Abstract

Land surface temperature (LST) is a fundamental Earth parameter, on both regional and global scales. We used seven Landsat images to derive LST at Suzhou City, in spring and summer 1996, 2004, and 2016, and examined the spatial factors that influence the LST patterns. Candidate spatial factors include (1) land coverage indices, such as the normalized difference built-up index (NDBI), the normalized difference vegetation index (NDVI), and the normalized difference water index (NDWI), (2) proximity factors such as the distances to the city center, town centers, and major roads, and (3) the LST location. Our results showed that the intensity of the surface urban heat island (SUHI) has continuously increased, over time, and the spatial distribution of SUHI was different between the two seasons. The SUHIs in Suzhou were mainly distributed in the city center, in 1996, but expanded to near suburban, in 2004 and 2016, with a substantial expansion at the highest level of SUHIs. Our buffer-zone-based gradient analysis showed that the LST decays logarithmically, or decreases linearly, with the distance to the Suzhou city center. As inferred by the generalized additive models (GAMs), strong relationships exist between the LST and the candidate factors, where the dominant factor was NDBI, followed by NDWI and NDVI. While the land coverage indices were the LST dominant factors, the spatial proximity and location also substantially influenced the LST and the SUHIs. This work improved our understanding of the SUHIs and their impacts in Suzhou, and should be helpful for policymakers to formulate counter-measures for mitigating SUHI effects.

Highlights

  • Land radiative temperature, more commonly known as Land Surface Temperature (LST) [1,2], is a key Earth surface parameter on regional and global scales [3,4,5]

  • Our results showed the ability of these factors to explain LST variations, with the most influential factor being D-Y in spring 1996 and 2016, normalized difference vegetation index (NDVI) in spring 2004, normalized difference built-up index (NDBI) in summer 1996 and 2004, and normalized difference water index (NDWI) in summer 2016

  • Our results showed that the surface urban heat islands (UHIs) (SUHI) level and magnitude have increased continuously, during the past 20 years, and the spatial distribution of SUHI intensity was different between the two seasons

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Summary

Introduction

More commonly known as Land Surface Temperature (LST) [1,2], is a key Earth surface parameter on regional and global scales [3,4,5]. The warmer areas are known as urban heat islands (UHIs) [7], which can result in local climate change. Understanding LST and SUHI dynamics may improve our awareness of regional environmental change and support sustainable development [13,14]. For this reason, it is important to analyze the spatial patterns of LST and SUHIs and identify their influencing factors

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