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Role of Sea Ice in the Formation of Annual Carbon Dioxide Cycle in the Arctic

机译:海冰在北极年度二氧化碳循环形成中的作用

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摘要

Exchange of carbon dioxide between the atmosphere and the ocean, which absorbs 25-50% of carbon dioxide released during fuel combustion, plays an important role in the global CO_2 cycle [1, 2]. At present, it has been established that absorption or emission of CO_2 by the World Ocean is irregular in space and variable in different seasons and years [3]. However, the role of the Arctic basin in the global and regional balance of CO_2 has not been examined by researchers, because they believed that the ice cover almost completely hampers gas exchange. The possibility of the significant influence of water areas with seasonal or constant ice cover on the regional and even global balance of CO_2 has been assumed in some recent publications [4, 5]. The present paper shows that sea ice could play a crucial role in variation of the annual cycle of CO_2 concentrations in polar latitudes.
机译:大气与海洋之间的二氧化碳交换吸收了燃料燃烧过程中释放的25-50%的二氧化碳,在全球CO_2循环中起着重要的作用[1,2]。目前,已经确定世界海洋对CO_2的吸收或排放在空间上是不规则的,并且在不同的季节和年份中是可变的[3]。然而,研究人员尚未研究北极盆地在全球和区域CO_2平衡中的作用,因为他们认为冰盖几乎完全阻碍了气体交换。在最近的一些出版物中[4,5],已经假定可能出现季节性或恒定冰覆盖的水域对区域甚至全球CO_2平衡产生重大影响的可能性。本文表明,海冰可能在极地纬度中CO_2浓度年循环的变化中起关键作用。

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