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From:Atmospheric Chemistry and Physics (Vol. 22, Issue 9) Peer-ReviewedWhile carbon dioxide is the main cause for global warming, modeling short-lived climate forcers (SLCFs) such as methane, ozone, and particles in the Arctic allows us to simulate near-term climate and health impacts for a...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 4) Peer-Reviewed
Motivated by the need to predict how the Arctic atmosphere will change in a warming world, this article summarizes recent advances made by the research consortium NETCARE (Network on Climate and Aerosols: Addressing...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 9) Peer-Reviewed
Dimethylsulfide (DMS), outgassed from ocean waters, plays an important role in the climate system, as it oxidizes to methane sulfonic acid (MSA) and sulfur dioxide (SO.sub.2 ), which can lead to the formation of...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 10) Peer-Reviewed
Satellite-derived aerosol products provide long-term and large-scale observations for analysing aerosol distributions and variations, climate-scale aerosol simulations, and aerosol-climate interactions. Therefore, a...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 13) Peer-ReviewedThe Arctic is warming 2 to 3 times faster than the global average, partly due to changes in short-lived climate forcers (SLCFs) including aerosols. In order to study the effects of atmospheric aerosols in this warming,...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 1) Peer-ReviewedLow clouds persist in the summer Arctic with important consequences for the radiation budget. In this study, we simulate the linear relationship between liquid water content (LWC) and cloud droplet number concentration...