Scaling intra-urban climate fluctuations
Marc Duran-Sala, Martin Hendrick, Gabriele Manoli
TL;DR
Urban climate variability within cities exhibits sensitivity to urban form, yet boundary-based scaling introduces biases. The authors assemble high-resolution data for $T$ and $PM_{2.5}$ across $142$ cities and link intra-urban fluctuations to a logarithmic dependence on urban features $x$ via $\Delta y = \alpha + \beta \ln x$, revealing a universal location–scale scaling form. After rescaling by city-specific means and variances, marginal and joint PDFs of $T$ and $PM_{2.5}$ collapse onto a common function $G$, approximately Gaussian, with clustering into $K=3$ groups improving collapse without altering $G$. A stochastic radial-decay extension, $\Delta y(r) = y_A \exp(-r^2/(2\lambda_y^2)) + \mathcal{N}(0,\sigma_{r,city}^2)$, reconciles traditional decay models with observed Gaussian statistics, linking urban morphology to intra-urban climate variability and enabling downscaling and planning applications.
Abstract
Urban-induced changes in local microclimate, such as urban heat islands and air pollution, are known to vary with city size, leading to distinctive relations between average climate variables and city-scale quantities (e.g., total population). However, these approaches suffer from biases related to the choice of city boundaries and they neglect intra-urban variations of urban characteristics. Here, we use high-resolution data of urban temperatures, air quality, population, and street networks from 142 cities worldwide and show that their marginal and joint probability distributions collapse onto a set of general scaling functions. Using a logarithmic relation between urban spatial features and climate variables, we find that average street network properties are sufficient to characterize the entire variability of the temperature and air pollution fields observed within and across cities. These findings provide a unified statistical framework for characterizing intra-urban climate variability, with important implications for climate modeling and urban planning.
