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GAO Shanhong,WU Wei,ZHU Leilei,FU Gang,HUANG Bin. 2009. Detection of nighttime sea fog/stratus over the Huanghai Sea using MTSAT-1R IR data. Acta Oceanologica Sinica, (2):23-35
Detection of nighttime sea fog/stratus over the Huanghai Sea using MTSAT-1R IR data
Detection of nighttime sea fog/stratus over the Huanghai Sea using MTSAT-1R IR data
Received:March 25, 2008  Revised:June 16, 2008
DOI:
Key words:Huanghai Sea  nighttime sea fog  MTSAT-1R  dual channel difference method
中文关键词:  Huanghai Sea  nighttime sea fog  MTSAT-1R  dual channel difference method
基金项目:The National Natural Science Foundation of China under contract No. 40706004, the National Basic Research Program ("973" program) of China under contract No. 2005CB422301; China Meteorological Administration's New Technology Extension Project under contract No. CMATG2008M41; the National Special Fund for public Sector Research of China under contract No. GYHY200706031, Shandong Provincial Meteorological Bureau Science Fund of China under contract No. 2004SDQXJ01.
Author NameAffiliationE-mail
GAO Shanhong Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China gaosh@ouc.edu.cn 
WU Wei Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China
Shandong Provincial Meteorological Institute, Jinan 250031, China 
 
ZHU Leilei Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China  
FU Gang Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China  
HUANG Bin National Meteorological Center, China Meteorological Administration, Beijing 100081, China  
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Abstract:
      A dual channel difference (DCD) method is applied to detect nighttime sea fog/stratus over the Huanghai Sea using the infrared (IR) data of shortwave (3.5-4.0 μm) and longwave (10.3-11.3 μm) channels from the Multi-functional Transport Satellite (MTSAT)-1R, i.e., shortwave minus longwave brightness temperature difference (SLTD). Twenty-four sea fog events over the Huanghai Sea during March to July of 2006 and 2007 are chosen to determine a suitable value of SLTD for nighttime sea fog/stratus detection, and it is found that the value of -5.5-2.5℃ can be taken as a criterion. Two case examples of sea fog events are especially demonstrated in detail utilizing the criterion, and the results show that the derived sea fog/stratus coverage is quite reasonable. This coverage information is very helpful to analyze the formation and evolution of sea fog/stratus during night and can provide sea fog researchers with observational evidences for model results verification. However, more efforts are needed to further obtain vertical extent information of sea fog/stratus and attempt to discriminate between sea fog and stratus.
中文摘要:
      A dual channel difference (DCD) method is applied to detect nighttime sea fog/stratus over the Huanghai Sea using the infrared (IR) data of shortwave (3.5-4.0 μm) and longwave (10.3-11.3 μm) channels from the Multi-functional Transport Satellite (MTSAT)-1R, i.e., shortwave minus longwave brightness temperature difference (SLTD). Twenty-four sea fog events over the Huanghai Sea during March to July of 2006 and 2007 are chosen to determine a suitable value of SLTD for nighttime sea fog/stratus detection, and it is found that the value of -5.5-2.5℃ can be taken as a criterion. Two case examples of sea fog events are especially demonstrated in detail utilizing the criterion, and the results show that the derived sea fog/stratus coverage is quite reasonable. This coverage information is very helpful to analyze the formation and evolution of sea fog/stratus during night and can provide sea fog researchers with observational evidences for model results verification. However, more efforts are needed to further obtain vertical extent information of sea fog/stratus and attempt to discriminate between sea fog and stratus.
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