Special Issue "Climate-Chemistry Interactions"

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A special issue of Atmosphere (ISSN 2073-4433).

Deadline for manuscript submissions: 31 March 2015

Special Issue Editor

Guest Editor
Prof. Dr Ivar S. A. Isaksen
Department of Geosciences, University of Oslo, Oslo, Norway
Website: http://www.mn.uio.no/geo/english/people/aca/metos/ivaris/index.html
E-Mail: i.s.a.isaksen@geo.uio.no
Interests: Atmospheric chemistry and climate-chemistry interactions, with emphasis on processes describing changes in chemical active greenhouse gases (ozone, methane, CFCs, HCFCs) and secondary particles (sulfate, nitrate organics) and of importance for ozone depletion and atmospheric oxidation and regional air pollution.

Special Issue Information

Dear Colleagues,

Climate–chemistry interaction is currently, and will in the future, be affected by pollutant emissions from different sources. There will also be interaction with emissions from natural sources. Key compounds affecting climate–chemistry interactions are emissions of NOx, CO, VOCs, sulfur dioxide, methane and isoprene. Furthermore, secondary compounds formed and broken down in the atmosphere, such as ozone (O3), the hydroksyl radical (OH), the hydrogen peroksy radical (HO2), hydrogen peroxygen (H2O2), sulfate and organic aerosols, play a role for the oxidation of gases. Oxidation of halogens will affect chemical processes in the stratosphere. Increased NOx emission will have enhanced impact on climate through direct O3 impact. Increased methane emissions will increase the direct climate impact. However, OH is reduced when methane increases, giving less climate impact. The impact of sulfate emissions will lead to cooling of the atmosphere. The impact of CO2, due to methane oxidation with increasing emissions, will give enhanced climate impact. The impact of emission of gases affecting climate will be highly different depending on sources. For instance, the emission of gases from aircraft, ship and land based transport sectors have differing impacts on climate–chemistry interations. Keypoints in studies of future climate–chemistry interactions are the development in gaseous emissions from different natural and anthropogenic sources, and the increases and reductions in climate impact from the different climate gases.

Prof. Dr. Ivar S. A. Isaksen
Guest Editor

Submission

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. Papers will be published continuously (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are refereed through a peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Atmosphere is an international peer-reviewed Open Access quarterly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 500 CHF (Swiss Francs). English correction and/or formatting fees of 250 CHF (Swiss Francs) will be charged in certain cases for those articles accepted for publication that require extensive additional formatting and/or English corrections.

Published Papers (1 paper)

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p. 518-535
by , , , , , , , ,  and
Atmosphere 2014, 5(3), 518-535; doi:10.3390/atmos5030518
Received: 13 September 2013; in revised form: 19 March 2014 / Accepted: 17 June 2014 / Published: 29 July 2014
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(This article belongs to the Special Issue Climate-Chemistry Interactions)
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Last update: 28 July 2014

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