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Search Results (1,090)

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19 pages, 3209 KiB  
Article
Global Climate Convergence from 1980 to 2022 Led to Significant Increase in Vegetation Productivity
by Hongjuan Zhu and Chuanhua Li
Land 2025, 14(3), 570; https://doi.org/10.3390/land14030570 (registering DOI) - 8 Mar 2025
Abstract
Changes in global temperature and precipitation over the past few decades have caused significant alterations in global climate patterns. However, the impact of these changes on global vegetation productivity remains unclear. This article evaluates the effect of converging climate patterns on global vegetation [...] Read more.
Changes in global temperature and precipitation over the past few decades have caused significant alterations in global climate patterns. However, the impact of these changes on global vegetation productivity remains unclear. This article evaluates the effect of converging climate patterns on global vegetation productivity, focusing on the land outside Antarctica as the study area, and theoretically substantiates the validity of the findings. The study reveals the climate status of the historical period of 1980–2022 and the SSP126 scenario, where convergence in precipitation patterns leads to a significant increase in global NPP, while the convergence of temperature patterns has a much smaller impact on NPP than precipitation. Under the high-emission scenarios SSP245 and SSP585, the laws are reversed: converging temperature patterns lead to a decrease in NPP, while converging precipitation patterns have an insignificant impact on NPP. Climate change under these three scenarios indicates the detrimental effects of climate patterns under high emissions on vegetation productivity. This study fills a gap in the literature on the impact of climate patterns on vegetation productivity. Full article
(This article belongs to the Section Land–Climate Interactions)
14 pages, 8437 KiB  
Article
Genetic Diversity and Landscape Genomics of Carya dabieshanensis (M.C. Liu and Z.J. Li) in a Heterogenous Habitat
by Huanhuan Li, Jiahong Hong, Jiaoyang Tian, Da Zhang, Ruifeng Yang, Guohua Xia and Youjun Huang
Forests 2025, 16(3), 455; https://doi.org/10.3390/f16030455 - 4 Mar 2025
Viewed by 141
Abstract
Carya dabieshanensis is a species of significant economic value due to its unique flavor and nutritional properties as a snack food, as well as its durable wood, which is highly suitable for furniture production. Known for its remarkable adaptability to environmental stress, this [...] Read more.
Carya dabieshanensis is a species of significant economic value due to its unique flavor and nutritional properties as a snack food, as well as its durable wood, which is highly suitable for furniture production. Known for its remarkable adaptability to environmental stress, this species serves as a valuable genetic resource for enhancing hickory cultivars. However, its restricted distribution and limited availability of high-quality germplasm have impeded large-scale cultivation and hindered industry development. While the genetic diversity and genomic basis of its environmental adaptation hold great promise for future breeding programs, no studies to date have utilized SNP markers to explore its genetic diversity or the genomic mechanisms underlying environmental adaptability. In this study, we analyzed 60 samples from 12 natural populations of C. dabieshanensis, representing its global distribution. Using the Carya illinoinensis (Wangenh. and K. Koch) genome as a reference, we employed Specific Locus Amplified Fragment Sequencing (SLAF-seq) to generate high-quality SNP data. By integrating population and landscape genomics approaches, we investigated the genetic structure and diversity of wild populations and identified key environmental factors driving genetic differentiation. Our population genomics analysis revealed 9,120,926 SNP markers, indicating substantial genetic diversity (π = 1.335 × 10−3 to 1.750 × 10−3) and significant genetic differentiation among populations (FST = 0.117–0.354). Landscape genomics analysis identified BIO3 (Isothermality), BIO6 (Min Temperature of Coldest Month), and BIO14 (Precipitation of Driest Month) as critical environmental factors shaping genetic diversity. This study provides essential insights into the genetic resources of C. dabieshanensis, facilitating the development of climate-resilient cultivars and offering a scientific foundation for the conservation and sustainable management of its wild populations. Full article
(This article belongs to the Section Forest Biodiversity)
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Figure 1
<p>Distribution information of natural samples of <span class="html-italic">C. dabieshanensis.</span> (<b>A</b>) Geographic distribution of sampling provinces (Hubei and Anhui) in China. (<b>B</b>) Localization of sampling sites within Hubei and Anhui provinces, indicated by red circles. (<b>C</b>) Spatial distribution of 12 natural populations, distinguished by color markers.</p>
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<p>Population structure and genetic diversity of <span class="html-italic">C. dabieshanensis</span>. (<b>A</b>) Phylogenetic tree of 12 populations. (<b>B</b>) PCA plot. (<b>C</b>) Population structure analysis. (<b>D</b>) Historical effective population size (<span class="html-italic">Ne</span>). (<b>E</b>) LD decay plot. (<b>F</b>) Genetic diversity analysis. (<b>G</b>) Gene flow diagram.</p>
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<p>Selective clearance analysis and gene function analysis of <span class="html-italic">C. dabieshanensis</span>. (<b>a</b>) ROD_Fst result diagram. The red dots represent selected areas of the analyzed population. (<b>b</b>) GO enrichment analysis. (<b>c</b>) KEGG enrichment analysis.</p>
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<p>Distribution of variable loadings on the first three RDA axes (RDA1, RDA2, and RDA3) in redundancy analysis, representing the weight or influence of each variable on the respective RDA axis.</p>
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<p>(<b>a</b>) Pearson correlation coefficient among 20 environmental factors. (<b>b</b>) Pearson correlation coefficients (r &lt; 0.85) among the selected six environmental factors. ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001.</p>
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<p>Based on the RDA analysis of 60 individuals of <span class="html-italic">C. dabieshanensis</span>, the figure shows the RDA plot based on RDA axis 1 and RDA axis 2.</p>
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21 pages, 6436 KiB  
Article
Climate Change Amplifies the Effects of Vegetation Restoration on Evapotranspiration and Water Availability in the Beijing–Tianjin Sand Source Region, Northern China
by Xiaoyong Li, Yan Lv, Wenfeng Chi, Zhongen Niu, Zihao Bian and Jing Wang
Land 2025, 14(3), 527; https://doi.org/10.3390/land14030527 - 3 Mar 2025
Viewed by 218
Abstract
Evapotranspiration (ET) and water availability (WA) are critical components of the global water cycle. Although the effects of ecological restoration on ET and WA have been widely investigated, quantifying the impacts of multiple environmental factors on plant water consumption and regional water balance [...] Read more.
