Abstract

This paper illustrates a proposed method for the retrieval of land surface temperature (LST) from the two thermal bands of the LANDSAT-8 data. LANDSAT-8, the latest satellite from Landsat series, launched on 11 February 2013, using LANDSAT-8 Operational Line Imager and Thermal Infrared Sensor (OLI & TIRS) satellite data. LANDSAT-8 medium spatial resolution multispectral imagery presents particular interest in extracting land cover, because of the fine spectral resolution, the radiometric quantization of 12 bits. In this search a trial has been made to estimate LST over Al-Hashimiya district, south of Babylon province, middle of Iraq. Two dates images acquired on 2nd &18th of March 2018 to retrieve LST and compare them with ground truth data from infrared thermometer camera (all the measurements contacted with target by using type-k thermocouple) at the same time of images capture. The results showed that the rivers had a higher LST which is different to the other land cover types, of less than 3.47 C ◦, and the LST different for vegetation and residential area were less than 0.4 C ◦ with correlation coefficient of the two bands 10 and 11 Rbnad10= 0.70, Rband11 = 0.89 respectively, for the imaged acquired on the 2nd of march 2018 and Rband10= 0.70 and Rband11 = 0.72 on the 18th of march 2018. These results confirm that the proposed approach is effective for the retrieval of LST from the LANDSAT-8 Thermal bands, and the IR thermometer camera data which is an effective way to validate and improve the performance of LST retrieval. Generally the results show that the closer measurement taken from the scene center time, a better quality to classify the land cover. The purpose of this study is to assess the use of LANDSAT-8 data to specify temperature differences in land cover and compare the relationship between land surface temperature and land cover types.

Highlights

  • Land surface temperature (LST) play an important role in research on agricultural analyses, effects of urban heat island, and environmental monitoring [1]

  • A series of sensors which have been sent into space, such as the Moderate-resolution Imaging Spectroradiometer (MODIS) aboard Terra and Aqua, Advanced Very High Resolution Radiometer (AVHRR) on series of National Oceanic and Atmospheric Administration (NOAA) satellite, have provided public range global thermal data twice daily, using two long wave infrared (LWIR) bands [17]

  • The Operational Land Imager (OLI) instrument with nine spectral bands in the visible (VIS), near infrared (NIR) (Table 1), and the shortwave infrared (SWIR) spectral regions, while the Thermal Infrared Sensor (TIRS) instrument with two thermal infrared spectral bands in the LWIR respectively centered at 10.9 μm and 12 μm (Table 2)

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Summary

Introduction

Land surface temperature (LST) play an important role in research on agricultural analyses, effects of urban heat island, and environmental monitoring [1]. LST divergences in space and time, measured by satellite remote sensing data, were used for the assessment of a lot of geophysical variables, such as soil moisture, vegetation water stress, evapotranspiration, and thermal inertia [5,6,7]. A series of sensors which have been sent into space, such as the Moderate-resolution Imaging Spectroradiometer (MODIS) aboard Terra and Aqua, Advanced Very High Resolution Radiometer (AVHRR) on series of National Oceanic and Atmospheric Administration (NOAA) satellite, have provided public range global thermal data twice daily, using two long wave infrared (LWIR) bands [17]. LANDSAT-8 was successfully launched on the 11th of February 2013 into space with two instrument on board, the Operational Land Imager (OLI) and the Thermal Infrared Sensor (TIRS) [18]. The objective of this paper is to retrieve LST and compare them with trained and validated ground truth data from infrared thermometer camera (IR thermometer) at the same time the images were acquired

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