Authors: Juha Kangasluoma; Xu-Cheng He; Sehyun Jang; Tuukka Petäjä; Radovan Krejci; Jani Hakala; Kitack Lee; Douglas R. Worsnop; Vito Vitale; F. Bianchi; Jyri Mikkilä; Olga Garmash; Ville Vakkari; Chiara Petroselli; Lisa Beck; Henrik Skov; Jenni Kontkanen; David Cappelletti; Linn Karlsson; Marjan Marbouti; Otso Peräkylä; Andreas Massling; Klara Wolf; Mikael Ehn; Nina Sarnela; Janne Lampilahti; Clara Jule Marie Hoppe; Tuija Jokinen; Yee Jun Tham; Markku Kulmala; Clémence Rose; Jakob Klenø Nøjgaard; Robert Lange; Veli-Matti Kerminen; Ella-Maria Duplissy; Daniela Wimmer; Heikki Junninen; Lauri Ahonen; Roseline C. Thakur; Matthieu Riva; Paul Zieger; Katri Leino; Mikko Sipilä; Angelo Viola; Erkki Siivola; Mauro Mazzola; Oskari Kausiala; Rita Traversi; Alfonso Saiz-Lopez

Venue: Geophysical Research Letters

Type: Publication

Abstract: AbstractNew particle formation in the Arctic atmosphere is an important source of aerosol particles. Understanding the processes of Arctic secondary aerosol formation is crucial due to their significant impact on cloud properties and therefore Arctic amplification. We observed the molecular formation of new particles from low‐volatility vapors at two Arctic sites with differing surroundings. In Svalbard, sulfuric acid (SA) and methane sulfonic acid (MSA) contribute to the formation of secondary aerosol and to some extent to cloud condensation... (read more)

DOI: 10.5281/zenodo.4292238