The OWEZ Meteorological Mast

Size: px
Start display at page:

Download "The OWEZ Meteorological Mast"

Transcription

1 The OWEZ Meteorological Mast Analysis of mast-top displacements P.J. Eecen E. Branlard ECN-E OWEZ_R_121_mast_top_movement

2 Acknowledgement/Preface The Off Shore wind Farm Egmond aan Zee has a subsidy of the Ministry of Economic Affairs under the CO2 Reduction Scheme of the Netherlands Abstract NoordzeeWind carries out an extensive measurement and evaluation program as part of the OWEZ project. The technical part of the measurement and evaluation program considers topics as climate statistics, wind and wave loading, detailed performance monitoring of the wind turbines, etc. The meteorological measurements at the 116m high meteorological mast at the location of the wind farm are published on the project website and are widely used. Data at measurement sample frequency have been stored since May 2007 and recently have become available. From the acceleration measurements at the mast top, the displacements are reconstructed and the effect of these movements on the uncertainty of the wind speed measurements are estimated. From the acceleration measurements it is found that the influence of the mast-top movements on the wind speed measurements is limited and smaller than the flow distortion of the mast itself. The project is carried out under assignment of NoordzeeWind BV. Principal NoordzeeWind Henk Kouwenhoven p.a. Shell Wind Energy BV Postbus BN Amsterdam Project information Contract number NZW-16-C-2-R01 ECN project number: ECN-E

3 Contents List of tables 4 List of figures 4 1. Introduction 5 2. Measured data Meteorological mast Sensor calibration Data validation 7 3. Interpretation of the acceleration data Selecting the data Overview of the data 9 4. Analysis of the Acceleration Measurements Estimate of the typical frequency Estimate of the speed and displacement amplitudes Results Effects of the mast-top motion on the measurements Comparison to other disturbances Conclusions References 21 ECN-E

4 List of tables Table 2.1 Coordinates of the meteorological mast at OWEZ... 7 Table 3.1 Date and time of the samples selected for each wind speed bin and for a wind direction around Table 3.2 Date and time of the samples selected for each wind speed bin and for a wind direction around Table 4.1 Frequency and maximum acceleration amplitude of the EW acceleration signal for each selected period are presented together with the maximum speed and displacement of the mast-top in the EW direction Table 4.2 Frequency and maximum acceleration amplitude of the NS acceleration signal for each selected period are presented together with the maximum speed and displacement of the mast-top in the NS direction Table 5.1 The maximum mast-top velocities and the ratio between the maximum mast-top velocity and the ambient wind speed List of figures Figure 1.1 The meteorological mast (right) at the time of installation of the wind turbines of the OWEZ wind farm Figure 1.2 The meteorological mast at the OWEZ wind farm... 6 Figure 2.1 Schematic drawing of the meteorological mast... 8 Figure 3.1 Acceleration measurements in the two directions EW and NS in the 10 minutes sample corresponding to a wind speed of 12 m/s and a wind direction of 206 ( , 10:50) Figure 3.2 EW acceleration data during a 1-minute period. The main oscillation frequency of 4Hz (T=2.5s) is readily observed Figure 4.1 Detailed fragment of the measured acceleration data and its sine estimate. The sine amplitude corresponds to the maximum amplitude of the acceleration signal in the 10 minutes period Figure 4.2 Typical Fourier spectrum of an acceleration signal Figure 4.3 Main frequency of the acceleration signal for the different samples where the wind direction is around 235 degrees Figure 4.4 Main frequency of the acceleration signal for the different samples where the wind direction is around 15 degrees Figure 4.5 Effect on integration on the amplitude of the signal with amplitude 0.06 m/s2 and frequency 0.4 Hz Figure 5.1 : Maximum acceleration amplitude as function of wind speed for the EW and NS acceleration measurements for wind directions around 235 degrees Figure 5.2 Maximum acceleration amplitude as function of wind speed for the EW and NS acceleration measurements for wind directions around 15 degrees Figure 5.3 Amplitude of the speed obtained by integration of the maximum acceleration estimation Figure 5.4 Ratios between anemometer readings mounted on the South (S), North-West (NW) and North-East (NE) booms of the meteorological mast. The wind speed ratios NW/NE are indicated in green, the ratios NE/S are indicated in blue and the ratios S/NW are indicated in red. The indicated wind direction along the horizontal axis is the derived wind direction as described in section Wind speeds above 4m/s have been selected ECN-E

5 1. Introduction NoordzeeWind carries out an extensive measurement and evaluation program (NSW-MEP) as part of the OWEZ project. NoordzeeWind contracted Bouwcombinatie Egmond (BCE) to build and operate an offshore meteorological mast at the location of the OWEZ wind farm. BCE contracted Mierij Meteo to deliver and install the instrumentation in the meteorological mast. After the data have been validated, BCE delivers the measured 10-minute statistics data to NoordzeeWind. ECN created a database under assignment of NoordzeeWind and fills the database with the delivered data. The technical part of the measurement and evaluation program considers topics as climate statistics, wind and wave loading, detailed performance monitoring of the wind turbines, etc. Before installation of the wind farm, a 116m high meteorological mast has been installed to measure the wind conditions. During this period, wind conditions are measured that are not disturbed by a nearby wind farm. This mast is in operation since the summer of After realisation of the wind farm, the mast has also been used to, among others, measure wind conditions in the wake of turbines and perform mechanical load and power performance measurements. The measurements at the 116m high mast are part of NSW-MEP tasks and and are reported in half-year reports [3-7]. An important design parameter of the meteorological mast is to limit the displacements of the mast-top. If the mast-top would have large deflections and associated speeds, the wind speed measurements could be disturbed. An earlier analysis has been performed [8, 9], but at that time, the data at measurement sample frequency were not available. Therefore, the analysis was limited. Since May 2007 the data at measurement sample frequency of the mast are stored and recently these have become available. These data are used to assess the displacements of the mast-top as function of wind speed. From the movement the effect on the accuracy of the wind speed measured at the mast-top is estimated. For this purpose the acceleration measurements are used. Figure 1.1 The meteorological mast (right) at the time of installation of the wind turbines of the OWEZ wind farm. ECN-E

6 Figure 1.2 The meteorological mast at the OWEZ wind farm. 6 ECN-E

7 2. Measured data 2.1 Meteorological mast The meteorological mast is a lattice tower with booms at three heights: 21m 70m and 116m above mean sea level (MSL). At each height, three booms are installed in the directions northeast (NE), south (S) and north-west (NW) [1]. Sensors attached to the meteorological mast are described in [2]. The location of the meteorological mast is given in Table 2.1. Table 2.1 Coordinates of the meteorological mast at OWEZ UTM31 ED50 WGS 84 x º23'22,7'' EL y º36'22,9'' NB The instrumentation is described in a report [1]. The data are reported in half-year reports [3-7]. 2.2 Sensor calibration The applied sensors in the meteorological mast are calibrated according to maintenance schedules of BCE (Mierij Meteo). The cup anemometers are calibrated at DEWI Germany. BCE (Mierij Meteo) calibrates the other sensors. The calibration constants are applied to the data during the stage of data processing at BCE (Mierij Meteo). It must be noted that the 10-minute statistics are calibrated; the 4Hz data do not have all calibration constants applied. 2.3 Data validation In the measuring period, defective sensors or cables or other malfunctioning of the measurement system can corrupt the measured data. For this reason, BCE (Mierij Meteo) validates all measured data [4]. The quality and consistency of the data is assessed by means of manual check of the received data on 1. Consistency 2. Out of range numbers 3. Followed by marking of incorrect and unavailable records Corrupt or missing data fields are marked by error values ( ). Mierij Meteo has specified that the acceleration measurements have a sample frequency of 32Hz. However, from the data it is found that the sample frequency for the acceleration data is 33Hz. In the analyses described in this report, the 33Hz sample frequency is used. ECN-E

