Alabama Irrigation Initiative Environmental Meeting 10/31/2008.
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Transcript of Alabama Irrigation Initiative Environmental Meeting 10/31/2008.
Alabama Irrigation InitiativeEnvironmental Meeting
10/31/2008
Ecological Approach
• Original approach was to statistically analyze volumetric withdrawals.
• Ecologically, the area of inundation is potentially just as important as volumetric flow
• Revised approach to analyze total flood plain affected by withdrawals
Center for Freshwater Studies Area of Interest – Sipsey River Swamp
Approach
USGS Historic Data & Rating Curves
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Interpolated Gage Height
Actual Gage Height
Rating CurveRating curve based on USGS dataRelates discharge (known) to gage height (needed)
• USGS provides table of Discharge versus Gage Height
• Estimated gage height in region of interest (approximately 4.5 miles downstream of Elrod station)
• Interpolation routine for Rating data is statistically accurate.
• Currently have rating data 11 & 12 (1995 – present).
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Actual Gage Height
Area of Interest – GIS Model
GIS Area Model
ArcGIS Area Data
• Similar to the Rating Curve table, the “Area Curve” table is used to estimate the area of inundation from a “synthetic” withdrawal.
• The interpolation routine for area data is accurate.
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Gage Height (above 185.66')
Acr
es Area (acres)
Interpolated Area (acres)
Statistical Analysis Method
• The Wilcoxon Rank-Sum test is used– The Wilcoxon rank-sum
test is a nonparametric alternative to the two sample t-test
– The null hypothesis is that the means of the two samples are statistically equal.
– If the shift is greater than the confidence level (α). For a two-tailed test (A=B versus A≠B), confidence level is α/2
Statistical Analysis Spreadsheet 365 vs. 120 day analysis
2001 365-day Analysis
• Before withdrawal in orange (burnt?)
• After withdrawal in blue (39.5% of discharge withdrawn)
• This was the highest flow day during withdrawal period (January through April)
2001 120-day Analysis
• Before withdrawal in orange…
• After withdrawal in blue (16.7% of discharge withdrawn)
• This was the highest flow day during withdrawal period (January through April)
Approximate Area before/after Synthetic Withdrawal
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1 19 37 55 73 91 109 127 145 163 181 199 217 235 253 271 289 307 325 343 361
Area of inundation BW (acreas)
Area of Inundation AW (acres)
Discharge (cfs)
Discharge AW (cfs)
• Withdrawal set at 12% of discharge.• That equates to 44225 acre-ft• Withdrawal period is Jan-April 1995 (Rating
Curve 11)
Year Total Withdrawal (acre-ft)
1995 44,225
1996 50,466
1997 45,025
1998 53,154
1999 47,435
2000 29,458
2001 65,731
2002 44,230
2003 55,296
2004 69,879
2005 31,039
2006 60,150
2007 35,963
2008 41,419
Average= 48,105
Max= 69,879
Min= 29,458
Scaling Up to the AL and TN RiversPercent Withdrawan Year Total Acre Feet
12.00% 1995 1,429,140
12.50% 1996 2,059,965
13.00% 1997 1,891,070
10.50% 1998 2,163,854
11.00% 1999 937,516
8.70% 2000 541,633
16.65% 2001 2,419,211
15.70% 2002 1,138,976
12.90% 2003 1,543,614
17.85% 2004 1,202,672
11.30% 2005 1,395,497
15.05% 2006 1,239,750
19.25% 2007 862,494
19.90% 2008 960,040
Average= 1,413,245
Max= 2,419,211
Minimum= 541,633
Percent Withdrawan Year Total Acre Feet
12.00% 1995 1,533,024
12.50% 1996 2,163,887
13.00% 1997 2,296,935
1998
1999
8.70% 2000 643,248
16.65% 2001 1,347,570
15.70% 2002 1,584,510
12.90% 2003 1,841,181
2004
11.30% 2005 1,344,564
2006
2007
2008
Average= 1,594,365
Max= 2,296,935
Minimum= 643,248
Alabama River - Claiborne Tennessee River - Whitesburg
Perspective
• The minimum available water from the AL and TN rivers could irrigate ~1,000,000 acres.
• That is approximately ~3% of the total area of Alabama
Conclusions/Issues
• Basing withdrawals on the cyclic inundation of a floodplain attempts to take the river ecology into account
• The method shows that statistically insignificant fractions are available that are within the total, annual variability of the river
• Each river is unique and analysis may have to be modified to account for different channel/floodplain characteristics