Evapotranspiration (ET) and water availability (WA) are critical components of the global water cycle. Although the effects of ecological restoration on ET and WA have been widely investigated, quantifying the impacts of multiple environmental factors on plant water consumption and regional water balance in dryland areas remains challenging. In this study, we investigated the spatial and temporal trends of ET and WA and isolated the contributions of vegetation restoration and climate change to variations in ET and WA in the Beijing–Tianjin Sand Source Region (BTSSR) in Northern China from 2001 to 2021, using the remote sensing-based Priestley–Taylor-Jet Propulsion Laboratory (PT-JPL) model and scenario simulation experiments. The results indicate that the estimated ET was consistent with field observations and state-of-the-art ET products. The annual ET in the BTSSR increased significantly by 1.28 mm yr−1 from 2001 to 2021, primarily driven by vegetation restoration (0.78 mm yr−1) and increased radiation (0.73 mm yr−1). In contrast, the drier climate led to a decrease of 0.56 mm yr−1 in ET. In semiarid areas, vegetation and radiation were the dominant factors driving the variability of ET, while in arid areas, relative humidity played a more critical role. Furthermore, reduced precipitation and increased plant water consumption resulted in a decline in WA by −0.91 mm yr−1 during 2001–2021. Climate factors, rather than vegetation greening, determined the WA variations in the BTSSR, accounting for 77.6% of the total area. These findings can provide valuable insights for achieving sustainable ecological restoration and ensuring the sustainability of regional water resources in dryland China under climate change. This study also highlights the importance of simultaneously considering climate change and vegetation restoration in assessing their negative impacts on regional water availability. Full article
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Figure 1
<p>Location of the study area, spatial pattern of land cover, and the distribution of eddy covariance flux sites in the BTSSR.</p>
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<p>Yearly (<b>a</b>) and monthly (<b>b</b>) ET comparisons between model simulations and observations.</p>
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<p>Monthly ET comparisons between model simulations and GLEAM4 (<b>a</b>), PML-V2 (<b>b</b>), SiTHv2 (<b>c</b>), and BESSv2 (<b>d</b>) datasets.</p>
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<p>Temporal (<b>a</b>) and spatial (<b>b</b>) trends of the leaf area index (LAI) in the BTSSR during 2001–2021. The black dash line in the subfigure (<b>a</b>) is the fitted linear regression.</p>
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<p>Temporal variations in air temperature (<b>a</b>), precipitation (<b>b</b>), net radiation (<b>c</b>), and relative humidity (<b>d</b>) in the BTSSR during 2001–2021. The black dash lines in the subfigures are the fitted linear regression.</p>
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<p>Spatial and temporal changes in ET during 2001–2021. Temporal variations in annual ET from 2001 to 2021 (<b>a</b>). Spatial pattern of multi-year average annual ET from 2001 to 2021 (<b>b</b>). Spatial trend of annual ET (<b>c</b>). Significance of the spatial trend in ET (<b>d</b>). The black dash line in the subfigure (<b>a</b>) is the fitted linear regression.</p>
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<p>Spatial and temporal trends in WA during 2001–2021. Temporal variations in annual WA from 2001 to 2021 (<b>a</b>). Spatial pattern of multi-year average annual WA from 2001 to 2021 (<b>b</b>). Spatial trend of annual WA (<b>c</b>). Significance of the spatial trend in WA (<b>d</b>). The black dash line in the subfigure (<b>a</b>) is the fitted linear regression.</p>
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<p>Contribution of vegetation change (<b>a</b>), net radiation (<b>b</b>), air temperature (<b>c</b>), and relative humidity (<b>d</b>) to ET variations in the BTSSR.</p>
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<p>Dominant factors of ET variations in the BTSSR (<b>a</b>,<b>c</b>) and arid and semiarid regions (<b>b</b>).</p>
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<p>Contribution of vegetation, climate, and precipitation to the trend of water availability in the BTSSR. (<b>a</b>–<b>c</b>) are the spatial pattern of the effects of three factors on ET variations and (<b>d</b>) shows the contribution of three factors to WA changes in the BTSSR, semiarid areas, and arid areas.</p>
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<p>Dominant factors of water availability variations in the BTSSR (<b>a</b>,<b>c</b>) and arid and semiarid regions (<b>b</b>).</p>
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39 pages, 12565 KiB  
Article
Integrating Land Use/Land Cover and Climate Change Projections to Assess Future Hydrological Responses: A CMIP6-Based Multi-Scenario Approach in the Omo–Gibe River Basin, Ethiopia
by Paulos Lukas, Assefa M. Melesse and Tadesse Tujuba Kenea
Climate 2025, 13(3), 51; https://doi.org/10.3390/cli13030051 - 28 Feb 2025
Viewed by 320
Abstract
It is imperative to assess and comprehend the hydrological processes of the river basin in light of the potential effects of land use/land cover and climate changes. The study’s main objective was to evaluate hydrologic response of water balance components to the projected [...] Read more.
It is imperative to assess and comprehend the hydrological processes of the river basin in light of the potential effects of land use/land cover and climate changes. The study’s main objective was to evaluate hydrologic response of water balance components to the projected land use/land cover (LULC) and climate changes in the Omo–Gibe River Basin, Ethiopia. The study employed historical precipitation, maximum and minimum temperature data from meteorological stations, projected LULC change from module for land use simulation and evaluation (MOLUSCE) output, and climate change scenarios from coupled model intercomparison project phase 6 (CMIP6) global climate models (GCMs). Landsat thematic mapper (TM) (2007) enhanced thematic mapper plus (ETM+) (2016), and operational land imager (OLI) (2023) image data were utilized for LULC change analysis and used as input in MOLUSCE simulation to predict future LULC changes for 2047, 2073, and 2100. The predictive capacity of the model was evaluated using performance evaluation metrics such as Nash–Sutcliffe Efficiency (NSE), the coefficient of determination (R2), and percent bias (PBIAS). The bias correction and downscaling of CMIP6 GCMs was performed via CMhyd. According to the present study’s findings, rainfall will drop by up to 24% in the 2020s, 2050s, and 2080s while evapotranspiration will increase by 21%. The findings of this study indicate that in the 2020s, 2050s, and 2080s time periods, the average annual Tmax will increase by 5.1, 7.3, and 8.7%, respectively under the SSP126 scenario, by 5.2, 10.5, and 14.9%, respectively under the SSP245 scenario, by 4.7, 11.3, and 20.7%, respectively, under the SSP585 scenario while Tmin will increase by 8.7, 13.1, and 14.6%, respectively, under the SSP126 scenario, by 1.5, 18.2, and 27%, respectively, under the SSP245 scenario, and by 4.7, 30.7, and 48.2%, respectively, under the SSP585 scenario. Future changes in the annual average Tmax, Tmin, and precipitation could have a significant effect on surface and subsurface hydrology, reservoir sedimentation, hydroelectric power generation, and agricultural production in the OGRB. Considering the significant and long-term effects of climate and LULC changes on surface runoff, evapotranspiration, and groundwater recharge in the Omo–Gibe River Basin, the following recommendations are essential for efficient water resource management and ecological preservation. National, regional, and local governments, as well as non-governmental organizations, should develop and implement a robust water resources management plan, promote afforestation and reforestation programs, install high-quality hydrological and meteorological data collection mechanisms, and strengthen monitoring and early warning systems in the Omo–Gibe River Basin. Full article
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Figure 1
<p>The study area map comprises meteorological stations, streamflow gauging stations, and stream networks.</p>
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<p>The general flowchart of the study comprises data input, preprocessing and processing, and outputs.</p>
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<p>Historical and projected LULC patterns of 2007, 2016, 2023, 2047, 2073, and 2100 in the Omo–Gibe River Basin.</p>
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<p>CMIP6 GCM selection procedure.</p>
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<p>Mean annual maximum temperature for the baseline (1985–2014), SSP126, SSP245, and SSP585 scenarios (2023–2100) considering the 95% confidence level in the OGRB.</p>
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<p>Mean annual minimum temperature for the baseline (1985–2014), SSP126, SSP245, and SSP585 scenarios (2023–2100) considering the 95% level of confidence in the OGRB.</p>
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<p>Mean annual minimum temperature for the baseline (1985–2014), SSP126, SSP245, and SSP585 scenarios (2023–2100) considering the 95% level of confidence in the OGRB.</p>
