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A Fog Event off the Coast of the Hangzhou Bay during Meiyu Period in June 2013

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Article In Press
DOI: 10.4209/aaqr.2016.11.0489
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Qian Wang1,2, Su-Ping Zhang 1,2, Qi Wang3, Zhao-Xi Meng4, Darko Korańćin5,6, Shan-Hong Gao1,2

  • 1 Physical Oceanography Laboratory/CIMST & Ocean-Atmosphere Interaction and Climate Laboratory, Ocean University of China, Qingdao 266100, China
  • 2 Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
  • 3 Meteorological Observatory of Jilin Province, Changchun 130062, China
  • 4 Hanban/Confucius Institute Headquarters, Beijing 100088, China
  • 5 Physics Department, Faculty of Science, University of Split, 21000 Split, Croatia
  • 6 Division of Atmospheric Sciences, Desert Research Institute, Reno, NV 89512, USA


The Meiyu front provided background conditions for the coastal fog process.
Coastal front was essential for the local fog episode.
Southeasterly wind induced by the coastal front brought air to cooler sea surface.
Subsiding motion from a secondary circulation lowered the ABL.
These results are helpful for coastal fog forecast in Meiyu period.


A dense fog with the visibility less than 100 m over 6 hours occurred around the Hangzhou Bay off the coast of the western part of the East China Sea on 24–25 June 2013 during Meiyu period. This study focuses on the physical mechanism involved in the fog process by using in-situ observations and model. The analysis indicates that the land-sea thermal contrast played an essential role in the fog episode, while a weak low-pressure wedge associated with the Meiyu front and the diurnal variation in temperature provided background conditions. Induced by the strong land-sea thermal contrast, a secondary circulation formed in the lower levels of the atmospheric boundary layer (ABL) over the coast. The southeasterly wind and subsiding motion associated with the secondary circulation contributed to the moisture supply and the lowering of the boundary layer, favoring fog formation and maintenance. The fog maintained until the weakening of the temperature gradient between land and sea, when the downward flow was replaced by upward motion controlled by the approaching of a low-pressure center. These results are helpful for improving coastal fog forecast in Meiyu period and for our understanding of mechanisms involved in coastal fog processes.


Coastal fog Land-sea thermal contrast Meiyu period Secondary circulatio

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