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Search Results (954)

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Keywords = Chlorophyll-a

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15 pages, 1651 KiB  
Technical Note
Reconstruction of Sea Surface Chlorophyll-a Concentration in the Bohai and Yellow Seas Using LSTM Neural Network
by Qing Xu, Guiying Yang, Xiaobin Yin and Tong Sun
Remote Sens. 2025, 17(1), 174; https://doi.org/10.3390/rs17010174 - 6 Jan 2025
Abstract
In order to improve the spatiotemporal coverage of satellite Chlorophyll-a (Chl-a) concentration products in marginal seas, a physically constrained deep learning model was established in this work to reconstruct sea surface Chl-a concentration in the Bohai and Yellow Seas using a Long Short-Term [...] Read more.
In order to improve the spatiotemporal coverage of satellite Chlorophyll-a (Chl-a) concentration products in marginal seas, a physically constrained deep learning model was established in this work to reconstruct sea surface Chl-a concentration in the Bohai and Yellow Seas using a Long Short-Term Memory (LSTM) neural network. Adopting the permutation feature importance method, time sequences of several geographical and physical variables, including longitude, latitude, time, sea surface temperature, salinity, sea level anomaly, wind field, etc., were selected and integrated to the reconstruction model as input parameters. Performance inter-comparisons between LSTM and other machine learning or deep learning models was conducted based on OC-CCI (Ocean Color Climate Change Initiative) Chl-a product. Compared with Gated Recurrent Unit, Random Forest, XGBoost, and Extra Trees models, the LSTM model exhibits the highest accuracy. The average unbiased percentage difference (UPD) of reconstructed Chl-a concentration is 11.7%, which is 2.9%, 7.6%, 10.6%, and 10.5% smaller than that of the other four models, respectively. Over the majority of the study area, the root mean square error is less than 0.05 mg/m3 and the UPD is below 10%, indicating that the LSTM model has considerable potential in accurately reconstructing sea surface Chl-a concentrations in shallow waters. Full article
31 pages, 7599 KiB  
Article
Integrating Remote Sensing and Machine Learning for Dynamic Monitoring of Eutrophication in River Systems: A Case Study of Barato River, Japan
by Dang Guansan, Ram Avtar, Gowhar Meraj, Saleh Alsulamy, Dheeraj Joshi, Laxmi Narayan Gupta, Malay Pramanik and Pankaj Kumar
Water 2025, 17(1), 89; https://doi.org/10.3390/w17010089 - 1 Jan 2025
Viewed by 508
Abstract
Rivers play a crucial role in nutrient cycling, yet are increasingly affected by eutrophication due to anthropogenic activities. This study focuses on the Barato River in Hokkaido, Japan, employing an integrated approach of field measurements and Sentinel-2 satellite remote sensing to monitor eutrophication [...] Read more.
Rivers play a crucial role in nutrient cycling, yet are increasingly affected by eutrophication due to anthropogenic activities. This study focuses on the Barato River in Hokkaido, Japan, employing an integrated approach of field measurements and Sentinel-2 satellite remote sensing to monitor eutrophication as the river experiencing huge sewage effluents. Key parameters such as chlorophyll-a (Chla), dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), and Secchi Disk Depth (SDD) were analyzed. The developed empirical models showed a strong predictive capability for water quality, particularly for Chla (R2 = 0.87), DIP (R2 = 0.61), and SDD (R2 = 0.82). Seasonal analysis indicated peak Chla concentrations in October, reaching up to 92.4 μg/L, alongside significant decreases in DIN and DIP, suggesting high phytoplankton activity. Advanced machine learning models, specifically back propagation neural networks, improved the prediction accuracy with R2 values up to 0.90 for Chla and 0.83 for DIN. Temporal analyses from 2018 to 2022 consistently revealed the Barato River’s eutrophic state, with severe eutrophication occurring for 33% of the year and moderate for over 50%, emphasizing the ongoing nutrient imbalance. The strong correlation between DIP and Chla highlights phosphorus as the main driver of eutrophication. These findings demonstrate the efficacy of integrating remote sensing and machine learning for dynamic monitoring of river eutrophication, providing critical insights for nutrient management and water quality improvement. Full article
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Figure 1
<p>Study area and sampling sites. (<b>a</b>) Location of Hokkaido, Sapporo, Japan, showing the regional context of the study. (<b>b</b>) Detailed view of the Barato River, the main focus area for water quality analysis. (<b>c</b>–<b>e</b>) Photographs of the sampling sites along the Barato River, illustrating different river segments where in-situ measurements were taken. (<b>f</b>) Detailed sampling locations.</p>
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<p>Flowchart of the overall methodological framework used in this study, showing the integration of field sampling, laboratory analysis, and satellite imagery.</p>
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<p>Correlation coefficients between Sentinel-2 spectral band combinations and in-situ measurements of water quality parameters (Chla, DIN, DIP, and SDD).</p>
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<p>Empirical regression models for the inversion of eutrophication parameters using Sentinel-2 spectral bands. (<b>a</b>) Chla model based on the combination (1/B2) × (1/B4); (<b>b</b>) DIN model using the band ratio B4/B3; (<b>c</b>) DIP model derived from the combination (B4/B3) − B5; (<b>d</b>) SDD model using the natural logarithmic transformation ln(B3/B7). The strong linear relationships depicted indicate the predictive potential of the spectral band combinations for estimating each eutrophication parameter.</p>
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<p>Accuracy assessment of empirical inversion models for eutrophication parameters. (<b>a</b>) Chla, (<b>b</b>) DIN, (<b>c</b>) DIP, and (<b>d</b>) SDD. Each plot compares the predicted and measured values of the respective parameters, providing an assessment of model accuracy.</p>
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<p>Staged seasonal modeling results for Chla and DIN. Separate models were developed for warm and cold seasons, with datasets from each season split into training and validation subsets. (<b>a</b>) Cool season inversion model for Chla, using the 1/B2 band combination, achieving an R<sup>2</sup> of 0.70, indicating a strong correlation between spectral data and measured Chla concentrations. (<b>b</b>) Cool season inversion model for DIN, based on the (1/B3) − (1/B4) band combination, with an R<sup>2</sup> of 0.69, reflecting an improved predictive performance for DIN concentrations in the cool season.</p>
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<p>Performance of BP neural network inversion models for predicting eutrophication parameters. Models were independently trained and validated within warm and cold season datasets. (<b>a</b>) Chla in the warm season, (<b>b</b>) Chla in the cold season, (<b>c</b>) DIN in the warm season, (<b>d</b>) DIN in the cold season, (<b>e</b>) DIP, and (<b>f</b>) SDD. Each plot compares estimated values from the BP neural network models against measured field data, demonstrating significant improvements in model accuracy.</p>
Full article ">Figure 7 Cont.
<p>Performance of BP neural network inversion models for predicting eutrophication parameters. Models were independently trained and validated within warm and cold season datasets. (<b>a</b>) Chla in the warm season, (<b>b</b>) Chla in the cold season, (<b>c</b>) DIN in the warm season, (<b>d</b>) DIN in the cold season, (<b>e</b>) DIP, and (<b>f</b>) SDD. Each plot compares estimated values from the BP neural network models against measured field data, demonstrating significant improvements in model accuracy.</p>
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<p>Accuracy assessment of BP neural network-based inversion models for eutrophication parameters across different seasons. (<b>a</b>) Model performance for Chla in the warm season. (<b>b</b>) Model performance for Chla in the cold season. (<b>c</b>) Model performance for DIN in the warm season. (<b>d</b>) Model performance for DIN in the cold season. (<b>e</b>) Model performance for DIP. (<b>f</b>) Model performance for SDD. These plots indicate the prediction accuracy of the BP neural network models for various water quality parameters.</p>
Full article ">Figure 8 Cont.