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<p>Anomalies of mean annual Tmax and Tmin for five CMIP6 models (<b>a</b>,<b>b</b>), and model ensemble mean for Tmax (<b>c</b>) and for Tmin (<b>d</b>) for the base historical period (1985–2014).</p>
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<p>Mean annual precipitation for the observed (1985–2022), SSP126, SSP245, and SSP585 scenarios (2023–2100) from five CMIP6 ensemble GCMs considering the 95% confidence level.</p>
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<p>Mean annual precipitation for the observed (1985–2022), SSP126, SSP245, and SSP585 scenarios (2023–2100) from five CMIP6 ensemble GCMs considering the 95% confidence level.</p>
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<p>Mean annual precipitation for the observed (1985–2022), SSP126, SSP245, and SSP585 scenarios (2023–2100) from five CMIP6 ensemble GCMs considering the 95% confidence level.</p>
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<p>Mean annual precipitation anomalies of five CMIP6 models (<b>a</b>) and model ensemble mean (<b>b</b>) for the base historical period (1985–2014).</p>
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<p>Mean annual precipitation anomalies of five CMIP6 models (<b>a</b>) and model ensemble mean (<b>b</b>) for the base historical period (1985–2014).</p>
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<p>Streamflow changes (<b>a</b>–<b>h</b>) in the observed and simulated data for the calibration (1995–2012) and validation periods (2013–2019).</p>
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<p>Streamflow changes (<b>a</b>–<b>h</b>) in the observed and simulated data for the calibration (1995–2012) and validation periods (2013–2019).</p>
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<p>Streamflow changes (<b>a</b>–<b>h</b>) in the observed and simulated data for the calibration (1995–2012) and validation periods (2013–2019).</p>
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<p>Effects of LULC changes on surface runoff during the 2020s (<b>left</b>), 2050s (<b>middle</b>), and 2080s (<b>right</b>) in the OGRB.</p>
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<p>Effects of LULC changes on evapotranspiration during the 2020s (<b>left</b>), 2050s, and 2080s in the OGRB.</p>
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<p>Effects of LULC changes on groundwater recharge during the 2020s, 2050s, and 2080s in the OGRB.</p>
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<p>Effects of climate change on surface runoff (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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<p>Effects of climate change on evapotranspiration (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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<p>Effects of climate change on groundwater recharge (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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<p>Effects of LULC and climate changes on surface runoff (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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<p>Effects of LULC and climate changes on evapotranspiration (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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<p>Effects of LULC and climate changes on groundwater recharge (mm) in the 2020s, 2050s, and 2080s from five CMIP6 GCMs under SSP126, SSP245, and SSP585 in the OGRB.</p>
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17 pages, 4259 KiB  
Article
Analyzing an Extreme Rainfall Event in Himachal Pradesh, India, to Contribute to Sustainable Development
by Nitin Lohan, Sushil Kumar, Vivek Singh, Raj Pritam Gupta and Gaurav Tiwari
Sustainability 2025, 17(5), 2115; https://doi.org/10.3390/su17052115 - 28 Feb 2025
Viewed by 303
Abstract
In the Himalayan regions of complex terrains, such as Himachal Pradesh, the occurrence of extreme rainfall events (EREs) has been increasing, triggering landslides and flash floods. Investigating the dynamics and precipitation characteristics and improving the prediction of such events are crucial and could [...] Read more.
In the Himalayan regions of complex terrains, such as Himachal Pradesh, the occurrence of extreme rainfall events (EREs) has been increasing, triggering landslides and flash floods. Investigating the dynamics and precipitation characteristics and improving the prediction of such events are crucial and could play a vital role in contributing to sustainable development in the region. This study employs a high-resolution numerical weather prediction framework, the weather research and forecasting (WRF) model, to deeply investigate an ERE which occurred between 8 July and 13 July 2023. This ERE caused catastrophic floods in the Mandi and Kullu districts of Himachal Pradesh. The WRF model was configured with nested domains of 12 km and 4 km horizontal grid resolutions, and the results were compared with global high-resolution precipitation products and the fifth-generation European Centre for Medium-Range Weather Forecasts atmospheric reanalysis dataset. The selected case study was amplified by the synoptic scale features associated with the position and intensity of the monsoon trough, including mesoscale processes like orographic lifting. The presence of a western disturbance and the heavy moisture transported from the Arabian Sea and the Bay of Bengal both intensified this event. The model has effectively captured the spatial distribution and large-scale dynamics of the phenomenon, demonstrating the importance of high-resolution numerical modeling in accurately simulating localized EREs. Statistical evaluation revealed that the WRF model overestimated extreme rainfall intensity, with the root mean square error reaching 17.33 mm, particularly during the convective peak phase. The findings shed light on the value of high-resolution modeling in capturing localized EREs and offer suggestions for enhancing disaster management and flood forecasting. Full article
(This article belongs to the Section Air, Climate Change and Sustainability)
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Figure 1
<p>The daily evolution of infrared brightness temperature (Unit: Kelvin) was derived from the INSAT-3DR satellite product. Panel figures (<b>a</b>–<b>f</b>) are plotted from 8 to 13 July 2023, respectively.</p>
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<p>The plotted area of the figure demonstrates the dimensions of the outer domain (D01). A rectangular box indicates the dimensions of the inner domain (D02), along with the topography of the study domains.</p>
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<p>(<b>a</b>) Climatological mean rainfall distribution (mm/day) for the six days (8 July to 13 July) over the 40 years (1984 to 2023); (<b>b</b>) Rainfall anomaly for the period from 8 July to 13 July for 2023.</p>
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<p>Spatiotemporal distribution of daily rainfall (mm) valid for six days (8 to 13 July 2023) from the IMD gridded data (<b>top row</b>), ERA5 (<b>second row</b>), MSWEP data (<b>third row</b>), and the WRF model’s inner domain simulation (<b>bottom row</b>).</p>
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<p>The Equitable Threat Score (ETS) for simulated rainfall (inner domain) validated against the MSWEP product at various threshold values from 8 July to 13 July 2023.</p>
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<p>Vertically integrated moisture transport (VIMT; kg.m<sup>−1</sup>.s<sup>−1</sup>) for all six days from the ERA5 data. The contours are presenting the VIMT and vectors denote the flow of moisture transport.</p>
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<p>Vertically integrated moisture transport (VIMT; kg.m<sup>−1</sup>.s<sup>−1</sup>) for all six days from the WRF model simulation.</p>
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<p>Area-averaged pressure vs. time vertical distribution of relative humidity (%) from (<b>a</b>) ERA5 and (<b>b</b>) WRF simulation for the inner domain.</p>
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<p>700 hPa daily geopotential height (m) and wind flow (m/s) from ERA5 (<b>first</b> and <b>second</b> rows) and WRF model’s outer domain simulation (<b>third</b> and <b>fourth</b> rows) valid for 8–13 July 2023.</p>
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<p>Extreme rainfall events disaster preparedness block diagram.</p>
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19 pages, 5377 KiB  
Article
Agroclimatic Indicator Analysis Under Climate Change Conditions to Predict the Climatic Suitability for Wheat Production in the Upper Blue Nile Basin, Ethiopia
by Wondimeneh Leul Demissew, Tadesse Terefe Zeleke, Kassahun Ture, Dejene K. Mengistu and Meaza Abera Fufa
Agriculture 2025, 15(5), 525; https://doi.org/10.3390/agriculture15050525 - 28 Feb 2025
Viewed by 275
Abstract
Agricultural productivity is significantly influenced by climate-related factors. Understanding the impacts of climate change on agroclimatic conditions is critical for ensuring sustainable agricultural practices. This study investigates how key agroclimatic variables—temperature, moisture conditions, and length of the growing season (LGS)—influence wheat suitability in [...] Read more.
