Air-sea carbon cycling in mixed ice-ocean environments

冰海混合环境中的海气碳循环

• 批准号: 227538-2012
• 负责人: Papakyriakou, Timothy
• 金额: $ 2.33万
• 依托单位: University of Manitoba
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2013
• 资助国家: 加拿大
• 起止时间: 2013-01-01 至 2014-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=524008
• 关键词: Air; sea; carbon; cycling; mixed

Because the world's oceans are the largest of the planet's carbon sinks, offsetting around 30% of present anthropogenic emissions, it is especially important that we understand important features of the marine carbon cycle and that these features are soundly represented in general circulation models. A critical gap in our understanding of the system's CO2 source/sink dynamics relates to the role played by sea ice. The traditional assumption adopted for both models and polar marine CO2 flux studies is for sea ice to exist as an impermeable layer, preventing air-sea exchange. Research in the last decade has shown sea ice to be an active participant in the marine carbon cycle, exchanging CO2 between both the ocean and atmosphere, and hence the assumption that sea ice is a passive participant in the polar marine carbon cycle is incorrect. Despite advancements in our understanding of the sea ice carbonate system, we still do not know exactly how sea ice influences air-sea CO2 exchange, and by extension, the net effect of sea ice on a region's carbon budget.

由于世界海洋是地球上最大的碳汇，抵消了目前人为排放量的约 30%，因此了解海洋碳循环的重要特征以及这些特征在大气环流模型中得到充分体现尤为重要。我们对系统二氧化碳源/汇动态的理解中的一个关键差距与海冰所扮演的角色有关。模型和极地海洋二氧化碳通量研究采用的传统假设是海冰作为不可渗透层存在，阻止空气与海洋的交换。过去十年的研究表明，海冰是海洋碳循环的积极参与者，在海洋和大气之间交换二氧化碳，因此海冰是极地海洋碳循环的被动参与者的假设是不正确的。 尽管我们对海冰碳酸盐系统的理解取得了进展，但我们仍然不确切地知道海冰如何影响海气二氧化碳交换，以及海冰对一个地区碳预算的净影响。