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17 pages, 4369 KiB  
Article
A Multi-Hazard Approach to Climate Migration: Testing the Intersection of Climate Hazards, Population Change, and Location Desirability from 2000 to 2020
by Zachary M. Hirsch, Jeremy R. Porter, Jasmina M. Buresch, Danielle N. Medgyesi, Evelyn G. Shu and Matthew E. Hauer
Climate 2024, 12(9), 140; https://doi.org/10.3390/cli12090140 - 7 Sep 2024
Viewed by 525
Abstract
Climate change intensifies the frequency and severity of extreme weather events, profoundly altering demographic landscapes globally and within the United States. This study investigates their impact on migration patterns, using propensity score matching and LASSO techniques within a larger regression modeling framework. Here, [...] Read more.
Climate change intensifies the frequency and severity of extreme weather events, profoundly altering demographic landscapes globally and within the United States. This study investigates their impact on migration patterns, using propensity score matching and LASSO techniques within a larger regression modeling framework. Here, we analyze historical population trends in relation to climate risk and exposure metrics for various hazards. Our findings reveal nuanced patterns of climate-induced population change, including “risky growth” areas where economic opportunities mitigate climate risks, sustaining growth in the face of observed exposure; “tipping point” areas where the amenities are slowly giving way to the disamenity of escalating hazards; and “Climate abandonment” areas experiencing exacerbated out-migration from climate risks, compounded by other out-migration market factors. Even within a single county, these patterns vary significantly, underscoring the importance of localized analyses. Projecting population impacts due to climate risk to 2055, flood risks are projected to impact the largest percentage of areas (82.6%), followed by heatwaves (47.4%), drought (46.6%), wildfires (32.7%), wildfire smoke (21.7%), and tropical cyclone winds (11.1%). The results underscore the importance of understanding hyperlocal patterns of risk and change in order to better forecast future patterns. Full article
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Figure 1
<p>Census block group relative population change from years 2000 to 2020 (%).</p>
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<p>County-level projected population change resulting from the combined climate effect over the next 30 years.</p>
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<p>County-level projected population change (%) resulting from the combined climate effect, socioeconomic impact under SSP2, and population redistribution due to climate migration over the next 30 years.</p>
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<p>Population projection trends in Miami-Dade County neighborhoods for areas of continual growth (blue), risky growth with tipping points (gray), and climate abandonment (red).</p>
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<p>Miami-Dade County block groups’ combined climate effect and projected population trend designation (risky growth, tipping point, or climate abandonment area).</p>
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17 pages, 4965 KiB  
Article
Identifying Habitat Productivity Thresholds to Assess the Effects of Drought on a Specialist Folivore
by Ivan Kotzur, Ben D. Moore, Chris Meakin, Maldwyn J. Evans and Kara N. Youngentob
Remote Sens. 2024, 16(17), 3279; https://doi.org/10.3390/rs16173279 - 4 Sep 2024
Viewed by 746
Abstract
Climate change has altered the frequency and severity of extreme weather, which can affect vegetation condition and habitat quality for wildlife. Declines in vegetation productivity during droughts and heatwaves can negatively impact animals that depend on vegetation for water and nutrition. We used [...] Read more.
Climate change has altered the frequency and severity of extreme weather, which can affect vegetation condition and habitat quality for wildlife. Declines in vegetation productivity during droughts and heatwaves can negatively impact animals that depend on vegetation for water and nutrition. We used the normalised difference vegetation index (NDVI) to look at relationships between vegetation productivity and the presence of koalas (Phascolarctos cinereus) in potential habitat throughout much of their range. Using a large, long-term koala presence dataset, we tested the hypothesis that locations where koalas had been observed would exhibit higher NDVI values than a random, representative sample from the same vegetation group. We also identified the minimum NDVI threshold at which koalas occurred across time for each vegetation group and compared these to the minimum NDVI values across potential koala habitat before and during the Millennium Drought, one of the worst recorded in Australia. Additionally, we investigated whether vegetation above the minimum NDVI thresholds was significantly closer to perennial water than unsuitable vegetation. We found that koalas tend to occur at locations with higher NDVI than average for all vegetation groups. Prior to the drought, 49% of potential koala habitat maintained a minimum NDVI above the koalas’ threshold, equating to 190,227 km2, which declined to 166,746 km2 during drought (i.e., a 12% reduction). We also found that unsuitable vegetation tended to occur farther from perennial water than suitable vegetation for some vegetation groups. Areas that remained above the NDVI thresholds during the drought should be considered potential refugia for populations during an event of similar magnitude and could indicate future habitat extent. Full article
(This article belongs to the Section Ecological Remote Sensing)
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Graphical abstract

Graphical abstract
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<p>The study area, covering most of the koala range in eastern Australia (i.e., coloured area). The colours show mean annual precipitation classes (<a href="http://www.bom.gov.au/climate/maps/" target="_blank">http://www.bom.gov.au/climate/maps/</a> [accessed on 17 March 2023]) and shading represent elevation increasing from lighter at sea level to darker at the highest mountains (<a href="https://www.gebco.net/data_and_products/" target="_blank">https://www.gebco.net/data_and_products/</a> [accessed on 17 March 2023]).</p>
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<p>Methodological framework of this study. Dashed box indicates the input datasets. Directional lines indicate steps in the methods and combinations of data to produce results.</p>
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<p>A violin plot of NDVI by vegetation group (colour) and data type (letters and shades): koala site (K, dark) and random landscape location (L, light). <span class="html-italic">n</span> = 4500. The landscape NDVI is random in space, within the respective vegetation group, and paired in time to the koala site NDVI, which is the NDVI value at the time and place of observations from anytime in the study period (1995–2009). The violins are scaled to have the same area. Shown inside the violins are simplified boxplots with a white dot at the median.</p>
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<p>Combined effect size plot of three binomial generalised linear mixed models, one per vegetation group, to determine whether the NDVI is a significant explanatory variable for the differences between where koalas have been observed and random pixels across the koala range within the same vegetation groups. The effect sizes are logarithm odds ratios. The error bars represent 95% confidence intervals with those not crossing zero indicating a significant effect. P-values: woodlands = 3.58 × 10<sup>−5</sup>, open forests = 8.41 × 10<sup>−12</sup>, tall open forests = 2.71 × 10<sup>−12</sup>. <span class="html-italic">n</span> = 4500 (i.e., <span class="html-italic">n</span> = 1500 per vegetation group/model). Models formulation: GLMM = Class ~ NDVI + SpatialCovariance (where class is a koala site or random location and the NDVI is standardised).</p>
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<p>Empirical cumulative distributions of the NDVI in koala sites at the time of observation with the 5th percentile thresholds overlaid as dashed lines (i.e., proportion = 0.05). The colours represent vegetation groups. The cut-off in maximum NDVI = 0.86 is visible, with this threshold used as an upper bound of the data to avoid potential saturation of the NDVI, which is known to occur above this NDVI value for this data type.</p>
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<p>Differences between pre-drought (1995–1999) and drought (2005–2009) periods in the NDVI minimum (5th percentile) of vegetation groups in the landscape. The NDVI minimum is the 5th percentile across time for each pixel. The boxes are interquartile ranges with a median dividing line.</p>
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<p>Maps of potential koala habitat that was (<b>a</b>) above the thresholds in 1995–1999 (pre-drought), (<b>b</b>) potential habitat that had been above thresholds in 1995–1999 that was below thresholds in 2005–2009 (drought).</p>
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<p>A map of potential koala habitat in the Liverpool Range, NSW, that was above (blue) the thresholds in 1995–1999 (pre-drought) and vegetation that had been above in 1995–1999 that was below (red) the thresholds in 2005–2009 (drought). Central coordinate: 150.23443, −31.93875 (coordinate system = EPSG:4326). Basemap is the NSW Imagery dataset, accessed via <a href="https://datasets.seed.nsw.gov.au/dataset/5601b661-3352-47ad-a8e5-09278927226f" target="_blank">https://datasets.seed.nsw.gov.au/dataset/5601b661-3352-47ad-a8e5-09278927226f</a> (accessed 28 May 2024).</p>
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<p>A plot of locations of koala observations across the study area in eastern Australia.</p>
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21 pages, 6877 KiB  
Article
Impacts of Drought and Heatwave on the Vegetation and Ecosystem in the Yangtze River Basin in 2022
by Siyuan Chen, Ruonan Qiu, Yumin Chen, Wei Gong and Ge Han
Remote Sens. 2024, 16(16), 2889; https://doi.org/10.3390/rs16162889 - 7 Aug 2024
Viewed by 928
Abstract
In 2022, a severe drought and heatwave occurred in the middle and lower reaches of the Yangtze River Basin. Previous studies have highlighted the severity of this event, yet the relevance of soil moisture (SM), as well as vapor pressure deficit (VPD) and [...] Read more.
