Publication:
Spatial and temporal distribution of biomass open burning emissions in the greater mekong subregion

dc.contributor.authorAgapol Junpenen_US
dc.contributor.authorJirataya Roemmontrien_US
dc.contributor.authorAthipthep Boonmanen_US
dc.contributor.authorPenwadee Cheewaphongphanen_US
dc.contributor.authorPham Thi Bich Thaoen_US
dc.contributor.authorSavitri Garivaiten_US
dc.contributor.otherFaculty of Environment and Resource Studies, Mahidol Universityen_US
dc.contributor.otherNational Institute for Environmental Studies of Japanen_US
dc.contributor.otherThailand Ministry of Educationen_US
dc.contributor.otherKing Mongkut s University of Technology Thonburien_US
dc.date.accessioned2020-10-05T04:49:40Z
dc.date.available2020-10-05T04:49:40Z
dc.date.issued2020-01-01en_US
dc.description.abstract© 2020 by the authors. Moderate Resolution Imaging Spectroradiometer (MODIS) burnt area products are widely used to assess the damaged area after wildfires and agricultural burning have occurred. This study improved the accuracy of the assessment of the burnt areas by using the MCD45A1 and MCD64A1 burnt area products with the finer spatial resolution product from the Landsat-8 Operational Land Imager/Thermal Infrared Sensor (OLI/TIRS) surface reflectance data. Thus, more accurate wildfires and agricultural burning areas in the Greater Mekong Subregion (GMS) for the year 2015 as well as the estimation of the fire emissions were reported. In addition, the results from this study were compared with the data derived from the fourth version of the Global Fire Emissions Database (GFED) that included small fires (GFED4.1s). Upon analysis of the data of the burnt areas, it was found that the burnt areas obtained from the MCD64A1 and MCD45A1 had lower values than the reference fires for all vegetation fires. These results suggested multiplying the MCD64A1 and MCD45A1 for the GMS by the correction factors of 2.11-21.08 depending on the MODIS burnt area product and vegetation fires. After adjusting the burnt areas by the correction factor, the total biomass burnt area in the GMS during the year 2015 was about 33.3 million hectares (Mha), which caused the burning of 109 ± 22 million tons (Mt) of biomass. This burning emitted 178 ± 42 Mt of CO2, 469 ± 351 kilotons (kt) of CH4, 18 ± 3 kt of N2O, 9.4 ± 4.9 Mt of CO, 345 ± 206 kt of NOX, 46 ± 25 kt of SO2, 147 ± 117 kt of NH3, 820 ± 489 kt of PM2.5, 60 ± 32 kt of BC, and 350 ± 205 kt of OC. Furthermore, the emission results of fine particulate matter (PM2.5) in all countries were slightly lower than GFED4.1s in the range between 0.3 and 0.6 times.en_US
dc.identifier.citationClimate. Vol.8, No.8 (2020)en_US
dc.identifier.doi10.3390/CLI8080090en_US
dc.identifier.issn22251154en_US
dc.identifier.other2-s2.0-85089853921en_US
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/20.500.14594/59056
dc.rightsMahidol Universityen_US
dc.rights.holderSCOPUSen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85089853921&origin=inwarden_US
dc.subjectEarth and Planetary Sciencesen_US
dc.titleSpatial and temporal distribution of biomass open burning emissions in the greater mekong subregionen_US
dc.typeArticleen_US
dspace.entity.typePublication
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85089853921&origin=inwarden_US

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