Size-dependent influence of nox on the growth rates of organic aerosol particles

C. Yan; W. Nie; A. L. Voge; L. Dada; K. Lehtipalo; D. Stolzenburg; R. Wagner; M. P. Rissanen; M. Xiao; L. Ahonen; L. Fischer; C. Rose; F. Bianchi; H. Gordon; M. Simon; M. Heinritzi; O. Garmash; P. Roldin; A. Dias; P. Ye; V. Hofbauer; A. Amorim; P. S. Bauer; A. Bergen; A. K. Bernhammer; M. Breitenlechner; S. Brilke; A. Buchholz; S. Buenrostro Mazon; M. R. Canagaratna; A. Ding; J. Dommen; D. C. Draper; J. Duplissy; C. Frege; C. Heyn; R. Guida; J. Hakala; L. Heikkinen; C. R. Hoyle; J. Kangasluoma; J. Kirkby; J. Kontkanen; A. Kürten; M. J. Lawler; H. Mai; S. Mathot; R. L.Mauldin Iii; U. Molteni; L. Nichman; T. Nieminen; J. Nowak; A. Ojdanic; A. Onnela; A. Pajunoja; T. Petäjä; F. Piel; L. L.J. Quéléver; N. Sarnela; S. Schallhart; K. Sengupta; A. Tomé; J. Tröst; O. Vaïsänen; A. C. Wagner; A. Ylisirniö; Q. Zha; U. Baltensperger; K. S. Carslaw; J. Curtius; R. C. Flagan; A. Hanse; I. Riipinen; J. N. Smith; P. M. Winkler; N. M. Donahue; V. M. Kerminen; M. Ehn; D. R. Worsnop

doi:10.1126/sciadv.aay4945

Size-dependent influence of nox on the growth rates of organic aerosol particles

C. Yan^*
, W. Nie
, A. L. Voge
, L. Dada
, K. Lehtipalo
, D. Stolzenburg
, R. Wagner
, M. P. Rissanen
, M. Xiao
, L. Ahonen
, L. Fischer
, C. Rose
, F. Bianchi
, H. Gordon
, M. Simon
, M. Heinritzi
, O. Garmash
, P. Roldin
, A. Dias
, P. Ye

V. Hofbauer, A. Amorim, P. S. Bauer, A. Bergen, A. K. Bernhammer, M. Breitenlechner, S. Brilke, A. Buchholz, S. Buenrostro Mazon, M. R. Canagaratna, A. Ding, J. Dommen, D. C. Draper, J. Duplissy, C. Frege, C. Heyn, R. Guida, J. Hakala, L. Heikkinen, C. R. Hoyle, J. Kangasluoma, J. Kirkby, J. Kontkanen, A. Kürten, M. J. Lawler, H. Mai, S. Mathot, R. L.Mauldin Iii, U. Molteni, L. Nichman, T. Nieminen, J. Nowak, A. Ojdanic, A. Onnela, A. Pajunoja, T. Petäjä, F. Piel, L. L.J. Quéléver, N. Sarnela, S. Schallhart, K. Sengupta, A. Tomé, J. Tröst, O. Vaïsänen, A. C. Wagner, A. Ylisirniö, Q. Zha, U. Baltensperger, K. S. Carslaw, J. Curtius, R. C. Flagan, A. Hanse, I. Riipinen, J. N. Smith, P. M. Winkler, N. M. Donahue, V. M. Kerminen, M. Ehn, D. R. Worsnop

^*Corresponding author for this work

Not published at VTT

University of Helsinki
Nanjing University
European Organization for Nuclear Research (CERN)
Paul Scherrer Institute (PSI)
Finnish Meteorological Institute (FMI)
University of Vienna
University of Innsbruck
University of Colorado Denver
Goethe University Frankfurt
Universidade de Lisboa
Carnegie Mellon University
Aerodyne Research Inc
University of Eastern Finland
Beijing University of Chemical Technology
University of California Irvine (UCI)
California Institute of Technology
University of Manchester
Lund University
University of Leeds
University of Beira Interior
University of Clermont Auvergne
Harvard University
University of Tartu
Swiss Federal Institute of Technology in Zurich (ETH Zürich)
National Research Council Canada (NRC)
National Aeronautics and Space Administration (NASA)
University of Oslo
IONICON Analytik GmbH
Stockholm University

