Articles | Volume 19, issue 15
https://doi.org/10.5194/acp-19-10279-2019
https://doi.org/10.5194/acp-19-10279-2019
Research article
 | 
14 Aug 2019
Research article |  | 14 Aug 2019

The influence of simulated surface dust lofting and atmospheric loading on radiative forcing

Stephen M. Saleeby, Susan C. van den Heever, Jennie Bukowski, Annette L. Walker, Jeremy E. Solbrig, Samuel A. Atwood, Qijing Bian, Sonia M. Kreidenweis, Yi Wang, Jun Wang, and Steven D. Miller

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Cited articles

Alfaro, S. C. and Gomes, L.: Modeling mineral aerosol production by wind erosion: Emission intensities and aerosol size distributions in source areas, J. Geophys. Res., 106, 18075–18084, https://doi.org/10.1029/2000JD900399, 2001. 
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Barnard, J., Fast, J., Paredes-Miranda, G., Arnott, W., and Laskin, A.: Technical Note: Evaluation of the WRF-Chem “Aerosol Chemical to Aerosol Optical Properties” Module using data from the MILAGRO campaign, Atmos. Chem. Phys., 10, 7325–7340, https://doi.org/10.5194/acp-10-7325-2010, 2010. 
Bohren, C. F. and Huffman, D. R.: Absorption and Scattering of Light by Small Particles, Chapter: Absorption and Scattering by a Sphere, John Wiley and Sons Ltd., 82–129, https://doi.org/10.1002/9783527618156.ch4, 1983. 
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This study seeks to understand how intense dust storms impact the heating and cooling of the land surface and atmosphere. Dust storms that are intense enough to substantially impact visibility can also alter how much sunlight reaches the surface during the day and how much heat is trapped in the atmosphere at night. These radiation changes can impact the temperature of the atmosphere and impact the weather in the vicinity.
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