Visit our poster on Monday, 11 May 2015 in the Poster Area C02 on Level C during 15:30 – 18:00  

Since the rate of warming in cities is higher than the average global warming, both urban planning and Earth system science communities need spatially disaggregated anthropogenic heat emission data; such information is practically impossible to derive by point in-situ fluxes measurements, while satellite remote sensing is considered in URBANFLUXES as a valuable tool for estimating the Urban Energy Budget (UEB) parameters. The basic idea behind URBANFLUXES is to break down UEB and to quantify the anthropogenic heat flux patterns of day and night, week and weekend, summer and winter times, by combining observations form different Copernicus Sentinels satellite missions. The anthropogenic heat flux is the heat flux resulting from vehicular emissions, space heating and cooling of buildings, industrial processing and the metabolic heat release by people. In URBANFLUXES, the UEB is considered in the context of a volume because of the three-dimensional nature of cities:

The urban surface energy budget is defined: Q* + Q_F = Q_H + Q_E + ΔQ_S + ΔQ_A + S, where Q_F is the anthropogenic heat flux, Q* is the net all-wave radiation flux, Q_H is the turbulent sensible heat flux and Q_E is the latent heat flux, ΔQ_S is the heat storage, ΔQ_A = Q_in – Q_out and S represents all other sources and sinks, within the control volume shown in this figure.

The major challenge for URBANFLUXES is the innovative exploitation of Copernicus Sentinels data to estimate the spatiotemporal patterns all UEB fluxes. The main research question is whether EO is able to provide reliable estimates of anthropogenic heat flux for the time of the satellite acquisition. URBANFLUXES will address it by combining Sentinels observations with conventional meteorological measurements, developing new methods for estimating each UEB term. The energy balance residual approach will be employed to estimate the anthropogenic heat flux: the anthropogenic heat flux will be estimated by regressing the turbulent heat fluxes vs available energy, for every pixel in each Local Climate Zone. The main assumptions in URBANFLUXES are: the energy consumed in buildings is released into the environment after use and the advection term is included in the error of the energy balance closure.

By exploiting Copernicus Sentinels synergistic observations, URBANFLUXES is expected to:

• generate a novel EO-based method for estimation of UEB, easily transferable to any urban area and enabling its integration into operational applications, as for example the evaluation of the implementation of climate change mitigation technologies such as solar-screening, green-belting and carbon-cooling.
• advance the current knowledge of the impacts of UEB fluxes on urban heat island and hence on urban climate and energy consumption and ssupport the development of tools and strategies to mitigate these effects, improving thermal comfort and energy efficiency.
• provide anthropogenic heat emissions benchmark data for different applications (UEB models, building energy models, etc.) and develop EO-based services capable of supporting urban planning.