Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/8174
Full metadata record
DC FieldValueLanguage
dc.contributor.authorShantikumar, N. S-
dc.contributor.authorKhatri, Pradeep-
dc.contributor.authorLarson, E. J. L-
dc.contributor.authorDumka, Umesh Chandra-
dc.contributor.authorSarangi, Chandan-
dc.contributor.authorVineeth, R-
dc.date.accessioned2023-03-21T05:40:34Z-
dc.date.available2023-03-21T05:40:34Z-
dc.date.issued2023-02-01-
dc.identifier.citationScience of the Total Environment, Vol. 858, Part. 2, 159898en_US
dc.identifier.issn1879-1026-
dc.identifier.urihttp://hdl.handle.net/2248/8174-
dc.descriptionRestricted Accessen_US
dc.description.abstractBiomass 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.isoenen_US
dc.publisherElsevier B.V.en_US
dc.relation.urihttps://doi.org/10.1016/j.scitotenv.2022.159898-
dc.rights© 2022 Elsevier B.V.-
dc.subjectBiomass burningen_US
dc.subjectAerosol optical depthen_US
dc.subjectAbsorption angstrom exponenten_US
dc.subjectFire-radiativeen_US
dc.subjectHeating rateen_US
dc.titleClassification of MODIS fire emission data based on aerosol absorption Angstrom exponent retrieved from AERONET dataen_US
dc.typeArticleen_US
Appears in Collections:IIAP Publications

Files in This Item:
File Description SizeFormat 
Classification of MODIS fire emission data based on aerosol absorption Angstrom exponent retrieved from AERONET data.pdf
  Restricted Access
© 2022 Elsevier B.V. All rights reserved.3.5 MBAdobe PDFView/Open Request a copy


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.