Multiple 3-d Scanning Doppler Lidar and Wind Energy Resource Assessment Raghu Krishna Environmental Remote Sensing Group, Arizona State University

Multiple 3-d Scanning Doppler Lidar and Wind Energy Resource Assessment Raghu Krishna Environmental Remote Sensing Group, Arizona State University Co-...
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Multiple 3-d Scanning Doppler Lidar and Wind Energy Resource Assessment Raghu Krishna Environmental Remote Sensing Group, Arizona State University Co-Authors: Ronald Calhoun & Aditya Choukulkar, ASU Gregory S. Poulos, V-Bar, LLC Keith Barr, David Mcreavy LMCT, Inc.

AWEA Wind Resource Assessment Seminar September 13th, 2012

Multiple 3-d Scanning Doppler Lidar and Wind Energy Resource Assessment

• • • •

Scanning Doppler Lidar Overview Scanning Lidar for WERA Dual-Doppler Lidar for WERA Value proposition of 1 year lidar deployment integrated into WERA and P-Values

Scanning Lidar: Principles of Operation Doppler Lidar Characteristics

Beam is Scanned to Provide 2-3D Spatial Coverage

Return Light is Doppler Shifted Moving Aerosols

Nd-Yag laser

Operating Wavelength

1.6/2µm

Energy per pulse

2mJ

Pulse repetition Pulse Envelope (50 – 80 m) frequency

50 – 80 m Pulse transmitted 500 times a second

‘Pencil’ Beam Width 10 – 30 cm

Doppler Doppler LIDAR Lidar

Transmitter

Portion of Scattered Light Collected By Transmit/Receive Telescope

Relative wind induces a Doppler frequency shift in the backscatter light; This frequency shift is detected by the sensor

Data Rate

5 Hz

Range resolution

~ 50 - 100 m

Min range

436 m

Max range

10/15 km

vr ( R, , )  U sin  cos  V cos cos W sin  Vr =Radial Velocity, ϕ = Azimuth Angle , θ = Elevation angle U, V, W = Components of wind speed

500 Hz

“LASER”

Scanning Lidar for WERA Terrain-following Surface 1hour RMS Difference

Mean (ms-1) 9.67 9.61

Instrument Tower @ 50 m Lidar @ 50 m

(ms-1) 0.72

1 hour RMS Difference

Mean Instrument Tower @ 50 m Lidar @ 50 m Wind speed RMS difference @ 50 m

(deg) 168.24 170.34

10 minute RMS (ms-1) 1.18

1 Hour RMS (ms-1) 0.72

(deg) 9.20

24 hour RMS (ms-1)

0.46

94% Correlation of wind speed Distance between tower and lidar – 3.2 km Krishnamurthy et al. 2012

Single Doppler Lidar Challenges vr ( R, , )  U sin  cos  V cos cos W sin  1. Why does lidar retrieval accuracy reduce in the off-mean wind direction? Radial velocity ~ 0 – No new information is provided! 2. What is the retrieval accuracy in the off-mean wind direction?

Conditional analysis with tower measurements shows correlation of 90% in wind speed. Krishnamurthy et al. 2012

Vr =Radial Velocity, θ = Elevation angle, ϕ = Azimuth Angle U, V, W = Components of wind speed

Dual-Doppler for Wind Energy Resource Assessment v

vr_L1

u u

Y • Intersecting lidar beams for 3-d wind vector •Sample – 250 MW Wind Farm • No. of Turbines – 125 • Rotor Diameter (RD) – 80m

vr_L2

X

• Spacing – Prevailing mean wind direction – 13 RD Off - mean wind direction – 3.5 RD Wind Farm Coverage – 14 km x 3 km

• Hub-height winds for 90% of the wind farm – ~42 sq km • Winds speed spatial accuracy – ~100 m

