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Search Results (894)

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10 pages, 279 KiB  
Editorial
Natural and Human Impacts on Coastal Areas
by Francisco Asensio-Montesinos, Rosa Molina, Giorgio Anfuso, Giorgio Manno and Carlo Lo Re
J. Mar. Sci. Eng. 2024, 12(11), 2017; https://doi.org/10.3390/jmse12112017 - 8 Nov 2024
Viewed by 358
Abstract
Coasts are the most densely populated regions in the world and are vulnerable to different natural and human factors, e.g., sea-level rise, coastal accretion and erosion processes, the intensification of sea storms and hurricanes, the presence of marine litter, chronic pollution and beach [...] Read more.
Coasts are the most densely populated regions in the world and are vulnerable to different natural and human factors, e.g., sea-level rise, coastal accretion and erosion processes, the intensification of sea storms and hurricanes, the presence of marine litter, chronic pollution and beach oil spill accidents, etc. Although coastal zones have been affected by local anthropic activities for decades, their impacts on coastal ecosystems is often unclear. Several papers are presented in this Special Issue detailing the interactions between natural processes and human impacts in coastal ecosystems all around the world. A better understanding of such natural and human impacts is therefore of great relevance to confidently predict their negative effects on coastal areas and thus promote different conservation strategies. The implementation of adequate management measures will help coastal communities adapt to future scenarios in the short and long term and prevent damage due to different pollution types, e.g., beach oil spill accidents, through the establishment of Environmental Sensitivity Maps. Full article
(This article belongs to the Special Issue Natural and Human Impacts in Coastal Areas)
33 pages, 9390 KiB  
Article
Seasonality and Predictability of Hydrometeorological and Water Chemistry Indicators in Three Coastal Forested Watersheds
by Andrzej Wałęga, Devendra M. Amatya, Carl Trettin, Timothy Callahan, Dariusz Młyński and Vijay Vulava
Sustainability 2024, 16(22), 9756; https://doi.org/10.3390/su16229756 - 8 Nov 2024
Viewed by 499
Abstract
Forests are recognized for sustaining good water chemistry within landscapes. This study focuses on the water chemistry parameters and their hydrological predictability and seasonality (as a component of predictability) in watersheds of varying scales, with and without human (forest management) activities on them, [...] Read more.
Forests are recognized for sustaining good water chemistry within landscapes. This study focuses on the water chemistry parameters and their hydrological predictability and seasonality (as a component of predictability) in watersheds of varying scales, with and without human (forest management) activities on them, using Colwell indicators for data collected during 2011–2019. The research was conducted in three forested watersheds located at the US Forest Service Santee Experimental Forest in South Carolina USA. The analysis revealed statistically significant (α = 0.05) differences between seasons for stream flow, water table elevation (WTE), and all water chemistry indicators in the examined watersheds for the post-Hurricane Joaquin period (2015–2019), compared to the 2011–2014 period. WTE and flow were identified as having the greatest influence on nitrogen concentrations. During extreme precipitations events, such as hurricanes or tropical storms, increases in WTE and flow led to a decrease in the concentrations of total dissolved nitrogen (TDN), NH4-N, and NO3-N+NO2-N, likely due to dilution. Colwell indicators demonstrated higher predictability (P) for most hydrologic and water chemistry indicators in the 2011–2014 period compared to 2015–2019, indicating an increase in the seasonality component compared to constancy (C), with a larger decrease in C/P for 2015–2019 compared to 2011–2014. The analysis further highlighted the influence of extreme hydrometeorological events on the changing predictability of hydrology and water chemistry indicators in forested streams. The results demonstrate the influence of hurricanes on hydrological behavior in forested watersheds and, thus, the seasonality and predictability of water chemistry variables within and emanating out of the watershed, potentially influencing the downstream ecosystem. The findings of this study can inform forest watershed management in response to natural or anthropogenic disturbances. Full article
(This article belongs to the Section Sustainable Water Management)
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<p>Location map of study watersheds WS77 (treatment) and WS80 (control) in the paired system and WS78 watershed, all within Francis Marion National Forest in coastal South Carolina.</p>
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<p>Response of (<b>A</b>) flow to precipitation, (<b>B</b>) water table elevation (WTE), (<b>C</b>) concentrations of TDN, TDP, NO<sub>3</sub>-N+NO<sub>2</sub>-N, and NH<sub>4</sub>-N, and (<b>D</b>) loads of biogenic compounds for the WS80 during event 23 September–9 October 2015.</p>
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<p>Response of (<b>A</b>) flow to precipitation, (<b>B</b>) water table elevation (WTE), (<b>C</b>) concentrations of TDN, TDP, NO<sub>3</sub>-N+NO<sub>2</sub>-N, and NH<sub>4</sub>-N, and (<b>D</b>) loads of biogenic compounds for the WS78 during event 23 September–9 October 2015.</p>
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<p>Relationships between observed average daily hydrological indicators: (<b>A</b>) flow, (<b>B</b>) precipitation, (<b>C</b>) WTE, and (<b>D</b>) PET and water chemistry indicators: (<b>E</b>) TDN, (<b>F</b>) TDP, (<b>G</b>) NH<sub>4</sub>-N, and (<b>H</b>) NO<sub>3</sub>-N by seasons for two periods in WS80: Period A—2011–2014, Period B—2015–2019, vertical lines represent standard deviations.</p>
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<p>Relationships between observed average seasonal hydrological indicators: (<b>A</b>) flow, (<b>B</b>) precipitation, and (<b>C</b>) WTE and water chemistry indicators: (<b>D</b>) TDN, (<b>E</b>) TDP, (<b>F</b>) NH<sub>4</sub>-N, and (<b>G</b>) NO<sub>3</sub>-N by periods in WS77: Period A—2011–2014, Period B—2015–2019, vertical lines represent standard deviations.</p>
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<p>Relationships between observed average seasonal hydrological indicators (<b>A</b>) flow, (<b>B</b>) precipitation, (<b>C</b>) WTE in Rain series, (<b>D</b>) WTE in Lenoir series, (<b>E</b>) WTE in Goldsboro series, (<b>F</b>) WTE in Lynchburg, and (<b>G</b>) WTE in Wahee series and water chemistry indicators: (<b>H</b>) TDN, (<b>I</b>) TDP, (<b>J</b>) NH<sub>4</sub>-N, and (<b>K</b>) NO<sub>3</sub>-N by periods in WS78: Period A—2011–2014, Period B—2015–2019, vertical lines represent standard deviations.</p>
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<p>Daily values of hydrologic and water chemistry indicators in WS80 (control watershed) during the 2011–2019 period.</p>
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<p>Daily values of hydrologic and water chemistry indicators in WS77 (treatment watershed) during the 2011–2019 period.</p>
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<p>Daily values of hydrologic and water chemistry indicators in WS78 (Turkey Creek) during the 2011–2019 period.</p>
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23 pages, 2150 KiB  
Article
Natural Hazards and Climate Change Impacts on Food Security and Rural–Urban Livelihoods in Mozambique—A Bibliometric Analysis and Framework
by Alexander Fekete
Earth 2024, 5(4), 761-783; https://doi.org/10.3390/earth5040040 - 2 Nov 2024
Viewed by 642
Abstract
Mozambique is confronted with numerous risks related to food security and natural disasters. The study conducted a literature review on natural hazards and food security. This can help to identify gaps and further areas of research. A bibliometric analysis was conducted using standardized [...] Read more.
