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23 pages, 8345 KiB  
Article
Daily PM2.5 and Seasonal-Trend Decomposition to Identify Extreme Air Pollution Events from 2001 to 2020 for Continental Australia Using a Random Forest Model
by Nicolas Borchers-Arriagada, Geoffrey G. Morgan, Joseph Van Buskirk, Karthik Gopi, Cassandra Yuen, Fay H. Johnston, Yuming Guo, Martin Cope and Ivan C. Hanigan
Atmosphere 2024, 15(11), 1341; https://doi.org/10.3390/atmos15111341 - 8 Nov 2024
Viewed by 521
Abstract
Robust high spatiotemporal resolution daily PM2.5 exposure estimates are limited in Australia. Estimates of daily PM2.5 and the PM2.5 component from extreme pollution events (e.g., bushfires and dust storms) are needed for epidemiological studies and health burden assessments attributable to [...] Read more.
Robust high spatiotemporal resolution daily PM2.5 exposure estimates are limited in Australia. Estimates of daily PM2.5 and the PM2.5 component from extreme pollution events (e.g., bushfires and dust storms) are needed for epidemiological studies and health burden assessments attributable to these events. We sought to: (1) estimate daily PM2.5 at a 5 km × 5 km spatial resolution across the Australian continent between 1 January 2001 and 30 June 2020 using a Random Forest (RF) algorithm, and (2) implement a seasonal-trend decomposition using loess (STL) methodology combined with selected statistical flags to identify extreme events and estimate the extreme pollution PM2.5 component. We developed an RF model that achieved an out-of-bag R-squared of 71.5% and a root-mean-square error (RMSE) of 4.5 µg/m3. We predicted daily PM2.5 across Australia, adequately capturing spatial and temporal variations. We showed how the STL method in combination with statistical flags can identify and quantify PM2.5 attributable to extreme pollution events in different locations across the country. Full article
(This article belongs to the Section Air Quality)
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<p>Summarized methods.</p>
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<p>Australian State/Territories with 185 PM monitoring stations (black dots), and climate (temperature/humidity) zones as defined by the Australian Bureau of Meteorology (<a href="http://www.bom.gov.au/climate/maps/averages/climate-classification/" target="_blank">http://www.bom.gov.au/climate/maps/averages/climate-classification/</a> (accessed on 15 September 2024)). NT = Northern Territory, QLD = Queensland, NSW = New South Wales, ACT = Australian Capital Territory, TAS = Tasmania, VIC = Victoria, SA = South Australia, WA = Western Australia.</p>
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<p>R-squared between predicted and observed PM<sub>2.5</sub>: (<b>A</b>) out of bag—daily, (<b>B</b>) testing set—daily, (<b>C</b>) training set—daily, (<b>D</b>) complete dataset—daily, (<b>E</b>) complete dataset—monthly, and (<b>F</b>) complete dataset—annual. NOTE: dashed red line represents the identity function.</p>
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<p>Correlation (Pearson’s) between predicted and observed PM<sub>2.5</sub> for each monitoring site.</p>
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<p>PM<sub>2.5</sub> prediction results (μg/m<sup>3</sup>): (<b>a</b>) mean PM<sub>2.5</sub> concentrations Jan 2001–June 2020, (<b>b</b>) standard deviation (SD) of PM<sub>2.5</sub> concentrations Jan 2001–June 2020, (<b>c</b>) Population-weighted mean PM<sub>2.5</sub> concentration by financial year 2001–2020 and State/Territory. (*) A financial year starts on July 1 and ends on June 30 (i.e., the 2001 financial year runs from 1 July 2001 to 30 June 2002).</p>
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<p>Example of extreme air pollution days identified with 95th percentile and 2SD remainder flags for: (<b>A</b>,<b>B</b>) Launceston 2005–2007 showing three winter smoke seasons and the 2006/2007 bushfire season, (<b>C</b>,<b>D</b>) Darwin 2011–2013 showing impact on smoke during three dry seasons, and (<b>E</b>,<b>F</b>) Sydney July 2017 to June 2020 showing three winter smoke seasons and the devastating 2019/2020 Black summer bushfires. NOTES: (1) For comparison purposes, panels (<b>E</b>,<b>F</b>) <span class="html-italic">y</span>-axis do not show values above 50 µg/m<sup>3</sup>. (2) For illustration purposes “seasonal + trend” and “2SD remainder + seasonal + trend” time series have been smoothed, and probable smoke days flagged with these.</p>
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8 pages, 757 KiB  
Reply
Conservation Agendas and the Denial of History. Reply to Penna, I. and Feller, M.C. Comments on “Laming et al. The Curse of Conservation: Empirical Evidence Demonstrating That Changes in Land-Use Legislation Drove Catastrophic Bushfires in Southeast Australia. Fire 2022, 5, 175”
by Michael-Shawn Fletcher, Anthony Romano, Simon Connor, Alice Laming, S. Yoshi Maezumi, Michela Mariani, Russell Mullett and Patricia S. Gadd
Fire 2024, 7(11), 391; https://doi.org/10.3390/fire7110391 - 30 Oct 2024
Viewed by 637
Abstract
This is a reply to the comments of Penna [...] Full article
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<p>Quantifying the differences in tree/shrub cover using aerial photography and GIS. (<b>a</b>) 1969 aerial photograph CAD7011-134 (16 January 1969) over Snowy River National Park [<a href="#B34-fire-07-00391" class="html-bibr">34</a>]. (<b>b</b>) Focus area of the 1969 aerial photograph CAD7011-134 (16 January 1969) (~37°29.392′ S, 148°20.544′ E) [<a href="#B34-fire-07-00391" class="html-bibr">34</a>]. (<b>c</b>) Raster result of inferred canopy cover change between 1969 and 1986 aerial photographs. The darker the colour (green), the greater the shift between light-frequency band inferred canopy cover between the 1969 and 1986 aerial photographs. Raw aerial photographs were processed in Adobe Photoshop 2023 to standardise the two photographs before quantifying temporal changes in ArcGIS Pro 3.1.0 [<a href="#B28-fire-07-00391" class="html-bibr">28</a>,<a href="#B29-fire-07-00391" class="html-bibr">29</a>,<a href="#B30-fire-07-00391" class="html-bibr">30</a>,<a href="#B31-fire-07-00391" class="html-bibr">31</a>,<a href="#B32-fire-07-00391" class="html-bibr">32</a>,<a href="#B33-fire-07-00391" class="html-bibr">33</a>]. (<b>d</b>) 1986 aerial photograph CAD2822-209 (29 January 1986) over Snowy River National Park [<a href="#B34-fire-07-00391" class="html-bibr">34</a>]. (<b>e</b>) Focus area of the 1986 aerial photograph CAD7011-134 (16 January 1969) (~37°29.392′ S, 148°20.544′ E) [<a href="#B34-fire-07-00391" class="html-bibr">34</a>]. (<b>f</b>) Frequency distribution plot of the magnitude of change (%) and the proportion of inferred canopy change (%) within the study area presented in (<b>c</b>). Table insert demonstrates the magnitude of change and proportion of pixels, with 88.10% of pixels demonstrating &gt; 20% of inferred canopy cover change between 1969 and 1986.</p>
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19 pages, 6929 KiB  
Article
Characterising the Chemical Composition of Bushfire Smoke and Implications for Firefighter Exposure in Western Australia
by Kiam Padamsey, Adelle Liebenberg, Ruth Wallace and Jacques Oosthuizen
Fire 2024, 7(11), 388; https://doi.org/10.3390/fire7110388 - 28 Oct 2024
Viewed by 781
Abstract
This study evaluates bushfire smoke as a workplace hazard for firefighters by characterising its chemical composition and potential health risks in Western Australia. Portable Fourier Transform Infrared (FTIR) spectrometry was used to measure airborne chemical concentrations at prescribed burns across five regions, including [...] Read more.
