Abstract

The lower spatial resolution of thermal infrared (TIR) satellite images and derived land surface temperature (LST) is one of the biggest challenges in mapping temperature at a detailed map scale. An extensive range of scientific and environmental applications depend on the availability of fine spatial resolution temperature data. All satellite-based sensor systems that are equipped with a TIR detector depict a spatial resolution that is coarser than most of the multispectral bands of the same system. Certain studies may therefore be not feasible if applied in areas that depict a high spatial variation in temperature at small spatial scales, such as urban centers and flooded pristine areas. To solve this problem, this study applied an image downscaling method to enhance the spatial resolution of LST data by combining TIR, multispectral images, and derived data, such as Normalized Difference Vegetation Index (NDVI), according to the geographically weighted regression (GWRK) and area-to-point kriging of regressed residuals. The resulting LST images of the natural and anthropogenic urban areas of the Brazilian Pantanal are very highly correlated to the reference LST images. The approach, combining ASTER TIR with ASTER visible/infrared (VNIR) and Sentinel-2 images according to the GWRK method, performed better than all of the remaining state-of-the-art downscaling methods.

Highlights

  • The precise estimation of the spatiotemporal variation of the land surface temperature (LST) is a key aspect employed to describe the processes of surface energy balance [1,2], soil surface moisture, and evapotranspiration [3,4,5], as well as to understand trends in future climatic change on various spatial scales [6,7]

  • The current thermal infrared (TIR) orbital sensors suitable for studying urban and natural regions that are characterized by high spatial variability at small spatial scales, such as Landsat-8 TIRS and ASTER TIR, depict a much coarser spatial resolution than is required to perform detailed studies

  • There are still a few remote sensing satellites equipped with thermal sensors that acquire imagery data at high spatial and temporal resolutions

Read more

Summary

Introduction

The precise estimation of the spatiotemporal variation of the land surface temperature (LST) is a key aspect employed to describe the processes of surface energy balance [1,2], soil surface moisture, and evapotranspiration [3,4,5], as well as to understand trends in future climatic change on various spatial scales [6,7]. The current thermal infrared (TIR) orbital sensors suitable for studying urban and natural regions that are characterized by high spatial variability at small spatial scales, such as Landsat-8 TIRS and ASTER TIR, depict a much coarser spatial resolution than is required to perform detailed studies. Both ASTER and Landsat-8 missions provide LST data with the highest spatial resolution among all of the optical satellite missions and depict spatial resolutions of 90 and 100 m, respectively. The downscaling of LST data provides surface temperature products with higher spatial resolutions that can be used to investigate UHI and regional evapotranspiration, as well as to perform several other studies related to the measurement of surface temperature [12]

Objectives
Methods
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