Abstract

In this study, we evaluated three different downscaling approaches to enhance spatial resolution of thermal imagery over Alpine vegetated areas. Due to the topographical and land-cover complexity and to the sparse distribution of meteorological stations in the region, the remotely-sensed land surface temperature (LST) at regional scale is of major area of interest for environmental applications. Even though the Moderate Resolution Imaging Spectroradiometer (MODIS) LST fills the gap regarding high temporal resolution and length of the time-series, its spatial resolution is not adequate for mountainous areas. Given this limitation, random forest algorithm for downscaling LST to 250 m spatial resolution was evaluated. This study exploits daily MODIS LST with a spatial resolution of 1 km to obtain sub-pixel information at 250 m spatial resolution. The nonlinear relationship between coarse resolution MODIS LST (CR) and fine resolution (FR) explanatory variables was performed by building three different models including: (i) all pixels (BM), (ii) only pixels with more than 90% of vegetation content (EM1) and (iii) only pixels with 75% threshold of homogeneity for vegetated land-cover classes (EM2). We considered normalized difference vegetation index (NDVI) and digital elevation model (DEM) as predictors. The performances of the thermal downscaling methods were evaluated by the Root Mean Square Error (RMSE) and the Mean Absolute Error (MAE) between the downscaled dataset and Landsat LST. Validation indicated that the error values for vegetation fraction (EM1, EM2) were smaller than for basic modelling (BM). BM model determined averaged RMSE of 2.3 K and MAE of 1.8 K. Enhanced methods (EM1 and EM2) gave slightly better results yielding 2.2 K and 1.7 K for RMSE and MAE, respectively. In contrast to the EMs, BM showed a reduction of 22% and 18% of RMSE and MAE respectively with regard to Landsat and the original MODIS LST. Despite some limitations, mainly due to cloud contamination effect and coarse resolution pixel heterogeneity, random forest downscaling exhibits a large potential for producing improved LST maps.

Highlights

  • In this study, we used Moderate Resolution Imaging Spectroradiometer (MODIS) datasets to increase spatial resolution of the land surface temperature (LST) images in the Alpine region

  • Since this paper is intended for vegetation analyses, Root Mean Square Error (RMSE) and Mean Absolute Error (MAE) were calculated for seven sharpened images acquired in different seasons

  • Similar situation applied to MAE evaluation index (MAEBM = 1.95 K, MAEEM1 = 1.88 K), which corresponded to an accuracy improvement of 4% compared to basic modelling (BM)

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Summary

Introduction

We used MODIS datasets to increase spatial resolution of the land surface temperature (LST) images in the Alpine region. With the use of different approaches, it was possible to examine in which way explanatory variables explain the spatio-temporal LST distribution within the study area. Thermal remote sensing has significantly contributed to the enhancement of spatio-temporal information about temperature distribution on the surface of the Earth. Land surface temperature (LST) retrieved from remote sensing data at different scales is an essential variable in environmental research studies, e.g., in agricultural management [4,5,6,7], in urban heat island assessment [8,9,10,11,12], for evapotranspiration (ET) modelling [13,14,15,16,17,18] and drought monitoring [5,6,19]

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