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University of Texas at Austin
Title: Space-Time Analysis of Water Availability Model Data in GIS Statistical Analysis of Naturalized Flows in Texas’ Water Availability Model Considerations on the impact of trends in the naturalized flows of Texas’ Water Availability Model (WAM), as evidenced by statistical analysis. Clark Siler, 28 Apr 2009 CE 397 – Statistics in Water Resources University of Texas at Austin
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Presentation Outline Introduction Correlation and Trend Analysis
What is a WAM What are Naturalized Flows Correlation and Trend Analysis Pearson’s r Kendall’s Tau Results Conclusions and Possible Future Work Presentation Outline
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Water Availability Model (WAM)
Texas’ Water Availability Model consists of: Water Rights Analysis Package Suite of programs to digitally manage water rights Based on probabilistic and statistical analyses Developed by Dr. Ralph Wurbs at Texas A&M Input datasets for Texas’ 23 River Basins This includes the naturalized flow datasets Wurbs (2005)
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Uses of WAM Texas Commission on Environmental Quality (TCEQ)
Assigning new or adjusting existing water right permits Determine if sufficient water to meet proposed use Evaluate impact of use on other water users Consultants and Water Management Entities Local and regional planning studies Preparing permit applications Texas Water Development Board (TWDB) Statewide planning Wurbs (2005)
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Naturalized Flows (Analytical)
NF naturalized flow GF gaged flow D water supply diversions upstream RF return flow upstream EP reservoir evaporation minus precipitation DS change in storage in upstream reservoirs Goal is homogeneous flow dataset NF = GF + SDi – SRFi + SEPi + SDSi NF GF D RF EP DS
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Naturalized Flows ?
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Purpose of Study Goal of naturalized flows is homogeneity
Trends may result from many causes Climate change El Niño-Southern Oscillation (ENSO) Incorrect calculations (not considered) Trended data are not homogeneous WRAP does not handle trended data Results from such are not considered representative
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Neches Basin Naturalized Flows: WRAP
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Correlation (Pearson’s)
to WRAP WRAP to WRAP WRAP
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Trend Analysis: Kendall’s Tau, t
Non-parametric Statistic (no assumptions on distribution) Based on rank; tests monotonicity H0: no correlation between time and flow Rejected (or not) based on comparison with standard normal calculations Can address seasonality through careful data separation and processing
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Overall Kendall Results
Regression using time Only one location rejected H0 WRAP to time
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Seasonal Kendall Results
Despite many individual seasons having H0 rejected, only one additional location is rejected overall WRAP to time
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Conclusions Kendall’s Tau provides non-parametric statistic
Failed to reject H0 for majority of Neches gages Suggests homogeneity of dataset Kendall’s test is for monotonicity; other trends may still exist (e.g. longer-term seasonality, ENSO)
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Possible Future Work Working to detect cycles (such as ENSO) following process outlined by Wurbs Comparing Spearman to Kendall rank correlation Exploring applications of Pearson (parametric) correlation to Neches datasets Represent results effectively in GIS Analyzing other Texas basins
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Personal Information Clark Siler Graduate Student
University of Texas at Austin Environmental Water Resources Engineering (EWRE) Center for Research in Water Resources BS – Brigham Young University Civil Engineering MS – University of Texas at Austin EWRE Personal Information (Presenter) Nov 2008
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Additional Information
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San Diego MSL
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Codes
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Tables WRAP to time WRAP to time
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