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The impact of embedded valleys on daytime pollution transport over a mountain range

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Academic year: 2017

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Figure 1. Idealized model topography of the reference run HMIN0 as (a) vertical cross section (gray shading) and (b) plan view  (show-ing the full domain)
Figure 2. Temporal evolution of mean boundary layer heights of the PLAIN simulation. Shown are three different temperature-based CBL heights and the AL height (see Sect
Figure 3. Cross sections of averaged (a–d) cross-mountain wind speed and (e–h) vertical wind speed as color contours after 6 h of simulation for four different mountain shapes: (from top to bottom) HMIN0, HMIN0.5, HMIN1, and S-RIDGE (cf
Figure 4. Vertical profiles of temporally and spatially averaged cross-mountain wind speed at (a) the middle of slope 1 (x = −18.2 km), (b) the middle of slope 2 (x = −10.7 km), and the middle of slope 3 (x = −3.7 km) for the mountain shapes HMIN0 (solid l
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