8 Figure 2.1 Schematic drawing of the meteorological mast 8 ECN-E

9 3. Interpretation of the acceleration data 3.1 Selecting the data The analysis presented in this report is based on the data from the acceleration sensors in the top of the meteorological mast and from the anemometer and vane of the NW boom at 116m. Wind data are sampled at 4Hz, whereas the acceleration data are sampled at 33Hz. From the validated 10 minutes statistics values (that are also publicly available at interesting time series are selected for further analysis. Data from two wind directions (WD) and various values for the wind speed are selected. These wind directions are around 15 and 235 with respect to North and wind speed is selected based on 2m/s bin values. For each wind speed bin, and each wind direction, a single sample of 10 minutes length was selected. The selected 10-minute periods are presented in Table 3.1 and Table 3.2. Table 3.1 Date and time of the selected samples for each wind speed bin for a wind direction around 235. WS Date Time 4 May :50 6 May :20 8 May :10 10 May :30 12 May :50 14 May :50 16 May :40 18 May :20 20 May :10 Table 3.2 Date and time of the selected samples for each wind speed bin for a wind direction around 15. WS Date Time 4 May :30 6 May :00 8 May :50 10 May :30 12 May : Overview of the data After selecting the interesting dates and times from the 10 minutes statistics database, the relevant 33Hz acceleration data samples are extracted. The acceleration sensor provides two signals corresponding to the acceleration in the North-South (NS) direction and in the East-West (EW) direction. Examples of the data are presented in Figure 3.1. A first glance at the acceleration data (Figure 3.1) leads to the following observations: The sensors have an offset of about 0.3m/s 2. Since the mast is fixed, the data should be centred around zero and this is clearly an offset due to measurement uncertainties. This offset is removed by subtracting the mean to each data series. The acceleration data at 33Hz have discrete values. However, the accelerations are large enough to be able to perform the analyses. By zooming on the time series (cf. Figure 3.2), it clearly appears that the acceleration oscillates with a frequency almost constant with time. This main frequency is approximately 0.4Hz (T = 2.5s). ECN-E

10 Figure 3.1 Acceleration measurements in the two directions EW and NS in the 10 minutes sample corresponding to a wind speed of 12 m/s and a wind direction of 206 ( , 10:50). Figure 3.2 EW acceleration data during a 1-minute period. The main oscillation frequency of 4Hz (T=2.5s) is readily observed. 10 ECN-E

11 4. Analysis of the Acceleration Measurements In order to asses the speed and movements of the mast-top for the various wind speeds and wind directions, a relatively straight-forward model is applied. The following procedure is applied to estimate the maximum amplitude of the mast-top oscillation. For each sample, the model of the acceleration consists of a sinusoidal function with the same frequency as the measured data and with an amplitude equal to the maximum of the acceleration signal in the entire 10 minute sample. This leads to an over-estimate of the values for the speed and displacement. This is the preferred approach. Figure 4.1 Detailed fragment of the measured acceleration data and its sine estimate. The sine amplitude corresponds to the maximum amplitude of the acceleration signal in the 10 minutes period. ECN-E

12 4.1 Estimate of the typical frequency For each 10-minte period (see Table 3.1 and Table 3.2) and for each signal (NS/EW), the main oscillation frequency is obtained by determining the abscissa of the maximum Fourier spectrum component of the measured acceleration data. Figure 4.2 Typical Fourier spectrum of an acceleration signal. The frequencies of each selected period are very similar as is illustrated in Figure 4.3 and Figure 4.4. For the different wind speeds and wind directions, the range of frequencies is [0.398 Hz; Hz]. As is clearly shown, there is no obvious dependency of the mast-top movement frequency on the wind speed and wind direction. 12 ECN-E

13 0,42 Main frequency of the different acceleration samples Wind direction around 235 degrees Acceleration frequency [Hz] 0,41 0,40 EW main frequency NS main frequency 0, WS [m/s] Figure 4.3 Main frequency of the acceleration signal for the different samples where the wind direction is around 235 degrees. 0,42 Main frequency of the different acceleration samples Wind direction around 15 degrees Acceleration frequency [Hz] 0,41 EW main frequency NS main frequency 0, WS [m/s] Figure 4.4 Main frequency of the acceleration signal for the different samples where the wind direction is around 15 degrees. ECN-E

14 4.2 Estimate of the speed and displacement amplitudes From the acceleration measurements, the speed and position of the mast-top in each direction are obtained analytically by integrating the estimated acceleration. If A is the maximum acceleration amplitude in the x direction (EW direction), and f the main frequency of the acceleration for the studied sample, the acceleration & x&, the speed x& and displacement x are: && x = Asin(2πf t) A x& = cos(2πf t) 2πf A x = 4π f sin(2πf ) t 2 2 The same results with different frequency, amplitude and phase are obtained in the other direction (NS direction). For all the samples the frequency is close to 0.4 Hz, and as a result 1 / 2π f < 1, which leads to a decrease of amplitude at each integration. As a result of this, by defining A as the maximum amplitude of the acceleration, both the speed and the position of the mast are over-estimated. Figure 4.5 illustrates this decrease in amplitude for an acceleration signal of amplitude 0.06 m/s 2. Figure 4.5 Effect on integration on the amplitude of the signal with amplitude 0.06 m/s2 and frequency 0.4 Hz. 14 ECN-E

15 Table 4.1 Frequency and maximum acceleration amplitude of the EW acceleration signal for each selected period are presented together with the maximum speed and displacement of the mast-top in the EW direction. Wind Direction Wind Speed Acceleration frequency Acceleration Amplitude Speed Amplitude Displacement Amplitude [degree] [m/s] [Hz] [m/s/s] [m/s] [m] 17,0 4,4 0,415 0,057 0,022 0,008 20,2 6,3 0,414 0,055 0,022 0,009 16,1 8,0 0,408 0,086 0,034 0,013 28,7 10,2 0,411 0,122 0,048 0, ,0 12,0 0,408 0,148 0,058 0, ,2 6,1 0,408 0,111 0,043 0, ,6 8,0 0,398 0,126 0,050 0, ,2 10,2 0,399 0,206 0,082 0, ,6 12,2 0,414 0,144 0,056 0, ,6 14,3 0,405 0,164 0,064 0, ,1 16,3 0,407 0,326 0,128 0, ,3 18,3 0,410 0,252 0,098 0, ,5 20,0 0,407 0,377 0,151 0,060 Table 4.2 Frequency and maximum acceleration amplitude of the NS acceleration signal for each selected period are presented together with the maximum speed and displacement of the mast-top in the NS direction. Wind Direction Wind Speed Acceleration frequency Acceleration Amplitude Speed Amplitude Displacement Amplitude [degree] [m/s] [Hz] [m/s/s] [m/s] [m] 17,0 4,4 0,411 0,048 0,019 0,007 20,2 6,3 0,401 0,048 0,019 0,008 16,1 8,0 0,406 0,099 0,039 0,015 28,7 10,2 0,401 0,188 0,075 0, ,0 12,0 0,409 0,210 0,082 0, ,2 6,1 0,408 0,070 0,027 0, ,6 8,0 0,404 0,129 0,051 0, ,2 10,2 0,403 0,196 0,077 0, ,6 12,2 0,409 0,112 0,043 0, ,6 14,3 0,406 0,119 0,047 0, ,1 16,3 0,405 0,251 0,099 0, ,3 18,3 0,408 0,251 0,098 0, ,5 20,0 0,398 0,375 0,150 0,060 ECN-E