Research output: Contribution to journal › Article › Scientific › peer-review

99 Citations (Scopus)

Abstract

Atmospheric new-particle formation (NPF) affects climate by contributing to a large fraction of the cloud condensation nuclei (CCN). Highly oxygenated organic molecules (HOMs) drive the early particle growth and therefore substantially influence the survival of newly formed particles to CCN. Nitrogen oxide (NOx) is known to suppress the NPF driven by HOMs, but the underlying mechanism remains largely unclear. Here, we examine the response of particle growth to the changes of HOM formation caused by NOx. We show that NOx suppresses particle growth in general, but the suppression is rather nonuniform and size dependent, which can be quantitatively explained by the shifted HOM volatility after adding NOx. By illustrating how NOx affects the early growth of new particles, a critical step of CCN formation, our results help provide a refined assessment of the potential climatic effects caused by the diverse changes of NOx level in forest regions around the globe.

Original language	English
Article number	eaay4945
Journal	Science advances
Volume	6
Issue number	22
DOIs	https://doi.org/10.1126/sciadv.aay4945
Publication status	Published - May 2020
MoE publication type	A1 Journal article-refereed

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Yan, C., Nie, W., Voge, A. L., Dada, L., Lehtipalo, K., Stolzenburg, D., Wagner, R., Rissanen, M. P., Xiao, M., Ahonen, L., Fischer, L., Rose, C., Bianchi, F., Gordon, H., Simon, M., Heinritzi, M., Garmash, O., Roldin, P., Dias, A., ... Worsnop, D. R. (2020). Size-dependent influence of nox on the growth rates of organic aerosol particles. Science advances, 6(22), Article eaay4945. https://doi.org/10.1126/sciadv.aay4945

@article{65dd746a0f1b464b9fbec8422702ec04,

title = "Size-dependent influence of nox on the growth rates of organic aerosol particles",

abstract = "Atmospheric new-particle formation (NPF) affects climate by contributing to a large fraction of the cloud condensation nuclei (CCN). Highly oxygenated organic molecules (HOMs) drive the early particle growth and therefore substantially influence the survival of newly formed particles to CCN. Nitrogen oxide (NOx) is known to suppress the NPF driven by HOMs, but the underlying mechanism remains largely unclear. Here, we examine the response of particle growth to the changes of HOM formation caused by NOx. We show that NOx suppresses particle growth in general, but the suppression is rather nonuniform and size dependent, which can be quantitatively explained by the shifted HOM volatility after adding NOx. By illustrating how NOx affects the early growth of new particles, a critical step of CCN formation, our results help provide a refined assessment of the potential climatic effects caused by the diverse changes of NOx level in forest regions around the globe.",

