2019
DOI: 10.1016/j.atmosres.2019.05.018
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Turbulence parameterizations for dispersion in sub-kilometer horizontally non-homogeneous flows

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Cited by 27 publications
(27 citation statements)
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“…The parameters in these schemes are therefore sometimes modified/tuned, or additional parameters are added. This has been done, for example, to represent some orographic effects in a surface layer scheme for improved simulations of surface wind speeds in complex terrain [151], and in an ABL scheme for an improved representation of dispersion processes in an alpine valley [152]. However, few if any large-scale datasets exist with which to evaluate these parameterizations in complex terrain.…”
Section: Conclusion and Thoughts On Future Researchmentioning
confidence: 99%
“…The parameters in these schemes are therefore sometimes modified/tuned, or additional parameters are added. This has been done, for example, to represent some orographic effects in a surface layer scheme for improved simulations of surface wind speeds in complex terrain [151], and in an ABL scheme for an improved representation of dispersion processes in an alpine valley [152]. However, few if any large-scale datasets exist with which to evaluate these parameterizations in complex terrain.…”
Section: Conclusion and Thoughts On Future Researchmentioning
confidence: 99%
“…In particular, an improved TKE can be obtained by suitably varying the length scales. The best results for the TKE are found using the TCF set of constants, as also found by Tomasi et al (2019). It is worth noting that this set of constants was derived from data measured in non-homogeneous conditions (Trini Castelli et al 1999).…”
Section: General Conclusionmentioning
confidence: 67%
“…From Figure 4a, it can be seen that the whole month of December was characterized by the “cold winter day” class. Further details on the meteorological conditions that occurred in the Bolzano basin during December 2015 are reported in Figure 5, highlighting that the weather was characterized by minimum temperatures below 0°C, as typical during wintertime, due to persistent ground‐based thermal inversions associated with calm wind conditions (Giovannini et al., 2017; Tomasi et al., 2019). In particular, the days simulated (highlighted by the gray‐shaded area) were characterized by clear‐sky conditions, with minimum temperatures around the average of the reference period 1981–2010 (∼−3°C), and maximum temperatures slightly above average values (∼9°C).…”
Section: Methodsmentioning
confidence: 99%