Wind Energy Data Analysis and Resource Mapping of Geba Catchment, North Ethiopia by Mulu Bayray, Anwar Mustefa, Ftwi Yohannes, Hailay Kiros, Asfafaw Haileslasie, Petros Gebray, Mesele Hayelom and Addisu Dagne R EPRINTED FROM WIND ENGINEERING VOLUME 37, N O . 4, 2013 M U LT I -S CIENCE P UBLISHING C O M PA N Y 5 W AT E S WAY • B RENTWOOD • E SSEX CM15 9TB • UK TEL : +44(0)1277 224632 • F AX: +44(0)1277 223453 E-MAIL: [email protected] • WEB SITE: www.multi-science.co.uk
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Wind Energy Data Analysis and Resource Mapping of Geba Catchment, North Ethiopia Wind Energy Data Analysis and Resource Mapping of Geba Catchment, North Ethiopia
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Wind Energy Data Analysis and Resource Mapping of Geba Catchment, North Ethiopia
ABSTRACTWind energy potential in Ethiopia is estimated to be enormous due to local peculiar
landscape situations. However, the country started to utilize the potential only very recently.
One of the reasons for low utilization of wind energy in Ethiopia is the absence of reliable and
accurate wind energy resource data. Development of reliable and accurate wind atlas helps
to identify candidate sites for wind energy applications and facilitates the planning and
implementation of wind energy projects. This paper presents wind energy data analysis and
wind atlas of Geba catchment in North Ethiopia.
The work reported in this paper is based on wind data collected over a period of one year
from measuring masts in six different sites in Tigray, Ethiopia. The data was analyzed using
various statistical software to evaluate the wind energy potential of the area. Average wind
speed and power density, distribution of the wind prevailing direction, turbulence intensity
and wind shear profile of each site were determined. Wind Atlas Analysis and Application
Programme (WAsP) was used to generate the wind atlas of the area and to develop the wind
speed and power density maps.
The data analysis indicates that the average wind speed at 10 m above ground level
(a.g.l.) varies from 3.7 m/s to 6.64 m/s. The mean power density at 10 m a.g.l varies from
64 W/m2 to 301 W/m2. The prevailing wind directions are East and South East directions.
The wind resource map developed by WAsP at 50 m indicated that the catchment has good
wind power potential having mean wind speed and power density of 6.5 m/s and 288 W/m2,
respectively.
1. INTRODUCTIONEthiopia’s current electrical energy supply is mainly from hydropower. Wind energy is an
alternative energy resource which can complement hydropower especially during the dry
season. Due to the fast economic development in the recent years, the country is looking for
more power plants to satisfy the high demand for electricity. Wind energy resource potential
in the country is estimated to be high. The objective of the study reported in this paper was to
conduct wind energy resource assessment of a specific catchment area of the river named
Geba located in Northern part of Ethiopia.
2. METHODOLOGY2.1. Description of the study areaGeba catchment is found in Tigray Region, North Ethiopia. The entire Geba catchment is
found between 13°18’ to14°15 N (latitude) and 38°38’ to 39°48’ E (longitude). It covers an area of
5133 km2. The elevation ranges from 955 m to 3315 m above sea level and the mean elevation
is 2146 m above sea level. Figure 1a) shows the base map of the catchment. The location of the
six measurement masts is indicated in Figure 1b). The details of the site location and available
date for analysis are indicated in Table 1. Masts of the sites number 1 to 4 are erected by the
Department while sites 5 and 6 are erected by the national utility corporation EEPCo. Details
of the masts and instrumentation are reported elsewhere [2−4].
2.2. Data collection, screening and validationAll the collected data was inspected for completeness and any erroneous records. The time
series of the data was checked to look for missing data values and a number of data validation
routines were used to screen all the data for suspect and erroneous values. General system
and parameter checks were used for data screening and validation. The validation checks
include: continuity test to identify missing records in the data, inspection of the average wind
speed at each 10-minutes interval records, inspection of negative and unrealistic high wind
speed and wind direction records and observation of vertical profile of wind speed on same
mast (negative and undefined wind shear coefficients).
