[go: up one dir, main page]
More Web Proxy on the site http://driver.im/
You seem to have javascript disabled. Please note that many of the page functionalities won't work as expected without javascript enabled.
 
 
Sign in to use this feature.

Years

Between: -

Subjects

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Journals

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Article Types

Countries / Regions

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Search Results (8,941)

Search Parameters:
Keywords = land cover/use

Order results
Result details
Results per page
Select all
Export citation of selected articles as:
12 pages, 5212 KiB  
Article
Identifying Ecological Corridors of the Bush Cricket Saga pedo in Fragmented Landscapes
by Francesca Della Rocca, Emanuele Repetto, Livia De Caria and Pietro Milanesi
Insects 2025, 16(3), 279; https://doi.org/10.3390/insects16030279 - 6 Mar 2025
Abstract
The bush cricket Saga pedo, listed as Vulnerable globally by the IUCN and included in Annex IV of the EU Habitats Directive, is a parthenogenetic species highly sensitive to environmental changes, facing threats from forest expansion and agricultural intensification. S. pedo prefers [...] Read more.
The bush cricket Saga pedo, listed as Vulnerable globally by the IUCN and included in Annex IV of the EU Habitats Directive, is a parthenogenetic species highly sensitive to environmental changes, facing threats from forest expansion and agricultural intensification. S. pedo prefers dry, open habitats with sparse vegetation, and its pronounced thermo-heliophily makes it an indicator of xerothermic habitats. In many areas of Italy, including the Northern Apennines (Piedmont), semi-natural grasslands are fragmented. Open habitats have been reduced to small, isolated patches surrounded by forests due to the abandonment of agropastoral activities. Consequently, the occurrence of open habitat species is related to the quality and availability of suitable areas and ecological connectivity. We developed a spatial Bayesian framework to identify areas of occurrence for S. pedo. Using the inverse probability of occurrence, we derived ecological corridors among suitable patches. Our findings indicate that the occurrence and connectivity of S. pedo are reduced by intensive cultivation but favored by open habitats with 10–50% woody tree cover, suggesting sustainable land management is crucial for supporting the species. Given the extinction risk S. pedo faces, we urge local administrations to maintain and improve suitable areas and guarantee the network of ecological corridors identified. Full article
(This article belongs to the Special Issue Women’s Special Issue Series: Insects)
Show Figures

Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>Study area. Black lines indicate Italian regional borders. Light–dark green scale indicates lower–higher elevation.</p>
Full article ">Figure 2
<p>Distribution maps of <span class="html-italic">Saga pedo</span> estimated by weighted ensemble prediction of GLM- and GAM-INLA SPDE and landscape connectivity with Omniscape.jl. (<b>A</b>) Areas of predicted species occurrence estimated using a threshold value of 64.01 (threshold values estimated by maximizing TSS): presence indicated by yellow; absence indicated by black. (<b>B</b>) Probability of occurrence: yellow–blue scale indicates higher–lower occurrence probability values, respectively. (<b>C</b>) Landscape connectivity: yellow–blue scale indicates higher–lower landscape connectivity values, respectively.</p>
Full article ">Figure 3
<p>Response curves (in blue) and relative 95% confidence intervals (in gray) of probability of occurrence of <span class="html-italic">Saga pedo</span> in relation to predictor variables.</p>
Full article ">Figure 4
<p>Response curves (in blue) and relative 95% confidence intervals (in gray) of landscape connectivity of <span class="html-italic">Saga pedo</span> in relation to predictor variables.</p>
Full article ">
17 pages, 704 KiB  
Article
Willingness to Pay to Adopt Conservation Agriculture in Northern Namibia
by Teofilus Shiimi and David Uchezuba
Agriculture 2025, 15(5), 568; https://doi.org/10.3390/agriculture15050568 - 6 Mar 2025
Abstract
This paper aims to explore the willingness of farmers in the northern Namibia to adopt conservation agriculture (CA), employing the conditional logit model to estimate the probability of farmers choosing to adopt CA in different villages relative to all other alternatives and examining [...] Read more.
This paper aims to explore the willingness of farmers in the northern Namibia to adopt conservation agriculture (CA), employing the conditional logit model to estimate the probability of farmers choosing to adopt CA in different villages relative to all other alternatives and examining the effects of omitted variance and correlations on coefficient estimates, willingness to pay (WTP), and decision predictions. This study has practical significance, as agriculture plays a crucial role in the economic development of and livelihoods in Namibia, especially for those farmers who rely on small-scale farming as a means of subsistence. In terms of methodology, the data for the experimental choice simulation were collected using a structured questionnaire administered through a face-to-face survey approach. This paper adopts the conditional logit model to estimate the probability of farmers choosing to adopt CA in different villages, which is an appropriate choice as the model is capable of handling multi-option decision problems. This paper further enhances its rigor and reliability by simulating discrete choice experiments to investigate the impact of omitted variables and correlations on the estimation results. The research findings indicate that crop rotation and permanent soil cover are the main factors positively influencing farmers’ WTP for adopting CA, while intercropping, the time spent on soil preparation in the first season, and the frequency and rate of weeding consistently negatively influence the WTP for adopting CA. These discoveries provide valuable insights for formulating policy measures to promote the adoption of CA. In terms of policy recommendations, this paper puts forward targeted suggestions, including the appointment of specialized extension technicians by the Ministry of Agriculture, Water, and Land Reform to disseminate information as well as coordinate, promote, and personally implement CA activities across all regions. Additionally, to expedite the adoption of CA, stakeholders should ensure the availability of appropriate farming equipment, such as rippers and direct seeders, in local markets. Full article
Show Figures