Agricultural productivity is significantly influenced by climate-related factors. Understanding the impacts of climate change on agroclimatic conditions is critical for ensuring sustainable agricultural practices. This study investigates how key agroclimatic variables—temperature, moisture conditions, and length of the growing season (LGS)—influence wheat suitability in the Upper Blue Nile Basin (UBNB), Ethiopia. The Global Agroecological Zones (GAEZ) methodology was employed to assess agroclimatic suitability, integrating climate projections from Climate Models Intercomparison Project v6 (CMIP6) under shared socioeconomic pathway (ssp370 and ssp585) scenarios. The CMIP6 data provided downscaled projections for temperature and precipitation, while the GAEZ framework translated these climatic inputs into agroclimatic indicators, enabling spatially explicit analyses of land suitability. Projections indicate significant warming, with mean annual temperatures expected to rise between 1.13 °C and 4.85 °C by the end of the century. Precipitation levels are anticipated to increase overall, although spatial variability may challenge moisture availability in some regions. The LGS is projected to extend, particularly in the southern and southeastern UBNB, enhancing agricultural potential in these areas. However, wheat suitability faces considerable declines; under ssp585, the highly suitable area is expected to drop from 24.21% to 13.31% by the 2080s due to thermal and moisture stress. This study highlights the intricate relationship between agroclimatic variables and agricultural productivity. Integrating GAEZ and CMIP6 projections provides quantified insights into the impacts of climate change on wheat suitability. These findings offer a foundation for developing adaptive strategies to safeguard food security and optimize land use in vulnerable regions. Full article
(This article belongs to the Section Ecosystem, Environment and Climate Change in Agriculture)
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<p>Conceptual framework.</p>
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<p>Mean annual daily mean temperature in the UBNB. The top panel shows the baseline period (1981–2010), and the middle and bottom panels display changes under ssp370 and ssp585 scenarios, respectively.</p>
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<p>Mean annual precipitation in the UBNB. The top panel shows the baseline period (1981–2010), and the middle and bottom panels display changes under ssp370 and ssp585 scenarios, respectively.</p>
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<p>Mean annual temperature sum (TS10) above 10 °C for the UBNB. The top panel represents the baseline period (1981–2010), while the middle and bottom panels illustrate changes in TS10 under ssp370 and ssp585 scenarios, respectively.</p>
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<p>Spatial distribution of humidity indices (HIs) in the UBNB. The top panel shows the baseline period (1981–2010), and the middle and bottom panels depict changes in HIs under ssp370 and ssp585 scenarios, respectively.</p>
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<p>Spatial distribution of the GSL in the UBNB. The top panel represents the baseline period (1981–2010), while the middle and bottom panels show changes in GSL under ssp370 and ssp585 scenarios, respectively.</p>
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<p>Spatial distribution of wheat suitability classes in the UBNB under three scenarios: (1) the baseline period (1981–2010), (2) the ssp370 scenario, and (3) the ssp585 scenario. Each panel clearly delineates areas classified from very suitable to not suitable, based on agroclimatic constraints and high agricultural input conditions in a rainfed system.</p>
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19 pages, 13417 KiB  
Article
Ecosystem Service Trade-Offs and Synergies in a Temperate Agricultural Region in Northeast China
by Yuhong Li, Yu Cong, Jin Zhang, Lei Wang and Long Fei
Remote Sens. 2025, 17(5), 852; https://doi.org/10.3390/rs17050852 - 28 Feb 2025
Viewed by 156
Abstract
Ecosystem services (ESs) are essential for balancing environmental sustainability and socio-economic development. However, the sustainability of ESs and their relationships are increasingly threatened by global climate change and intensifying human activities, particularly in ecologically sensitive and agriculturally-intensive regions. The Songnen Plain, a crucial [...] Read more.
Ecosystem services (ESs) are essential for balancing environmental sustainability and socio-economic development. However, the sustainability of ESs and their relationships are increasingly threatened by global climate change and intensifying human activities, particularly in ecologically sensitive and agriculturally-intensive regions. The Songnen Plain, a crucial agricultural region in Northeast China, faces considerable challenges in sustaining its ESs due to the overexploitation of agricultural land, environmental degradation, and climate variability. This study assessed five key ESs in the Songnen Plain from 2000 to 2020 across multiple scales: habitat quality (HQ), soil conservation (SC), water yield (WY), food production (FP), and windbreaking and sand fixing (WS). We evaluated the trade-offs and synergies between these ESs, as well as the driving factors of the main ES trade-offs. Our findings indicate that provisioning services (WY and FP) and regulating services (SC and WS) improved over time, with FP exhibiting the most significant increase at 203.90%, while supporting services (HQ) declined by 32.61%. The primary ecosystem service multifunctionality areas were those that provided FP, SC, and WY, accounting for 58% of the total. ES trade-offs and synergies varied across spatial scales, with stronger synergies being observed at the pixel scale and more pronounced trade-offs at the county scale. Climate factors, particularly precipitation and temperature, played a more significant role in shaping ES trade-offs than anthropogenic factors. Our study provides valuable insights into the restoration and sustainable management of ESs in temperate agriculturally-intensive regions, with significant implications for the protection of the northeastern black soil region and safeguarding national food security. Full article
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<p>Geographical location maps of study area. (<b>a</b>) Elevation and water distribution of western Songnen Plain; (<b>b</b>) location of western Songnen Plain; (<b>c</b>) land use/land cover in 2020 for western Songnen Plain.</p>
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<p>Technical framework of ES trade-off and synergy relationships and driving factors of these trade-offs in Northeast China’s Songnen Plain.</p>
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<p>Spatial distribution and changes in ESs from 2000 to 2020.</p>
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<p>Spatial patterns of hot and cold spots for ESs. Hotspots are shown in red, and cold spots are shown in blue, with different confidence intervals represented by darker and lighter colors.</p>
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<p>The concurrence of the five ES hotspots and the ecosystem service multifunctionality areas in the study area which provide three or more ESs.</p>
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<p>Relationships between ESs at (<b>a</b>) county scale and (<b>b</b>) pixel scale. Positive values indicate synergistic relationships, while negative coefficients suggest trade-offs (* <span class="html-italic">p</span> &lt; 0.05; ** <span class="html-italic">p</span> &lt; 0.01).</p>
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<p>Spatial distributions of synergies and trade-offs between ES pairs in 2000 at both (<b>a</b>) county scale and (<b>b</b>) pixel scale. Blue represents synergy, and red represents trade-off.</p>
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<p>The distribution of each driver’s influence on the trade-offs of ten ES pairs across the study area during the period from 2000 to 2020 (PRE: precipitation, EVP: evapotranspiration, TEM: temperature).</p>
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24 pages, 11231 KiB  
Article
Assessing AgERA5 and MERRA-2 Global Climate Datasets for Small-Scale Agricultural Applications
by Konstantinos Soulis, Evangelos Dosiadis, Evangelos Nikitakis, Ioannis Charalambopoulos, Orestis Kairis, Aikaterini Katsogiannou, Stergia Palli Gravani and Dionissios Kalivas
Atmosphere 2025, 16(3), 263; https://doi.org/10.3390/atmos16030263 - 24 Feb 2025
Viewed by 415
Abstract
AgERA5 (ECMWF) is a relatively new climate dataset specifically designed for agricultural applications. MERRA-2 (NASA) is also used in agricultural applications; however, it was not specifically designed for this purpose. Despite the proven value of these datasets in assessing global climate patterns, their [...] Read more.
