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Overview paper: New insights into aerosol and climate in the Arctic

Authors :
Abbatt, Jonathan P. D.
Leaitch, W. Richard
Aliabadi, Amir A.
Bertram, Allan K.
Blanchet, Jean-Pierre
Boivin-Rioux, Aude
Bozem, Heiko
Burkart, Julia
Chang, Rachel Y. W.
Charette, Joannie
Chaubey, Jai P.
Christensen, Robert J.
Cirisan, Ana
Collins, Douglas B.
Croft, Betty
Dionne, Joelle
Evans, Greg J.
Fletcher, Christopher G.
Galí, Martí
Ghahremaninezhad, Roghayeh
Girard, Eric
Gong, Wanmin
Gosselin, Michel
Gourdal, Margaux
Hanna, Sarah J.
Hayashida, Hakase
Herber, Andreas B.
Hesaraki, Sareh
Hoor, Peter
Huang, Lin
Hussherr, Rachel
Irish, Victoria E.
Keita, Setigui A.
Kodros, John K.
Köllner, Franziska
Kolonjari, Felicia
Kunkel, Daniel
Ladino, Luis A.
Law, Kathy
Levasseur, Maurice
Libois, Quentin
Liggio, John
Lizotte, Martine
Macdonald, Katrina M.
Mahmood, Rashed
Martin, Randall V.
Mason, Ryan H.
Miller, Lisa A.
Moravek, Alexander
Mortenson, Eric
Mungall, Emma L.
Murphy, Jennifer G.
Namazi, Maryam
Norman, Ann-Lise
O'Neill, Norman T.
Pierce, Jeffrey R.
Russell, Lynn M.
Schneider, Johannes
Schulz, Hannes
Sharma, Sangeeta
Si, Meng
Staebler, Ralf M.
Steiner, Nadja S.
Thomas, Jennie L.
von Salzen, Knut
Wentzell, Jeremy J. B.
Willis, Megan D.
Wentworth, Gregory R.
Xu, Jun-Wei
Yakobi-Hancock, Jacqueline D.
Abbatt, Jonathan P. D.
Leaitch, W. Richard
Aliabadi, Amir A.
Bertram, Allan K.
Blanchet, Jean-Pierre
Boivin-Rioux, Aude
Bozem, Heiko
Burkart, Julia
Chang, Rachel Y. W.
Charette, Joannie
Chaubey, Jai P.
Christensen, Robert J.
Cirisan, Ana
Collins, Douglas B.
Croft, Betty
Dionne, Joelle
Evans, Greg J.
Fletcher, Christopher G.
Galí, Martí
Ghahremaninezhad, Roghayeh
Girard, Eric
Gong, Wanmin
Gosselin, Michel
Gourdal, Margaux
Hanna, Sarah J.
Hayashida, Hakase
Herber, Andreas B.
Hesaraki, Sareh
Hoor, Peter
Huang, Lin
Hussherr, Rachel
Irish, Victoria E.
Keita, Setigui A.
Kodros, John K.
Köllner, Franziska
Kolonjari, Felicia
Kunkel, Daniel
Ladino, Luis A.
Law, Kathy
Levasseur, Maurice
Libois, Quentin
Liggio, John
Lizotte, Martine
Macdonald, Katrina M.
Mahmood, Rashed
Martin, Randall V.
Mason, Ryan H.
Miller, Lisa A.
Moravek, Alexander
Mortenson, Eric
Mungall, Emma L.
Murphy, Jennifer G.
Namazi, Maryam
Norman, Ann-Lise
O'Neill, Norman T.
Pierce, Jeffrey R.
Russell, Lynn M.
Schneider, Johannes
Schulz, Hannes
Sharma, Sangeeta
Si, Meng
Staebler, Ralf M.
Steiner, Nadja S.
Thomas, Jennie L.
von Salzen, Knut
Wentzell, Jeremy J. B.
Willis, Megan D.
Wentworth, Gregory R.
Xu, Jun-Wei
Yakobi-Hancock, Jacqueline D.

Abstract

Motivated by the need to predict how the Arctic atmosphere will change in a warming world, this article summarizes recent advances made by the research consortium NETCARE (Network on Climate and Aerosols: Addressing Key Uncertainties in Remote Canadian Environments) that contribute to our fundamental understanding of Arctic aerosol particles as they relate to climate forcing. The overall goal of NETCARE research has been to use an interdisciplinary approach encompassing extensive field observations and a range of chemical transport, earth system, and biogeochemical models. Several major findings and advances have emerged from NETCARE since its formation in 2013. (1) Unexpectedly high summertime dimethyl sulfide (DMS) levels were identified in ocean water (up to 75 nM) and the overlying atmosphere (up to 1 ppbv) in the Canadian Arctic Archipelago (CAA). Furthermore, melt ponds, which are widely prevalent, were identified as an important DMS source (with DMS concentrations of up to 6 nM and a potential contribution to atmospheric DMS of 20 % in the study area). (2) Evidence of widespread particle nucleation and growth in the marine boundary layer was found in the CAA in the summertime, with these events observed on 41 % of days in a 2016 cruise. As well, at Alert, Nunavut, particles that are newly formed and grown under conditions of minimal anthropogenic influence during the months of July and August are estimated to contribute 20 % to 80 % of the 30–50 nm particle number density. DMS-oxidation-driven nucleation is facilitated by the presence of atmospheric ammonia arising from seabird-colony emissions, and potentially also from coastal regions, tundra, and biomass burning. Via accumulation of secondary organic aerosol (SOA), a significant fraction of the new particles grow to sizes that are active in cloud droplet formation. Although the gaseous precursors to Arctic marine SOA remain poorly defined, the measured levels of common continental SOA precursors (isoprene

Details

Database :
OAIster
Notes :
application/pdf, http://archipel.uqam.ca/12408/7/Abbat_et_al_AtmosChemPhys-19-2527-2019-supplement.pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1096254764
Document Type :
Electronic Resource