Figure 1

Figure 1
<p>Location of villages in the selected study areas. Source: Authors’ compilation.</p>
Full article ">
27 pages, 3331 KiB  
Article
Potentiality Delineation of Groundwater Recharge in Arid Regions Using Multi-Criteria Analysis
by Heba El-Bagoury, Mahmoud H. Darwish, Sedky H. A. Hassan, Sang-Eun Oh, Kotb A. Attia and Hanaa A. Megahed
Water 2025, 17(5), 766; https://doi.org/10.3390/w17050766 - 6 Mar 2025
Abstract
This study integrates morphometric analysis, remote sensing, and GIS with the analytical hierarchical process (AHP) to identify high potential groundwater recharge areas in Wadi Abadi, Egyptian Eastern Desert, supporting sustainable water resource management. Groundwater recharge primarily comes from rainfall and Nile River water, [...] Read more.
This study integrates morphometric analysis, remote sensing, and GIS with the analytical hierarchical process (AHP) to identify high potential groundwater recharge areas in Wadi Abadi, Egyptian Eastern Desert, supporting sustainable water resource management. Groundwater recharge primarily comes from rainfall and Nile River water, particularly for Quaternary aquifers. The analysis focused on the Quaternary and Nubian Sandstone aquifers, evaluating 16 influencing parameters, including elevation, slope, rainfall, lithology, soil type, and land use/land cover (LULC). The drainage network was derived from a 30 m-resolution Digital Elevation Model (DEM). ArcGIS 10.8 was used to classify the basin into 13 sub-basins, with layers reclassified and weighted using a raster calculator. The groundwater potential map revealed that 24.95% and 29.87% of the area fall into very low and moderate potential categories, respectively, while low, high, and very high potential zones account for 18.62%, 17.65%, and 8.91%. Data from 41 observation wells were used to verify the potential groundwater resources. In this study, the ROC curve was applied to assess the accuracy of the GWPZ models generated through different methods. The validation results indicated that approximately 87% of the wells corresponded accurately with the designated zones on the GWPZ map, confirming its reliability. Over-pumping in the southwest has significantly lowered water levels in the Quaternary aquifer. This study provides a systematic approach for identifying groundwater recharge zones, offering insights that can support resource allocation, well placement, and aquifer sustainability in arid regions. This study also underscores the importance of recharge assessment for shallow aquifers, even in hyper-arid environments. Full article
(This article belongs to the Special Issue Advance in Groundwater in Arid Areas)
20 pages, 3868 KiB  
Article
Assessing Ecosystem Service Value Dynamics in Japan’s National Park Based on Land-Use and Land-Cover Changes from a Tourism Promotion Perspective
by Huixin Wang, Yilan Xie, Duy Thong Ta, Jing Zhang and Katsunori Furuya
Land 2025, 14(3), 554; https://doi.org/10.3390/land14030554 - 6 Mar 2025
Abstract
Understanding the changes in land use and land cover (LULC) in national parks and their corresponding ecosystem service value (ESV) shifts is crucial for shaping future management policies and directions. However, comprehensive analyses in this research area that integrate tourism development perspectives are [...] Read more.
Understanding the changes in land use and land cover (LULC) in national parks and their corresponding ecosystem service value (ESV) shifts is crucial for shaping future management policies and directions. However, comprehensive analyses in this research area that integrate tourism development perspectives are lacking. Therefore, this interdisciplinary study considers Akan-Mashu National Park in Japan as a case study. Using remote sensing data, LULC maps for the past 10 years were generated using the Google Earth Engine. The benefit transfer method was employed to calculate the corresponding ESV for each year, followed by a qualitative analysis of local tourism policy documents to explore how the park ecosystem has changed in the context of promoting tourism development. The results showed that LULC changes in Akan-Mashu National Park have been relatively stable over the past decade, with the most noticeable changes occurring in built-up areas. The results also confirm that tourism development has not had a significant negative impact on the ESV of the Akan-Mashu National Park. The recommendations proposed in this study can also be applied to other similar national parks or protected areas worldwide to achieve a dynamic balance between environmental protection and tourism development. Full article
(This article belongs to the Section Land Use, Impact Assessment and Sustainability)
Show Figures

Figure 1

Figure 1
<p>The location of the study site.</p>
Full article ">Figure 2
<p>Framework of this study.</p>
Full article ">Figure 3
<p>LULC maps of 2014 and 2023.</p>
Full article ">Figure 4
<p>The proportion of land-use types in the total study area.</p>
Full article ">Figure 5
<p>The changing trend of the area of each land-use type in the study period (Note: Here, we used different scales for each land-use type).</p>
Full article ">Figure 6
<p>Annual visitor numbers to Akan-Mashu National Park from 2014 to 2022 [<a href="#B36-land-14-00554" class="html-bibr">36</a>].</p>
Full article ">
18 pages, 4352 KiB  
Article
Ecotones in the Spotlight—Habitat Selection of the Golden Jackal (Canis aureus Linnaeus, 1758) in the Agricultural Landscapes of Central Europe
by Dorottya Karolin Gaál, Miklós Heltai, Gyula Sándor, Gergely Schally and Erika Csányi
Animals 2025, 15(5), 760; https://doi.org/10.3390/ani15050760 - 6 Mar 2025
Abstract
The large-scale expansion of the golden jackal (Canis aureus) across Europe in recent decades has been strongly influenced by its successful space and habitat use. In this study, we analyzed the habitat selection of seven golden jackals tracked with GPS collars [...] Read more.
The large-scale expansion of the golden jackal (Canis aureus) across Europe in recent decades has been strongly influenced by its successful space and habitat use. In this study, we analyzed the habitat selection of seven golden jackals tracked with GPS collars between 15 March 2021 and 25 November 2022 in a predominantly agricultural landscape in the southwestern part of the Pannonian Basin, Central Europe. Animals were tracked for an average of 29 weeks, and GPS collars recorded a total of 29,840 hourly localization points, which were compared to a high-resolution land cover dataset. We found that golden jackals maintain smaller home ranges in agricultural landscapes than in more pristine environments. Based on Jacobs’ index values calculated for monthly habitat preferences and the distribution of distances from land cover edges, we also found that preferences for the various habitat types differed significantly among individuals. Most of the time, golden jackals stayed near the edges of forests, agricultural lands, and shrublands, while they stayed away from artificial areas, wetlands, and water bodies. Forests and shrublands providing cover and safety were generally preferred by the golden jackals, especially during breeding and pup-rearing periods, while there was a strong avoidance of agricultural lands in general. Overall, our findings suggest that despite individual differences in the availability of habitat types within home ranges, forest–agricultural ecotones with relative proximity to food and shelter play a key role in the habitat selection of golden jackals. Full article
(This article belongs to the Section Wildlife)
Show Figures

Figure 1

Figure 1
<p>(<b>a</b>) Location of the study area within which 4 female and 3 male golden jackals (<span class="html-italic">Canis aureus</span>) were tracked with GPS collars. (<b>b</b>) First post-release localization points recorded by the collars. (<b>c</b>) The habitat structure of the study area indicating all localization points (<span class="html-italic">n</span> = 29,840) of seven GPS-tracked golden jackals.</p>
Full article ">Figure 2
<p>The dispersal of a female (F1) and male (M2) juvenile golden jackals in November and December of 2021.</p>
Full article ">Figure 3
<p>Habitat preferences of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>) in the agricultural landscapes of the southwestern part of the Pannonian Basin based on monthly Jacobs’ index values of habitat selection. The violin plots depict the distribution of Jacobs’ index values for each land cover category; jittered points represent individual data values, while X symbols indicate the mean Jacobs’ index for each category.</p>
Full article ">Figure 4
<p>Variety of the habitat preferences of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>) by individuals for artificial surface; agricultural land; shrubland; forest; and wetland and water body habitat types based on monthly Jacobs’ index values of habitat selection. The boxplots represent the distribution of Jacobs’ index values for each individual, where the central horizontal line indicates the median, the box shows the interquartile range (IQR; 25th to 75th percentiles), and the whiskers extend to 1.5 times the IQR. Jittered points depict individual data values, while the dashed horizontal line at zero represents no preference.</p>
Full article ">Figure 5
<p>Preference towards agricultural lands by month based on monthly Jacobs’ index values of habitat selection of seven GPS-collared golden jackals (<span class="html-italic">Canis aureus</span>). The boxplots represent the distribution of Jacobs’ index values for agricultural lands across months, where the central horizontal line indicates the median, the box shows the interquartile range (IQR; 25th to 75th percentiles), and the whiskers extend to 1.5 times the IQR. Jittered points depict individual data values, while the dashed horizontal line at zero represents no preference.</p>
Full article ">Figure 6
<p>Distribution of distances from landscape feature edges of the localization points (<span class="html-italic">n</span> = 29,840) of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>).</p>
Full article ">Figure A1
<p>Preference towards shrublands and forests by month based on monthly Jacobs’ index values of habitat selection of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>).</p>
Full article ">Figure A2
<p>Hourly distances (m) from different landscape features of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>) in the southwestern part of the Pannonian Basin.</p>
Full article ">Figure A2 Cont.
<p>Hourly distances (m) from different landscape features of seven GPS-tracked golden jackals (<span class="html-italic">Canis aureus</span>) in the southwestern part of the Pannonian Basin.</p>
Full article ">
21 pages, 30213 KiB  
Article
Landsat Time Series Reconstruction Using a Closed-Form Continuous Neural Network in the Canadian Prairies Region
by Masoud Babadi Ataabadi, Darren Pouliot, Dongmei Chen and Temitope Seun Oluwadare
Sensors 2025, 25(5), 1622; https://doi.org/10.3390/s25051622 - 6 Mar 2025
Abstract
The Landsat archive stands as one of the most critical datasets for studying landscape change, offering over 50 years of imagery. This invaluable historical record facilitates the monitoring of land cover and land use changes, helping to detect trends in and the dynamics [...] Read more.
The Landsat archive stands as one of the most critical datasets for studying landscape change, offering over 50 years of imagery. This invaluable historical record facilitates the monitoring of land cover and land use changes, helping to detect trends in and the dynamics of the Earth’s system. However, the relatively low temporal frequency and irregular clear-sky observations of Landsat data pose significant challenges for multi-temporal analysis. To address these challenges, this research explores the application of a closed-form continuous-depth neural network (CFC) integrated within a recurrent neural network (RNN) called CFC-mmRNN for reconstructing historical Landsat time series in the Canadian Prairies region from 1985 to present. The CFC method was evaluated against the continuous change detection (CCD) method, widely used for Landsat time series reconstruction and change detection. The findings indicate that the CFC method significantly outperforms CCD across all spectral bands, achieving higher accuracy with improvements ranging from 33% to 42% and providing more accurate dense time series reconstructions. The CFC approach excels in handling the irregular and sparse time series characteristic of Landsat data, offering improvements in capturing complex temporal patterns. This study underscores the potential of leveraging advanced deep learning techniques like CFC to enhance the quality of reconstructed satellite imagery, thus supporting a wide range of remote sensing (RS) applications. Furthermore, this work opens up avenues for further optimization and application of CFC in higher-density time series datasets such as MODIS and Sentinel-2, paving the way for improved environmental monitoring and forecasting. Full article
(This article belongs to the Special Issue Application of Satellite Remote Sensing in Geospatial Monitoring)
Show Figures

