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dc.contributor.authorPaasonen, Pauli
dc.contributor.authorAsmi, Ari
dc.contributor.authorPetäjä, Tuukka
dc.contributor.authorKajos, Maija K.
dc.contributor.authorÄijälä, Mikko
dc.date.accessioned2015-11-16T07:14:31Z
dc.date.available2015-11-16T07:14:31Z
dc.date.issued2013
dc.identifier.citationPaasonen, P. et al. 2013. Warming-induced increase in aerosol number concentration likely to moderate climate change. Nature geoscience, 6:438-442. [http://dx.doi.org/10.1038/ngeo1800]en_US
dc.identifier.issn1752-0894
dc.identifier.issn1752-0908 (Online)
dc.identifier.urihttp://hdl.handle.net/10394/15064
dc.identifier.urihttp://dx.doi.org/10.1038/ngeo1800
dc.description.abstractAtmospheric aerosol particles influence the climate system directly by scattering and absorbing solar radiation, and indirectly by acting as cloud condensation nuclei1, 2, 3, 4. Apart from black carbon aerosol, aerosols cause a negative radiative forcing at the top of the atmosphere and substantially mitigate the warming caused by greenhouse gases1. In the future, tightening of controls on anthropogenic aerosol and precursor vapour emissions to achieve higher air quality may weaken this beneficial effect5, 6, 7. Natural aerosols, too, might affect future warming2, 3, 8, 9. Here we analyse long-term observations of concentrations and compositions of aerosol particles and their biogenic precursor vapours in continental mid- and high-latitude environments. We use measurements of particle number size distribution together with boundary layer heights derived from reanalysis data to show that the boundary layer burden of cloud condensation nuclei increases exponentially with temperature. Our results confirm a negative feedback mechanism between the continental biosphere, aerosols and climate: aerosol cooling effects are strengthened by rising biogenic organic vapour emissions in response to warming, which in turn enhance condensation on particles and their growth to the size of cloud condensation nuclei. This natural growth mechanism produces roughly 50% of particles at the size of cloud condensation nuclei across Europe. We conclude that biosphere–atmosphere interactions are crucial for aerosol climate effects and can significantly influence the effects of anthropogenic aerosol emission controls, both on climate and air quality.en_US
dc.description.urihttp://www.nature.com/ngeo/journal/v6/n6/pdf/ngeo1800.pdf
dc.language.isoenen_US
dc.publisherNature Publishing Groupen_US
dc.subjectClimate sciencesen_US
dc.subjectAtmospheric scienceen_US
dc.titleWarming-induced increase in aerosol number concentration likely to moderate climate changeen_US
dc.typeArticleen_US


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