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Abstract

Aerosols play a key role in the radiation balance of the atmosphere. Here, we present evidence that the European boreal region is a substantial source of both aerosol mass and aerosol number. The investigation supplies a straightforward relation between emissions of monoterpenes and gas-to-particle formation over regions substantially lacking in anthropogenic aerosol sources. Our results show that the forest provides an aerosol population of 1000 to 2000 particles of climatically active sizes per cubic centimeter during the late spring to early fall period. This has important implications for radiation budget estimates and relevancy for the evaluation of feedback loops believed to determine our future climate.
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We acknowledge the financial support from International and National Abatement Strategies for Transboundary Air Pollution (ASTA) and Nordic Center of Excellence, research unit on Biosphere-Aerosol-Cloud-Climate Interactions (BACCI).

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Published In

Science
Volume 312 | Issue 5771
14 April 2006

Submission history

Received: 28 November 2005
Accepted: 17 March 2006
Published in print: 14 April 2006

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Authors

Affiliations

P. Tunved*
Department of Applied Environmental Science (ITM), Air Pollution Laboratory, Frescativägen 54, SE-106 91, Stockholm, Sweden.
H.-C. Hansson
Department of Applied Environmental Science (ITM), Air Pollution Laboratory, Frescativägen 54, SE-106 91, Stockholm, Sweden.
V.-M. Kerminen
Finnish Meteorological Institute, Post Office Box 503 (Erik Palmenin Aukio 1), FI-00101 Helsinki, Finland.
J. Ström
Department of Applied Environmental Science (ITM), Air Pollution Laboratory, Frescativägen 54, SE-106 91, Stockholm, Sweden.
M. Dal Maso
Department of Physical Sciences, University of Helsinki, Gustav Hällströmin katu 2, FI-00014 Helsinki, Finland.
H. Lihavainen
Finnish Meteorological Institute, Post Office Box 503 (Erik Palmenin Aukio 1), FI-00101 Helsinki, Finland.
Y. Viisanen
Finnish Meteorological Institute, Post Office Box 503 (Erik Palmenin Aukio 1), FI-00101 Helsinki, Finland.
P. P. Aalto
Department of Physical Sciences, University of Helsinki, Gustav Hällströmin katu 2, FI-00014 Helsinki, Finland.
M. Komppula
Finnish Meteorological Institute, Post Office Box 503 (Erik Palmenin Aukio 1), FI-00101 Helsinki, Finland.
M. Kulmala
Department of Physical Sciences, University of Helsinki, Gustav Hällströmin katu 2, FI-00014 Helsinki, Finland.

Notes

* To whom correspondence should be addressed. E-mail: [email protected]

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