School of Geography, Earth and Atmospheric Sciences - Research Publications

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    Measurement report: Understanding the seasonal cycle of Southern Ocean aerosols
    Humphries, RS ; Keywood, MD ; Ward, JP ; Harnwell, J ; Alexander, SP ; Klekociuk, AR ; Hara, K ; McRobert, IM ; Protat, A ; Alroe, J ; Cravigan, LT ; Miljevic, B ; Ristovski, ZD ; Schofield, R ; Wilson, SR ; Flynn, CJ ; Kulkarni, GR ; Mace, GG ; McFarquhar, GM ; Chambers, SD ; Williams, AG ; Griffiths, AD (COPERNICUS GESELLSCHAFT MBH, 2023-03-29)
    Abstract. The remoteness and extreme conditions of the Southern Ocean and Antarctic region have meant that observations in this region are rare, and typically restricted to summertime during research or resupply voyages. Observations of aerosols outside of the summer season are typically limited to long-term stations, such as Kennaook / Cape Grim (KCG; 40.7∘ S, 144.7∘ E), which is situated in the northern latitudes of the Southern Ocean, and Antarctic research stations, such as the Japanese operated Syowa (SYO; 69.0∘ S, 39.6∘ E). Measurements in the midlatitudes of the Southern Ocean are important, particularly in light of recent observations that highlighted the latitudinal gradient that exists across the region in summertime. Here we present 2 years (March 2016–March 2018) of observations from Macquarie Island (MQI; 54.5∘ S, 159.0∘ E) of aerosol (condensation nuclei larger than 10 nm, CN10) and cloud condensation nuclei (CCN at various supersaturations) concentrations. This important multi-year data set is characterised, and its features are compared with the long-term data sets from KCG and SYO together with those from recent, regionally relevant voyages. CN10 concentrations were the highest at KCG by a factor of ∼50 % across all non-winter seasons compared to the other two stations, which were similar (summer medians of 530, 426 and 468 cm−3 at KCG, MQI and SYO, respectively). In wintertime, seasonal minima at KCG and MQI were similar (142 and 152 cm−3, respectively), with SYO being distinctly lower (87 cm−3), likely the result of the reduction in sea spray aerosol generation due to the sea ice ocean cover around the site. CN10 seasonal maxima were observed at the stations at different times of year, with KCG and MQI exhibiting January maxima and SYO having a distinct February high. Comparison of CCN0.5 data between KCG and MQI showed similar overall trends with summertime maxima and wintertime minima; however, KCG exhibited slightly (∼10 %) higher concentrations in summer (medians of 158 and 145 cm−3, respectively), whereas KCG showed ∼40 % lower concentrations than MQI in winter (medians of 57 and 92 cm−3, respectively). Spatial and temporal trends in the data were analysed further by contrasting data to coincident observations that occurred aboard several voyages of the RSV Aurora Australis and the RV Investigator. Results from this study are important for validating and improving our models and highlight the heterogeneity of this pristine region and the need for further long-term observations that capture the seasonal cycles.
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    Quantifying the reduction of airborne infectious viral load using a ventilated patient hood
    Lee, LYY ; Landry, SA ; Jamriska, M ; Subedi, D ; Joosten, SA ; Barr, JJ ; Brown, R ; Kevin, K ; Schofield, R ; Monty, J ; Subbarao, K ; McGain, F (W B SAUNDERS CO LTD, 2023-06)
    BACKGROUND: Healthcare workers treating SARS-CoV-2 patients are at risk of infection by respiratory exposure to patient-emitted, virus-laden aerosols. Source control devices such as ventilated patient isolation hoods have been shown to limit the dissemination of non-infectious airborne particles in laboratory tests, but data on their performance in mitigating the airborne transmission risk of infectious viruses are lacking. AIM: We used an infectious airborne virus to quantify the ability of a ventilated hood to reduce infectious virus exposure in indoor environments. METHODS: We nebulized 109 plaque forming units (pfu) of bacteriophage PhiX174 virus into a ∼30-m3 room when the hood was active or inactive. The airborne concentration of infectious virus was measured by BioSpot-VIVAS and settle plates using plaque assay quantification on the bacterial host Escherichia coli C. The airborne particle number concentration (PNC) was also monitored continuously using an optical particle sizer. FINDINGS: The median airborne viral concentration in the room reached 1.41 × 105 pfu/m3 with the hood inactive. When active, the hood reduced infectious virus concentration in air samples by 374-fold. The deposition of infectious virus on the surface of settle plates was reduced by 87-fold. This was associated with a 109-fold reduction in total airborne particle number escape rate. CONCLUSION: A personal ventilation hood significantly reduced airborne particle escape, considerably lowering infectious virus contamination in an indoor environment. Our findings support the further development of source control devices to mitigate nosocomial infection risk among healthcare workers exposed to airborne viruses in clinical settings.