author = "C. Yan and W. Nie and Voge, \{A. L.\} and L. Dada and K. Lehtipalo and D. Stolzenburg and R. Wagner and Rissanen, \{M. P.\} and M. Xiao and L. Ahonen and L. Fischer and C. Rose and F. Bianchi and H. Gordon and M. Simon and M. Heinritzi and O. Garmash and P. Roldin and A. Dias and P. Ye and V. Hofbauer and A. Amorim and Bauer, \{P. S.\} and A. Bergen and Bernhammer, \{A. K.\} and M. Breitenlechner and S. Brilke and A. Buchholz and Mazon, \{S. Buenrostro\} and Canagaratna, \{M. R.\} and A. Ding and J. Dommen and Draper, \{D. C.\} and J. Duplissy and C. Frege and C. Heyn and R. Guida and J. Hakala and L. Heikkinen and Hoyle, \{C. R.\} and J. Kangasluoma and J. Kirkby and J. Kontkanen and A. K{\"u}rten and Lawler, \{M. J.\} and H. Mai and S. Mathot and Iii, \{R. L.Mauldin\} and U. Molteni and L. Nichman and T. Nieminen and J. Nowak and A. Ojdanic and A. Onnela and A. Pajunoja and T. Pet{\"a}j{\"a} and F. Piel and Qu{\'e}l{\'e}ver, \{L. L.J.\} and N. Sarnela and S. Schallhart and K. Sengupta and A. Tom{\'e} and J. Tr{\"o}st and O. Va{\"i}s{\"a}nen and Wagner, \{A. C.\} and A. Ylisirni{\"o} and Q. Zha and U. Baltensperger and Carslaw, \{K. S.\} and J. Curtius and Flagan, \{R. C.\} and A. Hanse and I. Riipinen and Smith, \{J. N.\} and Winkler, \{P. M.\} and Donahue, \{N. M.\} and Kerminen, \{V. M.\} and M. Ehn and Worsnop, \{D. R.\}",

note = "Copyright {\textcopyright} 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).",

year = "2020",

month = may,

doi = "10.1126/sciadv.aay4945",

language = "English",

volume = "6",

journal = "Science advances",

issn = "2375-2548",

publisher = "American Association for the Advancement of Science",

number = "22",

}

Yan, C, Nie, W, Voge, AL, Dada, L, Lehtipalo, K, Stolzenburg, D, Wagner, R, Rissanen, MP, Xiao, M, Ahonen, L, Fischer, L, Rose, C, Bianchi, F, Gordon, H, Simon, M, Heinritzi, M, Garmash, O, Roldin, P, Dias, A, Ye, P, Hofbauer, V, Amorim, A, Bauer, PS, Bergen, A, Bernhammer, AK, Breitenlechner, M, Brilke, S, Buchholz, A, Mazon, SB, Canagaratna, MR, Ding, A, Dommen, J, Draper, DC, Duplissy, J, Frege, C, Heyn, C, Guida, R, Hakala, J, Heikkinen, L, Hoyle, CR, Kangasluoma, J, Kirkby, J, Kontkanen, J, Kürten, A, Lawler, MJ, Mai, H, Mathot, S, Iii, RLM, Molteni, U, Nichman, L, Nieminen, T, Nowak, J, Ojdanic, A, Onnela, A, Pajunoja, A, Petäjä, T, Piel, F, Quéléver, LLJ, Sarnela, N, Schallhart, S, Sengupta, K, Tomé, A, Tröst, J, Vaïsänen, O, Wagner, AC, Ylisirniö, A, Zha, Q, Baltensperger, U, Carslaw, KS, Curtius, J, Flagan, RC, Hanse, A, Riipinen, I, Smith, JN, Winkler, PM, Donahue, NM, Kerminen, VM, Ehn, M & Worsnop, DR 2020, 'Size-dependent influence of nox on the growth rates of organic aerosol particles', Science advances, vol. 6, no. 22, eaay4945. https://doi.org/10.1126/sciadv.aay4945

TY - JOUR

T1 - Size-dependent influence of nox on the growth rates of organic aerosol particles

AU - Yan, C.

AU - Nie, W.

AU - Voge, A. L.

AU - Dada, L.

AU - Lehtipalo, K.

AU - Stolzenburg, D.

AU - Wagner, R.

AU - Rissanen, M. P.

AU - Xiao, M.

AU - Ahonen, L.

AU - Fischer, L.

AU - Rose, C.

AU - Bianchi, F.

AU - Gordon, H.

AU - Simon, M.

AU - Heinritzi, M.

AU - Garmash, O.

AU - Roldin, P.

AU - Dias, A.

AU - Ye, P.

AU - Hofbauer, V.

AU - Amorim, A.

