Research Article

Korean J. Remote Sens. 2024; 40(4): 397-418

Published online: August 31, 2024

https://doi.org/10.7780/kjrs.2024.40.4.7

© Korean Society of Remote Sensing

Comparison of Lambertian Model on Multi-Channel Algorithm for Estimating Land Surface Temperature Based on Remote Sensing Imagery

A Sediyo Adi Nugraha1,2 , Muhammad Kamal3* , Sigit Heru Murti4, Wirastuti Widyatmanti4

1PhD Candidate, Major in Geographical Sciences, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia
2Assistant Professor, Department of Geography, Faculty of Law and Social Science, Universitas Pendidikan Ganesha, Bali, Indonesia
3Professor, Department of Geographic Information Science, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia
4Associate Professor, Department of Geographic Information Science, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia

Correspondence to : Muhammad Kamal
E-mail: m.kamal@ugm.ac.id

Received: June 30, 2024; Revised: August 14, 2024; Accepted: August 19, 2024

This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (https://creativecommons.org/licenses/by-nc/4.0/) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

The Land Surface Temperature (LST) is a crucial parameter in identifying drought. It is essential to identify how LST can increase its accuracy, particularly in mountainous and hill areas. Increasing the LST accuracy can be achieved by applying early data processing in the correction phase, specifically in the context of topographic correction on the Lambertian model. Empirical evidence has demonstrated that this particular stage effectively enhances the process of identifying objects, especially within areas that lack direct illumination. Therefore, this research aims to examine the application of the Lambertian model in estimating LST using the Multi-Channel Method (MCM) across various physiographic regions. Lambertian model is a method that utilizes Lambertian reflectance and specifically addresses the radiance value obtained from Sun-Canopy-Sensor (SCS) and Cosine Correction measurements. Applying topographical adjustment to the LST outcome results in a notable augmentation in the dispersion of LST values. Nevertheless, the area physiography is also significant as the plains terrain tends to have an extreme LST value of ≥ 350 K. In mountainous and hilly terrains, the LST value often falls within the range of 310–325 K. The absence of topographic correction in LST results in varying values: 22 K for the plains area, 12–21 K for hilly and mountainous terrain, and 7–9 K for both plains and mountainous terrains. Furthermore, validation results indicate that employing the Lambertian model with SCS and Cosine Correction methods yields superior outcomes compared to processing without the Lambertian model, particularly in hilly and mountainous terrain. Conversely, in plain areas, the Lambertian model’s application proves suboptimal. Additionally, the relationship between physiography and LST derived using the Lambertian model shows a high average R2 value of 0.99. The lowest errors (K) and root mean square error values, approximately ±2 K and 0.54, respectively, were achieved using the Lambertian model with the SCS method. Based on the findings, this research concluded that the Lambertian model could increase LST values. These corrected values are often higher than the LST values obtained without the Lambertian model.

Keywords Lambertian model, Sun-Canopy-Sensor, Cosine correction

Research Article

Korean J. Remote Sens. 2024; 40(4): 397-418

Published online August 31, 2024 https://doi.org/10.7780/kjrs.2024.40.4.7

Copyright © Korean Society of Remote Sensing.

Comparison of Lambertian Model on Multi-Channel Algorithm for Estimating Land Surface Temperature Based on Remote Sensing Imagery

A Sediyo Adi Nugraha1,2 , Muhammad Kamal3* , Sigit Heru Murti4, Wirastuti Widyatmanti4

1PhD Candidate, Major in Geographical Sciences, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia
2Assistant Professor, Department of Geography, Faculty of Law and Social Science, Universitas Pendidikan Ganesha, Bali, Indonesia
3Professor, Department of Geographic Information Science, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia
4Associate Professor, Department of Geographic Information Science, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia

Correspondence to:Muhammad Kamal
E-mail: m.kamal@ugm.ac.id

Received: June 30, 2024; Revised: August 14, 2024; Accepted: August 19, 2024

This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (https://creativecommons.org/licenses/by-nc/4.0/) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

The Land Surface Temperature (LST) is a crucial parameter in identifying drought. It is essential to identify how LST can increase its accuracy, particularly in mountainous and hill areas. Increasing the LST accuracy can be achieved by applying early data processing in the correction phase, specifically in the context of topographic correction on the Lambertian model. Empirical evidence has demonstrated that this particular stage effectively enhances the process of identifying objects, especially within areas that lack direct illumination. Therefore, this research aims to examine the application of the Lambertian model in estimating LST using the Multi-Channel Method (MCM) across various physiographic regions. Lambertian model is a method that utilizes Lambertian reflectance and specifically addresses the radiance value obtained from Sun-Canopy-Sensor (SCS) and Cosine Correction measurements. Applying topographical adjustment to the LST outcome results in a notable augmentation in the dispersion of LST values. Nevertheless, the area physiography is also significant as the plains terrain tends to have an extreme LST value of ≥ 350 K. In mountainous and hilly terrains, the LST value often falls within the range of 310–325 K. The absence of topographic correction in LST results in varying values: 22 K for the plains area, 12–21 K for hilly and mountainous terrain, and 7–9 K for both plains and mountainous terrains. Furthermore, validation results indicate that employing the Lambertian model with SCS and Cosine Correction methods yields superior outcomes compared to processing without the Lambertian model, particularly in hilly and mountainous terrain. Conversely, in plain areas, the Lambertian model’s application proves suboptimal. Additionally, the relationship between physiography and LST derived using the Lambertian model shows a high average R2 value of 0.99. The lowest errors (K) and root mean square error values, approximately ±2 K and 0.54, respectively, were achieved using the Lambertian model with the SCS method. Based on the findings, this research concluded that the Lambertian model could increase LST values. These corrected values are often higher than the LST values obtained without the Lambertian model.

Keywords: Lambertian model, Sun-Canopy-Sensor, Cosine correction

KSRS
August 2024 Vol. 40, No.4, pp. 319-418

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Korean Journal of Remote Sensing