Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/9417
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dc.contributor.authorChambers, SD-
dc.contributor.authorKikaj, D-
dc.contributor.authorPodstawczyńska, A-
dc.contributor.authorWilliams, AG-
dc.contributor.authorCrawford, J-
dc.contributor.authorGriffiths, AD-
dc.date.accessioned2020-05-13T00:53:21Z-
dc.date.available2020-05-13T00:53:21Z-
dc.date.issued2020-05-01-
dc.identifier.citationChambers, S., Kikaj, D., Podstawczyńska, A., Willaiams, A., Crawford, J., & Griffiths, A. (2020) Characterising diurnal & synoptic timescale changes in urban air quality using Radon-222. Paper presented at the EGU General Assembly 2020 Online, 4-8 May 2020.en_AU
dc.identifier.govdoc9481-
dc.identifier.urihttps://presentations.copernicus.org/EGU2020/EGU2020-1506_presentation.pdfen_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/9417-
dc.identifier.urihttps://doi.org/10.5194/egusphere-egu2020-1506-
dc.description.abstractUrban air quality is strongly influenced by the atmosphere’s ability to disperse primary emissions and opportunities for secondary pollution formation. In mid- to high-latitude regions that experience enduring winter snow cover or soil freezing, regional subsidence and stagnation associated with persistent anti-cyclonic conditions such as the “Siberian High” can lead to “cold pool” or “persistent inversion” events. These events can result in life-threatening pollution episodes that last for weeks. While often associated with complex topography [1,2], persistent inversion events can also influence the air quality of urban centres in flat, inland regions [3]. This presentation will describe a recently-developed radon-based technique for identifying and characterising synoptic-timescale persistent inversion events, which is proving to be a simple and economical alternative to contemporary meteorological approaches that require regular sonde profiles [1]. Furthermore, key assumptions of the radon-based technique to characterise diurnaltimescale changes in the atmospheric mixing state described by Chambers et al. [4] are violated during persistent inversion conditions. Here we demonstrate how atmospheric class-typing, through successive application of radon-based techniques for identifying synoptic- and diurnaltimescale changes in the atmospheric mixing state, improves understanding of atmospheric controls on urban air quality in non-summer months across the full diurnal cycle. This knowledge translates directly to statistically-robust techniques for assessing public exposure to pollution, and for evaluating the efficacy of pollution mitigation measures. Lastly, we show how atmospheric class-typing can be used to enhance the evaluation of chemical transport models. © Author(s) 2020en_AU
dc.language.isoenen_AU
dc.publisherEuropenan Geosciences Unionen_AU
dc.relation.ispartofseriesEGU2020-1506-
dc.subjectDaily variationsen_AU
dc.subjectRadon 222en_AU
dc.subjectUrnan areasen_AU
dc.subjectAir qualityen_AU
dc.subjectAtmospheresen_AU
dc.subjectEmissionen_AU
dc.subjectPollutionen_AU
dc.subjectTemperature inversionsen_AU
dc.titleCharacterising diurnal & synoptic timescale changes in urban air quality using Radon-222en_AU
dc.typeConference Presentationen_AU
dc.date.statistics2020-05-13-
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