In 2022, a severe drought and heatwave occurred in the middle and lower reaches of the Yangtze River Basin. Previous studies have highlighted the severity of this event, yet the relevance of soil moisture (SM), as well as vapor pressure deficit (VPD) and vegetation damage, remained unclear. Here, we utilized solar-induced chlorophyll fluorescence (SIF) and various flux data to monitor the impact of drought on vegetation and analyze the influence of different environmental factors. The results indicated a severe situation of drought and heatwave in the Yangtze River Basin in 2022 that significantly affected vegetation growth and the ecosystem carbon balance. SIF and NDVI have respective advantages in reflecting damage to vegetation under drought and heatwave conditions; SIF is more capable of capturing the weakening of vegetation photosynthesis, while NDVI can more rapidly indicate vegetation damage. Additionally, the correlation of SM and SIF are comparable to that of VPD and SIF. By contrast, the differentiation in the severity of vegetation damage among different types of vegetation is evident; cropland is more vulnerable compared to forest ecosystems and is more severely affected by drought and heatwave. These findings provided important insights for assessing the impact of compound drought and heatwave events on vegetation growth. Full article
(This article belongs to the Special Issue Remote Sensing Application in the Carbon Flux Modelling)
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Graphical abstract

Graphical abstract
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<p>The Yangtze River Basin. The dark gray lines represent the primary and secondary water systems of the Yangtze River. The base map depicts the land cover type based on data processed from 2019 MCD12Q1 v006. Forest is a collective term encompassing evergreen coniferous forests, evergreen broad-leaved forests, deciduous broad-leaved forests, and mixed forests.</p>
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<p>Spatial distributions of temperature, precipitation, and VPD anomalies in the Yangtze River Basin during July ((<b>a</b>,<b>e</b>,<b>i</b>) in 1st row), August ((<b>b</b>,<b>f</b>,<b>j</b>) in 2nd row), September ((<b>c</b>,<b>g</b>,<b>k</b>) in 3rd row), and October ((<b>d</b>,<b>h</b>,<b>l</b>) in 4th row) in 2022.</p>
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<p>Spatial distributions of SM1, SM2, SM3, and SM4 anomalies in the Yangtze River Basin during July ((<b>a</b>,<b>e</b>,<b>i</b>,<b>m</b>) in 1st row), August ((<b>b</b>,<b>f</b>,<b>j</b>,<b>n</b>) in 2nd row), September ((<b>c</b>,<b>g</b>,<b>k</b>,<b>o</b>) in 3rd row), and October ((<b>d</b>,<b>h</b>,<b>l</b>,<b>p</b>) in 4th row) in 2022.</p>
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<p>The seasonal cycles of different environmental metrics: (<b>a</b>) temperature (κ), (<b>c</b>) precipitation (mm), and (<b>e</b>) VPD (hPa). The corresponding change percentages for the year 2022 compared to the average values from 2018 to 2021 are shown in (<b>b</b>) temperature, (<b>d</b>) precipitation, and (<b>f</b>) VPD. In (<b>a</b>,<b>c</b>,<b>e</b>), the black line represents the monthly average for 2022, and the red line represents the monthly average value from 2018 to 2021. In (<b>b</b>,<b>d</b>,<b>f</b>) the blue part represents the proportion of value in 2022 that exceeds the average from 2018 to 2021, while the red part represents the proportion of value in 2022 that falls below the average from 2018 to 2021.</p>
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<p>The seasonal cycles of different soil moisture metrics: (<b>a</b>) SM1 (unitless), (<b>c</b>) SM2 (unitless), (<b>e</b>) SM3 (unitless), and (<b>g</b>) SM4 (unitless). The corresponding change percentages for the year 2022 compared to the average values from 2018 to 2021 are shown in (<b>b</b>) SM1 (unitless), (<b>d</b>) SM2 (unitless), (<b>f</b>) SM3 (unitless), and (<b>h</b>) SM4 (unitless). In (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>), the black line represents the monthly average for 2022, and the red line represents the monthly average value from 2018 to 2021. In (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>), the blue part represents the proportion of value in 2022 that exceeds the average from 2018 to 2021, while the red part represents the proportion of value in 2022 that falls below the average from 2018 to 2021.</p>
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<p>The seasonal cycles of different soil moisture metrics: (<b>a</b>) NDVI (unitless), (<b>c</b>) SIF (unitless), (<b>e</b>) GPP (gC m<sup>−2</sup> d<sup>−1</sup>), and (<b>g</b>) NEE (gC m<sup>−2</sup> d<sup>−1</sup>). The corresponding change percentages for the year 2022 compared to the average values from 2018 to 2021 are shown in (<b>b</b>) NDVI (unitless), (<b>d</b>) SIF (unitless), (<b>f</b>) GPP (gC m<sup>−2</sup> d<sup>−1</sup>), and (<b>h</b>) NEE (gC m<sup>−2</sup> d<sup>−1</sup>). In (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>), the black line represents the monthly average for 2022, and the red line represents the monthly average value from 2018 to 2021. In (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>), the blue part represents the proportion of value in 2022 that exceeds the average from 2018 to 2021, while the red part represents the proportion of value in 2022 that falls below the average from 2018 to 2021.</p>
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<p>Spatial distributions of NDVI, SIF, and GPP anomalies in the Yangtze River Basin during July ((<b>a</b>,<b>e</b>,<b>i</b>,<b>m</b>) in 1st row), August ((<b>b</b>,<b>f</b>,<b>j</b>,<b>n</b>) in 2nd row), September ((<b>c</b>,<b>g</b>,<b>k</b>,<b>o</b>) in 3rd row), and October ((<b>d</b>,<b>h</b>,<b>l</b>,<b>p</b>) in 4th row) in 2022.</p>
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<p>Spatial distribution of partial correlations between July and October 2022: (<b>a</b>) correlations between SM1 anomalies and SIF anomalies, (<b>b</b>) correlations between VPD anomalies and SIF anomalies. The blue part represents a positive correlation, while the red part represents a negative correlation.</p>
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<p>The differential values of the seasonal cycles for the year 2022 compared to the average values from 2018 to 2021: (<b>a</b>) temperature(κ), (<b>b</b>) precipitation(mm), and (<b>c</b>–<b>f</b>) SM1–SM4 (unitless). The green line represents forest while the purple line represents cropland.</p>
Full article ">Figure 10
<p>The differential values of the seasonal cycles for the year 2022 compared to the average values from 2018 to 2021: (<b>a</b>) NDVI (unitless), (<b>b</b>) SIF (unitless), (<b>c</b>) GPP (gC m<sup>−2</sup> d<sup>−1</sup>), and (<b>d</b>) NEE (gC m<sup>−2</sup> d<sup>−1</sup>). The green line represents forest, while the purple line represents cropland.</p>
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9 pages, 1919 KiB  
Communication
Emergence of Arctic Extremes
by James E. Overland
Climate 2024, 12(8), 109; https://doi.org/10.3390/cli12080109 - 27 Jul 2024
Viewed by 839
Abstract
Recent increases in extreme events, especially those near and beyond previous records, are a new index for Arctic and global climate change. They vary by type, location, and season. These record-shattering events often have no known historical analogues and suggest that other climate [...] Read more.