<p>Accuracy assessment of BP neural network-based inversion models for eutrophication parameters across different seasons. (<b>a</b>) Model performance for Chla in the warm season. (<b>b</b>) Model performance for Chla in the cold season. (<b>c</b>) Model performance for DIN in the warm season. (<b>d</b>) Model performance for DIN in the cold season. (<b>e</b>) Model performance for DIP. (<b>f</b>) Model performance for SDD. These plots indicate the prediction accuracy of the BP neural network models for various water quality parameters.</p>
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<p>Temporal dynamics of water quality parameters in 2021. The concentration changes in the four key parameters throughout 2021: (<b>a</b>) Chla in μmol/L; (<b>b</b>) DIN in μmol/L; (<b>c</b>) DIP in μmol/L; (<b>d</b>) SDD in meters.</p>
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<p>Temporal trends of normalized water quality parameters in 2021. The graph displays the normalized concentrations of Chla, DIN, DIP, and SDD throughout the year. This graph highlights the relationships and variations between Chla, DIN, DIP, and SDD over time.</p>
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<p>Temporal changes in water quality parameters of the Barato River in 2018. (<b>a</b>) Chla, (<b>b</b>) DIN, (<b>c</b>) DIP, and (<b>d</b>) SDD.</p>
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<p>Temporal changes in water quality parameters of the Barato River in 2019. (<b>a</b>) Chla, (<b>b</b>) DIN, (<b>c</b>) DIP, and (<b>d</b>) SDD.</p>
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<p>Temporal changes in water quality parameters of the Barato River in 2020. (<b>a</b>) Chla, (<b>b</b>) DIN, (<b>c</b>) DIP, and (<b>d</b>) SDD.</p>
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<p>Temporal changes in water quality parameters of the Barato River in 2022. (<b>a</b>) Chla, (<b>b</b>) DIN, (<b>c</b>) DIP, and (<b>d</b>) SDD.</p>
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<p>Temporal dynamics of eutrophication indicators in the Barato River for 2021. (<b>a</b>) TSIM of Chla indicating fluctuations from slight to severe eutrophication throughout the year. (<b>b</b>) Pi for DIN showing significant variability, spanning from unpolluted to severely polluted states. (<b>c</b>) Pi for DIP, which consistently remains in the mild pollution category throughout the year. (<b>d</b>) Pie chart of TSIM illustrating that severe eutrophication occurred for 33% of the year, moderate eutrophication occurred for 54%, and slight eutrophication occurred for 13%. (<b>e</b>) Distribution of Pi for DIN, showing 48% unpolluted, 18% mild pollution, 32% moderate pollution, and 2% severe pollution. (<b>f</b>) Pie chart of Pi for DIP being consistently in a mild pollution state for the entire year, indicating sustained nutrient availability.</p>
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<p>Temporal dynamics and distribution of eutrophication indicators in the Barato River for 2022. (<b>a</b>) TSIM of Chla showing a consistent eutrophic state throughout the year. (<b>b</b>) TSIM values indicate a slight increase compared to 2021. (<b>c</b>) Pi for DIP, consistently indicating mild pollution throughout the year. (<b>d</b>) Pie chart illustrating TSIM distribution: slight eutrophication accounted for 15%, moderate eutrophication for 50%, and severe eutrophication for 35%. (<b>e</b>) Distribution of Pi for DIN, showing unpolluted conditions for 47% of the year, mild pollution for 36%, and moderate pollution for 17%. (<b>f</b>) Pie chart for Pi of DIP showing 100% mild pollution throughout the year.</p>
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26 pages, 2749 KiB  
Article
Environmental Assessment Using Phytoplankton Diversity, Nutrients, Chlorophyll-a, and Trophic Status Along Southern Coast of Jeddah, Red Sea
by Bandar A. Al-Mur
J. Mar. Sci. Eng. 2025, 13(1), 29; https://doi.org/10.3390/jmse13010029 - 29 Dec 2024
Viewed by 300
Abstract
The objective of this study is to better identify the state of eutrophication of coastal waters along the southern coast of the city of Jeddah in the Red Sea. Thirty-six samples from surface seawater were collected during the spring and autumn of 2021. [...] Read more.
The objective of this study is to better identify the state of eutrophication of coastal waters along the southern coast of the city of Jeddah in the Red Sea. Thirty-six samples from surface seawater were collected during the spring and autumn of 2021. Water temperature, pH, salinity, dissolved oxygen (DO), nutrients, and chlorophyll-a (Chl-a) content were examined as a guide of water quality indicators. The present data revealed low levels of Chl-a content (in the range of 0.11–0.24 µg L−1). The average concentrations of DIN (dissolved inorganic nitrogen) forms follow the order NO3-N > NH4-N ~ NO2-N (representing about 11.4–29.4% of the total nitrogen). To investigate the trophic status and water quality, numerical indicators were applied to the results of the analysis of chemical variables (NH4-N, NO3-N, and PO4-P) and the biological analysis (Chl-a) in the aqueous environment within the study area. These indicators are simplified based on the specialist, the non-specialist, the decision-maker, and the one responsible for managing the coastal areas. We also obtain through this method a single numerical value that expresses the state of the coastal waters. According to the analysis of phosphorus and nitrogen data and a trophic index (TRIX), the study area’s trophic status was determined as oligotrophic, due to low nutrient concentrations in the seawater. The current study identified a total of 58 species of phytoplankton comprised four classes in the investigated areas; Bacillariophyceae was the dominant algal class (Diatoms 30 species), followed by Chlorophyceae (9 species), Dinophyceae (11 species), and Cyanophyceae (8 species). Seasonally, spring recorded the highest value of total phytoplankton, recording a value of 251 × 103 cells/L with a percentage of 61%, while autumn recorded the lowest value of 186 × 103 cells/L with a percentage of 39%. Phytoplankton classes can be arranged in order of prevalence as follows: Bacillariophyceae >> Dinophyceae > Chlorophyceae > Cyanophyceae. Full article
(This article belongs to the Section Marine Environmental Science)
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<p>Sampling stations (1–18) of the study area.</p>
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<p>Spatial and temporal variations in physical and chemical parameters in the coastal region south of Jeddah in the Red Sea.</p>
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<p>Spatial and temporal changes in concentrations of NH<sub>4</sub>, NO<sub>2</sub>, NO<sub>3</sub>, TN, DIN, and DIN/TN in the coastal area south of Jeddah, Red Sea.</p>
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<p>Spatial and temporal changes in concentrations of chlorophyll-a (Chl-a), SiO<sub>4</sub>, reactive phosphate (PO<sub>4</sub>-P) and total phosphorus (TP).in the coastal area south of Jeddah, Red Sea.</p>
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<p>The abundance of phytoplankton composition in the coastal water of Jeddah during the period of 2022.</p>
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<p>The percentage abundance of phytoplankton composition in the coastal water of Jeddah during the period of 2022.</p>
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<p>Spatial assessments of the trophic status using the EUI based on NO<sub>3</sub>, NH<sub>4</sub>, and PO<sub>4</sub> concentration, eutrophication level (Ei), and TRIX values.</p>
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<p>The spatiotemporal trends of the diversity index and the number of planktonic species.</p>
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<p>The stoichiometric N/P ratios during the spring and autumn period in the coastal area south of Jeddah, Red Sea.</p>
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21 pages, 18678 KiB  
Article
Response of Subsurface Chlorophyll Maximum Depth to Evolution of Mesoscale Eddies in Kuroshio–Oyashio Confluence Region
by Ziwei Chuang, Chunling Zhang, Jiahui Fan and Huangxin Yang
J. Mar. Sci. Eng. 2025, 13(1), 24; https://doi.org/10.3390/jmse13010024 - 28 Dec 2024
Viewed by 300
Abstract
The subsurface chlorophyll maximum depth (SCMD) is an indicator of the spatial activity of marine organisms and changes in the ecological environment. Ubiquitous mesoscale eddies are among the important factors regulating the Kuroshio–Oyashio confluence region. In this study, we use satellite altimeter observations [...] Read more.
