Abstract

Land surface temperature (LST) is a critical parameter of surface energy fluxes and has become the focus of numerous studies. LST downscaling is an effective technique for supplementing the limitations of the coarse-resolution LST data. However, the relationship between LST and other land surface parameters tends to be nonlinear and spatially nonstationary, due to spatial heterogeneity. Nonlinearity and spatial nonstationarity have not been considered simultaneously in previous studies. To address this issue, we propose a multi-factor geographically weighted machine learning (MFGWML) algorithm. MFGWML utilizes three excellent machine learning (ML) algorithms, namely extreme gradient boosting (XGBoost), multivariate adaptive regression splines (MARS), and Bayesian ridge regression (BRR), as base learners to capture the nonlinear relationships. MFGWML uses geographically weighted regression (GWR), which allows for spatial nonstationarity, to fuse the three base learners’ predictions. This paper downscales the 30 m LST data retrieved from Landsat 8 images to 10 m LST data mainly based on Sentinel-2A images. The results show that MFGWML outperforms two classic algorithms, namely thermal image sharpening (TsHARP) and the high-resolution urban thermal sharpener (HUTS). We conclude that MFGWML combines the advantages of multiple regression, ML, and GWR, to capture the local heterogeneity and obtain reliable and robust downscaled LST data.

Highlights

  • IntroductionLand surface temperature (LST) refers to the radiative temperature of the Earth’s surface

  • Ebrahimy and Azadbakht (2019) [25] compared the random forest (RF), support vector machine (SVM), and extreme learning machine (ELM) for the spatial downscaling of Moderate Resolution Imaging Spectroradiometer (MODIS) Land surface temperature (LST) data, and the results showed that the RF and ELM outperformed the SVM

  • The results demonstrate that the two factors in the high-resolution urban thermal sharpener (HUTS) model are incapable of capturing the two factors in the HUTS model are incapable of capturing the LST heterogeneity

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Summary

Introduction

Land surface temperature (LST) refers to the radiative temperature of the Earth’s surface. LST is highly responsive to the interactions between the land surface and the atmosphere, water circulation, and energy exchange from the local scale to the global scale [1]. LST is an essential parameter in various environmental research fields, including climate change and urban heat island effect monitoring [2,3]; land-surface carbon, water, energy, and evapotranspiration mapping [4,5]; soil moisture condition and drought assessment [6,7]; and forest fire detection [8]. Accurate LST measurements at different scales can facilitate these environmental monitoring studies. Accurate LST measurements at different scales can facilitate these environmental monitoring studies. 4.0/).

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