A comparative assessment of the accuracies of split-window algorithms for retrieving of land surface temperature using L
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ORIGINAL ARTICLE
A comparative assessment of the accuracies of split‑window algorithms for retrieving of land surface temperature using Landsat 8 data Fahime Arabi Aliabad1 · Mohammad Zare1 · Hamidreza Ghafarian Malamiri2 Received: 13 July 2020 / Accepted: 8 October 2020 © Springer Nature Switzerland AG 2020
Abstract Land surface temperature (LST) is one of the most important physical parameters examined in modeling the land surface processes. There are several algorithms for estimating the LST using satellite imagery. The present study aims to evaluate the accuracy of ten split-window algorithms in estimating the LST using Landsat 8 images in the arid lands. The split-window algorithms were validated by employing the two methods of temperature-based (T-based) and cross-validation. In the T-based validation method, soil temperatures at depth of 5 cm within three meteorological stations were used at 6:30, 12:30, and 18:30 (local time). The land surface temperature was predicted at the moment when satellite overpass by implementing Fourier series. Results of the T-based validation indicated that the Li and Coll algorithms with RMSE values of 5.83 and 8.94 and MADE of 4.60 and 8.04 °C, have the lowest and highest errors, respectively. To conduct the cross-validation and prepare the RMSE statistical index images, the LST images associated with MODIS sensor and those of various split-window algorithms obtained via Landsat images were compared. Results of land-use analysis showed that areas with the RMSE of more than 5 °C, are located in valleys and regions with high humidity. The results of cross-validation showed that the Li and Jiménez’s split-window algorithms are the most accurate methods with RMSEs of 3.65 and 3.57 °C, respectively. The Parata, Price, Sobrino, Uliverii, Mcclain, Vidal, Kerr, and Coll algorithms are in the next grades, respectively. In general, using atmospheric water vapor increases the accuracy of retrieval LST in a split-window algorithm. Keywords Cross-validation · T-based validation · Time series · Remote sensing · Arid lands · Modeling land surface temperature
Introduction Land surface temperature (LST) has been defined as the skin temperature of the earth, that is, a feeling of the hotness of the surface of the earth (Kayet et al. 2016; Stemn and Kumi-Boateng 2020). Temperature is one of the most important physical parameters which controls the transfer and exchange of energy between different layers of the land surface and atmosphere (Wang et al. 2019a, b; Tafesse and Suryabhagavan 2019). In the past, soil temperature was measured point by point with contact thermometers at * Mohammad Zare [email protected] 1
Department of Arid Lands Management, Faculty of Natural Resources and Desert Studies, Yazd University, Yazd, Iran
Department of Geography, Yazd University, Yazd, Iran
2
stationary ground stations. However, due to the severe heterogeneity of the land surface characteristics, such as vegetation, topography, and soil moisture, LST changes rapidly in both time and space. Hen
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