The subsurface chlorophyll maximum depth (SCMD) is an indicator of the spatial activity of marine organisms and changes in the ecological environment. Ubiquitous mesoscale eddies are among the important factors regulating the Kuroshio–Oyashio confluence region. In this study, we use satellite altimeter observations and high-resolution reanalysis data to explore seasonal variations in the SCMD and its responses to different types of eddies based on methods of composite averaging and normalization. The results show that variations in the SCMD induced by the evolution of the eddies were prominent in the summer and autumn. The monopoles of the SCMD exhibited internally shallow and externally deep features in the cyclonic eddies (CEs), while the contrary trend was observed in the anticyclonic eddies (ACEs). The SCMD was positively correlated with the intensity of the eddies and sea surface temperature, and was negatively correlated with the depth of the mixed layer. These correlations were more pronounced in the CEs (summer) and ACEs (autumn). Both the CEs and ACEs prompted the westward transport of chlorophyll-a (Chl-A), where ACEs transported it over a longer distance than the CEs. Full article
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<p>Research area (<b>a</b>) and sea surface current corresponding to Chl-A on 3 June 2020 (<b>b</b>). The black frame in panel (<b>a</b>) denotes the research area. Blue and red arrows and circles represent CEs and ACEs, respectively.</p>
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<p>The number of eddies generated in different seasons.</p>
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<p>Anomalies in Chl-A over an area three times the radius of the eddy during different stages of its evolution. (<b>a1</b>–<b>a3</b>) represent anomalies in Chl-A corresponding to the stages of development, stability, and decay of CEs, while (<b>b1</b>–<b>b3</b>) represent the corresponding anomalies for ACEs. The solid black line represents the mean radius of the eddy, and the dashed black line represents twice its radius. The eastward and northward directions were set as the positive axes of the longitude and latitude, respectively. The anomalies in Chl-A concentration were obtained by subtracting the spatial average value within the region of the eddy, to obtain the composite average of each part for all eddies.</p>
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<p>The south–north sections of Chl-A concentration along the meridians of centers of the CEs (<b>a1</b>–<b>a4</b>) and ACEs (<b>b1</b>–<b>b4</b>) in different seasons. The positive radius is directed northward and the negative radius southward. The solid and dashed lines represent the mean radius and twice the mean radius, respectively.</p>
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<p>Spatial distributions of the SCMD in CEs and ACEs in different seasons. (<b>a1</b>–<b>a4</b>) show the horizontal distribution of the SCMD of the CEs, and (<b>b1</b>–<b>b4</b>) show the horizontal distribution of the SCMD of the ACEs. The solid black lines represent the mean eddy radius and the dashed black lines represent twice the eddy radius. (<b>c1</b>–<b>c4</b>) show the vertical profile of the average Chl-A concentration within the mean eddy radius. The dashed blue and red lines denote the SCMDs in the CEs and ACEs, respectively. (<b>d1</b>–<b>d4</b>) show the observed chlorophyll profiles in the eddies. “N” indicates the number of profiles.</p>
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<p>Spatiotemporal distributions of the SCMD of the CEs in summer (<b>a1</b>–<b>a3</b>,<b>b1</b>–<b>b3</b>) and autumn (<b>c1</b>–<b>c3</b>,<b>d1</b>–<b>d3</b>) in different stages of eddy evolution. (<b>a1</b>–<b>a3</b>,<b>c1</b>–<b>c3</b>) show the distributions of the SCMD in the stages of development, stability, and decay of the eddy, while (<b>b1</b>–<b>b3</b>,<b>d1</b>–<b>d3</b>) show the radially averaged monopoles of the SCMD.</p>
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<p>Spatiotemporal distributions of the SCMD of the ACEs in summer (<b>a1</b>–<b>a3</b>,<b>b1</b>–<b>b3</b>) and autumn (<b>c1</b>–<b>c3,d1</b>–<b>d3</b>) in different stages of eddy evolution. (<b>a1</b>–<b>a3</b>,<b>c1</b>–<b>c3</b>) show the distributions of the SCMD in the stages of development, stability, and decay of the eddy, while (<b>b1</b>–<b>b3</b>,<b>d1</b>–<b>d3</b>) show the radially averaged monopoles of the SCMD.</p>
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<p>Time series of the SCMD, <span class="html-italic">APD</span>, SST, and MLD within the mean radius of the eddies on each day. (<b>a1</b>,<b>a2</b>) show the sequences of parameters of the CEs, while (<b>b1</b>,<b>b2</b>) show those of the ACEs.</p>
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<p>Changes in the SCMD, <span class="html-italic">APD</span>, SST, and MLD within the mean radius of the eddies during their evolution in summer (<b>a1</b>,<b>b1</b>) and autumn (<b>a2</b>,<b>b2</b>). (<b>a</b>) shows the CEs and (<b>b</b>) shows the ACEs.</p>
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<p>Spatial distributions of the SCM in the stages of development, stability, and decay of eddy evolution. (<b>a1</b>–<b>a3</b>) CEs. (<b>b1</b>–<b>b3</b>) ACEs.</p>
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<p>Spatiotemporal transport of the SCM by the CEs (<b>a</b>) and ACEs (<b>b</b>) during their evolution. (<b>a1</b>–<b>a3</b>) represent SCM transport during the stages of development, stability, and decay of the CEs, while (<b>b1</b>–<b>b3</b>) show the corresponding results for the ACEs. The direction of the polar coordinates was divided into 16 azimuthal angles, and the radius was assumed to be the relative distance from the eddy center.</p>
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12 pages, 1633 KiB  
Article
Habitat Assessment for the Spiny Red Gurnard Chelidonichthys spinosus Using Habitat Suitability Index in the East China Sea and Southern Yellow Sea
by Hanye Zhang, Zunlei Liu, Xiaojing Song, Jiahua Cheng and Jianzhong Ling
Diversity 2025, 17(1), 10; https://doi.org/10.3390/d17010010 - 26 Dec 2024
Viewed by 133
Abstract
Chelidonichthys spinosus is a common fish distributed in the Northwest Pacific. To ensure sustainable utilization, it is crucial to understand the potential impacts of environmental changes on habitat suitability. A habitat suitability index (HSI) model was developed for C. spinosus based on seasonal [...] Read more.
Chelidonichthys spinosus is a common fish distributed in the Northwest Pacific. To ensure sustainable utilization, it is crucial to understand the potential impacts of environmental changes on habitat suitability. A habitat suitability index (HSI) model was developed for C. spinosus based on seasonal bottom trawling survey data and remote-sensing oceanographic data collected in the East China Sea and southern Yellow Sea from 2015 to 2017. The model examined the relationships between the spatio-temporal distribution of fish and environmental variables. The suitable ranges of sea bottom temperature, sea bottom salinity, depth and chlorophyll-a for C. spinosus in four seasons were identified. Each variable was then combined into the HSI model with weights defined by the Gradient Boosting Regression Tree. The spatial distribution and the centroid of the HSI revealed that C. spinosus exhibits a seasonal southward and southwestward migratory pattern throughout the year. This migration pattern indicates the suitable habitats for reproductive, feeding, and overwintering activities. The conservation of C. spinosus resources is a matter of great urgency, and some of the feasible proposals have been put forth in this purpose. Full article
(This article belongs to the Special Issue Diversity and Spatiotemporal Distribution of Nekton)
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<p>Map of the study area, with red and blue solid lines representing warm and cold currents, respectively (KC, Kuroshio Current; YSWC, Yellow Sea Warm Current; TWC, Taiwan Warm Current; CCC, China Coastal Current; YDW, Yangtze River diluted water; YSCWM, Yellow Sea Cold Water Mass; FFLMT, forbidden fishing line of motorized trawling).</p>
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<p>SI curves of environmental variables for <span class="html-italic">C. spinosus</span>.</p>
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<p>Relative contribution of different environmental variables based on GBRT.</p>
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<p>Spatial distribution and weighted SDE of the HSI for <span class="html-italic">C. spinosus</span> in four seasons.</p>
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17 pages, 2965 KiB  
Article
Typhoon Effects on Surface Phytoplankton Biomass Based on Satellite-Derived Chlorophyll-a in the East Sea During Summer
by HwaEun Jung, JiSuk Ahn, Jae Joong Kang, Jae Dong Hwang, SeokHyun Youn, HyunJu Oh, HuiTae Joo and Changsin Kim
J. Mar. Sci. Eng. 2024, 12(12), 2369; https://doi.org/10.3390/jmse12122369 - 23 Dec 2024
Viewed by 471
Abstract
The East Sea is a jointly managed maritime area of Korea, Russia, and Japan, where the frequency of strong typhoons is anticipated to increase with climate change, affecting its marine ecosystem and regional climate regulation. This study investigated the environmental and ecological impacts [...] Read more.
