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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 8 | Copyright
Atmos. Chem. Phys., 17, 5131-5154, 2017
https://doi.org/10.5194/acp-17-5131-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Apr 2017

Research article | 20 Apr 2017

The Climatology of Australian Aerosol

Ross M. Mitchell1, Bruce W. Forgan2, and Susan K. Campbell1 Ross M. Mitchell et al.
  • 1CSIRO Oceans and Atmosphere, Yarralumla, GPO Box 1700, Canberra, ACT, Australia
  • 2Australian Bureau of Meteorology, P.O. Box 1289K, Melbourne, Australia

Abstract. Airborne particles or aerosols have long been recognised for their major contribution to uncertainty in climate change. In addition, aerosol amounts must be known for accurate atmospheric correction of remotely sensed images, and are required to accurately gauge the available solar resource. However, despite great advances in surface networks and satellite retrievals over recent years, long-term continental-scale aerosol data sets are lacking. Here we present an aerosol assessment over Australia based on combined sun photometer measurements from the Bureau of Meteorology Radiation Network and CSIRO/AeroSpan. The measurements are continental in coverage, comprising 22 stations, and generally decadal in timescale, totalling 207 station-years. Monthly climatologies are given at all stations. Spectral decomposition shows that the time series can be represented as a weighted sum of sinusoids with periods of 12, 6 and 4 months, corresponding to the annual cycle and its second and third harmonics. Their relative amplitudes and phase relationships lead to sawtooth-like waveforms sharply rising to an austral spring peak, with a slower decline often including a secondary peak during the summer. The amplitude and phase of these periodic components show significant regional change across the continent. Fits based on this harmonic analysis are used to separate the periodic and episodic components of the aerosol time series. An exploratory classification of the aerosol types is undertaken based on (a) the relative periodic amplitudes of the Ångström exponent and aerosol optical depth, (b) the relative amplitudes of the 6- and 4-month harmonic components of the aerosol optical depth, and (c) the ratio of episodic to periodic variation in aerosol optical depth. It is shown that Australian aerosol can be broadly grouped into three classes: tropical, arid and temperate. Statistically significant decadal trends are found at 4 of the 22 stations. Despite the apparently small associated declining trends in mid-visible aerosol optical depth of between 0.001 and 0.002 per year, these trends are much larger than those projected to occur due to declining emissions of anthropogenic aerosols from the Northern Hemisphere. There is remarkable long-range coherence in the aerosol cycle across the continent, suggesting broadly similar source characteristics, including a possible role for intercontinental transport of biomass burning aerosol.

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We present a climatological analysis of Australian aerosol based on 22 sun photometer stations operated by the Australian Bureau of Meteorology and CSIRO/AeroSpan. A spectral analysis shows the dominance of the annual cycle and its second and third harmonics in the time series. Classification shows three primary Australian aerosol regimes: temperate, arid, and tropical. Further analysis quantifies trends and reveals remarkable long-range coherence in the aerosol cycle across the continent.
We present a climatological analysis of Australian aerosol based on 22 sun photometer stations...
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