AU - Bauer, P. S.

AU - Bergen, A.

AU - Bernhammer, A. K.

AU - Breitenlechner, M.

AU - Brilke, S.

AU - Buchholz, A.

AU - Mazon, S. Buenrostro

AU - Canagaratna, M. R.

AU - Ding, A.

AU - Dommen, J.

AU - Draper, D. C.

AU - Duplissy, J.

AU - Frege, C.

AU - Heyn, C.

AU - Guida, R.

AU - Hakala, J.

AU - Heikkinen, L.

AU - Hoyle, C. R.

AU - Kangasluoma, J.

AU - Kirkby, J.

AU - Kontkanen, J.

AU - Kürten, A.

AU - Lawler, M. J.

AU - Mai, H.

AU - Mathot, S.

AU - Iii, R. L.Mauldin

AU - Molteni, U.

AU - Nichman, L.

AU - Nieminen, T.

AU - Nowak, J.

AU - Ojdanic, A.

AU - Onnela, A.

AU - Pajunoja, A.

AU - Petäjä, T.

AU - Piel, F.

AU - Quéléver, L. L.J.

AU - Sarnela, N.

AU - Schallhart, S.

AU - Sengupta, K.

AU - Tomé, A.

AU - Tröst, J.

AU - Vaïsänen, O.

AU - Wagner, A. C.

AU - Ylisirniö, A.

AU - Zha, Q.

AU - Baltensperger, U.

AU - Carslaw, K. S.

AU - Curtius, J.

AU - Flagan, R. C.

AU - Hanse, A.

AU - Riipinen, I.

AU - Smith, J. N.

AU - Winkler, P. M.

AU - Donahue, N. M.

AU - Kerminen, V. M.

AU - Ehn, M.

AU - Worsnop, D. R.

N1 - Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

PY - 2020/5

Y1 - 2020/5

N2 - Atmospheric new-particle formation (NPF) affects climate by contributing to a large fraction of the cloud condensation nuclei (CCN). Highly oxygenated organic molecules (HOMs) drive the early particle growth and therefore substantially influence the survival of newly formed particles to CCN. Nitrogen oxide (NOx) is known to suppress the NPF driven by HOMs, but the underlying mechanism remains largely unclear. Here, we examine the response of particle growth to the changes of HOM formation caused by NOx. We show that NOx suppresses particle growth in general, but the suppression is rather nonuniform and size dependent, which can be quantitatively explained by the shifted HOM volatility after adding NOx. By illustrating how NOx affects the early growth of new particles, a critical step of CCN formation, our results help provide a refined assessment of the potential climatic effects caused by the diverse changes of NOx level in forest regions around the globe.

AB - Atmospheric new-particle formation (NPF) affects climate by contributing to a large fraction of the cloud condensation nuclei (CCN). Highly oxygenated organic molecules (HOMs) drive the early particle growth and therefore substantially influence the survival of newly formed particles to CCN. Nitrogen oxide (NOx) is known to suppress the NPF driven by HOMs, but the underlying mechanism remains largely unclear. Here, we examine the response of particle growth to the changes of HOM formation caused by NOx. We show that NOx suppresses particle growth in general, but the suppression is rather nonuniform and size dependent, which can be quantitatively explained by the shifted HOM volatility after adding NOx. By illustrating how NOx affects the early growth of new particles, a critical step of CCN formation, our results help provide a refined assessment of the potential climatic effects caused by the diverse changes of NOx level in forest regions around the globe.

UR - https://www.scopus.com/pages/publications/85086355828

U2 - 10.1126/sciadv.aay4945

DO - 10.1126/sciadv.aay4945

M3 - Article

C2 - 32518819

AN - SCOPUS:85086355828

SN - 2375-2548

VL - 6

JO - Science advances

JF - Science advances

IS - 22

M1 - eaay4945

ER -

Size-dependent influence of nox on the growth rates of organic aerosol particles

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