The East Sea is a jointly managed maritime area of Korea, Russia, and Japan, where the frequency of strong typhoons is anticipated to increase with climate change, affecting its marine ecosystem and regional climate regulation. This study investigated the environmental and ecological impacts of summer typhoons entering the East Sea by analyzing satellite-derived chlorophyll-a (Chl-a) data, Argo float measurements, and ERA5 wind data. Our findings revealed that summer typhoons generally increased surface Chl-a concentrations by 65.4%, with typhoon intensity substantially influencing this process. Weak typhoons caused marginal Chl-a increases attributed to redistribution rather than nutrient supply, whereas normal and strong typhoons increased Chl-a through enhanced vertical mixing and nutrient upwelling in the East Sea. Stronger typhoons notably impacted the mixed layer depth and isothermal layer depth, leading to greater Chl-a concentrations within the strong wind radius. However, the increased Chl-a magnitude was lower than that of other strong typhoons in other regions. The East Sea uniquely responds to typhoons with fewer upper environment changes, possibly due to a stable barrier layer limiting vertical mixing. These findings underscore the importance of continuous monitoring and integrated observational methods in order to better understand the ecological effects of typhoons, particularly as their intensity increases with climate change. Full article
(This article belongs to the Section Marine Environmental Science)
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<p>The pathway of typhoons and Argo float location during the study period. The dotted lines are pathways of typhoons. The triangles denote the locations of typhoons each day. The circle and asterisks indicate the Argo float location before and after typhoons, respectively. The colors of circles and asterisks indicate typhoon type. (Blue is SOULIK, green is TAPA, orange is MAYSAK, and red is HAISHEN).</p>
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<p>The surface Chl-<span class="html-italic">a</span> concentration in the strong wind radius of each typhoon during typhoons of SOULIK, TAPA, and MAYSAK AND HAISHEN (MH) in the strong wind radius of typhoons. (<b>A</b>) before. (<b>B</b>) after. (<b>C</b>) difference between before and after. The line represents the pathway of the typhoon.</p>
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<p>Vertical temperature profiles measured by ARGO Floats before and after typhoons ((<b>a</b>)-SOULIK, (<b>b</b>)-TAPA, (<b>c</b>)-MH).</p>
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<p>Average Ekman Depth (D<sub>E</sub>) of strong wind radius during typhoons SOULIK (<b>a</b>), TAPA (<b>b</b>), MH, and (<b>c</b>) in the East Sea (The black and yellow lines indicate the pathway of typhoons).</p>
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15 pages, 7166 KiB  
Article
Algal Pigment Estimation Models to Assess Bloom Toxicity in a South American Lake
by Lien Rodríguez-López, David Francisco Bustos Usta, Lisandra Bravo Alvarez, Iongel Duran-Llacer, Luc Bourrel, Frederic Frappart, Rolando Cardenas and Roberto Urrutia
Water 2024, 16(24), 3708; https://doi.org/10.3390/w16243708 - 22 Dec 2024
Viewed by 708
Abstract
In this study, we build an empirical model to estimate pigments in the South American Lake Villarrica. We use data from Dirección General de Aguas de Chile during the period of 1989–2024 to analyze the behavior of limnological parameters and trophic condition in [...] Read more.
In this study, we build an empirical model to estimate pigments in the South American Lake Villarrica. We use data from Dirección General de Aguas de Chile during the period of 1989–2024 to analyze the behavior of limnological parameters and trophic condition in the lake. Four seasonal linear regression models were developed by us, using a set of water quality variables that explain the values of phycocyanin pigment in Lake Villarrica. In the first case, we related chlorophyll-a (Chl-a) to phycocyanin, expecting to find a direct relationship between both variables, but this was not fulfilled for all seasons of the year. In the second case, in addition to Chl-a, we included water temperature, since this parameter has a great influence on the algal photosynthesis process, and we obtained better results. We discovered a typical seasonal variability given by temperature fluctuations in Lake Villarrica, where in the spring, summer, and autumn seasons, conditions are favorable for algal blooms, while in winter, the natural seasonal conditions do not allow increases in algal productivity. For a third case, we included the turbidity variable along with the variables mentioned above and the statistical performance metrics of the models improved significantly, obtaining R2 values of up to 0.90 in the case of the model for the fall season and a mean squared error (MSE) of 0.04 µg/L. In the last case used, we added the variable dissolved organic matter (MOD), and the models showed a slight improvement in their performance. These models may be applicable to other lakes with harmful algal blooms in order to alert the community to the potential toxicity of these events. Full article
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<p>(<b>a</b>) South America continent, (<b>b</b>) Chile in Latin America, (<b>c</b>) Region de la Araucanía and the location of Lake Villarrica in the black box, (<b>d</b>) Lake Villarrica and seven sampling stations.</p>
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<p>Behavior of limnological parameters in Lake Villarrica during the period 2021–2024.</p>
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<p>Correlation matrix between the predictors (NTU, Temp, O_D, Chl-a, MOD) and the dependent variable (PC) (<a href="#sec2dot3-water-16-03708" class="html-sec">Section 2.3</a> and <a href="#sec2dot4-water-16-03708" class="html-sec">Section 2.4</a>).</p>
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<p>Model performance is evaluated through a time series plot of predicted vs. actual FCA values (left) and comparisons of R<sup>2</sup> scores (top right) and mean squared errors (bottom right) across different models.</p>
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<p>Phytoplankton community present in Lake Villarica and their abundance according to depth over 2021–2024.</p>
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<p>Abundance percent of algal species in Lake Villarica over 2021–2024.</p>
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31 pages, 12950 KiB  
Article
Exploring Trends and Variability of Water Quality over Lake Titicaca Using Global Remote Sensing Products
by Vann Harvey Maligaya, Analy Baltodano, Afnan Agramont and Ann van Griensven
Remote Sens. 2024, 16(24), 4785; https://doi.org/10.3390/rs16244785 - 22 Dec 2024
Viewed by 424
Abstract
Understanding the current water quality dynamics is necessary to ensure that ecological and sociocultural services are provided to the population and the natural environment. Water quality monitoring of lakes is usually performed with in situ measurements; however, these are costly, time consuming, laborious, [...] Read more.
Understanding the current water quality dynamics is necessary to ensure that ecological and sociocultural services are provided to the population and the natural environment. Water quality monitoring of lakes is usually performed with in situ measurements; however, these are costly, time consuming, laborious, and can have limited spatial coverage. Nowadays, remote sensing offers an alternative source of data to be used in water quality monitoring; by applying appropriate algorithms to satellite imagery, it is possible to retrieve water quality parameters. The use of global remote sensing water quality products increased in the last decade, and there are a multitude of products available from various databases. However, in Latin America, studies on the inter-comparison of the applicability of these products for water quality monitoring is rather scarce. Therefore, in this study, global remote sensing products estimating various water quality parameters were explored on Lake Titicaca and compared with each other and sources of data. Two products, the Copernicus Global Land Service (CGLS) and the European Space Agency Lakes Climate Change Initiative (ESA-CCI), were evaluated through a comparison with in situ measurements and with each other for analysis of the spatiotemporal variability of lake surface water temperature (LSWT), turbidity, and chlorophyll-a. The results of this study showed that the two products had limited accuracy when compared to in situ data; however, remarkable performance was observed in terms of exhibiting spatiotemporal variability of the WQ parameters. The ESA-CCI LSWT product performed better than the CGLS product in estimating LSWT, while the two products were on par with each other in terms of demonstrating the spatiotemporal patterns of the WQ parameters. Overall, these two global remote sensing water quality products can be used to monitor Lake Titicaca, currently with limited accuracy, but they can be improved with precise pixel identification, accurate optical water type definition, and better algorithms for atmospheric correction and retrieval. This highlights the need for the improvement of global WQ products to fit local conditions and make the products more useful for decision-making at the appropriate scale. Full article
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<p>Lake Titicaca Landsat Satellite Image, 10 April 2013.</p>
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<p>Measurement frequency of the monitoring points over Lake Titicaca across 14 monitoring campaigns.</p>
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<p>Identified Water Quality Hotspots in Lake Titicaca.</p>
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<p>Long-term monthly mean LSWT maps for the period 2010–2020 for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI.</p>
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<p>Long-term monthly mean turbidity maps for the period 2010–2020 for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI.</p>
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<p>Long-term monthly mean chlorophyll-a concentration maps for the period 2010–2020 for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI.</p>
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<p>Temporal Pattern Comparison of Lake Surface Water Temperature (LSWT) for the Remote Sensing Products at Each Water Quality Hotspot (WQH).</p>
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<p>Temporal Pattern Comparison of Turbidity for the Remote Sensing Products at Each Water Quality Hotspot (WQH).</p>
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<p>Temporal Pattern Comparison of Chlorophyll-a Concentration for the Remote Sensing Products at Each Water Quality Hotspot (WQH).</p>
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<p>Mapped Mann–Kendall Test Results for Lake Surface Water Temperature.</p>
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<p>(<b>a</b>) Mapped Mann–Kendall Test Results for Turbidity and (<b>b</b>) Lake Aggregated Time Series of the Turbidity Data Indicating the Calculated MK Trend.</p>
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<p>(<b>a</b>) Mapped Mann–Kendall Test Results for Chlorophyll-a and (<b>b</b>) Lake Aggregated Time Series of the Chlorophyll-a Data Indicating the Calculated MK Trend.</p>
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<p>Scatterplot of RS, derived vs. in situ measured, LSWT for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI, considering all monitoring campaigns.</p>
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<p>Scatterplot of RS, derived vs. in situ measured, turbidity for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI, considering all monitoring campaigns.</p>
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<p>Scatterplot of RS, derived vs. in situ measured, LSWT for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI, considering only monitoring campaigns with the indicated dates.</p>
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<p>Scatterplot of RS, derived vs. in situ measured, turbidity for (<b>a</b>) CGLS and (<b>b</b>) ESA-CCI, considering only monitoring campaigns with the indicated dates.</p>
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26 pages, 15194 KiB  
Article
Cross-Attention-Based High Spatial-Temporal Resolution Fusion of Sentinel-2 and Sentinel-3 Data for Ocean Water Quality Assessment
by Yanfeng Wen, Peng Chen, Zhenhua Zhang and Yunzhou Li
Remote Sens. 2024, 16(24), 4781; https://doi.org/10.3390/rs16244781 - 22 Dec 2024
Viewed by 318
Abstract
Current marine research that leverages remote sensing data urgently requires gridded data of high spatial and temporal resolution. However, such high-quality data is often lacking due to the inherent physical and technical constraints of sensors. A necessary trade-off therefore exists between spatial, temporal, [...] Read more.
