The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic

• Main Authors: Boyer, Matthew, Aliaga, Diego, Quéléver, Lauriane L. J., Bucci, Silvia, Angot, Hélène, Dada, Lubna, Heutte, Benjamin, Beck, Lisa, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Sarnela, Nina, Thakur, Roseline C., Miljevic, Branka, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, Jokinen, Tuija
• Format: Text
• Language: English
• Published: 2024
• Subjects: Arctic Ocean; polar night; Sea ice
• Online Access: https://doi.org/10.5194/egusphere-2023-2953; https://egusphere.copernicus.org/preprints/2024/egusphere-2023-2953/

In this study, we present and analyze the first continuous timeseries of relevant aerosol precursor vapors from the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. These precursor vapors include sulfuric acid (SA), methanesulfonic acid (MSA), and iodic acid (IA). We use FLEXPART simulations, inverse modeling, sulfur dioxide (SO 2 ) mixing ratios, and chlorophyll-a (chl-a) observations to interpret the 20 seasonal variability of the vapor concentrations and identify dominant sources. Our results show that both natural and anthropogenic sources are relevant for the concentrations of SA in the Arctic, but anthropogenic sources associated with Arctic haze are the most prevalent. MSA concentrations are an order of magnitude higher during polar day than during polar night due to seasonal changes in biological activity. Peak MSA concentrations were observed in May, which corresponds with the timing of the annual peak in chl-a concentrations north of 75° N. IA concentrations exhibit two distinct peaks during 25 the year: a dominant peak in spring and a secondary peak in autumn, suggesting that seasonal IA concentrations depend on both solar radiation and sea ice conditions. In general, the seasonal cycles of SA, MSA, and IA in the central Arctic Ocean are related to sea ice conditions, and we expect that changes in the Arctic environment will affect the concentrations of these vapors in the future. The magnitude of these changes and the subsequent influence on aerosol processes remains uncertain, highlighting the need for continued observations of these precursor vapors in the Arctic.