Abstract

Generating spatiotemporally continuous land surface temperature (LST) data is in great demand for hydrology, meteorology, ecology, environmental studies, etc. However, the thermal infrared (TIR)-based LST measurements are prone to cloud contamination with missing pixels. To repair the missing pixels, a new XGBoost-based linking approach for reconstructing daytime and nighttime Moderate Resolution Imaging Spectroradiometer (MODIS) LST measurements was introduced. The instantaneous solar radiation and two soil-related predictors from China Data Assimilation System (CLDAS) 0.0625°/1-h data were selected as the linking variables to depict the relationship with instantaneous MODIS LST data. Other land surface properties, including two vegetation indices, the water index, the surface albedo, and topographic parameters, were also used as the predictor variables. The XGBoost method was used to fit an LST linking model by the training datasets from clear-sky pixels and was then applied to the MODIS Aqua-Terra LSTs during summer time (June to August) in 2017 and 2018 across China. The recovered LST data was further rectified with the Savitzky–Golay (SG) filtering method. The results showed the distribution of the reconstructed LSTs present a reasonable pattern for different land-cover types and topography. The evaluation results using in situ longwave radiation measurements showed the RMSE varies from 3.91 K to 5.53 K for the cloud-free pixels and from 4.42 K to 4.97 K for the cloud-covered pixels. In addition, the reconstructed LST products correlated well with CLDAS LST data with similar LST spatial patterns. The variable importance analysis revealed that the two soil-related predictors and the elevation variable are key parameters due to their great contribution to the XGBoost model performance.

Highlights

  • Land surface temperature (LST) is a key parameter in environmental change, ecological processes and land-atmosphere energy exchange for different spatial scopes [1,2,3,4]

  • The quality of Thermal infrared (TIR)-based LST data were greatly affected by frequent cloud cover, which severely restricted their applications in many related scientific fields

  • To explore a practical method for the reconstruction of missing data in TIR-based LSTs is of great significance

Read more

Summary

Introduction

Land surface temperature (LST) is a key parameter in environmental change, ecological processes and land-atmosphere energy exchange for different spatial scopes [1,2,3,4]. It enables monitoring of agricultural drought, urban heat, surface energy fluxes, and hydrological and meteorological processes [5,6,7,8,9,10,11], etc. Thermal infrared (TIR)-based methods, such as single-channel, split-window, and mono-window algorithms [13,15,16,17,18], have been widely used to retrieve satellite-based LST data. Compared with LST retrieval from PMW sensors, the TIR-based LST data has attracted more attention due to its finer

Objectives
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call