15 citations as recorded by crossref.

1. Snow Albedo Reduction in the Colombian Andes Mountains Due to 2000 to 2020 Saharan Dust Intrusions Events T. Bolaño-Ortiz et al. 10.3390/w15173150
2. Saharan, Aral-Caspian and Middle East dust travels to Finland (1980–2022) G. Varga et al. 10.1016/j.envint.2023.108243
3. How a mesoscale cyclonic vortex over Sahara leads to a dust outbreak in South-western Iberia F. Couto et al. 10.1016/j.atmosres.2020.105302
4. Atmospheric extremes caused high oceanward sea surface slope triggering the biggest calving event in more than 50 years at the Amery Ice Shelf D. Francis et al. 10.5194/tc-15-2147-2021
5. Climate Change and Weather Extremes in the Eastern Mediterranean and Middle East G. Zittis et al. 10.1029/2021RG000762
6. Transport of Mineral Dust Into the Arctic in Two Reanalysis Datasets of Atmospheric Composition S. Böö et al. 10.16993/tellusb.1866
7. Impact of Saharan dust outbreaks on short‐range weather forecast errors in Europe K. Hermes et al. 10.1002/qj.4666
8. The Atmospheric Drivers of the Major Saharan Dust Storm in June 2020 D. Francis et al. 10.1029/2020GL090102
9. Ground-based remote sensing of aerosol properties using high-resolution infrared emission and lidar observations in the High Arctic D. Ji et al. 10.5194/amt-16-1865-2023
10. Aeolian dust dynamics in the Fergana Valley, Central Asia, since ~30 ka inferred from loess deposits Y. Li et al. 10.1016/j.gsf.2021.101180
11. Atmospheric rivers drive exceptional Saharan dust transport towards Europe D. Francis et al. 10.1016/j.atmosres.2021.105959
12. Saharan dust and giant quartz particle transport towards Iceland G. Varga et al. 10.1038/s41598-021-91481-z
13. Sensitivity of Summertime Convection to Aerosol Loading and Properties in the United Arab Emirates R. Fonseca et al. 10.3390/atmos12121687
14. Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years N. Rimbu et al. 10.1029/2022GL101500
15. Millennial-scale variability of Greenland dust provenance during the last glacial maximum as determined by single particle analysis S. Ro et al. 10.1038/s41598-024-52546-x