Abstract

Validation and performance evaluations are beneficial for developing methods that estimate the remotely sensed land surface temperature (LST). However, such evaluations for Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data are rare. By selecting the middle reach of the Heihe River basin (HRB), China, as the study area, the atmospheric correction (AC), mono-window (MW), single-channel (SC), and split-window (SW) methods were evaluated based on in situ measured LSTs. Results demonstrate that the influences of surface heterogeneity on the validation are significant in the study area. For the AC, MW, and SC methods, the LSTs estimated from channel 13 are more accurate than those from channel 14 in general cases. When the in situ measured atmospheric profiles are available, the AC method has the highest accuracy, with a root-mean squared error (RMSE) of about 1.4–1.5 K at the homogenous oasis sites. In actual application without sufficient in situ measured inputs, the MW method is highly accurate; the RMSE is around 1.5–1.6 K. The SC method systematically overestimates LSTs and it is sensitive to error in the water vapor content. The two SW methods are simple to use but their performances are limited by accuracies, revealed by the simulation dataset. Therefore, when the in situ atmospheric profiles are available, the AC method is recommended to generate reliable ASTER LSTs for modeling the eco-hydrological processes in the middle reach of the HRB. When sufficient in situ measured inputs are not available, the MW method can be used instead.

Highlights

  • Land surface temperature (LST) is one of the most important parameters at the interface between the earth’s surface and the atmosphere

  • The varying coefficient of variation (CV) of EC04 reveals that the qualities of the calculated normalized difference vegetation index (NDVI) CV values were influenced by the atmospheric correction for the ASTER visible and near infrared (VNIR) images

  • By selecting a flat agricultural oasis and the surrounding bare land as the study area, this study evaluated the performance of four methods that can be applied to ASTER data to estimate the LST: the atmospheric correction (AC) method, the mono-window (MW) method, the single-channel (SC) method, and the split-window (SW) method

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Summary

Introduction

Land surface temperature (LST) is one of the most important parameters at the interface between the earth’s surface and the atmosphere. If the concurrent atmospheric profile (representing the vertical distributions of air temperature, water vapor, etc.) and the LSE were obtained when a TIR image was being acquired, it is possible to quantify the atmospheric influences with an atmospheric radiative transfer model, e.g., MODTRAN [2]. In this case, the LST can be calculated using an inversion method. Many methods have been reported in the literature for estimating LSTs assisted by some input parameters (such as atmospheric profile, water vapor, and LSE), e.g., the single-channel method, the multi-channel method, and the multi-angle method

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