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Decadal-Scale Increase of Anthropogenic CO2 in Antarctic Bottom Water in the Indian and Western Pacific Sectors of the Southern Ocean

机译:南海印度西太平洋南极地区南极底水的南极底水划分规模增加

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摘要

We determined decadal-scale increases of anthropogenic CO2 in the water column using data sets collected 17 years apart (1994-1996 and 2012-2013) along a transect at nominal 62 degrees S in the Indian and western Pacific sectors of the Southern Ocean. Large increases of anthropogenic CO2 (up to 9.1 +/- 1.5 mu mol/kg), closely following atmospheric CO2 increases, were found in Antarctic Bottom Water (AABW), previously considered a small sink of anthropogenic CO2. Vertical distributions of anthropogenic CO2 increases showed significant positive correlations with those of changes in CFC-12 and SF6, implying that the distributions were mainly controlled by physical processes such as ventilation and circulation. Calculated uptake rates of anthropogenic CO2 by AABW were between 0.29 and 0.39 mol.m(-2).yr(-1) in five longitudinal segments of the transect. In accounting for the large increase of anthropogenic CO2 in AABW, sea surface conditions in the formation region of AABW are important.
机译:我们使用17年(1994-1996和2012-2013)在印度和西部太平洋南海的西太平洋部门的标称62摄氏度的横断面收集的数据集确定了水柱中人为CO2的二等程度增加。 在南极底水(AABW)中发现大气压底部水(AABW)中发现大规模的人为CO 2(高达9.1 +/-1.5μmmol/ kg)的大增加,以前被认为是人为二氧化碳的一个小水槽。 人为CO2的垂直分布增加与CFC-12和SF6的变化显着呈显着阳性相关性,这意味着分布主要由通风和循环等物理过程控制。 通过AABW计算的人为CO 2的摄取率在0.29和0.39mol.m(-2)。晶体中的五个纵向区段之间。 在AABW中的人为CO2的大量增加,AABW的形成区域中的海面状况很重要。

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  • 来源
    《Geophysical Research Letters》 |2019年第2期|共9页
  • 作者单位

    Japan Agcy Marine Earth Sci &

    Technol Res &

    Dev Ctr Global Change Yokosuka Kanagawa Japan;

    Japan Agcy Marine Earth Sci &

    Technol Res &

    Dev Ctr Global Change Yokosuka Kanagawa Japan;

    Japan Agcy Marine Earth Sci &

    Technol Res &

    Dev Ctr Global Change Yokosuka Kanagawa Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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