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Classification of MODIS fire emission data based on aerosol absorption Angstrom exponent retrieved from AERONET data

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dc.contributor.author Shantikumar, N. S
dc.contributor.author Khatri, Pradeep
dc.contributor.author Larson, E. J. L
dc.contributor.author Dumka, Umesh Chandra
dc.contributor.author Sarangi, Chandan
dc.contributor.author Vineeth, R
dc.date.accessioned 2023-03-21T05:40:34Z
dc.date.available 2023-03-21T05:40:34Z
dc.date.issued 2023-02-01
dc.identifier.citation Science of the Total Environment, Vol. 858, Part. 2, 159898 en_US
dc.identifier.issn 1879-1026
dc.identifier.uri http://hdl.handle.net/2248/8174
dc.description Restricted Access en_US
dc.description.abstract Biomass burning emits a large quantity of gaseous pollutants and aerosols into the atmosphere, which perturbs the regional and global climate and has significant impacts on air quality and human health. In order to understand the temporal and spatial distributions of biomass burning and its contribution to aerosol optical and radiative impacts, we examined fire emission data and its contribution to aerosol optical and radiative impacts over six major hot-spot continents/sub-continents across the globe, namely North-Central (NC) Africa, South America, US-Hawaii, South Asia, South East Asia, and Australia-New Zealand, using long-term satellites, ground-based and re-analysis data during 2000–2021. The selected six sites contributed ∼70% of total global fire data. The classification of biomass burning, such as pre, active, and post burning phases, was performed based on the Absorption Angstrom Exponent (AAE) estimated from 55 AERONET (AErosol RObotic NETwork) stations. The study found the highest contribution of fire count (55 %) during the active burning phase followed by post (36 %) and pre (8 %) burning phases. Such high fire counts were associated with high absorption aerosol optical depth (AAOD) during the active fire event. Strong dominance of fine and coarse mode mixed aerosols were also observed during active and post fire regimes. High AAOD and low Extinction Angstrom Exponent (EAE) over NC Africa during the fire events suggested presence of mineral dust mixed with biomass burning aerosols. Brightness temperature, fire radiative power and fire count were also dominated by the active burning followed by post and pre burning phases. The maximum heating rate of 3.15 K day−1 was observed during the active fire events. The heating rate profile shows clear variations for three different fire regimes with the highest value of 1.80 K day−1 at ∼750 hPa altitude during the active fire event. en_US
dc.language.iso en en_US
dc.publisher Elsevier B.V. en_US
dc.relation.uri https://doi.org/10.1016/j.scitotenv.2022.159898
dc.rights © 2022 Elsevier B.V.
dc.subject Biomass burning en_US
dc.subject Aerosol optical depth en_US
dc.subject Absorption angstrom exponent en_US
dc.subject Fire-radiative en_US
dc.subject Heating rate en_US
dc.title Classification of MODIS fire emission data based on aerosol absorption Angstrom exponent retrieved from AERONET data en_US
dc.type Article en_US


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