comparison of a pulsed doppler lidar with a 200 m met mast in complex terrain
DESCRIPTION
COMPARISON OF A PULSED DOPPLER LiDAR WITH A 200 M MET MAST IN COMPLEX TERRAIN. Tobias Klaas 1 , Doron Callies 1 Christoph Langenmayr 1 ,Lukas Pauscher 1 , Saskia Hagemann 1 , Zouhair Khadiri-Yazami 1 , Bernhard Lange 1 (1) Fraunhofer IWES, Kassel, Germany . Outline. - PowerPoint PPT PresentationTRANSCRIPT
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COMPARISON OF A PULSED DOPPLER LiDAR WITH A 200 M MET MAST IN
COMPLEX TERRAIN
Tobias Klaas1, Doron Callies1 Christoph Langenmayr1,Lukas Pauscher1, Saskia Hagemann1, Zouhair Khadiri-Yazami1, Bernhard Lange1 (1) Fraunhofer IWES, Kassel, Germany
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Outline
Measurement site at Rödeser Berg Site description, measurement campaign, data basis
LiDAR measurements in complex terrain Performance of LiDAR vs. mast measurements
Correction with WAsP Engineering and Meteodyn WT Predicted bias compared to measured difference
Virtual met mast Conclusion and Outlook
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Project „Utilization of Inland Wind Power“
Source: RP Kassel, 2012Source: Die Auswärtige Presse, 2011
Complex Terrain
Forest
New onshore windturbines
Mesoscale modelling
Project duration 2012 – 2014 Wind characteristics, LiDAR measurements, onshore wind energy
potential
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Measurement location in central Germany
Source: Google Earth
measurement site
Wind measurements in complex terrain at Rödeser Berg Typical wind farm location in central / south Germany
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Mast layout and specifications
200 m wind measurement mast in complex forested terrain
IEC conform booms with 5,40 m length, orthogonal to main wind direction
13 measurement heights
Co-located LiDAR measurements with LEOSPHERE Windcube WLS7 V1
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Measurement campaign and data processingMast - LiDAR comparison Measurement period: 21 Jan – 30 June 2012 Periods of icing were removed by visual comparison of heated
vs. unheated cups Invalid and/or physically unreasonable values were removed Measurements are compared at 120, 160 and 200 m
Mean wind profile Scatter plots and linear regression Diurnal pattern Directional dependence of bias
Due to terrain complexity and wind LiDAR measurement principle we expect significant bias.
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LiDAR availability with height
More than 80% of measured valuesin 10 minute averaging interval must be available
Periods of rain were removed
Availability decreases with height:
85 % at 135m 60 % at 200m
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LiDAR vs. mast measurements:Mean wind profile
Mean profile fits well, LiDAR shows small underestimation Strong effects from forest and terrain below 60m height
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LiDAR vs. mast measurements:scatter plot at 120 m and 200 m
Compared to flat terrain (Hovsøre) the scatter is significantly higher
Source: Gottschall, Courtney 2010
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LiDAR vs. mast measurements:Diurnal variation at different heights
Significant diurnal pattern at all heights Deviations between mast and LiDAR increase during nighttime
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LiDAR vs. mast measurements:Directional dependence at 120 m
only wind speeds > 4m s-1
Mean bias approx. between -4% and +2%
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only wind speeds > 4m s-1
LiDAR vs. mast measurements:Directional dependence at 120 m
Positive deviation for flow along the ridge
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LiDAR vs. mast measurements:Directional dependence at 120 m
Significant underestimation in main wind direction
only wind speeds > 4m s-1
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LiDAR vs. mast measurements:Directional dependence with height
Lightning rod
only wind speeds > 4m s-1
Shape and mean bias similar for all heights Height dependency of about 1%, depending on sector
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LiDAR correction with flow simulation LiDAR measurement bias is
mainly caused by flow inhomogeneity
Flow simulation can be used to assess the wind conditions and develop correction methods WAsP Engineering with
Bingöl‘s correction script Meteodyn WT and LiDAR
correction module
measurement site
main w
ind
dir.
Source: Bingöl 2009
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Comparison of different correction algorithms to measured bias
WEng estimation is much too high, but the pattern is reproduced Bias estimated by Meteodyn WT fits much better, but is slightly too
low
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Correction with Meteodyn WT:Predicted bias for three heights
Less symmetry in estimation due to CFD simulation Height-dependency of bias for certain sectors
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Three Windcube v1 LiDARs mounted on maneuverable tilting platforms
Focusing of the three laser beams on one point
Automatically measuring heights from 40m to 200m
Results were compared to the 200m mast at Rödeser Berg
Realization of a virtual met mast using three Pulsed Doppler LiDARs
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Conclusions
LiDAR shows error in complex terrain: Patterns follow orography, effects are site specific Deviation follows same pattern at all heights (up to 200m!) Deviations approx. between -4% and +2% Compensating effects in mean wind profile Deviations during night time
Meteodyn and WEng correction: Shape of predicted bias fits (fairly) well for both tools Bias predicted by WEng is much too high Very good reproduction of bias by Meteodyn WT
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Outlook
Detailed evaluation of flow models at complex site with mast data Different stabilities Different forest/roughness parameterization
LiDAR vs. Mast in complex terrain at several other complex sites More complex sites, more forested sites
Evaluation of different CFD-tools for LiDAR correction Meteodyn WT / WindSim / WEng / OpenFoam
3D-LiDAR experiments Detailed comparison of virtual vs. real met. mast
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M. Sc. Tobias [email protected]
Fraunhofer Institute for Wind Energy and Energy System Technology IWES Königstor 59, 34119 Kassel, Germany
Thank you for your attentionVisit us at stand B-B77!Do not miss our related posters and presentations: Pauscher, Lukas:
Wind over complex, forested terrain: First year of measurement with 200m research mastTuesday, 5 February 2013 , Room: LEHAR 2-4 , 11:00 - 12:30 Wind Resources - Moving the barriers (part 1)
Khadiri-Yazami, Zouhair: The realization of a Virtual met mast based on three Doppler wind LiDAR, Poster No. 404