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69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Wind and Wave Measurements in 
Irrigation Reservoirs
Yavuz Ozeren
National Center for Computational Hydroscience and Engineering
The University of Mississippi, Oxford, MS
Daniel Wren
USDA‐ARS, National Sedimentation Laboratory, Oxford MS
Michele Reba
USDA‐ARS, Delta Water Management Research Unit, Jonesboro, AR
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Introduction
• The earthen embankments of these reservoirs 
often experience significant erosion primarily 
due to wind‐generated waves; therefore, 
require annual repairs if they are not 
protected. 
• The design of effective embankment 
protection requires knowledge of the wind‐
generated wave characteristics and their 
relationship to embankment erosion. 
• Irrigation reservoirs are commonly 
used for irrigation water storage in 
lower Mississippi river floodplain.  
• A field measurement station was installed in an 
irrigation reservoir near Harrisburg, AR, to 
acquire synchronous measurements of wind and 
wave properties along with levee erosion data. 
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Field Site
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Field Site
• Wave staffs
• Wind gauge
• Erosion pins
• Ground‐based LIDAR
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi



0
)( dffSfm i
i
omo mH 004.4
Field Measurements
An example time series water surface displacement data (June, 2012, 
Jonesboro, AR).  The vertical axis is vertical water surface displacement.
Five‐hour‐average energy spectrum of the 
measured waves in July 19, 2012
Wave period, wave height and wind speed histograms for the 
time period between June 2012 and October 2012.
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Field Measurements
Wave characteristics
R26
(March 2005)
R26
(June 2008)
R27
(June 2012)
Wind speed, U10 (m/s) 14 (NE) 13 (SW) 9.5 (S)
Fetch length 586 450 470
Wave height, Hm0 (m) 0.25 0.23 0.14
Peak period, Tp (s) 1.7 1.6 1.4
Significant period, Ts (s) 1.7 1.6 1.2
Mean period, Tm (s) 1.4 1.4 1.1
Significant wave height, Hs (m) 0.23 0.20 0.13
Maximum wave height, Hmax (m) 0.38 0.39 0.24
RMS wave height, Hrms (m) 0.17 0.12 0.09
The ranges of measured wave parameters compared to field 
measurements in 2005, 2008 and 2012.
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
44.0
22
0
0025.0 








AA
m
U
gF
U
gH
28.0
2
415.00 








AA
p
U
gF
U
gT
Wave Prediction
Method Hm0 (m) Tp (s) tmin
(min)
JONSWAP 0.11 1.1 15.2
Wilson (1965) 0.17 1.3 12.5
SMB, Bretschneider (1970) 0.19 1.7 9.4
Krylow (1976) 0.21 1.6 ‐
Donelan (1980) 0.16 1.4 10.3
Ozeren and Wren (2010) 0.14 1.3 11.8
Comparison of empirical wind wave prediction methods
72.0
2
min
087.42 