Mozambique is confronted with numerous risks related to food security and natural disasters. The study conducted a literature review on natural hazards and food security. This can help to identify gaps and further areas of research. A bibliometric analysis was conducted using standardized text search terms, and the VOSviewer tool was used to analyze over 7000 scientific articles and cluster over 60,000 keyword co-occurrences. The results show that research on natural hazards for food security needs to be integrated. The priority topic of disasters focuses on specific hazards such as climate change, floods, and hurricanes, which are also linked to demographic and other social variables. More studies on food security, such as droughts, sustainable development, and other human and social conditions, are being conducted. Resilience as an emerging research paradigm needs to be addressed in comparison. One result is an analytical framework on impacts on food security in the context of disaster risk, based on the empirical findings of the literature review. It shows how everyday risks such as disease or food security can be conceptually better linked to natural hazards and resilience. It shows that further research is needed on the interlinkages of multiple risks, of which Mozambique is an outstanding example. The methodology presented is also applied to provide a framework for linking multiple risks to food security and natural hazards. The innovative dimension of the research is that this inquiry constitutes one of the pioneering attempts to conduct a bibliometric analysis of the linkages between natural hazards, food security, and resilience in Mozambique. Another noteworthy contribution is introducing a novel analytical framework that integrates food security and disaster risks. Full article
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<p>All files with 22,643 keywords; 100 overall, meeting the threshold of minimum occurrence of 90; selection only of those keywords analyzed in the tables.</p>
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<p>Analytical framework on food security drivers, settings, conditions, and impacts in the context of disaster risk.</p>
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<p>Sankey diagram with relations and weighting factors for food security drivers on the left and impacts on the right, in the context of disaster risk and resilience.</p>
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21 pages, 15242 KiB  
Article
Assessment of a Tropical Transition over the Southwestern South Atlantic Ocean: The Case of Cyclone Akará
by Michelle Simões Reboita, Natan Chrysostomo de Oliveira Nogueira, Isabelly Bianca dos Santos Gomes, Lucas Lemos da Cunha Palma and Rosmeri Porfírio da Rocha
J. Mar. Sci. Eng. 2024, 12(11), 1934; https://doi.org/10.3390/jmse12111934 - 29 Oct 2024
Viewed by 636
Abstract
Tropical cyclones are rare in the South Atlantic Ocean. Hurricane Catarina (2004), developed from a tropical transition, was the first documented case, followed by Iba (2019), which had a purely tropical genesis. In February 2024, the southeastern South Atlantic recorded its third tropical [...] Read more.
Tropical cyclones are rare in the South Atlantic Ocean. Hurricane Catarina (2004), developed from a tropical transition, was the first documented case, followed by Iba (2019), which had a purely tropical genesis. In February 2024, the southeastern South Atlantic recorded its third tropical cyclone, Akará, initially a subtropical system. Due to the specific conditions required for tropical cyclones to develop in this ocean basin, the main purpose of this study is to describe the physical mechanisms that triggered the genesis of Akará’s precursor and its tropical transition. Data from various sources and methodologies, including the cyclone phase space diagram, are used in this study. Results show that the passage of a cold front created an environment with horizontal wind shear, contributing to most of the cyclonic relative vorticity in the genesis region. This was the primary driver of cyclogenesis at 1200 UTC on 15 February, along with other secondary processes. The tropical transition occurred as the vertical shear weakened, and turbulent heat fluxes from the ocean to the atmosphere increased, enhancing diabatic processes that warmed the atmosphere. This led to the tropical transition at 0600 UTC on 17 February. Full article
(This article belongs to the Special Issue Latest Advances in Physical Oceanography—2nd Edition)
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<p>Study area, cyclone track (black line with reddish markers indicates the mean sea level pressure (hPa) at the cyclone center every 6 h), and accumulated precipitation (mm, shaded) during the cyclone’s lifecycle (from 1200 UTC 15 February to 0000 UTC 23 February 2024).</p>
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<p>CPS from 1200 UTC on February 15 to 0000 UTC on 23 February 2024. (<b>a</b>) Diagram for B × the −|V<sub>T</sub><sup>L</sup>| and (<b>b</b>) for −|V<sub>T</sub><sup>U</sup>| × −|V<sub>T</sub><sup>L</sup>|. The green dashed line marks the area of the CPS indicative of subtropical cyclones over the South Atlantic Ocean, the black dashed line indicates the area for tropical cyclones using the classic approach, and the red dashed line represents the area for moderately warm core tropical cyclones. This latter overlaps with the other two areas in the −|V<sub>T</sub><sup>U</sup>| × −|V<sub>T</sub><sup>L</sup>| diagram (<b>b</b>). The cyclone’s initial position in the diagrams is indicated by a red circle, and the final position by a yellow circle. In (<b>b</b>) the black circles indicate the start and end of the tropical phase using the classic approach.</p>
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<p>Vertical cross-section of the zonal deviation of air temperature (°C) during the cyclone’s lifecycle. Dashed vertical lines indicate when the cyclone has a phase change.</p>
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<p>Mean sea level pressure (hPa; black lines), 1000–500 hPa thickness (red dashed lines [&gt;540 dam], and blue dashed lines [≤540 dam]), wind speed at 250 hPa (&gt;30 m s<sup>−1</sup>, shaded) during the cyclone’s phases: (<b>a</b>) pre-cyclogenesis at 1200 UTC on 14 February, (<b>b</b>) subtropical cyclogenesis at 1200 UTC on February 15, (<b>c</b>) tropical transition at 0600 UTC on February 17, and (<b>d</b>) intense tropical phase at 1800 UTC on 19 February 2024. Letters L and H indicate low and high-pressure systems, respectively. Cold front is indicated with blue color, warm front with red, and occluded front with purple.</p>
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<p>Vertical wind shear between 200 and 850 hPa (m s<sup>−1</sup>; shaded), divergence at 250 hPa (&gt;2 × 10<sup>−5</sup> s<sup>−1</sup>; green lines), and geopotential height at 500 hPa (dam; black lines) during the cyclone’s phases: (<b>a</b>) pre-cyclogenesis at 1200 UTC on 14 February, (<b>b</b>) subtropical cyclogenesis at 1200 UTC on February 15, (<b>c</b>) tropical transition at 0600 UTC on 17 February, and (<b>d</b>) intense tropical phase at 1800 UTC on 19 February 2024. L indicates the location of the cyclone center. A cold front is indicated with blue color, warm front with red, and occluded front with purple.</p>
