Research Article

Vertical Profile of Wind Diurnal Cycle in the Surface Boundary Layer over the Coast of Cotonou, Benin, under a Convective Atmosphere

Table 4

Mean Absolute Error (MAE) between models and measure corresponding to the 10–60 m extrapolation range (2013–2016).

Proposed model (best fitting equation)Mikhail and Justus [67]Mikhail [11]Nfaoui et al. [12]Kasbadji [13]
MAE (m·s−1)MAE (m·s−1)MAE (m·s−1)MAE (m·s−1)MAE (m·s−1)

Jan0.060.190.600.150.41
Feb0.050.210.590.080.66
Mar0.030.130.580.100.18
Apr0.020.140.590.230.08
May0.040.150.590.170.05
Jun0.070.130.460.240.14
Jul0.030.170.680.160.08
Aug0.020.190.720.210.03
Sep0.130.510.990.321.01
Oct0.070.230.640.080.32
Nov0.050.0720.370.220.08
Dec0.030.110.500.240.14
Yearly0.0180.140.60.370.23