2.3. Statistical data analysis2.3.1. Average Wind SpeedThe wind characterization in terms of speed, direction and wind power is the first step to
obtain the initial feasibility of generating electricity from wind power through a wind farm, in
a given region. The most critical factor influencing the power developed by a wind energy
conversion system is the wind speed. The average wind speed Vm is given as:
334 WIND ENERGY DATA ANALYSIS AND RESOURCE MAPPING OF
GEBA CATCHMENT, NORTH ETHIOPIA
Idaga HamusInda Tekle Haymanot
Senkata
Atsbi Inda SilaseWukro
May MekdanMekele
KwihaMay Keyah
Tigray Region
Dera Mast
Hagereselam Mast
Mosobo-Harena Mast
Mekelle University Mast
Ashegoda Mast
Mydehru Mast
Abiy adi
Figure 1: a) Base map of Geba catchment [1] b) location map of the six measurement masts.
Table 1: Location of the wind measuring masts in the catchmentSite Wind Location of wind Altitude Height Available data recordsNo. measuring measuring masts a.g.l
mast Latitude Longitude [m] [m] From Until1 Dera 13.99° N 39.73° E 2870 10, 30 01/07/2010 19/04/20122 Hagereselam 13.66° N 39.19° E 2628 10, 30 11/10/2010 17/04/20123 Mayderhu 13.29° N 39.40° E 2512 10, 30 15/01/2011 18/04/20124 Mekelle University 13.48° N 39.49° E 2208 10 09/04/2010 04/0520115 Ashegoda 13.42° N 39.60° E 2425 10, 40 08/06/2010 24/09/20116 Mosobo-Harena 13.57° N 39.51° E 2401 10, 40 01/01/2006 31/12/2007
(1)
Where Vi is the wind speed at interval i and n is the number of records. The average wind
speed is calculated at hourly, daily, monthly and annual interval.
2.3.2. Wind Power DensityThe wind power per unit area, P/A or wind power density at interval i is given by:
(2)
Where Vi is the wind speed at interval i, ρ is air density. Average power density is
calculated in similar way to the average speed shown previously.
The wind speed and power density at a certain height determines the wind power class of the
site. The wind power class of a site is determined as per the standard classification reported in [5].
2.3.3. Wind Shear CoefficientThe wind shear coefficient is calculated assuming power law relationship at the two heights.
The coefficient α is found from:
(3)
Where V1 is the wind speed at height z1 and V2 is the wind speed at height z2.
2.3.4. TurbulenceThe average turbulence intensity of the sites was calculated by taking the average of the
individual turbulence intensity values of 10 minutes records which were calculated by
dividing the standards deviation with the average speed of each record. The turbulence
intensity TI at interval i is given from [6]:
(4)
Where σi is the standard deviation of wind speed at interval i. The overall average
turbulence is found in similar way to that shown for wind speed. TI is a relative indicator of
turbulence with low levels indicated by values less than or equal to 0.10, moderate levels to
0.25, and high levels greater than 0.25.
2.4. Modeling with WAsP2.4.1. Observed Wind Climate (OWC)WAsP (Wind Atlas Analysis and Application Program) [7] was used to generate the Wind
Atlas and to develop the wind resource map of the Catchment. The flow modeling of WAsP is
discussed in [8] and application of the software for resource assessment may be found in
literature such as [9−11]. The various inputs needed in WAsP are Observed Wind Climate
(OWC) of sites, Vector Map of the catchment and Obstacle Groups to the measuring masts.
OWC is a tabular summary of the frequency of occurrence of wind speed and wind direction.
The OWC is produced from raw wind speed and direction measurements.
The OWC represents the data converted into Weibull probability density function. The
Weibull function is defined using two factors namely the scale parameter A and the shape
parameter k. The OWC also shows the wind direction distribution as wind rose. Wind rose
diagram shows the distribution of wind in different directions. The wind rose diagram is
generated by dividing into twelve equally spaced sectors. The frequency distribution for each
sector is calculated and plotted in the wind rose diagram.
2.4.2 Wind AtlasWind Atlas is a generalized wind climate of the observed wind climate. The data measured
from the wind measuring mast is a site specific data. The Wind Atlas data sets are site-
independent and the wind distributions have been reduced to certain standard conditions.
The Wind Atlas contains data for 5 reference roughness lengths (0.000 m, 0.030 m, 0.100 m,
0.200 m, 0.400 m) and 5 reference heights (10 m, 30 m, 50 m, 70 m, 100 m) a.g.l.
