Abstract

Land surface temperature (LST) is an important environmental parameter in climate change, urban heat islands, drought, public health, and other fields. Thermal infrared (TIR) remote sensing is the main method used to obtain LST information over large spatial scales. However, cloud cover results in many data gaps in remotely sensed LST datasets, greatly limiting their practical applications. Many studies have sought to fill these data gaps and reconstruct cloud-free LST datasets over the last few decades. This paper reviews the progress of LST reconstruction research. A bibliometric analysis is conducted to provide a brief overview of the papers published in this field. The existing reconstruction algorithms can be grouped into five categories: spatial gap-filling methods, temporal gap-filling methods, spatiotemporal gap-filling methods, multi-source fusion-based gap-filling methods, and surface energy balance-based gap-filling methods. The principles, advantages, and limitations of these methods are described and discussed. The applications of these methods are also outlined. In addition, the validation of filled LST values’ cloudy pixels is an important concern in LST reconstruction. The different validation methods applied for reconstructed LST datasets are also reviewed herein. Finally, prospects for future developments in LST reconstruction are provided.

Highlights

  • The existing reconstruction algorithms can be grouped into five categories: spatial gap-filling methods, temporal gap-filling methods, spatiotemporal gap-filling methods, multi-source fusion-based gapfilling methods, and surface energy balance-based gap-filling methods

  • These results indicated that the method performed well for unevenly distributed invalid Land surface temperature (LST) pixels, but there was some residual noise in the reconstructed LST

  • This reconstruction method is dependent on the quality of the Terra/MODIS and Aqua/MODIS LST obtained on the same day and might fail to produce completely gap-filled LST series under a persistent cloud cover

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Summary

Introduction

LST plays a key role in the energy balance of the Earth–atmosphere system as well as in ecosystems [1,2,3,4]. LST is widely used in various fields, including urban heat islands, drought disasters, and public health [5,6,7,8,9], and is an important input variable in. Earth system models, such as meteorological, ecological, hydrological, and biological models [10,11,12,13]. Field measurements can provide only a limited number of point-scale LST observations and cannot effectively characterize the spatial details of thermal environments. The data gaps caused by cloud cover obviously limit the application of remotely sensed LST datasets.

Bibliometric Analysis of the Published Literature on LST Reconstruction under
Variations in the Number of Published Papers
Most Relevant Journals
Most-Cited Papers
Most-Contributed Countries
Temperature Datasets Used for LST Reconstruction
LST from Polar-Orbiting Satellite Thermal Infrared Data
LST from Geostationary Satellite Thermal Infrared Data
Subsurface Temperature from Space-Borne Microwave Data
Temperature from Reanalysis Data
Spatial Gap-Filling Methods
Temporal Gap-Filling Methods
Spatiotemporal Gap-Filling Methods
Multi-Source Fusion-Based Gap-Filling Methods
Surface Energy Balance-Based Gap-Filling Methods
SURFRAD stations in the conterminous
Validation of Reconstructed LST
Validations Based on Artificially Simulated Cloud-Contaminated LST
Validations Based on Ground-Observed LST Data
Validations Based on Meteorological Station-Observed Temperature Data
Validations Based on Gridded Temperature Data from Other Sources
Conclusions and Perspectives
Findings
Method
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