Key Laboratory of Marine Environment and Ecology, Ministry
of Education/Institute for Advanced Ocean Study, Ocean University of China,
Qingdao, Shandong, 266100, China
Laboratory for Marine Ecology and
Environmental Science, Qingdao National Laboratory for Marine Science and
Technology, Qingdao, 266100, China
Atmospheric Chemistry and
Climate and Global Dynamics Divisions, National Center for Atmospheric
Research, Boulder, CO, USA
Jianren Fan
State Key Laboratory of Clean Energy, Department of Energy
Engineering, Zhejiang University, Hangzhou, Zhejiang, 310027,
China
Xiaohong Yao
Key Laboratory of Marine Environment and Ecology, Ministry
of Education/Institute for Advanced Ocean Study, Ocean University of China,
Qingdao, Shandong, 266100, China
Laboratory for Marine Ecology and
Environmental Science, Qingdao National Laboratory for Marine Science and
Technology, Qingdao, 266100, China
Key Laboratory of Marine Environment and Ecology, Ministry
of Education/Institute for Advanced Ocean Study, Ocean University of China,
Qingdao, Shandong, 266100, China
Laboratory for Marine Ecology and
Environmental Science, Qingdao National Laboratory for Marine Science and
Technology, Qingdao, 266100, China
Tatsuya Nagashima
National Institute for
Environmental Studies, Tsukuba, Japan
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849
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ACCMIP simulations were used to study NOy deposition over East Asia in the future. Both dry and wet NOy deposition show significant decreases in the 2100s under RCP4.5 and RCP8.5 due to large anthropogenic emission reduction. The changes in climate only significantly affect the wet deposition primarily linked to changes in precipitation. Over the coastal seas of China, weaker transport of NOy from land due to emission reduction infers a larger impact from shipping and lightning emissions.
ACCMIP simulations were used to study NOy deposition over East Asia in the future. Both dry and...
