Estimation of Land Surface Temperature in Northeast, Thailand Using Multi – Temporal Satellite Imageries

Authors

  • Marisa Mhokprakhon
  • Marisa Mhokprakhon
  • Thanyarat Chaiyakarm ภาควิชาภูมิศาสตร์ คณะมนุษยศาสตร์และสังคมศาสตร์ มหาวิทยาลัยมหาสารคาม

Abstract

The objectives of this research were 1) to estimate land surface temperature in the Northeast during 2000 to 2020, 2) to study the relationship between surface temperature and land cover, and 3) to study the relationship between land surface temperature and populations. This research studied the data from Terra/Aqua - MODIS satellite images and Landsat 8 image data from OLI (Operational Land Imager)/TIRS (Thermal Infrared Sensor) satellites using remote sensing techniques to evaluate the Normalized Difference Built-up Index (NDBI) and Normalized difference vegetation index (NDVI). The relationship between land surface temperature and land cover and population density was then determined using a simple linear regression equation. The results of the estimation of land surface temperature in the Northeast from 2000 to 2020 in each province had higher land surface temperature in all provinces both in summer and winter. The highest was 43.55 degrees celsius in ‎Nakhon Ratchasima province and Loei province had the lowest surface temperature at 16.71 degrees celsius, and by comparison, the difference between surface temperatures was 26.84 degrees celsius. It is found that the land surface temperature during summer is presumably higher than winter. Provinces with high temperature including Roi-Et, Maha Sarakham, Yasothorn, Bureeram and Surin. Meanwhile in Nong Khai, Chaiyaphum, Mukdaharn, Sakhon Nakorn and Buengkan are recorded as the provinces with lowest land surface temperature. The research also found that the relations between land surface temperature with land cover and its population; with the normalized difference vegetation index: NDVI and the normalized difference Built-up Index: NDBI have its high relation which are equal (R2) = 0.9318 and 0.897 chronologically. Additionally, the relation between land surface temperature and its population have resulted in (R2) = 0.6159 which is resulted in a median level. The relation between land surface temperature and its the density of population have resulted in (R2) = 0.0734 which is resulted in a low level. Keywords :  estimation ; land surface temperature ; multi – temporal satellite imageries

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Published

2023-01-04