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SUMMER SURFACE WATER pCO2 AND CO2 FLUX AT AIR-SEA INTERFACE IN WESTERN PART OF THE EAST CHINA SEA
Author(s): 
Pages: 239-245
Year: Issue:  3
Journal: OCEANOLOGIA ET LIMNOLOGIA SINICA

Keyword:  东海二氧化碳分压(pCO2)碳通量;
Abstract: 根据2001年夏季长江口及东海西部海域表层海水pCO2的实测数据,结合水文、化学和生物等要素的同步观测资料,对该海域pCO2分布和变化的重要影响因素进行了探讨.结果表明,长江冲淡水是造成东海西部海域表层海水pCO2分布不均匀的主要原因.利用Wanninkhof(1992)提出的通量模式计算,长江口口门附近海域和浙江近岸海域为CO2的源区,123°E以东的调查海域表现为大气CO2的汇,尤其是以123°E,32°N为中心,存在着一个极强的大气CO2汇区.就整个东海西部海域而言,夏季可从大气净吸收15.3×104 t C.
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