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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedCities represent a large and concentrated portion of global greenhouse gas emissions, including methane. Quantifying methane emissions from urban areas is difficult, and inventories made using bottom-up accounting...
From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedObservations of the boundary layer (BL) processes are analyzed statistically for dry seasons of 2 years and in detail, as case studies, for 4 shallow convective days (ShCu) and 4 shallow-to-deep convective days (ShDeep)...
From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedSevere haze or low-visibility events caused by abundant atmospheric aerosols have become a serious environmental issue in many countries. A framework based on deep convolutional neural networks containing more than 20...
From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedThe formation, properties, and lifetime of secondary organic aerosols in the atmosphere are largely determined by gas-particle partitioning coefficients of the participating organic vapours. Since these coefficients are...
From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedBiomass burning (BB) and coal combustion (CC) are important sources of brown carbon (BrC) in ambient aerosols. In this study, six biomass materials and five types of coal were combusted to generate fine smoke particles....
From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedMethane (CH.sub.4) emissions from human activities are a threat to the resilience of our current climate system. The stable isotopic composition of methane ([delta].sup.13 C and [delta].sup.2 H) allows us to distinguish...
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