Atmospheric Environment. Part A. General Topics
Size distributions of atmospheric trace elements at dye 3, Greenland — I. Distribution characteristics and dry deposition velocities
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Size distributions of atmospheric trace elements at Dye 3, Greenland—I. Distribution characteristics and dry deposition velocities
Atmospheric Environment
Aerosol variations in the Western Hemisphere Arctic
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The Dye Gas 3 and Aerosol Sampling Program (DGASP): an overview
Atmospheric Environment
Modes in the size distributions of atmospheric inorganic aerosol
Atmospheric Environment
A cautionary note on the use of air trajectories in interpreting arctic air chemistry
Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Atmospheric Environment
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Composition of Br-containing aerosols and gases related to boundary layer ozone destruction in the Arctic
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Chlorine, bromine and iodine in arctic aerosols
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Introduction: the first 40 years
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Mechanisms of wet and dry deposition of atmospheric contaminants to snow surfaces
Cited by (60)
A method for estimating the ratio of aerosol mass concentration to the imaginary part of the atmospheric complex refractive index and its application
2021, Atmospheric ResearchCitation Excerpt :Based on the geographical locations of the selected sites, there is no clear trend between the value of RMN and the geographical location, and the relationships between the Dg, moisture absorption characteristics and geographical location are relatively random. In general, Chongming, Shenyang and Lushan have larger geometric mean diameters, where aerosol particles mainly originate from natural sources, while Zhengzhou, Yaoxian, Hefei and Panyu have smaller geometric mean diameters, where aerosol particles primarily originate from anthropogenic sources (Hillamo et al., 1993). Fig. 11 shows that there is little difference in the hygroscopicity of aerosol particles among sites.
Dry deposition of particulate matter and its associated soluble ions on five broadleaved species in Taichung, central Taiwan
2021, Science of the Total EnvironmentCitation Excerpt :Significant positive and modest correlations only occurred between relative humidity and small particles in this study. This phenomenon may be related to the hygroscopicity of particles, which enhances particle deposition (Hillamo et al., 1993). This study, which analyzed results from field experiments, confirmed that the PM accumulation varied according to sampling time, site, and tree species.
Trends and source apportionment of atmospheric heavy metals at a subarctic site during 1996–2018
2020, Atmospheric EnvironmentCitation Excerpt :In contrast, the soil elements iron and aluminum were mostly (about 60%) in the coarse fraction (2.5–10 μm), as was 48% of the manganese. In Greenland, Hillamo et al. (1993) found that trace elements were associated with <PM10 fraction of particles, while many rural studies indicate that crustal elements can be found in particulates > PM10 (Pakkanen et al., 2001; Wang et al., 2016). In the winter season, when the soil is covered with snow at Pallas for several months (typically October/November to April/May), we do not expect to have much of particles larger than PM10.
Chemical composition and size of particles in emissions of a coal-fired power plant with flue gas desulfurization
2014, Journal of Aerosol ScienceCitation Excerpt :The flow rate was 11 l min−1. Battelle is a 7-stage cascade-impactor that collects particles within 0.2 and 11 μm (Hillamo et al., 1993) with the flow rate of 1 l min−1. Here, the smallest size range for TEM-EDX-analysis was collected with the SDI (86–153 nm) and four particle size ranges between 0.2 and 11 μm were collected with the Battelle impactor.
Aerosols and their sources at Summit Greenland - First results of continuous size- and time-resolved sampling
2012, Atmospheric EnvironmentCitation Excerpt :This approach allows easy recognition of certain diagnostic trace species, such as metals associated with combustion processes, while avoiding the confusing similarity of the profiles that would be driven by the large loading of common elements, such as Si or Na. The PMF analysis was run step-wise, increasing the number of factors until sufficient discrimination among the factors produced physically meaningful profiles, recognizably similar to a priori expectations of aerosol types based on literature review for previous work in Greenland (e.g. Hillamo et al., 1993; Jaffrezo et al., 1993a; Davidson et al., 1993b) and previous experience with PMF analyses for aerosols in other remote locations. The normalized and mass-based versions of the factors map onto one another because the PMF process is driven by temporal correlations among variables in the data sets, thus the PMF-3 program itself automatically produces both versions of the results.
Dry deposition velocity of total suspended particles and meteorological influence in four locations in Guangzhou, China
2012, Journal of Environmental Sciences