16 5. Results In the model previously described, the acceleration is fitted with a sine with amplitude equal to the maximum amplitude of the measured acceleration signal and with a fixed frequency. The latter is due to the fact that the frequency is not dependent on the wind speed and it can be assumed that the frequency of the mast-top movements is constant. Consequently, speed and position linearly depend on the acceleration. For this reason, if a correlation holds for acceleration, it also holds for the speed and the displacement of the mast-top. For each 10-minte period (see Table 3.1 and Table 3.2), the maximum amplitude of the measured acceleration is calculated. These amplitude values are presented in Figure 5.1 and Figure 5.2 as function of the averaged wind speed. Figure 5.1 and Figure 5.2 show that the maximum acceleration amplitude is a function of the ambient wind speed. With increasing wind speed, the frequency of the mast-top oscillating motion does not change, but the accelerations increase. Moreover, a similar trend is followed by both EW and NS components of the acceleration measurements. The two curves are quite similar. This means that the displacements in both directions are equally sensitive to a change of wind speed and thus evolve in the same order. In Figure 5.3 the maximum speed of the mast-top movements corresponding to the accelerations presented in Figure 5.1 and Figure 5.2 are presented. From Figure 5.3 it is concluded that at a given wind speed and direction, the mast speed (and thus, the mast displacement) in the EW direction is larger than in the NS direction. This might be correlated with the mast structure and main structural directions that play a role on the mast stiffness but it is not within the scope of this report. 16 ECN-E

17 Acceleration amplitude [m/s/s] - 0,40 0,35 0,30 0,25 0,20 0,15 0,10 0,05 0,00 Acceleration : maximum amplitude of the different samples Wind direction around 235 degrees EW acceleration NS Acceleration WS [m/s] Figure 5.1 : Maximum acceleration amplitude as function of wind speed for the EW and NS acceleration measurements for wind directions around 235 degrees. Acceleration amplitude [m/s/s] - 0,40 0,35 0,30 0,25 0,20 0,15 0,10 0,05 0,00 Acceleration : maximum amplitude of the different samples Wind direction around 15 degrees EW Acceleration NS Acceleration WS [m/s] Figure 5.2 Maximum acceleration amplitude as function of wind speed for the EW and NS acceleration measurements for wind directions around 15 degrees. ECN-E

18 Speed after integrating the estimated acceleration Speed amplitude [m/s] 0,16 0,14 0,12 0,10 0,08 0,06 0,04 0,02 0,00 EW-135 EW-235 NS-135 NS WS [m/s] Figure 5.3 Amplitude of the speed obtained by integration of the maximum acceleration estimation. 5.1 Effects of the mast-top motion on the measurements The motion of the mast-top will have the largest effect on the measurements of wind speed. The motion of the mast-top will add an oscillating speed to the ambient wind speed. In this section, an estimate is presented of the uncertainty of the wind speed measurement due to the oscillating movements of the mast-top. For each 10-minute period that has been studied, the largest effects are selected, so that in a sense, an overestimate is presented here. The largest speeds of the mast-top are associated with the EW movements, at an ambient wind direction of 235 degrees (see Figure 5.3). An estimate of the effect on the scalar wind speed measurements is to assume the EW and NS components of the mast speed to be equal: V mast 2 EW 2 NS = V + V 2 V EW. The ratio is defined between the mast speed and the ambient wind speed, which is an indication for the relative influence of the mast-top movements on the wind speed measurements. The results are presented in Table 5.1. The result of the analysis presented here is that (shown in Table 5.1) the disturbance of the mast-top movement on the measured wind speed does not exceed 1.1%. 18 ECN-E

19 Table 5.1 The maximum mast-top velocities and the ratio between the maximum mast-top velocity and the ambient wind speed. Mast-top velocity EW (max) Mast-top velocity NS (max) Wind Speed [m/s] [m/s] [m/s] [-] 6,1 0,04 0,06 0,010 8,0 0,05 0,07 0,009 10,2 0,08 0,12 0,011 12,2 0,06 0,08 0,007 14,3 0,06 0,09 0,006 16,3 0,13 0,18 0,011 18,3 0,10 0,14 0,008 20,0 0,15 0,21 0,011 Speed Ratio V mast /WS 5.2 Comparison to other disturbances The largest other effect on the measured wind speed is the disturbance of the mast itself. From other reports it is known that the disturbance of the mast is significant. This is illustrated in Figure 5.4, where the ratios between anemometer readings mounted on the South (S), North- West (NW) and North-East (NE) booms of the meteorological mast are presented (taken from other report [7]). The typical disturbance at 116m height is 3% (excluding the anemometer measurements in the wake of the mast). In that respect, the mast motion will have a small contribution to the measurement uncertainty of the wind speed. ECN-E

20 Figure 5.4 Ratios between anemometer readings mounted on the South (S), North-West (NW) and North-East (NE) booms of the meteorological mast. The wind speed ratios NW/NE are indicated in green, the ratios NE/S are indicated in blue and the ratios S/NW are indicated in red. The indicated wind direction along the horizontal axis is the derived wind direction as described in section Wind speeds above 4m/s have been selected. 20 ECN-E

21 6. Conclusions The data at higher sample rate have recently become available in the MEP-NSW project. The acceleration data available at 33Hz have been investigated to assess the displacements of the mast-top and the associated velocities. The effect of the mast movements on the measured wind speed has been assessed and it is found that a limited effect of maximum 1.1% is found. Compared to the influence of the flow distortion of the mast itself which is in the order of 3%, the mast movement effects are insignificant. 7. References 1. H.J. Kouwenhoven, User manual data files meteorological mast NoordzeeWind, Document code: NZW-16-S-4-R03, Date: 1 October 2007, 2. BCE (Mierij Meteo), sensor overview, OWEZ document 3672-OV 3. P.J. Eecen, L.A.H. Machielse, A.P.W.M. Curvers, Meteorological Measurements OWEZ, Half year report ( ), ECN-E P.J. Eecen, L.A.H. Machielse, A.P.W.M. Curvers, Meteorological Measurements OWEZ, Half year report ( ), ECN-E P.J. Eecen, L.A.H. Machielse, A.P.W.M. Curvers, Meteorological Measurements OWEZ, Half year report ( ), ECN-E P.J. Eecen, L.A.H. Machielse, A.P.W.M. Curvers, Meteorological Measurements OWEZ, Half year report ( ), ECN-E P.J. Eecen, Meteorological Measurements OWEZ, Half year report ( ), ECN-E A.J. Brand and J.J. Heijdra, Kwantificeren invloed mastbeweging op gemeten windsnelheid, 17 oktober 2001, internal ECN communication 9. P.J. Eecen, Analysis of mast movements, note to project manager MEP-NSW, ECN-E

Meteorological Measurements OWEZ

Meteorological Measurements OWEZ Meteorological Measurements OWEZ Half year report 01-01-2008-30-06-2008 H. Korterink P.J. Eecen ECN-E--08-062 OWEZ_R_121_20080101-20080630_wind_resource_2008_1 Abstract NoordzeeWind carries out an extensive

More information

Meteorological Measurements OWEZ

Meteorological Measurements OWEZ Meteorological Measurements OWEZ Half year report - 01-07-2008-31-12-2008 H. Korterink P.J. Eecen J.W. Wagenaar ECN-E--09-018 OWEZ_R_121_20080701-20081231_WIND_RESOURCE_2008_2 Abstract NoordzeeWind carries

More information

3D Turbulence at the Offshore Wind Farm Egmond aan Zee J.W. Wagenaar P.J. Eecen

3D Turbulence at the Offshore Wind Farm Egmond aan Zee J.W. Wagenaar P.J. Eecen 3D Turbulence at the Offshore Wind Farm Egmond aan Zee J.W. Wagenaar P.J. Eecen OWEZ_R_121_3Dturbulence_20101008 ECN-E--10-075 OCTOBER 2010 Abstract NoordzeeWind carries out an extensive measurement and

