2019
DOI: 10.4236/sgre.2019.1011016
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Vertical Profile of Wind Speed in the Atmospheric Boundary Layer and Assessment of Wind Resource on the Bobo Dioulasso Site in Burkina Faso

Abstract: This study investigates both the characteristics of the vertical wind profile at the Bobo Dioulasso site located in the Sudanian climate zone in Burkina Faso during a day and night convective wind cycle and the estimation and variability of the wind resource. Wind data at 10 m above ground level and satellite data at 50 m altitude in the atmospheric boundary layer were used for the period going from January 2006 to December 2016. Based on Monin-Obukhov theory, the logarithmic law and the power law made it poss… Show more

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Cited by 8 publications
(7 citation statements)
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“…It is evaluated at 56 W.m Togo and Nigeria. The results obtained in the Ivory Coast more precisely in Korhogo in the northern savannah zone and reported by the studies of Boro et al [33] indicates that the highest monthly wind potential is recorded in May and estimated at 29.28 W.m -2 at 10 m. On the Bobo-Dioulasso site in Burkina Faso, the annual wind potential is estimated at 53.13 W.m -2 at 20 m and 84.05 W.m -2 at 50 m according to the studies of Boro et al [33]. Several sites in Chad have been the subject of the wind potential study [31].…”
Section: Variation Of the Wind Energysupporting
confidence: 75%
“…It is evaluated at 56 W.m Togo and Nigeria. The results obtained in the Ivory Coast more precisely in Korhogo in the northern savannah zone and reported by the studies of Boro et al [33] indicates that the highest monthly wind potential is recorded in May and estimated at 29.28 W.m -2 at 10 m. On the Bobo-Dioulasso site in Burkina Faso, the annual wind potential is estimated at 53.13 W.m -2 at 20 m and 84.05 W.m -2 at 50 m according to the studies of Boro et al [33]. Several sites in Chad have been the subject of the wind potential study [31].…”
Section: Variation Of the Wind Energysupporting
confidence: 75%
“…It should be noted that these convective movements, less intense than during the day, could therefore explain the instability observed at this time. This characterisation of the atmosphere in Conakry is confirmed by the studies of Donnou et al [3], Boro et al [58], Gualtieri et al [4], Yahaya et al [59] and Fritz et al [60] who also estimate that the atmosphere is generally unstable during the day and stable during the night.…”
Section: Fig 6 Monthly Variation Of Obukhov Length In Conakry (2001-2...supporting
confidence: 69%
“…During the period from November to mid-May (dry season), the production of wind energy is more important during the day than night. In sum, based on the wind power density classes used in the studies of Donnou et al [52] and Boro et al [58], the power densities calculated at the Conakry site belong to class 3 (300 W.m -2 ; 400 W.m -2…”
Section: Wind Energy Distributionmentioning
confidence: 99%
“…where V(H) is the speed of the wind, H is the height, Y 0 is the roughness length, v 0 is the friction velocity, q is the Von Kaman constant, and ψ is the atmospheric stability function [2]. ψ value is greater than zero for the daytime and is less than zero in the night.…”
Section: Introductionmentioning
confidence: 99%