AgERA5 (ECMWF) is a relatively new climate dataset specifically designed for agricultural applications. MERRA-2 (NASA) is also used in agricultural applications; however, it was not specifically designed for this purpose. Despite the proven value of these datasets in assessing global climate patterns, their effectiveness in small-scale agricultural contexts remains unclear. This research aims to fill this gap by assessing the suitability and performance of AgERA5 and MERRA-2 in precision irrigation management, which is crucial for regions with limited ground data availability. The wine-making region of Nemea, Greece, with its complex and challenging terrain is used as a characteristic case study. The datasets are assessed for key weather variables and for irrigation planning, using detailed local meteorological station data as a reference. The results reveal that both products have serious limitations in small scale irrigation scheduling applications in contrast to what was reported in previous studies for other regions. The uneven performance of global datasets in different regions due to lack of sufficient observation data for reanalysis data calibration was also indicated. Comparing the two datasets, AgERA5 outperforms MERRA-2, especially in precipitation and reference evapotranspiration. MERRA-2 shows comparable potential in irrigation planning, as it occasionally matches or exceeds AgERA5’s performance. The study findings underscore the importance of evaluating metanalysis datasets in the application area before their use for precision agriculture, particularly in regions with complex topography. Full article
(This article belongs to the Section Biometeorology and Bioclimatology)
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<p>Map of the study area (<b>a</b>) where the grids of the AgERA5 (<b>b</b>) and MERRA-2 (<b>c</b>) climate datasets are overlaid over the weather stations.</p>
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<p>Soil taxonomical classes of the study area at the level of reference soil group.</p>
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<p>Relationship between observed and estimated total annual precipitation values using AgERA5 and MERRA-2 datasets with various interpolation methods. The linear regression lines in blue color, the 95% confidence intervals, and the x = y lines in black color are also plotted.</p>
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<p>Relationship between observed and estimated total annual potential evapotranspiration values using AgERA5 and MERRA-2 datasets with various interpolation methods. The linear regression lines in blue color, the 95% confidence intervals, and the x = y lines in black color are also plotted.</p>
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<p>Relationship between annual irrigation requirements values calculated using observed vs. estimated data using AgERA5 and MERRA-2 datasets with various interpolation methods. The linear regression lines in blue color, the 95% confidence intervals, and the x = y lines in black color are also plotted.</p>
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<p>Map with the station coverage which is the basis for the E-OBS precipitation dataset for (<b>a</b>) Greece and (<b>b</b>) all over Europe. E-OBS is a land-only gridded daily observational dataset for precipitation, temperature, sea level pressure, global radiation, wind speed, and relative humidity in Europe [<a href="#B47-atmosphere-16-00263" class="html-bibr">47</a>].</p>
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19 pages, 7061 KiB  
Article
Monitoring and Evaluation of Ecological Environment Quality in the Tianshan Mountains of China Using Remote Sensing from 2001 to 2020
by Yuting Liu, Chunmei Chai, Qifei Zhang, Xinyao Huang and Haotian He
Sustainability 2025, 17(4), 1673; https://doi.org/10.3390/su17041673 - 17 Feb 2025
Viewed by 473
Abstract
High-altitude mountainous regions are highly vulnerable to climate and environmental shifts, with the current global climate change exerting a profound influence on the ecological landscape of the Tianshan Mountains in China. This study assesses the ecological security quality in the Tianshan Mountains of [...] Read more.
High-altitude mountainous regions are highly vulnerable to climate and environmental shifts, with the current global climate change exerting a profound influence on the ecological landscape of the Tianshan Mountains in China. This study assesses the ecological security quality in the Tianshan Mountains of China from 2001 to 2020 by employing various remote sensing techniques such as the Remote Sensing Ecological Index (RSEI) for evaluation, Normalized Difference Vegetation Index (NDVI) for fractional vegetation cover (FVC) analysis, the CASA model for estimating vegetation primary productivity (NPP), and a carbon source/sink model for calculating the net ecosystem productivity (NEP) of vegetation. The research also delves into the evolutionary trends and impact mechanisms on the ecological environment using land use and meteorological data. The findings reveal that the RSEI’s principal component (PC1) exhibits significant explanatory power, showing a notable increase of 5.90% from 2001 to 2020. Despite relatively stable changes in the RSEI over the past two decades covering 61.37% of the study area, there is a prevalent anti-persistence pattern at 72.39%. Notably, NDVI, FVC, and NPP display upward trends in vegetation characteristics. While most areas in the Tianshan Mountains continue to emit carbon, there is a marked increase in NEP, signifying an enhanced carbon absorption capacity. The partial correlation coefficients between the RSEI and temperature, as well as precipitation, demonstrate statistically significant relationships (p < 0.05), encompassing 6.36% and 1.55% of the study area, respectively. Temperature displays a predominantly negative correlation in 98.71% of the significantly correlated zones, while precipitation exhibits a prevalent positive correlation. An in-depth analysis of how climate change affects the quality of the ecological environment provides crucial insights for strategic interventions to enhance regional environmental protection and promote ecological sustainability. Full article
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<p>Overview of the study area.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of RSEI in 2001, (<b>b</b>) spatiotemporal characteristics of RSEI in 2010, (<b>c</b>) spatiotemporal characteristics of RSEI in 2020, and (<b>d</b>) spatiotemporal characteristics of the average RSEI values from 2001 to 2020.</p>
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<p>Proportion of different levels of RSEI in the Tianshan Mountains from 2001 to 2020.</p>
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<p>The sustainability and stability of the ecological environment in the Tianshan Mountains of China from 2001 to 2020. (<b>a</b>) Spatial distribution of the RSEI coefficient of variation; (<b>b</b>) spatial distribution of Hurst exponent of the RSEI.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of the average NDVI values from 2001 to 2020; (<b>b</b>) temporal changes in NDVI from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of FVC in 2001, (<b>b</b>) spatiotemporal characteristics of FVC in 2010, (<b>c</b>) spatiotemporal characteristics of FVC in 2020, and (<b>d</b>) spatiotemporal characteristics of the average FVC values from 2001 to 2020.</p>
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<p>Area and proportion of vegetation coverage grades in the Tianshan Mountains from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of NPP in 2001, (<b>b</b>) spatiotemporal characteristics of NPP in 2010, (<b>c</b>) spatiotemporal characteristics of NPP in 2020, and (<b>d</b>) temporal changes in NPP in China’s Tianshan Mountains from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of NEP in 2001, (<b>b</b>) spatiotemporal characteristics of NEP in 2010, (<b>c</b>) spatiotemporal characteristics of NEP in 2020, and (<b>d</b>) temporal changes in NEP in China’s Tianshan Mountains from 2001 to 2020.</p>
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<p>Annual spatiotemporal characteristics of climate factors in Tianshan Mountains from 2001 to 2020. (<b>a</b>) Precipitation spatial patterns, (<b>b</b>) precipitation temporal trends, (<b>c</b>) temperature spatial patterns, and (<b>d</b>) temperature temporal trends.</p>
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<p>Correlation coefficients between the RSEI and precipitation, temperature in the Tianshan Mountains from 2001 to 2020.</p>
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<p>Dynamic changes in land types in the Chinese Tianshan Mountains from 2000 to 2020.</p>
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21 pages, 20266 KiB  
Article
Spatiotemporal Variation in Carbon and Water Use Efficiency and Their Influencing Variables Based on Remote Sensing Data in the Nanling Mountains Region
by Sha Lei, Ping Zhou, Jiaying Lin, Zhaowei Tan, Junxiang Huang, Ping Yan and Hui Chen
Remote Sens. 2025, 17(4), 648; https://doi.org/10.3390/rs17040648 - 14 Feb 2025
Viewed by 365
Abstract
A comprehensive evaluation of the variations in carbon use efficiency (CUE) and water use efficiency (WUE) in the Nanling Mountains Region (NMR) is crucial for gaining insights into the intricate relationships between climate change and ecosystem processes. This study evaluates the spatiotemporal rates [...] Read more.