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<p>Geopotential height anomaly at 500 hPa (dam; shaded) using the climatology of 2004–2023, and geopotential height (dam; black lines) during the cyclone’s phases: (<b>a</b>) pre-cyclogenesis at 1200 UTC on 14 February, (<b>b</b>) subtropical cyclogenesis at 1200 UTC on 15 February, (<b>c</b>) tropical transition at 0600 UTC on February 17, and (<b>d</b>) intense tropical phase at 1800 UTC on 19 February 2024. L indicates the location of the cyclone center.</p>
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<p>(<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) Horizontal wind shear vorticity at 925 hPa (×10<sup>−5</sup> s<sup>−1</sup>, shaded) and 10-m wind (m s<sup>−1</sup>; arrows), and (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) the ratio (%) between the horizontal wind shear vorticity and total relative vorticity at 925 hPa, only for regions where the ratio is negative (cyclonic relative vorticity).</p>
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<p>(<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) Horizontal temperature advection at 850 hPa (10<sup>−5</sup> K s<sup>−1</sup>; shaded) and wind at 850 hPa (m s<sup>−1</sup>, arrows), and (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) vertically integrated moisture flux (kg m<sup>−1</sup> s<sup>−1</sup>, arrows) between 1000 hPa and 200 hPa and its divergence (10<sup>−5</sup> kg m<sup>−2</sup> s<sup>−1</sup>; shaded).</p>
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<p>Brightness temperature at the top of the clouds (°C) from channel 13/GOES-16, and 10-m wind (m s<sup>−1</sup>; arrows in color). The symbol x represents the cyclone’s center. In (<b>a</b>), x shows the region where the cyclogenesis will occur.</p>
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<p>(<b>a</b>) Mean vertical profile of <span class="html-italic">θ<sub>e</sub></span> (K) for the cyclone’s phases: pre-cyclogenesis at 1200 UTC on February 14, subtropical cyclogenesis at 1200 UTC on 15 February, 12 h before the tropical transition at 1800 UTC on 16 February, tropical transition at 0600 UTC on 17 February, and intense tropical phase at 1800 UTC on 19 February 2024. The mean is calculated using a box with borders 1° away from the cyclone’s center. For the pre-cyclogenesis phase, we used the same center position as for the cyclogenesis. (<b>b</b>,<b>c</b>) vertical cross-section of <span class="html-italic">θ<sub>e</sub></span> (K, lines) and relative cyclonic vorticity (×10<sup>−5</sup> s<sup>−1</sup>; shaded) considering the central latitude of the cyclone at 1800 UTC on February 18 and 1200 UTC on 20 February.</p>
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<p>(<b>a</b>) Mininum MSLP (hPa) at the cyclone’s center and maximum 10-m wind speed (m s<sup>−1</sup>). The variables in the other panels correspond to an areal mean within a 2° box around the cyclone’s center. (<b>b</b>) 250–850 hPa vertical shear of the horizontal wind (m s<sup>−1</sup>) and total heat flux (W m<sup>−2</sup>), (<b>c</b>) SST (°C), 2-m air temperature (°C), and vertical temperature gradient (SST–T<sub>2m</sub>), and (<b>d</b>) vertically integrated moisture flux divergence (10<sup>−5</sup> kg m<sup>−2</sup> s<sup>−1</sup>; negative signal indicates convergence). Vertical lines mark the cyclone’s phases: subtropical, tropical, and subtropical. The first vertical line corresponds to the tropical transition (0600 UTC on 17 February), and the second to the subtropical transition (1200 UTC on February 21).</p>
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21 pages, 7085 KiB  
Article
Space-Based Mapping of Pre- and Post-Hurricane Mangrove Canopy Heights Using Machine Learning with Multi-Sensor Observations
by Boya Zhang, Daniel Gann, Shimon Wdowinski, Chaohao Lin, Erin Hestir, Lukas Lamb-Wotton, Khandker S. Ishtiaq, Kaleb Smith and Yuepeng Li
Remote Sens. 2024, 16(21), 3992; https://doi.org/10.3390/rs16213992 - 28 Oct 2024
Viewed by 733
Abstract
Coastal mangrove forests provide numerous ecosystem services, which can be disrupted by natural disturbances, mainly hurricanes. Canopy height (CH) is a key parameter for estimating carbon storage. Airborne Light Detection and Ranging (LiDAR) is widely viewed as the most accurate method for estimating [...] Read more.
Coastal mangrove forests provide numerous ecosystem services, which can be disrupted by natural disturbances, mainly hurricanes. Canopy height (CH) is a key parameter for estimating carbon storage. Airborne Light Detection and Ranging (LiDAR) is widely viewed as the most accurate method for estimating CH but data are often limited in spatial coverage and are not readily available for rapid impact assessment after hurricane events. Hence, we evaluated the use of systematically acquired space-based Synthetic Aperture Radar (SAR) and optical observations with airborne LiDAR to predict CH across expansive mangrove areas in South Florida that were severely impacted by Category 3 Hurricane Irma in 2017. We used pre- and post-Irma LiDAR-derived canopy height models (CHMs) to train Random Forest regression models that used features of Sentinel-1 SAR time series, Landsat-8 optical, and classified mangrove maps. We evaluated (1) spatial transfer learning to predict regional CH for both time periods and (2) temporal transfer learning coupled with species-specific error correction models to predict post-Irma CH using models trained by pre-Irma data. Model performance of SAR and optical data differed with time period and across height classes. For spatial transfer, SAR data models achieved higher accuracy than optical models for post-Irma, while the opposite was the case for the pre-Irma period. For temporal transfer, SAR models were more accurate for tall trees (>10 m) but optical models were more accurate for short trees. By fusing data of both sensors, spatial and temporal transfer learning achieved the root mean square errors (RMSEs) of 1.9 m and 1.7 m, respectively, for absolute CH. Predicted CH losses were comparable with LiDAR-derived reference values across height and species classes. Spatial and temporal transfer learning techniques applied to readily available spaceborne satellite data can enable conservation managers to assess the impacts of disturbances on regional coastal ecosystems efficiently and within a practical timeframe after a disturbance event. Full article
(This article belongs to the Section Forest Remote Sensing)
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<p>(<b>a</b>) Florida state boundary and Hurricane Irma track. (<b>b</b>) Level 3 mangrove classification map. (<b>c</b>) Level 4 mangrove species classification. (<b>d</b>) The 30 m G-LiHT footprint of pre-Irma CHM. (<b>e</b>–<b>p</b>) Zoom-in views for four representative sites.</p>
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<p>Timeline of pre-Irma (orange lines) and post-Irma (purple lines) observations separated by September 2017 Hurricane Irma (the dark vertical line).</p>
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<p>(<b>a</b>) Flow chart of data filtering. (<b>b</b>) Spatial and temporal transfer learning based on <span class="html-italic">DS2_pre</span> and <span class="html-italic">DS2_post</span> data that are separately used in the spatial transfer but collectively used in the temporal transfer learning. Blue and green rectangles are input variables; white and red rectangles are intermediate products; ovals indicate model processes; pink and orange rectangles are output products.</p>
