Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Sara Marie Blichner"'
Publikováno v:
Atmospheric Chemistry and Physics. 21:17243-17265
Historically, aerosols of anthropogenic origin have offset some of the warming from increased atmospheric greenhouse gas concentrations. The strength of this negative aerosol forcing, however, is highly uncertain – especially the part originating f
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 3335-3359 (2021)
Aerosol–cloud interactions contribute to a large portion of the spread in estimates of climate forcing, climate sensitivity and future projections. An important part of this uncertainty is how much new particle formation (NPF) contributes to cloud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::963a511f742d1d4a702f651cb1f01e87
http://hdl.handle.net/10852/91536
http://hdl.handle.net/10852/91536
Cloud-aerosol interactions give rise to much of the uncertainty in estimates of climate forcing, climate sensitivity and thus also future climate predictions. Furthermore, the modelled concentration of cloud condensation nuclei (CCN) in the past, pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00370bbf574f048e0759f8e4541518d3
https://doi.org/10.5194/egusphere-egu2020-9740
https://doi.org/10.5194/egusphere-egu2020-9740
Autor:
Declan O'Donnell, Roland Schrödner, Sara Marie Blichner, Twan van Noije, Moa K. Sporre, Inger Helene Hafsahl Karset, Terje Koren Berntsen, Tommi Bergman, Risto Makkonen
Biogenic volatile organic compounds (BVOCs) emitted from vegetation are oxidized in the atmosphere and can form aerosol particles either by contributing to new particle formation or by condensing onto existing aerosol particles. As the understanding
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fdcdd60af12975842c3eed4bac139df4
https://doi.org/10.5194/acp-2019-1166
https://doi.org/10.5194/acp-2019-1166