Revisiting properties and concentrations of ice-nucleating particles in the sea surface microlayer and bulk seawater in the Canadian Arctic during summer

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Irish, Victoria E., Hanna, Sarah J., Xi, Yu, Boyer, Matthew, Polishchuk, Elena, Ahmed, Mohamed, Chen, Jessie, Abbatt, Jonathan P. D., Gosselin, Michel, Chang, Rachel, Miller, Lisa A., Bertram, Allan K.
• Format: Text
• Language: English
• Published: 2019
• Subjects: Arctic
• Online Access: https://doi.org/10.5194/acp-19-7775-2019; https://www.atmos-chem-phys.net/19/7775/2019/

Despite growing evidence that the ocean is an important source of ice-nucleating particles (INPs) in the atmosphere, our understanding of the properties and concentrations of INPs in ocean surface waters remains limited. We have investigated INPs in sea surface microlayer and bulk seawater samples collected in the Canadian Arctic during the summer of 2016. Consistent with our 2014 studies, we observed that INPs were ubiquitous in the microlayer and bulk seawaters; heat and filtration treatments reduced INP activity, indicating that the INPs were likely heat-labile biological materials between 0.22 and 0.02 µm in diameter; there was a strong negative correlation between salinity and freezing temperatures; and concentrations of INPs could not be explained by chlorophyll a concentrations. Unique in the current study, the spatial distributions of INPs were similar in 2014 and 2016, and the concentrations of INPs were strongly correlated with meteoric water (terrestrial runoff plus precipitation). These combined results suggest that meteoric water may be a major source of INPs in the sea surface microlayer and bulk seawater in this region, or meteoric water may be enhancing INPs in this region by providing additional nutrients for the production of marine microorganisms. In addition, based on the measured concentrations of INPs in the microlayer and bulk seawater, we estimate that the concentrations of INPs from the ocean in the Canadian Arctic marine boundary layer range from approximately 10 −4 to <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo><</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">6</mn></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="35pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="b710c03026df2228c6f0d24806c2f0b1"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-19-7775-2019-ie00001.svg" width="35pt" height="13pt" src="acp-19-7775-2019-ie00001.png"/></svg:svg> L −1 at −10 ∘ C.