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<p>(<b>a</b>) Boxplots for the reference pre- and post-Irma CHM from <span class="html-italic">DS2</span> dataset. Red line indicates the median value; the boxes represent the interquartile range between the first quartile (25th percentile) and the third quartile (75th percentile); the whiskers extend from the edges of the box to the smallest and largest values within 1.5 times the interquartile range. (<b>b</b>) Comparison of backscatter time series and optical observations using a representative pixel from each species. For each subplot, darker color represents pre-Irma values and lighter color post-Irma values. CH values are displayed in the last row.</p>
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<p>(<b>a</b>) Scatter plot of predicted and referenced CH for pre- and post-Irma from one of the cross-validation evaluation datasets. The yellow lines mark the least-square linear regression model. “BW” in the legend indicates “buttonwood” species. (<b>b</b>) Mean and standard deviation of variable importance of top ten variables using the mixed feature.</p>
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<p>Scatter plots of prediction error and percentage (Perc) error versus reference CH for both time periods by species. Red lines are the least-squared linear models.</p>
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<p>Predicted CH (<b>a</b>) pre-Irma, (<b>b</b>) post-Irma, and (<b>c</b>) CH loss (positive values indicate losses). (<b>d</b>) Comparison between mean and standard deviation of predicted and reference CH loss from evaluation datasets in cross-validation. Deep color represents predicted values and light color reference values. Missing data are due to no pixel samples. (<b>e</b>) Local maps of CH loss. White circles in (<b>e3</b>) indicate (<b>left</b>) the bank areas and (<b>right</b>) the boundary between white and red mangroves according to <a href="#remotesensing-16-03992-f001" class="html-fig">Figure 1</a>f.</p>
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<p>(<b>a</b>) Scatter plot of predicted and corrected CH versus reference post-Irma CH from a cross-validation dataset. (<b>b</b>) Mean and standard deviation of top ten ranking of variable importance using mixed features.</p>
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<p>(<b>a</b>–<b>l</b>) Local maps of post-Irma CH reference, corrected predictions, and errors. White circle outlines indicate areas with large errors. (<b>m</b>) Comparison of the corrected predictions and reference CH losses across pre-Irma canopy height and species classes. Deep color indicates predicted values and light color reference values.</p>
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<p>(<b>a</b>,<b>b</b>) Pre-Irma CH maps for (<b>a</b>) remake of <a href="#remotesensing-16-03992-f007" class="html-fig">Figure 7</a>a and (<b>b</b>) Figure from Jamaluddin et al. (2024) [<a href="#B32-remotesensing-16-03992" class="html-bibr">32</a>]. (<b>c</b>) Remake of CH loss predictions from <a href="#remotesensing-16-03992-f007" class="html-fig">Figure 7</a>c. (<b>d</b>) CH loss predictions from Lagomasino et al. (2021) [<a href="#B10-remotesensing-16-03992" class="html-bibr">10</a>].</p>
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20 pages, 3250 KiB  
Article
Knowledge, Attitudes, and Practices Related to Mold Remediation Following Hurricane Ida in Southeast Louisiana
by Anne M. Foreman, Amel Omari, Kristin J. Marks, Alyssa N. Troeschel, Emily J. Haas, Susan M. Moore, Ethan Fechter-Leggett, Ju-Hyeong Park, Jean M. Cox-Ganser, Scott A. Damon, Shannon Soileau, Colette Jacob, Arundhati Bakshi, Anna Reilly, Kathleen Aubin, Kate Puszykowski and Ginger L. Chew
Int. J. Environ. Res. Public Health 2024, 21(11), 1412; https://doi.org/10.3390/ijerph21111412 - 25 Oct 2024
Viewed by 401
Abstract
Hurricane Ida, a Category 4 hurricane, made landfall in southern Louisiana in August of 2021, causing widespread wind damage and flooding. The objective of this study was to investigate knowledge, attitudes, and practices related to post-hurricane mold exposure and cleanup among residents and [...] Read more.
Hurricane Ida, a Category 4 hurricane, made landfall in southern Louisiana in August of 2021, causing widespread wind damage and flooding. The objective of this study was to investigate knowledge, attitudes, and practices related to post-hurricane mold exposure and cleanup among residents and workers in areas of Louisiana affected by Hurricane Ida and assess changes in knowledge, attitudes, and practices that have occurred over the past 16 years since Hurricane Katrina. We conducted in-person interviews with 238 residents and 68 mold-remediation workers in areas in and around New Orleans to ask about their mold cleanup knowledge and practices, personal protective equipment use, and risk perceptions related to mold. Knowledge of recommended safety measures increased since the post-Katrina survey but adherence to recommended safety measures did not. Many residents and some workers reported using insufficient personal protective equipment when cleaning up mold despite awareness of the potential negative health effects of mold exposure. Full article
(This article belongs to the Section Environmental Health)
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<p>Markers indicate survey recruitment sites (<span class="html-italic">n</span> = 17) by type. Hurricane Ida path and range information were obtained from the National Hurricane Center. Three visited work sites are not included on the map to protect the confidentiality of the workers.</p>
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<p>Display of items shown to participants. From the upper left, the items are (1) surgical mask; (2) Dongguan Sengtor Plastics Products Co. KN95 Particulate Disposable Respirator (Dongguan City, Guangdong Province, China); (3) 3M™ 8511 N95 Particulate Disposable Respirator with Valve (Aberdeen, SD, USA); (4) photo of a 3M™ Half Facepiece Respirator with Cartridge; (5) photo of a Honeywell 2760008A Full-Face Respirator; (6) 3M™ 8210 Plus N95 Particulate Disposable Respirator (Aberdeen, SD, USA); (7) cotton cloth face mask; (8) Kyungin Flax KF94 (Incheon, South Korea); (9) polyester neck gaiter; (10) dust mask; (11) cotton bandana; (12) 3M™9205 N95 Particulate Disposable Respirator (Aberdeen, SD, USA).</p>
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18 pages, 10462 KiB  
Article
Multi-Year Hurricane Impacts Across an Urban-to-Industrial Forest Use Gradient
by Carlos Topete-Pozas, Steven P. Norman and William M. Christie
Remote Sens. 2024, 16(20), 3890; https://doi.org/10.3390/rs16203890 - 19 Oct 2024
Viewed by 615
Abstract
Coastal forests in the eastern United States are increasingly threatened by hurricanes; however, monitoring their initial impacts and subsequent recovery is challenging across scales. Understanding disturbance impacts and responses is essential for sustainable forest management, biodiversity conservation, and climate change adaptation. Using Sentinel-2 [...] Read more.