This study evaluates bushfire smoke as a workplace hazard for firefighters by characterising its chemical composition and potential health risks in Western Australia. Portable Fourier Transform Infrared (FTIR) spectrometry was used to measure airborne chemical concentrations at prescribed burns across five regions, including peat (acid sulphate) fire events. Samples were collected during both flaming and smouldering phases, as well as in perceived “clear” air resting zones. Results indicated that carbon monoxide (CO) was the dominant gas, reaching concentrations of 205 ppm at the fire front, followed by nitrogen monoxide (26 ppm) and methane (19 ppm). Peat fires produced distinct profiles, with ammonia (21.5 ppm) and sulphur dioxide (9.5 ppm) concentrations higher than those observed in typical bushfires. Smouldering phases emitted higher chemical concentrations than flaming phases 75% of the time. Even clear air zones contained measurable chemicals, with CO levels averaging 18 ppm, suggesting that firefighters are not free from exposure during rest periods. These findings highlight the need for fit-for-purpose respiratory protective equipment (RPE) and improved rest protocols to minimise exposure. The study underscores the importance of comprehensive health monitoring programs for firefighters to mitigate long-term health risks. Full article
(This article belongs to the Special Issue Patterns, Drivers, and Multiscale Impacts of Wildland Fires)
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<p>Scenes at a typical burn.</p>
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<p>The principal researcher in full wildland PPE collecting data inside a smouldering area of Jarrah Forest.</p>
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<p>The dense vegetation of Blackwood Forest.</p>
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<p>Manjimup peat fire, pictured with the Gasmet Technology DX4040.</p>
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<p>The sandy soils and low-lying vegetation of Wilbinga, pictured with the DBCA commencing a prescribed burn.</p>
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<p>The laterite soils and kwongan heathland of Badgingarra.</p>
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<p>The tall, open canopies and sparse groundcover of the Julimar region.</p>
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<p>The ten most prevalent chemicals present in bushfire smoke, reported in parts per million (ppm).</p>
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<p>The tenth to nineteenth most prevalent gases in general bushfire smoke reported in ppm.</p>
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<p>The ten most prevalent chemicals present in peat fire smoke, reported in ppm.</p>
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<p>Mean concentration of chemicals present inside prescribed burn smoke across five unique ecoregions in WA expressed as parts per million (ppm). * Sulphur dioxide concentration at Manjimup was 9.5 ppm.</p>
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<p>Comparison of the mean chemical emissions across the flaming and smouldering phases of prescribed burns across four different prescribed burns (ppm).</p>
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36 pages, 9570 KiB  
Article
Random Forest Spatial-Temporal and State Space Models to Assess the Impact of Bushfire-Induced Aerosol Events on Ozone Depletion in Australia
by Irene Hudson, Phillip Pedro-Suvorov and Servet Kocak
Appl. Sci. 2024, 14(21), 9825; https://doi.org/10.3390/app14219825 - 28 Oct 2024
Viewed by 755
Abstract
Serious concerns exist that the increasing frequency of fires may delay the recovery of ozone given increasing temperatures due to climate change. Australian bushfires from September 2019 to February 2020 were catastrophic. A random forest spatial-temporal (RF sp) analysis using satellite data to [...] Read more.
Serious concerns exist that the increasing frequency of fires may delay the recovery of ozone given increasing temperatures due to climate change. Australian bushfires from September 2019 to February 2020 were catastrophic. A random forest spatial-temporal (RF sp) analysis using satellite data to detect an association between Australian bushfires and stratosphere ozone on the local depletion of ozone in the vicinity of fires in three regions of Australia (Pacific Ocean, Victoria, NSW) has shown a significant reduction in ozone attributable to aerosols from fires. By intervention analysis, increases in aerosols in all three regions were shown to have a significant and ongoing impact 1–5 days later on reducing ozone (p < 0.0001). Intervention analysis also gave similar periods of aerosol exceedance to those found by Hidden Markov models (HMMs). HMMs established a significant and quantifiable decline in ozone due to bushfire-induced aerosols, with significant lags of 10–25 days between times of aerosol exceedance and subsequent ozone level decline in all three regions. Full article
(This article belongs to the Special Issue AI-Enhanced 4D Geospatial Monitoring for Healthy and Resilient Cities)
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<p>(<b>left</b>) NASA measurements of aerosols optical thickness over April 2019. (<b>right</b>) NASA measurements of aerosols’ optical thickness over December 2020.</p>
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<p>(<b>A</b>) Ammonium sulfate particles containing soot (marked by the small arrows) and fly-ash spheres (marked by the bold arrow in the lower-right corner). (<b>B</b>) In a typical branching soot aggregate; the arrows point to a carbon film that connects individual spherules within the aggregate. (<b>C</b>) Fly-ash spheres. Source: [<a href="#B12-applsci-14-09825" class="html-bibr">12</a>].</p>
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<p>Pathway for smoke particles from intense bushfires to enter the stratosphere and for those same particles to, in turn, lead to ozone depletion. Source: [<a href="#B26-applsci-14-09825" class="html-bibr">26</a>].</p>
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<p>Schematic of ozone levels ozone within a column of air from the Earth’s surface (0 km) to the top of the atmosphere (&gt;35 km). Taken from <a href="https://csl.noaa.gov/assessments/ozone/2018/twentyquestions/" target="_blank">https://csl.noaa.gov/assessments/ozone/2018/twentyquestions/</a>, accessed on 30 June 2023.</p>
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<p>Outline of the map of Australia showing the locations of the three regions. The regions in order from top to bottom: Region 1 (Blue), Region 2 (Red) and Region 3 (Green). The checkerboard shading pattern identifies the study area.</p>
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<p>Observed from data of daily gridded aerosol values plot of entire study area over the 20 days from 3 November 2019.</p>
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<p>Observed from data of daily gridded ozone values plot of entire study area over the 20 days from 3 November 2019.</p>
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<p>Time series plot of Total Sum Ozone for each region.</p>
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<p>Time series plot of Total Sum Aerosol for each region.</p>
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<p>Graphical models associated with extensions to the basic HMM. (<b>A</b>) state sequence with a memory order of 2. (<b>B</b>) influence of covariate <math display="inline"><semantics> <mrow> <msub> <mi>z</mi> <mn>1</mn> </msub> <mo>,</mo> <mo>…</mo> <mo>,</mo> <msub> <mi>z</mi> <mi>T</mi> </msub> </mrow> </semantics></math> on state dynamics. (<b>C</b>) observations depending on both states and previous observations. (<b>D</b>) bivariate observation sequence, conditionally independent given the states. Source: [<a href="#B72-applsci-14-09825" class="html-bibr">72</a>].</p>
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<p>Spatial-temporal predictions of daily gridded ozone values over 20 days from 3 November 2019.</p>
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<p>Spatial-temporal predictions of daily gridded ozone values over 20 days from 1 December 2019.</p>
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<p>Spatial-temporal predictions of daily gridded ozone values over 20 days from 20 January 2020.</p>
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<p>Quantile prediction intervals of daily gridded ozone values over 20 days from 3 November 2019.</p>
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<p>Quantile prediction intervals of daily gridded ozone values over 20 days from 1 December 2019.</p>
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<p>Quantile prediction intervals of daily gridded ozone values over 20 days from 20 January 2020.</p>
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<p>CPs for TSA and TSO for Region 1 (Pacific Ocean) as shown by vertical grey dashed lines.</p>
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<p>CPs for TSA and TSO for Region 2 (Vic) as shown by vertical grey dashed lines.</p>
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<p>CPs for TSA and TSO for Region 3 (NSW) as shown by vertical grey dashed lines.</p>
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<p>HMM bivariate state changes in total sum ozone time-series with respect to total sum aerosol time-series as a covariate for Region 3.</p>
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<p>Summary of the BinSeg CPs and the HMM derived CPs. In the RHS table, the O columns show the ozone CP (day) based on HMM without covariate adjustment. The A columns show the ozone CP (day) for HMMs with aerosol as a covariate.</p>
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<p>Detected Change Points for Total Sum Ozone (Region 3).</p>
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<p>Intervention Analysis Output for Region 3 with Model R3.</p>
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<p>Detected Change Points for Total Sum Ozone (Region 1).</p>
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<p>Intervention Analysis Output for Region 1.</p>
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<p>Detected Change Points for Total Sum Ozone (Region 2).</p>
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<p>Intervention Analysis Output for Region 2.</p>
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<p>HMM bivariate state changes in total sum ozone time-series with respect to total sum aerosol time-series as a covariate for Region 1.</p>
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<p>HMM bivariate state changes in total sum ozone time-series with respect to total sum aerosol time-series as a covariate for Region 2.</p>
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20 pages, 19130 KiB  
Article
Spatiotemporal Analysis of Land Use and Land Cover Dynamics of Dinderesso and Peni Forests in Burkina Faso
by Alphonse Maré David Millogo, Boalidioa Tankoano, Oblé Neya, Fousseni Folega, Kperkouma Wala, Kwame Oppong Hackman, Bernadin Namoano and Komlan Batawila
Geomatics 2024, 4(4), 362-381; https://doi.org/10.3390/geomatics4040019 - 4 Oct 2024
Viewed by 652
Abstract
The sustainable management of protected areas has increasingly become difficult due to the lack of updated information on land use and land cover transformations caused by anthropogenic pressures. This study investigates the spatiotemporal dynamics of the Dinderesso and Peni classified forests in Burkina [...] Read more.