L2 15 km

L1

Dual-Doppler Lidar • Why? – – – – – –

Higher confidence in velocity retrievals Reduces directional dependence Measured hub-height winds at nearly all turbine locations Turbulence parameters (u* , σu ,σv ,σw , u' w',v' w' etc.) Input to mesoscale models – data assimilation Can track atmospheric events – harmful to turbines

• Challenges – Synchronizing lidar beams from two instruments – Pointing accuracy and complex terrain blockage/placement Newsom et al. 2005, Calhoun et al. 2006, Krishnamurthy et al. 2010

Value Proposition of Dual-Doppler Lidar in Wind Energy Resource Assessment 90% wind farm area dual-Doppler coverage at hub height • Cost of dual 3-d Doppler lidar deployment for 1 year: ~$1.5 M • ROI for a 250MW Wind Farm with 60-m towers? Uncertainty

60-m Towers a

dual 3-d Doppler

Shear

2%

0.25%

Micro-siting

6%

2%

a

Lower range of uncertainty estimates Other uncertainties in P-value calculation remain the same

95% Confidence limits

P95/P50 ratio

P95 Production (D )

20 Year NPV (@$60/ MWh)

ROI

1 Year

Drops ~250 basis points

D 0.781 to 0.801

17,500 MWh

~ 9.4 M

~650%

20 Year

Drops ~400 basis points

D 0.852 to 0.883

27,500 MWh

~ 14.8 M

~1000%

Depends on your wind farm’s financing terms

Dual-Doppler to Track & Quantify Harmful Atmospheric Events

L1

15 km

L2

2.9 km

• Coplanar scans along 80 degree azimuth • Height difference between Lidars • Validation - Pointing accuracy Hill et al. 2009

15 km

Dual-Doppler to Track & Quantify Harmful Atmospheric Events Colors – Vorticity (s-1); Contour – Swirl Strength; Arrows – Wind Direction

Lidar can quantify: a. Vorticity b. Sub-rotors c. Dissipation rate Turbine not to scale

Hill et al. 2009

Scanning Lidar’s Tool or Toy? • Scientific advantage over towers for WERA? – Large spatial extent coverage – reduces micro-siting uncertainty – Dual-Doppler – Higher retrieval accuracy – Dual-Doppler – reduces directional challenges

• Financially viable or good ROI? – Uncertainty reduction by ~ 4% in WERA – 5x or 10x ROI for a 250MW wind farm

• Year long dual-Doppler lidar deployment is promising both financially and scientifically amidst PTC uncertainty!

Questions?

References Choukulkar, A., 2012: A Modified Optimal Interpolation Technique for Vector Retrieval for Coherent Doppler Lidar. IEEE GeoScience and remote sensing letters. Krishnamurthy, R et al., 2012: Coherent Doppler lidar for wind farm characterization. Wind Energy, doi: 10.1002/we.539 Krishnamurthy, R. 2011: Wind Turbulence Estimates in a Valley by Coherent Doppler Lidar, Meteo. App, doi: 10.1002/met.263. Hill, M et al., 2010: Coplanar Doppler Lidar Retrieval of Rotors from T-REX. J. Atmos. Sci., 67, 713–729.

Calhoun, R 2006: Virtual towers using coherent Doppler lidar during the Joint Urban 2003 Experiment, J. App. Meteo. Newsom et al. 2005: Linearly Organized Turbulence Structures Observed over a suburban area by dual-Doppler lidar, Bound. Layer. Meteo. Boccippio, D 1995: A diagnostic analysis of the VVP single-Doppler retrieval technique, J. Atmos. Ocean Tech Browning and Wexler, 1968: The determination of kinematic properties of a wind field using Doppler radar. J. Appl. Meteor.

Email: Raghu.Krishna@ asu.edu Contact: 480-234-4807

http://more.engineering.asu.edu/windlab/

Additional Slides

Dual-Doppler Lidar “Virtual Towers”

Cautions:  Height difference between Lidar’s should be taken into account  Pointing accuracy Calhoun et al. 2006,

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