Simulation of bulk aerosol direct radiative effects and its climatic feedbacks in South Africa using RegCM4

M. Tesfaye, J. Botai, V. Sivakumar, G. Mengistu Tsidu, C. J.de W. Rautenbach, Shadung J. Moja

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

In this study, 12 year runs of the Regional Climate Model (RegCM4) have been used to analyze the bulk aerosol radiative effects and its climatic feedbacks in South Africa. Due to the geographical locations where the aerosol potential source regions are situated and the regional dynamics, the South African aerosol spatial-distribution has a unique feature. Across the west and southwest areas, desert dust particles are dominant. However, sulfate and carbonaceous aerosols are primarily distributed over the east and northern regions of the country. Analysis of the Radiative Effects (RE) shows that in South Africa the bulk aerosols play a role in reducing the net radiation absorbed by the surface via enhancing the net radiative heating in the atmosphere. Hence, across all seasons, the bulk aerosol-radiation-climate interaction induced statistically significant positive feedback on the net atmospheric heating rate. Over the western and central parts of South Africa, the overall radiative feedbacks of bulk aerosol predominantly induces statistically significant Cloud Cover (CC) enhancements. Whereas, over the east and southeast coastal areas, it induces minimum reductions in CC. The CC enhancement and RE of aerosols jointly induce radiative cooling at the surface which in turn results in the reduction of Surface Temperature (ST: up to -1 K) and Surface Sensible Heat Flux (SSHF: up to -24 W/m2). The ST and SSHF decreases cause a weakening of the convectively driven turbulences and surface buoyancy fluxes which lead to the reduction of the boundary layer height, surface pressure enhancement and dynamical changes. Throughout the year, the maximum values of direct and semi-direct effects of bulk aerosol were found in areas of South Africa which are dominated by desert dust particles. This signals the need for a strategic regional plan on how to reduce the dust production and monitoring of the dust dispersion as well as it initiate the need of further research on different aspects of dust particle in South Africa.

Original languageEnglish
Pages (from-to)1-19
Number of pages19
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume142
DOIs
Publication statusPublished - May 1 2016

Fingerprint

Republic of South Africa
aerosols
aerosol
simulation
dust
cloud cover
deserts
augmentation
atmospheric heating
desert
heating
effect
Africa
positive feedback
climate models
net radiation
surface pressure
radiation
sensible heat flux
buoyancy

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Atmospheric Science
  • Space and Planetary Science

Cite this

Tesfaye, M. ; Botai, J. ; Sivakumar, V. ; Mengistu Tsidu, G. ; Rautenbach, C. J.de W. ; Moja, Shadung J. / Simulation of bulk aerosol direct radiative effects and its climatic feedbacks in South Africa using RegCM4. In: Journal of Atmospheric and Solar-Terrestrial Physics. 2016 ; Vol. 142. pp. 1-19.
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Simulation of bulk aerosol direct radiative effects and its climatic feedbacks in South Africa using RegCM4. / Tesfaye, M.; Botai, J.; Sivakumar, V.; Mengistu Tsidu, G.; Rautenbach, C. J.de W.; Moja, Shadung J.

In: Journal of Atmospheric and Solar-Terrestrial Physics, Vol. 142, 01.05.2016, p. 1-19.

Research output: Contribution to journalArticle

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