New inventory of dust emission sources in Central Asia and Northwestern China derived from MODIS imagery using dust enhancement technique

Nobakht, M., Shahgedanova, M. ORCID: https://orcid.org/0000-0002-2320-3885 and White, K. (2021) New inventory of dust emission sources in Central Asia and Northwestern China derived from MODIS imagery using dust enhancement technique. Journal of Geophysical Research: Atmospheres, 126 (4). e2020JD033382. ISSN 2169-8996 doi: 10.1029/2020JD033382

Abstract/Summary

The first inventory of dust emission sources in Central Asia and northwestern China (35–50°N, 50–100°E) derived from the twice daily MODIS imagery from 2003 to 2012 is presented. A high‐resolution (1 km) dust enhancement product was generated to produce maps of dust point sources (DPS), indicating geographical locations of the observed dust emissions, and gridded data sets of dust emission frequencies. About 13,500 DPS were detected over an area of ∼5 × 106 km2, however, their distribution was uneven. The highest frequency of DPS occurred in the northern and eastern Taklimakan, in the Aralkum, and in the regions, which were not widely reported in literature before, the Balkh delta in northern Afghanistan and the pre‐Aral, from the northern Caspian coast to the Betpak‐Dala desert in Kazakhstan. South of the Aral, DPS were mainly associated with fluvial features: drying lakes, dry river beds, alluvial deposits and agricultural activity which is closely linked to water availability in this arid region. In the pre‐Aral and Balkhash‐Junggar regions, land damaged by wildfire was the main source of dust. In China and eastern Kazakhstan dust emissions peaked in spring; in Central Asia and western Kazakhstan—in summer. The Aralkum was active throughout the year with a positive trend in emission frequency over the study period. Locations of DPS did not always correlate with high atmospheric optical depth (AOD) particularly west of the Aral and in the southern Taklimakan where few DPS were detected despite the high AOD values. This was attributed to dust transport from the upwind sources.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/96133
Identification Number/DOI	10.1029/2020JD033382
Refereed	Yes
Divisions	Science > School of Archaeology, Geography and Environmental Science > Department of Geography and Environmental Science
Publisher	American Geophysical Union
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