气候变化领域集成服务门户(CCPortal): Major ion chemistry of snow cores along a transect in central Dronning Maud Land, Antarctica

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DOI	https://doi.org/10.1594/PANGAEA.854380
	Major ion chemistry of snow cores along a transect in central Dronning Maud Land, Antarctica
	Mahalinganathan; K; Thamban; M
发布日期	2015-11-06
数据集类型	dataset
英文简介	Among the large variety of particulates in the atmosphere, calcic mineral dust particles have highly reactive surfaces that undergo heterogeneous reactions with nitrogen oxides contiguously. The association between Ca2+, an important proxy indicator of mineral dust and NO3-, a dominant anion in the Antarctic snow pack was analysed. A total of 41 snow cores (~ 1 m each) that represent snow deposited during 2008-2009 were studied along coastal-inland transects from two different regions - the Princess Elizabeth Land (PEL) and central Dronning Maud Land (cDML) in East Antarctica. Correlation statistics showed a strong association (at 99 % significance level) between NO3- and Ca2+ at the near-coastal sections of both PEL (r = 0.72) and cDML (r = 0.76) transects. Similarly, a strong association between these ions was also observed in snow deposits at the inland sections of PEL (r = 0.8) and cDML (r = 0.85). Such systematic associations between Ca2+ and NO3- is attributed to the interaction between calcic mineral dust and nitrogen oxides in the atmosphere, leading to the possible formation of calcium nitrate (Ca(NO3)2). Forward and back trajectory analyses using HYSPLIT model v. 4 revealed that Southern South America (SSA) was an important dust emitting source to the study region, aided by the westerlies. Particle size distribution showed that over 90 % of the dust was in the range < 4 µm, indicating that these dust particles reached the Antarctic region via long range transport from the SSA region. We propose that the association between Ca2+ and NO3- occurs during the long range transport due to the formation of Ca(NO3)2. The Ca(NO3)2 thus formed in the atmosphere undergo deposition over Antarctica under the influence of anticyclonic polar easterlies. However, influence of local dust sources from the nunataks in cDML evidently mask such association in the mountainous region. The study indicates that the input of dust-bound NO3– may contribute a significant fraction of the total NO3- deposited in Antarctic snow.
空间范围	Median Latitude: -71.664167 * Median Longitude: 10.927498 * South-bound Latitude: -72.483330 * West-bound Longitude: 10.133330 * North-bound Latitude: -70.850000 * East-bound Longitude: 11.733330
语种	英语
国家	国际
学科大类	气候变化
学科子类	冰冻圈
文献类型	数据集
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/213757
推荐引用方式 GB/T 7714	Mahalinganathan,K,Thamban,et al. Major ion chemistry of snow cores along a transect in central Dronning Maud Land, Antarctica.2015-11-06.https://doi.org/10.1594/PANGAEA.854380.