Urban land-surface schemes simulate exchanges between the urban surface and the first layer of larger-scale atmospheric models. Note that with changing wind direction the frontal area index will vary. For example, with respect to the capability of the 33 models: five that model vegetation in a separate tile (Vs), have slab morphology (L1) while in application to the VL92 dataset, only two were run this way.ĭefinitions of fundamental morphometric parameters (see Table 3). 2) gives this combination of approaches: (top right) the capability of the models and (bottom left) how the models were applied for the VL92 runs analyzed here. In (b), the dagger symbol indicates that one is also 343 and § indicates that one is 3P3 and one is 343.Īnalysis of the individual characteristics ( Fig. (c) Combined features GZA or “Other” used in the turbulent flux modeling for the VL92 runs with the numbers in each class shown. (b) Approaches used to simulate the built (B) and vegetated (V) turbulent heat fluxes ( Q H, Q E). Classes with few models (asterisks) are amalgamated for analysis. (a) Class code and number of models that have this capability (cap) and were applied this way for VL92. 2).Ĭharacteristics used to classify the models (see Fig. Characteristics used to classify models (see Fig.
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