Characterization of size-segregated turbulent fluxes and deposition velocity by eddy correlation method in an Arctic site
Authors: Donateo Antonio , Pappaccogli Gianluca , Mazzola Mauro , Decesari Stefano , Famulari Daniela 
Published: March 2022

&lt;p&gt;Aerosols represent a fundamental component of the atmosphere, and their behaviour in the Arctic surface layer determines deposition on snow or ice surfaces. Deposition processes lead to a decrease in the snow albedo enhancing its melting, which has major impacts on climate change in polar regions, particularly in the Arctic. Many aerosols properties have been investigated in the Arctic region, with regards to chemical composition (Quinn et al, 2009; K&amp;#246;llner et al, 2021), total number and mass concentrations (Croft et al, 2016), optical properties (Ferrero et al, 2019), their ability to act as cloud condensation nuclei (Bulatovic et al., 2021), their number and size distribution (Lupi et al., 2016). Relatively few cases exist of aerosol deposition measurements on snow or iced surfaces, especially by eddy&amp;#8208;correlation (EC) method. The first example was reported by Duann et al. (1988), who analysed deposition of particles in two size ranges (0.15&amp;#8211;0.30 and 0.5&amp;#8211;1.0 mm) using the EC in a snow covered field in central Pennsylvania. Successively, the deposition velocity of particles larger than 10 nm in diameter over an iced surface in the Arctic (Nilsson and Rannik, 2001) and Antarctic (Contini et al, 2010) was measured using the EC method. The aim of the present work is to analyse the deposition velocity of atmospheric particles on snow surfaces at Ny-&amp;#197;lesund (Svalbard Islands) in relation to local micrometeorological conditions. This work reports an analysis of the concentration, size distribution, and size segregated deposition velocity of atmospheric particles. Measurements were performed using the eddy&amp;#8208;correlation method at the research laboratory of Gruvebadet from March to August 2021. The measurement system was based on a condensation particle counter (CPC) able to measure particles down to 5 nm in diameter with a 50% efficiency and an Optical Particle Counter (OPC) for evaluating particle size fluxes in the accumulation mode (0.25 &lt; dp &lt; 0.58 &amp;#956;m) and coarse mode (0.65 &lt; dp &lt; 3 &amp;#956;m). The average number concentration was 595 cm&lt;sup&gt;&amp;#8722;3&lt;/sup&gt;, 25 cm&lt;sup&gt;&amp;#8722;3&lt;/sup&gt; and 0.7 cm&lt;sup&gt;&amp;#8722;3&lt;/sup&gt; for ultrafine, accumulation and coarse particles mode. Higher concentrations were observed at low wind velocities. Results gave an average deposition velocity of 3.66 mm/s for ultrafine particles. Deposition velocity was 18.89 mm/s and 52.83 mm/s for accumulation and coarse particles, respectively. Deposition increased with friction velocity. We present an overview of the results discussed in terms of average concentration, deposition velocity, and the relationship between deposition, friction velocity, and atmospheric stability.&lt;/p&gt;&lt;p&gt;Bulatovic et al., Atmospheric Chemistry and Physics, 21, 3871-3897, 2021&lt;br&gt;Contini et al., Journal of Geophysical Research, 115, 2010&lt;br&gt;Croft et al., Atmospheric Chemistry and Physics, 16, 3665-3682, 2016&lt;br&gt;Duann, B., Journal of Applied Meteorology, 27, 642-652, 1988&lt;br&gt;Ferrero et al., Science of the Total Environment 686, 452-467, 2019&lt;br&gt;K&amp;#246;llner et al., Atmospheric Chemistry and Physics, 21, 6509-6539, 2021&lt;br&gt;Lupi et al., Rendiconti Lincei &amp;#8211; Scienze Fisiche e Naturali, ISSN 2037-4631, 27, 2016&lt;br&gt;Nilsson, E.D., and U. Rannik, Journal of Geophysical Research 106(D23), 32125-32137, 2001&lt;br&gt;Quinn et al., Atmos. Chem. Phys., 9, 8883-8888, 2009&lt;/p&gt;