Coastal forests in the eastern United States are increasingly threatened by hurricanes; however, monitoring their initial impacts and subsequent recovery is challenging across scales. Understanding disturbance impacts and responses is essential for sustainable forest management, biodiversity conservation, and climate change adaptation. Using Sentinel-2 imagery, we calculated the annual Normalized Difference Vegetation Index change (∆NDVI) of forests before and after Hurricane Michael (HM) in Florida to determine how different forest use types were impacted, including the initial wind damage in 2018 and subsequent recovery or reactive management for two focal areas located near and far from the coast. We used detailed parcel data to define forest use types and characterized multi-year impacts using sampling and k-means clustering. We analyzed five years of timberland logging activity up to the fall of 2023 to identify changes in logging rates that may be attributable to post-hurricane salvage efforts. We found uniform impacts across forest use types near the coast, where winds were the most intense but differences inland. Forest use types showed a wide range of multi-year responses. Urban forests had the fastest 3-year recovery, and the timberland response was delayed, apparently due to salvage logging that increased post-hurricane, peaked in 2021–2022, and returned to the pre-hurricane rate by 2023. The initial and secondary consequences of HM on forests were complex, as they varied across local and landscape gradients. These insights reveal the importance of considering forest use types to understand the resilience of coastal forests in the face of potentially increasing hurricane activity. Full article
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<p>The study area location is in northwestern Florida, USA. The letters on the map indicate focal areas: “A” near and “B” far from the coast.</p>
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<p>Workflow diagram showing the methodological steps for this study.</p>
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<p>Annual ∆NDVI by forest use type near (<b>a</b>) and far (<b>b</b>) from the coast for two years prior to Hurricane Michael, the year of the storm (2018–2019), and for two years after. The boxes represent the 25th and 75th percentiles of each distribution and the lines inside the boxes represent the medians.</p>
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<p>Three-year recovery of forest use types standardized to the pre-HM condition for the coastal focal area (<b>a</b>) and inland focal area (<b>b</b>).</p>
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<p>Patterns of NDVI decline and recovery from spatio-temporal clustering over three years of annual post-hurricane ∆NDVI behavior (2018–2019 to 2020–2021). Note that warmer colors (clusters 1–6) mostly surround the track, indicating stronger declines in NDVI (see corresponding cluster numbers in <a href="#remotesensing-16-03890-f006" class="html-fig">Figure 6</a>): (<b>a</b>) the southwest corner of the study area showing the hurricane track, (<b>b</b>) industrial forests, (<b>c</b>) interface forests (i.e., woodlot, farm-woodlot, and other), and (<b>d</b>) urban forests.</p>
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<p>Relative annual NDVI behavior of the 10 clusters with respect to the immediate pre-storm condition. The cluster numbers and colors in the legend correspond to the clusters shown in <a href="#remotesensing-16-03890-f005" class="html-fig">Figure 5</a>.</p>
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<p>Annual logging for timberland and all other non-urban forest use types within the study area for the pre-hurricane baseline of 2016–2017 and for five subsequent years.</p>
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<p>Classification key used to define forest cover types from forest canopy cover, building density, and parcel data. The same colors are used in <a href="#remotesensing-16-03890-f0A2" class="html-fig">Figure A2</a>.</p>
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<p>Forest cover types derived from forest canopy cover, building density, and parcel data.</p>
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18 pages, 10210 KiB  
Article
A Disparate Disaster: Spatial Patterns of Building Damage Caused by Hurricane Ian and Associated Socio-Economic Factors
by Md Zakaria Salim, Yi Qiang, Barnali Dixon and Jennifer Collins
Remote Sens. 2024, 16(20), 3792; https://doi.org/10.3390/rs16203792 - 12 Oct 2024
Viewed by 653
Abstract
The literature shows that communities under different socio-economic conditions suffer different levels of damage in disasters. In addition to the physical intensity of hazards, such differences are also related to the varying abilities of communities to prepare for and respond to disasters. This [...] Read more.
The literature shows that communities under different socio-economic conditions suffer different levels of damage in disasters. In addition to the physical intensity of hazards, such differences are also related to the varying abilities of communities to prepare for and respond to disasters. This study analyzes the spatial patterns of building damage in Hurricane Ian in 2022 and investigates the socio-economic disparities related to the damage. Specifically, this study employs NASA’s Damage Proxy Map (DPM2) to analyze spatial patterns of building damage caused by the hurricane. Then, it uses statistical analysis to assess the relationships between building damage and hurricane intensity, building conditions, and socio-economic variables at the building and census tract levels. Furthermore, the study applies geographically weighted regression (GWR) to examine the spatial variation of the damage factors. The results provide valuable insights into the potential factors related to building damage and the spatial variation in the factors. The results also reveal the uneven distribution of building damage among different population groups, implying socio-economic inequalities in disaster adaptation and resilience. Moreover, the study provides actionable information for policymakers, emergency responders, and community leaders in formulating strategies to mitigate the impact of future hurricanes by identifying vulnerable communities and population groups. Full article
(This article belongs to the Special Issue Advances in GIS and Remote Sensing Applications in Natural Hazards)
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<p>Study area.</p>
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<p>The analytical workflow.</p>
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<p>Spatial pattern of damage ratios in census tracts.</p>
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<p>Comparative box plot of standardized factors affecting building damage.</p>
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<p>Correlation between damage ratios and all variables.</p>
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<p>Coefficient surfaces of the three hurricane intensity variables: (<b>a</b>) sustained wind speed, (<b>b</b>) distance to the coast, and (<b>c</b>) distance to hurricane track in the GWR models. The colored polygons are census tracts that show a significant relationship (<span class="html-italic">p</span> &lt; 0.05) in the neighborhoods. The color intensity represents the regression coefficient.</p>
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<p>Coefficient surfaces of four independent socio-economic variables: (<b>a</b>) Building_Size; (<b>b</b>) Asian population; (<b>c</b>) elderly population; and (<b>d</b>) children. The colored polygons are census tracts that show a significant relationship (<span class="html-italic">p</span> &lt; 0.05) in the neighborhoods. The color intensity represents the regression coefficient.</p>
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14 pages, 3655 KiB  
Article
Analyzing Public Interest in Geohazards Using Google Trends Data
by Dmitry Erokhin and Nadejda Komendantova
Geosciences 2024, 14(10), 266; https://doi.org/10.3390/geosciences14100266 - 11 Oct 2024
Viewed by 510
Abstract
This study investigates public interest in geological disasters by analyzing Google Trends data from 2023. This research focuses on earthquakes, hurricanes, floods, tornadoes, and tsunamis to understand how search behaviors reflect public awareness and concern. This study identifies temporal and geographical patterns in [...] Read more.
This study investigates public interest in geological disasters by analyzing Google Trends data from 2023. This research focuses on earthquakes, hurricanes, floods, tornadoes, and tsunamis to understand how search behaviors reflect public awareness and concern. This study identifies temporal and geographical patterns in search trends. Key findings reveal that public interest spikes during significant disaster events, such as the February 2023 earthquake in Turkey and Syria and the August 2023 hurricanes in the United States. This study highlights the importance of timely and accurate information dissemination for disaster preparedness and response. Google Trends proves to be a valuable tool for monitoring public interest, offering real-time insights that can enhance disaster management strategies and improve community resilience. This study’s insights are essential for policymakers, disaster management agencies, and educational efforts aimed at mitigating the impacts of natural disasters. Full article
(This article belongs to the Section Natural Hazards)
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<p>“Earthquake” Google Trends global scores in 2023. (In this and the subsequent figures, the vertical axis represents the Google Trends score, while the horizontal axis displays the timeline).</p>
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<p>“Earthquake” Google Trends geographical distribution in 2023. (In this and the subsequent figures, the darker blue color indicates a higher Google Trends score).</p>
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<p>“Hurricane” Google Trends global scores in 2023.</p>
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<p>“Hurricane” Google Trends geographical distribution in 2023.</p>
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<p>“Flood” Google Trends global scores in 2023.</p>
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<p>“Flood” Google Trends geographical distribution in 2023.</p>
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<p>“Tornado” Google Trends global scores in 2023.</p>
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<p>“Tornado” Google Trends geographical distribution in 2023.</p>
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<p>“Tsunami” Google Trends global scores in 2023.</p>
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<p>“Tsunami” Google Trends geographical distribution in 2023.</p>
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<p>Google Trends global scores in 2023 across various geohazards.</p>
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<p>Google Trends geographical distribution in 2023 across various geohazards.</p>
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22 pages, 13312 KiB  
Article
Extracting Wetlands in Coastal Louisiana from the Operational VIIRS and GOES-R Flood Products
by Tianshu Yang, Donglian Sun, Sanmei Li, Satya Kalluri, Lihang Zhou, Sean Helfrich, Meng Yuan, Qingyuan Zhang, William Straka, Viviana Maggioni and Fernando Miralles-Wilhelm
Remote Sens. 2024, 16(20), 3769; https://doi.org/10.3390/rs16203769 - 11 Oct 2024
Viewed by 463
Abstract
Visible Infrared Imaging Radiometer Suite (VIIRS) and Advanced Baseline Imager (GOES-R ABI) flood products have been widely used by the National Weather Service (NWS) for river flood monitoring, and by the Federal Emergency Management Agency (FEMA) for rescue and relief efforts. Some water [...] Read more.
