{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362262943944337280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1093/nsr/nwx117"}},{"identifier":{"@type":"URI","@value":"http://academic.oup.com/nsr/article-pdf/4/6/810/31567664/nwx117.pdf"}}],"dc:title":[{"@value":"Aerosol and boundary-layer interactions and impact on air quality"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>Air quality is concerned with pollutants in both the gas phase and solid or liquid phases. The latter are referred to as aerosols, which are multifaceted agents affecting air quality, weather and climate through many mechanisms. Unlike gas pollutants, aerosols interact strongly with meteorological variables with the strongest interactions taking place in the planetary boundary layer (PBL). The PBL hosting the bulk of aerosols in the lower atmosphere is affected by aerosol radiative effects. Both aerosol scattering and absorption reduce the amount of solar radiation reaching the ground and thus reduce the sensible heat fluxes that drive the diurnal evolution of the PBL. Moreover, aerosols can increase atmospheric stability by inducing a temperature inversion as a result of both scattering and absorption of solar radiation, which suppresses dispersion of pollutants and leads to further increases in aerosol concentration in the lower PBL. Such positive feedback is especially strong during severe pollution events. Knowledge of the PBL is thus crucial for understanding the interactions between air pollution and meteorology. A key question is how the diurnal evolution of the PBL interacts with aerosols, especially in vertical directions, and affects air quality. We review the major advances in aerosol measurements, PBL processes and their interactions with each other through complex feedback mechanisms, and highlight the priorities for future studies.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943944337282","@type":"Researcher","foaf:name":[{"@value":"Zhanqing Li"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earth Surface Processes and Resource Ecology, GCESS, Beijing Normal University, Beijing 1000875, China"},{"@value":"Department of Atmospheric and Oceanic Sciences, University of Maryland, MD 21029, USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337281","@type":"Researcher","foaf:name":[{"@value":"Jianping Guo"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337289","@type":"Researcher","foaf:name":[{"@value":"Aijun Ding"}],"jpcoar:affiliationName":[{"@value":"School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337288","@type":"Researcher","foaf:name":[{"@value":"Hong Liao"}],"jpcoar:affiliationName":[{"@value":"School of Environmental Science and Engineering, Nanjing University of Information Science and Technology, Nanjing 210044, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337286","@type":"Researcher","foaf:name":[{"@value":"Jianjun Liu"}],"jpcoar:affiliationName":[{"@value":"Department of Atmospheric and Oceanic Sciences, University of Maryland, MD 21029, USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337283","@type":"Researcher","foaf:name":[{"@value":"Yele Sun"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China"},{"@value":"Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337284","@type":"Researcher","foaf:name":[{"@value":"Tijian Wang"}],"jpcoar:affiliationName":[{"@value":"School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337285","@type":"Researcher","foaf:name":[{"@value":"Huiwen Xue"}],"jpcoar:affiliationName":[{"@value":"Department of Atmospheric and Oceanic Sciences, Peking University, Beijing 100871, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337280","@type":"Researcher","foaf:name":[{"@value":"Hongsheng Zhang"}],"jpcoar:affiliationName":[{"@value":"Department of Atmospheric and Oceanic Sciences, Peking University, Beijing 100871, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943944337287","@type":"Researcher","foaf:name":[{"@value":"Bin Zhu"}],"jpcoar:affiliationName":[{"@value":"School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing 210044, China"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"20955138"},{"@type":"EISSN","@value":"2053714X"}],"prism:publicationName":[{"@value":"National Science Review"}],"dc:publisher":[{"@value":"Oxford University Press (OUP)"}],"prism:publicationDate":"2017-09-22","prism:volume":"4","prism:number":"6","prism:startingPage":"810","prism:endingPage":"833"},"reviewed":"false","dc:rights":["http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"http://academic.oup.com/nsr/article-pdf/4/6/810/31567664/nwx117.pdf"}],"createdAt":"2017-09-16","modifiedAt":"2020-01-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050865187562935680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aerosol Optical Properties of Extreme Global Wildfires and Estimated Radiative Forcing With GCOM-C SGLI"},{"@value":"Aerosol Optical Properties of Extreme Global Wildfires and Estimated Radiative Forcing With GCOM‐C SGLI"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306904389993856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unveiling microbial highways in the free troposphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092412643072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessing CALIOP-Derived Planetary Boundary Layer Height Using Ground-Based Lidar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360585255520234112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Historical (1960–2014) lightning and LNO\n                  <sub>x</sub>\n                  trends and their controlling factors in a chemistry–climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066363776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantitative evaluation of mixed biomass burning and anthropogenic aerosols over the Indochina Peninsula using MERRA-2 reanalysis products validated by sky radiometer and MAX-DOAS observations"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1093/nsr/nwx117"},{"@type":"CROSSREF","@value":"10.1029/2022jd037914_references_DOI_3efJ4fihO0n9OZlt4HhaikxiV5g"},{"@type":"CROSSREF","@value":"10.1073/pnas.2414774121_references_DOI_3efJ4fihO0n9OZlt4HhaikxiV5g"},{"@type":"CROSSREF","@value":"10.3390/rs13081496_references_DOI_3efJ4fihO0n9OZlt4HhaikxiV5g"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00520-4_references_DOI_3efJ4fihO0n9OZlt4HhaikxiV5g"},{"@type":"CROSSREF","@value":"10.5194/acp-23-13061-2023_references_DOI_3efJ4fihO0n9OZlt4HhaikxiV5g"}]}