Recent increases in extreme events, especially those near and beyond previous records, are a new index for Arctic and global climate change. They vary by type, location, and season. These record-shattering events often have no known historical analogues and suggest that other climate surprises are in store. Twenty-six unprecedented events from 2022, 2023, and early 2024 include record summer temperatures/heatwaves, storms, major Canadian wildfires, early continental snow melt, Greenland melt, sea temperatures of 5–7 °C above normal, drought in Iceland, and low northern Alaskan salmon runs. Collectively, such diverse extremes form a consilience, the principle that evidence from independent, unrelated sources converge as a strong indicator of ongoing Arctic change. These new behaviors represent emergent phenomenon. Emergence occurs when multiple processes interact to produce new properties, such as the interaction of Arctic amplification with the normal range of major weather events. Examples are typhon Merbok that resulted in extensive coastal erosion in the Bering Sea, Greenland melt, and record temperatures and melt in Svalbard. The Arctic can now be considered to be in a different state to before fifteen years ago. Communities must adapt for such intermittent events to avoid worst-case scenarios. Full article
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<p>Conceptual model of extremes combines Arctic amplification interacting with internal atmosphere and ocean processes that then can impact ecosystems. Reprinted from [<a href="#B8-climate-12-00109" class="html-bibr">8</a>].</p>
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<p>(<b>A</b>) Correlation of the 500 hPa pressure pattern over Greenland, with the runoff as a proxy for snow melt. Modified from Tedesco and Fettweis [<a href="#B10-climate-12-00109" class="html-bibr">10</a>]. The red dot is the 2019 data point. (<b>B</b>) 2 m air temperatures obtained from the MAR model forced by the reanalysis NCEP/NCAR reanalysis for June–August 2019. Reprinted from Tedesco and Fettweis [<a href="#B10-climate-12-00109" class="html-bibr">10</a>].</p>
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<p>The spatial pattern of changes in surface air temperature in the Barents Sea area for 2001–2020 [<a href="#B18-climate-12-00109" class="html-bibr">18</a>]. (<b>c</b>,<b>f</b>) Annual SAT trends (°C/decade) derived from CARRA and ERA5 reanalysis. Reprinted from [<a href="#B18-climate-12-00109" class="html-bibr">18</a>].</p>
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<p>Typhoon <span class="html-italic">Merbok</span> spins off the Alaskan coast. Credit: NOAA National Weather Service.</p>
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18 pages, 6278 KiB  
Review
Why Do Farmers Not Irrigate All the Areas Equipped for Irrigation? Lessons from Southern Africa
by Luxon Nhamo, Sylvester Mpandeli, Stanley Liphadzi, Tinashe Lindel Dirwai, Hillary Mugiyo, Aidan Senzanje, Bruce A Lankford and Tafadzwanashe Mabhaudhi
Agriculture 2024, 14(8), 1218; https://doi.org/10.3390/agriculture14081218 - 24 Jul 2024
Viewed by 947
Abstract
The reliance on rainfed agriculture exposes southern Africa to low agricultural productivity and food and nutritional insecurity; yet, the region is endowed with vast irrigation potential. Extreme weather events including drought, floods, and heatwaves exacerbate the existing challenges, underscoring the need to improve [...] Read more.
The reliance on rainfed agriculture exposes southern Africa to low agricultural productivity and food and nutritional insecurity; yet, the region is endowed with vast irrigation potential. Extreme weather events including drought, floods, and heatwaves exacerbate the existing challenges, underscoring the need to improve agricultural water management as a climate change adaptation strategy. This mixed-methods review followed the Search, Appraisal, Synthesis, and Analysis (SALSA) framework to explore the irrigation opportunities and challenges in southern Africa by critically analysing the drivers and constraints of irrigation systems in southern Africa. The premise is to understand the reasons behind the abandonment of some of the areas equipped for irrigation. In cases where irrigation systems are present, the study assesses whether such technologies are effectively being used to generate the expected agricultural productivity gains, and what factors, in cases where that is not the case, constrain farmers from fully using the existing infrastructure. The review further discusses the enabling environment supporting irrigated agriculture and the role of gender in irrigation development. An assessment of the role of women in agriculture on the share of land equipped for irrigation to total cultivated land area, as well as on the proportion of the area equipped for irrigation versus the area that is actually irrigated is conducted. The review found a divergence between countries’ land areas equipped for irrigation and actually irrigated areas. Specific to irrigation expansion, the review rebuts the notion that increasing the irrigated area increases crop production and ensures food security. This may not always be true as irrigation development needs to consider the impacts on other closely linked water and energy sectors through transformative approaches like the water–energy–food (WEF) nexus and scenario planning. If well-planned and implemented, sustainable irrigated agriculture could be catalytic to transforming southern Africa’s food system to be inclusive, equitable, socially just, and resilient, benefiting people and the planet. Full article
(This article belongs to the Section Agricultural Water Management)
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<p>Schematic flowchart detailing the phases of literature search, handling, and screening.</p>
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<p>Share of irrigated and rainfed agricultural system in southern Africa. Source: Siddiqui et al., 2016 [<a href="#B27-agriculture-14-01218" class="html-bibr">27</a>].</p>
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<p>Existing and proposed dams in southern Africa indicating the uneven distribution across the region. Source: Data obtained from FAO AQUASTAT, 2024 [<a href="#B26-agriculture-14-01218" class="html-bibr">26</a>].</p>
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<p>Economically active population in agriculture in Africa, which is predominantly women. Source: Data obtained from FAO AQUASTAT, 2024 [<a href="#B26-agriculture-14-01218" class="html-bibr">26</a>].</p>
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15 pages, 9143 KiB  
Technical Note
Vegetation Warming and Greenness Decline across Amazonia during the Extreme Drought of 2023
by Juan Carlos Jiménez, Vitor Miranda, Isabel Trigo, Renata Libonati, Ronaldo Albuquerque, Leonardo F. Peres, Jhan-Carlo Espinoza and José Antonio Marengo
Remote Sens. 2024, 16(14), 2519; https://doi.org/10.3390/rs16142519 - 9 Jul 2024
Viewed by 705
Abstract
In 2023, most parts of the world experienced exceptional heat. In particular, anomalous warm temperatures and heatwave events were evidenced across South America during the second half of the year. The situation was particularly critical in the Amazon region in terms of not [...] Read more.