The sustainable management of protected areas has increasingly become difficult due to the lack of updated information on land use and land cover transformations caused by anthropogenic pressures. This study investigates the spatiotemporal dynamics of the Dinderesso and Peni classified forests in Burkina Faso from 1986 to 2022. First, a data driven method was adopted to investigate these forests degradation dynamics. Hence, relevant Landsat images data were collected, segmented, and analyzed using QGIS SCP plugin Random Forest algorithm. Ninety percent of the overall adjusted classification accuracies were obtained. The analysis also showed significant degradation and deforestation with high wooded vegetation classes such as clear forest and wooded savannah (i.e., tree savannah) converging to lower vegetation classes like shrub savannah and agroforestry parks. A second investigation carried out through surveys and field trips revealed key anthropogenic drivers including agricultural expansion, demographic pressure, bad management, wood cutting abuse, overexploitation, overgrazing, charcoal production, and bushfires. These findings highlight the critical need for better management to improve these protected areas. Full article
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<p>Dinderesso and Peni classified forest location.</p>
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<p>Landsat land use land cover assessment and household heads survey flowchart.</p>
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<p>Land uses land cover classes in Dinderesso and Peni classified forests.</p>
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<p>Land use land cover map of Dinderesso classified forest in 1986, 2006, 2010, 2016, and 2022.</p>
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<p>Land use land cover map of Peni classified forest in 1986, 2006, 2010, 2016, and 2022.</p>
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<p>Land use land cover change in the classified forest of Dinderesso in 1986, 2006, 2010, 2016, and 2022.</p>
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<p>Land use land change in the classified forest of Peni in 1986, 2006, 2010, 2016, and 2022.</p>
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<p>Anthropogenic drivers of Dinderesso and Peni classified forests degradation and deforestation.</p>
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<p>Dinderesso classified forest degradation and deforestation drivers.</p>
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<p>Peni classified forest degradation and deforestation drivers.</p>
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12 pages, 2387 KiB  
Article
Preliminary Assessment of Tunic Off-Gassing after Wildland Firefighting Exposure
by Kiam Padamsey, Adelle Liebenberg, Ruth Wallace and Jacques Oosthuizen
Fire 2024, 7(9), 321; https://doi.org/10.3390/fire7090321 - 14 Sep 2024
Cited by 1 | Viewed by 550
Abstract
Evidence has previously shown that outer tunics (turnout coats) worn by firefighters at structural fires are contaminated with harmful chemicals which subsequently off-gas from the material. However, there is limited research on whether this phenomenon extends to wildland firefighter uniforms. This pilot study [...] Read more.
Evidence has previously shown that outer tunics (turnout coats) worn by firefighters at structural fires are contaminated with harmful chemicals which subsequently off-gas from the material. However, there is limited research on whether this phenomenon extends to wildland firefighter uniforms. This pilot study aimed to explore if the tunics of volunteer bushfire and forestry firefighters in Western Australia off-gas any contaminants after exposure to prescribed burns or bushfires, and whether there is a need to explore this further. Nine tunics were collected from firefighters following nine bushfire and prescribed burn events, with a set of unused tunics serving as a control. Chemical analysis was performed on these tunics to assess levels of acrolein, benzene, formaldehyde, and sulphur dioxide contamination. The assessment involved measuring chemical off-gassing over a 12 h period using infrared spectrometry. Tunics worn by firefighters appear to adsorb acrolein, benzene, formaldehyde, and sulphur dioxide from bushfire smoke and these contaminants are emitted from firefighting tunics following contamination at elevated concentrations. Further investigation of this research with a larger study sample will be beneficial to understand this phenomenon better and to determine the full extent and range of chemical contaminants absorbed by all firefighter clothing. Full article
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<p>Summary of acrolein off-gassing from fire-fighting tunics.</p>
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<p>Summary of benzene off-gassing from firefighting tunics.</p>
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<p>Summary of formaldehyde off-gassing from firefighting tunics.</p>
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<p>Summary of sulphur dioxide off-gassing from firefighting tunics.</p>
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19 pages, 3020 KiB  
Article
Assessing the Provisioning of Ecosystem Services Provided by the Relics Forest in Togo’s Mono Biosphere Reserve
by Kokouvi Gbétey Akpamou, Somiyabalo Pilabina, Hodabalo Egbelou, Kokou Richard Sewonou, Yvonne Walz, Luca Luiselli, Gabriel H. Segniagbeto, Daniele Dendi and Kouami Kokou
Conservation 2024, 4(3), 486-504; https://doi.org/10.3390/conservation4030030 - 10 Sep 2024
Viewed by 840
Abstract
In most Sub-Saharan African countries, such as Togo, forest ecosystems provide ecosystem services to the local population. These ecosystem services are of vital importance to the local populations, who depend on the benefits derived from their use to meet their socio-economic needs. The [...] Read more.
In most Sub-Saharan African countries, such as Togo, forest ecosystems provide ecosystem services to the local population. These ecosystem services are of vital importance to the local populations, who depend on the benefits derived from their use to meet their socio-economic needs. The permanent dependence of these populations on ecosystem services is a major factor accelerating the degradation of natural resources, which are already under pressure from climatic factors. The present study assesses the provisioning of ecosystem services provided by the relics forest in the southeast region of the Mono Biosphere Reserve in Togo. Individual interviews and group discussions were carried out with 420 households in fourteen villages around the reserve to identify the current uses of woody species. The results show that 100% of the respondents cited plant species, such as Mitragyna inermis, Lonchocarpus sericeus, and Diospyros mespiliformis, as used for wood. Species, such as Mimusops andogensis and Triplohiton scleroxylon, were cited as exclusively used for wood by 94% and 86%, respectively. Other species, such as Vitex doniana and Dialium guineense, in addition to their use for wood (93% and 70%), were cited, respectively, by 97% and 98% of respondents as used for fruit, and by 82% and 90% for their leaves. The heavy daily use of these species compromises their sustainability. An analysis of Sorensen’s similarity index, according to gender, age, ethnic group, and sector of activity, revealed a variation in this index ranging from 0.6 to 1, reflecting households’ knowledge of the use of these seven species. The local populations are already feeling the effects of the low availability of these commonly used species. According to them, the depletion of these resources is caused mainly by agricultural clearing, illegal logging, and bushfires. Full article
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<p>Location of Togo’s Mono Biosphere Reserve.</p>
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<p>Location of TMBR villages surveyed.</p>
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<p>Principal component analysis (PCA) of the matrix, for 7 woody species X 6 use categories.</p>
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<p>Local people’s knowledge of woody species.</p>
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<p>Availability of woody species over the last ten (10) years.</p>
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<p>Sought-after organ parts of seven most commonly used woody species.</p>
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<p>Uses of seven woody species.</p>
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<p>Reasons for the disappearance of woody species.</p>
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16 pages, 278 KiB  
Article
Individual Resilience and Disaster-Specific Adaptation and Resilience Following a Bushfire Event in Regional Queensland
by Susan F. Rockloff, Carina C. Anderson, Lucinda P. Burton, Victoria R. Terry, Sally K. Jensen, Anne Nolan and Peter C. Terry
Sustainability 2024, 16(16), 7011; https://doi.org/10.3390/su16167011 - 15 Aug 2024
Cited by 1 | Viewed by 1224
Abstract
Natural disasters such as bushfires are a test of individual and group resilience, and in extreme cases, threaten the sustainability of communities. Bushfires have long been common in Australia, although anthropogenic climate change has exacerbated their prevalence and severity. The aim of the [...] Read more.
