Abstract
Abstract. After aerosol deposition from the atmosphere, black carbon (BC) takes part in the snow albedo feedback contributing to the modification of the Arctic radiative budget. With the initial goal of quantifying the concentration of BC in the Arctic snow and subsequent climatic impacts, snow samples were collected during the research vessel (R/V) Polarstern expedition of PASCAL (Physical Feedbacks of Arctic Boundary Layer, Sea Ice, Cloud and Aerosol; Polarstern cruise 106) in the sea-ice-covered Fram Strait in early summer 2017. The refractory BC (rBC) content was then measured in the laboratory of the Alfred Wegener Institute with the single particle soot photometer (SP2). Based on the strong observational correlations between both rBC concentration and rBC diameter with snow salinity, we hypothesize a salt-induced matrix effect interfering with the SP2 analysis. This paper evaluates the impact of sea salt, based on the measurement of electrical conductivity (κ) in water samples, on rBC measurements made with a SP2 nebulizer technique. Under realistic salinity conditions, laboratory experiments indicated a dramatic six-fold reduction in observed rBC concentration with increasing salinity. In the salinity conditions tested in the present work (salt concentration below 0.4 g L−1) the impact of salt on the nebulization of water droplets might be negligible. However, the SP2 mass detection efficiency systematically decreased with increasing salinity, with the smaller rBC particles being preferentially undetected. The high concentration of suspended salt particles and the formation of thick salt coatings on rBC cores caused problems in the SP2 analog-to-digital conversion of the signal and incandescence quenching, respectively. Changes to the signal acquisition parameters and the laser power of the SP2 improved the mass detection efficiency, which, nonetheless, stayed below unity. The present work provides evidence that a high concentration of sea salt undermines the quantification of rBC in snow performed with the SP2 nebulizer system described here. This interference has not been previously reported and might affect the future such analysis of rBC particles in snow collected, especially over sea ice or coastal regions strongly affected by sea salt deposition.
Highlights
Black carbon (BC) aerosol, produced by incomplete combustion of biomass and fossil fuels, is transported from extensive mid-latitude source regions to the Arctic atmosphere (Schacht et al, 2019), where it influences the regional climate (Quinn et al, 2015)
Laboratory experiments were conducted to assess the interference caused by inorganic salt on SP2 quantification of refractory BC (rBC) mass and size distribution in saline snow samples nebulized with a Marin-5
These experiments were designed to reproduce the salinity conditions of snow samples collected over the sea-ice-covered Fram Strait in summer 2017 during the PASCAL drift shipborne campaign
Summary
Black carbon (BC) aerosol, produced by incomplete combustion of biomass and fossil fuels, is transported from extensive mid-latitude source regions to the Arctic atmosphere (Schacht et al, 2019), where it influences the regional climate (Quinn et al, 2015). Once removed from the atmosphere, BC particles continue to affect the Arctic radiative budget by directly decreasing the snow albedo (Dou and Xiao, 2016) and promoting snow grain growth M. Zanatta et al.: Sea salt interference with black carbon quantification in snow. The overall process is usually called snow albedo feedback and might be considered among the strongest forcing mechanisms in the Arctic region (Hansen and Nazarenko, 2004; Flanner et al, 2007; Skiles et al, 2018)
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