Glacially sourced dust as a potentially significant source of ice nucleating particles

冲积平原 冰核 北极的 冰川 矿物粉尘 冰期 地质学 冰芯 大气科学 环境科学 北极冰盖 自然地理学 气候学 海洋学 地貌学 成核 气溶胶 气象学 地理 化学 有机化学
作者
Yutaka Tobo,Kouji Adachi,Paul J. DeMott,Thomas C. J. Hill,Douglas S. Hamilton,N. M. Mahowald,Naoko Nagatsuka,Sho Ohata,Jun Uetake,Y. Kondo,M. Koike
出处
期刊:Nature Geoscience [Nature Portfolio]
卷期号:12 (4): 253-258 被引量:160
标识
DOI:10.1038/s41561-019-0314-x
摘要

Aeolian dusts serve as ice nucleating particles in mixed-phase clouds, and thereby alter the cloud properties and lifetime. Glacial outwash plains are thought to be a major dust source in cold, high latitudes. Due to the recent rapid and widespread retreat of glaciers, high-latitude dust emissions are projected to increase, especially in the Arctic region, which is highly sensitive to climate change. However, the potential contribution of high-latitude dusts to ice nucleation in Arctic low-level clouds is not well acknowledged. Here we show that glacial outwash sediments in Svalbard (a proxy for glacially sourced dusts) have a remarkably high ice nucleating ability under conditions relevant for mixed-phase cloud formation, as compared with typical mineral dusts. The high ice nucleating ability of the sediments is probably governed by the presence of small amounts of organic matter (<1 wt% organic carbon) rather than mineral components. In addition, our results from intensive field measurements and model simulations indicate that the concentrations of atmospheric ice nucleating particles over the Svalbard region are expected to be enhanced in the summertime under the influence of dust emissions from Svalbard and its surroundings. We suggest that high-latitude dust sources have the potential to significantly influence glaciation of Arctic low-level clouds. Dusts from glaciers may contribute significantly to ice nucleation in Arctic low-level clouds, according to analyses of glacial outwash sediments in Svalbard.
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