New 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 nuclei (CCN). This occurs via ion-induced nucleation of SA and NH3 and subsequent growth by mainly SA and MSA condensation during springtime and highly oxygenated organic molecules during summertime. By contrast, in an ice-covered region around Villum, we observed new particle formation driven by iodic acid but its concentration was insufficient to grow nucleated particles to CCN sizes. Our results provide new insight about sources and precursors of Arctic secondary aerosol particles.

Differing Mechanisms of New Particle Formation at Two Arctic Sites / Beck L.J.; Sarnela N.; Junninen H.; Hoppe C.J.M.; Garmash O.; Bianchi F.; Riva M.; Rose C.; Perakyla O.; Wimmer D.; Kausiala O.; Jokinen T.; Ahonen L.; Mikkila J.; Hakala J.; He X.-C.; Kontkanen J.; Wolf K.K.E.; Cappelletti D.; Mazzola M.; Traversi R.; Petroselli C.; Viola A.P.; Vitale V.; Lange R.; Massling A.; Nojgaard J.K.; Krejci R.; Karlsson L.; Zieger P.; Jang S.; Lee K.; Vakkari V.; Lampilahti J.; Thakur R.C.; Leino K.; Kangasluoma J.; Duplissy E.-M.; Siivola E.; Marbouti M.; Tham Y.J.; Saiz-Lopez A.; Petaja T.; Ehn M.; Worsnop D.R.; Skov H.; Kulmala M.; Kerminen V.-M.; Sipila M.. - In: GEOPHYSICAL RESEARCH LETTERS. - ISSN 0094-8276. - ELETTRONICO. - 48:(2021), pp. 1-11. [10.1029/2020GL091334]

Differing Mechanisms of New Particle Formation at Two Arctic Sites

Traversi R.;
2021

Abstract

New 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 nuclei (CCN). This occurs via ion-induced nucleation of SA and NH3 and subsequent growth by mainly SA and MSA condensation during springtime and highly oxygenated organic molecules during summertime. By contrast, in an ice-covered region around Villum, we observed new particle formation driven by iodic acid but its concentration was insufficient to grow nucleated particles to CCN sizes. Our results provide new insight about sources and precursors of Arctic secondary aerosol particles.
2021
48
1
11
Beck L.J.; Sarnela N.; Junninen H.; Hoppe C.J.M.; Garmash O.; Bianchi F.; Riva M.; Rose C.; Perakyla O.; Wimmer D.; Kausiala O.; Jokinen T.; Ahonen L....espandi
File in questo prodotto:
File Dimensione Formato  
Beck21 Differing nucleation mechanism Arctic - GRL.pdf

accesso aperto

Tipologia: Pdf editoriale (Version of record)
Licenza: Tutti i diritti riservati
Dimensione 2.25 MB
Formato Adobe PDF
2.25 MB Adobe PDF

I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/1258310
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 90
  • ???jsp.display-item.citation.isi??? 88
social impact