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Can CFCs be used to determine anthropogenic CO_2?

机译:可以使用氟氯化碳确定人为的CO_2吗?

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From model simulations of the uptake of CFC-11, CFC-12 and anthropogenic CO_2, we investigate the method of using CFC-derived water ages to determine the anthropogenic CO_2 accumulation in the ocean. The CFC age method is best suited to water younger than 30 years where CFC water ages are most reliable. For water younger than 30 years, the CFC-12 and CFC-11 age method can estimate the global 1980–1990 accumulation of anthropogenic CO_2 to within 10% and 22%, respectively. With the exception of the Southern Ocean south of 50 °S and the equatorial upwelling areas, these CFC-derived estimates of the water column inventory of anthropogenic CO2 are within 10% of the simulated values. Our results suggest that the CFC age method provides another way of determining the accumulation of anthropogenic CO_2 in the ocean. We applied the CFC age method to observed CFC data to estimate the accumulation of anthropogenic CO_2 in the North Pacific (20 °N–65 °N) between 1980 and 1990. For water younger than 30 years the CFC-derived estimate of accumulation is 1.1 Gt C. In comparison, the estimate from the simulated CFC distribution is 1.3 Gt C. Our model simulation overestimated the accumulation north of 40 °N and underestimated the penetration of anthropogenic CO_2 into the subtropical gyre. From the observed CFC data we estimate the anthropogenic CO_2 uptake by the North Pacific to be 1.1 Gt C/yr for the 1980s.
机译:通过对CFC-11,CFC-12和人为CO_2吸收的模型模拟,我们研究了使用CFC衍生的水龄确定海洋中人为CO_2积累的方法。 CFC年龄方法最适合于30岁以下最可靠的CFC水年龄的水。对于30岁以下的水,CFC-12和CFC-11年龄法可以估计1980-1990年全球人为CO_2的积累分别在10%和22%之内。除了南半球50°S以南和赤道上升区以外,这些CFC得出的人为CO2水柱清单估算值均在模拟值的10%以内。我们的结果表明,CFC年龄方法提供了另一种确定海洋中人为CO_2积累的方法。我们将CFC年龄方法应用于观测到的CFC数据,以估算1980年至1990年之间北太平洋(20°N–65°N)人为CO_2的累积。对于30岁以下的水,CFC得出的累积估计值为1.1 GtC。相比之下,模拟CFC分布的估计值为1.3 GtC。我们的模型模拟高估了40°N以北的累积量,而低估了人为CO_2向亚热带回旋的渗透。根据观测到的CFC数据,我们估计1980年代北太平洋人为吸收的CO_2为1.1 Gt C / yr。

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