海洋碳循环模型研究进展

Xu Yong-fu, Zhao Liang, PU Yi-fen
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引用次数: 2

摘要

本文从最简单的三盒模式开始,简要回顾了海洋碳循环模式的发展历史,讨论了各种模式在不同时期的特点,指出了海洋吸收大气co_2的能力。近年来,全球海洋循环碳循环模型多采用简单的生物地球化学模型,而基于过程的模型和一维模型则比较详细地探讨了生态系统在海洋碳循环中的作用。1995年,IGBP/GAIM启动了海洋碳循环模式比对项目(OCMIP)。两个阶段已经完成。第二阶段有13个建模组参与项目。虽然OCMIP目前处于第三阶段,但第一或第二阶段的一些文件仍在编写中。最新的全球海洋环流模式估计,20世纪80年代海洋年平均人为co2吸收量为1.5-2.2 GtC。尽管取得了许多成果,揭示了海洋吸收和大气CO_(2)分布的基本特征,但仍存在许多需要进一步研究的挑战,对此进行了讨论。其中一个严重的问题是物理场的一致性,这可以通过人为示踪剂的检查来评估。CO_(2)的海气交换参数化仍需进一步研究。采用带明确生态系统的碳循环模型是二氧化碳生物地球化学循环及其对全球变化响应研究的发展趋势。
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ADVANCES IN THE STUDIES OF OCEAN CARBON-CYCLE MODEL
This paper briefly reviews the history of development of ocean carbon-cycle models from the beginning of the simplest three-box model,discusses the features of various models at different times,and points out the ability of oceanic uptake of atmospheric CO_(2.)In recent years,the global ocean-circulation model of carbon cycle often uses a simple biogeochemical model,while in the process-based model and one-dimensional model the role of ecosystem in the ocean carbon cycle is explored in relative detail.In 1995,the Ocean Carbon-Cycle Model Intercomparison Project(OCMIP) was initiated by IGBP/GAIM.Two phases have been completed.In the second phase,13 modeling groups participated in the project.Although OCMIP is now in its third phase,some papers from the first or second phase are still in preparation.The newest global ocean-circulation models estimate an annual mean oceanic uptake of 1.5-2.2 GtC of anthropogenic CO_(2) for the 1980s.In spite of many achievements,which have revealed the basic features of oceanic uptake and distributions of atmospheric CO_(2),many challenges still remain that require further research,which is discussed.One of serious issues is the consistency of physical fields,which can be assessed through examination of anthropogenic tracers.The parameterization of air-sea exchange of CO_(2) still needs to be further studied.The use of the carbon cycle model with an explicit ecosystem is a developing trend in the study of biogeochemical cycle of carbon dioxide and its response to global change.
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