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Effect of small‐scale surface heterogeneities and buildings on radiation fog: Large‐eddy simulation study at Paris–Charles de Gaulle airport

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Large‐eddy simulations (LES) of radiation fog were performed over an airport area to study the effect of urban canopy on fog. These LES were performed with the Meso‐NH research model at very high resolution: 1.5 m in the horizontal and 1 m in the vertical and over a domain 4.5 km × 1.5 km.The blocking effect of the airport buildings led to strong wind shear and consequently to the production of turbulent kinetic energy (TKE). The airport buildings also had a strong effect on vertical velocity, with a subsidence region behind the buildings. The increase of both turbulence and vertical velocity strongly modified the fog formation. The fog layer took more time to form in the airport area, but the increase in turbulence facilitated the vertical development of the fog layer.The fog took 1.5 h to form over the whole simulated airport area. The fog height was heterogeneous during the formation phase, with the formation of very low clouds locally. The effect of airport buildings on vertical velocity could explain these heterogeneities of the fog height. During the mature phase of the fog, the buildings had little impact on the fog layer characteristics. The fog dynamics were mainly controlled by processes at its top.These results suggest that the inclusion of high levels of detail in the building representation remains important for the local forecasting of fog formation. Particularly, small‐scale heterogeneities can explain the spatial variability of fog formation. It seems necessary to take small‐scale variability of the urban canopy into account for local and accurate forecasts of fog formation over airport areas.
Title: Effect of small‐scale surface heterogeneities and buildings on radiation fog: Large‐eddy simulation study at Paris–Charles de Gaulle airport
Description:
Large‐eddy simulations (LES) of radiation fog were performed over an airport area to study the effect of urban canopy on fog.
These LES were performed with the Meso‐NH research model at very high resolution: 1.
5 m in the horizontal and 1 m in the vertical and over a domain 4.
5 km × 1.
5 km.
The blocking effect of the airport buildings led to strong wind shear and consequently to the production of turbulent kinetic energy (TKE).
The airport buildings also had a strong effect on vertical velocity, with a subsidence region behind the buildings.
The increase of both turbulence and vertical velocity strongly modified the fog formation.
The fog layer took more time to form in the airport area, but the increase in turbulence facilitated the vertical development of the fog layer.
The fog took 1.
5 h to form over the whole simulated airport area.
The fog height was heterogeneous during the formation phase, with the formation of very low clouds locally.
The effect of airport buildings on vertical velocity could explain these heterogeneities of the fog height.
During the mature phase of the fog, the buildings had little impact on the fog layer characteristics.
The fog dynamics were mainly controlled by processes at its top.
These results suggest that the inclusion of high levels of detail in the building representation remains important for the local forecasting of fog formation.
Particularly, small‐scale heterogeneities can explain the spatial variability of fog formation.
It seems necessary to take small‐scale variability of the urban canopy into account for local and accurate forecasts of fog formation over airport areas.

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