 1995) SWRRB (Williams, 1995) SPUR (Carison et al., 1995) AGNPS (Young et al., 1995) - WATFLOOD (Kouwen et al., 1993) - UBC (Quick, 1995) - SHE (Abbott et al., 1986) - TOPMODEL (Beven, 1995) - IHDM (Calver and Wood, 1995) - SHETRAN (Ewen et al., 2000) MI
  • 11.
    WATERSHED MODELS - WBNM(Boyd et al., 1979) - RORB (Laurenson and Mein, 1995) - THALES (Grayson et al., 1995) LASCAM (Sivapalan et al., 1996) - Tank Model (Sugawara, 1975) - Xinanjiang Model (Zhao et al., 1980) - HBV Model (Bergstrom, 1976) - ARNO Model (Todini, 1988) - TOPIKAPI Model (Todini, 1995) - HYDROTEL (Fortin et al., 2001)
  • 12.
    CLASSIFICATION OF WATERSHED MODELS 0 CRITERIAFOR CLASSIFICATION - Process Description - Dynamics and Simplification Time Scale - Space Scale - Method of Solution - Land Use - Model Use - Model Complexity
  • 13.
    f Vote r able vi w(t) .S • ','•'S 5 •.".I'.* ••1I..S.. .5•.. 'lPh• .0 •'• 'S5 C x,y,z,f''S s ,
  • 14.
  • 15.
    MODEL CONSTRUCTION • MODELARCHITECTURE AND STRUCTURE • WATERSHED REPRESENTATION • HYDROLOGIC PROCESS - Precipitation - Storage Abstractions - Evaporation and Evapotranspiration - Infiltration Soil Moisture Accounting - Runoff Production Snowmelt Runoff - Surface Runoff Routing - Channel Flow Routing - Interflow - Groundwater Flow - Stream-Aquifer Interaction - Water Quality
  • 16.
    MODEL CONSTRUCTION • MODELCALIBRATION • GOODNESS-.OF-TEST • MODEL VALIDATION • MODEL ERROR ANALYSIS • MODEL RELIABILITY
  • 17.
    RECENT ADVANCES o HYDROLOGIC PATANEEDS - Hydrometeorologic - Topographic - Geomorphologic - Pedologic - Land Use Lithologic Hydraulic HYDROLOGIC PATA ACQUISITION - Remote Sensing - Satellite Technology Radar Technology - Digital Terrain and Elevation Modeis - Chemical Tracers o PATA PROCESSING AND MANAGEMENT - Geographical Information Systems (GIS) - Pata Base Management Systems (DBMS)
  • 18.
    RAINFALL VARIABILITY • STORMMOVEMENT • SPATIAL VARIABILITY • TEMPORAL VARIABILITY • RAINFALL FIELD DESCRIPTION • RAINFALL FORECASTING
  • 19.
    VARIABILITY IN WATERSHED CHARACTERISTICS 0 SPATIAL VARIABILITYOF HYDRAULIC ROUGHNESS - Effect 011 Runoff Dynamics and Hydrograph - Formation of Shocks SPATIAL VARIABILITY OF INFILTRATION - Hydraulic Conductivity Steady Infiltration - Mean Infiltration Effect on Runoff Hydrograph
  • 20.
    SCALING AND VARIABILITY • SPATIALSCALING - Spatial Heterogeneity in Watershed Characteristics - Spatial Variability in Processes • PHYSICAL SPATIAL SIZE - Representative Elementary Area - Hydrologic Response Units - Computational Grid Size • TEMPORAL SCALING - Time Interval of Observations - Computational Grid Size - Temporal Variability of Processes
  • 21.
    LIN NG HYDROLOGIC MODELS •GEOCHEMISTRY • ENVIRONMENTAL BIOLOGY • METEOROLOGY • CLIMATOLOGY • OCEANOGRAPHY • SOCIAL SCIENCES • ECONOMICS • DECISION MAKING
  • 22.
    MODEL CALIBRATION 9 PARAMETER ESTIMATION ALGORITHM Objective Function Optimization Algorithm - Termination Criteria - Calibration Data • HANDLING DATA ERRORS • DETERMINATION OF DATA NEEDS-QUANTITY AND INFORMATION-RICHNESS REPRESENTATION OF UNCERTAINTY OF CALIBRATED MODEL • ARTIFICIAL NEURAL NETWORKS
  • 23.
    FUTURE OUTLOOK • INCREASINGSOCIETAL DEMAND FOR MODELS • INCREASING EMPHASIS ON LINKING MODELS TO ENVIRONMENTAL AND ECO- SYSTEMS • EMPHASIS ON USER- FRIENDLINE SS • INC ORPORATION OF INFORMATION TECHNOLOGy, COMPUTER-BASED DESIGN, ARTIFICIAL INTELLIGENCE, AND SPACE TECHNOLOGY • MODEL UNCERTAINTY AND RELIABILITY • MODEL COMPETITIVENESS