Current marine research that leverages remote sensing data urgently requires gridded data of high spatial and temporal resolution. However, such high-quality data is often lacking due to the inherent physical and technical constraints of sensors. A necessary trade-off therefore exists between spatial, temporal, and spectral resolution in satellite remote sensing technology: increasing spatial resolution often reduces the coverage area, thereby diminishing temporal resolution. This manuscript introduces an innovative remote sensing image fusion algorithm that combines Sentinel-2 (high spatial resolution) and Sentinel-3 (relatively high spectral and temporal resolution) satellite data. The algorithm, based on a cross-attention mechanism and referred to as the Cross-Attention Spatio-Temporal Spectral Fusion (CASTSF) model, accounts for variations in spectral channels, spatial resolution, and temporal phase among different sensor images. The proposed method enables the fusion of atmospherically corrected ocean remote sensing reflectance products (Level 2 OSR), yielding high-resolution spatial data at 10 m resolution with a temporal frequency of 1–2 days. Subsequently, the algorithm generates chlorophyll-a concentration remote sensing products characterized by enhanced spatial and temporal fidelity. A comparative analysis against existing chlorophyll-a concentration products demonstrates the robustness and effectiveness of the proposed approach, highlighting its potential for advancing remote sensing applications. Full article
(This article belongs to the Section Ocean Remote Sensing)
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<p>Study area schematic.</p>
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<p>Spectral channel coverage schematic.</p>
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<p>Overall Flowchart.</p>
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<p>CASTSF model structure diagram.</p>
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<p>Flowchart of fitting task.</p>
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<p>Input images and output results of the CASTSF model in Region A vs. other models. (<b>a</b>) T0-LR, (<b>b</b>) T0-HR, (<b>c</b>) T1-LR, (<b>d</b>) T1-HR, (<b>e</b>) STARFM, (<b>f</b>) FSDAF, (<b>g</b>) SSR-NET, (<b>h</b>) MLFF-GAN, (<b>i</b>) CASTSF.</p>
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<p>Input images and output results of the CASTSF model in Region B vs. other models. (<b>a</b>) T0-LR, (<b>b</b>) T0-HR, (<b>c</b>) T1-LR, (<b>d</b>) T1-HR, (<b>e</b>) STARFM, (<b>f</b>) FSDAF, (<b>g</b>) SSR-NET, (<b>h</b>) MLFF-GAN, (<b>i</b>) CASTSF.</p>
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<p>Comparison of quantitative scores for fitting models. (<b>a</b>) NN-Fit, (<b>b</b>) OC4ME-Fit.</p>
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<p>Fitting scatter plots for different methods on NN-dataset. (<b>a</b>) LR, (<b>b</b>) LassoCV, (<b>c</b>) DNN, (<b>d</b>) CART, (<b>e</b>) XGBoost, (<b>f</b>) KNN, (<b>g</b>) RF.</p>
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<p>Scatter plot of fitting results for different models on two types of CHL-NN data. (<b>a</b>) LR, (<b>b</b>) LassoCV, (<b>c</b>) DNN, (<b>d</b>) CART, (<b>e</b>) XGBoost, (<b>f</b>) KNN, (<b>g</b>) RF.</p>
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<p>Visualization of the two types of 10 m spatial resolution chlorophyll-a concentration products predicted for Regions A and B based on the CASTSF fusion results. (<b>a</b>) Region A-CASTSF-NN, (<b>b</b>) Region A-CASTSF-OC4ME, (<b>c</b>) Region B-CASTSF-NN, (<b>d</b>) Region B-CASTSF-OC4ME.</p>
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<p>Visual comparison of the 10 m spatial resolution chlorophyll-a concentration products predicted for Region A from the CASTSF fusion results and the existing 300 m spatial resolution S3 products. (<b>a</b>) CASTSF-NN-10 m, (<b>b</b>) S3-NN-300 m, (<b>c</b>) CASTSF-OC4M-10 m, (<b>d</b>) S3-OC4ME-300 m.</p>
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<p>Visual comparison of the 10 m spatial resolution chlorophyll-a concentration products predicted for Region B from the CASTSF fusion results and the existing 300 m spatial resolution S3 products. (<b>a</b>) CASTSF-NN, (<b>b</b>) S3-OC4ME, (<b>c</b>) CASTSF-OC4ME, (<b>d</b>) S3-OC4ME.</p>
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<p>Comparison of data from different datasets across two regions. (<b>a</b>) Scatter plot of NN vs. OC4ME in Region A, (<b>b</b>) histogram of difference (NN—OC4ME) in Region A, (<b>c</b>) scatter plot of NN vs. OC4ME in Region B, (<b>d</b>) histogram of difference (NN—OC4ME) in Region B.</p>
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18 pages, 6588 KiB  
Article
Three-Year Follow-Up Assessment of Anthropogenic Contamination in the Nichupte Lagoon
by Jorge Herrera-Silveira, Flor Arcega-Cabrera, Karina León-Aguirre, Elizabeth Lamas-Cosio, Ismael Oceguera-Vargas, Elsa Noreña-Barroso, Daniela Medina-Euán and Claudia Teutli-Hernández
Appl. Sci. 2024, 14(24), 11889; https://doi.org/10.3390/app142411889 - 19 Dec 2024
Viewed by 597
Abstract
Tourism still represents a means of generating revenues in the coastal areas in the Mexican Caribbean, despite the growing concern about the social and environmental impacts. The Nichupte Lagoon System (NLS), the most representative lagoon of Quintana Roo State for being in the [...] Read more.