Figure 1

Figure 1
<p>The flowchart of the method used in this study for Landsat time series reconstruction.</p>
Full article ">Figure 2
<p>The study area situated in southeast Alberta. The right section provides an overview of a Landsat 5 TM image captured on 27 July 1999, displayed with a true-color band composition. Basemap: Esri, TomTom, Garmin, FAO, NOAA, USGS, EPA, NRCan, Parks Canada.</p>
Full article ">Figure 3
<p>The architecture of the CFC neural network. A backbone neural network layer processes the input signals and distributes them to three head networks: <math display="inline"><semantics> <mrow> <mi>g</mi> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>f</mi> </mrow> </semantics></math>, and <math display="inline"><semantics> <mrow> <mi>h</mi> </mrow> </semantics></math>. In this configuration, <math display="inline"><semantics> <mrow> <mi>f</mi> </mrow> </semantics></math> serves as a liquid time constant that regulates the sigmoidal time gates, while g and <math display="inline"><semantics> <mrow> <mi>h</mi> </mrow> </semantics></math> create the nonlinear components of the complete CFC network [<a href="#B22-sensors-25-01622" class="html-bibr">22</a>].</p>
Full article ">Figure 4
<p>The Landsat missions’ timeline from 1985 to the present.</p>
Full article ">Figure 5
<p>Training sample preparation in forward (<b>left</b>) and backward (<b>right</b>) approaches.</p>
Full article ">Figure 6
<p>The architecture of a CFC deep neural network.</p>
Full article ">Figure 7
<p>Results of test image reconstruction based on RMSE.</p>
Full article ">Figure 8
<p>Results of time series reconstruction of a sample grassland pixel in the study area using CCD (<b>left</b>) and CFC (<b>right</b>) for different bands from 2008 to 2014.</p>
Full article ">Figure 8 Cont.
<p>Results of time series reconstruction of a sample grassland pixel in the study area using CCD (<b>left</b>) and CFC (<b>right</b>) for different bands from 2008 to 2014.</p>
Full article ">Figure 9
<p>Average of error maps and histogram of error values on average for reconstructed test images using CCD (<b>left</b>) and CFC (<b>right</b>).</p>
Full article ">Figure 10
<p>(<b>a</b>) Reconstruction errors of test image bands for different land cover types based on RMSE. (<b>b</b>) A sample grassland pixel in the red band reconstructed using CFC. (<b>c</b>) A sample cropland pixel in the red band reconstructed using CFC.</p>
Full article ">Figure 11
<p>Results of image reconstruction based on RMSE for (<b>a</b>) spring, (<b>b</b>) summer, (<b>c</b>) fall and (<b>d</b>) winter.</p>
Full article ">Figure 12
<p>Results of time series reconstructions for a sample grassland pixel in the study area using CCD (<b>left</b>) and CFC (<b>right</b>) for SWIR bands from 2010 to 2015. Although variations arise due to cloud cover and haze around the winter test samples (red dots), CCD yielded a lower RMSE for these samples, as it is more closely centered around the time series mean.</p>
Full article ">Figure 13
<p>Image reconstruction using CCD and CFC for four test images, each selected from a different season.</p>
Full article ">Figure 14
<p>Relation between observation density and RMSE of test image bands reconstruction.</p>
Full article ">Figure 14 Cont.
<p>Relation between observation density and RMSE of test image bands reconstruction.</p>
Full article ">Figure 15
<p>Relation between observation density and RMSE of NIR band reconstruction for (<b>a</b>) spring, (<b>b</b>) summer, (<b>c</b>) fall, and (<b>d</b>) winter.</p>
Full article ">Figure 15 Cont.
<p>Relation between observation density and RMSE of NIR band reconstruction for (<b>a</b>) spring, (<b>b</b>) summer, (<b>c</b>) fall, and (<b>d</b>) winter.</p>
Full article ">Figure 16
<p>Relation between observation density and RMSE of NIR band reconstruction for different land covers.</p>
Full article ">Figure 17
<p>The effect of density level on reconstructing a sample cropland time series using CCD (<b>left</b>) and CFC (<b>right</b>).</p>
Full article ">Figure 17 Cont.
<p>The effect of density level on reconstructing a sample cropland time series using CCD (<b>left</b>) and CFC (<b>right</b>).</p>
Full article ">Figure 18
<p>Relation between observation density and accuracy of NIR band reconstruction for different parts of Landsat time series with different numbers of active satellites.</p>
Full article ">
40 pages, 16537 KiB  
Article
Adopting Land Cover Standards for Sustainable Development in Ghana: Challenges and Opportunities
by Elisha Njomaba, Fatima Mushtaq, Raymond Kwame Nagbija, Silas Yakalim, Ben Emunah Aikins and Peter Surovy
Land 2025, 14(3), 550; https://doi.org/10.3390/land14030550 - 5 Mar 2025
Viewed by 189
Abstract
The adoption of land cover standards is essential for resolving inconsistencies in global, regional, and national land cover datasets. This study examines the challenges associated with integrating existing datasets, including variations in land cover class definitions, classification methodologies, limited interoperability, and reduced comparability [...] Read more.
The adoption of land cover standards is essential for resolving inconsistencies in global, regional, and national land cover datasets. This study examines the challenges associated with integrating existing datasets, including variations in land cover class definitions, classification methodologies, limited interoperability, and reduced comparability across scales. Focusing on Ghana as a case study, this research aims to develop a land cover legend and land cover map aligned with International Organization for Standardization (ISO) 19144-2 standards, evaluate the effectiveness of improving land cover classification and accuracy of data, and finally, assess the challenges and opportunities for the adoption of land cover standards. This study uses a multi-sensor remote sensing approach, integrating Sentinel-1 and Sentinel-2 optical imagery with ancillary data (elevation, slope, and aspect), to produce a national land cover dataset for 2023. Using the random forest (RF) algorithm, the land cover map was developed based on a land cover legend derived from the West African land cover reference system (WALCRS). The study also collaborates with national and international organizations to ensure the dataset meets global reporting standards for Sustainable Development Goals (SDGs), including those for land degradation neutrality. Using a survey form, stakeholders in the land cover domain were engaged globally (world), regionally (Africa), and nationally (Ghana), to assess the challenges to and opportunities for the adoption of land cover standards. The key findings reveal a diverse range of land cover types across Ghana, with cultivated rainfed areas (28.3%), closed/open forest areas (19.6%), and savanna areas (15.9%) being the most dominant classes. The classification achieved an overall accuracy of 90%, showing the robustness of the RF model for land cover mapping in a heterogeneous landscape such as Ghana. This study identified a limited familiarity with land cover standards, lack of documentation, cost implication, and complexity of standards as challenges to the adoption of land cover standards. Despite the challenges, this study highlights opportunities for adopting land cover standards, including improved data accuracy, support for decision-making, and enhanced capacity for monitoring sustainable land cover changes. The findings highlight the importance of integrating land cover standards to meet international reporting requirements and contribute to effective environmental monitoring and sustainable development initiatives. Full article
26 pages, 6547 KiB  
Article
Classifying Rocky Land Cover Using Random Forest Modeling: Lessons Learned and Potential Applications in Washington, USA
by Joe V. Celebrezze, Okikiola M. Alegbeleye, Doug A. Glavich, Lisa A. Shipley and Arjan J. H. Meddens
Remote Sens. 2025, 17(5), 915; https://doi.org/10.3390/rs17050915 - 5 Mar 2025
Viewed by 133
Abstract
Rocky land cover provides vital habitat for many different species, including endemic, vulnerable, or threatened plants and animals; thus, various land management organizations prioritize the conservation of rocky habitat. Despite its importance, land cover classification maps rarely classify rocky land cover explicitly, and [...] Read more.
Rocky land cover provides vital habitat for many different species, including endemic, vulnerable, or threatened plants and animals; thus, various land management organizations prioritize the conservation of rocky habitat. Despite its importance, land cover classification maps rarely classify rocky land cover explicitly, and if they do, they are limited in spatial resolution or extent. Consequently, we used random forest models in Google Earth Engine (GEE) to classify rocky land cover at a high spatial resolution across a broad spatial extent in the Cascade Mountains and Columbia River Gorge in Washington, USA. The spectral indices derived from Sentinel-2 satellite data and NAIP aerial imagery, the specialized multi-temporal predictors formulated using time series of normalized burn ratio (NBR) and normalized difference in vegetation index (NDVI), and topographical predictors were especially important to include in the rocky land cover classification models; however, the predictors’ relative variable importance differed regionally. Beyond evaluating random forest models and developing classification maps of rocky land cover, we conducted three case studies to highlight potential avenues for future work and form connections to land management organizations’ needs. Our replicable approach relies on open-source data and software (GEE), aligns with the goals of land management organizations, and has the potential to be elaborated upon by future research investigating rocky habitats or other rare habitat types. Full article
Show Figures

Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>A map of the study area, including delineations for the Cascades (green) and Columbia (blue) regions and their associated sub-regions (italicized, with labels colored according to their region) in Washington, USA. Base map: Bing VirtualEarth.</p>
Full article ">Figure 2
<p>Conceptual diagrams conveying our reasoning for formulating multi-temporal predictors based on Sentinel-2 data. (<b>A</b>) The seasonal difference in NDVI was calculated to distinguish rocky land cover from grasses or drought-deciduous shrubs, while (<b>B</b>) NBR interannual metrics were used to distinguish rocky land cover, expected to have low NBR interannual variability, from disturbed landscapes (typically, burned or clearcut forests in the Cascades region), expected to have higher interannual variability in NBR.</p>
Full article ">Figure 3
<p>A workflow diagram exhibiting the point selection, attribution, classification, and iterative process utilized to classify rocky land cover for each sub-region.</p>
Full article ">Figure 4
<p>Land cover classified as rocky (black) and non-rocky (green). Full random forest models (40 predictors) for sub-regions in the Cascades and Columbia regions of Washington, USA, yielded land cover classification apart from the Portland sub-region, which had limited rocky land cover points (see <a href="#remotesensing-17-00915-t002" class="html-table">Table 2</a>). Base map: Bing VirtualEarth.</p>
Full article ">Figure 5
<p>(<b>A</b>) Variable importance of 40 predictors for the Cascades region (large black points) and associated sub-regions (smaller gray points), with boxes colored by predictor group. (<b>B</b>) Variable importance for 40 predictors for the Columbia region (large black points) and associated sub-regions (smaller gray points), with boxes colored by predictor group.</p>
Full article ">Figure 6
<p>Segmented regression results for overall accuracy, producer’s accuracy, and user’s accuracy statistics for (<b>A</b>) the Cascades and (<b>B</b>) the Columbia regions. For both regions, the mean breakpoint (vertical dashed line) was between six and seven predictors; thus, the optimized models utilize seven predictors for both regions.</p>
Full article ">Figure 7
<p>For optimized models, predictor values and their distributions vary between rocky and non-rocky land cover classifications for the Cascades and Columbia regions. Violin plots display seven ‘optimal’ predictors for each region, ordered by variable importance (see <a href="#app1-remotesensing-17-00915" class="html-app">Figure S2</a> for predictors’ variable importance in optimized models; see <a href="#app1-remotesensing-17-00915" class="html-app">Figure S3</a> for violin plots for all predictors).</p>
Full article ">Figure 8
<p>Case Study 1: A rocky patch in the southeast corner of the <span class="html-italic">Forbidden</span> sub-region shown using (<b>A</b>) NAIP imagery via Google Earth, (<b>B</b>) classified rocky land cover using 10 m full models and (<b>C</b>) 1 m resolution NAIP- and topography-based models, and (<b>D</b>) the overlap (purple) between 10 m (red) and 1 m resolution (blue) rocky land cover classification.</p>
Full article ">Figure 9
<p>Case Study 2: classification of non-rocky and rocky land covers and various unstable classes, determined by a (<b>A</b>) time series stability analysis for the <span class="html-italic">Snoqualmie</span> sub-region and (<b>B</b>–<b>D</b>) a zoomed-in area in the sub-region. The zoomed-in area shows (<b>B</b>) the stability classes, (<b>C</b>) the natural color image, and (<b>D</b>) the rocky land cover classification without stability classes included.</p>
Full article ">Figure 10
<p>Applications of Case Study 2: comparing sub-regions by investigating (<b>A</b>) proportions of classified area fitting in rocky and unstable land cover classifications and (<b>B</b>) their stability ratios, showing that sub-regions in the Cascades region have more stable classifications of rocky land cover than those in the Columbia region. Proportions of non-rocky land cover are not displayed, as their proportions were significantly higher than those of rocky or unstable classifications.</p>
Full article ">Figure 11
<p>Case Study 3: comparing rocky habitat classification to WDFW priority habitat maps for talus slopes and cliffs. Maps show the spatial extent of (<b>A</b>) WDFW priority habitat polygons and (<b>B</b>) the rocky land cover classification derived from our random forest modeling approach for the full Cascades region. Selected zoomed-in areas (shown in (<b>A</b>,<b>B</b>) with (<b>C</b>–<b>F</b>) blue and (<b>G</b>–<b>J</b>) red rectangles) exhibit differences in spatial extent and precision of rocky land cover classification, showing (<b>C</b>,<b>G</b>) natural color images, (<b>D</b>,<b>H</b>) WDFW priority habitat polygons, (<b>E</b>,<b>I</b>) our rocky habitat classification, and (<b>F</b>,<b>J</b>) how the two directly compare.</p>
Full article ">
28 pages, 8540 KiB  
Article
Snow Cover Variability and Trends over Karakoram, Western Himalaya and Kunlun Mountains During the MODIS Era (2001–2024)
by Cecilia Delia Almagioni, Veronica Manara, Guglielmina Adele Diolaiuti, Maurizio Maugeri, Alessia Spezza and Davide Fugazza
Remote Sens. 2025, 17(5), 914; https://doi.org/10.3390/rs17050914 - 5 Mar 2025
Viewed by 179
Abstract
Monitoring the snow cover variability and trends is crucial due to its significant contribution to river formation and sustenance. Using gap-filled MODIS data over the 2001–2024 period, the spatial distribution and temporal evolution of three snow cover metrics were studied: number of days, [...] Read more.
Monitoring the snow cover variability and trends is crucial due to its significant contribution to river formation and sustenance. Using gap-filled MODIS data over the 2001–2024 period, the spatial distribution and temporal evolution of three snow cover metrics were studied: number of days, onset and end of the snow cover season across fourteen regions covering the Karakoram, Western Himalayas and Kunlun Mountains. The obtained signals exhibit considerable complexity, making it difficult to find a unique factor explaining their variability, even if elevation emerged as the most important one. The mean values of snow-covered days span from about 14 days in desert regions to about 184 days in the Karakoram region. Given the high interannual variability, the metrics show no significant trend across the study area, even if significant trends were identified in specific regions. The obtained results correlate well with the ERA5 and ERA5-Land values: the Taklamakan Desert and the Kunlun Mountains experienced a significant decrease in the snow cover extent possibly associated with an increase in temperature and a decline in precipitation. Similarly, the Karakoram and Western Himalayas region show a positive snow cover trend possibly associated with a stable temperature and a positive precipitation trend. Full article
(This article belongs to the Section Environmental Remote Sensing)
Show Figures

