2011
DOI: 10.1016/j.jastp.2011.06.016
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Seasonal variation of aerosol size distributions in Darwin, Australia

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Cited by 12 publications
(11 citation statements)
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“…This reflects a dependence on proximity to the coast and the associated maritime influence on the aerosol loading, as discussed by Bouya et al . [], Bouya and Box [], and Radhi et al . [].…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…This reflects a dependence on proximity to the coast and the associated maritime influence on the aerosol loading, as discussed by Bouya et al . [], Bouya and Box [], and Radhi et al . [].…”
Section: Resultsmentioning
confidence: 99%
“…More recently, Bouya et al . [] and Bouya and Box [] analyzed data from Bureau and TWP/ARM photometers to delineate the seasonal characteristics of the aerosol at Darwin, while Radhi et al . [] applied a similar technique to the data from the CSIRO stations at Lake Argyle and Jabiru.…”
Section: Introductionmentioning
confidence: 99%
“…Large values of a are generally indicative of smaller particles, and vice versa. A quadratic version of Eqn (3) may sometimes be used to extract additional information (Bouya and Box 2011).…”
Section: Study Area and Data Sourcesmentioning
confidence: 99%
“…In this study we investigate the daily and monthly variation of aerosol optical thickness, Ångström exponent and size distribution at two sites in northern Australia (Lake Argyle and Jabiru). Previous studies of this aerosol include Bouya et al (2010) and Bouya and Box (2011), who studied these optical properties in Darwin, for both morning and afternoon (in order to note any sea breeze effects), and Radhi et al (2006) who examined similar data for Tennant Creek (on the southern edge of the burning zone, ~750 km south of Jabiru).…”
Section: Introductionmentioning
confidence: 99%
“…The aerosol accumulation mode number concentration (N a ) and cloud condensation nuclei (CCN) number concentration (N CCN ) at 0.1% supersaturation (S = 0.1%) simulated by CAM5 (Table 1) show a maximum in JJA and a minimum in DJF at both SGP and TWP. Observational studies have also shown that more accumulation mode aerosol and CCN (S = 0.1%) are observed in JJA than other seasons due to stronger photochemical production of aerosols at SGP [ Liu et al , 2011], and due to more frequent continental winds rather than marine winds at TWP [ Bouya and Box , 2011]. Therefore, CAM5 simulates the aerosol properties reasonably well at SGP and TWP.…”
Section: Evaluation Of Simulated Aerosol and Cloud Propertiesmentioning
confidence: 99%