Natural disasters such as bushfires are a test of individual and group resilience, and in extreme cases, threaten the sustainability of communities. Bushfires have long been common in Australia, although anthropogenic climate change has exacerbated their prevalence and severity. The aim of the present study was to assess the individual resilience and disaster-specific adaptation and resilience of community members in the wake of a bushfire event. Using a quantitative, cross-sectional design, an adult community sample of 165 residents of Noosa Shire in regional Queensland, Australia completed the 25-item Connor-Davidson Resilience Scale (CD-RISC©) and the 43-item Disaster Adaptation and Resilience Scale (DARS). Mean scores for the CD-RISC© indicated significantly greater resilience (p < 0.001) than reported previously for a large Australian community cohort. Similarly, the DARS scores indicated significantly greater adaptation and resilience (p < 0.001) than that of a comparable cohort in the USA. The two oldest groups of residents (66+ years and 51–65 years) reported significantly greater adaptation and resilience than the group of younger residents (≤50 years; p < 0.001). The study findings provide the Noosa Shire community with an objective baseline from which they can assess the efficacy of future resilience-building initiatives and, more broadly, offer a valuable point of reference for future disaster-related research. Full article
15 pages, 8036 KiB  
Article
Global Warming Impacts on Southeast Australian Coastally Trapped Southerly Wind Changes
by Lance M. Leslie, Milton Speer and Shuang Wang
Climate 2024, 12(7), 96; https://doi.org/10.3390/cli12070096 - 1 Jul 2024
Viewed by 1046
Abstract
Coastally trapped southerly wind changes are prominent during southeast Australia’s warm season (spring and summer). These abrupt, often gale force, wind changes are known locally as Southerly Busters (SBs) when their wind speeds reach 15 m/s. They move northwards along the coast, often [...] Read more.
Coastally trapped southerly wind changes are prominent during southeast Australia’s warm season (spring and summer). These abrupt, often gale force, wind changes are known locally as Southerly Busters (SBs) when their wind speeds reach 15 m/s. They move northwards along the coast, often producing very large temperature drops. SBs exceeding 21 m/s are severe SBs (SSBs). SBs have both positive and negative impacts. They bring relief from oppressively hot days but can cause destructive wind damage, worsen existing bushfires, and endanger aviation and marine activities. This study assesses the impacts of global warming (GW) and associated climate change on SBs and SSBs, using observational data from 1970 to 2022. Statistical analyses determine significant trends in annual frequency counts of SBs and SSBs, particularly during the accelerated GW period from the early–mid-1990s. It was found that the annual combined count of SBs and SSBs had increased, with SSBs dominating from 1970 to 1995, but SB frequencies exceeded SSBs from 1996 to 2023. The ascendency of SB frequencies over SSBs since 1996 is explained by the impact of GW on changes in global and local circulation patterns. Case studies exemplify how these circulation changes have increased annual frequencies of SBs, SSBs, and their combined total. Full article
(This article belongs to the Special Issue Coastal Hazards under Climate Change)
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<p>Australian Bureau of Meteorology mean sea level pressure (MSLP) archived analysis showing contours of manually plotted observations, (<b>a</b>) at 0200 UTC 20 November 1972, before the SB passage, (<b>b</b>) at 0200 UTC 21 November 1972, after the SB passage. The wind direction changes from northwesterly in Sydney (left panel), to southerly (right panel) as the ridging moves up the east coast.</p>
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<p>Himawari-8 satellite at 0600 UTC, 7 October 2021, showing satellite-derived wind vectors close to the surface. Note the marked delineation between NW winds before the SB and southerly winds after the passage of the SB at the coast through Sydney. Half-length yellow wind barbs indicate from 3 to 7 knots and full-length wind barbs indicate from 8 to 12 knots.</p>
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<p>Mean sea level pressure (MSLP) analysis, (<b>a</b>) on 26 December 2021 00 UTC, before the SB passage, (<b>b</b>) on 26 December 2021 12 UTC, after the SB passage. The wind direction changes from northwesterly in Sydney (left panel), to southerly (right panel).</p>
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<p>(<b>a</b>) SB and SSB frequencies October to March 1970–1971 to 2022–2023. Blue and red lines are the SBs and SSBs, respectively. Blue and red dashed lines represent the linear trends in the SBs and SSBs. Note the steady increase in SBs from the mid-1990s. (<b>b</b>) Frequency of all SBs (SBs plus SSBs) October to March 1970–1971 to 2022–2023. Frequency is indicated by open, blue circles. The dashed red line is the linear trend.</p>
Full article ">Figure 4 Cont.
<p>(<b>a</b>) SB and SSB frequencies October to March 1970–1971 to 2022–2023. Blue and red lines are the SBs and SSBs, respectively. Blue and red dashed lines represent the linear trends in the SBs and SSBs. Note the steady increase in SBs from the mid-1990s. (<b>b</b>) Frequency of all SBs (SBs plus SSBs) October to March 1970–1971 to 2022–2023. Frequency is indicated by open, blue circles. The dashed red line is the linear trend.</p>
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<p>(<b>a</b>) The 1970–1971 to 2022–2023 frequency distribution of SB maximum gust strength values (15.0–20 m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>b</b>) The 1970–1971 to 2022–2023 frequency distribution of SSB maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>c</b>) The 1970–1971 to 2022–2023 total frequency distribution of maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend.</p>
Full article ">Figure 5 Cont.
<p>(<b>a</b>) The 1970–1971 to 2022–2023 frequency distribution of SB maximum gust strength values (15.0–20 m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>b</b>) The 1970–1971 to 2022–2023 frequency distribution of SSB maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>c</b>) The 1970–1971 to 2022–2023 total frequency distribution of maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend.</p>
Full article ">Figure 5 Cont.
<p>(<b>a</b>) The 1970–1971 to 2022–2023 frequency distribution of SB maximum gust strength values (15.0–20 m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>b</b>) The 1970–1971 to 2022–2023 frequency distribution of SSB maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend. (<b>c</b>) The 1970–1971 to 2022–2023 total frequency distribution of maximum gust strength values (21.0–maximum recorded value, m/s). Increasing numbers of the same maximum gust strength value within an October to March period are shown by the increasing size of the open circles, enumerated in the legend.</p>
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<p>(<b>a</b>) Southern Hemisphere NOAA/PSL MSLP anomalies (hPa) October to March 1997–2023, (<b>b</b>) South Hemisphere NOAA/PSL MSLP anomalies (hPa) October to March 1971–1996.</p>
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<p>(<b>a</b>) Shows the 30 min plots of wind speeds (m/s, blue lines) and wind gusts (m/s, grey lines) for the passage of the southerly buster through Sydney on 20 November 1973. The orange line is the wind direction in degrees. The maximum wind gust is 27 m/s at approximately 0600 UTC. (<b>b</b>) Shows the 30 min plots of MSLP (green line) and temperature (red line) for the passage of the southerly buster through Sydney on 20 November 1973. The precise passage time is shown by the vertical black arrow at approximately 0600 UTC.</p>
Full article ">Figure 7 Cont.
<p>(<b>a</b>) Shows the 30 min plots of wind speeds (m/s, blue lines) and wind gusts (m/s, grey lines) for the passage of the southerly buster through Sydney on 20 November 1973. The orange line is the wind direction in degrees. The maximum wind gust is 27 m/s at approximately 0600 UTC. (<b>b</b>) Shows the 30 min plots of MSLP (green line) and temperature (red line) for the passage of the southerly buster through Sydney on 20 November 1973. The precise passage time is shown by the vertical black arrow at approximately 0600 UTC.</p>
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<p>(<b>a</b>) Shows the 30 min plots of wind speeds (m/s, blue lines) and wind gusts (m/s, grey lines) for the passage of the southerly buster through Sydney on 31 January 2019. The orange line is the wind direction in degrees. The maximum wind gusts of about 23–25 m/s occurred during the period at approximately 0645–0900 UTC. (<b>b</b>) Shows the 30 min plots of MSLP (green line) and temperature (reed line) for the passage of the southerly buster through Sydney on 31 January 2019. The precise passage time is shown by the vertical black arrow at approximately 0640 UTC.</p>
Full article ">Figure 8 Cont.
