4.7 Article

A Simple Normalized Difference Approach to Burnt Area Mapping Using Multi-Polarisation C-Band SAR

期刊

REMOTE SENSING
卷 9, 期 8, 页码 -

出版社

MDPI
DOI: 10.3390/rs9080764

关键词

burnt area; synthetic aperture radar (SAR); polarimetric decomposition; Sentinel-1; RADARSAT-2

资金

  1. Council for Scientific and Industrial Research (CSIR)
  2. National Research Foundation (NRF) of South Africa [94023]

向作者/读者索取更多资源

In fire-prone ecosystems, periodic fires are vital for ecosystem functioning. Fire managers seek to promote the optimal fire regime by managing fire season and frequency requiring detailed information on the extent and date of previous burns. This paper investigates a Normalised Difference alpha-Angle (ND alpha I) approach to burn-scar mapping using C-band data. Polarimetric decompositions are used to derive alpha-angles from pre-burn and post-burn scenes and ND alpha I is calculated to identify decreases in vegetation between the scenes. The technique was tested in an area affected by a wildfire in January 2016 in the Western Cape, South Africa. The quad-pol H-A-alpha decomposition was applied to RADARSAT-2 data and the dual-pol H-alpha decomposition was applied to Sentinel-1A data. The ND alpha I results were compared to a burn scar extracted from Sentinel-2A data. High overall accuracies of 97.4% (Kappa = 0.72) and 94.8% (Kappa = 0.57) were obtained for RADARSAT-2 and Sentinel-1A, respectively. However, large omission errors were found and correlated strongly with areas of high local incidence angle for both datasets. The combined use of data from different orbits will likely reduce these errors. Furthermore, commission errors were observed, most notably on Sentinel-1A results. These errors may be due to the inability of the dual-pol H-alpha decomposition to effectively distinguish between scattering mechanisms. Despite these errors, the results revealed that burnt areas could be extracted and were in good agreement with the results from Sentinel-2A. Therefore, the approach can be considered in areas where persistent cloud cover or smoke prevents the extraction of burnt area information using conventional multispectral approaches.

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