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Atmospheric Supply of Nitrogen, Cadmium, Mercury and B(a)P to the Baltic Sea in 2022

Gauss, Michael; Travnikov, Oleg; Gačnik, Jan; Aas, Wenche; Klein, Heiko; Nyiri, Agnes

Norwegian Meteorological Institute

2024

Atmospheric Supply of Nitrogen, Cadmium, Lead, Mercury, PCDD/Fs, PCB-153, and B(a)P to the Baltic Sea EMEP/MSC-W Report for HELCOM

Gauss, Michael; Gusev, Alexey; Aas, Wenche; Hjellbrekke, Anne-Gunn; Ilyin, Ilia; Klein, Heiko; Nyiri, Agnes; Rozovskaya, Olga; Shatalov, Victor; Strijkina, Irina; Travnikov, Oleg

Norwegian Meteorological Institute

2020

Atmospheric sub-domain progress report

Myhre, Cathrine Lund; Boulanger, Damien; Rivier, Leo; Fiebig, Markus

2020

Atmospheric signals of methane emissions from the Arctic seabed around Svalbard: What flux rates are needed in order to be identified?

Myhre, C. L.; Ferré, B.; Platt, S. M.; Pisso, I.; Allen, G.; Pitt, J.; Schmidbauer, N.; Hermansen, O.; Silyakova, A.; Vadakkepuliyambatta, S.; Stohl, A.; Myhre, G.; Pyle, J.; Mienert, J.

2016

Atmospheric short-chain-chlorinated paraffins in Melbourne, Australia - first extensive Southern Hemisphere observations.

Gillett, R. W.; Galbally, I. E.; Keywood, M. D.; Powell, J. C.; Stevenson, G.; Yates, A.; Borgen, A. R.

2017

Atmospheric polychlorinated biphenyls in Indian cities: Levels, emission sources and toxicity equivalents.

Chakraborty, P.; Zhang, G.; Eckhardt, S.; Li, J.; Breivik, K.; Lam, P.K.S.; Tanabe, S.; Jones, K.C.

2013

Atmospheric particles evolution during Hg depletion events.

Ferrari, C.P.; Gauchard, P.-A.; Dommergue, A.; Magand, O.; Nagorski, S.; Boutron, C.F.; Temme, C.; Bahlmann, E.; Ebinghaus, R.; Steffen, A.; Banic, C.; Aspmo, K.,, Berg, T.

2004

Atmospheric ozone and methane in a changing climate.

Isaksen, I.S.A.; Berntsen, T.K.; Dalsøren, S.B.; Eleftheratos, K.; Orsolini, Y.; Rognerud, B.; Stordal, F.; Søvde, O.A.; Zerefos, C.; Holmes, C.D.

2014

Atmospheric occurrence and gas-particle partitioning of PBDEs in an industrialised and urban area of Florence, Italy.

Cincinelli, A.; Pieri, F.; Martellini, T.; Passaponti, M.; Del Bubba, M.; Del Vento, S.; Katsoyiannis, A.

2014

Atmospheric observations of methane at the Zeppelin Observatory, Ny Ålesund, Svalbard

Platt, Stephen Matthew; Aas, Wenche; Lunder, Chris Rene; Hermansen, Ove; Thompson, Rona Louise; Pisso, Ignacio

2024

Atmospheric new particle formation characteristics in the Arctic as measured at Mount Zeppelin, Svalbard, from 2016 to 2018

Lee, Haebum; Lee, Kwangyul; Lunder, Chris Rene; Krejci, Radovan; Aas, Wenche; Park, Jiyeon; Park, Ki-Tae; Lee, Bang Yong; Yoon, Young Jun; Park, Kihong

We conducted continuous measurements of nanoparticles down to 3 nm size in the Arctic at Mount Zeppelin, Ny Ålesund, Svalbard, from October 2016 to December 2018, providing a size distribution of nanoparticles (3–60 nm). A significant number of nanoparticles as small as 3 nm were often observed during new particle formation (NPF), particularly in summer, suggesting that these were likely produced near the site rather than being transported from other regions after growth. The average NPF frequency per year was 23 %, having the highest percentage in August (63 %). The average formation rate (J) and growth rate (GR) for 3–7 nm particles were 0.04 cm−3 s−1 and 2.07 nm h−1, respectively. Although NPF frequency in the Arctic was comparable to that in continental areas, the J and GR were much lower. The number of nanoparticles increased more frequently when air mass originated over the south and southwest ocean regions; this pattern overlapped with regions having strong chlorophyll a concentration and dimethyl sulfide (DMS) production capacity (southwest ocean) and was also associated with increased NH3 and H2SO4 concentration, suggesting that marine biogenic sources were responsible for gaseous precursors to NPF. Our results show that previously developed NPF occurrence criteria (low loss rate and high cluster growth rate favor NPF) are also applicable to NPF in the Arctic.

2020

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