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dc.contributor.authorDai, Minhanzh_CN
dc.contributor.authorCao, Zhimianzh_CN
dc.contributor.authorGuo, Xianghuizh_CN
dc.contributor.authorZhai, Weidongzh_CN
dc.contributor.authorLiu, Zhiyuzh_CN
dc.contributor.authorYin, Zhiqiangzh_CN
dc.contributor.authorXu, Yanpingzh_CN
dc.contributor.authorGan, Jianpingzh_CN
dc.contributor.authorHu, Jianyuzh_CN
dc.contributor.authorDu, Chuanjunzh_CN
dc.contributor.author戴民汉zh_CN
dc.contributor.author郭香会zh_CN
dc.contributor.author翟惟东zh_CN
dc.contributor.author刘志宇zh_CN
dc.contributor.author甘剑平zh_CN
dc.contributor.author胡建宇zh_CN
dc.date.accessioned2015-07-22T03:12:24Z
dc.date.available2015-07-22T03:12:24Z
dc.date.issued2013-May 28zh_CN
dc.identifier.citationGEOPHYSICAL RESEARCH LETTERS, 2013,40(10):2154-2158zh_CN
dc.identifier.otherWOS:000328840200048zh_CN
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/88027
dc.descriptionNational Basic Research Program (973); Ministry of Science and Technology [2009CB421200, 2009CB421201]; National Natural Science Foundation of China [41121091, 90711005, 41130857]zh_CN
dc.description.abstractThe contemporary coastal ocean, characterized by abundant nutrients and high primary productivity, is generally seen as a significant CO2 sink at the global scale. However, mechanistic understanding of the coastal ocean carbon cycle remains limited, leading to the unanswered question of why some coastal systems are sources while others are sinks of atmospheric CO2. Here we proposed a distinct physical-biogeochemical setting, Ocean-dominated Margin (OceMar), in order for better shaping the concept of the coastal ocean carbon study. OceMars, in contrast to previously recognized River-dominated Ocean Margins, are characterized by dynamic interactions with the open ocean, which may provide nonlocal CO2 sources thereby modulating the CO2 fluxes in OceMars. Using the basin areas of the largest marginal seas of the Pacific and the Atlantic, the South China Sea and the Caribbean Sea as examples of OceMars, we demonstrated that such external CO2 sources controlled the CO2 fluxes.zh_CN
dc.language.isoen_USzh_CN
dc.publisherAMER GEOPHYSICAL UNIONzh_CN
dc.source.urihttp://dx.doi.org/10.1002/grl.50390zh_CN
dc.subjectOPEN-OCEAN STORAGEzh_CN
dc.subjectSOUTH CHINA SEAzh_CN
dc.subjectCARBON-DIOXIDEzh_CN
dc.subjectCOASTAL OCEANzh_CN
dc.subjectCARIBBEAN SEAzh_CN
dc.subjectFLUXESzh_CN
dc.subjectVARIABILITYzh_CN
dc.subjectEXCHANGEzh_CN
dc.subjectSYSTEMzh_CN
dc.subjectSINKSzh_CN
dc.titleWhy are some marginal seas sources of atmospheric CO2?zh_CN
dc.typeArticlezh_CN


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