A Comprehensive Analysis of New Particle Formation Across the Northwest Atlantic: Analysis of ACTIVATE Airborne Data

SOODABEH NAMDARI, Taiwo Ajayi, Yonghoon Choi, Ewan Crosbie, Josh DiGangi, Glenn Diskin, Simon Kirschler, Hongyu Liu, John Nowak, Michael Shook, Cassidy Soloff, Kenneth Thornhill, Christiane Voigt, Edward Winstead, Bo Zhang, Luke Ziemba, Armin Sorooshian, University of Arizona

     Abstract Number: 14
     Working Group: Aerosol Physics

Abstract
New particle formation (NPF) is a critical source of particles and cloud condensation nuclei, yet there are scarce vertically-resolved measurements addressing NPF across different seasons in marine regions. This study leverages a multi-season set of airborne data from the NASA ACTIVATE mission between 2020-2022 to examine NPF characteristics over the northwest Atlantic ranging from the polluted U.S. East Coast to as far downwind (>1000 km) as Bermuda. Using the number concentration ratio above 3 and 10 nm (N3:N10) as a NPF indicator, we observe the highest ratios in the coldest months and comparable ratios over Bermuda relative to the U.S. East Coast. Within seasons, the highest and lowest ratios are found immediately above cloud tops and at the lowest possible flight altitudes (~ 150 m above sea level), respectively. The ratio of (N3-N10)/N3 ranges from 0.16-0.29 depending on altitude, proximity to clouds, and season. The N3:N10 and (N3-N10)/N3 ratios increase with altitude up to as high as 9 km, with a case study showing favorable conditions around relatively thicker and precipitating cloud systems presumably due to high actinic fluxes and reduced aerosol surface area. Regression modeling reveals that increased N3:N10 is influenced most by reductions in temperature, relative humidity, and aerosol surface area. This work emphasizes the importance of both NPF in remote marine regions like Bermuda and vertical heterogeneity that exists in its contribution to aerosol and cloud condensation nuclei number budgets.