A comprehensive evaluation of the variations in carbon use efficiency (CUE) and water use efficiency (WUE) in the Nanling Mountains Region (NMR) is crucial for gaining insights into the intricate relationships between climate change and ecosystem processes. This study evaluates the spatiotemporal rates of dynamics in CUE, WUE, gross primary productivity (GPP), net primary productivity (NPP), and evapotranspiration (ET) over the period from 2001 to 2023, using remote sensing data and linear regression analysis. Trend analysis, Hurst exponent analysis, and stability analysis were applied to examine the long-term patterns of CUE and WUE, while partial correlation analysis was employed to explore the spatial relationships between these efficiencies and climatic factors. The main findings of the study are as follows: (1) The CUE and WUE of the NMR decreased geographically from 2001 to 2023, and both the CUE and WUE of NMR showed a significant declining trend (p < 0.05) with the CUE decreasing at a rate of 0.0014/a (a: year) and the WUE falling at a rate of 0.0022/a. (2) The average values of the CUE and WUE of the NMR from 2001 to 2023 were 0.47 and 0.82 g C·m−2·mm−1, respectively, with a clear geographical difference. (3) The CUE and WUE in the NMR showed widespread degradation trends with some localized improvements, yet sustainability analysis indicates a likely continued decline across most areas, particularly for forests, while grasslands exhibit the greatest resilience. (4) Precipitation had a significantly stronger impact on WUE, while temperature appeared to exert a more substantial effect on CUE, with vegetation types responding differently; notably, shrubland displayed a direct association between CUE and temperature. In summary, multi-source data were employed to comprehensively analyze the spatiotemporal dynamics of CUE and WUE in the NMR over the past 23 years. We also examined the features of their responses to global warming, offering valuable theoretical insights into the carbon and water dynamics within the terrestrial ecosystems of the NMR. Full article
(This article belongs to the Special Issue Big Earth Data in Support of the Sustainable Development Goals)
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<p>Elevation maps and plant types of the NMR.</p>
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<p>Variation in (<b>a</b>) vegetation CUE and WUE from 2001 to 2023 in the NMR. (<b>b</b>) NPP, GPP, and ET from 2001 to 2023 in the NMR. Statistical significance is indicated as follows: * for <span class="html-italic">p</span> &lt; 0.05 and ** for <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>Spatial distribution patterns of vegetation CUE (<b>a</b>) and WUE (<b>b</b>) in the NMR.</p>
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<p>Variation in CUE (<b>a</b>) and WUE (<b>b</b>) across different vegetation types from 2001 to 2023 in the NMR.</p>
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<p>Spatial variation rates and their significance tests of vegetation CUE (<b>a</b>,<b>b</b>) and WUE (<b>c</b>,<b>d</b>) in the NMR from 2001 to 2023.</p>
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<p>The area proportions of vegetation CUE and WUE trend changes for different vegetation types in the NMR.</p>
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<p>Sustainability of vegetation CUE (<b>a</b>,<b>b</b>) and WUE (<b>c</b>,<b>d</b>) trends in the NMR from 2001 to 2023.</p>
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<p>Significant correlations between vegetation CUE and WUE with precipitation (<b>a</b>,<b>b</b>) and temperature (<b>c</b>,<b>d</b>) in the NMR from 2001 to 2023.</p>
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<p>Spatial patterns of correlation coefficients between CUE and WUE with precipitation (<b>a</b>,<b>b</b>) and temperature (<b>c</b>,<b>d</b>) in the NMR from 2001 to 2023.</p>
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<p>Mean correlation coefficients between CUE and WUE with precipitation and temperature across different vegetation types in the NMR from 2001 to 2023.</p>
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24 pages, 9886 KiB  
Article
Comparison of Machine Learning Algorithms for Daily Runoff Forecasting with Global Rainfall Products in Algeria
by Rayane Bounab, Hamouda Boutaghane, Tayeb Boulmaiz and Yves Tramblay
Atmosphere 2025, 16(2), 213; https://doi.org/10.3390/atmos16020213 - 13 Feb 2025
Viewed by 381
Abstract
Rainfall–runoff models are crucial tools for managing water resources. The absence of reliable rainfall data in many regions of the world is a major limitation for these models, notably in many African countries, although some recent global rainfall products can effectively monitor rainfall [...] Read more.
Rainfall–runoff models are crucial tools for managing water resources. The absence of reliable rainfall data in many regions of the world is a major limitation for these models, notably in many African countries, although some recent global rainfall products can effectively monitor rainfall from space. In Algeria, to identify a relevant modeling approach using this new source of rainfall information, the present research aims to (i) compare a conceptual model (GR4J) and seven machine learning algorithms (FFNN, ELM, LSTM, LSTM2, GRU, SVM, and GPR) and (ii) compare different types of precipitation inputs, including four satellite products (CHIRPS, SM2RAIN, GPM, and PERSIANN), one reanalysis product (ERA5), and observed precipitation, to assess which combination of models and precipitation data provides the optimal performance for river discharge simulation. The results show that the ELM, FFNN, and LSTM algorithms give the best performance (NSE > 0.6) for river runoff simulation and provide reliable alternatives compared to a conceptual hydrological model. The SM2RAIN-ASCAT and ERA5 rainfall products are as efficient as observed precipitation in this data-scarce context. Consequently, this work is the first step towards the implementation of these tools for the operational monitoring of surface water resources in Algeria. Full article
(This article belongs to the Section Meteorology)
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<p>Map of the study area.</p>
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<p>The method used for rainfall–runoff simulation.</p>
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<p>Impact of time lag between rainfall and runoff on hydrological forecast accuracy.</p>
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<p>KGE coefficient between simulated flow and observed flow of the different rainfall products for the different models. (<b>A</b>) is during calibration and (<b>B</b>) is during validation.</p>
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<p>Nash scores for each rainfall input in combination with the different hydrological models in calibration (<b>A</b>) and validation (<b>B</b>).</p>
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<p>Time series of observed and forecast runoff in the Aissi basin.</p>
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<p>Time series of observed and forecast runoff in the Boukdir basin.</p>
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<p>Time series of observed and forecast runoff in the Aissi Isser.</p>
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<p>Time series of observed and forecast runoff in the Malah basin.</p>
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<p>Time series of observed and forecast runoff in the Zddine basin.</p>
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<p>Taylor diagrams for the different rainfall inputs.</p>
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19 pages, 250 KiB  
Article
Perceptions of the Barriers to the Implementation of a Successful Climate Change Policy in Bulgaria
by Antonina Atanasova and Kliment Naydenov
Climate 2025, 13(2), 40; https://doi.org/10.3390/cli13020040 - 13 Feb 2025
Viewed by 348
Abstract
Climate change is increasingly recognized as a significant issue facing humanity. The World Health Organization (WHO) designates climate change as the greatest threat to global health in the 21st century. Bulgaria is under imminent threat from climate change. The country is projected to [...] Read more.
