Latitudinal and Seasonal Distribution of Particulate MSA over the Atlantic using a Validated Quantification Method with HR-ToF-AMS
Methanesulfonic acid (MSA) has been widely used as a proxy for marine biogenic sources, but it is still a challenge to provide an accurate MSA mass concentration with high time resolution. This study offers an improved MSA quantification method using high resolution time of-flight aerosol mass spect...
Published in: | Environmental Science & Technology |
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Main Authors: | , , , , , , |
Other Authors: | , , , |
Format: | Journal/Newspaper |
Language: | English |
Published: |
ENVIRONMENTAL SCIENCE & TECHNOLOGY
2017
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11897/475779 https://doi.org/10.1021/acs.est.6b03186 |
Summary: | Methanesulfonic acid (MSA) has been widely used as a proxy for marine biogenic sources, but it is still a challenge to provide an accurate MSA mass concentration with high time resolution. This study offers an improved MSA quantification method using high resolution time of-flight aerosol mass spectrometer (HR-ToF-AMS). Particularly, the method was validated based on an excellent agreement with parallel offline measurements (slope = 0.88, R-2 = 0.89). This comparison is much better than those using previously reported methods, resulting in underestimations of 31-54% of MSA concentration. With this new method, MSA mass concentrations were obtained during 4 North/South Atlantic cruises in spring and autumn of 2011 and 2012. The seasonal and spatial variation of the particulate MSA mass concentration as well as the MSA to non-sea-salt sulfate ratio (MSA:nssSO(4)) over the North/South Atlantic Ocean were determined for the first time. Seasonal variation of the MSA mass concentration was observed, with higher values in spring (0.03 mu g m(-3)) than in autumn (0.01 mu g m(-3)). The investigation of MSA:nssSO(4) suggests a ubiquitous and significant influence of anthropogenic sources on aerosols in the marine boundary layer. Gottfried Wilhelm Leibniz Association (OCEANET project); [AWI_ANT27/4]; [AWI_ANT28/1]; [AWI_ANT28/5]; [AWIANT29/1] SCI(E) ARTICLE 1 418-426 51 |
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