More information

Flow analysis with nacellemounted

Flow analysis with nacellemounted Flow analysis with nacellemounted LiDAR E.T.G. Bot September 2016 ECN-E--16-041 Acknowledgement The work reported here is carried out in the TKI LAWINE project which is partially funded by the Dutch government

More information

7 th International Conference on Wind Turbine Noise Rotterdam 2 nd to 5 th May 2017

7 th International Conference on Wind Turbine Noise Rotterdam 2 nd to 5 th May 2017 7 th International Conference on Wind Turbine Noise Rotterdam 2 nd to 5 th May 2017 Sound power level measurements 3.0 ir. L.M. Eilders, Peutz bv: l.eilders@peutz.nl ing. E.H.A. de Beer, Peutz bv: e.debeer@peutz.nl

More information

Torrild - WindSIM Case study

Torrild - WindSIM Case study Torrild - WindSIM Case study Note: This study differs from the other case studies in format, while here another model; WindSIM is tested as alternative to the WAsP model. Therefore this case should be

More information

WIND DATA REPORT. Paxton, MA

WIND DATA REPORT. Paxton, MA WIND DATA REPORT Paxton, MA July 1, 2011 September 30, 2011 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Eric Morgan James F. Manwell Anthony F. Ellis

More information

FINO1 Mast Correction

FINO1 Mast Correction FINO1 Mast Correction A. Westerhellweg, T. Neunn; DEWI GmbH, Wilhelmshaven V. Riedel; DEWI North America Inc. A. Westerhellweg English Abstract Lateral speed-up effects, upwind flow retardation and downwind

More information

Available online at ScienceDirect. Energy Procedia 53 (2014 )

Available online at   ScienceDirect. Energy Procedia 53 (2014 ) Available online at www.sciencedirect.com ScienceDirect Energy Procedia 53 (2014 ) 156 161 EERA DeepWind 2014, 11th Deep Sea Offshore Wind R&D Conference Results and conclusions of a floating-lidar offshore

More information

Nanortalik A preliminary analysis of the wind measurements rev 1

Nanortalik A preliminary analysis of the wind measurements rev 1 Nanortalik A preliminary analysis of the wind measurements rev 1 Introduction Note pr 14.08.2009 Tove Risberg, Kjeller Vindteknikk AS A 50 m met mast has been measuring the wind speed at Nanortalik Heliport

More information

Validation of Measurements from a ZephIR Lidar

Validation of Measurements from a ZephIR Lidar Validation of Measurements from a ZephIR Lidar Peter Argyle, Simon Watson CREST, Loughborough University, Loughborough, United Kingdom p.argyle@lboro.ac.uk INTRODUCTION Wind farm construction projects

More information

WIND DATA REPORT. Paxton, MA

WIND DATA REPORT. Paxton, MA WIND DATA REPORT Paxton, MA September 1 2003 November 30 2003 by James F. Manwell Anthony F. Ellis Kai Wu April 15, 2004 Renewable Energy Research Laboratory 160 Governors Drive, www.ceere.org/rerl (413)

More information

Hollandse Kust (zuid) Wind resource assessment. 17 January 2017 Anthony Crockford

Hollandse Kust (zuid) Wind resource assessment. 17 January 2017 Anthony Crockford Hollandse Kust (zuid) Wind resource assessment 17 January 2017 Overview > Introduction > Wind measurements > Mesoscale model > Calculation of wind climate > Comparisons > Conclusions 2 ECOFYS WTTS 17/01/2017

More information

Gravity wave effects on the calibration uncertainty of hydrometric current meters

Gravity wave effects on the calibration uncertainty of hydrometric current meters Gravity wave effects on the calibration uncertainty of hydrometric current meters Marc de Huu and Beat Wüthrich Federal Office of Metrology METAS, Switzerland E-mail: marc.dehuu@metas.ch Abstract Hydrometric

More information

Scoping analysis of the potential yield of the Hollandse Kust (noord) wind farm and the influence on the existing wind farms in the proximity

Scoping analysis of the potential yield of the Hollandse Kust (noord) wind farm and the influence on the existing wind farms in the proximity Scoping analysis of the potential yield of the Hollandse Kust (noord) wind farm and the influence on the existing wind farms in the proximity B.H. Bulder E.T.G. Bot G. Bedon April 2018 ECN-E--18-033 Executive

More information

Scoping analysis of the potential yield of the Hollandse Kust (zuid) wind farm sites and the influence on the existing wind farms in the proximity

Scoping analysis of the potential yield of the Hollandse Kust (zuid) wind farm sites and the influence on the existing wind farms in the proximity Scoping analysis of the potential yield of the Hollandse Kust (zuid) wind farm sites and the influence on the existing wind farms in the proximity B.H. Bulder E.T.G. Bot A.J Marina August 2016 ECN-E--16-021

More information

EWTW Meteorological database

EWTW Meteorological database ECN-I--05-007 EWTW Meteorological database Description June 2003 - May 2005 P.J. Eecen M. de Noord JUNE 2005 ECN-I--05-007 1 Abstract The ECN Wind Turbine Test Station Wieringermeer (EWTW) is a test location

More information

Special edition paper

Special edition paper Development of a Track Management Method for Shinkansen Speed Increases Shigeaki Ono** Takehiko Ukai* We have examined the indicators of appropriate track management that represent the ride comfort when

More information

HOUTEN WIND FARM WIND RESOURCE ASSESSMENT

HOUTEN WIND FARM WIND RESOURCE ASSESSMENT CIRCE CIRCE Building Campus Río Ebro University de Zaragoza Mariano Esquillor Gómez, 15 50018 Zaragoza Tel.: 976 761 863 Fax: 976 732 078 www.fcirce.es HOUTEN WIND FARM WIND RESOURCE ASSESSMENT CIRCE AIRE

More information

WIND DATA REPORT. Ragged Mt Maine

WIND DATA REPORT. Ragged Mt Maine WIND DATA REPORT Ragged Mt Maine December 1 st 2007 to February 29 th 2007 by James R. Browning James F. Manwell Utama Abdulwahid Anthony F. Ellis April 10, 2008 Report template version 3.1 Renewable Energy

More information

Executive Summary of Accuracy for WINDCUBE 200S

Executive Summary of Accuracy for WINDCUBE 200S Executive Summary of Accuracy for WINDCUBE 200S The potential of offshore wind energy has gained significant interest due to consistent and strong winds, resulting in very high capacity factors compared

More information

Measurement and simulation of the flow field around a triangular lattice meteorological mast

Measurement and simulation of the flow field around a triangular lattice meteorological mast Measurement and simulation of the flow field around a triangular lattice meteorological mast Matthew Stickland 1, Thomas Scanlon 1, Sylvie Fabre 1, Andrew Oldroyd 2 and Detlef Kindler 3 1. Department of

More information

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks LONG TERM SITE WIND DATA QUARTERLY REPORT Bishop and Clerks April 1, 2012 June 30, 2012 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Frederick Letson James

More information

Remote sensing standards: their current status and significance for offshore projects

Remote sensing standards: their current status and significance for offshore projects Remote sensing standards: their current status and significance for offshore projects Peter J M Clive Technical Development Consultant SgurrEnergy Ltd 225 Bath Street Glasgow G2 4GZ E: peter.clive@sgurrenergy.com

More information

WIND DATA REPORT. Quincy DPW, MA

WIND DATA REPORT. Quincy DPW, MA WIND DATA REPORT Quincy DPW, MA March 1 st 2007 to May 31 st 2007 Prepared for Massachusetts Technology Collaborative 75 North Drive Westborough, MA 01581 by James R. Browning James F. Manwell Anthony

