Abstract:
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.
Significance:
• Three fire hotspots were found primarily in savanna vegetation, which burns more regularly than forestdominated
vegetation.
• The fire season occurs over 7 months, the majority of active fires (91%) occurring in just 3 months
(December-January-February) with a peak in January (39%).
• Fire activity has declined over the past decade with a return time of above-average fires from 1 to 4 years.
• Fire density is positively correlated to the amount of rainfall in preceding years, whereas fire density and
rainfall of the same year were negatively correlated in the region of rainfall >1000 mm.
