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The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system

Roldin, Pontus LU ; Ehn, Mikael ; Kurtén, Theo ; Olenius, Tinja ; Rissanen, Matti P. ; Sarnela, Nina ; Elm, Jonas ; Rantala, Pekka ; Hao, Liqing and Hyttinen, Noora , et al. (2019) In Nature Communications 10. p.1-15
Abstract
Over Boreal regions, monoterpenes emitted from the forest are the main precursors for secondary organic aerosol (SOA) formation and the primary driver of the growth of new aerosol particles to climatically important cloud condensation nuclei (CCN). Autoxidation of monoterpenes leads to rapid formation of Highly Oxygenated organic Molecules (HOM). We have developed the first model with near-explicit representation of atmospheric new particle formation (NPF) and HOM formation. The model can reproduce the observed NPF, HOM gas-phase composition and SOA formation over the Boreal forest. During the spring, HOM SOA formation increases the CCN concentration by ~10 % and causes a direct aerosol radiative forcing of −0.10 W/m2. In contrast, NPF... (More)
Over Boreal regions, monoterpenes emitted from the forest are the main precursors for secondary organic aerosol (SOA) formation and the primary driver of the growth of new aerosol particles to climatically important cloud condensation nuclei (CCN). Autoxidation of monoterpenes leads to rapid formation of Highly Oxygenated organic Molecules (HOM). We have developed the first model with near-explicit representation of atmospheric new particle formation (NPF) and HOM formation. The model can reproduce the observed NPF, HOM gas-phase composition and SOA formation over the Boreal forest. During the spring, HOM SOA formation increases the CCN concentration by ~10 % and causes a direct aerosol radiative forcing of −0.10 W/m2. In contrast, NPF reduces the number of CCN at updraft velocities < 0.2 m/s, and causes a direct aerosol radiative forcing of +0.15 W/m2. Hence, while HOM SOA contributes to climate cooling, NPF can result in climate warming over the Boreal forest. (Less)
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@article{a5eb58ca-3a04-4178-b01b-c81e1c61c697,
  abstract     = {{Over Boreal regions, monoterpenes emitted from the forest are the main precursors for secondary organic aerosol (SOA) formation and the primary driver of the growth of new aerosol particles to climatically important cloud condensation nuclei (CCN). Autoxidation of monoterpenes leads to rapid formation of Highly Oxygenated organic Molecules (HOM). We have developed the first model with near-explicit representation of atmospheric new particle formation (NPF) and HOM formation. The model can reproduce the observed NPF, HOM gas-phase composition and SOA formation over the Boreal forest. During the spring, HOM SOA formation increases the CCN concentration by ~10 % and causes a direct aerosol radiative forcing of −0.10 W/m2. In contrast, NPF reduces the number of CCN at updraft velocities &lt; 0.2 m/s, and causes a direct aerosol radiative forcing of +0.15 W/m2. Hence, while HOM SOA contributes to climate cooling, NPF can result in climate warming over the Boreal forest.}},
  author       = {{Roldin, Pontus and Ehn, Mikael and Kurtén, Theo and Olenius, Tinja and Rissanen, Matti P. and Sarnela, Nina and Elm, Jonas and Rantala, Pekka and Hao, Liqing and Hyttinen, Noora and Heikkinen, Liine and Worsnop, Douglas R. and Pichelstorfer, Lukas and Xavier, Carlton and Clusius, Petri and Öström, Emilie and Petäjä, Tuukka and Kulmala, Markku and Vehkamäki, Hanna and Virtanen, Annele and Riipinen, Ilona and Boy, Michael}},
  issn         = {{2041-1723}},
  language     = {{eng}},
  month        = {{09}},
  pages        = {{1--15}},
  publisher    = {{Nature Publishing Group}},
  series       = {{Nature Communications}},
  title        = {{The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system}},
  url          = {{http://dx.doi.org/10.1038/s41467-019-12338-8}},
  doi          = {{10.1038/s41467-019-12338-8}},
  volume       = {{10}},
  year         = {{2019}},
}