Abstract
Over the past few decades, there has been a rapid change in forest and land cover, especially in tropical forests due to massive deforestation. The major factor responsible for the changes is to fulfill the growing demand of increasing population through agricultural intensification, rural settlements, and urbanization. Monitoring forest cover and vegetation are essential for detecting regional and global environmental changes. The present study evaluates the influence of deforestation on land surface temperature (LST) in the states of Kedah and Perak, Malaysia, between 1988 and 2017. The trend in forest cover change over the time span of 29 years, was analyzed using Landsat 5 and Landsat 8 satellite images to map the sequence of forest cover change. With the measurement of deforestation and its relationship with LST as an end goal, the Normalized Difference Vegetation Index (NDVI) was used to determine forest health, and the spectral radiance model was used to extract the LST. The findings of the study show that nearly 16% (189,423 ha) of forest cover in Perak and more than 9% (33,391 ha) of forest cover in Kedah have disappeared within these 29 years as a result of anthropogenic activities. The correlation between the LST and NDVI is related to the distribution of forests, where LST is inversely related to NDVI. A strong correlation between LST and NDVI was observed in this study, where the average mean of LST in Kedah (25 °C) is higher than in Perak (22.6 °C). This is also reflected by the decreased NDVI value from 0.6 to 0.5 in 2017 at both states. This demonstrated that a decrease in the vegetation area leads to an increase in the surface temperature. The resultant forest change map would be helpful for forest management in terms of identifying highly vulnerable areas. Moreover, it could help the local government to formulate a land management plan.
Highlights
Land cover and land use change are one of the major drivers that affect land surface temperature (LST)
58% in 1988 to 49% and forest cover in Kedah dropped from 39% in 1988 to 35% in 2017. This has led to more open areas and deforestation, causing an increase in LST
It was observed that areas with vegetation and forest had lower LST
Summary
Land cover and land use change are one of the major drivers that affect land surface temperature (LST). This relation is even more pronounced at urban forest interfaces where forests are crucial in maintaining micro and regional climate [1]. Deforestation can accelerate climate warming, directly as a result of surface albedo and indirectly due to the increase of greenhouse gasses. It is one of the main causes of biodiversity loss around the world [3]. Deng et al agreed that vegetation could effectively influence land surface temperature (LST) by selectively absorbing and reflecting solar radiation energy and regulating latent and sensible heat exchange
Sign-in/Register to view highlights & summary 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 callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
