1Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA
*now at: Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, USA
Received: 29 Apr 2011 – Published in Atmos. Chem. Phys. Discuss.: 14 Jul 2011
Abstract. The size distribution of mineral dust aerosols partially determines their interactions with clouds, radiation, ecosystems, and other components of the Earth system. Several theoretical models predict that the dust size distribution depends on the wind speed at emission, with larger wind speeds predicted to produce smaller aerosols. The present study investigates this prediction using a compilation of published measurements of the size-resolved vertical dust flux emitted by eroding soils. Surprisingly, these measurements indicate that the size distribution of naturally emitted dust aerosols is independent of the wind speed. The recently formulated brittle fragmentation theory of dust emission is consistent with this finding, whereas other theoretical models are not. The independence of the emitted dust size distribution with wind speed simplifies both the interpretation of geological records of dust deposition and the parameterization of dust emission in atmospheric circulation models.
Revised: 20 Sep 2011 – Accepted: 28 Sep 2011 – Published: 07 Oct 2011
Kok, J. F.: Does the size distribution of mineral dust aerosols depend on the wind speed at emission?, Atmos. Chem. Phys., 11, 10149-10156, doi:10.5194/acp-11-10149-2011, 2011.