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  • 2020-2024  (34)
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  • 1
    Keywords: mass movements; landslides
    Description / Table of Contents: Introduction --- Subaqueous mass movements in the context of observations of contemporary slope failure / Joshu J. Mountjoy, Aggeliki Georgiopoulou, Jason Chaytor, Michael A. Clare, Davide Gamboa and Jasper Moernaut / Geological Society, London, Special Publications, 500, 1-12, 26 May 2020, https://doi.org/10.1144/SP500-2019-237 --- Section A: consequences and implications --- Revisiting the tsunamigenic volcanic flank collapse of Fogo Island in the Cape Verdes, offshore West Africa / Rachel Barrett, Elodie Lebas, Ricardo Ramalho, Ingo Klaucke, Steffen Kutterolf, Andreas Klügel, Katja Lindhorst, Felix Gross and Sebastian Krastel / Geological Society, London, Special Publications, 500, 13-26, 13 March 2020, https://doi.org/10.1144/SP500-2019-187 --- The sedimentology and tsunamigenic potential of the Byron submarine landslide off New South Wales, Australia / Kendall C. Mollison, Hannah E. Power, Samantha L. Clarke, Alan T. Baxter, Emily M. Lane and Thomas C. T. Hubble / Geological Society, London, Special Publications, 500, 27-40, 7 April 2020, https://doi.org/10.1144/SP500-2019-160 --- Effects of rotational submarine slump dynamics on tsunami genesis: new insight from idealized models and the 1929 Grand Banks event / T. Zengaffinen, F. Løvholt, G. K. Pedersen and C. B. Harbitz / Geological Society, London, Special Publications, 500, 41-61, 11 May 2020, https://doi.org/10.1144/SP500-2019-201 --- A scenario-based assessment of the tsunami hazard in Palermo, northern Sicily, and the southern Tyrrhenian Sea / Jack Dignan, Aaron Micallef, Christof Mueller, Attilio Sulli, Elisabetta Zizzo and Daniele Spatola / Geological Society, London, Special Publications, 500, 63-80, 31 March 2020, https://doi.org/10.1144/SP500-2019-181 --- A workflow for the rapid assessment of the landslide-tsunami hazard in peri-alpine lakes / Michael Strupler, Flavio S. Anselmetti, Michael Hilbe, Katrina Kremer and Stefan Wiemer / Geological Society, London, Special Publications, 500, 81-95, 18 March 2020, https://doi.org/10.1144/SP500-2019-166 --- Towards a national-scale assessment of the subaqueous mass movement hazard in Canada / D. Gwyn Lintern, Jessica Rutherford, Philip R. Hill, Calvin Campbell and Alexandre Normandeau / Geological Society, London, Special Publications, 500, 97-113, 11 May 2020, https://doi.org/10.1144/SP500-2019-206 --- Structural constraints on the subduction of mass-transport deposits in convergent margins / Jacob Geersen, Andrea Festa and Francesca Remitti / Geological Society, London, Special Publications, 500, 115-128, 13 March 2020, https://doi.org/10.1144/SP500-2019-174 --- Evaluating the sealing potential of young and thin mass-transport deposits: Lake Villarrica, Chile / Jasper Moernaut, Gauvain Wiemer, Achim Kopf and Michael Strasser / Geological Society, London, Special Publications, 500, 129-146, 13 March 2020, https://doi.org/10.1144/SP500-2019-155 --- Influence of mass transport deposit (MTD) surface topography on deep-water deposition: an example from a predominantly fine-grained continental margin, New Zealand / Suzanne Bull, Greg H. Browne, Malcolm J. Arnot and Lorna J. Strachan / Geological Society, London, Special Publications, 500, 147-171, 28 April 2020, https://doi.org/10.1144/SP500-2019-192 --- Section B: initiation, triggers and preconditioning --- A multi-disciplinary investigation of the AFEN Slide: the relationship between contourites and submarine landslides / Ricarda Gatter, Michael A. Clare, James E. Hunt, Millie Watts, B. N. Madhusudhan, Peter J. Talling and Katrin Huhn / Geological Society, London, Special Publications, 500, 173-193, 28 April 2020, https://doi.org/10.1144/SP500-2019-184 --- Indonesian Throughflow as a preconditioning mechanism for submarine landslides in the Makassar Strait / Rachel E. Brackenridge, Uisdean Nicholson, Benyamin Sapiie, Dorrik Stow and Dave R. Tappin / Geological Society, London, Special Publications, 500, 195-217, 1 April 2020, https://doi.org/10.1144/SP500-2019-171 --- Morphological signature of gully development by rapid slide retrogression in a layered coarse-grained delta foreslope / Jacques Locat, Ali Azizian, Jim Stronach, Aurélien Hospital, Chris Young, Dominique Turmel and Andrew Bevan / Geological Society, London, Special Publications, 500, 219-234, 13 March 2020, https://doi.org/10.1144/SP500-2019-159 --- Morphology and spatio-temporal distribution of lacustrine mass-transport deposits in Wörthersee, Eastern Alps, Austria / Christoph Daxer, Maddalena Sammartini, Ariana Molenaar, Thomas Piechl, Michael Strasser and Jasper Moernaut / Geological Society, London, Special Publications, 500, 235-254, 19 March 2020, https://doi.org/10.1144/SP500-2019-179 --- A numerical investigation of excess pore pressures and continental slope stability in response to ice-sheet dynamics / Morelia Urlaub, Isabel Kratzke and Berit Oline Hjelstuen / Geological Society, London, Special Publications, 500, 255-266, 13 March 2020, https://doi.org/10.1144/SP500-2019-185 --- Impact of sea-level fluctuations on the sedimentation patterns of the SE African margin: implications for slope instability / Aaron Micallef, Aggeliki Georgiopoulou, Andrew Green and Vittorio Maselli / Geological Society, London, Special Publications, 500, 267-276, 13 March 2020, https://doi.org/10.1144/SP500-2019-172 --- Geomechanical behaviour of gassy soils and implications for submarine slope stability: a literature analysis / P. Kaminski, M. Urlaub, J. Grabe and C. Berndt / Geological Society, London, Special Publications, 500, 277-288, 13 March 2020, https://doi.org/10.1144/SP500-2019-149 --- From gravity cores to overpressure history: the importance of measured sediment physical properties in hydrogeological models / Davide Mencaroni, Jaume Llopart, Roger Urgeles, Sara Lafuerza, Eulàlia Gràcia, Anne Le Friant and Morelia Urlaub / Geological Society, London, Special Publications, 500, 289-300, 22 May 2020, https://doi.org/10.1144/SP500-2019-176 --- The influence of clay content on submarine slope failure: insights from laboratory experiments and numerical models / M. M. W. Silver and B. Dugan / Geological Society, London, Special Publications, 500, 301-309, 26 March 2020, https://doi.org/10.1144/SP500-2019-186 --- Subduction of an extinct rift and its role in the formation of submarine landslides in NW South America / Carlos A. Vargas, Gustavo A. Gutiérrez and Gustavo A. Sarmiento / Geological Society, London, Special Publications, 500, 311-322, 12 May 2020, https://doi.org/10.1144/SP500-2019-189 --- Section C: characterization and regional controls --- Mass wasting on Alpha Ridge in the Arctic Ocean: new insights from multibeam bathymetry and sub-bottom profiler data / Kai Boggild, David C. Mosher, Paola Travaglini, Catalina Gebhardt and Larry Mayer / Geological Society, London, Special Publications, 500, 323-340, 13 May 2020, https://doi.org/10.1144/SP500-2019-196 --- The Last Glacial Maximum Balearic Abyssal Plain megabed revisited / Antonio Cattaneo, Shray Badhani, Cristina Caradonna, Massimo Bellucci, Estelle Leroux, Nathalie Babonneau, Sébastien Garziglia, Jeffrey Poort, Grigorii G. Akhmanov, Germain Bayon, Bernard Dennielou, Gwenäel Jouet, Sébastien Migeon, Marina Rabineau, Laurence Droz and Michael Clare / Geological Society, London, Special Publications, 500, 341-357, 14 May 2020, https://doi.org/10.1144/SP500-2019-188 --- Integrated geophysical, sedimentological and geotechnical investigation of submarine landslides in the Gulf of Lions (Western Mediterranean) / Shray Badhani, Antonio