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黑潮与毗邻陆架海域的碳交换

DOI: 10.11867/j.issn.1001-8166.2015.02.0214, PP. 214-225

Keywords: 碳交换,黑潮,东海陆架,南海陆架

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Abstract:

作为沟通陆架边缘海与开放大洋的北太平洋西边界流,黑潮对毗邻中国陆架海域碳循环有着不可忽视的影响。分析总结了黑潮与毗邻陆架海域海水中溶解有机碳(DOC)、颗粒有机碳(POC)、溶解无机碳(DIC)和颗粒无机碳(PIC)分布与交换的现有研究成果。分析表明,黑潮通过表层水涡旋、入侵以及次表层以下水体上涌等形式携碳进入毗邻陆架海域。在黑潮与毗邻陆架海域,DOC和POC的分布受生物活动、水团混合以及沉积物—水界面相互作用的共同影响,表层与陆架水中含量较高,DIC受海水碳酸盐体系平衡影响,表层含量低于底层,在陆架海域与上升流区有高值,PIC含量较低。在台湾东北海域,DOC,POC和DIC由东海陆架海域向黑潮有净输出,输出量分别为2431×109,1051×109和21733×109molC/a,PIC通过陆架源悬浮颗粒物向黑潮主流输送,通量为1852×109molC/a。DOC,POC和PIC由南海经吕宋海峡向黑潮有净输出,输出量分别为2652×109,1009×109和230×109molC/a,但DIC由黑潮向南海有净输出,通量为13005×109molC/a。台湾海峡碳循环受黑潮输运的影响,但影响机制及过程至今并不清楚。因此,黑潮与毗邻陆架海域的碳交换过程研究还有若干重大科学问题亟待解决,尚需深入系统的研究。

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