In 2023, most parts of the world experienced exceptional heat. In particular, anomalous warm temperatures and heatwave events were evidenced across South America during the second half of the year. The situation was particularly critical in the Amazon region in terms of not only hydrometeorological drought but also ecological and socioeconomic impacts. In this study, remote-sensing data collected from the Moderate Resolution Imaging Spectroradiometer (MODIS) were used to observe the changes in temperature and vegetation across Amazonia during the exceptional drought of 2023. This analysis was based on anomalies in the land surface temperature (LST) and vegetation indices: the enhanced vegetation index (EVI) and the normalized difference vegetation index (NDVI). The amplitude of the LST (AMP-LST), an indicator of the energy partitioning between the latent and sensible heat flux, and fire counts were also considered. The results show widespread and extreme warming across Amazonia during the austral spring in 2023, accompanied by a decline in vegetation greenness, water stress conditions across northern Amazonia, and an enhanced fire occurrence across central and northern Amazonia. Full article
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<p>Land cover of the study area. The thick black line delineates the Amazon River basin, including the Tocantins–Araguaia drainage basin. Grey thin lines indicate the country’s borders. The study area is arbitrarily divided into four quarters (black lines): Northeast (NE), Northwest (NW), Southwest (SW), and Southeast (SE). Five different land-cover classes are visualized: evergreen broadleaf forests (EBF), deciduous broadleaf forests (DBF), savannas and woody savannas (SAV), grasslands (GRA), and croplands (CRO). Brazilian states within the Amazon basin are also labeled: AM (Amazonas), RR (Roraima), AP (Amapá), PA (Pará), MA (Maranhão), TO (Tocantins), CO (Goiás), MT (Matto Grosso), RO (Rondônia), and AC (Acre).</p>
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<p>Maps of land surface temperature (LST) standardized anomalies for DJF, MAM, JJA, and SON seasons during 2022 and 2023.</p>
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<p>Monthly values of land surface temperature (LST) for years of occurrence of some of the most recent severe droughts across Amazonia, including the drought of 2023. Results are provided for the four quarters delimiting the north–east and west–east regions (NW, NE, SW, and SE). The climatological mean (2003–2020) is also included.</p>
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<p>Maps of amplitude of land surface temperature (AMP-LST) standardized anomalies for DJF, MAM, JJA, and SON seasons during 2022 and 2023.</p>
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<p>Maps based on classification via the combination of LST (<a href="#remotesensing-16-02519-f002" class="html-fig">Figure 2</a>) and AMP-LST (<a href="#remotesensing-16-02519-f004" class="html-fig">Figure 4</a>) standardized anomalies. Regions colored in red can be interpreted as water-stressed, whereas regions colored in orange can be interpreted as heat-stressed.</p>
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<p>Maps of normalized difference vegetation index (NDVI) standardized anomalies for DJF, MAM, JJA, and SON seasons during 2022 and 2023.</p>
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<p>Monthly values of normalized difference vegetation index (NDVI) for years of occurrence of some of the most recent severe droughts across Amazonia, including the drought of 2023. Results are provided for the four quarters delimiting the north–east and west–east regions (NW, NE, SW, and SE). The climatological mean (2003–2020) is also included.</p>
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<p>Maps of enhanced vegetation index (EVI) standardized anomalies for DJF, MAM, JJA, and SON seasons during 2022 and 2023.</p>
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<p>Maps of active fire counts standardized anomalies in 0.25° cells for DJF, MAM, JJA, and SON seasons during 2022 and 2023.</p>
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12 pages, 852 KiB  
Review
Exploring the Nexus of Climate Change and Substance Abuse: A Scoping Review
by Luca Tomassini, Massimo Lancia, Angela Gambelunghe, Abdellah Zahar, Niccolò Pini and Cristiana Gambelunghe
Int. J. Environ. Res. Public Health 2024, 21(7), 896; https://doi.org/10.3390/ijerph21070896 - 9 Jul 2024
Viewed by 844
Abstract
Introduction: The increase in average air temperature and multiple extreme weather events, such as heatwaves and droughts, pose significant health risks to humans. This scoping review aims to examine the current state of the existing literature concerning the potential relationship between substance abuse [...] Read more.
Introduction: The increase in average air temperature and multiple extreme weather events, such as heatwaves and droughts, pose significant health risks to humans. This scoping review aims to examine the current state of the existing literature concerning the potential relationship between substance abuse and climate change, along with the aspects it encompasses. Material and methods: The review followed PRISMA guidelines for methodological rigor, aiming to identify studies on drug abuse. Searches were conducted across the primary databases using specific search strings. Quality assessment involved evaluating the research question’s clarity, search strategy transparency, consistency in applying the inclusion/exclusion criteria, and reliability of data extraction. Results: Most studies were conducted in the USA. They included observational and retrospective quantitative studies, as well as qualitative and prospective observational ones. Research examined the correlation between extreme weather and some substance abuse. All studies analyzed the adverse effects of climate change, especially heatwaves, on both physiological and pathological levels. Conclusions: The scoping review notes the scarcity of studies about the correlation between substance abuse and climate change, and emphasizes the threats faced by individuals with substance abuse and mental health disorders due to climate change. Full article
(This article belongs to the Special Issue Global Climate Change and Public Health)
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<p>Diagram obtained through Prisma 2020 regarding the articles identified and screened.</p>
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22 pages, 10599 KiB  
Article
Cooling Potential of Urban Tree Species during Extreme Heat and Drought: A Thermal Remote Sensing Assessment
by Harald Zandler and Cyrus Samimi
Remote Sens. 2024, 16(12), 2059; https://doi.org/10.3390/rs16122059 - 7 Jun 2024
Viewed by 831
Abstract
The cooling potential of tree species in Central European cities is insufficiently studied during extreme heat and drought, although a stronger surge in heatwaves compared to the global average is observed in this region. Remote sensing-based thermal surveys are an important tool to [...] Read more.