More information

Reference wind speed anomaly over the Dutch part of the North Sea

Reference wind speed anomaly over the Dutch part of the North Sea Reference wind speed anomaly over the Dutch part of the North Sea A.J. Brand This report has been presented at the European Offshore Wind 2009 Conference, Stockholm, 4-6 September, 2009 ECN-M--09-28 2

More information

WIND DATA REPORT. Vinalhaven

WIND DATA REPORT. Vinalhaven WIND DATA REPORT Vinalhaven January - December, 2003 Prepared for Fox Islands Electric Cooperative by Anthony L. Rogers May 12, 2004 Report template version 1.1 Renewable Energy Research Laboratory 160

More information

Currents measurements in the coast of Montevideo, Uruguay

Currents measurements in the coast of Montevideo, Uruguay Currents measurements in the coast of Montevideo, Uruguay M. Fossati, D. Bellón, E. Lorenzo & I. Piedra-Cueva Fluid Mechanics and Environmental Engineering Institute (IMFIA), School of Engineering, Research

More information

Analysis of Traditional Yaw Measurements

Analysis of Traditional Yaw Measurements Analysis of Traditional Yaw Measurements Curiosity is the very basis of education and if you tell me that curiosity killed the cat, I say only the cat died nobly. Arnold Edinborough Limitations of Post-

More information

E. Agu, M. Kasperski Ruhr-University Bochum Department of Civil and Environmental Engineering Sciences

E. Agu, M. Kasperski Ruhr-University Bochum Department of Civil and Environmental Engineering Sciences EACWE 5 Florence, Italy 19 th 23 rd July 29 Flying Sphere image Museo Ideale L. Da Vinci Chasing gust fronts - wind measurements at the airport Munich, Germany E. Agu, M. Kasperski Ruhr-University Bochum

More information

ITTC Recommended Procedures and Guidelines

ITTC Recommended Procedures and Guidelines Page 1 of 6 Table of Contents 1. PURPOSE...2 2. PARAMETERS...2 2.1 General Considerations...2 3 DESCRIPTION OF PROCEDURE...2 3.1 Model Design and Construction...2 3.2 Measurements...3 3.5 Execution of

More information

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks LONG TERM SITE WIND DATA QUARTERLY REPORT Bishop and Clerks January 1, 2012 March 31, 2012 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Frederick Letson

More information

WIND DATA REPORT. Mt. Tom

WIND DATA REPORT. Mt. Tom WIND DATA REPORT Mt. Tom September 1, 2003 November 31, 2003 Prepared for Massachusetts Technology Collaborative 7 North Drive Westborough, MA 0181 by James F. Manwell Anthony F. Ellis Taylor Geer January

More information

Wind Data Verification Report Arriga 50m

Wind Data Verification Report Arriga 50m Page 1 of 11 Site Name Site Details 9531 - Arriga 5m Arriga 5m Date/Time of report generation 27/11/212 4:22 PM Site Number 9531 Mast Height 5m Mast Location 32568 E 811256 N Coordinate System UTM 55K

More information

WIND DATA REPORT. Swan s Island, ME

WIND DATA REPORT. Swan s Island, ME WIND DATA REPORT Swan s Island, ME June 1, 2009 August 31, 2009 Prepared for US Department of Energy by Daniel T. Grip Utama Abdulwahid James F. Manwell Anthony F. Ellis September 17, 2009 Report template

More information

PUV Wave Directional Spectra How PUV Wave Analysis Works

PUV Wave Directional Spectra How PUV Wave Analysis Works PUV Wave Directional Spectra How PUV Wave Analysis Works Introduction The PUV method works by comparing velocity and pressure time series. Figure 1 shows that pressure and velocity (in the direction of

More information

Full Classification acc. to IEC for SoDAR AQ510 Wind Finder. Vincent Camier, Managing Director, Ammonit Measurement GmbH

Full Classification acc. to IEC for SoDAR AQ510 Wind Finder. Vincent Camier, Managing Director, Ammonit Measurement GmbH Full Classification acc. to IEC 61400-12-1 for SoDAR AQ510 Wind Finder Vincent Camier, Managing Director, Ammonit Measurement GmbH Ammonit Company Profile German company, based in Berlin +25 years of know-how

More information

OPERATIONAL AMV PRODUCTS DERIVED WITH METEOSAT-6 RAPID SCAN DATA. Arthur de Smet. EUMETSAT, Am Kavalleriesand 31, D Darmstadt, Germany ABSTRACT

OPERATIONAL AMV PRODUCTS DERIVED WITH METEOSAT-6 RAPID SCAN DATA. Arthur de Smet. EUMETSAT, Am Kavalleriesand 31, D Darmstadt, Germany ABSTRACT OPERATIONAL AMV PRODUCTS DERIVED WITH METEOSAT-6 RAPID SCAN DATA Arthur de Smet EUMETSAT, Am Kavalleriesand 31, D-64295 Darmstadt, Germany ABSTRACT EUMETSAT started its Rapid Scanning Service on September

More information

! " " # $% $ % % & %

!   # $% $ % % & % !" "#$%%& CNS Meteorological System Upgraded 100-meter tower in 2004 to include a dual elevator on the same tower face Dual monitoring systems with independence from sensor to Plant Computer Wind Sensors

More information

A Wind Profiling Platform for Offshore Wind Measurements and Assessment. Presenter: Mark Blaseckie AXYS Technologies Inc.

A Wind Profiling Platform for Offshore Wind Measurements and Assessment. Presenter: Mark Blaseckie AXYS Technologies Inc. A Wind Profiling Platform for Offshore Wind Measurements and Assessment Presenter: Mark Blaseckie AXYS Technologies Inc. Any Sensor, Any Telemetry, Any Environment Founded in 1974 Part of the AXYS Group

More information

COMPARISON OF CONTEMPORANEOUS WAVE MEASUREMENTS WITH A SAAB WAVERADAR REX AND A DATAWELL DIRECTIONAL WAVERIDER BUOY

COMPARISON OF CONTEMPORANEOUS WAVE MEASUREMENTS WITH A SAAB WAVERADAR REX AND A DATAWELL DIRECTIONAL WAVERIDER BUOY COMPARISON OF CONTEMPORANEOUS WAVE MEASUREMENTS WITH A SAAB WAVERADAR REX AND A DATAWELL DIRECTIONAL WAVERIDER BUOY Scott Noreika, Mark Beardsley, Lulu Lodder, Sarah Brown and David Duncalf rpsmetocean.com

More information

LONG TERM SITE WIND DATA ANNUAL REPORT. Mass Turnpike Authority Blandford, MA

LONG TERM SITE WIND DATA ANNUAL REPORT. Mass Turnpike Authority Blandford, MA LONG TERM SITE WIND DATA ANNUAL REPORT Mass Turnpike Authority Blandford, MA July 1, 2012 June 30, 2013 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Dylan

More information

SCIENCE OF TSUNAMI HAZARDS

SCIENCE OF TSUNAMI HAZARDS SCIENCE OF TSUNAMI HAZARDS ISSN 8755-6839 Journal of Tsunami Society International Volume 31 Number 2 2012 SEA LEVEL SIGNALS CORRECTION FOR THE 2011 TOHOKU TSUNAMI A. Annunziato 1 1 Joint Research Centre,

More information

Friction properties of the face of a hand-held tennis racket

Friction properties of the face of a hand-held tennis racket Available online at www.sciencedirect.com Procedia Engineering 34 (2012 ) 544 549 9 th Conference of the International Sports Engineering Association (ISEA) Friction properties of the face of a hand-held

More information

g L Agenda Chapter 13 Problem 28 Equations of Motion for SHM: What if we have friction or drag? Driven Oscillations; Resonance 4/30/14 k m f = 1 2π

g L Agenda Chapter 13 Problem 28 Equations of Motion for SHM: What if we have friction or drag? Driven Oscillations; Resonance 4/30/14 k m f = 1 2π Agenda Today: HW quiz, More simple harmonic motion and waves Thursday: More waves Midterm scores will be posted by Thursday. Chapter 13 Problem 28 Calculate the buoyant force due to the surrounding air

More information

WIND DATA REPORT. Mt. Lincoln Pelham, MA

WIND DATA REPORT. Mt. Lincoln Pelham, MA WIND DATA REPORT Mt. Lincoln Pelham, MA May 2009 to April 2010 Prepared for Massachusetts Department of Energy Resources 100 Cambridge Street, Suite 1020 Boston, MA 02114 by Jonathan D. Black James F.