<p>(<b>a</b>) Shows the 30 min plots of wind speeds (m/s, blue lines) and wind gusts (m/s, grey lines) for the passage of the southerly buster through Sydney on 31 January 2019. The orange line is the wind direction in degrees. The maximum wind gusts of about 23–25 m/s occurred during the period at approximately 0645–0900 UTC. (<b>b</b>) Shows the 30 min plots of MSLP (green line) and temperature (reed line) for the passage of the southerly buster through Sydney on 31 January 2019. The precise passage time is shown by the vertical black arrow at approximately 0640 UTC.</p>
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25 pages, 37691 KiB  
Article
African Lovegrass Segmentation with Artificial Intelligence Using UAS-Based Multispectral and Hyperspectral Imagery
by Pirunthan Keerthinathan, Narmilan Amarasingam, Jane E. Kelly, Nicolas Mandel, Remy L. Dehaan, Lihong Zheng, Grant Hamilton and Felipe Gonzalez
Remote Sens. 2024, 16(13), 2363; https://doi.org/10.3390/rs16132363 - 27 Jun 2024
Viewed by 1037
Abstract
The prevalence of the invasive species African Lovegrass (Eragrostis curvula, ALG thereafter) in Australian landscapes presents significant challenges for land managers, including agricultural losses, reduced native species diversity, and heightened bushfire risks. Uncrewed aerial system (UAS) remote sensing combined with AI [...] Read more.
The prevalence of the invasive species African Lovegrass (Eragrostis curvula, ALG thereafter) in Australian landscapes presents significant challenges for land managers, including agricultural losses, reduced native species diversity, and heightened bushfire risks. Uncrewed aerial system (UAS) remote sensing combined with AI algorithms offer a powerful tool for accurately mapping the spatial distribution of invasive species and facilitating effective management strategies. However, segmentation of vegetations within mixed grassland ecosystems presents challenges due to spatial heterogeneity, spectral similarity, and seasonal variability. The performance of state-of-the-art artificial intelligence (AI) algorithms in detecting ALG in the Australian landscape remains unknown. This study compared the performance of four supervised AI models for segmenting ALG using multispectral (MS) imagery at four sites and developed segmentation models for two different seasonal conditions. UAS surveys were conducted at four sites in New South Wales, Australia. Two of the four sites were surveyed in two distinct seasons (flowering and vegetative), each comprised of different data collection settings. A comparative analysis was also conducted between hyperspectral (HS) and MS imagery at a single site within the flowering season. Of the five AI models developed (XGBoost, RF, SVM, CNN, and U-Net), XGBoost and the customized CNN model achieved the highest validation accuracy at 99%. The AI model testing used two approaches: quadrat-based ALG proportion prediction for mixed environments and pixel-wise classification in masked regions where ALG and other classes could be confidently differentiated. Quadrat-based ALG proportion ground truth values were compared against the prediction for the custom CNN model, resulting in 5.77% and 12.9% RMSE for the seasons, respectively, emphasizing the superiority of the custom CNN model over other AI algorithms. The comparison of the U-Net demonstrated that the developed CNN effectively captures ALG without requiring the more intricate architecture of U-Net. Masked-based testing results also showed higher F1 scores, with 91.68% for the flowering season and 90.61% for the vegetative season. Models trained on single-season data exhibited decreased performance when evaluated on data from a different season with varying collection settings. Integrating data from both seasons during training resulted in a reduction in error for out-of-season predictions, suggesting improved generalizability through multi-season data integration. Moreover, HS and MS predictions using the custom CNN model achieved similar test results with around 20% RMSE compared to the ground truth proportion, highlighting the practicality of MS imagery over HS due to operational limitations. Integrating AI with UAS for ALG segmentation shows great promise for biodiversity conservation in Australian landscapes by facilitating more effective and sustainable management strategies for controlling ALG spread. Full article
(This article belongs to the Special Issue Remote Sensing for Management of Invasive Species)
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Figure 1

Figure 1
<p>Overview of the study methodology, illustrating the key steps in data acquisition, data preprocessing, pixel-wise labeling, multispectral-based prediction, and multispectral and hyperspectral comparison.</p>
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<p>Map of the study sites. Site 1 and Site 2 correspond to Bunyan sites, while Site 3 and Site 4 correspond to Cooma sites, located in in New South Wales, Australia.</p>
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<p>Illustration of quadrat species diversity at Bunyan and Cooma sites.</p>
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<p>Labeled polygons of three randomly selected quadrats from Sites 1 and 4, along with their corresponding close-up images.</p>
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<p>Spectral signature differences for spectral indices.</p>
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<p>Modelling and augmentation of data points during ALG model development.</p>
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<p>Custom CNN model architecture for MS-based ALG segmentation. For MS and HS comparison, the third dimension of the first layer captures the channel depth, which is 5 for MS and 448 for HS imagery. The remaining dimensions are unchanged.</p>
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<p>U-Net architecture used for ALG classification.</p>
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<p>Multispectral-based prediction maps of three quadrats from test sites using the models developed from the combined seasonal dataset. The filled black regions represent the ALG.</p>
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<p>The ground truth and the predicted ALG proportion from the Bunyan test site (flowering) using the models developed from the combined seasonal dataset.</p>
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<p>The ground truth and the predicted ALG proportion from the Cooma test site (vegetative) using the models developed from the combined seasonal dataset.</p>
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<p>Multispectral-based segmented ALG spatial distribution map of test sites. (<b>a</b>) Cooma site; (<b>b</b>) Bunyan site. The hashed black polygon represents the ALG detected region.</p>
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<p>The ground truth and the predicted ALG proportion of the quadrats from the test region of Site 2 by the custom CNN model.</p>
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<p>Comparison of multispectral and hyperspectral imagery-based models prediction maps of three quadrats from test sites. The filled black regions represent the ALG.</p>
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21 pages, 12213 KiB  
Article
A 3D Numerical Model to Estimate Lightning Types for PyroCb Thundercloud
by Surajit Das Barman, Rakibuzzaman Shah, Syed Islam and Apurv Kumar
Appl. Sci. 2024, 14(12), 5305; https://doi.org/10.3390/app14125305 - 19 Jun 2024
Viewed by 796
Abstract
Pyrocumulonimbus (pyroCb) thunderclouds, produced from extreme bushfires, can initiate frequent cloud-to-ground (CG) lightning strikes containing extended continuing currents. This, in turn, can ignite new spot fires and inflict massive harm on the environment and infrastructures. This study presents a 3D numerical thundercloud model [...] Read more.
