Articles | Volume 18, issue 12
Atmos. Chem. Phys., 18, 9025–9048, 2018
https://doi.org/10.5194/acp-18-9025-2018
Atmos. Chem. Phys., 18, 9025–9048, 2018
https://doi.org/10.5194/acp-18-9025-2018

Research article 28 Jun 2018

Research article | 28 Jun 2018

Can explicit convection improve modelled dust in summertime West Africa?

Alexander J. Roberts et al.

Viewed

Total article views: 1,811 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,102 668 41 1,811 34 36
  • HTML: 1,102
  • PDF: 668
  • XML: 41
  • Total: 1,811
  • BibTeX: 34
  • EndNote: 36
Views and downloads (calculated since 04 Jan 2018)
Cumulative views and downloads (calculated since 04 Jan 2018)

Viewed (geographical distribution)

Total article views: 1,823 (including HTML, PDF, and XML) Thereof 1,811 with geography defined and 12 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Feb 2021
Download
Short summary
The summer Saharan dust hotspot is seasonally tied to the occurrence of convective storms. Global weather and climate models parameterise convection and so are unable to represent their associated dust uplift (haboobs). However, this work shows that even when simulations represent convection explicitly: (1) dust fields are not strongly affected, (2) convective storms are too small, (3) haboobs are too weak and (4) the land surface (bare soil and soil moisture) is dominant in controlling dust.
Altmetrics
Final-revised paper
Preprint