46 research outputs found
Radon: a universal baseline indicator at sites with contrasting physical settings
The primary goal of World Meteorological Organisation Global Atmosphere Watch (WMOâGAW) baseline stations is systematic global monitoring of chemical composition of the atmosphere, requiring a reliable, consistent and unambiguous approach for the identification of baseline air. Premier stations in the GAW baseline network span a
broad range of physical settings, from remote marine to highâaltitude continental sites, necessitating carefully tailored
siteâspecific requirements for baseline sampling, data selection, and analysis. Radonâ222 is a versatile and unambiguous terrestrial tracer, widelyâused in transport and mixing studies. Since the majority of anthropogenic pollution sources also have terrestrial origins, radon has become a popular addition to the âbaseline selection
toolkitâ at numerous GAW stations as a proxy for âpollution potentialâ. In the past, detector performance and postprocessing
methods necessitated the adoption of a relaxed (e.g. 100 mBq mâ3) radon threshold for minimal terrestrial influence, intended to be used in conjunction with other baseline criteria and analysis procedures, including wind speed, wind direction, particle number, outlier rejection and filtering. However, recent improvements in detector sensitivity, stability and postâprocessing procedures have reduced detection limits below 10 mBq mâ3 at Cape Grim and to ïŸ25 mBq mâ3 at other baseline stations. Consequently, for suitably sensitive instruments (such as the ANSTO designed and built twoâfilter dualâflowâloop detectors), radon concentrations alone can be used to unambiguously identify air masses that have been removed from terrestrial sources (at altitude or over ice), or in equilibrium
with the ocean surface, for periods of >2â3 weeks (radon †40 mBq mâ3). Potentially, radon observations alone can thus provide a consistent and universal (site independent) means for baseline identification. Furthermore, for continental sites with complex topography and meteorology, where true âbaselineâ conditions may never
occur, radon can be used to indicate the least terrestriallyâperturbed air masses, and provide a means by which to apply limits to the level of âacceptable terrestrial influenceâ for a given application. We demonstrate the efficacy of the radonâbased selection at a range of sites in contrasting physical settings, including: Cape Grim (Tasmania), Cape Point (South Africa), Mauna Loa (Hawaii), Jungfraujoch (Switzerland) and Schneefernerhaus (Germany).Bureau of Meteorology and CSIRO Oceans and Atmosphere,Climate Science Centre
Chlamydial infections in feral pigeons in Europe: Review of data and focus on public health implications
Modelling human choices: MADeM and decisionâmaking
Research supported by FAPESP 2015/50122-0 and DFG-GRTK 1740/2. RP and AR are also part of the Research, Innovation and Dissemination Center for Neuromathematics FAPESP grant (2013/07699-0). RP is supported by a FAPESP scholarship (2013/25667-8). ACR is partially supported by a CNPq fellowship (grant 306251/2014-0)