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HUANG Jian,ZHOU Faxiu. 2006. The cooling and moistening effect on the formation of sea fog in the Huanghai Sea. Acta Oceanologica Sinica, (2):49－62
The cooling and moistening effect on the formation of sea fog in the Huanghai Sea
The cooling and moistening effect on the formation of sea fog in the Huanghai Sea
Received:August 05, 2005  Revised:January 16, 2006
DOI：
Key words:sea fog in Huanghai Sea  cooling effect  moistening effect  water vapor transportation
中文关键词:  sea fog in Huanghai Sea  cooling effect  moistening effect  water vapor transportation
基金项目:
Author NameAffiliationE-mail
HUANG Jian Department of Marine Meteorology, Ocean University of China, Qingdao 266003, China
Institute of Tropical and Marine Meteorology of Guangzhou, China Meteorological Administration, Guangzhou 510080, China 		hj@grmc.gov.cn 
ZHOU Faxiu Department of Marine Meteorology, Ocean University of China, Qingdao 266003, China  
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Abstract:
      With the sea surface observations from ICOADS for the years 1960~2002, the conditions of cooling, evaporation and water vapor transportation are analyzed and compared for the formation of seasonal sea fog in April-July in the Huanghai Sea.It is found that sea surface cooling is always existent during the fog seasons while sea surface evaporation only appears in April-June in the Huanghai Sea.Local evaporation alone is not sufficient to form fogs though it may lead to light ones.Water vapor transported from the low-latitudes accomplished by specific synoptic systems is the most important condition for sea fog formation.In general, the moistening effect is more important than the cooling one.
中文摘要:
      With the sea surface observations from ICOADS for the years 1960~2002, the conditions of cooling, evaporation and water vapor transportation are analyzed and compared for the formation of seasonal sea fog in April-July in the Huanghai Sea.It is found that sea surface cooling is always existent during the fog seasons while sea surface evaporation only appears in April-June in the Huanghai Sea.Local evaporation alone is not sufficient to form fogs though it may lead to light ones.Water vapor transported from the low-latitudes accomplished by specific synoptic systems is the most important condition for sea fog formation.In general, the moistening effect is more important than the cooling one.
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