Visible Infrared Imaging Radiometer Suite (VIIRS) and Advanced Baseline Imager (GOES-R ABI) flood products have been widely used by the National Weather Service (NWS) for river flood monitoring, and by the Federal Emergency Management Agency (FEMA) for rescue and relief efforts. Some water bodies, like wetlands, are detected as water but not marked as permanent or normal water, which may result in their misclassification as floodwaters by VIIRS and GOES-R flood products. These water bodies generally do not cause significant property damage or fatalities, but they can complicate the identification of truly hazardous floods. This study utilizes the severe Louisiana flood event caused by Hurricane Ida to demonstrate how to differentiate wetlands from real-hazard flooding. Since Hurricane Ida made landfall in 2021, and there was no major flood event in 2022, VIIRS and ABI flood data from 2021 and 2022 were selected. The difference in annual total flooding days between 2021 and 2022 was calculated and combined with long-time flood frequency to distinguish non-hazard floodwaters due to wetlands identified from real-hazard floods caused by the hurricane. The results were compared with the wetlands from the change detection analysis. The confusion matrix analysis indicated an accuracy of 91.58%, precision of 89.97%, and F1-score of 76.63% for the VIIRS flood products. For the GOES-R ABI flood products, the confusion matrix analysis yielded an accuracy of 86.88%, precision of 97.49%, and F1-score of 75.21%. The accuracy and F1-score values for the GOES-R ABI flood products are slightly lower than those for the VIIRS flood products, possibly due to their lower spatial resolution, but still within a feasible range. Full article
(This article belongs to the Special Issue Big Earth Data for Climate Studies)
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<p>Surface type classification map of the study region (<b>top</b>) and Louisiana’s top 10 wetlands and swamps covering large tracts of the state (<b>bottom</b>). (Photo: JupiterImages/Comstock/Getty Images).</p>
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<p>Data processing and analysis flow chart for this study.</p>
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<p>VIIRS five-day composite flood product for the Louisiana region: before Hurricane Ida (22–26 August 2021) (<b>upper</b>) and after Hurricane Ida (29 August–2 September 2021) (<b>lower</b>).</p>
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<p>VIIRS five-day composite flood product showing wetlands in the Louisiana region.</p>
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<p>VIIRS five-day composite flood product highlighting the identified wetlands in the Louisiana region.</p>
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<p>Map illustrating the confusion matrix analysis: flood map with the identified wetland mask (<b>upper</b>), and VIIRS five-day composite flood map showing wetlands (<b>lower</b>).</p>
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<p>Sample for confusion matrix analysis: flood map showing identified wetlands marked in light blue (<b>left</b>) and flood map indicating wetlands marked in turquoise blue (<b>right</b>).</p>
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<p>GOES-R ABI flood product in the Louisiana coastal region: before Hurricane Ida (25 August 2021) (<b>upper</b>) and after Hurricane Ida (31 August 2021) (<b>lower</b>).</p>
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<p>GOES-R ABI flood product showing pre-event wetlands in the Louisiana coastal region.</p>
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<p>GOES-R ABI flood product with the identified wetlands for the Louisiana coastal region.</p>
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<p>Sample for confusion matrix analysis of GOES-R ABI data: flood map highlighting identified wetlands in light blue (<b>left</b>) and flood map showing wetlands in turquoise blue (<b>right</b>).</p>
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<p>The GFM product Exclusion Mask for 2022 in coastal Louisiana.</p>
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<p>Flood Water Frequency in 2022 for the GFM flood extent product in Louisiana State.</p>
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<p>SAR-based flood mapping of Hurricane Ida flooding using AI by Microsoft.</p>
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13 pages, 870 KiB  
Article
Cancer Treatment Disruption by Residence Region in the Aftermath of Hurricanes Irma and María in Puerto Rico
by Francisco Muñoz-Torres, Marievelisse Soto-Salgado, Karen J. Ortiz-Ortiz, Xavier S. López-León, Yara Sánchez-Cabrera and Vivian Colón-López
Int. J. Environ. Res. Public Health 2024, 21(10), 1334; https://doi.org/10.3390/ijerph21101334 - 8 Oct 2024
Viewed by 931
Abstract
Since 2017, Puerto Rico has faced environmental, economic, and political crises, leading to the emigration of healthcare workers and weakening the healthcare system. These challenges have affected cancer treatment continuity, exacerbating healthcare access challenges island-wide. In this study, we estimate the effect of [...] Read more.
Since 2017, Puerto Rico has faced environmental, economic, and political crises, leading to the emigration of healthcare workers and weakening the healthcare system. These challenges have affected cancer treatment continuity, exacerbating healthcare access challenges island-wide. In this study, we estimate the effect of the residence region on cancer treatment disruption following Hurricanes Irma and María (2017). Telephone surveys were conducted with 241 breast and colorectal cancer patients aged 40 and older who were diagnosed within six months before the hurricanes and were receiving treatment at the time of the hurricanes. Treatment disruption was defined as any pause in surgery, chemotherapy, radiotherapy, or oral treatment due to the hurricanes. Prevalence ratios (PRs) of treatment disruption by residence region were estimated using the San Juan Metropolitan Area (SJMA) as the reference. Fifty-nine percent of respondents reported treatment disruption; among them, half experienced disruptions lasting more than 30 days, with 14% of these enduring disruptions longer than 90 days. Adjusted models showed a 48% higher prevalence of disruption outside the SJMA (PR = 1.48, 95% CI: 1.06–2.07). Specific geographic regions (Arecibo, Bayamón, Caguas, and Mayagüez) exhibited higher disruption prevalence. These findings emphasize the need for disaster preparedness strategies that ensure equitable healthcare access for all cancer patients following environmental calamities. Full article
(This article belongs to the Special Issue Health Emergencies and Disasters Preparedness)
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<p>Case ascertainment protocol for population research to select participants from PRCCR data.</p>
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<p>Cancer treatment disruption and location of hospitals in the Puerto Rico Department of Health Regions.</p>
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23 pages, 6299 KiB  
Article
Impact of Pulse Disturbances on Phytoplankton: How Four Storms of Varying Magnitude, Duration, and Timing Altered Community Responses
by Noah Claflin, Jamie L. Steichen, Darren Henrichs and Antonietta Quigg
Environments 2024, 11(10), 218; https://doi.org/10.3390/environments11100218 - 4 Oct 2024
Viewed by 810
Abstract
Estuarine phytoplankton communities are acclimated to environmental parameters that change seasonally. With climate change, they are having to respond to extreme weather events that create dramatic alterations to ecosystem function(s) on the scale of days. Herein, we examined the short term (<1 month) [...] Read more.
