(LSA) Land suitability assessment for a Wind Farm location (2011)
What is a Land Suitability Assesment?:
Also known as layer-based GIS, this is the most frequent form of geographic-data space representation. Particularly, LSA (Land Suitability Assessments) is a very complex analysis in which the overlapping of thematic maps result helpful.
Also known as layer-based GIS, this is the most frequent form of geographic-data space representation. Particularly, LSA (Land Suitability Assessments) is a very complex analysis in which the overlapping of thematic maps result helpful.
The analysis is based on the combination of different thematic layers such as topographic, geologic or drainage as well as in their interpretation independently from one to another.
Wind Farm location selection:
Wind Farm location selection:
Criteria to locate a wind farm in Europe differ a little bit from one country to another.
Land suitability analysis. wind farm UK
In the case of the British Isles, the British Wind Energy Association (BWEA) estimates that the extension average of a wind farm with 20 turbines is "1" square kilometer (BWEA).
The principal objective was to locate a suitable area to construct a 90 MW Wind Farm.
The analysis was divided into two levels:
- A national level to obtain potential areas suitable to undertake a new wind development.
- A local level to select the final location.
- Two ‘asc’ files (wspeed45.asc and dominant.asc) together with roads map extracted from the 1:250000 OS map (Digimap) were used to achieve the aims of the analysis.
- Land cover data from CIS2000:
- Factors such as woodlands, water bodies (rivers, lakes, reservoirs, etc.) and man-made built structures (cities or urban agglomerations).
- Road map extracted from digimap (OS strategi, 1:250000). Urban and roads cause a ‘distance decay effect’ that affect the suitability for any new wind farm location.
Data gathering and management is particularly important in the selection and estimation of areas suitable for a wind farm complex.
The Mapping process:
The mapping process used two
different sources.
The ‘asc’ files were converted into raster in order to map
water, wood and urban agglomerations which they are variables frequently used in
wind farm constraints maps, and roads which were also estimated in the
assessment and extracted from the 1:250000 OS UK map.
Infrastructures such as
roads are usually employed as a relevant factor that determines the final
location of a wind farm. Henning (2005:82) and Baban & Parry (2000:68) recognise
roads proximity as one of the most important factors in a GIS-based multi-criteria
analysis.
After converting ‘asc’ files, number
‘0’ was extracted from the classification in both new raster files but a new
error raised. Both maps showed differences in their screen position, making it
hard the analysis. The problem was resolved by adding a shapefile of a correct
UK map.
UK Map Suitable areas wind Farms |
This permitted to know which of the new maps had to be fixed. The
ArcGis option ‘shift management’ enabled the analyst to resolve the differences
by adding 54 in ‘x’ and 11 in ‘y’. These numbers were obtained by comparing the
shapefile with the damaged new raster ‘domland’.
Euclidean distance was computed in
the three extracted thematic maps from the dominant file water (water_euc_dis),
wood (wood_euc_dis) and urban (urban_euc_dis)) and the roads map buffering
distances to obtain the most suitable places for the final location. After
buffering distances, thematic maps as well as roads and wind speed maps were
reclassified from ‘0’ or non suitable to ‘1’ or suitable to develop constraint
maps at the national level. Finally, the five maps were computed in the raster
calculator to get the suitability national map (Output_NL.img).
As commented above, the analysis is
divided into two main parts. The national level and the local level permitted
to verify the suitability of the area by multiplying the national map with two
local factors, slope and aspect, each of which influence in the location of the
wind farm. At the local level, both, slope and aspect were derived from OS
Land-Form Panorama DTM (1:50000) tiles of a Scottish region.
The tiles were
processed by the function ‘mosaic to raster’ selecting the British coordinate
system. Then, ‘define projection (management)’ and ‘project raster’ in which
the tiles are modified from meters to kilometres, complete the process prior
the slope and aspect calculation.
Slope and aspect were finally
calculated and then reclassified to permit the final estimation of the most
appropriate area to install a wind farm. Slope was classified following
criteria found in relevant literature, selecting as unsuitable those areas in
which the slope is higher than 6ยบ. Aspect was obtained in three phases, from computing
the radiant [Aspect_Sampl1*.0174] and sin [sin (aspect_rad)] to reclassifying ‘aspect_sin’
from suitable ‘1’ to unsuitable ‘0’.
Finally, the analysis was completed
by computing the two derived local maps with the final output or national map
[(slope_rec)*( aspect_rec)*(
Output_NL.img)].
Conclusions:
The location and how turbines are
distributed goes from 300-600 meters distance between turbines to a kilometer
in Spain or Scotland (National Wind Watch).
In this case study, the location selected, North-eastern Scotland has an extension of more than 7.5 square kilometres meeting the requirements of energy production (90 MW) exposed in the beginning of the work.
Local analysis. Scotland |
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