Figure 1

Figure 1
<p>Study area. The border of the MODIS tile is represented with a bold black line and the fourteen subregions with a thin black line. The subregions are named following the acronyms defined in <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>, and the four different colors cluster them into four different groups by means of the PCA discussed in <a href="#sec3dot3-remotesensing-17-00914" class="html-sec">Section 3.3</a>. The color scheme of the labels represents these four groups: Group 1 is yellow, Group 2 is green, Group 3 is red, and Group 4 is blue.</p>
Full article ">Figure 2
<p>Orography of the study area, alongside elevation distribution of the fourteen subregions represented by means of the percentage of pixels for each 500 m elevation band. The acronyms of the subregions are defined in <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 3
<p>Total precipitation averaged over the 1991–2020 period using ERA5 data for the study area, alongside monthly precipitation distributions for the fourteen subregions represented by means of the percentage of precipitation with respect to the annual total. The acronyms of the subregions are defined in <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 4
<p>(<b>a</b>) Average snow-covered days (SCD); (<b>b</b>) average snow onset date (SOD) and (<b>c</b>) average snow end date (SED). The three metrics refer to the 2001–2024 period and are expressed in days. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 5
<p>Snow-covered days (SCD) distribution with respect to the elevation of all the grid points (black points) and the mean value for each subregion (colored points). The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 6
<p>Difference between the snow-covered days (SCD) of each grid point and the corresponding average SCD value over the whole considered area of points in the same 5 m elevation band. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 7
<p>Quantiles (colored points) of the snow-covered days (SCD) distributions for every 5 m elevation band in the different subregions. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 8
<p>Median (colored points) of the snow-covered days (SCD) distributions for every 5 m elevation band in the different regions. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 9
<p>Additive anomaly series with respect to the whole period of the snow-covered days (SCD—blue line), snow onset date (SOD—orange line), and snow end date (SED—yellow line) over the whole area in the 24-year study period.</p>
Full article ">Figure 10
<p>Additive anomaly series with respect to the whole period of the snow-covered days (SCD) in the 24-year study period for the fourteen subregions (thin lines) clustered into 4 groups using PCA. The bold red lines represent the average series within each cluster. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 11
<p>Snow-covered days (SCD) series for each subregion and 1000 m elevation band. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 12
<p>Sen’s slope of the significant SCD trends (<span class="html-italic">p</span>-value &lt; 0.1) for each grid point, expressed in days per decade. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 13
<p>Comparison between SCD (MODIS) and SCE (ERA5-Land) 24-year temporal series for the four groups of regions defined with the PCA (see <a href="#remotesensing-17-00914-f001" class="html-fig">Figure 1</a>).</p>
Full article ">Figure 14
<p>Comparison between SCE (ERA5-Land) average anomalies in the study area (blue) and in the latitudinal band 25–45°N (orange) over 1951–2024 and 2001–2024.</p>
Full article ">Figure 15
<p>Sen’s slope of the significant SCE (ERA5-Land) trends (<span class="html-italic">p</span>-value &lt; 0.1) for each grid point, expressed in % per decade. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 16
<p>Sen’s slope of the significant temperature (ERA5-Land) trends (<span class="html-italic">p</span>-value &lt; 0.1) for each grid point, expressed in °C per decade. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 17
<p>Sen’s slope of the significant precipitation (ERA5) trends (<span class="html-italic">p</span>-value &lt; 0.1) for each grid point, expressed in mm per decade. The acronyms of the subregions follow the definition of <a href="#remotesensing-17-00914-t001" class="html-table">Table 1</a>.</p>
Full article ">
27 pages, 780 KiB  
Review
Artificial Intelligence in Hydrology: Advancements in Soil, Water Resource Management, and Sustainable Development
by Seyed M. Biazar, Golmar Golmohammadi, Rohit R. Nedhunuri, Saba Shaghaghi and Kourosh Mohammadi
Sustainability 2025, 17(5), 2250; https://doi.org/10.3390/su17052250 - 5 Mar 2025
Viewed by 210
Abstract
Hydrology relates to many complex challenges due to climate variability, limited resources, and especially, increased demands on sustainable management of water and soil. Conventional approaches often cannot respond to the integrated complexity and continuous change inherent in the water system; hence, researchers have [...] Read more.
Hydrology relates to many complex challenges due to climate variability, limited resources, and especially, increased demands on sustainable management of water and soil. Conventional approaches often cannot respond to the integrated complexity and continuous change inherent in the water system; hence, researchers have explored advanced data-driven solutions. This review paper revisits how artificial intelligence (AI) is dramatically changing the most important facets of hydrological research, including soil and land surface modeling, streamflow, groundwater forecasting, water quality assessment, and remote sensing applications in water resources. In soil and land modeling, AI techniques could further enhance accuracy in soil texture analysis, moisture estimation, and erosion prediction for better land management. Advanced AI models could also be used as a tool to forecast streamflow and groundwater levels, therefore providing valuable lead times for flood preparedness and water resource planning in transboundary basins. In water quality, AI-driven methods improve contamination risk assessment, enable the detection of anomalies, and track pollutants to assist in water treatment processes and regulatory practices. AI techniques combined with remote sensing open new perspectives on monitoring water resources at a spatial scale, from flood forecasting to groundwater storage variations. This paper’s synthesis emphasizes AI’s immense potential in hydrology; it also covers the latest advances and future prospects of the field to ensure sustainable water and soil management. Full article
(This article belongs to the Section Social Ecology and Sustainability)
Show Figures

