The relationship between methanesulfonic acid and organic carbon on the North Slope of Alaska

 
Poster PDF

Author

Rebecca Jacobs Sheesley — Baylor University

Category

Secondary organic aerosol

Description

Aerosols in the Arctic have large potential impacts on the radiative balance via direct and indirect effect such as scattering solar radiation and acting as cloud condensation nuclei (CCN). Marine aerosols, consisting of both inorganic particles and organic carbon (OC) contribute to these effects greatly. There are many sources of OC in the atmosphere such as oil and gas emissions, fossil fuel combustion, biomass burning, and biogenic sources, which includes marine aerosols. Dimethyl sulfide (DMS), a gas produced by phytoplankton, is photo oxidized in the atmosphere to form methanesulfonic acid (MSA). MSA can be important in forming cloud condensation nuclei, especially in remote regions such as the Arctic. While MSA has been studied in the Arctic, its relationship to particulate OC is not well understood. Total suspended particulate matter samples were collected at two sites, Utqiaġvik, AK, and Oliktok Point, AK, from June 2016 to August 2017 (ARM Field Campaign: 2014-6694). Utqiaġvik, AK, is located on the northern most point of the United States with a population of 4,581. The site is 7.4 km north of the village of Utqiaġvik. Oliktok Point, AK, is 300 km south east of Utqiaġvik in a region of intense petroleum development. Potential marine biogenic inputs to gas and particle phase organics include phytoplankton and algae in the Arctic Ocean. Terrestrial sources may also impact biogenic OC for these North Slope sites. For this study our primary focus is the relationship between MSA and OC. In addition, we are investigating the variability in summertime organic acid concentrations and relationship with OC and MSA. Samples were analyzed for OC and organic and inorganic ions including MSA. MSA may exist primarily in the smaller size fraction so the method was modified to measure it in the presence of high chloride. Measurements of MSA were also completed using an aerosol time-of-flight mass spectrometer (ATOFMS). Preliminary results show that MSA concentrations follow previously reported results (Quinn et. al., 2009). The ambient concentrations of MSA range from 0.34 to 35 ng/m3 at Utqiaġvik and 1.4 to 25 ng/m3 at Oliktok Point. Other organic acids detected include formic acid, acetic acid, and malonic acid. The data collected from this campaign can also be compared to results collected in 2012 and 2015.