Abstract

Land surface temperature (LST) is an important indicator for assessing the surface urban heat island (SUHI) effect. This paper presents a novel approach to derive LST estimates by integrating machine learning algorithm and spatiotemporal fusion model at high spatial and temporal resolution. The spatial resolutions of Landsat TM and Landsat 8 LST data were first downscaled using random forest (RF) algorithm from 120 m and 100 m, respectively, to 30 m. The resultant LST data were fused with MODerate-resolution Imaging Spectroradiometer (MODIS) LST data, by means of the Flexible Spatiotemporal Data Fusion method (FSDAF), in order to generate high spatiotemporal resolution summer daytime LST data covering the center of Chengdu city in China. The proposed new method was used to estimate the spatiotemporal variations of the summer daytime SUHI from 2009 to 2018 over Chengdu city. Results show that: (1) RF performs way better than the classical downscaling algorithm-thermal sharpening algorithm (TsHARP) for LST, and produces higher accuracy for different land covers; (2) the fused high spatiotemporal resolution summer daytime LST values were evaluated with in situ LST obtained from Chengdu Meteorological Office and the final validation results indicated that the proposed method, in generating LST dataset, can provide more details of urban thermal environment and produce higher accuracy than the traditional FSDAF; (3) significantly increasing trends of summer daytime SUHI intensity (SUHII) in the study area were observed. SUHII increased from 2.78 °C in 2009 to 4.04 °C in 2018. The highest and lowest summer daytime LST estimates were recorded over impervious surface area (ISA) and waters, respectively.

Highlights

  • The urban heat island (UHI) refers to the urban centers experiencing higher temperatures than their surrounding rural areas due to human activities, and is one of the most well-known negative impacts of rapid urbanization in local environment, climate, human health and energy consumption [1], [2]

  • In order to further study the impact of urbanization on the urban thermal environment, we investigated the changes of summer mean land surface temperature (LST) data derived from the new method, the traditional Flexible Spatiotemporal Data Fusion method (FSDAF) method and MOD11A2, respectively, over four dominant land cover types, such as impervious surface area (ISA), vegetation, bare soil, and water body during 2009 to 2018

  • Several conclusions were drawn from this research: (1) the performance of the proposed method could predict LST with relatively strong accuracies (R2, average difference (AAD), root mean square error (RMSE) values were in the range of 0.9025-0.9415; 0.027-0.037; 0.082-0.089, respectively)

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Summary

Introduction

The urban heat island (UHI) refers to the urban centers experiencing higher temperatures than their surrounding rural areas due to human activities, and is one of the most well-known negative impacts of rapid urbanization in local environment, climate, human health and energy consumption [1], [2]. Better monitoring and understanding the variation of UHI intensity (UHII) at various temporal (inter-annual, seasonal, diurnal) and spatial (from local to global) scales. Satellite remote sensing provides an unhindered tool for studying UHI, especially the Surface Urban Heat Island (SUHI), which represents the spatial temporal structures of land surface temperature (LST) differences between urban and suburban areas [5]. Various studies have been conducted using satellite derived LST to study SUHI for hundreds of cities around the world [6].

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