Figure 1

Figure 1
<p>Key areas and trends in research growth.</p>
Full article ">
24 pages, 14408 KiB  
Article
Spatial and Temporal Variations of Habitat Quality and Influencing Factors in Urban Agglomerations on the North Slope of Tianshan Mountains, China
by Ran Wang, Honglin Zhuang, Mingkai Cheng, Hui Yang, Wenfeng Wang, Hui Ci and Zhaojin Yan
Land 2025, 14(3), 539; https://doi.org/10.3390/land14030539 - 5 Mar 2025
Viewed by 43
Abstract
The northern slope of the Tianshan Mountains city cluster (NSTM), as a key urban agglomeration for the development of western China, has experienced rapid regional economic development and high population concentration since the twenty-first century. Accompanied by the increase in human activities in [...] Read more.
The northern slope of the Tianshan Mountains city cluster (NSTM), as a key urban agglomeration for the development of western China, has experienced rapid regional economic development and high population concentration since the twenty-first century. Accompanied by the increase in human activities in the NSTM, it has significantly altered the land use structure, leading to varying levels of habitat disturbance and degradation. In this paper, based on the land use and land cover (LULC) of NSTM from 2000 to 2020. The InVEST model was employed to assess habitat quality, revealing notable spatial and temporal variations. A geoprobe was further employed to explore the key drivers of the spatially distributed pattern of habitat quality in the research region. The results show that (1) from 2000 to 2020, the NSTM was largely characterized by grassland, unused land, and cropland in terms of land use, with a notable expansion of cropland and construction land; (2) the overall habitat quality in the study area is poor, with a clear spatial distribution pattern of high in the south and low in the north, with a predominance of low grades, and a trend of decreasing and then increasing is shown in the temporal direction; (3) under the influence of rapid urbanization in the region, the degradation degree of habitat quality on the NSTM shows a distinct radial structure, with high degradation in the middle and low degradation at the edges, and shows the trend of “increase-decrease-increase” over time; and (4) the results of the geodetector show that altitude and land use type have the greatest influence on habitat quality on the NSTM, indicating that the habitat quality of the research region is primarily influenced by the type of land use. Full article
Show Figures

Figure 1

Figure 1
<p>Study area: DEM of the north slope of Tianshan Mountain city cluster.</p>
Full article ">Figure 2
<p>Spatial distribution of the different threat sources on the northern slopes of Tianshan Mountain, 2020.</p>
Full article ">Figure 3
<p>Overall study process.</p>
Full article ">Figure 4
<p>Spatial distribution of land use on NSTM, 2000–2020.</p>
Full article ">Figure 5
<p>Land use transfer map, 2000–2020.</p>
Full article ">Figure 6
<p>Spatial and temporal distribution of HQ on NSTM, 2000–2020.</p>
Full article ">Figure 7
<p>Changes in HQ on NSTM.</p>
Full article ">Figure 8
<p>Spatial and temporal distribution of habitat degradation on NSTM, 2000–2020.</p>
Full article ">Figure 9
<p>Spatial distribution patterns of factors affecting HQ (2020).</p>
Full article ">Figure 10
<p>Area share and Pearson’s correlation analysis.</p>
Full article ">Figure 11
<p>Results of single-factor detection by geodetector.</p>
Full article ">Figure 12
<p>Geo-detector two-factor detection results.</p>
Full article ">
24 pages, 1668 KiB  
Review
Progress and Prospects of Research on Physical Soil Crust
by Huiyun Xu, Xuchao Zhu and Meixia Mi
Soil Syst. 2025, 9(1), 23; https://doi.org/10.3390/soilsystems9010023 - 4 Mar 2025
Viewed by 161
Abstract
Physical soil crust (PSC) is a dense structural layer formed on the surface of bare or very low-cover land due to raindrop splashes or runoff. The formation of crust changes the properties of the soil and strongly affects water infiltration and runoff and [...] Read more.
Physical soil crust (PSC) is a dense structural layer formed on the surface of bare or very low-cover land due to raindrop splashes or runoff. The formation of crust changes the properties of the soil and strongly affects water infiltration and runoff and sediment production processes on slopes. The irrational use of soil and water resources and frequent human production activity under the influence of urbanization increase the possibility of inducing erosion. Studying the formation and structural characteristics of PSC to predict terrestrial hydrological processes and improve models for predicting erosion is very important. Many studies of PSC have been carried out in China and abroad, but they are mainly unilateral discussions of the basic properties and characteristics of crust and its effects on runoff and sediment yield on slopes. Studies systematically analyzing and synthesizing the progress of crust research, however, are lacking. By reading the literature and analyzing the developmental history of PSC, we provide a comprehensive review of the following: (1) the meaning, main types, and classification of PSC, (2) the mechanism of formation and the characteristics and dynamic development of crust, (3) the factors affecting the formation of crust, including natural and anthropogenic factors and comprehensive effects, and (4) the development and formation of crust in the soil environment, i.e., hydrological processes and erosion. We also summarize the potential directions for future research on PSC: (1) studying the dynamics of soil structure during the development of crust, (2) developing an objective and standardized quantitative method for studying crust formation, (3) using models of erosion influenced by crust development, (4) improving the scale of the degree of crust development and structural characteristics, and (5) rationalizing the management of crust to optimize land structure and increase crop yield. Full article
Show Figures

Figure 1

Figure 1
<p>Methods for measuring the thickness of physical crust. (<b>a</b>). Vernier calipers. (<b>b</b>). Observation of microscope sections. (<b>c</b>). CT scanning and porosity thresholding.</p>
Full article ">Figure 2
<p>Four stages of quantifying physical crust. (<b>a</b>). Qualitative description. (<b>b</b>). Semi-quantitative representation. (<b>c</b>). Preliminary quantification. (<b>d</b>). Quantitative expression.</p>
Full article ">Figure 3
<p>Simulation of the processes and trends in the development of physical crust in Quaternary red clay in southern China.</p>
Full article ">
21 pages, 8035 KiB  
Article
Identify Tea Plantations Using Multidimensional Features Based on Multisource Remote Sensing Data: A Case Study of the Northwest Mountainous Area of Hubei Province
by Pengnan Xiao, Jianping Qian, Qiangyi Yu, Xintao Lin, Jie Xu and Yujie Liu
Remote Sens. 2025, 17(5), 908; https://doi.org/10.3390/rs17050908 - 4 Mar 2025
Viewed by 184
Abstract
Accurate identification of tea plantation distribution is critical for optimizing agricultural practices, informing land-use policies, and preserving ecological balance. However, challenges persist in mountainous regions with persistent cloud cover and heterogeneous vegetation, where conventional methods relying on single-source remote sensing features face limitations [...] Read more.
Accurate identification of tea plantation distribution is critical for optimizing agricultural practices, informing land-use policies, and preserving ecological balance. However, challenges persist in mountainous regions with persistent cloud cover and heterogeneous vegetation, where conventional methods relying on single-source remote sensing features face limitations due to spectral confusion and information redundancy. This study proposes a novel framework integrating multisource remote sensing data and feature optimization to address these challenges. Leveraging the Google Earth Engine (GEE) cloud platform, this study synthesized 108 spectral, textural, phenological, and topographic features from Sentinel-1 SAR and Sentinel-2 optical data. SVM-RFE (support vector machine recursive feature elimination) was employed to identify the optimal feature subset, prioritizing spectral indices, radar texture metrics, and terrain parameters. Comparative analysis of three classifiers, namely random forest (RF), support vector machine (SVM), and decision tree (DT), revealed that RF achieved the highest accuracy, with an overall accuracy (OA) of 95.03%, a kappa coefficient of 0.95. The resultant 10 m resolution spatial distribution map of tea plantations in Shiyan City (2023) demonstrates robust performance in distinguishing plantations from forests and farmlands, particularly in cloud-prone mountainous terrain. This methodology not only mitigates dimensionality challenges through feature optimization but also provides a scalable solution for large-scale agricultural monitoring, offering critical insights for sustainable land management and policy formulation in subtropical mountainous regions. Full article
Show Figures