AA U
gF
U
gt
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Erosion
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Protection techniques
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Floating Wave Barriers
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Floating Wave Barriers
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Floating Wave Barriers
T = 0.6 s, H = 28 mm, h = 0.466m
2.00 2.24 2.48 2.72 2.96 3.20
x (m)
0.0
0.6
z (m)
t=24.399208 s
2.00 2.24 2.48 2.72 2.96 3.20
x (m)
t=24.598543 s
Laboratory and numerical experiments
Shafer lake (2005‐2009)
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Shape and Orientation
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Shape and Orientation
Internal Levees (U = 10 m/s) Floating wave barriers (U = 10 m/s, Breakwater size =  0.5 m)
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
LMRB
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Irrigation 
reservoir 
(R)
Area – A
(m2
)
Levee 
Length (m)
Max. Fetch 
– Fmax (m)
Max. fetch 
azimuth 
(deg.)
Shape 
factor
17 116,500 1,336 483 ‐35 1.02
21 123,525 1,421 516 33 0.95
14 125,753 1,404 500 ‐47 1.01
20 126,755 1,377 510 49 1.02
19 128,328 1,411 510 43 1.01
7 132,719 1,422 508 ‐49 1.04
3 138,417 1,585 636 22 0.78
27 142,109 1,529 562 26 0.94
9 151,950 1,931 772 12 0.58
11 163,354 1,927 796 72 0.6
4 164,865 1,626 605 ‐59 0.95
2 167,344 1,687 666 ‐37 0.84
8 180,782 1,842 715 22 0.78
22 198,299 1,802 662 ‐31 0.94
13 206,061 1,737 610 ‐51 1.1
23 209,621 2,150 660 ‐80 0.84
10 234,147 1,871 677 ‐43 1.05
18 251,165 2,199 866 19 0.75
26 286,009 2,239 851 65 0.85
12 300,383 2,244 836 ‐33 0.91
5 303,328 2,267 840 ‐31 0.9
15 341,414 2,368 865 ‐58 0.94
1 351,303 2,413 920 ‐30 0.9
6 462,435 2,742 1030 ‐44 0.93
24 464,613 3,119 1119 19 0.75
16 774,962 3,814 1472 47 0.78
28 818,208 4,106 1311 ‐81 0.86
25 1,264,481 4,561 1690 ‐24 0.93
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
• For a given wind speed, fetch length is the key parameter that 
controls the size of the waves generated in irrigation 
reservoirs.
• The orientation of the reservoir relative to the predominant 
wind direction has a strong influence on embankment erosion 
in irrigation reservoirs, such that, reducing the fetch length in 
the prevailing wind direction can significantly reduce 
embankment erosion. 
• Ongoing experimental research and reservoir assessment field 
studies will provide better information about the relations 
between the wave size and the erosion retreat rate.
Conclusions
69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational
Hydroscience and Engineering
The University of
Mississippi
Acknowledgments 
Carlos Alonso
USDA‐ARS National Sedimentation Lab. Oxford, MS (retired)
Denis Carman
White River Irrigation District, AR
Keith Admire
USDA‐NRCS National Water Management Center Little Rock, AR
Mustafa Altinakar
NCCHE, The University of Mississippi, Oxford, MS
Paul Work
USGS, Sacramento, CA
Technical support:
Glen Grey
Jacob Ferguson
Alan Barger

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Wind and wave measurments in irrigation reservoirs

