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From weak to intense downslope winds: origin, interaction with boundary layer turbulence and impact on CO2 variability

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Table 1. Specifications about the variables measured and the devices employed in this study over the intensive summer 2017 campaign (22 June–26 September).
Table 2. Algorithm for thermally driven downslope criteria. First column indicates the filter number; second column shows the physical description of the filter; third column lists the criteria to be fulfilled in order to pass each of the filters.
Figure 3. Box plots of the wind-speed profile at 3, 6 and 10 m for the downslope events, (a) at the time of the onset and (b) at the time of the maximum value at 6 m (from the onset to 00:00 UTC) for each event
Figure 5. Wind roses representing the maximum downslope wind speed at 6 m in colours, for different directions from the National Centers for Environmental Prediction (NCEP) reanalysis wind at 850 hPa, at the closest grid point from La Herrería (40.5 ◦ N, 4
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