Figure 1

Figure 1
<p>Study area layout.</p>
Full article ">Figure 2
<p>Time series of vegetation indices for typical land cover.</p>
Full article ">Figure 3
<p>Technical workflow of tea plantation identification.</p>
Full article ">Figure 4
<p>An example of the dynamics of vegetation for a selected tea plantation in Shiyan. (<b>a</b>) Sentinel-2 time series data in 2023 visualized as true color composites; (<b>b</b>) NDVI time series for 2023 corresponding to the true color composite in (<b>a</b>); (<b>c</b>) NDVI time series following cloud masking and snow filtering, where start of season (SoS) and end of season (EoS) correspond to the earliest and latest linearly interpolated NDVI values, respectively, above a threshold dynamically defined as 50% of the annual amplitude; and (<b>d</b>) application of the threshold method over a smoothed and interpolated time series.</p>
Full article ">Figure 5
<p>Feature selection results using SVM-RFE. (<b>a</b>) represents the results obtained with the SVM-RFE algorithm; (<b>b</b>) and (<b>c</b>) represent the mean values and variance of ground object spectral curves, respectively.</p>
Full article ">Figure 6
<p>Spatial distribution of tea plantations in Shiyan City in 2023.</p>
Full article ">Figure 7
<p>Area statistics of tea gardens in Shiyan City at different elevations and slopes in 2023.</p>
Full article ">Figure 8
<p>Comparison with MAP tea results.</p>
Full article ">Figure A1
<p>The spatial distribution of the number of (<b>a</b>) total observations, (<b>b</b>) good observations in 2023, and (<b>c</b>–<b>f</b>) good observations from Sentinel-2 data in January, April, August, and November.</p>
Full article ">Figure A2
<p>Sentinel-1 SAR image of four selected regions.</p>
Full article ">
21 pages, 19423 KiB  
Article
Analysis of Landscape Fragmentation Evolution Characteristics and Driving Factors in the Wei River Basin, China
by Changzheng Gao, Qisen Dang, Chu Li and Yongming Fan
Land 2025, 14(3), 538; https://doi.org/10.3390/land14030538 - 4 Mar 2025
Viewed by 186
Abstract
Historically, the Wei River has served as part of the Yongji Canal section of the Grand Canal, playing a crucial role in connecting northern and southern China. However, with the acceleration of urbanization in China, issues such as excessive land development and ecological [...] Read more.
Historically, the Wei River has served as part of the Yongji Canal section of the Grand Canal, playing a crucial role in connecting northern and southern China. However, with the acceleration of urbanization in China, issues such as excessive land development and ecological landscape fragmentation have emerged. Exploring the mechanisms of landscape fragmentation evolution in the Wei River basin and proposing optimization strategies is of significant importance for land use and ecological stability within small- to medium-sized river basins. This study selected land use data from the Weihe River basin between 2000 and 2020, using landscape pattern indices to analyze the trend of landscape fragmentation. The principal component analysis (PCA) and geographical detector methods were employed to explore the distribution characteristics and driving factors of landscape fragmentation. The research results indicate that: (1) The degree of landscape fragmentation in the Wei River basin has progressively intensified over time. The edge density index (ED), the landscape division index (DIVISION), the landscape shape index (LSI), and the Shannon diversity index (SHDI) have increased annually, while the contagion index (CONTAG) and area-weighted mean patch size (Area_AM) have continuously decreased; (2) Landscape fragmentation in the Wei River basin is characterized by stable changes in the source and tributary fragmentation areas, a concentrated distribution of fragmentation in the tributaries, and a significant increase in fragmentation in the main stream; (3) The analysis using the geographic detector method indicates that vegetation coverage (FVC), human activity intensity (HAI), and land use/land cover change (LUCC) are the main driving factors of landscape fragmentation in the Wei River basin. The findings explore the mechanisms of landscape fragmentation in the basin and provide a reference for land use planning and ecological restoration in the region. Full article
Show Figures

