COMET Hydromet 00-2 7 March 2000 - PowerPoint PPT Presentation

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COMET Hydromet 00-2 7 March 2000

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Estimation of parameter values which will minimize differences between observed ... Low flows. Convergence criteria. Optimize SAC-SMA, SNOW-17, UG, API-SLC, XIN-SMA ... – PowerPoint PPT presentation

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Title: COMET Hydromet 00-2 7 March 2000


1
National Weather ServiceRiver Forecast
SystemModel Calibration
  • COMETHydromet 00-27 March 2000
  • 2290 East Prospect Road, Suite 1
  • Fort Collins, Colorado 80525

2
Calibration
  • Calibration process
  • Estimation of parameter values which will
    minimize differences between observed and
    simulated streamflows
  • Calibration problems
  • Parameter interaction
  • Non-unique solutions
  • Time-consuming
  • Inaccuracies
  • Non-linearities
  • Lack of understanding

3
Calibration System
  • Parameter estimation/optimization and watershed
    simulation
  • Input
  • Point or areal estimates of historical
    precipitation, temperature, and potential
    evaporation
  • Initial hydrologic conditions
  • Output
  • Basin areal averages for point value inputs
  • Simulated hydrographs for historical analysis or
    use in ESP
  • Parameter values for models in operational
    forecast and ESP systems

4
Calibration System (continued)
  • Characteristics
  • Performs computations for few forecast points for
    many time steps
  • Uses operations table
  • Compatible with operational system and ESP
  • Produces graphical output for manual calibration
  • Includes algorithms for automatic optimization
  • Applications
  • Historical watershed simulation
  • Model calibration

5
Model Calibration
  • Strategy
  • Select river system
  • Prepare data
  • MAP - Mean Areal Precipitation
  • MAT - Mean Areal Temperature
  • PE - Potential Evaporation
  • QME - Mean Daily Discharge
  • QIN - Instantaneous Discharge

6
Model Calibration (continued)
  • Calibrate least complicated headwater basins
  • Select calibration period
  • Estimate initial parameter - observed Qs
  • Trial and error using MCP
  • Statistics, observed versus simulated plots
  • Proper approach to parameter adjustment
  • Automatic parameter optimization - OPT
  • Fine tuning - MCP
  • Calibrate other headwater areas
  • Calibrate local areas

7
Model Calibration (continued)
  • Important considerations
  • Model structure, simulation processes
  • Effects of parameter changes
  • Use of the forecast information

8
Data Preparation
  • MAP Algorithms - Mean Areal Precipitation
  • Techniques for converting point precipitation
    measurements into areal measurements and
    distributing them properly in time
  • Daily and hourly data
  • Grid point algorithm
  • Estimating precipitation at a point (1/D2)
  • Estimate gtleast, ltgreatest
  • 100-150 points within basin
  • Normalize at each grid point, then renormalize
  • Thiessen weights
  • Grid point versus Thiessen
  • Two-pass algorithm - distribute daily, then
    estimate missing
  • Consistency plots
  • MAT Algorithms - Mean Areal Temperature
  • Max - min data
  • Grid point algorithm (1/D)
  • Elevation weighting factor
  • Centroid (1/DP)
  • Conversion to mean temperatures
  • Consistency plots

9
Historical Data Analysis
  • General Information Needed
  • Station data on Calibration files
  • Station history infro - obs times, changes,
    location, moves
  • Topog map of basin

MAP Specific Information Non- Mountainous
Mountains --basin boundary --isohyetal
map
--station weights
MAT Specific Information --mean max/min
temperatures Non-Mountainous Mountains
--basin boundary --areal-elev curve
MAPE Specific Information --Evaporation
maps --mean monthly evap --station weights
  • PXPP
  • check consistency
  • compute normals
  • MAT3
  • check consistency
  • MAPE
  • check consistency
  • generate daily time
  • series of MAPE
  • TAPLOT3
  • get mean max/min for
  • mean zone elevation
  • MAP3
  • (re)check consistency
  • generate time series
  • of MAP
  • MAT3
  • generate time
  • series of MAT

Temperature
Evaporation
Precipitation
10
Sacramento Soil Moisture Accounting Model
11
Sacramento Model Structure
12
Hydrograph Decomposition
13
Sacramento Soil Moisture Components
14
Initial Soil-moisture ParameterEstimates By
Hydrograph Analysis
15
Initial Soil-moisture Parameter Estimates By
Hydrograph Analysis (continued)
  • LZSK - Supplemental baseflow recession
    (always gt LZPK)
  • Flow that typically persists anywhere from 15
    days to 3 or 4 months

16
Initial Soil Moisture Parameters Estimates by
Hydrograph Analysis (continued)
17
Initial Soil Moisture Estimates by Hydrograph
Analysis (continued)
18
Multiyear Statistical Output
19
Multiyear Statistical Output (continued)
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Automatic Optimization
  • Program OPT3
  • Uses operations table
  • Compatible with MCP, OFS, ESP
  • Objective functions
  • Daily RMS error
  • Monthly volume RMS error
  • S - O Exp.
  • log S - log O Exp.
  • Correlation coefficient
  • Maximum Likelihood Estimator

45
Automatic Optimization (continued)
  • Program OPT3 (continued)
  • Optimization schemes
  • Pattern search
  • Adaptive random search
  • Shuffled complex evolution
  • Buffer
  • Exclusion periods
  • Low flows
  • Convergence criteria
  • Optimize SAC-SMA, SNOW-17, UG, API-SLC, XIN-SMA

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