4.7 Article

Land Use and Land Cover Mapping with VHR and Multi-Temporal Sentinel-2 Imagery

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REMOTE SENSING
卷 15, 期 10, 页码 -

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MDPI
DOI: 10.3390/rs15102501

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GEOBIA; LULC; temporal analysis; Google Earth Engine; GLCM; VHR

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Land Use/Land Cover (LULC) mapping is the first step in monitoring urban sprawl and its impacts. This study utilizes very high-resolution (VHR) optical imagery to improve object recognition for GEOBIA LULC classification. The results show that adding a single VHR image improves the classification accuracy from 62.62% to 67.05%, and the inclusion of temporal analysis further improves it to 74.30%.
Land Use/Land Cover (LULC) mapping is the first step in monitoring urban sprawl and its environmental, economic and societal impacts. While satellite imagery and vegetation indices are commonly used for LULC mapping, the limited resolution of these images can hamper object recognition for Geographic Object-Based Image Analysis (GEOBIA). In this study, we utilize very high-resolution (VHR) optical imagery with a resolution of 50 cm to improve object recognition for GEOBIA LULC classification. We focused on the city of Nice, France, and identified ten LULC classes using a Random Forest classifier in Google Earth Engine. We investigate the impact of adding Gray-Level Co-Occurrence Matrix (GLCM) texture information and spectral indices with their temporal components, such as maximum value, standard deviation, phase and amplitude from the multi-spectral and multi-temporal Sentinel-2 imagery. This work focuses on identifying which input features result in the highest increase in accuracy. The results show that adding a single VHR image improves the classification accuracy from 62.62% to 67.05%, especially when the spectral indices and temporal analysis are not included. The impact of the GLCM is similar but smaller than the VHR image. Overall, the inclusion of temporal analysis improves the classification accuracy to 74.30%. The blue band of the VHR image had the largest impact on the classification, followed by the amplitude of the green-red vegetation index and the phase of the normalized multi-band drought index.

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