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GAO Rongzhen,SUN Donghuai,WANG Dongxiao,YANG Xiaoyi. 2005. Cloudiness regime shift during 1946-1992 recorded by coral in the South China Sea. Acta Oceanologica Sinica, (5):27-34
Cloudiness regime shift during 1946-1992 recorded by coral in the South China Sea
Cloudiness regime shift during 1946-1992 recorded by coral in the South China Sea
Received:April 26, 2005  Revised:July 21, 2005
DOI:
Key words:coral gray value  cloudiness  regime shift  South China Sea
中文关键词:  coral gray value  cloudiness  regime shift  South China Sea
基金项目:
Author NameAffiliationE-mail
GAO Rongzhen Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Qingdao Meteorological Administration, Qingdao 266003, China 
 
SUN Donghuai Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology & Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510301, China  
WANG Dongxiao Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China dxwang@scsio.ac.cn 
YANG Xiaoyi Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China  
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Abstract:
      By extracting and comparing long-term trend components of coral gray value, sea surface temperature, cloudiness, and net heat flux for the period of 1946~1992, the relationships among them are addressed.There exists a prominent regime shift in the cloudiness associated with the corresponding variabilities of sea surface temperature and net heat flux occurred in the mid-1960s, which can be successfully recorded by coral gray value, a climatic proxy.Long-term cloudiness variations in the South China Sea are completely opposite to the equatorial western Pacific in the past five decades, whereas they share a similar trend to that over Asian monsoon prevailing waters.The fact that the coral gray value is highly correlated to cloudiness provides a unique perspective on utilizing this coral to study cloudiness variations in the pre-instrumental period.
中文摘要:
      By extracting and comparing long-term trend components of coral gray value, sea surface temperature, cloudiness, and net heat flux for the period of 1946~1992, the relationships among them are addressed.There exists a prominent regime shift in the cloudiness associated with the corresponding variabilities of sea surface temperature and net heat flux occurred in the mid-1960s, which can be successfully recorded by coral gray value, a climatic proxy.Long-term cloudiness variations in the South China Sea are completely opposite to the equatorial western Pacific in the past five decades, whereas they share a similar trend to that over Asian monsoon prevailing waters.The fact that the coral gray value is highly correlated to cloudiness provides a unique perspective on utilizing this coral to study cloudiness variations in the pre-instrumental period.
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