Abstract

The urban thermal environment is closely related to landscape patterns and land surface characteristics. Several studies have investigated the relationship between land surface characteristics and land surface temperature (LST). To explore the effects of the urban landscape on urban thermal environments, multiple land-use/land-cover (LULC) remote sensing-based indices have emerged. However, the function of the indices in better explaining LST in the heterogeneous urban landscape has not been fully addressed. This study aims to investigate the effect of remote-sensing-based LULC indices on LST, and to quantify the impact magnitude of green spaces on LST in the city built-up blocks. We used a random forest classifier algorithm to map LULC from the Gaofen 2 (GF-2) satellite and retrieved LST from Landsat-8 ETM data through the split-window algorithm. The pixel values of the LULC types and indices were extracted using the line transect approach. The multicollinearity effect was excluded before regression analysis. The vegetation index was found to have a strong negative relationship with LST, but a positive relationship with built-up indices was found in univariate analysis. The preferred indices, such as normalized difference impervious index (NDISI), dry built-up index (DBI), and bare soil index (BSI), predicted the LST (R2 = 0.41) in the multivariate analysis. The stepwise regression analysis adequately explained the LST (R2 = 0.44) due to the combined effect of the indices. The study results indicated that the LULC indices can be used to explain the LST of LULC types and provides useful information for urban managers and planners for the design of smart green cities.

Highlights

  • Land surface temperature (LST) is an indispensable parameter that is highly responsive to energy fluxes of the Earth’s surface [1]

  • The mean land surface temperature (LST) pattern was ranked as built-up area > barren land >

  • We found a moderate relationship (R2 = 0.28) between NDWI, normalized difference vegetation index (NDVI), and LST along line transect I, decreased by a little in transect II (R2 = 0.24), and it was found higher in line transects III and IV (R2 = 0.39)

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Summary

Introduction

Land surface temperature (LST) is an indispensable parameter that is highly responsive to energy fluxes of the Earth’s surface [1]. It is crucial to estimate LST because it can be used to assess the effect of surface energy and water exchange with the atmosphere [6]. LST may affect surface energy and water exchange with the overlying atmosphere, and each variable is dependent on the interaction of the land surface with the atmosphere. The urban thermal environment is diverse, and each pixel has a different emissivity due to landscape heterogeneity [9,10]. A study [13] showed an increased spatiotemporal variability of surface temperatures at a high resolution due to boundary-layer turbulence, which induces errors in LST and heat flux estimates. The Geographic Information System (GIS), and remote sensing (RS)

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