Abstract

Abstract. Due to rapid urbanization and intense human activities, the urban heat island (UHI) effect has become a more concerning climatic and environmental issue. A high-spatial-resolution canopy UHI monitoring method would help better understand the urban thermal environment. Taking the city of Nanjing in China as an example, we propose a method for evaluating canopy UHI intensity (CUHII) at high resolution by using remote sensing data and machine learning with a random forest (RF) model. Firstly, the observed environmental parameters, e.g., surface albedo, land use/land cover, impervious surface, and anthropogenic heat flux (AHF), around densely distributed meteorological stations were extracted from satellite images. These parameters were used as independent variables to construct an RF model for predicting air temperature. The correlation coefficient between the predicted and observed air temperature in the test set was 0.73, and the average root-mean-square error was 0.72 ∘C. Then, the spatial distribution of CUHII was evaluated at 30 m resolution based on the output of the RF model. We found that wind speed was negatively correlated with CUHII, and wind direction was strongly correlated with the CUHII offset direction. The CUHII reduced with the distance to the city center, due to the decreasing proportion of built-up areas and reduced AHF in the same direction. The RF model framework developed for real-time monitoring and assessment of high spatial and temporal resolution (30 m and 1 h) CUHII provides scientific support for studying the changes and causes of CUHII, as well as the spatial pattern of urban thermal environments.

Highlights

  • Throughout the world, cities have formed rapidly due to population growth and people gathering in certain areas to settle and build their lives

  • Based on the random forest (RF) model and combined with local environment and background weather data, the pattern and causes of canopy urban heat island (CUHI) can be analyzed in detail

  • The canopy UHI intensity (CUHII) in the southeast direction was strong (Fig. 10b), which was mainly affected by the heat transport of the prevailing winds (Chuanyan et al, 2005), causing the CUHI to shift toward the downwind area

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Summary

Introduction

Throughout the world, cities have formed rapidly due to population growth and people gathering in certain areas to settle and build their lives. Such urbanization brings economic development and the urban heat island (UHI) phenomenon (Oke, 1982; Mirzaei, 2015; Cao et al, 2016; Zhao et al, 2020). The UHI effect has become an indisputable fact and brings adverse impacts on urban ecology and energy consumption UHIs have the potential to impact vegetation phenology (Kabano et al, 2021), diurnal temperature

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