Estuarine phytoplankton communities are acclimated to environmental parameters that change seasonally. With climate change, they are having to respond to extreme weather events that create dramatic alterations to ecosystem function(s) on the scale of days. Herein, we examined the short term (<1 month) shifts in phytoplankton communities associated with four pulse disturbances (Tax Day Flood in 2016, Hurricane Harvey in 2017, Tropical Storm Imelda in 2019, and Winter Storm Uri in 2021) that occurred in Galveston Bay (TX, USA). Water samples collected daily were processed using an Imaging FlowCytobot (IFCB), along with concurrent measurements of temperature, salinity, and chlorophyll-a. Stronger storm events with localized heavy precipitation and flooding had greater impacts on community composition, increasing diversity (Shannon–Weiner and Simpson Indices) while a cold wave event lowered it. Diatoms and dinoflagellates accounted for the largest fraction of the community, cyanobacteria and chlorophytes varied mostly with salinity, while euglenoids, cryptophytes, and raphidophytes, albeit at lower densities, fluctuated greatly. The unconstrained variance of the redundancy analysis models pointed to additional environmental processes than those measured being responsible for the changes observed. These findings provide insights into the impact of pulse disturbances of different magnitudes, durations, and timings on phytoplankton communities. Full article
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<p>Galveston Bay, Texas located in the northwestern Gulf of Mexico. The IFCB samples and water quality data were collected from the marina located on the Texas A&amp;M University at Galveston Campus.</p>
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<p>Relative abundances of the major taxonomic groups pre- and post-major storm events (denoted with a vertical dashed line). Phytoplankton were categorized as diatoms (orange), chlorophytes (dark green), cyanobacteria (blue), dinoflagellates (red), cryptophytes (pink), euglenoids (light green), and raphidophytes (light red) are shown. (<b>a</b>) Tax Day Flood in 2016, (<b>b</b>) Hurricane Harvey in 2017, (<b>c</b>) Tropical Storm Imelda in 2019, and (<b>d</b>) Winter Storm Uri in 2021.</p>
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<p>Redundancy analysis of the major taxonomic groups and significant water quality parameters pre- (green) and post- (blue) storm. Phytoplankton category codes: DIA—diatoms, CHL—chlorophytes, CYA—cyanobacteria, DIN—dinoflagellates, CRY—cryptophytes, EUG—euglenoids, and RAP—raphidophytes. Vector codes: Temp—temperature (°C), Sal—salinity, and Chl—chlorophyll-a (μg/L). (<b>a</b>) Tax Day Flood in 2016, (<b>b</b>) Hurricane Harvey in 2017, (<b>c</b>) Tropical Storm Imelda in 2019, and (<b>d</b>) Winter Storm Uri in 2021. These ellipsoids represent normalized 95% confidence intervals of community composition by multivariate t-distribution (<span class="html-italic">p</span>-value = 0.05).</p>
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<p>Diversity indices calculated for the phytoplankton community pre- (left) and post- (right) major storm events: Tax Day Flood in 2016 (green), Hurricane Harvey in 2017 (blue), Tropical Storm Imelda in 2019 (red), and Winter Storm Uri in 2021 (orange). (<b>a</b>) Species richness, (<b>b</b>) Shannon–Weiner index, (<b>c</b>) Simpson index, and (<b>d</b>) Pielou index.</p>
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<p>Bubble plots were used to examine changes in the abundance of the major phytoplankton categories classified with the IFCB pre- and post-major storm events (denoted with a vertical dashed line). (<b>a</b>) Tax Day Flood in 2016, (<b>b</b>) Hurricane Harvey in 2017, (<b>c</b>) Tropical Storm Imelda in 2019, and (<b>d</b>) Winter Storm Uri in 2021. Bubble size and the continuous color scale represent the abundance (cells mL<sup>−1</sup>) (data no transformed). No bubble was displayed when the abundance was equal to zero. Data is shown as day to day (MM/DD) in the <span class="html-italic">x</span>-axis. A side color bar refers to each major phytoplankton category: diatoms (orange), chlorophytes (dark green), cyanobacteria (blue), dinoflagellates (red), cryptophytes (pink), euglenoids (light green), and raphidophytes (light red).</p>
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<p>Bubble plots were used to examine changes in the abundance of the major phytoplankton categories classified with the IFCB pre- and post-major storm events (denoted with a vertical dashed line). (<b>a</b>) Tax Day Flood in 2016, (<b>b</b>) Hurricane Harvey in 2017, (<b>c</b>) Tropical Storm Imelda in 2019, and (<b>d</b>) Winter Storm Uri in 2021. Bubble size and the continuous color scale represent the abundance (cells mL<sup>−1</sup>) (data no transformed). No bubble was displayed when the abundance was equal to zero. Data is shown as day to day (MM/DD) in the <span class="html-italic">x</span>-axis. A side color bar refers to each major phytoplankton category: diatoms (orange), chlorophytes (dark green), cyanobacteria (blue), dinoflagellates (red), cryptophytes (pink), euglenoids (light green), and raphidophytes (light red).</p>
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<p>Bubble plots were used to examine changes in the abundance of the major phytoplankton categories classified with the IFCB pre- and post-major storm events (denoted with a vertical dashed line). (<b>a</b>) Tax Day Flood in 2016, (<b>b</b>) Hurricane Harvey in 2017, (<b>c</b>) Tropical Storm Imelda in 2019, and (<b>d</b>) Winter Storm Uri in 2021. Bubble size and the continuous color scale represent the abundance (cells mL<sup>−1</sup>) (data no transformed). No bubble was displayed when the abundance was equal to zero. Data is shown as day to day (MM/DD) in the <span class="html-italic">x</span>-axis. A side color bar refers to each major phytoplankton category: diatoms (orange), chlorophytes (dark green), cyanobacteria (blue), dinoflagellates (red), cryptophytes (pink), euglenoids (light green), and raphidophytes (light red).</p>
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24 pages, 3135 KiB  
Review
Current Status of Remote Sensing for Studying the Impacts of Hurricanes on Mangrove Forests in the Coastal United States
by Abhilash Dutta Roy, Daria Agnieszka Karpowicz, Ian Hendy, Stefanie M. Rog, Michael S. Watt, Ruth Reef, Eben North Broadbent, Emma F. Asbridge, Amare Gebrie, Tarig Ali and Midhun Mohan
Remote Sens. 2024, 16(19), 3596; https://doi.org/10.3390/rs16193596 - 26 Sep 2024
Viewed by 1389
Abstract
Hurricane incidents have become increasingly frequent along the coastal United States and have had a negative impact on the mangrove forests and their ecosystem services across the southeastern region. Mangroves play a key role in providing coastal protection during hurricanes by attenuating storm [...] Read more.