Pyrocumulonimbus (pyroCb) thunderclouds, produced from extreme bushfires, can initiate frequent cloud-to-ground (CG) lightning strikes containing extended continuing currents. This, in turn, can ignite new spot fires and inflict massive harm on the environment and infrastructures. This study presents a 3D numerical thundercloud model for estimating the lightning of different types and its striking zone for the conceptual tripole thundercloud structure which is theorized to produce the lightning phenomenon in pyroCb storms. More emphasis is given to the lower positive charge layer, and the impacts of strong wind shear are also explored to thoroughly examine various electrical parameters including the longitudinal electric field, electric potential, and surface charge density. The simulation outcomes on pyroCb thunderclouds with a tripole structure confirm the presence of negative longitudinal electric field initiation at the cloud’s lower region. This initiation is accompanied by enhancing the lower positive charge region, resulting in an overall positive electric potential increase. Consequently, negative surface charge density appears underneath the pyroCb thundercloud which has the potential to induce positive (+CG) lightning flashes. With wind shear extension of upper charge layers in pyroCb, the lightning initiation potential becomes negative to reduce the absolute field value and would generate negative (−CG) lightning flashes. A subsequent parametric study is carried out considering a positive correlation between aerosol concentration and charge density to investigate the sensitivity of pyroCb electrification under the influence of high aerosol conditions. The suggested model would establish the basis for identifying the potential area impacted by lightning and could also be expanded to analyze the dangerous conditions that may arise in wind energy farms or power substations in times of severe pyroCb events. Full article
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Figure 1
<p>(<b>a</b>) Active fire and (<b>b</b>) lightning strike observations on Black Saturday, 7 February 2009 [<a href="#B11-applsci-14-05305" class="html-bibr">11</a>].</p>
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<p>PyroCb thunderclouds exhibit the following: (<b>a</b>) a tripole structure characterized by a prevailing upper positive (UP) charge layer, a prominent middle negative (MN) and a minor lower positive (LP) charge layers, accompanied by an extra negative screening layer (SC) positioned at the top, and (<b>b</b>) the effect of wind shear to create the titled structure.</p>
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<p>The vertical profile of the pyroCb thundercloud model (in xz plane) exhibits a tripole charge structure under two different conditions: (<b>a</b>) without LP charge enhancement (configuration 1) and (<b>b</b>) with increased LP charge region (configuration 2).</p>
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<p>Plots of the distributions of electric potential (<b>a1</b>,<b>a2</b>) and the changes in the electric field (<b>b1</b>,<b>b2</b>) for configurations 1 and 2 of the tripole structure-based pyroCb thundercloud, respectively.</p>
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<p>Graphs depicting the electric potential <span class="html-italic">V</span> (MV) are shown at the point of maximum field where the initiation of flash is marked with an “x” (<b>a1</b>,<b>a2</b>). The longitudinal electric field <math display="inline"><semantics> <msub> <mi>E</mi> <mi>z</mi> </msub> </semantics></math> (kV/m) for two different thundercloud configurations is also illustrated in (<b>b1</b>,<b>b2</b>).</p>
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<p>Plots of surface charge density <math display="inline"><semantics> <mi>σ</mi> </semantics></math> for: (<b>a</b>) configuration 1 and (<b>b</b>) configuration 2 to identify probable CG lightning types in pyroCb thunderclouds. Detailed views of the temporal changes in <math display="inline"><semantics> <mi>σ</mi> </semantics></math> on Earth’s surface (<math display="inline"><semantics> <mrow> <mi>x</mi> <mi>y</mi> </mrow> </semantics></math> plane) are presented for two tripole charge configurations.</p>
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<p>Vertical cross-sectional representation of pyroCb thunderclouds incorporating the wind shear extension of SC and UP charge layers when (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>4</mn> </mrow> </semantics></math>, and (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>8</mn> </mrow> </semantics></math> km.</p>
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<p>With the wind shear extension of SC and UP charge layers, projections of potential (<b>a1</b>–<b>a3</b>) and electric field (<b>b1</b>–<b>b3</b>) distributions in the conceptual pyroCb thundercloud.</p>
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<p>Graphs showing the electric potential <span class="html-italic">V</span> (MV) at maximum field point of pyroCb thundercloud (<b>a1</b>–<b>a3</b>) and its corresponding longitudinal electric field <math display="inline"><semantics> <msub> <mi>E</mi> <mi>z</mi> </msub> </semantics></math> (kV/m) (<b>b1</b>–<b>b3</b>) under the effect of wind shear. The symbol “x” in (<b>a1</b>–<b>a3</b>) represents the flash initiation point, and the red-dashed dotted line in (<b>b1</b>–<b>b3</b>) indicates the initiation threshold field.</p>
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<p>Plots of surface charge density <math display="inline"><semantics> <mi>σ</mi> </semantics></math> (<b>a</b>–<b>c</b>) for a pyroCb thundercloud under the effect of wind shear.</p>
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<p>Figures illustrating (<b>a1</b>–<b>c1</b>) the electric potential <span class="html-italic">V</span> (MV) at maximum field point, and (<b>a2</b>–<b>c2</b>) the longitudinal electric field <math display="inline"><semantics> <msub> <mi>E</mi> <mi>z</mi> </msub> </semantics></math> (kV/m) for pyroCb thundercloud with wind shear extension values of (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>4</mn> </mrow> </semantics></math> and (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>d</mi> <mo>=</mo> <mn>8</mn> </mrow> </semantics></math> km. The threshold field value of initiation is shown by red dash-dotted lines.</p>
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<p>Variations in surface charge density <math display="inline"><semantics> <mi>σ</mi> </semantics></math> in pyroCb for aerosol concentrations: <math display="inline"><semantics> <mrow> <mi>N</mi> <mo>=</mo> </mrow> </semantics></math> 1000 cm<sup>−3</sup> (<b>a1</b>–<b>c1</b>) and 5000 cm<sup>−3</sup> (<b>a2</b>–<b>c2</b>) in the presence of wind shear.</p>
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<p>Variations in surface charge density <math display="inline"><semantics> <mi>σ</mi> </semantics></math> in pyroCb for aerosol concentrations: <math display="inline"><semantics> <mrow> <mi>N</mi> <mo>=</mo> </mrow> </semantics></math> 10,000 cm<sup>−3</sup> (<b>a1</b>–<b>c1</b>) and 20,000 cm<sup>−3</sup> (<b>a2</b>–<b>c2</b>).</p>
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18 pages, 6144 KiB  
Article
The Machine Learning Attribution of Quasi-Decadal Precipitation and Temperature Extremes in Southeastern Australia during the 1971–2022 Period
by Milton Speer, Joshua Hartigan and Lance Leslie
Climate 2024, 12(5), 75; https://doi.org/10.3390/cli12050075 - 17 May 2024
Cited by 1 | Viewed by 1779
Abstract
Much of eastern and southeastern Australia (SEAUS) suffered from historic flooding, heat waves, and drought during the quasi-decadal 2010–2022 period, similar to that experienced globally. During the double La Niña of the 2010–2012 period, SEAUS experienced record rainfall totals. Then, severe [...] Read more.
Much of eastern and southeastern Australia (SEAUS) suffered from historic flooding, heat waves, and drought during the quasi-decadal 2010–2022 period, similar to that experienced globally. During the double La Niña of the 2010–2012 period, SEAUS experienced record rainfall totals. Then, severe drought, heat waves, and associated bushfires from 2013 to 2019 affected most of SEAUS, briefly punctuated by record rainfall over parts of inland SEAUS in the late winter/spring of 2016, which was linked to a strong negative Indian Ocean Dipole. Finally, from 2020 to 2022 a rare triple La Niña generated widespread extreme rainfall and flooding in SEAUS, resulting in massive property and environmental damage. To identify the key drivers of the 2010–2022 period’s precipitation and temperature extremes due to accelerated global warming (GW), since the early 1990s, machine learning attribution has been applied to data at eight sites that are representative of SEAUS. Machine learning attribution detection was applied to the 52-year period of 1971–2022 and to the successive 26-year sub-periods of 1971–1996 and 1997–2022. The attributes for the 1997–2022 period, which includes the quasi-decadal period of 2010–2022, revealed key contributors to the extremes of the 2010–2022 period. Finally, some drivers of extreme precipitation and temperature events are linked to significant changes in both global and local tropospheric circulation. Full article
(This article belongs to the Special Issue Addressing Climate Change with Artificial Intelligence Methods)
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Figure 1
<p>A map of <b>SEAUS</b> showing the locations of eight Australian Bureau of Meteorology stations with complete records of precipitation and temperature used in the study period (bold) (<a href="http://www.bom.gov.au/climate/data/" target="_blank">http://www.bom.gov.au/climate/data/</a> accessed on 1 April 2024). The four states, namely Queensland, New South Wales, Victoria, and Tasmania, are also delineated. Other locations mentioned in the text are also marked (italics).</p>
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<p>(<b>a</b>) Australian rainfall deciles from 1 January 2017 to 31 December 2019; <a href="http://www.bom.gov.au/climate/maps/rainfall" target="_blank">http://www.bom.gov.au/climate/maps/rainfall</a> (accessed on 1 April 2024) (<b>b</b>) Australian rainfall deciles from 1 September 2019 to 31 August 2023; <a href="http://www.bom.gov.au/climate/maps/rainfall" target="_blank">http://www.bom.gov.au/climate/maps/rainfall</a> (accessed on 1 April 2024).</p>
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<p>(<b>a</b>) Australian rainfall deciles from 1 January 2017 to 31 December 2019; <a href="http://www.bom.gov.au/climate/maps/rainfall" target="_blank">http://www.bom.gov.au/climate/maps/rainfall</a> (accessed on 1 April 2024) (<b>b</b>) Australian rainfall deciles from 1 September 2019 to 31 August 2023; <a href="http://www.bom.gov.au/climate/maps/rainfall" target="_blank">http://www.bom.gov.au/climate/maps/rainfall</a> (accessed on 1 April 2024).</p>
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<p>The total precipitation and mean TMax time series for the 8 stations in <b>SEAUS</b> in the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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<p>The total precipitation and mean TMax time series for the 8 stations in <b>SEAUS</b> in the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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<p>The total precipitation and mean TMax time series for the 4 stations in <b>N</b> in the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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<p>The total precipitation and mean TMax time series for the 4 stations in <b>N</b> in the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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<p>The total precipitation and mean TMax time series for the 4 stations in <b>S</b> over the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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<p>The total precipitation and mean TMax time series for the 4 stations in <b>S</b> over the 1970–2022 period (<b>a</b>–<b>h</b>). The horizontal dashed lines indicate the 5th and 95th percentiles (red); 10th and 90th percentiles (orange); 15th and 85th percentiles (light green); 20th and 80th percentiles (brown); and 25th and 75th percentiles (dark blue). The horizontal solid black line is the median.</p>
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14 pages, 245 KiB  
Article
Climate Change in Rural Australia: Natural Hazard Preparedness and Recovery Needs of a Rural Community
by Caitlin E. Pike, Amy D. Lykins, Warren Bartik, Phillip J. Tully and Suzanne M. Cosh
Climate 2024, 12(5), 57; https://doi.org/10.3390/cli12050057 - 23 Apr 2024
Viewed by 1938
Abstract
Climate change has resulted in a worldwide increase in intensity and frequency of extreme weather events including bushfires. Previous research has shown that communities often do not engage in disaster preparedness, even when sufficient education and resources are provided. With the projected increase [...] Read more.