The cooling potential of tree species in Central European cities is insufficiently studied during extreme heat and drought, although a stronger surge in heatwaves compared to the global average is observed in this region. Remote sensing-based thermal surveys are an important tool to shed light on the mitigation effects of green infrastructure, but approaches covering extreme events are scarce. In this study, we present a simple, low-cost thermal airborne methodology that covers the current daily heat record in 2022, after the second warmest and third driest spring-to-summer period since 1949, in the medium-sized German city of Forchheim. We found that in spite of record-breaking heat and drought conditions, trees still had a considerable cooling potential with surface temperatures of 2 °C to 6 °C below air temperatures. Tree species were characterized by substantial median differences in tree surface temperatures up to 3.64 °C. Conifers and drought-sensitive broadleaf species showed the highest temperatures during the extreme event, while riparian species with potentially good water provision showed the highest cooling potential. In addition to tree species, imperviousness and tree NDVI were important variables for urban tree surface temperature, showing positive (imperviousness) and negative (NDVI) correlations with tree surface temperatures. Our study provides a methodological remote sensing example for the spontaneous and rapid coverage of extreme events, documenting the benefits of tree species in the urban context. Full article
(This article belongs to the Special Issue Remote Sensing for Land Surface Temperature and Related Applications)
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<p>Coverage of flight campaign, distribution of urban trees from the cadastre [<a href="#B27-remotesensing-16-02059" class="html-bibr">27</a>], and location of climate [<a href="#B28-remotesensing-16-02059" class="html-bibr">28</a>,<a href="#B29-remotesensing-16-02059" class="html-bibr">29</a>] or active hydrological stations [<a href="#B30-remotesensing-16-02059" class="html-bibr">30</a>], with ELC-10 land cover classes [<a href="#B31-remotesensing-16-02059" class="html-bibr">31</a>] and Sentinel-2 imagery from 20 July 2022 [<a href="#B32-remotesensing-16-02059" class="html-bibr">32</a>] in the background. Projection: ETRS89/UTM zone 32N (CRS 25832). The red rectangle in the small overview map shows the location of the large scale map.</p>
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<p>Climate situation during and before the survey flight on 20 July 2022 (2022 values marked by the red line), compared to density distribution curves of precipitation sums from May to July (<b>a</b>), mean temperatures from May to July (<b>b</b>), and daily maximum temperatures from June to August (<b>c</b>) in the period 1949 to 2023. All data were derived from the German Weather Service (DWD) [<a href="#B28-remotesensing-16-02059" class="html-bibr">28</a>].</p>
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<p>Detail of the thermal orthomosaic with a LIDAR-derived hillshade in the background [<a href="#B50-remotesensing-16-02059" class="html-bibr">50</a>]. Trees and water surfaces show clear differences from buildings and streets. The red rectangle in the small map indicates the location of the large-scale illustration in relation to the flight area.</p>
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<p>Species results for observed tree pixel temperature differences (T<sub>surf</sub> − T<sub>air</sub>) in descending order by median values. Mean values are marked by black diamonds. Means of species sharing the same letter in the group label (e.g., a, b, or c) are not significantly different at the 95% confidence level. The number of analyzed trees is provided by n.</p>
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<p>Species differences of imperviousness in a 91 m window around tree pixels in descending order by median values. Mean values are marked by black diamonds. Means of species sharing the same letter in the group label (e.g., a, b, or c) are not significantly different at the 95% confidence level. The number of analyzed trees is provided by n.</p>
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<p>Species differences of tree pixel NDVI ascendingly sorted by median values. Mean values are marked by black diamonds. Means of species sharing the same letter in the group label (e.g., a, b, or c) are not significantly different at the 95% confidence level. The number of analyzed trees is provided by n.</p>
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<p>Species differences of tree pixel <span class="html-italic">adjusted tree surface temperatures</span> in descending order by median values. Mean values are marked by black diamonds. Means of species sharing the same letter in the group label (e.g., a, b, or c) are not significantly different at the 95% confidence level. The number of analyzed trees is provided by n. The red line shows the mean air temperature of urban reference stations during the survey.</p>
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<p>Importance score of the selected variables of interest using a 500-repeated Boruta algorithm with T<sub>diff</sub> as the dependent variable. Shadow variables are randomly shuffled variables to remove any potential correlation with the response [<a href="#B70-remotesensing-16-02059" class="html-bibr">70</a>].</p>
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26 pages, 2977 KiB  
Review
Weather Extremes Shock Maize Production: Current Approaches and Future Research Directions in Africa
by Shaolong Du and Wei Xiong
Plants 2024, 13(12), 1585; https://doi.org/10.3390/plants13121585 - 7 Jun 2024
Viewed by 1008
Abstract
Extreme weather events have led to widespread yield losses and significant global economic damage in recent decades. African agriculture is particularly vulnerable due to its harsh environments and limited adaptation capacity. This systematic review analyzes 96 articles from Web of Science, Science Direct, [...] Read more.
Extreme weather events have led to widespread yield losses and significant global economic damage in recent decades. African agriculture is particularly vulnerable due to its harsh environments and limited adaptation capacity. This systematic review analyzes 96 articles from Web of Science, Science Direct, and Google Scholar, focusing on biophysical studies related to maize in Africa and worldwide. We investigated the observed and projected extreme weather events in Africa, their impacts on maize production, and the approaches used to assess these effects. Our analysis reveals that drought, heatwaves, and floods are major threats to African maize production, impacting yields, suitable cultivation areas, and farmers’ livelihoods. While studies have employed various methods, including field experiments, statistical models, and process-based modeling, African research is often limited by data gaps and technological constraints. We identify three main gaps: (i) lack of reliable long-term experimental and empirical data, (ii) limited access to advanced climate change adaptation technologies, and (iii) insufficient knowledge about specific extreme weather patterns and their interactions with management regimes. This review highlights the urgent need for targeted research in Africa to improve understanding of extreme weather impacts and formulate effective adaptation strategies. We advocate for focused research on data collection, technology transfer, and integration of local knowledge with new technologies to bolster maize resilience and food security in Africa. Full article
(This article belongs to the Special Issue Climate Change and Weather Extremes’ Impacts on Crops)
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<p>PRISMA flowchart showing the process and criteria applied to the search process. The number of records identified in each step is also reported.</p>
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<p>Number of publications per year from 2010 to 2023.</p>
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<p>Extreme climate events addressed in the publications and their proportions (%). CC: mean climate change with extreme weather being implicitly included; D: drought; H: heatwave; F: flood; R: extreme rainfall; W: wet; C: cold; HF: heatwave and flood; HD: heatwave and drought; DW: drought and wet; HDR: heatwave, drought and flood; HDCW: heatwave, drought cold and wet; HDFC: heatwave, drought, flood and cold; HDFW: heatwave, drought, flood and wet; M: multiple events (more than four).</p>
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<p>Investigation methods used in the literature.</p>
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<p>Maize yield loss mechanisms are due to three types of extremes and compound extremes (i.e., heat and drought, heat and wetness).</p>
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22 pages, 9102 KiB  
Article
Evaluation of the Compound Effects of the 2022 Drought and Heatwave on Selected Forest Monitoring Sites in Hungary in Relation to Its Multi-Year Drought Legacy
by Bence Bolla, Miklós Manninger, Tamás Molnár, Bálint Horváth, Jan Szolgay, Zoltán Gribovszki, Péter Kalicz and András Szabó
Forests 2024, 15(6), 941; https://doi.org/10.3390/f15060941 - 29 May 2024
Viewed by 688
Abstract
The effects of the changing frequency and severity of drought events in Central Europe may become a growing concern for its forests. In this study, we looked into how Hungary’s forests have been affected by the 2022 compound heatwave and drought, following an [...] Read more.