Climate change is increasingly recognized as a significant issue facing humanity. The World Health Organization (WHO) designates climate change as the greatest threat to global health in the 21st century. Bulgaria is under imminent threat from climate change. The country is projected to experience a temperature increase of up to 4 °C by 2100. This will lead to changes in precipitation patterns, resulting in numerous consequences. These include reduced water storage, impacts on public health, disruptions in agricultural production, stress on the country’s biodiversity and forests, damage to infrastructure and private property, changes in tourism patterns, and many other potential issues. Climate change has recently become a significant concern in Bulgaria due to its impact on ecosystems, the economy, society, and infrastructure. This study provides a comprehensive analysis of the barriers to climate adaptation in Bulgaria, integrating sources from the literature with empirical data gathered from a survey. By employing cluster analysis, this research identifies five primary groups of barriers, offering a fresh perspective on the complexities involved in this process. The findings contribute to the existing body of knowledge on climate adaptation and hold the potential to guide policy development aimed at addressing these challenges. Full article
17 pages, 6429 KiB  
Article
Impacts of Reference Precipitation on the Assessment of Global Precipitation Measurement Precipitation Products
by Ye Zhang, Leizhi Wang, Yilan Li, Yintang Wang, Fei Yao and Yiceng Chen
Remote Sens. 2025, 17(4), 624; https://doi.org/10.3390/rs17040624 - 12 Feb 2025
Viewed by 380
Abstract
Reference precipitation (RP) serves as a benchmark for evaluating the accuracy of precipitation products; thus, the selection of RP considerably affects the evaluation. In order to quantify this impact and provide guidance for RP selection, three interpolation methods, namely inverse distance weighting (IDW), [...] Read more.
Reference precipitation (RP) serves as a benchmark for evaluating the accuracy of precipitation products; thus, the selection of RP considerably affects the evaluation. In order to quantify this impact and provide guidance for RP selection, three interpolation methods, namely inverse distance weighting (IDW), ordinary kriging (OK), and geographical weighted regression (GWR), along with six groups of station densities, were adopted to generate different RPs, based on the super-high-density rainfall observations as true values, and we analyzed the errors of different RPs and the impacts of RP selection on the assessment of GPM precipitation products. Results indicate that the RPs from IDW and GWR both approached the true values as the station density increased (CC > 0.90); while the RP from OK showed some differences (CC < 0.80), it was similar to GWR when the station density was low, but the accuracy improved at first and then worsened as the station density continued to increase; the evaluation results based on different RPs showed remarkable differences even under the same conditions; when the average distance between rainfall gauges that were utilized to generate RPs was below the medium value (i.e., d < 20 km), the evaluation based on RP derived from IDW and GWR was close enough to that based on the true precipitation, which indicates its feasibility in evaluating satellite precipitation products. Full article
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<p>The geography survey of the study area.</p>
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<p>Technical scheme.</p>
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<p>Boxplots of the area-averaged <span class="html-italic">MAE</span> of RP.</p>
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<p>Spatial distribution of the accumulated precipitation when <math display="inline"><semantics> <mrow> <mi>M</mi> <mi>A</mi> <mi>E</mi> <mo>=</mo> <msub> <mrow> <mi>M</mi> <mi>A</mi> <mi>E</mi> </mrow> <mrow> <mi mathvariant="normal">M</mi> <mi mathvariant="normal">e</mi> <mi mathvariant="normal">d</mi> <mi mathvariant="normal">i</mi> <mi mathvariant="normal">a</mi> <mi mathvariant="normal">n</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
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<p>Boxplots of the evaluation index of interpolated precipitation relative to the true precipitation.</p>
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<p>Comprehensive evaluation results of the median and mean values of the total composite index in multi-group experiments.</p>
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<p>Normalized median distributions of the evaluation indices of the RP and true precipitation for evaluating near-real-time satellite precipitation products: (a), (b), and (c) present the RP obtained by the IDW, OK, and GWR methods to evaluate the IMERG early, and (d), (e), and (f) present the RP obtained by the IDW, OK, and GWR methods to evaluate the IMERG late. The circular symbols represent the average station distance <span class="html-italic">d</span> of 32.6, 23.1 km, 16.3 km, 13.3 km, 10.3 km, and 8.7 km. The smaller the average distance is, the larger the diameter of the circles is. The blue and red lines represent the results of the IMERG early and IMERG late products relative to the true precipitation.</p>
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21 pages, 4028 KiB  
Article
The Spatio-Temporal Analysis of Droughts Using the Standardized Precipitation Evapotranspiration Index and Its Impact on Cereal Yields in a Semi-Arid Mediterranean Region
by Chaima Elair, Khalid Rkha Chaham, Ismail Karaoui and Abdessamad Hadri
Appl. Sci. 2025, 15(4), 1865; https://doi.org/10.3390/app15041865 - 11 Feb 2025
Viewed by 551
Abstract
Over the last century, significant climate changes, including more intense droughts and floods, have impacted agriculture and socio-economic development, particularly in rain-dependent regions like Marrakech–Safi (MS) in Morocco. Limited data availability complicates the accurate monitoring and assessment of these natural hazards. This study [...] Read more.
