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Dust source activation frequency across East Asia

Dust source activation frequency across East Asia
Dust source activation frequency across East Asia
Plumes of mineral dust in East Asia deleteriously impact the health and livelihoods of hundreds of millions of people in Mongolia, China, Korea, and Japan and perturb Earth’s energy balance and climate. However, the sources of this dust are not well-documented, limiting understanding of dust emissions. Here, we systematically quantify dust source activation frequency (DSAF) across East Asia (80–130°E; 27–52°N) between January 2016 and December 2023. Our data reveal a vast dust-active area extending from the Tibetan Plateau in the southwest to the Huin Bair Sandy Land in the northeast, but two regions dominate: southern sources centred on the margins of the Taklimakan Desert and northern ones centred on the valleys of the Gobi Desert. East Asia is most dust-active in boreal spring (46% of all recorded events). This seasonal peak is pronounced in northern sources where snow cover, vegetation and orographic/topographic influence on winds are clear controls on DSAF. The main southern sources are active year-round with DSAF-hotspots attributable to desiccated lakes and riverbeds. The Tibetan Plateau, commonly considered a sink for in-bound windblown dust, is also a dust source, particularly in winter, with emissions controlled by precipitation patterns, snow cover and wind funnelling through deep river gorges. Contrary to suggestions, our data show that the Loess Plateau is not a major dust source. We document a marked increase in dust source activation during the 2020 extreme heat wave on the overgrazed Mongolian Plateau grasslands. Our data provide a framework to study past variability in the two-way climate interactions that control dust emissions on historical and geological timescales and a baseline from which to measure future change.
East Asia, Himawari-8/9 imagery, dust source activation, land surface, the Tibetan Plateau
1748-9326
Chen, Lingle
6a1fed39-dbb7-4a72-ba7b-fbfdfa9cb6c5
Schepanski, Kerstin
776788dd-66ac-46f2-b5f0-68c23d8c303d
Crocker, Anya
1215fbdd-ad43-408a-bd79-c54c6847e68c
Xuan, Chuang
3f3cad12-b17b-46ae-957a-b362def5b837
Wilson, Paul
f940a9f0-fa5a-4a64-9061-f0794bfbf7c6
Chen, Lingle
6a1fed39-dbb7-4a72-ba7b-fbfdfa9cb6c5
Schepanski, Kerstin
776788dd-66ac-46f2-b5f0-68c23d8c303d
Crocker, Anya
1215fbdd-ad43-408a-bd79-c54c6847e68c
Xuan, Chuang
3f3cad12-b17b-46ae-957a-b362def5b837
Wilson, Paul
f940a9f0-fa5a-4a64-9061-f0794bfbf7c6

Chen, Lingle, Schepanski, Kerstin, Crocker, Anya, Xuan, Chuang and Wilson, Paul (2025) Dust source activation frequency across East Asia. Environmental Research Letters, 20 (7), [074056]. (doi:10.1088/1748-9326/addee6).

Record type: Article

Abstract

Plumes of mineral dust in East Asia deleteriously impact the health and livelihoods of hundreds of millions of people in Mongolia, China, Korea, and Japan and perturb Earth’s energy balance and climate. However, the sources of this dust are not well-documented, limiting understanding of dust emissions. Here, we systematically quantify dust source activation frequency (DSAF) across East Asia (80–130°E; 27–52°N) between January 2016 and December 2023. Our data reveal a vast dust-active area extending from the Tibetan Plateau in the southwest to the Huin Bair Sandy Land in the northeast, but two regions dominate: southern sources centred on the margins of the Taklimakan Desert and northern ones centred on the valleys of the Gobi Desert. East Asia is most dust-active in boreal spring (46% of all recorded events). This seasonal peak is pronounced in northern sources where snow cover, vegetation and orographic/topographic influence on winds are clear controls on DSAF. The main southern sources are active year-round with DSAF-hotspots attributable to desiccated lakes and riverbeds. The Tibetan Plateau, commonly considered a sink for in-bound windblown dust, is also a dust source, particularly in winter, with emissions controlled by precipitation patterns, snow cover and wind funnelling through deep river gorges. Contrary to suggestions, our data show that the Loess Plateau is not a major dust source. We document a marked increase in dust source activation during the 2020 extreme heat wave on the overgrazed Mongolian Plateau grasslands. Our data provide a framework to study past variability in the two-way climate interactions that control dust emissions on historical and geological timescales and a baseline from which to measure future change.

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Accepted/In Press date: 30 May 2025
Published date: 18 June 2025
Keywords: East Asia, Himawari-8/9 imagery, dust source activation, land surface, the Tibetan Plateau

Identifiers

Local EPrints ID: 503105
URI: http://eprints.soton.ac.uk/id/eprint/503105
ISSN: 1748-9326
PURE UUID: 91dd683c-d3c0-4509-aeb4-3d03039a45f1
ORCID for Lingle Chen: ORCID iD orcid.org/0000-0002-3525-9480
ORCID for Anya Crocker: ORCID iD orcid.org/0000-0001-9561-5750
ORCID for Chuang Xuan: ORCID iD orcid.org/0000-0003-4043-3073
ORCID for Paul Wilson: ORCID iD orcid.org/0000-0001-6425-8906

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Date deposited: 21 Jul 2025 17:00
Last modified: 13 Sep 2025 02:27

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Contributors

Author: Lingle Chen ORCID iD
Author: Kerstin Schepanski
Author: Anya Crocker ORCID iD
Author: Chuang Xuan ORCID iD
Author: Paul Wilson ORCID iD

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