Cattaneo, Stefano Collico, Roger Urgeles, Bernard Dennielou, Estelle Leroux, Florent Colin, Sebastien Garziglia, Marina Rabineau and Laurence Droz / Geological Society, London, Special Publications, 500, 359-376, 14 May 2020, https://doi.org/10.1144/SP500-2019-175 --- Characterization of recent deep-sea debrites in the eastern Mediterranean based on foraminiferal taphonomy / Oded Katz, Leeron Ashkenazi, Shani Sultan-Levi, Sigal Abramovich, Ahuva Almogi-Labin and Orit Hyams-Kaphzan / Geological Society, London, Special Publications, 500, 377-391, 11 May 2020, https://doi.org/10.1144/SP500-2019-170 --- Widespread mass-wasting processes off NE Sicily (Italy): insights from morpho-bathymetric analysis / Daniele Casalbore, Romano Clementucci, Alessandro Bosman, Francesco Latino Chiocci, Eleonora Martorelli and Domenico Ridente / Geological Society, London, Special Publications, 500, 393-403, 15 May 2020, https://doi.org/10.1144/SP500-2019-195 --- Geomorphology and event-stratigraphy of recent mass-movement processes in Lake Hallstatt (UNESCO World Heritage Cultural Landscape, Austria) / Michael Strasser, T. Berberich, S. Fabbri, M. Hilbe, J-J. S. Huang, S. Lauterbach, M. Ortler, H. Rechschreiter, A. Brauer, F. Anselmetti and K. Kowarik / Geological Society, London, Special Publications, 500, 405-426, 31 March 2020, https://doi.org/10.1144/SP500-2019-178 --- Slope stability hazard in a fjord environment: Douglas Channel, Canada / Cooper D. Stacey, D. Gwyn Lintern, John Shaw and Kim W. Conway / Geological Society, London, Special Publications, 500, 427-451, 20 May 2020, https://doi.org/10.1144/SP500-2019-191 --- Submarine canyons, slope failures and mass transport processes in southern Cascadia / Jenna C. Hill, Janet T. Watt, Daniel S. Brothers and Jared W. Kluesner / Geological Society, London, Special Publications, 500, 453-475, 20 May 2020, https://doi.org/10.1144/SP500-2019-169 --- Tectonic and geomorphic controls on the distribution of submarine landslides across active and passive margins, eastern New Zealand / S. J. Watson, J. J. Mountjoy and G. J. Crutchley / Geological Society, London, Special Publications, 500, 477-494, 13 March 2020, https://doi.org/10.1144/SP500-2019-165 --- Geological and tectonic controls on morphometrics of submarine landslides of the Spanish margins / Ricardo León, Roger Urgeles, Raul Pérez-López, Emilio Payo, Amanda Vázquez-Izquierdo, Carmen Julia Giménez-Moreno and David Casas / Geological Society, London, Special Publications, 500, 495-513, 20 May 2020, https://doi.org/10.1144/SP500-2019-153 --- Section D: mobility and kinematics --- Megaclasts within mass-transport deposits: their origin, characteristics and effect on substrates and succeeding flows / Jefferson Nwoko, Ian Kane and Mads Huuse / Geological Society, London, Special Publications, 500, 515-530, 31 March 2020, https://doi.org/10.1144/SP500-2019-146 --- Line length balancing to evaluate multi-phase submarine landslide development: an example from the Storegga Slide, Norway / Suzanne Bull and Joseph A. Cartwright / Geological Society, London, Special Publications, 500, 531-549, 23 March 2020, https://doi.org/10.1144/SP500-2019-168 --- A new depositional model for the Tuaheni Landslide Complex, Hikurangi Margin, New Zealand / Benjamin Couvin, Aggeliki Georgiopoulou, Joshu J. Mountjoy, Lawrence Amy, Gareth J. Crutchley, Morgane Brunet, Sebastian Cardona, Felix Gross, Christoph Böttner, Sebastian Krastel and Ingo Pecher / Geological Society, London, Special Publications, 500, 551-566, 19 May 2020, https://doi.org/10.1144/SP500-2019-180 --- Mass transport deposits in the Donegal Barra Fan and their association with British–Irish Ice Sheet dynamics / Srikumar Roy, Aggeliki Georgiopoulou, Sara Benetti and Fabio Sacchetti / Geological Society, London, Special Publications, 500, 567-586, 18 March 2020, https://doi.org/10.1144/SP500-2019-177 --- Short- and long-term movement of mudflows of the Mississippi River Delta Front and their known and potential impacts on oil and gas infrastructure / Jason D. Chaytor, Wayne E. Baldwin, Samuel J. Bentley, Melanie Damour, Douglas Jones, Jillian Maloney, Michael D. Miner, Jeff Obelcz and Kehui Xu / Geological Society, London, Special Publications, 500, 587-604, 26 March 2020, https://doi.org/10.1144/SP500-2019-183 --- Lessons learned from the monitoring of turbidity currents and guidance for future platform designs / Michael Clare, D. Gwyn Lintern, Kurt Rosenberger, John E. Hughes Clarke, Charles Paull, Roberto Gwiazda, Matthieu J. B. Cartigny, Peter J. Talling, Daniel Perara, Jingping Xu, Daniel Parsons, Ricardo Silva Jacinto and Ronan Apprioual / Geological Society, London, Special Publications, 500, 605-634, 22 May 2020, https://doi.org/10.1144/SP500-2019-173
    Pages: Online-Ressource (VII, 639 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786204776
    Language: English
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  • 2
    Publication Date: 2023-06-10
    Description: Measurements of volatile organic compounds (VOCs) were collected using an Ionicon 4000 Proton Transfer Reaction Time of Flight Mass Spectrometer (PTR-ToF-MS). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29S 150°49'24.97E) from an inlet 10 m above ground level as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The campaign ran from mid-January to mid-March, 2020, with the instrument running from early February. Data presented here corresponds to data used in paper by Mouat et al. (2021a) which spans from 2-6 Feb. 2020. These species are in addition to directly calibrated species archived by Mouat et al. (2021b) in a seperate PANGAEA record. Sample air was drawn down a 20 m PTFE inlet line with a bypass pump (flow rate 1.5 – 3 Lmin-1). Concentrations for compounds presented in this dataset were calculated using methodology proposed in Sekimoto et al. (2017).
    Keywords: 1-Butene; 2-(3H)Furanone + cis-2-butenediol; 2-Furanmethanol; 2-Furfural; 2-Hydroxy-3-methyl-2-cyclopenten-1-one; 5-Methyl furfural + catechol; Acetic acid; Appin, Australia; Australia; Benzaldehyde; Biogenic VOC; biomass burning; C3-Furan; Calculated, according to Sekimoto et al. (2017); Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; Creosol; Cyclopentanone + HCO1; DATE/TIME; Formamide; Formic acid; Furan; Guaiacol; Hydrocarbons, assorted; Maleic anhydride; Methyl acetate; Methylglyoxal; Methyl methacrylate; Methyl propanoate; MULT; Multiple investigations; Nitromethane; Phenol; Propene; PTR-ToF-MS; Styrene; volatile organic compounds
    Type: Dataset
    Format: text/tab-separated-values, 26975 data points
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  • 3
    Publication Date: 2023-07-18
    Description: Measurements of volatile organic compounds (VOCs) were collected using an Ionicon 4000 Proton Transfer Reaction Time of Flight Mass Spectrometer (PTR-ToF-MS). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 10 m above ground level as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The campaign ran from mid-January to mid-March, 2020, with the instrument running from early February. Sample air was drawn down a 20 m PTFE inlet line with a bypass pump (flow rate 1.5 - 3 L min-1). Calibration occurred in situ using standard cylinders for the compounds reported below. Calibration uncertainty is ±20%. Additional compounds may be available on request. Measurements were processed using the Ionicon PTR-MS Viewer software. Measurements from February 2 - February 7 have been corrected to account for an identified inlet leak. A flat subtraction was applied, and resulting compound offsets are provided in the parameter comments. Data from February 7 – February 16 have been removed due to identified leak requiring greater corrections.