Over the last century, significant climate changes, including more intense droughts and floods, have impacted agriculture and socio-economic development, particularly in rain-dependent regions like Marrakech–Safi (MS) in Morocco. Limited data availability complicates the accurate monitoring and assessment of these natural hazards. This study evaluates the role of satellite data in drought monitoring in the MS region using rain gauge observations from 18 stations, satellite-based precipitation estimates from Climate Hazards Group InfraRed Precipitation with Station (CHIRPS), and temperatures from the fifth generation of the atmospheric global climate reanalyzed Era5-Land data. The Standardized Precipitation Evapotranspiration Index (SPEI) was calculated at various timescales to characterize droughts. Statistical analysis was then performed to assess the correlation between the SPEI and the cereal yields. The results show that CHIRPS effectively monitors droughts, demonstrating strong statistically significant correlations (r ~ 0.9) with the observed data in the plains, the plateaus, Essaouira–Chichaoua Basin, and the coastal zones, along with a good BIAS score and lower root mean square error (RMSE). However, discrepancies were observed in the High Atlas foothills and the mountainous regions. Correlation analysis indicates the significant impact of droughts on agricultural productivity, with strong correlations between the Standardized Yield Residual Series (SYRS) and SPEI-6 in April and SPEI-12 in June (r ~ 0.80). These findings underscore the importance of annual and late-season precipitation for cereal yields. Analysis provides valuable insights for decision-makers in designing adaptation strategies to enhance small-scale farmers’ resilience to current and projected droughts. Full article
(This article belongs to the Section Earth Sciences)
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<p>(<b>A</b>) Morocco; (<b>B</b>) provinces of the MS region; (<b>C</b>) study area.</p>
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<p>Percentage of cereal land and production by province in MS region (2003–2018).</p>
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<p>Scatter plots comparing CHIRPS data with observed rainfall data for multiple stations on monthly scale.</p>
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<p>Variability in SPEI-12 derived from observed data and CHIRPS satellite rainfall estimates for four stations (Adamna, El Massira Dam, Iloudjane, and Nkouris).</p>
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<p>The spatial distribution of the monthly drought index SPEI-3 in March for each year from 1981 to 2018 in the MS region.</p>
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<p>Temporal variations in SYRS for each province in MS region (2003–2018).</p>
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<p>Heatmap of Pearson correlation coefficients (<span class="html-italic">r</span>) between SYRS and SPEI at different timescales and months (December, January, April, and June) for each province in MS region (2003–2018).</p>
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25 pages, 2639 KiB  
Review
Review of Carbonate Rock Experiments at Different Pressure and Temperature Conditions in the Context of Geothermal Energy Exploitation
by Ozioma Carol Uwakwe, Sylvia Riechelmann, Thomas Reinsch, Mathias Nehler and Adrian Immenhauser
Geosciences 2025, 15(2), 61; https://doi.org/10.3390/geosciences15020061 - 11 Feb 2025
Viewed by 359
Abstract
Geothermal energy exploitation has emerged as a critical solution to combat global climate crises, such as reducing CO2 emissions and climate warming. Scaling is the process of mineral precipitation in fluid pathways and geothermal equipment. It is known to significantly hamper geothermal [...] Read more.
Geothermal energy exploitation has emerged as a critical solution to combat global climate crises, such as reducing CO2 emissions and climate warming. Scaling is the process of mineral precipitation in fluid pathways and geothermal equipment. It is known to significantly hamper geothermal energy production by decreasing the rates of heat extraction. Numerous research efforts are dedicated to characterising dissolution and precipitation processes, not only to provide know-how for further and safer developments in geothermal energy, but also to adapt such findings to the ever emerging field of geothermal energy recovery. This paper presents an overview of experiments—performed under variable pressure and temperature conditions—with a focus on scaling. We assess the different factors that influence disequilibrium reactions in carbonate rocks, the different experimental setups, and their application to the field. The influence of experimental variables (such as temperature and pressure) on mineral dissolution and precipitation is discussed, and the main learning points from experiments are compared and contrasted. We address techniques for preventing and controlling scaling in geothermal wells based on a comprehensive analysis of experimental studies in carbonate rocks. We propose that the intelligent combination of fieldwork, numerical approaches, and laboratory experience provides a foundation for the success of future work in this field. Full article
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<p>Schematic diagram of heat extraction in a geothermal system and possible mineral precipitation/dissolution points in the system. The black star depicts the region of scale formation. Energy is produced from the reservoir in the subsurface by extracting fluids using artificial lift systems.</p>
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<p>Effect of temperature on calcite dissolution rate. All data are based on batch reactor experiments [<a href="#B67-geosciences-15-00061" class="html-bibr">67</a>,<a href="#B68-geosciences-15-00061" class="html-bibr">68</a>,<a href="#B69-geosciences-15-00061" class="html-bibr">69</a>,<a href="#B70-geosciences-15-00061" class="html-bibr">70</a>]. Dashed lines are the least square fits of the data. The plot was modified after [<a href="#B62-geosciences-15-00061" class="html-bibr">62</a>]. The data shows a weak temperature dependence on calcite dissolution rates. Increasing dissolution rates are recorded at higher temperatures.</p>
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<p>Effect of temperature on calcite solubility. Dotted lines are the least square fits of the data. Calcite solubility increases as temperature decreases. Calcite solubility increases with increasing pressure. Modified after [<a href="#B88-geosciences-15-00061" class="html-bibr">88</a>,<a href="#B91-geosciences-15-00061" class="html-bibr">91</a>].</p>
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<p>Effect of pCO<sub>2</sub> on calcite dissolution rate. All data are based on batch reactor experiments [<a href="#B67-geosciences-15-00061" class="html-bibr">67</a>,<a href="#B68-geosciences-15-00061" class="html-bibr">68</a>,<a href="#B69-geosciences-15-00061" class="html-bibr">69</a>,<a href="#B70-geosciences-15-00061" class="html-bibr">70</a>]. Dotted lines are the least square fits of the data. The plot was modified after [<a href="#B62-geosciences-15-00061" class="html-bibr">62</a>]. The results show that a variation in dissolution with pCO<sub>2</sub> it is more obvious at lower pCO<sub>2</sub> than at a higher pCO<sub>2</sub>. The dissolution rate increases by two orders of magnitude with pCO<sub>2</sub> value (1–10 bars).</p>
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<p>Schematic diagrams of the different types of setups for hydrothermal experiments. (<b>a</b>) Flow-through setup type with a CO<sub>2</sub> ultrasonic device to stimulate precipitation. (<b>b</b>) Batch rector modified from [<a href="#B103-geosciences-15-00061" class="html-bibr">103</a>]. (<b>c</b>) Flow-through stimulation experimental setup with a device (RESECO) that allows flow without a confining pressure modified after [<a href="#B99-geosciences-15-00061" class="html-bibr">99</a>].</p>
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<p>Solubility-supersaturation diagram of a sparingly soluble salt (e.g., CaCO<sub>3</sub>). The solid line corresponds to equilibrium. At point A, the solute is in equilibrium with the corresponding solid salt. Any deviation from this equilibrium may lead to either an isothermal reaction (line AB), at constant solute concentration, increasing the solution temperature (AC), or a metastable reaction by varying both concentration and temperature (AD). A solution departing from equilibrium is bound to return to this state by the precipitation of the excess solute. For most of the scale forming sparingly soluble salts, supersaturated solutions may be stable for practically infinite periods. These solutions are termed ‘metastable’. There is, however, a threshold in the extent of deviation from equilibrium marked by the dashed line, which, if reached, first wall crystallisation (scaling) and subsequently spontaneous precipitation may occur with or without an induction period preceding precipitation. This range of supersaturation defines the labile region, and the dashed line is known as the super solubility curve. Scaling cannot take place below the solubility curve. Modified after [<a href="#B3-geosciences-15-00061" class="html-bibr">3</a>].</p>
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<p>Partial deprotonation of polycarboxylic acid results in the formation of a polyelectrolyte, depicted in red, with carboxylate groups carrying electric charges. Modified after [<a href="#B49-geosciences-15-00061" class="html-bibr">49</a>].</p>
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<p>Schematic illustration of scaling inhibition through the proposed threshold mechanism; green: CaCO<sub>3</sub>-microcrystals, red: carboxylate groups, black: polymer backbone. Modified after [<a href="#B49-geosciences-15-00061" class="html-bibr">49</a>].</p>
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