2.4.3 Resource MapResource grid is a rectangular set of points for which summary of predicted wind climate data
are calculated. WAsP uses data from one metrological mast to generate Wind Atlas and
Resource Grid of an area. However, it doesn’t support multiple masts. The area of Geba
catchment is too large that it is not recommended to use data from a single mast to generate
the Wind Atlas and Resource Grid of the catchment. In order to use data from different wind
measuring masts the study area was divided in to six zones equal to the number of masts. The
area was divided in such a way that each zone contains one wind measuring mast as shown in
Figure 2. Wind Atlas and Resource map of each area was generated using observed wind
climate of each wind measuring mast and vector map of each area. The wind resource map of
the catchment was found by the combination of the resource maps of each zone.
336 WIND ENERGY DATA ANALYSIS AND RESOURCE MAPPING OF
GEBA CATCHMENT, NORTH ETHIOPIA
Dera Mast
Hagereselam Mast
Mosobo-Harena Mast
MU Mast
Ashegoda Mast
Myderhu Mast
Figure 2: Six zones of the study area.
3. RESULTS AND DISCUSSION3.1. Data recovery and validationData recovery and validation was conducted as per the procedure discussed in section 2.2.
The summary of results of the data screening and validation is shown in Table 2. The data
recovery rate was greater than 96% in all the measuring stations except in Hagereselam
which was 94%. The reason for low data recovery rate in Hagereselam mast was that the mast
was taken down for 20 days from 21-05-2011 to 11-06-2011 to replace a broken anemometer
accounting for 4% of the missing data. The data recovery rate in the other masts was good
except for the loss of some data during transfer from data loggers to laptops because the
memory card had to be removed.
Measures were taken to replace the missing and erroneous data records when
necessary. Data lost during transfer of data due to removal of memory card was filled with
average data record of the same hour where the data was missing. The missing data
records at 30 m in Hagereselam mast due to break down of the anemometer were filled by
interpolating from the 10 m records using the power low and the wind shear coefficient
calculated based on overall average wind speeds at 10 and 30 m. Data lost at both heights
for extended period of time was found in Hagereselam, Ashegoda and Mosobo-Harena
masts. Since the overall data recovery rate was above 94% in these sites this will not affect
the overall data quality of the sites. No measure was taken to fill the loss of data for
extended period of time. Negative and undefined wind shear coefficients occurred when
the wind speed at 30 or 40 m height is less than the 10 m record. This was corrected by
replacing the 30 or 40 m wind speed records by interpolating from the 10 m records using
the power law and the wind shear coefficient calculated based on overall average wind
speeds at 10 and 30 or 40 m.
3.2. Results of statistical data analysis3.2.1. Average Wind Speed and Power DensityThe overall average wind speed and average power density of the data during the period
were calculated based on the equations discussed in section 2.3. The results obtained for each
site are shown in Table 3. Included in this table is the maximum wind speed recorded averaged
in the ten minutes measurement interval for each site. The wind power density class at each
height for the respective sites is also shown in the table. The class ranges from class 6 in
Hagereselam site to class 1 at Dera and Mekelle University sites.
Table 2: Data screening and validationSite Data Available Total number of Gross Number of negative No. measuring data records missing data data and undefined wind
mast (10 minute records recovery shear coefficientsaverage) rate (%)
Mayderhu, Ashegoda and Mesebo-Harena sites. High turbulence (> 0.25) intensities are found
at Mekelle University and Dera sites.
3.3. Results of WAsP modeling and analysis3.3.1. Observed Wind ClimateObserved wind climate is a tabular summary of the frequency of occurrence of wind speed
versus wind direction. The time-series of wind speed and direction data were transformed into
a table which describes a time-independent summary of the conditions found at the measuring
site using the WAsP software. Figure 4 shows the results for each site based on the 10 m raw data.
Table 5: Average Turbulence intensityWind measuring Average turbulence
mast intensity10 m 30 /40 m
Dera 0.466 0.267Hagereselam 0.175 0.137Mayderhu 0.230 0.165Mekelle University 0.54 NAAshegoda 0.128 0.099Mosobo-Harena 0.176 0.136