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首页> 外文期刊>Ocean Science Discussions >Variability and stability of anthropogenic CO2 in Antarctic Bottom Water observed in the Indian sector of the Southern Ocean, 1978–2018
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Variability and stability of anthropogenic CO2 in Antarctic Bottom Water observed in the Indian sector of the Southern Ocean, 1978–2018

机译:1978 - 2018年印度海洋印度部门观察到南极底水中人为CO2的变异性和稳定性

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Antarctic Bottom Water (AABW) is known as a long-term sink for anthropogenic CO2 (Cant), but the sink is hardly quantified because of the scarcity of observations, specifically at an interannual scale. We present in this paper an original dataset combining 40?years of carbonate system observations in the Indian sector of the Southern Ocean (Enderby Basin) to evaluate and interpret the interannual variability of Cant in the AABW. This investigation is based on regular observations collected at the same location (63°?E–56.5°?S) in the framework of the French observatory OISO from 1998 to 2018 extended by GEOSECS and INDIGO observations (1978, 1985 and 1987). At this location the main sources of AABW sampled is the low-salinity Cape Darnley Bottom Water (CDBW) and the Weddell Sea Deep Water (WSDW). Our calculations reveal that Cant concentrations increased significantly in the AABW, from an average concentration of 7?μmol?kg?1 calculated for the period 1978–1987 to an average concentration of 13?μmol?kg?1 for the period 2010–2018. This is comparable to previous estimates in other Southern Ocean (SO) basins, with the exception of bottom water close to formation sites where Cant concentrations are about twice as large. Our analysis shows that total carbon (CT) and Cant increasing rates in the AABW are about the same over the period 1978–2018, and we conclude that the long-term change in CT is mainly due to the uptake of Cant in the different formation regions. This is, however, modulated by significant interannual to multi-annual variability associated with variations in hydrographic (potential temperature, Θ; salinity, S) and biogeochemical (CT; total alkalinity, AT; dissolved oxygen, O2) properties. A surprising result is the apparent stability of Cant concentrations in recent years despite the increase in CT and the gradual acceleration of atmospheric CO2. The interannual variability at play in AABW needs to be carefully considered in the extrapolated estimation of Cant sequestration based on sparse observations over several years.
机译:南极底水(AABW)被称为人类学二氧化碳(不能)的长期水槽,但由于观察的稀缺,特别是处于际规模,水槽几乎没有量化。我们在本文中展示了一个原始数据集结合了40个?多年的碳酸盐系统观察在南海(内切盆地)的印度部门中的观察,以评估和解释AABW中无法际变化。本调查基于在法国天文台Oiso的同一地点(63°C-56.5°5°S)的定期观察从1998年到2018年由Geosecs和Indigo观察(1978,1985和1987年)延伸。在这个位置,AABW采样的主要来源是低盐度Cape Darnley底水(CDBW)和Weddell Sea Deep Water(WSDW)。我们的计算揭示了AABW中不能显着增加的浓度,从平均浓度为7?μmol?1,在1978-1987期间计算的平均浓度为13Ωμmol?kg?1,在2010-2018期间。这与其他南海(SO)盆地的先前估计相当,除了靠近形成部位的底部水,不能浓度约为大约两倍。我们的分析表明,AABW中总碳(CT)和增加的速率在1978 - 2018年期间大致相同,我们得出结论,CT的长期变化主要是由于不同地层中不能摄取的地区。然而,这是通过与水文(潜在温度,θ;盐度,S)和生物地晶体(CT;总碱度)的变化相关的多年来持续的多年可变性来调节。令人惊讶的结果是近年来CT和大气二氧化碳逐渐加速度的近年来Cr Colt浓度的表观稳定性。基于几年后的稀疏观察,需要在AABW中的续集估计中仔细考虑AABW的续变度。

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