More information

PROPAGATION OF LONG-PERIOD WAVES INTO AN ESTUARY THROUGH A NARROW INLET

PROPAGATION OF LONG-PERIOD WAVES INTO AN ESTUARY THROUGH A NARROW INLET PROPAGATION OF LONG-PERIOD WAVES INTO AN ESTUARY THROUGH A NARROW INLET Takumi Okabe, Shin-ichi Aoki and Shigeru Kato Department of Civil Engineering Toyohashi University of Technology Toyohashi, Aichi,

More information

National Renewable Energy Laboratory. Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009

National Renewable Energy Laboratory. Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009 National Renewable Energy Laboratory Wind Resource Data Summary Guam Naval Ordnance Annex Data Summary and Retrieval for November 2009 Prepared for: National Renewable Energy Laboratory 1617 Cole Boulevard

More information

WIND DATA REPORT. Bourne Water District

WIND DATA REPORT. Bourne Water District WIND DATA REPORT Bourne Water District July to September 2010 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Dylan Chase James F. Manwell Utama Abdulwahid

More information

Conventional Ship Testing

Conventional Ship Testing Conventional Ship Testing Experimental Methods in Marine Hydrodynamics Lecture in week 34 Chapter 6 in the lecture notes 1 Conventional Ship Testing - Topics: Resistance tests Propeller open water tests

More information

Results and conclusions of a floating Lidar offshore test

Results and conclusions of a floating Lidar offshore test Results and conclusions of a floating Lidar offshore test J. Gottschall, G. Wolken-Möhlmann, Th. Viergutz, B. Lange [Fraunhofer IWES Wind Lidar Buoy next to FINO1 met. mast] EERA DeepWind'2014 Conference,

More information

GEA FOR ADVANCED STRUCTURAL DYNAMIC ANALYSIS

GEA FOR ADVANCED STRUCTURAL DYNAMIC ANALYSIS SMART SOLUTIONS FOR VIBRATION MONITORING GEA FOR ADVANCED STRUCTURAL DYNAMIC ANALYSIS ANALYSIS OF CIVIL STRUCTURES - EXPO MERLATA PEDESTRIAN BRIDGE ABSTRACT Civil structures and in particular bridges and

More information

WIND DATA REPORT. Bishop and Clerks

WIND DATA REPORT. Bishop and Clerks WIND DATA REPORT Bishop and Clerks March 1, 2004 May 31, 2004 Prepared for Massachusetts Technology Collaborative 75 North Drive Westborough, MA 01581 by James F. Manwell Anthony L. Rogers Anthony F. Ellis

More information

WIND DATA REPORT. Mt. Tom

WIND DATA REPORT. Mt. Tom WIND DATA REPORT Mt. Tom June 1, 2003 August 31, 2003 Prepared for Massachusetts Technology Collaborative 7 North Drive Westborough, MA 0181 by James F. Manwell Anthony F. Ellis Taylor Geer October 30,

More information

RESOURCE DECREASE BY LARGE SCALE WIND FARMING

RESOURCE DECREASE BY LARGE SCALE WIND FARMING ECN-RX--4-14 RESOURCE DECREASE BY LARGE SCALE WIND FARMING G.P. Corten A.J. Brand This paper has been presented at the European Wind Energy Conference, London, -5 November, 4 NOVEMBER 4 Resource Decrease

More information

WIND DATA REPORT. Mass Turnpike Authority Blandford, MA

WIND DATA REPORT. Mass Turnpike Authority Blandford, MA WIND DATA REPORT Mass Turnpike Authority Blandford, MA October 2011 December 2011 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Preeti Verma James F. Manwell

More information

LONG TERM SITE WIND DATA ANNUAL REPORT. Paxton, MA

LONG TERM SITE WIND DATA ANNUAL REPORT. Paxton, MA LONG TERM SITE WIND DATA ANNUAL REPORT Paxton, MA July 1, 2012 June 30, 2013 Prepared for Massachusetts Clean Energy Center Summer Street, 9th Floor Boston, MA 021 by Dylan D. Chase James F. Manwell Anthony

More information

23 RD INTERNATIONAL SYMPOSIUM ON BALLISTICS TARRAGONA, SPAIN APRIL 2007

23 RD INTERNATIONAL SYMPOSIUM ON BALLISTICS TARRAGONA, SPAIN APRIL 2007 23 RD INTERNATIONAL SYMPOSIUM ON BALLISTICS TARRAGONA, SPAIN 16-20 APRIL 2007 AN INVESTIGATION INTO THE INTERRELATION BETWEEN THE INTERNAL AND EXTERNAL BALLISTICS OF FIRING A TP-T TANK AMMUNITION M. H.

More information

Certification of AMS acc. EN 15267, Part 3 - Overview and First Experience -

Certification of AMS acc. EN 15267, Part 3 - Overview and First Experience - Certification of AMS acc. EN 15267, Part 3 - Overview and First Experience - Dr. Wolfgang Jockel, Martin Schneider, TÜV Rheinland Group, D-51105 Cologne / Germany 1. Introduction A new basis for the certification

More information

Increased Project Bankability : Thailand's First Ground-Based LiDAR Wind Measurement Campaign

Increased Project Bankability : Thailand's First Ground-Based LiDAR Wind Measurement Campaign Increased Project Bankability : Thailand's First Ground-Based LiDAR Wind Measurement Campaign Authors: Velmurugan. k, Durga Bhavani, Ram kumar. B, Karim Fahssis As wind turbines size continue to grow with

More information

Wind Project Siting & Resource Assessment

Wind Project Siting & Resource Assessment Wind Project Siting & Resource Assessment David DeLuca, Project Manager AWS Truewind, LLC 463 New Karner Road Albany, NY 12205 ddeluca@awstruewind.com www.awstruewind.com AWS Truewind - Overview Industry

More information

Windcube FCR measurements

Windcube FCR measurements Windcube FCR measurements Principles, performance and recommendations for use of the Flow Complexity Recognition (FCR) algorithm for the Windcube ground-based Lidar Summary: As with any remote sensor,

More information

WIND DIRECTION ERROR IN THE LILLGRUND OFFSHORE WIND FARM

WIND DIRECTION ERROR IN THE LILLGRUND OFFSHORE WIND FARM WIND DIRECTION ERROR IN THE LILLGRUND OFFSHORE WIND FARM * Xi Yu*, David Infield*, Eoghan Maguireᵜ Wind Energy Systems Centre for Doctoral Training, University of Strathclyde, R3.36, Royal College Building,

More information

3D Nacelle Mounted Lidar in Complex Terrain

3D Nacelle Mounted Lidar in Complex Terrain ENERGY 3D Nacelle Mounted Lidar in Complex Terrain PCWG Hamburg, Germany Paul Lawson 25.03.2015 1 DNV GL 125.03.2015 SAFER, SMARTER, GREENER Agenda Introduction and Project Background Lidar Specifications

More information

Measuring power performance with a Wind Iris 4- beam in accordance with EUDP procedure

Measuring power performance with a Wind Iris 4- beam in accordance with EUDP procedure Measuring power performance with a Wind Iris 4- beam in accordance with EUDP procedure This document evaluates the applicability of the EUDP procedure for wind turbine measuring power performance using

More information

Spinner Anemometry Pedersen, T.F.; Sørensen, Niels; Madsen, H.A.; Møller, R.; Courtney, M.; Enevoldsen, P.; Egedal, P.

