Abstract:
Atmospheric aerosols are small solid and liquid particles suspended in the Earth's atmosphere which originate from
anthropogenic and natural activities. Unlike greenhouse gases, aerosol particles are relatively short-lived in the
atmosphere and exhibit multidimensional heterogeneity with respect to their composition, size, sources, mixing state
and the spatio-temporal distributions. The concentration and climatic influences of atmospheric aerosols are much
higher closer to their source regions. Therefore, to have a better understanding of the role of aerosols, their
distribution and climatic impacts must be understood and quantified on a regional scale rather than on a
global‐average basis. There are multiple sources of aerosols/precursor gases in South Africa (SA) which build a
complex mixture of atmospheric particulates. This contribution presents a detailed study of aerosol climatology over
SA as well as examines the direct radiative and semi-direct climatic effects of individual/total aerosol particles based
on their sources. The climatological study has shown that, in terms of aerosol load spatial variation, SA can be
classified into three parts: the upper, central, and lower part; which corresponds to high, medium and low aerosol
loads. The seasonal variation of aerosol optical signatures shows that the prevailing sources of aerosols are different
in each part of SA. The lower part is dominated by particles that are induced from the air mass transport from the
surrounding marine environment and other SA/neighbouring regions. The central and upper parts of SA are primarily
loaded by windblown mineral dust particles and aerosols that result from anthropogenic/biomass burning activities.
Following the aerosol climatological study, using the 12 year (1997 - 2008) runs of the Regional Climate Model
(RegCM4), the mass distribution, radiative influences and semi-direct climatic effects of wind-eroded desert dust
particles, different species of aerosols that are induced from anthropogenic and biomass burning activities over SA
are examined. Investigating the influence of aerosols, based on their sources, is essential to improve the scientific
understanding about the two-way interaction and feedback among various species of aerosols, radiation and different
climatic variables. This is also important to distinguish the climatic signals of anthropogenic aerosols from that of
natural aerosols as well as to devise climate change mitigation strategies. Before employing RegCM4 for these
purposes, the model’s performance in reproducing the major observational features of aerosol optical fields over SA
was evaluated. Among various semi-direct climatic influences of aerosols, this study examined their effects on:
surface temperature, surface sensible heat flux, net atmospheric radiative heating rate, hydrological variables (in
terms of cloud cover and cloud liquid water path), boundary layer, surface pressure and surface wind fields. The
study also assessed the dependency of aerosols’ semi-direct effects on seasonal variation of meteorological
parameters as well as its reliance on atmospheric aerosol distributions and properties. Overall, the semi-direct effect
assessments delivered not only an important contribution towards the understanding of the interaction and feedback
between different types of aerosols-radiation-climate (at a regional level), but also offered insightful information
about the mutual interrelationships among different climatic feedbacks. Among different aerosol species in SA, this
study critically underscores that the wind-eroded desert dust particles have a dominant climatic signal in SA.
Therefore, wind-eroded desert dust particles are of high importance and need to be incorporated in climate change
studies over South Africa. Additionally, the dominance of dust particle climatic signals perhaps requires some
attention from governmental or non-governmental environmental organizations which are working in and around
South Africa: at least in terms of making some strategic plans on how to reduce the dust production and dispersion.