SWC Methodology - TWG February 19, 2015 Settlement Document Subject to I.R.E. 408.
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Transcript of SWC Methodology - TWG February 19, 2015 Settlement Document Subject to I.R.E. 408.
SWC Methodology - TWG
February 19, 2015
Settlement Document Subject to I.R.E. 408
Update on Natural Flow Predictor Models
April 1 Models• Considering using other forecasts• Predictor models for all SWC members • Relationship between Box Canyon and
Blackfoot to Milner reach gains.
NRCS USACOE/USBR Averaged NRCS/USACOE&USBR
2000 25% 12% 18%
2001 1% 13% 7%
2002 14% 12% 13%
2003 7% 3% 5%
2004 -19% -13% -16%
2005 10% 10% 10%
2006 25% 24% 24%
2007 1% 0% 1%
2008 -10% -12% -11%
2009 -36% -26% -31%
2010 -13% -20% -17%
2011 -2% 12% 5%
2012 5% 16% 11%
2013 23% 14% 19%
2014 2% 3% 3%
Average 2% 3% 3%
Standard Deviation 18% 15% 16%
New TFCC April Natural Flow Predictor
TFCC= 62.01 (Heise) +12,980(Box) – 609,600
Where:TFCC = TFCC natural flow supply from April to October;Hei = Heise natural flow forecast from April – July in (KAF);Box = Box Canyon total flow from November through March (KAF).
Adjusted R2 p SE DOF F-statistic0.8664 <0.001 38,010 21 75.6
Current April Natural Flow ModelsSWC
MemberEquation
(less one standard error)R2
A&B y = 0.0092x - 19.747 0.887
AFRD2 y = 0.0742x - 141.14 0.8317
BID y = 0.0344x - 2.5853 0.7964
Milner y = 0.0102x - 19.412 0.9243
MID y = 0.0484x + 2.7178 0.7896
NSCC y = 0.1562x - 53.005 0.8952
TFCC y = 0.0658x + 626.37 0.5416
Where:y = Natural flow April – October for the SWC Member (AF);x = Heise Natural Flow (April 1 – July 31). USBR/ACOE Heise forecast is used in April.
*To error on the side of the SWC , natural flow predictions are one standard error below regression line.
April 1 Predictor Models for other SWC Members
• Used the same variables that were used for TFCC model:– Heise– Box Canyon
• Found no model improvement for:– A&B– AFRD2 ?– Milner– All have late priority NF rights
SWC Member
Water Right Priorities
A&B 1939
AFRD2 1921
BID 1903, 1908, 1939
Milner 1916, 1939, 1939
MID 1903, 1908, 1939
NSCC 1900, 1905, 1908, 1915, 1920
TFCC 1900, 1915, 1939
Multilinear Regression Model : AFRD24to10 = HeiseAprtoJulKAF + Box11to3)Residuals: Min 1Q Median 3Q Max -64494 -22886 -6416 19101 64373
Coefficients: Estimate Std. Error t value Pr(>|t|) (Intercept) -435713.23 170094.89 -2.562 0.0182 * HeiseAprtoJulKAF 73.22 6.70 10.928 4.01e-10 ***Box11to3 3317.91 1673.59 1.983 0.0607 . ---Signif. codes: 0 ‘***’ 0.001 ‘**’ 0.01 ‘*’ 0.05 ‘.’ 0.1 ‘ ’ 1
Residual standard error: 37290 on 21 degrees of freedomMultiple R-squared: 0.8583, Adjusted R-squared: 0.8448 F-statistic: 63.58 on 2 and 21 DF, p-value: 1.233e-09
AFRD2 April 1 Models
Linear Regression Model: AFRD24to10 = HeiseAprtoJulKAF
Residuals: Min 1Q Median 3Q Max -69999 -23845 -1323 20850 79034
Coefficients: Estimate Std. Error t value Pr(>|t|) (Intercept) -1.014e+05 2.389e+04 -4.247 0.00033 ***HeiseAprtoJulKAF 7.418e+01 7.114e+00 10.428 5.6e-10 ***---Signif. codes: 0 ‘***’ 0.001 ‘**’ 0.01 ‘*’ 0.05 ‘.’ 0.1 ‘ ’ 1
Residual standard error: 39700 on 22 degrees of freedomMultiple R-squared: 0.8317, Adjusted R-squared: 0.8241 F-statistic: 108.7 on 1 and 22 DF, p-value: 5.604e-10
April 1 MLR Predictor ModelsSWC
MemberPredictor Model
Natural Flow Diversions (April – October)Adjusted
R2SE F-Statistic
BID BID = 33.64(Heise) + 2570(Box) – 240,800 0.8546 17,100 68.61
MID MID = 47.12(Heise) + 4302(Box) – 401,000 0.8786 22,070 84.22
NSCC NSCC = 154.19(Heise) + 6834.23(Box) – 677,949 0.9151 55,950 125
TFCC TFCC= 62.01 (Heise) +12,980(Box) – 609,600 0.8664 38,010 75.6
Where:Heise is the total Heise natural flow from April – June in (KAF); Box = Box Canyon total flow from November through March (KAF).
Current April Natural Flow ModelsSWC
MemberEquation
(less one standard error)R2
A&B y = 0.0092x - 19.747 0.887
AFRD2 y = 0.0742x - 141.14 0.8317
BID y = 0.0344x - 2.5853 0.7964
Milner y = 0.0102x - 19.412 0.9243
MID y = 0.0484x + 2.7178 0.7896
NSCC y = 0.1562x - 53.005 0.8952
TFCC y = 0.0658x + 626.37 0.5416
Where:y = Natural flow April – October for the SWC Member (AF);x = Heise Natural Flow (April 1 – July 31). USBR/ACOE Heise forecast is used in April.
*To error on the side of the SWC , natural flow predictions are one standard error below regression line.
Box Canyon Discussion
July 1 Models• Two Oceans Plateau SWE – Consider using an earlier date to remove years with
zeros• Concerns over using Spring Creek data.– Consider using only metered data– Investigate using other indicators
• Tyhee (missing data 1995 – 2001)• Wells
• Predict total natural flow in the Blackfoot to Milner reach then allocate by priority
Two Oceans Plateau
• Looked at June 1 and June 15.• June 15 had better results than June 1. • June 15 data set has 4 years with zero SWE• July 1 data set has 13 years with zero SWE
July 1 MLR Predictor ModelsSWC
MemberAdjusted
R2SE F-Statistic
BID Old 0.8672New 0.828
12,81014,580
51.0637.9
MID Old 0.8808New 0.8438
17,49020,020
57.6342.42
NSCC 0.9003New 0.8593
39,82047,300
70.2247.83
TFCC 0.8304New 0.8511
31,24029,270
38.5444.83
Where:Heise is the total Heise natural flow from April – June in (KAF);SpringCreek is Spring Creek total flow from January - May (KAF);TwoOceans is the July 15 Snow Water Equivalent (in).
Spring Creek Alternatives