格陵兰岛的北极气溶胶

N.Z. Heidam, P. Wåhlin, K. Kemp
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引用次数: 22

摘要

目前正在格陵兰冰盖和格陵兰东北部研究北极气溶胶的元素组成,以确定气溶胶的水平、组成、季节变化和来源,而在偏远和高海拔的中部地区,人们对这些气溶胶知之甚少。特别是,北极雾霾气溶胶的渗透程度是令人感兴趣的,因为这可能引起气候参数的扰动。此前在格陵兰岛北部的四个沿海地区发现了北极雾霾气溶胶。因子分析对气溶胶的受体模拟揭示了三到五个来自自然和人为来源的遥远来源的成分。在北格陵兰岛,人为成分表现出较大的年周期,在冬季由中纬度地区的远距离大气输送引起的显著最大值。这些测量已经恢复,作为冰盖实验的参考。在冰冠上,与1989-1993年格陵兰冰芯方案同时在海拔3200米的Summit连续收集两个大小范围的气溶胶样品。采样设备的设计是每周收集样品,特别适合于PIXE分析,每年检索一次,在极冷条件下自动操作,能耗极低。本文讨论了首次覆盖中部冰盖冬季的样品的初步结果与海平面上北极雾霾的关系。
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Arctic aerosols in Greenland

Elemental composition of Arctic aerosols is being studied on the Greenland Icecap and in northeast Greenland to determine the level, composition, seasonal variation and origin of the aerosols, of which little is known in the remote and elevated central region. In particular, the degree of penetration of arctic haze aerosols is of interest since this may cause perturbations of climatic parameters.

Arctic haze aerosols have previously been found at four coastal sites notably in north Greenland. Receptor modelling of the aerosol by factor analysis revealed three to fivecomponents of remote origin from both natural and anthropogenic sources. In north Greenland the anthropogenic components exhibited large annual cycles with pronounced maxima in winter caused by long-range atmospheric transport from midlatitude areas. These measurements have been resumed as a reference to the Icecap Experiment.

On the Icecap, aerosol samples are being collected in two size ranges on a continuous basis concurrent with the Greenland Icecore Programme 1989–1993 at Summit, 3200 m a.s.l. The sampling equipment is designed for collection of weekly samples especially suited for PIXE analysis, retrieval once a year, automatic operation under extremely cold conditions and very low energy consumption. Preliminary results from samples covering for the first time also the winter season on the central Icecap are discussed in relation to arctic haze occurrences at sea level.

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Introduction Calendar Errata Arctic aerosols in Greenland Size distributions of atmospheric trace elements at dye 3, Greenland—II. Sources and transport
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