Frontiers Science Center for Deep Ocean Multispheres and Earth System,
and Key Laboratory of Marine Environment and Ecology, Ministry of Education,
Ocean University of China, Qingdao, 266100, China
Laboratory for Marine Ecology and Environmental Science, Qingdao
National Laboratory for Marine Science and Technology, Qingdao, 266237,
China
Deqiang Zhang
Frontiers Science Center for Deep Ocean Multispheres and Earth System,
and Key Laboratory of Marine Environment and Ecology, Ministry of Education,
Ocean University of China, Qingdao, 266100, China
Juntao Wang
Frontiers Science Center for Deep Ocean Multispheres and Earth System,
and Key Laboratory of Marine Environment and Ecology, Ministry of Education,
Ocean University of China, Qingdao, 266100, China
Frontiers Science Center for Deep Ocean Multispheres and Earth System,
and Key Laboratory of Marine Environment and Ecology, Ministry of Education,
Ocean University of China, Qingdao, 266100, China
Laboratory for Marine Ecology and Environmental Science, Qingdao
National Laboratory for Marine Science and Technology, Qingdao, 266237,
China
Frontiers Science Center for Deep Ocean Multispheres and Earth System,
and Key Laboratory of Marine Environment and Ecology, Ministry of Education,
Ocean University of China, Qingdao, 266100, China
Laboratory for Marine Ecology and Environmental Science, Qingdao
National Laboratory for Marine Science and Technology, Qingdao, 266237,
China
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Through the cruise campaign conducted over marginal seas in China, we found that the concentrations of condensation nuclei (Ncn) and cloud condensation nuclei (Nccn) were 1 order of magnitude larger than those in remote clear marine atmospheres, indicating overwhelming contributions from marine traffic emissions and long-range continental transport. Moreover, we derived regression equations used to estimate Ncn and Nccn from SO2 when the direct observations of Ncn and Nccn are not available.
Through the cruise campaign conducted over marginal seas in China, we found that the...
