Correction to: Atmospheric Turbulence Measurements at a Coastal Zone with and without Fog

1 Correction to: Boundary-Layer Meteorology https://doi.org/10.1007/s10546-021-00655-9

In the original publication, the last sentence in caption of Fig. 11 was published incompletely. The correct caption for the figure is provided in this correction.

Fig. 11

The non-dimensional; a, b dissipation rate of TKE (9), and standard deviations of the; c, d air temperature (7), and e, f specific humidity (8) plotted in log–log coordinates versus the local Monin–Obukhov stability parameter (5) for the 15-min-averaged data collected during only clear sky days with high visibility (i.e., fog-free conditions) when the PWD22 visibility was greater than 6 km. Plots in the left panels; a, c, e correspond to unstable conditions, or CBL, $\zeta < 0$; the right panels b, d, f represent stable conditions, or SBL, $\zeta > 0$. The black dashed lines correspond to $\varphi_{\varepsilon } \left( \zeta \right) = \left( {1 + 0.5 \left| \zeta \right|^{2/3} } \right)^{3/2}$ for $\zeta <0$ and ${\varphi}_{\varepsilon } \left( \zeta \right) = \left( {1 + 5 \zeta} \right)$ for $\zeta > 0$; and $\varphi_{\theta } (\zeta ) = \varphi_{q} (\zeta ) = 2(1 - 9.5\zeta )^{-1/3}$ for $\zeta < 0$ and $\varphi_{\theta } (\zeta ) = \varphi_{q} (\zeta ) = 2(1 + 0.5\zeta )^{-1}$ for $\zeta > 0$ (Kaimal and Finnigan 1994)

The original article has been corrected.