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Measurements of atmospheric Δ14CO2 along the R/V Xuelong cruise track from Zhongshan Station (Antarctica) to Shanghai
Tellus Series B: Chemical and Physical Meteorology ( IF 2.3 ) Pub Date : 2020-08-20 , DOI: 10.1080/16000889.2020.1807245
Xiangdong Zheng 1 , Ping Ding 2 , Zhengbin Han 3 , Chende Shen 2 , Kexin Liu 4 , Jie Tang 1 , Linggen Bian 1
Affiliation  

Abstract

During January–March 2011, 29 atmospheric Δ14CO2 samples were measured along the R/V Xuelong cruise track from Zhongshan Station (69.37°S, 76.38°E; Antarctica) to Shanghai. The extent of fossil fuel contamination in the samples was evaluated by comparison with contemporary hemispheric-scale averages of Δ14CO2, together with transport analysis and consideration of the δ13CO2 levels in the samples. Generally, the Δ14CO2 levels along the route south to 40.67°S were lower than the hemispheric-scale average. Circumpolar deep water (CDW) upwelling, stratosphere–troposphere transport (STT), and regional transport associated with the Fukushima nuclear power plant (NPP) accident in Japan on 12 March 2011 were found to have influenced Δ14CO2 levels at the sampling sites. In comparison with the atmospheric Δ14CO2 level (45.7 ± 3.5‰ (1σ)) measured in the coastal region of East Antarctica, CDW upwelling caused reduction of ∼10‰ in Δ14CO2 in two cross sections: 62.0°–64.0°S along 74.0°E and 51.7°–54.0°S along 80.5°–84.0°E. Conversely, STT-enhanced Δ14CO2 was ∼7‰ (∼3‰) at Zhongshan (around 45.0°S). The linkage was supported by a certain Model-3/CMAQ simulation that indicated dispersion of radionuclides from the Fukushima NPP accident over the East Asian region, which explained the individual high Δ14CO2 (52‰) level on 29 March 2011 in Shanghai.



中文翻译:

从中山站(南极洲)到上海,沿雪龙R / V巡航轨道测量大气Δ14CO2

摘要

2011年1月- 3月29大气压Δ期间14个CO 2被沿R / V测量样品雪龙至上海;中山站(南极洲69.37°S,76.38。E)巡航轨迹。样品中的化石燃料污染的程度通过用Δ的当代半球尺度的平均值比较来评价14 CO 2,与δ的运输分析和考虑一起13 CO 2水平的样品英寸 通常,Δ 14 CO 2沿南至40.67°S的路线的水平低于半球平均水平。北极圈的深层水(CDW)上涌,平流层-对流层传输(STT),以及区域交通与福岛核电站(NPP)事故发生在日本2011年12月相关的发现影响了Δ 14 CO 2的采样点水平。在与大气Δ比较14 CO 2(45.7±3.5‰(1σ))在东南极洲,CDW的沿海区域中测量上升流在Δ减少引起的〜10‰水平14 CO 2在两个横截面:62.0°-64.0沿74.0°E的°S和沿80.5°-88.4°E的51.7°-54.0°S。相反地,STT-增强Δ 14 CO 2在中山(大约45.0°S),约为7‰(〜3‰)。联动装置是由某些型号-3 / CMAQ仿真支持从福岛NPP事故在东亚区域,其解释了单独的高Δ放射性核素的指示的分散体14 CO 2在上海(52‰)的水平上29 2011年3月。

更新日期:2020-08-20
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