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DOI | 10.1038/s41561-019-0314-x |
Glacially sourced dust as a potentially significant source of ice nucleating particles | |
Tobo, Yutaka1,2; Adachi, Kouji3; DeMott, Paul J.4; Hill, Thomas C. J.4; Hamilton, Douglas S.5; Mahowald, Natalie M.5; Nagatsuka, Naoko1; Ohata, Sho6,7,8; Uetake, Jun1,4; Kondo, Yutaka1; Koike, Makoto6 | |
2019-04-01 | |
发表期刊 | NATURE GEOSCIENCE |
ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2019 |
卷号 | 12期号:4页码:253-+ |
文章类型 | Article |
语种 | 英语 |
国家 | Japan; USA |
英文摘要 | 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. |
领域 | 地球科学 ; 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000462621700009 |
WOS关键词 | HIGH-LATITUDE DUST ; AEROSOL-PARTICLES ; CHEMICAL-PROPERTIES ; ZEPPELIN STATION ; ORGANIC-MATTER ; MARINE AIR ; NUCLEI ; SVALBARD ; CARBON ; GLACIERS |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/182195 |
专题 | 地球科学 气候变化 |
作者单位 | 1.Natl Inst Polar Res, Tachikawa, Tokyo, Japan; 2.SOKENDAI Grad Univ Adv Studies, Sch Multidisciplinary Sci, Dept Polar Sci, Tachikawa, Tokyo, Japan; 3.Meteorol Res Inst, Atmospher Environm & Appl Meteorol Res Dept, Tsukuba, Ibaraki, Japan; 4.Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA; 5.Cornell Univ, Dept Earth & Atmospher Sci, Ithaca, NY USA; 6.Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Tokyo, Japan; 7.Nagoya Univ, Inst Space Earth Environm Res, Nagoya, Aichi, Japan; 8.Nagoya Univ, Inst Adv Res, Nagoya, Aichi, Japan |
推荐引用方式 GB/T 7714 | Tobo, Yutaka,Adachi, Kouji,DeMott, Paul J.,et al. Glacially sourced dust as a potentially significant source of ice nucleating particles[J]. NATURE GEOSCIENCE,2019,12(4):253-+. |
APA | Tobo, Yutaka.,Adachi, Kouji.,DeMott, Paul J..,Hill, Thomas C. J..,Hamilton, Douglas S..,...&Koike, Makoto.(2019).Glacially sourced dust as a potentially significant source of ice nucleating particles.NATURE GEOSCIENCE,12(4),253-+. |
MLA | Tobo, Yutaka,et al."Glacially sourced dust as a potentially significant source of ice nucleating particles".NATURE GEOSCIENCE 12.4(2019):253-+. |
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