  • 1. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Wind and Wave Measurements in  Irrigation Reservoirs Yavuz Ozeren National Center for Computational Hydroscience and Engineering The University of Mississippi, Oxford, MS Daniel Wren USDA‐ARS, National Sedimentation Laboratory, Oxford MS Michele Reba USDA‐ARS, Delta Water Management Research Unit, Jonesboro, AR
  • 2. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Introduction • The earthen embankments of these reservoirs  often experience significant erosion primarily  due to wind‐generated waves; therefore,  require annual repairs if they are not  protected.  • The design of effective embankment  protection requires knowledge of the wind‐ generated wave characteristics and their  relationship to embankment erosion.  • Irrigation reservoirs are commonly  used for irrigation water storage in  lower Mississippi river floodplain.   • A field measurement station was installed in an  irrigation reservoir near Harrisburg, AR, to  acquire synchronous measurements of wind and  wave properties along with levee erosion data. 
  • 3. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Field Site
  • 4. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Field Site • Wave staffs • Wind gauge • Erosion pins • Ground‐based LIDAR
  • 5. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi    0 )( dffSfm i i omo mH 004.4 Field Measurements An example time series water surface displacement data (June, 2012,  Jonesboro, AR).  The vertical axis is vertical water surface displacement. Five‐hour‐average energy spectrum of the  measured waves in July 19, 2012 Wave period, wave height and wind speed histograms for the  time period between June 2012 and October 2012.
  • 6. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Field Measurements Wave characteristics R26 (March 2005) R26 (June 2008) R27 (June 2012) Wind speed, U10 (m/s) 14 (NE) 13 (SW) 9.5 (S) Fetch length 586 450 470 Wave height, Hm0 (m) 0.25 0.23 0.14 Peak period, Tp (s) 1.7 1.6 1.4 Significant period, Ts (s) 1.7 1.6 1.2 Mean period, Tm (s) 1.4 1.4 1.1 Significant wave height, Hs (m) 0.23 0.20 0.13 Maximum wave height, Hmax (m) 0.38 0.39 0.24 RMS wave height, Hrms (m) 0.17 0.12 0.09 The ranges of measured wave parameters compared to field  measurements in 2005, 2008 and 2012.
  • 7. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi 44.0 22 0 0025.0          AA m U gF U gH 28.0 2 415.00          AA p U gF U gT Wave Prediction Method Hm0 (m) Tp (s) tmin (min) JONSWAP 0.11 1.1 15.2 Wilson (1965) 0.17 1.3 12.5 SMB, Bretschneider (1970) 0.19 1.7 9.4 Krylow (1976) 0.21 1.6 ‐ Donelan (1980) 0.16 1.4 10.3 Ozeren and Wren (2010) 0.14 1.3 11.8 Comparison of empirical wind wave prediction methods 72.0 2 min 087.42          AA U gF U gt
  • 8. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Erosion
  • 9. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Protection techniques
  • 10. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Floating Wave Barriers
  • 11. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Floating Wave Barriers
  • 12. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Floating Wave Barriers T = 0.6 s, H = 28 mm, h = 0.466m 2.00 2.24 2.48 2.72 2.96 3.20 x (m) 0.0 0.6 z (m) t=24.399208 s 2.00 2.24 2.48 2.72 2.96 3.20 x (m) t=24.598543 s Laboratory and numerical experiments Shafer lake (2005‐2009)
  • 13. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Shape and Orientation
  • 14. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Shape and Orientation Internal Levees (U = 10 m/s) Floating wave barriers (U = 10 m/s, Breakwater size =  0.5 m)
  • 15. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi LMRB
  • 16. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Irrigation  reservoir  (R) Area – A (m2 ) Levee  Length (m) Max. Fetch  – Fmax (m) Max. fetch  azimuth  (deg.) Shape  factor 17 116,500 1,336 483 ‐35 1.02 21 123,525 1,421 516 33 0.95 14 125,753 1,404 500 ‐47 1.01 20 126,755 1,377 510 49 1.02 19 128,328 1,411 510 43 1.01 7 132,719 1,422 508 ‐49 1.04 3 138,417 1,585 636 22 0.78 27 142,109 1,529 562 26 0.94 9 151,950 1,931 772 12 0.58 11 163,354 1,927 796 72 0.6 4 164,865 1,626 605 ‐59 0.95 2 167,344 1,687 666 ‐37 0.84 8 180,782 1,842 715 22 0.78 22 198,299 1,802 662 ‐31 0.94 13 206,061 1,737 610 ‐51 1.1 23 209,621 2,150 660 ‐80 0.84 10 234,147 1,871 677 ‐43 1.05 18 251,165 2,199 866 19 0.75 26 286,009 2,239 851 65 0.85 12 300,383 2,244 836 ‐33 0.91 5 303,328 2,267 840 ‐31 0.9 15 341,414 2,368 865 ‐58 0.94 1 351,303 2,413 920 ‐30 0.9 6 462,435 2,742 1030 ‐44 0.93 24 464,613 3,119 1119 19 0.75 16 774,962 3,814 1472 47 0.78 28 818,208 4,106 1311 ‐81 0.86 25 1,264,481 4,561 1690 ‐24 0.93
  • 17. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi • For a given wind speed, fetch length is the key parameter that  controls the size of the waves generated in irrigation  reservoirs. • The orientation of the reservoir relative to the predominant  wind direction has a strong influence on embankment erosion  in irrigation reservoirs, such that, reducing the fetch length in  the prevailing wind direction can significantly reduce  embankment erosion.  • Ongoing experimental research and reservoir assessment field  studies will provide better information about the relations  between the wave size and the erosion retreat rate. Conclusions
  • 18. 69th SWCS International Annual Conference, 27 - 30 July, 2014, Lombard, ILNational Center for Computational Hydroscience and Engineering The University of Mississippi Acknowledgments  Carlos Alonso USDA‐ARS National Sedimentation Lab. Oxford, MS (retired) Denis Carman White River Irrigation District, AR Keith Admire USDA‐NRCS National Water Management Center Little Rock, AR Mustafa Altinakar NCCHE, The University of Mississippi, Oxford, MS Paul Work USGS, Sacramento, CA Technical support: Glen Grey Jacob Ferguson Alan Barger