Tourism still represents a means of generating revenues in the coastal areas in the Mexican Caribbean, despite the growing concern about the social and environmental impacts. The Nichupte Lagoon System (NLS), the most representative lagoon of Quintana Roo State for being in the middle of Cancun’s hotel development, has experienced a continuous drop-off in its water quality due to several factors, including dredging and wastewater discharges from different anthropogenic activities, which modify the flux of nutrients, increase the number of pathogenic microorganisms, and promote physicochemical changes in this ecosystem. Three sampling campaigns (2018, 2019, and 2020) were carried out in the NLS in August, which is the month of greatest tourist occupancy. To evidence the presence of anthropogenic wastewater in the NLS, the caffeine tracer was used, and to determine the water quality, 43 sampling stations were monitored for “in situ” physicochemical parameters (salinity and dissolved oxygen), and water samples were collected for the quantification of nutrients (NO2 + NO3, NH4+, SRP and SRSi) and chlorophyll-a (Chl-a). For data analysis, the lagoon was subdivided into five zones (ZI, ZII, ZIII, ZIV, and ZV). Caffeine spatial and time variation evidence (1) the presence of anthropogenic wastewater in all areas of the NLS probably resulting from the tourist activity, and (2) wastewater presence is directly influenced by the coupling of the hydrological changes driven by anomalous rain events and the number of tourists. This same tendency was observed for nutrients that increased from 2018 to 2019 and the trophic state changed from oligotrophic to hypertrophic in all areas, as a result of previous anomalous precipitations in 2018, followed by normal precipitations in 2019. From 2019 to 2020, the nutrients decreased due to the drop in tourism due to COVID-19, promoting fewer nutrients in the lagoon, but, also coupled with an anomalous precipitation event (Cristobal storm), resulted in a dilution phenomenon and an oligotrophic state. The cluster analysis indicated that the least similar zones in the lagoon were the ZI and ZV due to their geomorphology that restricts the connection with the rest of the system. Principal component analysis revealed that wastewater presence evidenced by the caffeine tracer had a positive association with dissolved oxygen and chlorophyll-a, indicating that the arrival of nutrients from wastewater amongst other sources promotes algal growth, but this could develop into an eutrophic or hypertrophic state under normal precipitation conditions as seen in 2019. This study shows the relevance of monitoring in time of vulnerable karstic systems that could be affected by anthropogenic contamination from wastewater inputs, stressing the urgent need for efficient wastewater treatment in the area. The tourist industry in coastal karstic lagoons such as the NLS must have a Wastewater Treatment Program as a compensation measure for the anthropic pressure that is negatively changing the water quality of this highly relevant socio-environmental system. Full article
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<p>Location of the sampling stations along the five main zones of the Nichupte Lagoon System and the main current patterns in the lagoon (represented by the dashed arrows) adapted from the numerical model by [<a href="#B11-applsci-14-11889" class="html-bibr">11</a>]. Land use is a modification of the metadata obtained from the National Biodiversity Information System, SNIB for its initials in Spanish [<a href="#B18-applsci-14-11889" class="html-bibr">18</a>].</p>
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<p>Average annual variation in the concentration of caffeine and number of tourists (<b>left</b> side) and monthly precipitation in Cancun 2018–2020 (<b>right</b> side).</p>
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<p>Distribution of caffeine throughout the zones of the NLS in the three-year follow-up.</p>
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<p>Spatial and temporal variations in the NLS of (<b>a</b>) NO<sub>3</sub><sup>−</sup>, (<b>b</b>) NO<sub>2</sub><sup>−</sup>, (<b>c</b>) NH<sub>4</sub><sup>+</sup>, (<b>d</b>) SRP, (<b>e</b>) SRSi, (<b>f</b>) Cha-a, (<b>g</b>) salinity, and (<b>h</b>) DO.</p>
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<p>Spatial and temporal variations in the NLS of (<b>a</b>) NO<sub>3</sub><sup>−</sup>, (<b>b</b>) NO<sub>2</sub><sup>−</sup>, (<b>c</b>) NH<sub>4</sub><sup>+</sup>, (<b>d</b>) SRP, (<b>e</b>) SRSi, (<b>f</b>) Cha-a, (<b>g</b>) salinity, and (<b>h</b>) DO.</p>
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<p>Spatial and temporal variations in the NLS of (<b>a</b>) NO<sub>3</sub><sup>−</sup>, (<b>b</b>) NO<sub>2</sub><sup>−</sup>, (<b>c</b>) NH<sub>4</sub><sup>+</sup>, (<b>d</b>) SRP, (<b>e</b>) SRSi, (<b>f</b>) Cha-a, (<b>g</b>) salinity, and (<b>h</b>) DO.</p>
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<p>Spatial and temporal variations in the NLS of (<b>a</b>) NO<sub>3</sub><sup>−</sup>, (<b>b</b>) NO<sub>2</sub><sup>−</sup>, (<b>c</b>) NH<sub>4</sub><sup>+</sup>, (<b>d</b>) SRP, (<b>e</b>) SRSi, (<b>f</b>) Cha-a, (<b>g</b>) salinity, and (<b>h</b>) DO.</p>
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<p>Overall water quality health status of the NLS in 2018, 2019, and 2020.</p>
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<p>Cluster analysis by NLS area.</p>
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<p>Principal component analysis of the measured variables in the NSL.</p>
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15 pages, 7631 KiB  
Article
Spatiotemporal Evolution of Air–Sea CO2 Flux in the South China Sea and Its Response to Environmental Factors
by Ying Chen, Hui Zhao and Hui Gao
Remote Sens. 2024, 16(24), 4724; https://doi.org/10.3390/rs16244724 - 18 Dec 2024
Viewed by 391
Abstract
Increasing atmospheric carbon dioxide (CO2) from human activities underscores the need to understand air–sea CO2 flux in marine environments, particularly in marginal seas like the South China Sea (SCS). This research analyzes the spatial and temporal patterns of air–sea CO [...] Read more.
Increasing atmospheric carbon dioxide (CO2) from human activities underscores the need to understand air–sea CO2 flux in marine environments, particularly in marginal seas like the South China Sea (SCS). This research analyzes the spatial and temporal patterns of air–sea CO2 flux across four typical regions of the SCS: the northern SCS, western SCS, SCS basin, and northeastern SCS. Our results show that the SCS serves as a carbon source from spring to autumn and shifts to a carbon sink in winter. The northern SCS exhibits strong carbon sink behavior during winter, transitioning to a source in warmer months, while the western SCS and SCS basin consistently act as carbon sources year-round, with summer peaks. The northeastern SCS acts as a source in warmer months, becoming a weak sink in winter. Partial correlation analysis reveals that temperature and wind speed significantly influence air–sea CO2 flux, though regional differences exist. Notably, chlorophyll-a in the northern SCS is negatively correlated with air–sea CO2 flux, indicating that high primary productivity enhances CO2 absorption, whereas other regions show contrasting relationships. These findings provide valuable insights into the complex carbon cycle mechanisms in the SCS. Full article
(This article belongs to the Special Issue Remote Sensing for Monitoring Water and Carbon Cycles)
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<p>(<b>a</b>) Depth map of the study region. (<b>b</b>) The climatological air–sea CO<sub>2</sub> flux (mmol/m<sup>2</sup>/day) from 2003 to 2019. Box A represents the northern SCS, Box B represents the western SCS, Box C represents the SCS basin, and Box D represents the northeastern SCS.</p>
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<p>Time series of air–sea CO<sub>2</sub> flux (mmol/m<sup>2</sup>/day) in the SCS from 2003 to 2019. The red dashed line represents a zero air–sea CO<sub>2</sub> flux.</p>
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<p>Distribution characteristics of air–sea CO<sub>2</sub> flux (mmol/m<sup>2</sup>/day) in the SCS from 2003 to 2019 in (<b>a</b>) spring, (<b>b</b>) summer, (<b>c</b>) autumn, and (<b>d</b>) winter. Box A represents the northern SCS, Box B represents the western SCS, Box C represents the SCS basin, and Box D represents the northeastern SCS.</p>
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<p>Distribution of (<b>a</b>) Chl-<span class="html-italic">a</span> (mg/m<sup>3</sup>), (<b>b</b>) SST (°C), and (<b>c</b>) SSW (m/s) in the SCS from 2003 to 2019 in spring, summer, autumn, and winter. The black arrow represents the direction of the wind. The Chl-<span class="html-italic">a</span> concentration is processed by logarithm. Box A represents the northern SCS, Box B represents the western SCS, Box C represents the SCS basin, and Box D represents the northeastern SCS.</p>
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<p>EOF analysis of the climatological air–sea CO<sub>2</sub> flux (mmol/m<sup>2</sup>/day) in the SCS from 2003 to 2019. (<b>a</b>) Eigenvector space distribution. (<b>b</b>) Time coefficient map. Box A represents the northern SCS, Box B represents the western SCS, Box C represents the SCS basin, and Box D represents the northeastern SCS.</p>
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<p>The components extracted by ensemble Empirical Mode Decomposition (EEMD). The extracted IMFs from high-frequency to low-frequency of (<b>a</b>) semi-annual (SemiA), (<b>b</b>) modulated annual cycle (MAC), (<b>c</b>) interannual (InterA), and (<b>d</b>) residual trend (R).</p>
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<p>Distribution of partial correlation analysis REGARDING air–sea CO<sub>2</sub> flux and (<b>a</b>) SST, (<b>b</b>) SSW, and (<b>c</b>) Chl-<span class="html-italic">a</span> in different regions (Significance <span class="html-italic">p</span> &lt; 0.05).</p>
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20 pages, 3134 KiB  
Article
Evaluating MULTIOBS Chlorophyll-a with Ground-Truth Observations in the Eastern Mediterranean Sea
by Eleni Livanou, Raphaëlle Sauzède, Stella Psarra, Manolis Mandalakis, Giorgio Dall’Olmo, Robert J. W. Brewin and Dionysios E. Raitsos
Remote Sens. 2024, 16(24), 4705; https://doi.org/10.3390/rs16244705 - 17 Dec 2024
Viewed by 665
Abstract
Satellite-derived observations of ocean colour provide continuous data on chlorophyll-a concentration (Chl-a) at global scales but are limited to the ocean’s surface. So far, biogeochemical models have been the only means of generating continuous vertically resolved Chl-a profiles on a regular grid. MULTIOBS [...] Read more.