The effects of the changing frequency and severity of drought events in Central Europe may become a growing concern for its forests. In this study, we looked into how Hungary’s forests have been affected by the 2022 compound heatwave and drought, following an arid period from 2018 to 2021. We used our active intensive monitoring plots of the Forest Protection Measuring and Monitoring System (Level II in the ICP Forests) across the country between 2017 and 2022. We analyzed satellite images to support a survey of the large-scale drought utilizing moderate and high-resolution data. The health state of the forest calculated and mapped on the NDVI, ZNDVI, and NDWI indices showed damage and regeneration throughout the period studied. Overall, the forest stands observed tolerated the negative impacts of the drought (126–204 mm water deficit in 2022) based on our biomass data (the summer leaf loss was 14% in each monitoring plot). However, the classified Z-NDVI values of the Sentinel-2 satellite imagery for the period 2017–2022 showed a severe drought in 2022, which was followed by some improvement in 2023. Full article
(This article belongs to the Special Issue Forest Hydrology under Climate Change)
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<p>Location of the monitoring plots.</p>
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<p>Measuring devices in the monitoring plots: (<b>A</b>): (1) weather station, (<b>B</b>): (2) stemflow measurements, (3) throughfall measuring bucket, (4) litterfall trap, (<b>C</b>): (5) measuring of girth band.</p>
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<p>Walter diagrams in each sample area between 2017 and 2022 (the thick line is the year 2022; the thin line is the average between 2017 and 2021).</p>
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<p>Monthly early leaf fall (July, August, September) in the monitoring sites in 2022.</p>
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<p>Yearly leaf fall in the monitored sites during 2017–2022.</p>
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<p>Growth in girth values in 2022.</p>
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<p>Yearly actual evapotranspiration during 2018–2022.</p>
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<p>Yearly actual transpiration between 2018–2021 and 2022.</p>
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<p>Impact of the drought in 2022 in the first (<b>A</b>), and second half of June (<b>B</b>), the first (<b>C</b>) and second half of July (<b>D</b>), the first (<b>E</b>) and second half of August (<b>F</b>) on the classified Z NDVI maps. Damaged forest areas are shown in red, while areas with little or no damage are shown in blue.</p>
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<p>NDWI chart derived from satellite imagery of 2022 showing the water content of the canopy at the seven sites monitored. Due to the severe drought, the photosynthetic activity of the forest stands and the water content decreased, which can be seen in the form of forest status classification.</p>
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17 pages, 14015 KiB  
Article
A New Remote Sensing Index for Forest Dryness Monitoring Using Multi-Spectral Satellite Imagery
by Thai Son Le, Bernard Dell and Richard Harper
Forests 2024, 15(6), 915; https://doi.org/10.3390/f15060915 - 24 May 2024
Viewed by 838
Abstract
Canopy water content is a fundamental indicator for assessing the level of plant water stress. The correlation between changes in water content and the spectral reflectance of plant leaves at near-infrared (NIR) and short-wave infrared (SWIR) wavelengths forms the foundation for developing a [...] Read more.
Canopy water content is a fundamental indicator for assessing the level of plant water stress. The correlation between changes in water content and the spectral reflectance of plant leaves at near-infrared (NIR) and short-wave infrared (SWIR) wavelengths forms the foundation for developing a new remote sensing index, the Infrared Canopy Dryness Index (ICDI), to monitor forest dryness that can be used to predict the consequences of water stress. This study introduces the index, that uses spectral reflectance analysis at near-infrared wavelengths, encapsulated by the Normalized Difference Infrared Index (NDII), in conjunction with specific canopy conditions as depicted by the widely recognized Normalized Difference Vegetation Index (NDVI). Development of the ICDI commenced with the construction of an NDII/NDVI feature space, inspired by a conceptual trapezoid model. This feature space was then parameterized, and the spatial region indicative of water stress conditions, referred to as the dry edge, was identified based on the analysis of 10,000 random observations. The ICDI was produced from the combination of the vertical distance (i.e., under consistent NDVI conditions) from an examined observation to the dry edge. Comparisons between data from drought-affected and non-drought-affected control plots in the Australian Northern Jarrah Forest affirmed that the ICDI effectively depicted forest dryness. Moreover, the index was able to detect incipient water stress several months before damage from an extended drought and heatwave. Using freely available satellite data, the index has potential for broad application in monitoring the onset of forest dryness. This will require validation of the ICDI in diverse forest systems to quantify the efficacy of the index. Full article
(This article belongs to the Special Issue Monitoring Forest Change Dynamic with Remote Sensing)
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<p>Relationship between canopy cover and water content in response to canopy dryness (original by Thai Son Le).</p>
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<p>Map of the Northern Jarrah Forest showing the study area (purple frame) with sample (drought-affected) and control (healthy forest) locations.</p>
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<p>Example of a drought-affected sample at location (X: 429525; Y: −3583515) on 14 October 2010 (<b>A</b>) and 23 March 2011 (<b>B</b>) (source: Google Earth Pro). This is during the dry, summer period.</p>
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<p>General conceptual model of the NIR-SWIR/NDVI feature space (original by Thai Son Le).</p>
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<p>The dry edge from a 10,000-point random model at two different times for the study area.</p>
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<p>Flowchart illustrating the construction of the ICDI.</p>
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<p>Dry edge identification in the NDII/NDVI feature space (14 October 2010).</p>
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<p>Example of an ICDI map for the study area (see <a href="#forests-15-00915-f002" class="html-fig">Figure 2</a> for location) from the Landsat 7 image captured on 14 October 2010 (lower values indicate higher stress).</p>
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<p>Example of ICDI output delineating different dryness values according to a range of contributory factors (14 October 2010).</p>
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<p>The change over time of the ICDI index from drought-affected samples and control plots during 2010–2011 dry season. Note that in March 2011 the canopies were dead in the drought-affected sites and their ICDI was lower than for the healthy control plots.</p>
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25 pages, 9428 KiB  
Article
The Effects of Climate Change on Streamflow, Nitrogen Loads, and Crop Yields in the Gordes Dam Basin, Turkey
by Ayfer Özdemir, Martin Volk, Michael Strauch and Felix Witing
Water 2024, 16(10), 1371; https://doi.org/10.3390/w16101371 - 11 May 2024
Viewed by 896
Abstract
The Mediterranean region is highly vulnerable to climate change. Longer and more intense heatwaves and droughts are expected. The Gordes Dam in Turkey provides drinking water for Izmir city and irrigation water for a wide range of crops grown in the basin. Using [...] Read more.