Hurricane incidents have become increasingly frequent along the coastal United States and have had a negative impact on the mangrove forests and their ecosystem services across the southeastern region. Mangroves play a key role in providing coastal protection during hurricanes by attenuating storm surges and reducing erosion. However, their resilience is being increasingly compromised due to climate change through sea level rises and the greater intensity of storms. This article examines the role of remote sensing tools in studying the impacts of hurricanes on mangrove forests in the coastal United States. Our results show that various remote sensing tools including satellite imagery, Light detection and ranging (LiDAR) and unmanned aerial vehicles (UAVs) have been used to detect mangrove damage, monitor their recovery and analyze their 3D structural changes. Landsat 8 OLI (14%) has been particularly useful in long-term assessments, followed by Landsat 5 TM (9%) and NASA G-LiHT LiDAR (8%). Random forest (24%) and linear regression (24%) models were the most common modeling techniques, with the former being the most frequently used method for classifying satellite images. Some studies have shown significant mangrove canopy loss after major hurricanes, and damage was seen to vary spatially based on factors such as proximity to oceans, elevation and canopy structure, with taller mangroves typically experiencing greater damage. Recovery rates after hurricane-induced damage also vary, as some areas were seen to show rapid regrowth within months while others remained impacted after many years. The current challenges include capturing fine-scale changes owing to the dearth of remote sensing data with high temporal and spatial resolution. This review provides insights into the current remote sensing applications used in hurricane-prone mangrove habitats and is intended to guide future research directions, inform coastal management strategies and support conservation efforts. Full article
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<p>PRISMA workflow representing the systematic literature review process.</p>
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<p>Applications of remote sensing for studying impacts of hurricanes on mangroves.</p>
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<p>Coastal southeastern United States showing some locations where studies on hurricane impact on mangroves were carried out, that included (<b>A</b>) Everglades National Park, Florida, (<b>B</b>) Florida Keys, (<b>C</b>) Port Fourchon, Louisiana, (<b>D</b>) (Inset): Puerto Rico.</p>
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<p>The regional frequency of remote sensing based peer-reviewed articles published on studying impacts of hurricanes on mangroves in the United States from January 2010 to September 2024.</p>
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<p>Percentage breakdown of sensors used for studying impacts of hurricanes on mangroves in the United States from January 2010 to September 2024.</p>
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<p>Data analysis methods used to study the impacts of hurricanes on mangroves in the United States from January 2010 to September 2024.</p>
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13 pages, 4351 KiB  
Article
Optimizing Wildfire Evacuations through Scenario-Based Simulations with Autonomous Vehicles
by Asad Ali, Mingwei Guo, Salman Ahmad, Ying Huang and Pan Lu
Fire 2024, 7(10), 340; https://doi.org/10.3390/fire7100340 - 26 Sep 2024
Viewed by 899
Abstract
Natural disasters like hurricanes, wildfires, and floods pose immediate hazards. Such events often necessitate prompt emergency evacuations to save lives and reduce fatalities, injuries, and property damage. This study focuses on optimizing wildfire evacuations by analyzing the influence of different transportation infrastructures and [...] Read more.
Natural disasters like hurricanes, wildfires, and floods pose immediate hazards. Such events often necessitate prompt emergency evacuations to save lives and reduce fatalities, injuries, and property damage. This study focuses on optimizing wildfire evacuations by analyzing the influence of different transportation infrastructures and the penetration of autonomous vehicles (AVs) on a historical wildfire event. The methodology involves modeling various evacuation scenarios and incorporating different intersection traffic controls such as roundabouts and stop signs and an evacuation strategy like lane reversal with various AV penetration rates. The analysis results demonstrate that specific interventions on evacuation routes can significantly reduce travel times during evacuations. Additionally, a comparative analysis across different scenarios shows a promising improvement in travel time with a higher level of AV penetration. These findings advocate for the integration of autonomous technologies as a crucial component of future emergency response strategies, demonstrating the potential for broader applications in disaster management. Future studies can expand on these findings by examining the broader implications of integrating AVs in emergency evacuations. Full article
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<p>Evacuation area, Knolls Fire of 2020, Saratoga Springs, Utah.</p>
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<p>Study area map: Saratoga Springs, Utah, United States.</p>
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<p>Traffic control structure in Segment 3.</p>
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<p>Travel times across the different scenarios.</p>
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<p>Typical travel times across the different scenarios (Impact of AV penetration).</p>
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<p>Percentage change in travel time compared to “No Change 0% AV”.</p>
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10 pages, 293 KiB  
Review
Compound Crises: The Impact of Emergencies and Disasters on Mental Health Services in Puerto Rico
by Fernando I. Rivera, Sara Belligoni, Veronica Arroyo Rodriguez, Sophia Chapdelaine, Varun Nannuri and Ashley Steen Burgos
Int. J. Environ. Res. Public Health 2024, 21(10), 1273; https://doi.org/10.3390/ijerph21101273 - 25 Sep 2024
Viewed by 1471
Abstract
Background: Mental health in Puerto Rico is a complex and multifaceted issue that has been shaped by the island’s unique history, culture, and political status. Recent challenges, including disasters, economic hardships, and political turmoil, have significantly affected the mental well-being of the population, [...] Read more.
Background: Mental health in Puerto Rico is a complex and multifaceted issue that has been shaped by the island’s unique history, culture, and political status. Recent challenges, including disasters, economic hardships, and political turmoil, have significantly affected the mental well-being of the population, coupled with the limitations in the accessibility of mental health services. Thus, Puerto Rico has fewer mental health professionals per capita than any other state or territory in the United States. Objective: This comprehensive review examines the impact of disasters on mental health and mental health services in Puerto Rico. Given the exodus of Puerto Ricans from the island, this review also provides an overview of mental health resources available on the island, as well as in the continental United States. This review identifies efforts to address mental health issues, with the intent of gaining a proper understanding of the available mental health services, key trends, as well as observable challenges and achievements within the mental health landscape of the Puerto Rican population. Design: A comprehensive search using the PRIMO database of the University of Central Florida (UCF) library database was conducted, focusing on key terms related to disasters and mental healthcare and services in Puerto Rico. The inclusion criteria encompassed studies on Puerto Rican individuals, both those who remained on the island and those who migrated post-disaster, addressing the mental health outcomes and services for adults and children. We included peer-reviewed articles published from 2005 onwards in English and/or Spanish, examining the impact of disasters on mental health, accessibility of services, and/or trauma-related consequences. Results: In this scoping review, we identified 39 studies addressing the mental health profile of Puerto Ricans, identifying significant gaps in service availability and accessibility and the impact of environmental disasters on mental health. The findings indicate a severe shortage of mental health services in Puerto Rico, exacerbated by disasters such as Hurricanes Irma and Maria, the earthquakes of late 2019 and early 2020 that followed, and the COVID-19 pandemic, resulting in substantial delays in accessing care, and limited insurance coverage, particularly in rural regions. Despite these challenges, efforts to improve mental health services have included substantial federal funding and community initiative aimed at enhancing care availability and infrastructure. Limitations include the use of a single database, language restrictions, and potential variability in data extraction and synthesis. Conclusions: This scoping review highlights the significant impact of disasters on mental health in Puerto Rico and the challenges in accessing mental health services exacerbated by disasters. Despite efforts, significant gaps in mental healthcare and services persist, emphasizing the need for more rigorous research and improvements in infrastructure and workforce to enhance mental health outcomes for Puerto Ricans both on the island and in the continental United States. Full article
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