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Identified main fire hotspots and seasons in Côte d’Ivoire (West Africa) using MODIS fire data
Author(s) -
Tionhonkélé Drissa Soro,
M. Koné,
Aya Brigitte N’Dri,
N’Datchoh Evelyne Touré
Publication year - 2021
Publication title -
south african journal of science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.317
H-Index - 61
eISSN - 1996-7489
pISSN - 0038-2353
DOI - 10.17159/sajs.2021/7659
Subject(s) - geography , vegetation (pathology) , fire regime , physical geography , biomass burning , environmental science , climatology , ecology , meteorology , geology , ecosystem , biology , aerosol , medicine , pathology
Biomass burning has become more frequent and widespread worldwide, with a significant proportion occurring in tropical Africa. Fire dynamics have been generally studied at global or regional scales. At local scale, however, fire impacts can be severe or catastrophic, suggesting local analyses are warranted. This study aimed to characterise the spatio-temporal variations of vegetation fires and identify the main fire hotspots in Côte d’Ivoire, a country of West Africa, one of the world’s burn centres. Using MODISderived fire data over a 10-year period (2007–2016), the number of fire days, active fires and fire density were assessed across the entire country. In the southern part dominated by forests, fire activity was low. Three main fire hotspots were identified between 2°30’–8°30’W and 7°00’–10°30’N in the North-West, North-East and Central areas all dominated by savannas. In these areas, Bafing, Bounkani and Hambol regions recorded the highest fire activity where fire density was 0.4±0.02, 0.28±0.02 and 0.18±0.01 fires/km²/year, respectively. At national scale, the annual fire period stretched from October to April with 91% of fires occurring between December and February, with a peak in January. Over the decade, there was a decreasing trend of fire activity. Fire density also was negatively correlated with rainfall >1000 mm for the synchronic analysis, whereas fire density was positively correlated with rainfall in the previous years. Results suggest that the positive relationship between the previous year’s rainfall and fire activity could operate on a cycle from 1 to 4 years.

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