Spinner Anemometry Pedersen, T.F.; Sørensen, Niels; Madsen, H.A.; Møller, R.; Courtney, M.; Enevoldsen, P.; Egedal, P. Aalborg Universitet Spinner Anemometry Pedersen, T.F.; Sørensen, Niels; Madsen, H.A.; Møller, R.; Courtney, M.; Enevoldsen, P.; Egedal, P. Published in: Proceedings of The European Wind Energy Conference

More information

The Wind Resource: Prospecting for Good Sites

The Wind Resource: Prospecting for Good Sites The Wind Resource: Prospecting for Good Sites Bruce Bailey, President AWS Truewind, LLC 255 Fuller Road Albany, NY 12203 bbailey@awstruewind.com Talk Topics Causes of Wind Resource Impacts on Project Viability

More information

OFFSHORE CREDENTIALS. Accepted for wind resource assessment onshore and offshore by leading Banks Engineers, globally

OFFSHORE CREDENTIALS. Accepted for wind resource assessment onshore and offshore by leading Banks Engineers, globally OFFSHORE CREDENTIALS Accepted for wind resource assessment onshore and offshore by leading Banks Engineers, globally ZEPHIR OFFSHORE CREDENTIALS Accepted for wind resource assessment onshore and offshore

More information

Offshore platforms survivability to underwater explosions: part I

Offshore platforms survivability to underwater explosions: part I Computational Ballistics III 123 Offshore platforms survivability to underwater explosions: part I A. A. Motta 1, E. A. P. Silva 2, N. F. F. Ebecken 2 & T. A. Netto 2 1 Brazilian Navy Research Institute,

More information

Full scale experimental analysis of extreme coherent gust with wind direction changes (EOD)

Full scale experimental analysis of extreme coherent gust with wind direction changes (EOD) Journal of Physics: Conference Series Full scale experimental analysis of extreme coherent gust with wind direction changes (EOD) To cite this article: K S Hansen and G C Larsen 27 J. Phys.: Conf. Ser.

More information

PROJECT CYCLOPS: THE WAY FORWARD IN POWER CURVE MEASUREMENTS?

PROJECT CYCLOPS: THE WAY FORWARD IN POWER CURVE MEASUREMENTS? Title Authors: Organisation PROJECT CYCLOPS: THE WAY FORWARD IN POWER CURVE MEASUREMENTS? Simon Feeney(1), Alan Derrick(1), Alastair Oram(1), Iain Campbell(1), Gail Hutton(1), Greg Powles(1), Chris Slinger(2),

More information

DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT

DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT 10 th Wind Energy Conference DEWEK 2010 DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT Annette Westerhellweg, Beatriz Canadillas, Thomas Neumann DEWI GmbH, Wilhelmshaven, Germany,

More information

OPERATIONAL TEST OF SONIC WIND SENSORS AT KNMI

OPERATIONAL TEST OF SONIC WIND SENSORS AT KNMI OPERATIONAL TEST OF SONIC WIND SENSORS AT KNMI Wiel M.F. Wauben 1 and Rob van Krimpen 2 1 R&D Information and Observation Technology, 2 Observation Systems Operations Royal Netherlands Meteorological Institute

More information

Comparison of flow models

Comparison of flow models Comparison of flow models Rémi Gandoin (remga@dongenergy.dk) March 21st, 2011 Agenda 1. Presentation of DONG Energy 2. Today's presentation 1. Introduction 2. Purpose 3. Methods 4. Results 3. Discussion

More information

A Study of the Normal Turbulence Model in IEC

A Study of the Normal Turbulence Model in IEC WIND ENGINEERING VOLUME 36, NO. 6, 212 PP 759-766 759 A Study of the Normal Turbulence Model in 614-1 Takeshi Ishihara *,1, Atsushi Yamaguchi *,2 and Muhammad Waheed Sarwar *,3 *1 Professor, Department

More information

Site Summary. Wind Resource Summary. Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser

Site Summary. Wind Resource Summary. Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser Site Summary Wind Resource Assessment For King Cove Date Last Modified: 8/6/2013 By: Rich Stromberg & Holly Ganser Station ID: 2857 Latitude: 55 7 45.8 N Longitude: 162 16 10.6 W Tower Type: 30 m NRG Tall

More information

INSTRUMENT INSTRUMENTAL ERROR (of full scale) INSTRUMENTAL RESOLUTION. Tutorial simulation. Tutorial simulation

INSTRUMENT INSTRUMENTAL ERROR (of full scale) INSTRUMENTAL RESOLUTION. Tutorial simulation. Tutorial simulation Lab 1 Standing Waves on a String Learning Goals: To distinguish between traveling and standing waves To recognize how the wavelength of a standing wave is measured To recognize the necessary conditions

More information

CORRELATION EFFECTS IN THE FIELD CLASSIFICATION OF GROUND BASED REMOTE WIND SENSORS

CORRELATION EFFECTS IN THE FIELD CLASSIFICATION OF GROUND BASED REMOTE WIND SENSORS CORRELATION EFFECTS IN THE FIELD CLASSIFICATION OF GROUND BASED REMOTE WIND SENSORS Will Barker (1), Julia Gottschall (2), Michael Harris (3), John Medley (4), Edward Burin des Roziers (5), Chris Slinger

More information

EMPOWERING OFFSHORE WINDFARMS BY RELIABLE MEASUREMENTS

EMPOWERING OFFSHORE WINDFARMS BY RELIABLE MEASUREMENTS EMPOWERING OFFSHORE WINDFARMS BY RELIABLE MEASUREMENTS Joerg Bendfeld University of Paderborn Fakultät Elektrotechnik, Mathematik und Informatik Lehrstuhl für Elektrische Energietechnik Pohlweg 55 D-33014

More information

Tidal influence on offshore and coastal wind resource predictions at North Sea. Barbara Jimenez 1,2, Bernhard Lange 3, and Detlev Heinemann 1.

Tidal influence on offshore and coastal wind resource predictions at North Sea. Barbara Jimenez 1,2, Bernhard Lange 3, and Detlev Heinemann 1. Tidal influence on offshore and coastal wind resource predictions at North Sea Barbara Jimenez 1,2, Bernhard Lange 3, and Detlev Heinemann 1. 1 ForWind - Center for Wind Energy Research, University of

More information

Strategic Advice about Floating LiDAR Campaigns. Borssele offshore wind farm

Strategic Advice about Floating LiDAR Campaigns. Borssele offshore wind farm Strategic Advice about Floating LiDAR Campaigns Borssele offshore wind farm Strategic Advice about Floating LiDAR Campaigns Borssele offshore wind farm Project number: ESMWT16419 Prepared: Dhruv Dhirendra

More information

WIND DATA REPORT. Mass Turnpike Authority Blandford, MA

WIND DATA REPORT. Mass Turnpike Authority Blandford, MA WIND DATA REPORT Mass Turnpike Authority Blandford, MA April 2012 June 2012 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Preeti Verma James F. Manwell

