To this end, Local Climate Zones’ information (Stewart and Oke 2012), obtained following the WUDAPT framework (Ching et al. 2018), are fed them into the urban canopy model TERRA-URB (Wouters et al. 2016, Brousse et al. 2019) embedded in the COSMO-CLM model. The COSMO-CLM model is then run at a convection permitting scale of 2.8 km horizontal resolution, forced by ERA5 reanalysis data, before dynamically downscaling at 1 km over Kampala. Model outputs are evaluated against cloud-free land surface temperature, and precipitation measurements from satellite observations for the period 2010-2015.
Model outputs are used to calculate the dynamic temperature suitability index (TSI) proposed by Gething et al. (2011) to capture the temporal and seasonal evolution of the TSI. Brousse et al. (2019) already demonstrated using the static TSI – which doesn’t account for the temporal variability – that the urbanization of Kampala could lead to a 30% increase of the TSI in the city. In fact, this measure calculates the vectorial capacity of an environment for the development of malaria-infected mosquitoes out of air temperature. Thereby, hotter urban areas could have higher vectorial capacities. Hence, we also compute the effect of relative humidity on the survival of mosquitoes following Yamana and Eltahir (2013) in order to see how the dryer city may also influence the TSI. Both results of the suitability modelling are compared temporally and spatially.