TY - JOUR
T1 - The wind energy potential of Iceland
AU - Nawri, Nikolai
AU - Petersen, Gudrún Nína
AU - Bjornsson, Halldór
AU - Hahmann, Andrea N.
AU - Jónasson, Kristján
AU - Hasager, Charlotte Bay
AU - Clausen, Niels Erik
PY - 2014/9
Y1 - 2014/9
N2 - Downscaling simulations performed with the Weather Research and Forecasting (WRF) model were used to determine the large-scale wind energy potential of Iceland. Local wind speed distributions are represented by Weibull statistics. The shape parameter across Iceland varies between 1.2 and 3.6, with the lowest values indicative of near-exponential distributions at sheltered locations, and the highest values indicative of normal distributions at exposed locations in winter. Compared with summer, average power density in winter is increased throughout Iceland by a factor of 2.0-5.5. In any season, there are also considerable spatial differences in average wind power density. Relative to the average value within 10km of the coast, power density across Iceland varies between 50 and 250%, excluding glaciers, or between 300 and 1500Wm-2 at 50m above ground level in winter. At intermediate elevations of 500-1000m above mean sea level, power density is independent of the distance to the coast. In addition to seasonal and spatial variability, differences in average wind speed and power density also exist for different wind directions. Along the coast in winter, power density of onshore winds is higher by 100-700Wm-2 than that of offshore winds. Based on these results, 14 test sites were selected for more detailed analyses using the Wind Atlas Analysis and Application Program (WAsP).
AB - Downscaling simulations performed with the Weather Research and Forecasting (WRF) model were used to determine the large-scale wind energy potential of Iceland. Local wind speed distributions are represented by Weibull statistics. The shape parameter across Iceland varies between 1.2 and 3.6, with the lowest values indicative of near-exponential distributions at sheltered locations, and the highest values indicative of normal distributions at exposed locations in winter. Compared with summer, average power density in winter is increased throughout Iceland by a factor of 2.0-5.5. In any season, there are also considerable spatial differences in average wind power density. Relative to the average value within 10km of the coast, power density across Iceland varies between 50 and 250%, excluding glaciers, or between 300 and 1500Wm-2 at 50m above ground level in winter. At intermediate elevations of 500-1000m above mean sea level, power density is independent of the distance to the coast. In addition to seasonal and spatial variability, differences in average wind speed and power density also exist for different wind directions. Along the coast in winter, power density of onshore winds is higher by 100-700Wm-2 than that of offshore winds. Based on these results, 14 test sites were selected for more detailed analyses using the Wind Atlas Analysis and Application Program (WAsP).
KW - Iceland
KW - Mesoscale modelling
KW - Wind atlas
KW - Wind energy potential
KW - Wind resource mapping
UR - http://www.scopus.com/inward/record.url?scp=84898830088&partnerID=8YFLogxK
U2 - 10.1016/j.renene.2014.03.040
DO - 10.1016/j.renene.2014.03.040
M3 - Article
AN - SCOPUS:84898830088
SN - 0960-1481
VL - 69
SP - 290
EP - 299
JO - Renewable Energy
JF - Renewable Energy
ER -