    Keywords: Acetaldehyde; Acetone; Acetonitrile; Appin, Australia; Australia; Benzene; Biogenic VOC; biomass burning; Butan-2-one; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; DATE/TIME; HEIGHT above ground; Isoprene; Methacrolein + methyl vinyl ketone; Methanol; Monoterpenes; MULT; Multiple investigations; Precision; Prop-2-enal; Proton Transfer Reaction Time of Flight Mass Spectrometer, Ionicon 4000; PTR-ToF-MS, Ionicon 4000; Sum C8H10; Sum C9H12; Toluene; volatile organic compounds
    Type: Dataset
    Format: text/tab-separated-values, 885045 data points
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  • 4
    Publication Date: 2023-07-11
    Description: Measurements of radon-222 (222Rn) concentration were collected using a 1500 L dual-flow loop radon detector, designed and built by the Australian Nuclear Science and Technology Organisation (ANSTO; Lucas Heights, NSW, Australia) (Chambers et al., 2011; Whittlestone and Zahorowski, 1998). Sampling occurred at 65-75 L min^-1. Calibration occurred during the campaign from a Pylon (Ottawa, ON, Canada) source. Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 3.94 m above ground level as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The campaign ran from mid-January to mid-March, 2020. Reported measurements are at 30-minute time resolution. Concentrations have not been corrected for the response time of the detector but can be on the request of users. See Griffiths et al. (2016) for details.
    Keywords: aerosol; Appin, Australia; boundary layer; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; DATE/TIME; Dual-flow loop radon detector, Australian Nuclear Science and Technology Organisation (ANSTO), Australia; HEIGHT above ground; MULT; Multiple investigations; radon; Radon-222 activity; Radon-222 activity uncertainty fraction; stability; tracer
    Type: Dataset
    Format: text/tab-separated-values, 5928 data points
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  • 5
    Publication Date: 2023-07-11
    Description: Measurements of aerosol size distribution between 14 and 661 nm diameter were measured using a TSI Scanning Mobility Particle Sizer (consisting of 3080 DMA, 3772 CPC and x-ray aerosol neutraliser, TSI Incorporated, Shoreview, MN, USA). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 5.13 m above ground level as part of the Characterising Organics and Aerosol Loading over Australia (COALA-2020) campaign. Zero and flow checks logged have been removed from the published measurements, presented at 1-minute temporal resolution. 1-minute data are spline interpolations of the 5-minute scan measurements output by the instrument. Measurements span from January 29 2020 until March 15 2020. Please note that the instrument was run with leaky impactor until February 18 2020. Measurements in this period should be treated with caution. Measurements made during February 18-20 were disrupted due to impactor testing and have been removed. Following February 20, measurements were made without an impactor. Measurements were not made between February 25 and February 29.
    Keywords: aerosol; Aerosol size distribution; Appin, Australia; biomass burning; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; DATE/TIME; HEIGHT above ground; Log-normal particle size distribution, normalized concentration at particle diameter 101.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 105.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 109.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 113.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 117.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 121.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 126.3 nm; Log-normal particle size distribution, normalized concentration at particle diameter 131 nm; Log-normal particle size distribution, normalized concentration at particle diameter 135.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 14.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 140.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 145.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 15.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 15.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 151.2 nm; Log-normal particle size distribution, normalized concentration at particle diameter 156.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 16.3 nm; Log-normal particle size distribution, normalized concentration at particle diameter 16.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 162.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 168.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 17.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 174.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 18.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 18.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 181.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 187.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 19.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 194.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 20.2 nm; Log-normal particle size distribution, normalized concentration at particle diameter 20.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 201.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 209.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 21.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 216.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 22.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 224.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 23.3 nm; Log-normal particle size distribution, normalized concentration at particle diameter 232.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 24.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 241.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 25.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 250.3 nm; Log-normal particle size distribution, normalized concentration at particle diameter 259.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 25 nm; Log-normal particle size distribution, normalized concentration at particle diameter 26.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 269 nm; Log-normal particle size distribution, normalized concentration at particle diameter 27.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 278.