The Mediterranean region is highly vulnerable to climate change. Longer and more intense heatwaves and droughts are expected. The Gordes Dam in Turkey provides drinking water for Izmir city and irrigation water for a wide range of crops grown in the basin. Using the Soil and Water Assessment Tool (SWAT), this study examined the effects of projected climate change (RCP 4.5 and RCP 8.5) on the simulated streamflow, nitrogen loads, and crop yields in the basin for the period of 2031–2060. A hierarchical approach to define the hydrological response units (HRUs) of SWAT and the Fast Automatic Calibration Tool (FACT) were used to reduce computational time and improve model performance. The simulations showed that the average annual discharge into the reservoir is projected to increase by between 0.7 m3/s and 4 m3/s under RCP 4.5 and RCP 8.5 climate change scenarios. The steep slopes and changes in precipitation in the study area may lead to higher simulated streamflow. In addition, the rising temperatures predicted in the projections could lead to earlier spring snowmelt. This could also lead to increased streamflow. Projected nitrogen loads increased by between 8.8 and 25.1 t/year. The results for agricultural production were more variable. While the yields of poppy, tobacco, winter barley, and winter wheat will increase to some extent because of climate change, the yields of maize, cucumbers, and potatoes are all predicted to be negatively affected. Non-continuous and limited data on water quality and crop yields lead to uncertainties, so that the accuracy of the model is affected by these limitations and inconsistencies. However, the results of this study provide a basis for developing sustainable water and land management practices at the catchment scale in response to climate change. The changes in water quality and quantity and the ecological balance resulting from changes in land use and management patterns for economic benefit could not be fully demonstrated in this study. To explore the most appropriate management strategies for sustainable crop production, the SWAT model developed in this study should be further used in a multi-criteria land use optimization analysis that considers not only crop yields but also water quantity and quality targets. Full article
(This article belongs to the Topic Hydrology and Water Resources Management)
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<p>Study area.</p>
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<p>(<b>a</b>) Soil map and (<b>b</b>) land use/cover map of the study area.</p>
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<p>Steps for the generation of the land use and land cover map of the study area.</p>
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<p>(<b>a</b>) Comparison of observed and simulated discharge and (<b>b</b>) comparation of observed and simulated nutrients.</p>
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<p>Calibration results of crop yields in the Gordes basin (red symbols: measured crop yields; boxes: simulated crop yields, black circle: outlier).</p>
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<p>(<b>a</b>) Temperature and (<b>b</b>) precipitation values under climate change scenarios RCP 4.5 and RCP 8.5 based on the sub-periods of 2031–2060; (<b>c</b>) planting and harvest time of each crop; (<b>d</b>) table of average monthly temperature and precipitation values based on sub-periods of climate change scenarios (blue color: average monthly precipitation (mm/month); orange color: average mean monthly temperature °C; green color: planting and harvesting period of each crop).</p>
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<p>(<b>a</b>) Effects of RCP 4.5 and RCP 8.5 climate change scenarios on streamflow; (<b>b</b>) Effects of RCP 4.5 and RCP 8.5 climate change scenarios on nitrogen loads (rf: reference period; cc: climate change, e.g., cc.4.5 shows climate change RCP 4.5).</p>
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<p>Climate change impacts on crop yields under the RCP 4.5 and RCP 8.5 climate change scenarios (black circle: outlier).</p>
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20 pages, 927 KiB  
Review
Changing Conditions: Global Warming-Related Hazards and Vulnerable Rural Populations in Mediterranean Europe
by Sandra Graus, Tiago Miguel Ferreira, Graça Vasconcelos and Javier Ortega
Urban Sci. 2024, 8(2), 42; https://doi.org/10.3390/urbansci8020042 - 25 Apr 2024
Viewed by 1636
Abstract
Human-induced climate change has profound effects on extreme events, particularly those linked to global warming, such as heatwaves, droughts, and wildfires. These events disrupt ecosystems, emphasizing the imperative to understand the interactions among them to gauge the risks faced by vulnerable communities. Vulnerability [...] Read more.
Human-induced climate change has profound effects on extreme events, particularly those linked to global warming, such as heatwaves, droughts, and wildfires. These events disrupt ecosystems, emphasizing the imperative to understand the interactions among them to gauge the risks faced by vulnerable communities. Vulnerability levels vary primarily based on a community’s resources. Rural areas, especially in the Mediterranean region of Europe, are experiencing acute depopulation, creating a complex situation affecting various aspects of society, from economic declines to cultural heritage loss. Population decline in rural regions weakens resources, leading to the abandonment of built environments, fostering desertification, and elevating the risk of wildfires. Communities undergoing this deterioration process become exceptionally vulnerable, especially when dealing with and recovering from extreme natural phenomena. This review offers insights into the dynamics of these hazards and the predominant challenges in rural areas. By focusing on a topic that has received limited attention, the aim is to inform future research initiatives, ultimately improving risk assessment and mitigation strategies for these vulnerable communities. Full article
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<p>Graphic scheme of challenges in rural areas due to depopulation and multiple hazards.</p>
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17 pages, 4549 KiB  
Article
From Oasis to Desert: The Struggle of Urban Green Spaces Amid Heatwaves and Water Scarcity
by Lennart Scharfstädt, Peer Schöneberger, Helge Simon, Tim Sinsel, Tim Nahtz and Michael Bruse
Sustainability 2024, 16(8), 3373; https://doi.org/10.3390/su16083373 - 17 Apr 2024
Viewed by 952
Abstract
In the summer of 2022, an intense heatwave swept through Northern Europe, with London bearing a significant impact. While nature-based solutions are often considered to be ideal responses to such heatwaves, experiences from the 2022 heatwave and others revealed potential drawbacks, particularly for [...] Read more.
