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

Tobo, Yutaka; Adachi, Kouji; DeMott, Paul J.; Hill, Thomas C.  J.; Hamilton, Douglas S.; Mahowald, Natalie M.; Nagatsuka, Naoko; Ohata, Sho; Uetake, Jun; Kondo, Yutaka; Koike, Makoto

doi:10.1038/s41561-019-0314-x

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

Journal Article · Mon Mar 25 00:00:00 EDT 2019 · Nature Geoscience

DOI:https://doi.org/10.1038/s41561-019-0314-x· OSTI ID:1594096

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National Inst. of Polar Research, Tachikawa, Tokyo (Japan); Graduate Univ. for Advanced Studies, Tachikawa, Tokyo (Japan)
Meteorological Research Inst., Tsukuba, Ibaraki (Japan)
Colorado State Univ., Fort Collins, CO (United States)
Cornell Univ., Ithaca, NY (United States)
National Inst. of Polar Research, Tachikawa, Tokyo (Japan)
Univ. of Tokyo (Japan); Nagoya Univ. (Japan)
National Inst. of Polar Research, Tachikawa, Tokyo (Japan); Colorado State Univ., Fort Collins, CO (United States)
Univ. of Tokyo (Japan)

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. In conclusion, we suggest that high-latitude dust sources have the potential to significantly influence glaciation of Arctic low-level clouds.

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Research Organization:: Cornell Univ., Ithaca, NY (United States)

Sponsoring Organization:: Office of Science (SC), Biological and Environmental Research (BER). Earth and Environmental Systems Science Division; Japan Society for the Promotion of Science (KAKENHI); National Science Foundation (NSF); USDOE Office of Science (SC), Advanced Scientific Computing Research (ASCR). Scientific Discovery through Advanced Computing (SciDAC)

Grant/Contract Number:: SC0006791; 15K13570; 15K16120; 16H06020; 16J08380; 16K16188; 18H04143; AGS-1358495

OSTI ID:: 1594096

Journal Information:: Nature Geoscience, Vol. 12, Issue 4; ISSN 1752-0894

Publisher:: Nature Publishing GroupCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 68 works

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