Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation
Abstract Open biomass burning has major impacts on the Earth system, including on air quality via the emission of primary fine particulate matter (PM2.5). Its effect on secondary inorganic PM2.5 formation is comparatively little investigated. Simulations with the EMEP MSC-W WRF atmospheric chemistry...
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Nature Portfolio
2025-07-01
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| Series: | npj Climate and Atmospheric Science |
| Online Access: | https://doi.org/10.1038/s41612-025-01150-5 |
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| author | Damaris Y. T. Tan Mathew R. Heal Massimo Vieno David S. Stevenson Stefan Reis Eiko Nemitz |
| author_facet | Damaris Y. T. Tan Mathew R. Heal Massimo Vieno David S. Stevenson Stefan Reis Eiko Nemitz |
| author_sort | Damaris Y. T. Tan |
| collection | DOAJ |
| description | Abstract Open biomass burning has major impacts on the Earth system, including on air quality via the emission of primary fine particulate matter (PM2.5). Its effect on secondary inorganic PM2.5 formation is comparatively little investigated. Simulations with the EMEP MSC-W WRF atmospheric chemistry transport model reveal that global biomass burning emissions lead to elevated annual mean ammonium nitrate (NH4NO3) concentrations in densely populated regions where biomass burning mostly does not occur. These regions include eastern USA, northwestern Europe, the Indo-Gangetic Plain and eastern China, where NH4NO3 conditional on biomass burning emissions constitutes between 29% and 51% of the annual mean PM2.5 conditional on biomass burning emissions. Biomass burning emissions of CO, NO x (NO and NO2) and volatile organic compounds perturb the HO x (OH and HO2) cycle globally, such that there is increased oxidation of anthropogenic NO x to HNO3. This results in additional contributions to local-scale secondary NH4NO3 in areas with high emissions of anthropogenic NO x and NH3. These teleconnections increase, by up to a factor of two, the contribution of biomass burning emissions to long-term PM2.5 concentrations, which measurements alone cannot identify as an impact of biomass burning activity. This may become relatively more important as anthropogenic sources of PM2.5 are reduced and as the wildfire component of biomass burning increases under climate change. |
| format | Article |
| id | doaj-art-684c0f1eccee45e3b188e99f47e44c92 |
| institution | Kabale University |
| issn | 2397-3722 |
| language | English |
| publishDate | 2025-07-01 |
| publisher | Nature Portfolio |
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| series | npj Climate and Atmospheric Science |
| spelling | doaj-art-684c0f1eccee45e3b188e99f47e44c922025-08-20T03:42:27ZengNature Portfolionpj Climate and Atmospheric Science2397-37222025-07-01811810.1038/s41612-025-01150-5Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formationDamaris Y. T. Tan0Mathew R. Heal1Massimo Vieno2David S. Stevenson3Stefan Reis4Eiko Nemitz5UK Centre for Ecology & HydrologySchool of Chemistry, University of EdinburghUK Centre for Ecology & HydrologySchool of GeoSciences, University of EdinburghUK Centre for Ecology & HydrologyUK Centre for Ecology & HydrologyAbstract Open biomass burning has major impacts on the Earth system, including on air quality via the emission of primary fine particulate matter (PM2.5). Its effect on secondary inorganic PM2.5 formation is comparatively little investigated. Simulations with the EMEP MSC-W WRF atmospheric chemistry transport model reveal that global biomass burning emissions lead to elevated annual mean ammonium nitrate (NH4NO3) concentrations in densely populated regions where biomass burning mostly does not occur. These regions include eastern USA, northwestern Europe, the Indo-Gangetic Plain and eastern China, where NH4NO3 conditional on biomass burning emissions constitutes between 29% and 51% of the annual mean PM2.5 conditional on biomass burning emissions. Biomass burning emissions of CO, NO x (NO and NO2) and volatile organic compounds perturb the HO x (OH and HO2) cycle globally, such that there is increased oxidation of anthropogenic NO x to HNO3. This results in additional contributions to local-scale secondary NH4NO3 in areas with high emissions of anthropogenic NO x and NH3. These teleconnections increase, by up to a factor of two, the contribution of biomass burning emissions to long-term PM2.5 concentrations, which measurements alone cannot identify as an impact of biomass burning activity. This may become relatively more important as anthropogenic sources of PM2.5 are reduced and as the wildfire component of biomass burning increases under climate change.https://doi.org/10.1038/s41612-025-01150-5 |
| spellingShingle | Damaris Y. T. Tan Mathew R. Heal Massimo Vieno David S. Stevenson Stefan Reis Eiko Nemitz Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation npj Climate and Atmospheric Science |
| title | Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| title_full | Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| title_fullStr | Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| title_full_unstemmed | Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| title_short | Changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| title_sort | changes in atmospheric oxidants teleconnect biomass burning and ammonium nitrate formation |
| url | https://doi.org/10.1038/s41612-025-01150-5 |
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