Climate change has resulted in a worldwide increase in intensity and frequency of extreme weather events including bushfires. Previous research has shown that communities often do not engage in disaster preparedness, even when sufficient education and resources are provided. With the projected increase in natural disasters, preparedness is paramount, and more research is needed to gain an understanding into what impacts community preparedness in the face of climate change. This study investigated one rural Australian community’s preparedness for the 2019–2020 bushfires. Thirteen Australian adults who resided within a small rural community in New South Wales during the 2019–2020 bushfires participated in semi-structured interviews. Data were analysed using inductive thematic analysis. Participants reported being unprepared for the 2019–2020 bushfires and that the community has started to prepare for future bushfires. However, they also described a belief in ‘climate cycles’ rather than climate change, limiting engagement in preparedness for future hazards. Participants also reported that they did not talk about the 2019–2020 bushfires, although described experiencing residual anxiety. Recommendations included support needed for rural communities to help with future preparedness efforts and mental health symptoms. Full article
(This article belongs to the Special Issue Recent Climate Change Impacts in Australia)
16 pages, 3619 KiB  
Article
Severe and Short Interval Fires Rearrange Dry Forest Fuel Arrays in South-Eastern Australia
by Christopher E. Gordon, Rachael H. Nolan, Matthias M. Boer, Eli R. Bendall, Jane S. Williamson, Owen F. Price, Belinda J. Kenny, Jennifer E. Taylor, Andrew J. Denham and Ross A. Bradstock
Fire 2024, 7(4), 130; https://doi.org/10.3390/fire7040130 - 10 Apr 2024
Viewed by 1530
Abstract
Fire regimes have shaped extant vegetation communities, and subsequently fuel arrays, in fire-prone landscapes. Understanding how resilient fuel arrays are to fire regime attributes will be key for future fire management actions, given global fire regime shifts. We use a network of 63-field [...] Read more.
Fire regimes have shaped extant vegetation communities, and subsequently fuel arrays, in fire-prone landscapes. Understanding how resilient fuel arrays are to fire regime attributes will be key for future fire management actions, given global fire regime shifts. We use a network of 63-field sites across the Sydney Basin Bioregion (Australia) to quantify how fire interval (short: last three fires <10 years apart, long: last two fires >10 years apart) and severity (low: understorey canopy scorched, high: understorey and overstorey canopy scorched), impacted fuel attribute values 2.5 years after Australia’s 2019–2020 Black Summer fires. Tree bark fuel hazard, herbaceous (near-surface fuels; grasses, sedges <50 cm height) fuel hazard, and ground litter (surface fuels) fuel cover and load were higher in areas burned by low- rather than high-severity fire. Conversely, midstorey (elevated fuels: shrubs, trees 50 cm–200 m in height) fuel cover and hazard were higher in areas burned by high- rather than low-severity fire. Elevated fuel cover, vertical connectivity, height and fuel hazard were also higher at long rather than short fire intervals. Our results provide strong evidence that fire regimes rearrange fuel arrays in the years following fire, which suggests that future fire regime shifts may alter fuel states, with important implications for fuel and fire management. Full article
(This article belongs to the Special Issue Understanding Heterogeneity in Wildland Fuels)
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Figure 1

Figure 1
<p>(<b>a</b>) Map of the study area in the Sydney Basin Bioregion showing the location of 63 sites (points) where fuel recovery was assessed following the 2019–2020 Black Summer fires. Field sites were stratified by fire interval (long, short) and fire severity (understorey: low, moderate; overstorey fire: high, extreme), indicated in the underlying map. (<b>b</b>) Map shows the location of the Sydney Basin Bioregion (grey polygon) in south-east Australia.</p>
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<p>Associations of fire interval and/or severity to: (<b>a</b>) surface fuel load, (<b>b</b>) surface fuel cover, (<b>c</b>) elevated fuel cover, (<b>d</b>) elevated fuel vertical connectivity, (<b>e</b>) elevated mean maximum fuel height, (<b>f</b>) near-surface and elevated fuel vertical connectivity, and (<b>g</b>) dead and live tree canopy cover. Only significant associations from <a href="#fire-07-00130-t001" class="html-table">Table 1</a> are shown. Violin plots show the range (height) and density (width) of transect-level data and the 25th, 50th and 75th percentiles are shown as horizontal lines. For (<b>a</b>), the dashed line shows fuel load predictions made using the Olson curve.</p>
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<p>Associations between fire severity and (<b>a</b>) near-surface, (<b>c</b>) elevated and (<b>d</b>) bark fuel hazard and fire interval and (<b>b</b>) elevated fuel hazard. For (<b>a</b>–<b>c</b>), L: low, M: medium, H: high, VH.E: very high or extreme. For (<b>d</b>), L: low, M: medium, H.VH: high or very high. Only significant associations from <a href="#fire-07-00130-t001" class="html-table">Table 1</a> are shown. Bar plots show the percentage of field sites falling within fuel hazard score groups.</p>
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<p>Hypothesised state-and-transition model describing how fire regime shifts may impact dry forest fuel states in south-eastern Australia. Low- or high-severity fire differently impacts fuel states in the years following fire (pathway ab; solid lines; low = blue fill, high = red fill), with high-severity fire promoting denser midstorey fuel load/connectivity due to fire-stimulated shrub seed/bud regeneration, and sparser litter and herb fuel load/connectivity due to fuel consumption. Fuel arrays return to pre-fire states given long fire return intervals owing to shrub maturation and tree canopy regrowth (pathway a; solid lines; green fill), irrespective of fire severity. However, fuel arrays transition to a more open state given multiple high- or low-severity short-interval fires (pathway b; dashed lines; yellow fill). This is because short-interval fire kills shrubs before maturation, depleting seed/bud banks and regeneration vigour. Herbaceous fuel load/connectivity may then increase due to competitive release and herb resilience to short-interval fire. The recurrence of long- or short-interval fire determines fuel states, with intermediate states present when recurrent short-interval fires are followed by long-interval fire.</p>
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<p>A schematic showing the field plot design. Fieldwork was conducted within a 50 m × 40 m plot, with subplots (SP), transects (T), quadrats (Q) and sub-quadrats (SQ) nested within plots. Different fuel attributes were sampled (Sampled) within each plot, subplot, transect, quadrat, and sub-quadrat.</p>
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30 pages, 6582 KiB  
Article
Trends in Rescue and Rehabilitation of Marsupials Surviving the Australian 2019–2020 Bushfires
by Holly R. Cope, Clare McArthur, Rachael Gray, Thomas M. Newsome, Christopher R. Dickman, Aditi Sriram, Ron Haering and Catherine A. Herbert
Animals 2024, 14(7), 1019; https://doi.org/10.3390/ani14071019 - 27 Mar 2024
Viewed by 2706
Abstract
The 2019–2020 Australian bushfire season had a devastating impact on native wildlife. It was estimated that 3 billion native animals were impacted by the fires, yet there are few estimates of the number of animals that were rescued and rehabilitated post-fire. Focusing on [...] Read more.