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 28.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 289 nm; Log-normal particle size distribution, normalized concentration at particle diameter 299.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 30 nm; Log-normal particle size distribution, normalized concentration at particle diameter 31.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 310.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 32.2 nm; Log-normal particle size distribution, normalized concentration at particle diameter 322 nm; Log-normal particle size distribution, normalized concentration at particle diameter 33.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 333.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 34.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 346 nm; Log-normal particle size distribution, normalized concentration at particle diameter 35.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 358.7 nm; Log-normal particle size distribution, normalized concentration at particle diameter 37.2 nm; Log-normal particle size distribution, normalized concentration at particle diameter 371.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 38.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 385.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 40 nm; Log-normal particle size distribution, normalized concentration at particle diameter 41.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 414.2 nm; Log-normal particle size distribution, normalized concentration at particle diameter 42.9 nm; Log-normal particle size distribution, normalized concentration at particle diameter 429.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 44.5 nm; Log-normal particle size distribution, normalized concentration at particle diameter 445.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 46.1 nm; Log-normal particle size distribution, normalized concentration at particle diameter 461.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 47.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 478.3 nm; Log-normal particle size distribution, normalized concentration at particle diameter 49.6 nm; Log-normal particle size distribution, normalized concentration at particle diameter 495.8 nm; Log-normal particle size distribution, normalized concentration at particle diameter 51.4 nm; Log-normal particle size distribution, normalized concentration at particle diameter 514 nm; Log-normal particle size distribution, normalized concentration at particle diameter 53.3 nm; Log-normal particle size distribution, normalized
    Type: Dataset
    Format: text/tab-separated-values, 5717224 data points
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  • 6
    Publication Date: 2023-07-11
    Description: Measurements of black carbon aerosol were collected using a multi-angle absorption photometer (MAAP 5012, Thermo Fisher Scientific, Waltham, MA, USA). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 4.8 m above ground level as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The instrument was operated using a sample flow rate of 1000 L/hr (16.67 LPM). The inlet was not heated. It was fitted with a PM10 cap, restricting the measured aerosol to diameters less than 10 µm. Measurements are taken at 1-minute time resolution, as reported here. Flagged measurements have been removed, except for the "Temperature error" flag. This flag was persistent throughout the campaign and relates to the use of a non-heated inlet. Measurements below 0.0005 ug/cm3 have been removed as this is below the detection limit of the instrument. Instrumental details and calculation of aerosol absorption coefficient can be found in Petzold et al. (2002).
    Keywords: aerosol; Aerosol absorption coefficient; Appin, Australia; biomass burning; black carbon; Black carbon, aerosol; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; DATE/TIME; HEIGHT above ground; MAAP 5012; MULT; Multi-angle absorption photometer 5012, Thermo Fisher Scientific; Multiple investigations
    Type: Dataset
    Format: text/tab-separated-values, 125260 data points
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  • 7
    Publication Date: 2023-07-11
    Description: Measurements of photosynthetically active radiation (PAR) were taken using an Apogee SQ-110 sensor (Apogee Instruments, Inc., Logan, UT, USA). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The sensor was placed on an exposed railing 4.35 m above ground level. Measurements were taken at 1 Hz resolution. The measurements reported here are 1-minute averages of 1 Hz measurements. Both PPFD (Photosynthetic Photon Flux Density, measured wavelength range 400-700 nm) and YPFD (Yield Photon Flux Density, measured wavelength range 360-760 nm) are reported.
    Keywords: Apogee sun calibration quantum sensor SQ-110; Appin, Australia; Biogenic VOC; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; DATE/TIME; HEIGHT above ground; MULT; Multiple investigations; PAR; photosynthetically active radiation; Photosynthetic photon, flux density; Photosynthetic photon, flux density, maximum; Photosynthetic photon, flux density, minimum; Photosynthetic photon, flux density, standard deviation; Yield photon, flux density; Yield photon, flux density, maximum; Yield photon, flux density, minimum; Yield photon, flux density, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 529032 data points
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  • 8
    Publication Date: 2023-07-11
    Description: Cloud condensation number concentration was measured using a Cloud Condensation Nuclei Counter (CCN100, Droplet Measurement Technologies, Longmont, Colorado, USA). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 5.13 m above ground level as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The instrument was operated for the majority of the campaign at either 0.2% supersaturation or 0.5% supersaturation, with occasional measurements made at 1.0% supersaturation. Periods when zero and flow checks were carried out have been removed from the published measurements, presented at 1-hour temporal resolution. Data presented are hourly averages of the 1 Hz measurements output by the instrument. Hourly standard deviations are also reported generated from time-averaging of the measurements, and data at finer temporal resolution are available on request.