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    We studied how to reduce airborne COVID spread in hospitals. Here’s what we learnt
    Buising, K ; Marshall, C ; McGain, F ; Monty, J ; Irving, L ; Kainer, M ; Schofield, R ( 2021-08-16)
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    Scenarios and Information for Policymakers
    Daniel, JS ; Reimann, S ; Ashford, P ; Fleming, EL ; Hossaini, R ; Lickley, MJ ; Schofield, R ; Walter-Terrinoni, H ; Fahey, D ; Newman, PA ; Pyle, JA ; Safari, B (World Meteorological Organization, 2022)
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    Atmospheric goals for sustainable development
    Keywood, M ; Paton-Walsh, C ; Lawrence, M ; George, C ; Formenti, P ; Schofield, R ; Cleugh, H ; Borgford-Parnell, N ; Capon, A (AMER ASSOC ADVANCEMENT SCIENCE, 2023-01-20)
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    Key challenges for tropospheric chemistry in the Southern Hemisphere
    Paton-Walsh, C ; Emmerson, KM ; Garland, RM ; Keywood, M ; Hoelzemann, JJ ; Huneeus, N ; Buchholz, RR ; Humphries, RS ; Altieri, K ; Schmale, J ; Wilson, SR ; Labuschagne, C ; Kalisa, E ; Fisher, JA ; Deutscher, NM ; van Zyl, PG ; Beukes, JP ; Joubert, W ; Martin, L ; Mkololo, T ; Barbosa, C ; Andrade, MDF ; Schofield, R ; Mallet, MD ; Harvey, MJ ; Formenti, P ; Piketh, SJ ; Olivares, G (UNIV CALIFORNIA PRESS, 2022-01-07)
    This commentary paper from the recently formed International Global Atmospheric Chemistry (IGAC) Southern Hemisphere Working Group outlines key issues in atmospheric composition research that particularly impact the Southern Hemisphere. In this article, we present a broad overview of many of the challenges for understanding atmospheric chemistry in the Southern Hemisphere, before focusing in on the most significant factors that differentiate it from the Northern Hemisphere. We present sections on the importance of biogenic emissions and fires in the Southern Hemisphere, showing that these emissions often dominate over anthropogenic emissions in many regions. We then describe how these and other factors influence air quality in different parts of the Southern Hemisphere. Finally, we describe the key role of the Southern Ocean in influencing atmospheric chemistry and conclude with a description of the aims and scope of the newly formed IGAC Southern Hemisphere Working Group.
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    The contribution of coral-reef-derived dimethyl sulfide to aerosol burden over the Great Barrier Reef: a modelling study
    Fiddes, SL ; Woodhouse, MT ; Utembe, S ; Schofield, R ; Alexander, SP ; Alroe, J ; Chambers, SD ; Chen, Z ; Cravigan, L ; Dunne, E ; Humphries, RS ; Johnson, G ; Keywood, MD ; Lane, TP ; Miljevic, B ; Omori, Y ; Protat, A ; Ristovski, Z ; Selleck, P ; Swan, HB ; Tanimoto, H ; Ward, JP ; Williams, AG (COPERNICUS GESELLSCHAFT MBH, 2022-02-22)
    Abstract. Coral reefs have been found to produce the sulfur compound dimethyl sulfide (DMS), a climatically relevant aerosol precursor predominantly associated with phytoplankton. Until recently, the role of coral-reef-derived DMS within the climate system had not been quantified. A study preceding the present work found that DMS produced by corals had negligible long-term climatic forcing at the global–regional scale. However, at sub-daily timescales more typically associated with aerosol and cloud formation, the influence of coral-reef-derived DMS on local aerosol radiative effects remains unquantified. The Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) has been used in this work to study the role of coral-reef-derived DMS at sub-daily timescales for the first time. WRF-Chem was run to coincide with an October 2016 field campaign over the Great Barrier Reef, Queensland, Australia, against which the model was evaluated. After updating and scaling the DMS surface water climatology, the model reproduced DMS and sulfur concentrations well. The inclusion of coral-reef-derived DMS resulted in no significant change in sulfate aerosol mass or total aerosol number. Subsequently, no direct or indirect aerosol effects were detected. The results suggest that the co-location of the Great Barrier Reef with significant anthropogenic aerosol sources along the Queensland coast prevents coral-reef-derived aerosol from having a modulating influence on local aerosol burdens in the current climate.
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    Aerosol generation related to respiratory interventions and the effectiveness of a personal ventilation hood.
    McGain, F ; Humphries, RS ; Lee, JH ; Schofield, R ; French, C ; Keywood, MD ; Irving, L ; Kevin, K ; Patel, J ; Monty, J (College of Intensive Care Medicine of Australia and New Zealand, 2020-09)
    OBJECTIVE: To quantify aerosol generation from respiratory interventions and the effectiveness of their removal by a personal ventilation hood. DESIGN AND SETTING: Determination of the aerosol particle generation (in a single, healthy volunteer in a clean room) associated with breathing, speaking, wet coughing, oxygen (O2) 15 L/min via face mask, O2 60 L/min via nasal prongs, bilevel non-invasive positive-pressure ventilation (BiPAP) and nebulisation with O2 10 L/min. INTERVENTIONS: Aerosol generation was measured with two particle sizer and counter devices, focusing on aerosols 0.5-5 μm (human-generated aerosols), with and without the hood. An increase from baseline of less than 0.3 particles per mL was considered a low level of generation. MAIN OUTCOME MEASURES: Comparisons of aerosol generation between different respiratory interventions. Effectiveness of aerosol reduction by a personal ventilation hood. RESULTS: Results for the 0.5-5 μm aerosol range. Quiet breathing and talking demonstrated very low increase in aerosols (< 0.1 particles/mL). Aerosol generation was low for wet coughing (0.1 particles/mL), O2 15 L/min via face mask (0.18 particles/mL), and high flow nasal O2 60 L/min (0.24 particles/mL). Non-invasive ventilation generated moderate aerosols (29.7 particles/mL) and nebulisation very high aerosols (1086 particles/mL); the personal ventilation hood reduced the aerosol counts by 98% to 0.5 particles/mL and 8.9 particles/mL respectively. CONCLUSIONS: In this human volunteer study, the administration of O2 15 L/min by face mask and 60 L/min nasal therapy did not increase aerosol generation beyond low levels. Non-invasive ventilation caused moderate aerosol generation and nebulisation therapy very high aerosol generation. The personal ventilation hood reduced the aerosol counts by at least 98%.