Articles | Volume 11, issue 16
https://doi.org/10.5194/acp-11-8677-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-11-8677-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
25 Aug 2011
Research article |
| 25 Aug 2011
Anthropogenic emissions during Arctas-A: mean transport characteristics and regional case studies
D. L. Harrigan
National Oceanic and Atmospheric Administration, National Weather Service, Tallahassee, FL, USA
Department of Meteorology, Florida State University, Tallahassee, FL, USA
H. E. Fuelberg
Department of Meteorology, Florida State University, Tallahassee, FL, USA
I. J. Simpson
Department of Chemistry, University of California, Irvine, CA, USA
D. R. Blake
Department of Chemistry, University of California, Irvine, CA, USA
G. R. Carmichael
Center for Global and Regional Environmental Research, University of Iowa, Iowa City, IA, USA
G. S. Diskin
NASA Langley Research Center, Hampton, VA, USA
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- On the relationship between Arctic ice clouds and polluted air masses over the North Slope of Alaska in April 2008 C. Jouan et al. 10.5194/acp-14-1205-2014
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- Detection in the summer polar stratosphere of pollution plume from East Asia and North America by balloon-borne in situ CO measurements G. Krysztofiak et al. 10.5194/acp-12-11889-2012
- Long-term variations in wintertime Arctic frontal positions and their mercury anthropogenic emission impacts D. Wang & H. Mao 10.1016/j.atmosenv.2020.118027
2 citations as recorded by crossref.
- Accumulation-mode aerosol number concentrations in the Arctic during the ARCTAS aircraft campaign: Long-range transport of polluted and clean air from the Asian continent H. Matsui et al. 10.1029/2011JD016189
- Patterns of CO2and radiocarbon across high northern latitudes during International Polar Year 2008 S. Vay et al. 10.1029/2011JD015643
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