Figure 1

Figure 1
<p>Study area of the Wei River basin.</p>
Full article ">Figure 2
<p>Division of independent variables in the geographic detector.</p>
Full article ">Figure 3
<p>Land use type distribution map of the Wei River basin. (<b>a</b>–<b>c</b>) represent the land use data for the Wei River Basin in 2000, 2010, and 2020, respectively. Note: The percentages represent the proportion of each land use type’s area relative to the total area of the basin.</p>
Full article ">Figure 4
<p>Changes in the land type index of the Wei River basin from 2000 to 2020. (<b>a</b>) trend of the ED index for each land use type, (<b>b</b>) trend of the LSI index for each land use type, (<b>c</b>) trend of the Area_AM index for each land use type, and (<b>d</b>) trend of the DIVISION index for each land use type.</p>
Full article ">Figure 5
<p>Spatial distribution maps of ED, LSI, and Area_AM in the Wei River basin. (<b>a</b>–<b>c</b>) represent the county-level spatial distribution of landscape pattern indices in the Wei River Basin for 2000, 2010, and 2020, respectively.</p>
Full article ">Figure 6
<p>Spatial distribution maps of CONTAG, DIVISION, and SHDI in the Wei River basin. (<b>a</b>–<b>c</b>) represent the county-level spatial distribution of landscape pattern indices in the Wei River Basin for 2000, 2010, and 2020, respectively.</p>
Full article ">Figure 7
<p>Spatiotemporal distribution pattern of comprehensive landscape fragmentation in the Wei River basin from 2000 to 2020. (<b>a</b>–<b>c</b>) represent the spatial distribution of comprehensive landscape fragmentation in the Wei River Basin for 2000, 2010, and 2020, respectively.</p>
Full article ">Figure 8
<p>Spatial distribution map of hotspots of comprehensive landscape fragmentation in the Wei River basin from 2000 to 2020. (<b>a</b>–<b>c</b>) represent the concentrated areas of moderate and severe comprehensive landscape fragmentation in the Wei River Basin for 2000, 2010, and 2020, respectively.</p>
Full article ">Figure 9
<p>Spatiotemporal distribution pattern of landscape fragmentation in each sub-basin of the Wei River from 2010 to 2020. (<b>a</b>–<b>c</b>) represent the spatial distribution of moderate and severe comprehensive landscape fragmentation in the headwaters, tributaries, and main stream of the Wei River Basin for 2000, 2010, and 2020, respectively.</p>
Full article ">Figure 10
<p>Optimal parameter discretization results of OPGD. Note: Digital Elevation Model (X1), Fractional Vegetation Cover (X2), Normalized Difference Vegetation Index (X3), Average Annual Precipitation (X4), Average Annual Temperature (X5), Annual Average Evaporation (X6), Human Activity Intensity (X7), Road Density (X8), Population Density (X9), Nighttime Lights (X10), and Land Use Classification (X11).</p>
Full article ">Figure 11
<p>Single-factor detection of the geographic detector in the Wei River basin. (<b>a</b>) represents the factor detector results for the driving factors: Digital Elevation Model (X1), Fractional Vegetation Cover (X2), Normalized Difference Vegetation Index (X3), Average Annual Precipitation (X4), Average Annual Temperature (X5), and Annual Average Evaporation (X6). (<b>b</b>) represents the factor detector results for the driving factors: Human Activity Intensity (X7), Road Density (X8), Population Density (X9), Nighttime Lights (X10), and Land Use Classification (X11).</p>
Full article ">Figure 12
<p>Interaction detection results of the geographic detector in the Wei River basin. Note: Digital Elevation Model (X1), Fractional Vegetation Cover (X2), Normalized Difference Vegetation Index (X3), Average Annual Precipitation (X4), Average Annual Temperature (X5), Annual Average Evaporation (X6), Human Activity Intensity (X7), Road Density (X8), Population Density (X9), Nighttime Lights (X10), and Land Use Classification (X11).</p>
Full article ">Figure 13
<p>Interaction detection types of major driving factors. Note: Digital Elevation Model (X1), Fractional Vegetation Cover (X2), Normalized Difference Vegetation Index (X3), Average Annual Precipitation (X4), Average Annual Temperature (X5), Annual Average Evaporation (X6), Human Activity Intensity (X7), Road Density (X8), Population Density (X9), Nighttime Lights (X10), and Land Use Classification (X11).</p>
Full article ">
22 pages, 3827 KiB  
Article
Species Richness of Arbuscular Mycorrhizal Fungi in Heterogenous Saline Environments
by Jahangir A. Malik, Basharat A. Dar, Abdulaziz A. Alqarawi, Abdulaziz M. Assaeed, Fahad Alotaibi, Arafat Alkhasha, Abdelmalik M. Adam and Ahmed M. Abd-ElGawad
Diversity 2025, 17(3), 183; https://doi.org/10.3390/d17030183 - 4 Mar 2025
Viewed by 156
Abstract
Sabkha (inland and coastal—saline beds or saline lands) are widespread in Saudi Arabia and are distinguished by their hypersaline nature. These hypersaline habitats are commonly covered by halophytic vegetation. Moreover, Arbuscular mycorrhizal fungi (AMF) are an essential component of these habitats and exhibit [...] Read more.
Sabkha (inland and coastal—saline beds or saline lands) are widespread in Saudi Arabia and are distinguished by their hypersaline nature. These hypersaline habitats are commonly covered by halophytic vegetation. Moreover, Arbuscular mycorrhizal fungi (AMF) are an essential component of these habitats and exhibit a unique adaptation and contribute significantly to ecosystem variability, diversity, and function. Additionally, AMF from saline habitats are an essential component for the successful rehabilitation of salinity-affected areas. Despite their importance, little is known about the distribution and abundance of AMF along inland and coastal sabkhat of Saudi Arabia. Therefore, the main objective of this study was to investigate the abundance and diversity of AMF in the coastal and inland sabkhat of Saudi Arabia. Five soil samples, each from five randomly selected spots (considering the presence of dominant and co-dominant halophytic species), were collected from every location and were used to assess the AMF abundance and diversity. The study indicated that the highest number of AMF spores was recorded from Jouf, averaging ≈ 346 spores 100 g−1 dry soil, and the lowest from Uqair, averaging ≈ 96 spores 100 g−1 dry soil. A total of 25 AMF species were identified, belonging to eight identified genera viz., Acaulospora, Diversispora, Gigaspora, Scutellospora, Claroideoglomus, Funneliformis, Glomus, and Rhizophagus and five families. Of the total identified species, 52% belonged to the family Glomeraceae. Moreover, the highest number of species was isolated from the sabkha in Qasab. Additionally, Glomeraceae was abundant in all the studied locations with the highest relative abundance in Uqair (48.34%). AMF species Claroideoglomus etunicatum, Funneliformis mosseae, Glomus ambisporum, and Rhizophagus intraradices were the most frequently isolated species from all the Sabkha locations with isolation frequency (IF) ≥ 60%, and Claroideoglomus etunicatum (Ivi ≥ 50%) was the dominant species in all the studied locations. Furthermore, data on the Shannon–Wiener diversity index showed that the highest AMF species diversity was in Qaseem and Qasab habitats. The highest Pielou’s evenness index was recorded in Jouf. Moreover, the soil parameters that positively affected the diversity of identified species included Clay%, Silt%, HCO31−, OM, MC, N, and P, while some soil parameters such as EC, Na+, SO42−, and Sand% had a significant negative correlation with the isolated AMF species. This study revealed that AMF can adapt and survive the harshest environments, such as hypersaline sabkhas, and thus can prove to be a vital component in the potential restoration of salinity-inflicted/degraded ecosystems. Full article
(This article belongs to the Special Issue Microbial Community Dynamics in Soil Ecosystems)
Show Figures

Figure 1

Figure 1
<p>Map of Saudi Arabia showing the different Sabkha locations (marked as red) assessed for investigating AMF abundance and diversity. Arabic terms denote the names of the different cities as: الرياض = Riyadh; المدينة المنورة = Medina; جدة = Jeddah; مكة المكرمة = Makkah; دبي = Dubai; مسقط = Muscat; صنعاء = Sana’a; دمشق = Damascus.</p>
Full article ">Figure 2
<p>AMF spore density in the samples collected from different inland and coastal sabkha locations around Saudi Arabia. The colored bars represent mean values (<span class="html-italic">n</span> = 5), while the error bars indicate the standard error (SE). Different letters above the error bars represent significant difference (<span class="html-italic">p</span> = 0.05) based on Tukey’s test. <span class="html-italic">*** p</span> &lt; 0.0001 (Tukey test).</p>
Full article ">Figure 3
<p>Relative abundance of AMF communities at order (<b>A</b>), and family (<b>B</b>) level in the soil samples collected from different sabkha habitats.</p>
Full article ">Figure 4
<p>Relative abundance of AMF communities at genus (<b>A</b>) and species (<b>B</b>) level in the soil samples collected from different sabkha habitats.</p>
Full article ">Figure 5
<p>The variation in AMF species among different hypersaline sabkha habitats with the Shannon–Wiener diversity index (<b>A</b>); Simpson’s dominance index (<b>B</b>); and Pielou’s evenness index (<b>C</b>) of species. Different letters above the error bars represent significant differences (<span class="html-italic">p</span> = 0.05) based on Tukey’s test. <span class="html-italic">* p</span> &lt; 0.01.</p>
Full article ">Figure 6
<p>The similarity index of AMF species between different hypersaline sabkha habitats.</p>
Full article ">Figure 7
<p>A correlation heatmap of the relationship between soil parameters and the AMF species isolated along different sabkha habitats. Red colors indicate a strong positive correlation while blue indicates a significant negative correlation between species and soil parameters.</p>
Full article ">Figure 8
<p>Principal component analysis (PCA) plot showing the associations between soil physiochemical parameters and AMF species along different sabkha locations.</p>
Full article ">
Back to TopTop