Abstract

This article presents the burned area (BA) product of the Copernicus Climate Change Service (C3S) of the European Commission. This product, named C3SBA10, is based on the adaptation to Sentinel-3 OLCI images of a BA algorithm developed within the Fire Climate Change Initiative (FireCCI) project, which used MODIS data. We first reviewed the adaptation process and then analysed the results of both products for common years (2017–2019). Comparisons were performed using four different grid sizes (0.05°, 0.10°, 0.25°, and 0.50°). Annual correlations between the two products ranged from 0.94 to 0.99. Global BA estimates were found to be more similar when the two Sentinel-3 satellites were active (2019), as the temporal resolution was closer to that of the MODIS sensor. Global validation was performed using reference data derived from Landsat-8 images, following a stratified random sampling design. The C3SBA10 showed commission errors between 16 and 21% and omission errors from 48 to 50%, similar to those found in the FireCCI product. The temporal reporting accuracy was also validated using 19 million active fires. In total, 87% of the detections were made within 10 days after the fire by both products. The high consistency between both products ensures global BA data provision from 2001 to the present. The datasets are freely available through the Copernicus Climate Data Store (CDS) repository.

Highlights

  • Interactions between climate and fire are bidirectional

  • This paper presents the adaptation of the FireCCI51 burned area (BA) algorithm to the Ocean and Land Colour Instrument (OLCI) sensor and the generation of the new BA dataset, named C3SBA10, which is part of the

  • The third variable was generated from neighbour active fires that are sufficiently close in space (

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Summary

Introduction

Climate impacts fire regimes [1,2,3,4], mostly by modifying temperature and precipitation patterns, which in turn impacts fire ignition and behaviour through changes in soil and fuel moisture, vegetation productivity, and fuel availability [5,6,7,8]. Emissions from fires increase aerosol optical depth, modifying the radiation budget and, warming the lower atmosphere, which affects regional temperature, clouds, and precipitation patterns [14,15]. Fires have important ecological implications as well. They are closely related to biodiversity, either favouring or degrading it depending on fire severity and persistency [16,17,18]

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