Satellite-derived observations of ocean colour provide continuous data on chlorophyll-a concentration (Chl-a) at global scales but are limited to the ocean’s surface. So far, biogeochemical models have been the only means of generating continuous vertically resolved Chl-a profiles on a regular grid. MULTIOBS is a multi-observations oceanographic dataset that provides depth-resolved biological data based on merged satellite- and Argo-derived in situ hydrological data. This product is distributed by the European Union’s Copernicus Marine Service and offers global multiyear, gridded Chl-a profiles within the ocean’s productive zone at a weekly temporal resolution. MULTIOBS addresses the scarcity of observation-based vertically resolved Chl-a datasets, particularly in less sampled regions like the Eastern Mediterranean Sea (EMS). Here, we conduct an independent evaluation of the MULTIOBS dataset in the oligotrophic waters of the EMS using in situ Chl-a profiles. Our analysis shows that this product accurately and precisely retrieves Chl-a across depths, with a slight 1% overestimation and an observed 1.5-fold average deviation between in situ data and MULTIOBS estimates. The deep chlorophyll maximum (DCM) is adequately estimated by MULTIOBS both in terms of positioning (root mean square error, RMSE = 13 m) and in terms of Chl-a (RMSE = 0.09 mg m−3). The product accurately reproduces the seasonal variability of Chl-a and it performs reasonably well in reflecting its interannual variability across various depths within the productive layer (0–120 m) of the EMS. We conclude that MULTIOBS is a valuable dataset providing vertically resolved Chl-a data, enabling a holistic understanding of euphotic zone-integrated Chl-a with an unprecedented spatiotemporal resolution spanning 25 years, which is essential for elucidating long-term trends and variability in oceanic primary productivity. Full article
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<p>Locations of sampling stations for the available in situ data (red dots). The orange × symbol marks the position of the E1-M3A monitoring station. The grid lines represent the pixels of the MULTIOBS product. Bathymetry data were obtained from GEBCO_2021 grid dataset.</p>
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<p>Monthly averaged vertical chlorophyll-a concentration (Chl-a) profiles obtained from in situ data over the Eastern Mediterranean Sea and the corresponding matched (in space and time) monthly averaged vertical profiles obtained from the MULTIOBS product. N denotes the number of matched profiles per month.</p>
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<p>Scatterplots of the matchups between in situ- and MULTIOBS-derived chlorophyll-a concentration (Chl-a) over the Eastern Mediterranean Sea, with colours indicating the different depth layers. (<b>a</b>) Overall relationship across all depths within the 0–120 m layer, (<b>b</b>) surface layer scatterplot considering matchups within 0 to 50 m of depth, (<b>c</b>) intermediate layer scatterplot considering matchups within 60 to 100 m of depth, and (<b>d</b>) deeper layer relationship considering matchups within 110 to 120 m of depth. For clarity, only values at every 10 m interval within the 0–120 m depth layer are plotted. Different symbols represent distinct time periods: bloom [circle]—January–March; intermediate [× symbol]—April; stratified [triangle]—May–September; and early mixing [square]—October–December. The 1:1 line is shown as a black dotted line. Statistical metrics for MULTIOBS performance are provided in each panel (see <a href="#sec2-remotesensing-16-04705" class="html-sec">Section 2</a> for abbreviations of metrics).</p>
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<p>Distribution of in situ and MULTIOBS data derived for the Eastern Mediterranean Sea, showing (<b>a</b>) the position of deep chlorophyll maximum (DCM) and (<b>b</b>) the chlorophyll-a concentration (Chl-a) at the DCM, calculated as the mean integral of a 20 m layer centred at the DCM. Data are presented using kernel density estimation plots with boxplots shown as insets. Only matched-up profiles characterised as DCM type are analysed. Dashed line represents the mean of each distribution.</p>
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<p>Time series of chlorophyll-a concentration (Chl-a) at the E1-M3A site at the Eastern Mediterranean Sea (north of Crete), derived from the in situ data (circles) and from the MULTIOBS data (line), presented as mean integrals of successive depth layers: (<b>a</b>) (0–20 m), (<b>c</b>) (20–60 m), (<b>e</b>) (60–100 m), and (<b>g</b>) (100–120 m). Statistical metrics are calculated for the log<sub>10</sub>-transformed data (see <a href="#sec2-remotesensing-16-04705" class="html-sec">Section 2</a> for abbreviations of metrics). N indicates the number of observations per depth layer. The corresponding distributions of Chl-a at the E1-M3A site derived from the in situ data and their matchups from MULTIOBS data are summarised using kernel density estimation plots of the distributions of in situ- and MULTIOBS-derived Chl-a mean integrals of successive depth layers: (<b>b</b>) (0–20 m), (<b>d</b>) (20–60 m), (<b>f</b>) (60–100 m), and (<b>h</b>) (100–120 m). The dashed line indicates the mean of each distribution.</p>
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<p>(<b>a</b>) Time series of chlorophyll-a concentration (Chl-a) at the E1-M3A site at the Eastern Mediterranean Sea (north of Crete) derived from the in situ data (dots, N = 42 profiles) and from the MULTIOBS data (line), presented as mean integrals of the 0–120 m layer. Statistical metrics are calculated for the log<sub>10</sub>-transformed data (see <a href="#sec2-remotesensing-16-04705" class="html-sec">Section 2</a> for abbreviations of metrics). (<b>b</b>) Distributions of Chl-a at the E1-M3A site derived from the in situ data and their corresponding estimates from MULTIOBS (N = 42 profiles). Data are summarised using kernel density estimation plots of the distributions of in situ- and MULTIOBS-derived Chl-a presented as mean integrals of the 0–120 m layer. The dashed line indicates the mean of each distribution.</p>
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18 pages, 6778 KiB  
Article
An Interpretable CatBoost Model Guided by Spectral Morphological Features for the Inversion of Coastal Water Quality Parameters
by Baofeng Chen, Yunzhi Chen and Hongmei Chen
Water 2024, 16(24), 3615; https://doi.org/10.3390/w16243615 - 15 Dec 2024
Viewed by 575
Abstract
Chlorophyll-a (Chla) and total suspended solid (TSS) concentrations are important parameters for water quality assessment, and in recent years, machine learning has been shown to have great potential in this field. However, current water quality parameter inversion models lack interpretability and rarely consider [...] Read more.
Chlorophyll-a (Chla) and total suspended solid (TSS) concentrations are important parameters for water quality assessment, and in recent years, machine learning has been shown to have great potential in this field. However, current water quality parameter inversion models lack interpretability and rarely consider the morphological characteristics of the spectrum. To address this limitation, we used Sentinel-3 OLCI data to construct an interpretable CatBoost model guided by spectral morphological characteristics for remote sensing monitoring of Chla and TSS along the coast of Fujian. The results show that the coastal waters of Fujian Province can be divided into five clusters, and the areas of different clusters will change with the alternation of seasons. Clusters 2 and 4 are the main types of coastal waters. The CatBoost model combined with spectral feature engineering has a high accuracy in predicting Chla and TSS, among which Chla is slightly better than TSS (R2 = 0.88, MSE = 8.21, MAPE = 1.10 for Chla predictions; R2 = 0.77, MSE = 380.49, MAPE = 2.48 for TSS predictions). We further conducted an interpretability analysis on the model output and found that the combination of BRI and TBI indexes composed of bands such as b8, b9, and b10 and the fluctuation of spectral curves will have a significant impact on the prediction of model output. The interpretable CatBoost model based on spectral morphological features proposed in this study can provide an effective technical means of estimating the chlorophyll-a and total suspended particulate matter concentrations in the coastal areas of Fujian. Full article
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<p>Location of Fujian Province and study area.</p>
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<p>GLORIA data points used in the study.</p>
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<p>Research flow chart.</p>
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<p>(<b>a</b>) Average spectral curve of each category. (<b>b</b>) Chla concentration distribution of different clusters. (<b>c</b>) TSS concentration distribution of different clusters.</p>
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<p>Clustering results of coastal water bodies in Fujian Province in different seasons. Figures (<b>a</b>–<b>d</b>) show the average maps of water classification for spring, summer, autumn, and winter.</p>
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<p>The structure of the CatBoost algorithm.</p>
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<p>Prediction results of the CatBoost model on the test set (the red line is the trend line).</p>
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<p>Interpretability results of spectral features for CatBoost inversion model of Chla and TSS by SHAP analysis. Figure (<b>a</b>) shows the local explainable results of Chla, Figure (<b>b</b>) shows the global explainable results of Chla, Figure (<b>c</b>) shows the local explainable results of TSS, and Figure (<b>d</b>) shows the global explainable results of TSS. (In the left column chart, one dot represents a sample, where warmer colors indicate larger values of the feature, and vice versa. The wider the distribution of SHAP values for a feature, the larger its global SHAP value, indicating that the feature has a greater impact on the model. In the right column chart, the white numbers on the blue bar represent the average absolute SHAP value [<a href="#B44-water-16-03615" class="html-bibr">44</a>].)</p>
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<p>Annual average concentration distribution map of Chla and TSS along the coast of Fujian Province from 2021 to 2023. (<b>a</b>–<b>c</b>) is the average concentration of Chla, and (<b>d</b>–<b>f</b>) is the average concentration of TSS.</p>
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<p>Average Chla and TSS concentration values in different seasons along the coast of Fujian Province from 2021 to 2023. The four graphs on the left (<b>a</b>–<b>d</b>) show the average concentration of Chla, while the four graphs on the right (<b>e</b>–<b>h</b>) show the average concentration of TSS.</p>
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20 pages, 18277 KiB  
Article
Observations of Optical Properties and Chlorophyll-a Concentration in Qiandao Lake Using Shipborne Lidar
by Xuan Sang, Zhihua Mao, Youzhi Li, Xianliang Zhang, Chang Han, Longwei Zhang and Haiqing Huang
Remote Sens. 2024, 16(24), 4663; https://doi.org/10.3390/rs16244663 - 13 Dec 2024
Viewed by 461
Abstract
Lidar technology is increasingly applied to the inversion of oceanic biological parameters and optical properties based on empirical and semi-empirical bio-optical models. However, these models cannot be directly applied to inland waters due to their complex composition, and research on the biological parameters [...] Read more.
