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Secondary Organic Contribution to Particles Formed on the Ice Melted Arctic Ocean
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2013 (English)In: International Journal of Environmental, Chemical, Ecological, Geological and Geophysical Engineering, ISSN P:2010-376X, E:2010-3778, Vol. 7, no 10, 716-719 p.Article in journal (Refereed) Published
Abstract [en]

Due to climate warming and consequently due to ice and snow melting of the Arctic Ocean, the highly biologically active ocean surface area has been expanding quickly making possible longer marine biota growth seasons during polar summers. That increase the probability of the remote marine environment secondary contribution, especially secondary organic contribution, to the particle production and particle growth events and particle properties, consequently effecting on the open ocean, pack ice and ground based regions radiation budget and thus on the feedbacks between arctic biota, particles, clouds, and climate.

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2013. Vol. 7, no 10, 716-719 p.
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Natural Sciences
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URN: urn:nbn:se:polar:diva-3307OAI: oai:DiVA.org:polar-3307DiVA: diva2:1052978
Available from: 2016-12-07 Created: 2016-12-07 Last updated: 2016-12-07

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