In the summer of 2022, an intense heatwave swept through Northern Europe, with London bearing a significant impact. While nature-based solutions are often considered to be ideal responses to such heatwaves, experiences from the 2022 heatwave and others revealed potential drawbacks, particularly for urban green spaces. Prolonged dry spells, frequently accompanying heatwaves, result in excessively dry soil and the subsequent decline of vegetation in large parks. In the present study, microclimate simulations were conducted for Hyde Park in London, a location that experienced such drought during the 2022 heatwave, to examine its microclimatic performance in terms of thermal comfort and tree health. In alignment with the observations, ENVI-met could replicate the lack of noticeable cooling effects during the daytime and only marginal cooling during the nighttime. To address these challenges, mitigation scenarios were explored, incorporating heat mitigation measures such as part-time irrigation, temporary sun sails, and façade greenery. The findings demonstrated that implementing these measures could reduce heat stress by up to 13 K PET (physiologically equivalent temperature). These practical solutions emerged as effective remedies for mitigating the impact of heatwaves on urban green spaces and, hence, improving future urban development overall. Full article
(This article belongs to the Section Sustainable Urban and Rural Development)
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<p>Model area dimensions.</p>
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<p>Model area configurations with the application of heat mitigation measures using temporary sun sails (<b>a</b>) and façade greenery in addition (<b>b</b>).</p>
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<p>Full forcing boundary conditions used for all scenarios depicting direct shortwave (black line), diffuse shortwave (dashed line), and longwave radiation (dotted line) (<b>a</b>) as well as potential air temperature (black line) and specific air humidity (dashed line) (<b>b</b>).</p>
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<p>Observed trees’ location in the model area.</p>
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<p>PET result maps at 1 p.m. (<b>a</b>) and 10 p.m. (<b>b</b>) at a cut height level of 1.25 m. PET* is the default name for PET in ENVI-met as the model implemented the corrected PET calculations with V5.5.</p>
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<p>Daytime PET comparison maps at 1 p.m. at a cut height level of 1.25 m, showing differences between status quo and the scenarios using irrigation only (<b>a</b>), additional sun sails (<b>b</b>), and additional façade greenery (<b>c</b>). PET* is the default name for PET in ENVI-met as the model implemented the corrected PET calculations with V5.5.</p>
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<p>Nighttime PET comparison maps for 10 p.m. at a cut height level of 1.25 m showing differences between status quo and the scenarios using irrigation only (<b>a</b>), additional sun sails (<b>b</b>), and additional façade greenery (<b>c</b>). PET* is the default name for PET in ENVI-met as the model implemented the corrected PET calculations with V5.5.</p>
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<p>Tree health plots presenting transpiration rates in status quo and irrigated scenarios in different development stages of plane trees (<b>a</b>) as well as lime trees (<b>b</b>), and average leaf temperatures of plane and lime trees in the status quo scenario (<b>c</b>) as well as in the irrigated scenario (<b>d</b>).</p>
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17 pages, 6039 KiB  
Article
Spatiotemporal Variation in Water Deficit- and Heatwave-Driven Flash Droughts in Songnen Plain and Its Ecological Impact
by Jiahao Sun, Yanfeng Wu, Qingsong Zhang, Lili Jiang, Qiusheng Ma, Mo Chen, Changlei Dai and Guangxin Zhang
Remote Sens. 2024, 16(8), 1408; https://doi.org/10.3390/rs16081408 - 16 Apr 2024
Viewed by 926
Abstract
The phenomenon of flash droughts, marked by their fast onset, limited predictability, and formidable capacity for devastation, has elicited escalating concern. Despite this growing interest, a comprehensive investigation of the spatiotemporal dynamics of flash drought events within zones of ecological sensitivity, alongside their [...] Read more.
The phenomenon of flash droughts, marked by their fast onset, limited predictability, and formidable capacity for devastation, has elicited escalating concern. Despite this growing interest, a comprehensive investigation of the spatiotemporal dynamics of flash drought events within zones of ecological sensitivity, alongside their consequential ecological ramifications, remains elusive. The Songnen Plain, distinguished as both an important granary for commodity crops and an ecological keystone within China, emerges as an indispensable locus for the inquiry into the dynamics of flash droughts and their repercussions on terrestrial biomes. Through the application of daily soil moisture raster datasets encompassing the years 2002 to 2022, this investigation delves into the spatiotemporal progression of two distinct categories of flash droughts—those instigated by heatwaves and those precipitated by water deficits—within the Songnen Plain. Moreover, the ecosystem’s response, with a particular focus on gross primary productivity (GPP), to these climatic variables was investigated. Flash drought phenomena have been observed to manifest with a relative frequency of approximately one event every three years within the Songnen Plain, predominantly lasting for periods of 28–30 days. The incidence of both heatwave-induced and water deficit-induced flash droughts was found to be comparable, with a pronounced prevalence during the summer and autumn. Nevertheless, droughts caused by water scarcity demonstrated a more extensive distribution and a heightened frequency of occurrence, whereas those rooted in heatwaves were less frequent but exhibited a propensity for localization in specific sectors. The sensitivity of GPP to these meteorological anomalies was pronounced, with an average response rate surpassing 70%. This spatial distribution of the response rate revealed elevated values in the northwestern segment of the Songnen Plain and diminished values towards the southeastern sector. Intriguingly, GPP’s reaction pace to the onset of heatwave-driven flash droughts was observed to be more rapid in comparison to that during periods of water scarcity. Additionally, the spatial distribution of water use efficiency during both the development and recovery periods of flash droughts largely deviated from that of base water use efficiency. The insights from this study hold profound implications for the advancement of regional drought surveillance and adaptive management. Full article
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<p>A map of the Songnen Plain.</p>
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<p>A schematic representation of the method used to identify a flash drought event. The subfigure shows the development period of flash drought revealed by changes in soil moisture.</p>
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<p>Spatial distribution of the (<b>a</b>) number and (<b>b</b>) average duration of flash drought events in the Songnen Plain during 2002–2022.</p>
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<p>Spatial distribution of the number (<b>a</b>,<b>c</b>) and average duration (<b>b</b>,<b>d</b>) of water scarcity- (the first line) and heatwave-driven (the second line) flash droughts in the Songnen Plain during 2002–2022.</p>
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<p>Bubble plots of the duration (days) and onset time of (<b>a</b>) water deficit- and (<b>b</b>) heatwave-driven flash drought events during 2002–2022.</p>
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<p>Annual variation (the left panel), data distribution, and probability density of areas’ proportion (the right panel) affected by water deficit (P-deficit)- and high-temperature (Heat-wave)-driven flash drought events during the spring, summer, and autumn in the Songnen Plain from 2002 to 2022. The red and purple color refer to P-deficit and Heat-wave driven flash drought events respectively.</p>
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<p>The spatial distribution of the GPP response rates to (<b>a</b>) water deficit- and (<b>b</b>) heatwave-driven flash drought events across the Songnen Plain from 2002 to 2022.</p>
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<p>Spatial distribution of water use efficiency (WUE) versus base water use efficiency (uWUE) during the development (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) and recovery periods (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) of water deficit-type and heatwave-driven flash droughts events from 2002 to 2022.</p>
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<p>Spatial distribution of water use efficiency (WUE) versus base water use efficiency (uWUE) during the development (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) and recovery periods (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) of water deficit-type and heatwave-driven flash droughts events from 2002 to 2022.</p>
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