    Keywords: aerosol; Appin, Australia; biomass burning; Cataract_scout_park; ccn; Characterizing Organics and Aerosol Loading over Australia; cloud condensation nuclei; Cloud condensation nuclei; Cloud condensation nuclei, standard deviation; COALA; COALA-2020; DATE/TIME; HEIGHT above ground; MULT; Multiple investigations; SMPS, TSI; Supersaturation; TSI Scanning Mobility Particle Sizer
    Type: Dataset
    Format: text/tab-separated-values, 9361 data points
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  • 9
    Publication Date: 2023-07-11
    Description: Measurements of greenhouse gases were collected using a Fourier transform infrared (FTIR) trace gas and isotope analyser (Spectronus Trace Greenhouse Gas and Isotope Analyser, Ecotech, Knoxfield, VIC, Australia; Griffith et al., 2012). Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) from an inlet 4.68 m above ground level in eucalypt forest as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. The instrument was operated with a sample flow rate into the 2.5 L cell of ~0.9 slpm. The instrument was calibrated against a suite of four reference gases traceable to WMO-GAW scales before deployment. Measurements of a target tank were performed every two days during the campaign to monitor instrument drift. Measurements are reported at one-minute time resolution.
    Keywords: Appin, Australia; biomass burning; Carbon dioxide; Carbon monoxide; Cataract_scout_park; Characterizing Organics and Aerosol Loading over Australia; CO2 isotopes; COALA; COALA-2020; DATE/TIME; Fourier Transform Infrared (FTIR) spectrometer, Echotech, Spectronus Trace Greenhouse Gas and Isotope Analyser; Greenhouse gases; HEIGHT above ground; Methane; MULT; Multiple investigations; Nitrous oxide; δ13C, carbon dioxide; δ18O, carbon dioxide
    Type: Dataset
    Format: text/tab-separated-values, 452616 data points
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2023-11-30
    Description: Measurements of emission rates (µg/g/h) of volatile organic compounds were captured using thermal desorption tubes from a Teflon enclosure. Measurements were taken at Cataract Scout Park, Appin, N.S.W. (34°14'42.29"S 150°49'24.97"E) as part of the Characterizing Organics and Aerosol Loading over Australia (COALA-2020) campaign. Enclosures captured branches of select local tree species. Branch level VOC samples were made using a custom built, 9L branch enclosure. The two ends of the chamber were made from polytetrafluoroethylene (PTFE) supporting a transparent enclosure made from polyvinyl fluoride film (Dupont Chemicals, Macquarie Park, NSW, Australia). Ambient air, passed through an activated charcoal scrubber, was supplied to the chamber at 12 L/min using a mass flow controller (Aalborg, Orangeburg, NY, USA). Temperatures inside and outside the chamber were recorded manually every 5 minutes using a Digitech thermocouple thermometer with type K thermocouples (Jaycar Electronics, Rydalmere, NSW, Australia). Photosynthetically active radiation (PAR; µmol/m^2^/s) was recorded at the top of the chamber manually every 5 minutes using an Asensetek Lighting Passport (Asensetek, Taipei, Taiwan). VOCs were collected from the enclosures using a sorbent tube containing Tenax TA (Markes International Ltd, Llantrisant, U.K) connected to an air pump (AirChek 2000; SKC Inc., Eighty-Four, PA, USA) flowing air at 200mL/min for 30 minutes. Branches were allowed 30 minutes to acclimate to conditions within the enclosure before VOC sampling commenced. Background (control) enclosure samples were taken at the beginning and end of each day. Post-sampling, tubes were maintained at 4°C until analysis by GC-MS. Sampling occurred over a two-week period in January 2020 and again in March 2020. After VOC sampling, the branch was removed and subsequently dried in a fan-forced convection drying oven (Model TD-78T-2-D, Thermoline Scientific, Wetherill Park, NSW Australia) at 65 °C for 7 days before weighing. Sorbent tubes were analysed by thermal desorption GC-MS using the same equipment and protocols described in Lawson et al., (2020; doi:10.3389/fmars.2020.00106).