The 2019–2020 Australian bushfire season had a devastating impact on native wildlife. It was estimated that 3 billion native animals were impacted by the fires, yet there are few estimates of the number of animals that were rescued and rehabilitated post-fire. Focusing on the state of New South Wales (NSW) and Kangaroo Island, South Australia, we used a case study approach to determine the number of marsupials that were reported rescued due to the 2019–2020 bushfires in these areas and analysed species-specific trends in rescue and release success. In NSW, we found 889 reports of fire-affected marsupials in 2019–2020, mostly comprising kangaroos and wallabies (macropods; n = 458), koalas (n = 204), and possums (n = 162), with a smaller number of wombats (n = 43) and other marsupial species. Most reports of fire-affected marsupials occurred 6–8 weeks after fire ignition, and there was no difference in temporal frequency of rescues between marsupial groups. For the three main groups, the probability of survival and subsequent release differed, with macropods having the lowest probability of release after rescue (0.15 ± 0.04) compared to koalas (0.47 ± 0.04) and possums (0.55 ± 0.10). The type of injury was the main predictor of survival during rehabilitation for all three marsupial groups, with those malnourished/moribund or with traumatic injuries less likely to survive rehabilitation. Death or euthanasia occurred on the day of rescue for 77% of macropods, 48% of possums and 15% of koalas. Koalas most often died during rehabilitation rather than on the day of rescue, with 73% either dying or being euthanised between day 1 and 30 post-rescue, representing a potential welfare concern. On Kangaroo Island, koalas were the most frequently rescued marsupial species; most euthanasia cases and deaths occurred in a hospital, whereas other marsupials were mostly euthanised at triage. In both jurisdictions, koalas were over-represented while possums were under-represented relative to baseline population densities and wildlife rescue trends in the years before the 2019–2020 bushfires. These species differences in presentation post-fire warrant further investigation, as do the differences in triage, survival and release outcomes. It is hypothesised that the high intensity and large scale of the 2019–2020 fires impeded marsupial fire evasion tactics, as evidenced by the small number of animals found for rescue, and the differing rates of presentation relative to underlying population densities for the main marsupial groups. Based on our findings, there is a need for detailed record keeping and data sharing, development of consistent and evidence-based triage, treatment and euthanasia guidelines and deployment of trained wildlife emergency rescue teams with advanced search techniques to minimise animal suffering where safe to do so. Full article
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Figure 1
<p>Marsupial group as a proportion (%) of (<b>a</b>) all marsupial records and (<b>b</b>) fire-affected marsupial records for the years 2015/16–2018/19 (blue columns; <span class="html-italic">n</span> = 125,439 for all records; <span class="html-italic">n</span> = 235 for fire records) and 2019/20 (red columns; <span class="html-italic">n</span> = 37,076 for all records; <span class="html-italic">n</span> = 889 for fire records). Record counts (<span class="html-italic">n</span>) are presented above columns for each taxonomic group.</p>
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<p>Fate as a proportion (%) of (<b>a</b>) all marsupial records and (<b>b</b>) fire-affected marsupial records in 2015/16–2018/19 (blue columns) and 2019/20 (red columns). Record counts (<span class="html-italic">n</span>) are presented above columns. The fate of “In care” indicates that the animal was still in care at the time of reporting, and the fate of “Dead on arrival” indicates that the animal died between the time it was reported and when a rescuer arrived.</p>
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<p>Mean ± 95% CI probability of release (0 = euthanised/died in care, 1 = released/relocated) of fire-affected marsupials in 2019/20 for koalas, macropods, and possums and gliders, by injury type. Superscript letters indicate injury types for each marsupial group that are significantly different based on pairwise comparisons.</p>
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<p>Number of fire-affected marsupial rescue records in 2015/16–2018/19 and 2019/20 for koalas, possums and macropods by sex (<b>a</b>, <b>b</b> and <b>c</b>, respectively) and by age (<b>d</b>, <b>e</b> and <b>f</b>, respectively). The data for the period 2015/16–2018/19 are presented as yearly mean ± SD, while the data for the year 2019/20 are absolute numbers. LR chi-squared analyses are testing for an overall difference in proportions of ages (where no change occurred between years), and chi-squared analyses are testing for a change in relative proportions of sexes between years.</p>
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<p>Cumulative number of koalas, macropods, and possums rescued due to fires in 2019/20 (<span class="html-italic">n</span> = 480 with accurate dates of rescue and fire ignition, excluding those found dead) over 12 months following ignition of the fire at the relevant rescue location. Cumulative <span class="html-italic">n</span> values are presented above each line.</p>
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<p>Mean ± 95% CI length of stay (days) of fire-affected koalas, macropods, and possums and gliders that were (<b>a</b>) released or relocated (<span class="html-italic">n</span> = 183) and (<b>b</b>) died or euthanised in rehabilitation after rescue (<span class="html-italic">n</span> = 369) in 2019/20. Note the different scales on the <span class="html-italic">y</span>-axis between figure (<b>a</b>,<b>b</b>). Marsupial groups with significantly different lengths of stay are denoted with different superscript letters (a or b) at <span class="html-italic">p</span> ≤ 0.001.</p>
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<p>Mean ± 95% CI length of stay (days) relative to significant predictor variables for fire-affected marsupial groups released/relocated in 2019/20: (<b>a</b>) macropods by injury type, (<b>b</b>) koalas by fire severity, (<b>c</b>) koalas by injury type, and (<b>d</b>) possums and gliders by injury type that were. Note: The 95% CI for koala injury type malnourished/moribund was wide [−763 and 902] and is not displayed. Superscript letters denote significant differences between categorical variables as determined using pairwise comparisons.</p>
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<p>Length of stay (days) for fire-affected macropods and koalas that died or were euthanised in rehabilitation after rescue in 2019/20 relative to the significant predictor variables outlined in <a href="#animals-14-01019-t003" class="html-table">Table 3</a>. Macropod mean (±95% CI) length of stay (days) versus (<b>a</b>) injury type and (<b>b</b>) age. Superscript letters denote significant differences between categorical variables as determined using pairwise comparisons.</p>
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<p>Location of rescue due to 2019–2020 bushfires for (<b>a</b>) macropods, (<b>b</b>) possums and gliders, (<b>c</b>) koalas and (<b>d</b>) wombats.</p>
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<p>Number of records for possums, macropods and koalas in each of four main IBRA regions (NSW North Coast, South East Corner, South Eastern Highlands, Sydney Basin) with any cause for rescue (all records) and fire-affected animals (fire records) across the years preceding the 2019–2020 bushfires in eastern Australia (2015/16–2018/19; blue columns) and the year of the 2019–2020 bushfires (2019/20; red columns). Density estimates for possums, macropods and koalas are annotated down the centre of the chart (per ha); macropod and possum densities were extracted from van Eeden et al. [<a href="#B4-animals-14-01019" class="html-bibr">4</a>]; koala densities were calculated as mean population size from Adams-Hosking et al. [<a href="#B38-animals-14-01019" class="html-bibr">38</a>] over IBRA size (ha) from DAWE [<a href="#B41-animals-14-01019" class="html-bibr">41</a>].</p>
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<p>Wildlife rescue records in NSW between 2015/16 and 2019/20 for all species and for marsupials alone. Data sourced from NSW Wildlife Rehabilitation dashboard [<a href="#B29-animals-14-01019" class="html-bibr">29</a>].</p>
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