More information

FIVE YEARS OF OPERATION OF THE FIRST OFFSHORE WIND RESEARCH PLATFORM IN THE GERMAN BIGHT FINO1

FIVE YEARS OF OPERATION OF THE FIRST OFFSHORE WIND RESEARCH PLATFORM IN THE GERMAN BIGHT FINO1 FIVE YEARS OF OPERATION OF THE FIRST OFFSHORE WIND RESEARCH PLATFORM IN THE GERMAN BIGHT FINO1 Andreas Beeken, DEWI GmbH, Ebertstraße 96, D-26382 Wilhelmshaven Thomas Neumann, DEWI GmbH, Ebertstraße 96,

More information

VINDKRAFTNET MEETING ON TURBULENCE

VINDKRAFTNET MEETING ON TURBULENCE VINDKRAFTNET MEETING ON TURBULENCE On-going Work on Wake Turbulence in DONG Energy 28/05/2015 Cameron Brown Load Engineer Lucas Marion R&D graduate Who are we? Cameron Brown Load Engineer from Loads Aerodynamics

More information

Inlet Influence on the Pressure and Temperature Distortion Entering the Compressor of an Air Vehicle

Inlet Influence on the Pressure and Temperature Distortion Entering the Compressor of an Air Vehicle Distortion Entering the Compressor of an Air Vehicle P. Hendrick Université Libre de Bruxelles, ULB Avenue F.D. Roosevelt, 50 1050 Brussels BELGIUM patrick.hendrick@ulb.ac.be ABSTRACT One of the possible

More information

Circuit breaker diagnostic testing. Megger is a registered trademark

Circuit breaker diagnostic testing. Megger is a registered trademark WWW.MEGGER.COM Megger is a registered trademark Title Author Nils Wäcklén Date January 2010 Keywords TM1600, TM1800, CIGRÉ, vibration analysis, dynamic resistance measurement, circuit breaker testing,

More information

1811G/H PITOT-STATIC TEST SET

1811G/H PITOT-STATIC TEST SET 1811G/H PITOT-STATIC TEST SET USER INSTRUCTION MANUAL M/N: 1811G/H, P/Ns: 101-00165 101-00168 101-00169 Doc. P/N: 56-101-00165_00168_00169 Revision C December 9, 2014 BARFIELD, INC. Corporate Headquarters

More information

Conditions for occurrence of vortex shedding on a large cable stayed bridge. Full scale data from monitoring system

Conditions for occurrence of vortex shedding on a large cable stayed bridge. Full scale data from monitoring system Conditions for occurrence of vortex shedding on a large cable stayed bridge. Full scale data from monitoring system O. Flamand 1, F. De Oliveira 1 and A. Stathopoulos-Vlamis, P. Papanikolas 2 1 Centre

More information

VALIDATION OF WIND SPEED DISTURBANCES TO CUPS AT THE METEORLOCICAL MAST ON THE OFFSHORE PLATFORM FINO1 USING WIND-LIDAR MEASUREMENTS.

VALIDATION OF WIND SPEED DISTURBANCES TO CUPS AT THE METEORLOCICAL MAST ON THE OFFSHORE PLATFORM FINO1 USING WIND-LIDAR MEASUREMENTS. VALIDATION OF WIND SPEED DISTURBANCES TO CUPS AT THE METEORLOCICAL MAST ON THE OFFSHORE PLATFORM FINO1 USING WIND-LIDAR MEASUREMENTS Authors: Detlef Kindler K.-W.-Koog GmbH Andy Oldroyd Oldbaum Services

More information

SUPPLEMENTARY GUIDANCE NOTE 4: WIND SHEAR

SUPPLEMENTARY GUIDANCE NOTE 4: WIND SHEAR A GOOD PRACTICE GUIDE TO THE APPLICATION OF ETSU-R-97 FOR THE ASSESSMENT AND RATING OF WIND TURBINE NOISE SUPPLEMENTARY GUIDANCE NOTE 4: WIND SHEAR ISSUE 1 JULY 2014 Page 1 of 14 PREFACE This document

More information

El Niño climate disturbance in northern Madagascar and in the Comoros

El Niño climate disturbance in northern Madagascar and in the Comoros El Niño climate disturbance in northern Madagascar and in the Comoros Rabeharisoa J. M.¹, Ratiarison A.¹, Rakotovao N.¹, Salim Ahmed Ali¹ ² (*) ¹ Laboratoire de Dynamique de l Atmosphère, du Climat et

More information

WCA Wind Research Project Report

WCA Wind Research Project Report WCA Wind Research Project Report Steven Selvaggio Hasz Consulting Company Whitestone Community Association Presented to: Alaska Energy Authority September 25 Table of Contents I. Project Overview II. Results

More information

Overview. 2 Module 13: Advanced Data Processing

Overview. 2 Module 13: Advanced Data Processing 2 Module 13: Advanced Data Processing Overview This section of the course covers advanced data processing when profiling. We will discuss the removal of the fairly gross effects of ship heave and talk

More information

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks

LONG TERM SITE WIND DATA QUARTERLY REPORT. Bishop and Clerks LONG TERM SITE WIND DATA QUARTERLY REPORT Bishop and Clerks July 1, 2010 September 30, 2010 Prepared for Massachusetts Clean Energy Center 55 Summer Street, 9th Floor Boston, MA 02110 by Frederick Letson

More information

Validation Study of the Lufft Ventus Wind Sensor

Validation Study of the Lufft Ventus Wind Sensor Weather Forecasts Renewable Energies Air and Climate Environmental Information Technology METEOTEST Cooperative Fabrikstrasse 14, CH-3012 Bern Tel. +41 (0)31 307 26 26 Fax +41 (0)31 307 26 10 office@meteotest.ch,

More information

EXPERIMENTAL RESULTS OF GUIDED WAVE TRAVEL TIME TOMOGRAPHY

EXPERIMENTAL RESULTS OF GUIDED WAVE TRAVEL TIME TOMOGRAPHY 18 th World Conference on Non destructive Testing, 16-20 April 2012, Durban, South Africa EXPERIMENTAL RESULTS OF GUIDED WAVE TRAVEL TIME TOMOGRAPHY Arno VOLKER 1 and Hendrik VOS 1 TNO, Stieltjesweg 1,

More information

MEMO CC: Summary. ESMWT16419: _MEM_RVO_HKZ floating LiDAR uncertainty_v3.docx 1/8

MEMO CC: Summary. ESMWT16419: _MEM_RVO_HKZ floating LiDAR uncertainty_v3.docx 1/8 MEMO Prepared: Anthony Crockford 23.02.2016 Reviewed: Erik Holtslag 24.02.2016 Approved: Michiel Müller 29.02.2016 Filename 20160224_MEM_RVO_HKZ floating LiDAR uncertainty_v3.docx Pages 8 Version Author

More information

Chapter 11 Waves. Waves transport energy without transporting matter. The intensity is the average power per unit area. It is measured in W/m 2.

Chapter 11 Waves. Waves transport energy without transporting matter. The intensity is the average power per unit area. It is measured in W/m 2. Energy can be transported by particles or waves: Chapter 11 Waves A wave is characterized as some sort of disturbance that travels away from a source. The key difference between particles and waves is

More information

Queue analysis for the toll station of the Öresund fixed link. Pontus Matstoms *

Queue analysis for the toll station of the Öresund fixed link. Pontus Matstoms * Queue analysis for the toll station of the Öresund fixed link Pontus Matstoms * Abstract A new simulation model for queue and capacity analysis of a toll station is presented. The model and its software

More information

Title: Standard Operating Procedure for R&R Environmental Devices Model MFC201 Gas Dilution Calibrator

Title: Standard Operating Procedure for R&R Environmental Devices Model MFC201 Gas Dilution Calibrator Procedure No: SOP-029 Revision No: 1.1 (December 29, 2010) Page No.: 1 of 7 1. INTRODUCTION AND SCOPE To obtain timely data for the purpose of air quality assessment, air quality trend reporting, air quality

More information