Secondary Organic Contribution to Particles Formed on the Ice Melted Arctic Ocean

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 environmen...

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Bibliographic Details
Main Authors: Petri Vaattovaara, Zoran D. Ristovski, Martin Graus, Marcus Müller, EijaAsmi, Luca Di Liberto, StaffanSjögren, Douglas Orsini, Caroline Leck, Ari Laaksonen
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Arctic Ocean
ice melting
nucleation
secondary organics
clouds
climate
Arctic
Online Access:https://zenodo.org/record/1092154
https://doi.org/10.5281/zenodo.1092154
Description
Summary: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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