Articles | Volume 25, issue 19
https://doi.org/10.5194/acp-25-11867-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-25-11867-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
01 Oct 2025
Research article |
| 01 Oct 2025
| 01 Oct 2025
An observational estimate of Arctic UV-absorbing aerosol direct radiative forcing on instantaneous and climatic scales
Department of Atmospheric Sciences, University of North Dakota, Grand Forks, ND 58202, United States of America
now at: the National Research Council, Monterey, CA 93943, United States of America
Jianglong Zhang
Department of Atmospheric Sciences, University of North Dakota, Grand Forks, ND 58202, United States of America
Jeffrey S. Reid
Marine Meteorology Division, U.S. Naval Research Laboratory, Monterey, CA 93943, United States of America
Peng Xian
Marine Meteorology Division, U.S. Naval Research Laboratory, Monterey, CA 93943, United States of America
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Peng Xian, Philip J. Klotzbach, Jason P. Dunion, Matthew A. Janiga, Jeffrey S. Reid, Peter R. Colarco, and Zak Kipling
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Short summary
Plumes of wildfire smoke in the Arctic affect the Arctic radiative budget. Using a neural network and observations from satellite-based sensors, we analyzed the direct radiative forcing of smoke particles on the Arctic climate and estimated long-term forcing trends. Strong negative trends in aerosol direct radiative forcing were found in northern Russia and Canada, with positive trends found over parts of the Arctic Ocean. Overall, smoke plumes may act to counter future Arctic warming.
Plumes of wildfire smoke in the Arctic affect the Arctic radiative budget. Using a neural...
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