    Keywords: 1,8-Cineol, emission rate per unit branch mass as dry weight; alpha-Pinene, emission rate per unit branch mass as dry weight; Appin, Australia; Asensetek Lighting Passport (Taiwan); Australia; beta-Caryophyllene, emission rate per unit branch mass as dry weight; beta-pinene, emission rate per unit branch mass as dry weight; Biogenic VOC; Cataract_scout_park_Backhousia_citriodora_1; Cataract_scout_park_Backhousia_citriodora_2; Cataract_scout_park_Backhousia_citriodora_3; Cataract_scout_park_Backhousia_citriodora_4; Cataract_scout_park_Backhousia_citriodora_5; Cataract_scout_park_Backhousia_citriodora_6; Cataract_scout_park_Banksia_serrata_1; Cataract_scout_park_Banksia_serrata_2; Cataract_scout_park_Banksia_serrata_3; Cataract_scout_park_Banksia_serrata_4; Cataract_scout_park_Banksia_serrata_5; Cataract_scout_park_Banksia_serrata_6; Cataract_scout_park_Corymbia_gummifera_1; Cataract_scout_park_Corymbia_gummifera_2; Cataract_scout_park_Corymbia_gummifera_3; Cataract_scout_park_Corymbia_gummifera_4; Cataract_scout_park_Corymbia_gummifera_5; Cataract_scout_park_Corymbia_gummifera_6; Cataract_scout_park_Eucalyptus_haemastoma_1; Cataract_scout_park_Eucalyptus_haemastoma_2; Cataract_scout_park_Eucalyptus_haemastoma_3; Cataract_scout_park_Eucalyptus_haemastoma_4; Cataract_scout_park_Eucalyptus_haemastoma_5; Cataract_scout_park_Eucalyptus_haemastoma_6; Cataract_scout_park_Eucalyptus_sieberi_1; Cataract_scout_park_Eucalyptus_sieberi_2; Cataract_scout_park_Eucalyptus_sieberi_3; Cataract_scout_park_Eucalyptus_sieberi_4; Cataract_scout_park_Eucalyptus_sieberi_5; Cataract_scout_park_Eucalyptus_sieberi_6; Cataract_scout_park_Melaleuca_quinquenervia_1; Cataract_scout_park_Melaleuca_quinquenervia_2; Cataract_scout_park_Melaleuca_quinquenervia_3; Cataract_scout_park_Melaleuca_quinquenervia_4; Cataract_scout_park_Melaleuca_quinquenervia_5; Cataract_scout_park_Melaleuca_quinquenervia_6; Characterizing Organics and Aerosol Loading over Australia; COALA; COALA-2020; CSP_Backhousia_citriodora_1; CSP_Backhousia_citriodora_2; CSP_Backhousia_citriodora_3; CSP_Backhousia_citriodora_4; CSP_Backhousia_citriodora_5; CSP_Backhousia_citriodora_6; CSP_Banksia_serrata_1; CSP_Banksia_serrata_2; CSP_Banksia_serrata_3; CSP_Banksia_serrata_4; CSP_Banksia_serrata_5; CSP_Banksia_serrata_6; CSP_Corymbia_gummifera_1; CSP_Corymbia_gummifera_2; CSP_Corymbia_gummifera_3; CSP_Corymbia_gummifera_4; CSP_Corymbia_gummifera_5; CSP_Corymbia_gummifera_6; CSP_Eucalyptus_haemastoma_1; CSP_Eucalyptus_haemastoma_2; CSP_Eucalyptus_haemastoma_3; CSP_Eucalyptus_haemastoma_4; CSP_Eucalyptus_haemastoma_5; CSP_Eucalyptus_haemastoma_6; CSP_Eucalyptus_sieberi_1; CSP_Eucalyptus_sieberi_2; CSP_Eucalyptus_sieberi_3; CSP_Eucalyptus_sieberi_4; CSP_Eucalyptus_sieberi_5; CSP_Eucalyptus_sieberi_6; CSP_Melaleuca_quinquenervia_1; CSP_Melaleuca_quinquenervia_2; CSP_Melaleuca_quinquenervia_3; CSP_Melaleuca_quinquenervia_4; CSP_Melaleuca_quinquenervia_5; CSP_Melaleuca_quinquenervia_6; DATE/TIME; Digitech thermometer (Jaycar Electronics, Australia); emission; Event label; Gas chromatography - Mass spectrometry (GC-MS); HAND; Isoprene, emission rate per unit branch mass as dry weight; LATITUDE; Limonene, emission rate per unit branch mass as dry weight; LONGITUDE; p-Cymene, emission rate per unit branch mass as dry weight; Radiation, photosynthetically active; Replicates; Sample comment; Sampling by hand; Species; temperate forests; Temperature, technical; thermal desorption
    Type: Dataset
    Format: text/tab-separated-values, 443 data points
    Location Call Number Expected Availability
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