Lidar technology is increasingly applied to the inversion of oceanic biological parameters and optical properties based on empirical and semi-empirical bio-optical models. However, these models cannot be directly applied to inland waters due to their complex composition, and research on the biological parameters and optical properties of inland waters remains limited. In this study, the Fernald method was employed to retrieve the vertical distribution of optical properties in Qiandao Lake for the first time using shipborne lidar data obtained in June 2019. By quantifying the depth-resolved optical contributions of biological components, the vertical distributions of chlorophyll-a concentration were mapped with greater precision. The lidar-estimated optical properties exhibited characteristic spatiotemporal distributions, which were closely related to water quality. At the inflow of Xin’an River, the attenuation and scattering coefficient showed a gradual increase with depth. At the north–south-oriented reservoir area and the outflow of Qiandao Lake, an apparently continuous subsurface layer with the maximum signal occurred at approximately 3.5 m. The vertical distributions of chlorophyll-a profiles were consistently classified as subsurface chlorophyll maxima, with the maximum value of chlorophyll-a concentration fluctuating between 4 and 12 μg/L. The subsurface phytoplankton layer was observed at water depths ranging from 1.5 to 3.5 m, with a thickness of 3 to 6 m. Furthermore, the influences of lidar ratio Sp(z) and reference value bbp(zm) were discussed as significant sources of inversion error in the Fernald method. These results indicate that lidar technology holds great potential for the long-term monitoring of lakes. Full article
(This article belongs to the Special Issue Oceanographic Lidar in the Study of Marine Systems)
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<p>Map of shipborne lidar measurement tracks and in situ measurement stations conducted on (<b>A</b>) 3–5 June 2019 and (<b>B</b>) 10–12 July 2020 in Qiandao Lake. All stations are divided into three groups based on our study. The red pentagram represents the location of the Qiandao Lake.</p>
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<p>An example of lidar data preprocessing. (<b>A</b>) Raw lidar data and (<b>B</b>) water column signal from smoothed data. The distance 0 m is the position of the water surface, the distance below 0 m is the atmosphere altitude, and the distance above 0 m is the water depth.</p>
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<p>The depth-varying lidar ratio <span class="html-italic">S</span><sub>p</sub>(<span class="html-italic">z</span>) of the six measurement stations (S1–S6).</p>
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<p>Results of regression analysis of (<b>A</b>) fractions at different depths and (<b>B</b>) lidar-estimated and in-situ-observed chlorophyll-a concentrations.</p>
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<p>Step-by-step example of a lidar inversion along the lidar track. Vertical profile distributions of (<b>A</b>) signal after preprocessing, (<b>B</b>) lidar attenuation coefficient, (<b>C</b>) lidar volume scattering function at a scattering angle of π rad, (<b>D</b>) particulate backscatter coefficient, and (<b>E</b>) chlorophyll-a concentration.</p>
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<p>Comparisons of vertical profiles between lidar-estimated and in-situ-observed <span class="html-italic">b</span><sub>bp</sub> values at (<b>A</b>) S1, (<b>B</b>) S2, (<b>C</b>) S3, (<b>D</b>) S4, (<b>E</b>) S5, and (<b>F</b>) S6. Yellow dots are lidar estimations and blue dots are in situ observations.</p>
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<p>Comparisons of vertical profiles between lidar-estimated and in-situ-observed <span class="html-italic">K</span><sub>d</sub> values at (<b>A</b>) S1, (<b>B</b>) S2, (<b>C</b>) S3, (<b>D</b>) S4, (<b>E</b>) S5, and (<b>F</b>) S6. Yellow dots are lidar estimations and blue dots are in situ observations.</p>
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<p>Scatter plots of regression analysis results between lidar-estimated and in-situ-observed (<b>A</b>) <span class="html-italic">b</span><sub>bp</sub> and (<b>B</b>) <span class="html-italic">K</span><sub>d</sub> profiles for stations 1–6. The solid line is the linear regression.</p>
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<p>Three-dimensional profile distributions of (<b>A</b>) diffusion attenuation coefficient, (<b>B</b>) lidar volume scattering function at a scattering angle of π rad, (<b>C</b>) particulate backscatter coefficient, and (<b>D</b>) chlorophyll-a concentration estimated from the lidar data obtained during the 2019 cruise in Qiandao Lake.</p>
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<p>The distributions of SCM maximum depth (Z<sub>scm</sub>), SCM thickness (T<sub>scm</sub>), and maximum value of chlorophyll-a concentration (Chl<sub>max</sub>) along (<b>A</b>) Track 1, (<b>B</b>) Track 2, (<b>C</b>) Track 3, and (<b>D</b>) Track 4. All lidar tracks are plotted from north to south.</p>
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<p>The influence of setting different <span class="html-italic">S</span><sub>p</sub>(z) values. (<b>A</b>,<b>B</b>) Inversion results of <span class="html-italic">b</span><sub>bp</sub> and <span class="html-italic">K</span><sub>d</sub> under constant and depth-varying lidar ratios. (<b>C</b>,<b>D</b>) <span class="html-italic">b</span><sub>bp</sub> and <span class="html-italic">K</span><sub>d</sub> values obtained by setting different values of the constant S<sub>p</sub>(z).</p>
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<p>Comparison between lidar-estimated particulate backscatter coefficient with (<b>A</b>) different <span class="html-italic">b</span><sub>bp</sub>(<span class="html-italic">z</span><sub>m</sub>) values and (<b>B</b>) different <span class="html-italic">z</span><sub>m</sub> values.</p>
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<p>(<b>A</b>) Simulated echo signals with different reflectance of the bottom (Rb) and (<b>B</b>) the inversed value of the particulate backscatter coefficient.</p>
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17 pages, 3482 KiB  
Article
Improving Lettuce Tolerance to Cadmium Stress: Insights from Raw vs. Cystamine-Modified Biochar
by Rongqi Chen, Xi Duan, Ruoxuan Xu and Tao Zhao
Horticulturae 2024, 10(12), 1323; https://doi.org/10.3390/horticulturae10121323 - 11 Dec 2024
Viewed by 402
Abstract
Understanding the interactions among biochar, plants, soils, and microbial communities is essential for developing effective and eco-friendly soil remediation strategies. This study investigates the role of cystamine-modified biochar (Cys-BC) in alleviating cadmium (Cd) toxicity in lettuce, comparing its effects to those of raw [...] Read more.
Understanding the interactions among biochar, plants, soils, and microbial communities is essential for developing effective and eco-friendly soil remediation strategies. This study investigates the role of cystamine-modified biochar (Cys-BC) in alleviating cadmium (Cd) toxicity in lettuce, comparing its effects to those of raw biochar. Lettuce plants were exposed to Cd stress (1–5 mg kg−1), and the effects of Cys-BC were assessed by measuring plant biomass, photosynthetic efficiency, antioxidant activity, Cd bioavailability, and soil microbial diversity. Cys-BC significantly enhanced plant biomass, with increases in above-ground growth (40.54–44.95%) and root biomass (37.54–47.44%) compared to Cd-stressed controls. Photosynthetic parameters improved by up to 91.02% for chlorophyll-a content and 37.93% for the net photosynthetic rate. Cys-BC mitigated oxidative stress, increasing antioxidant activities by 73.83% to 99.39%. Additionally, Cys-BC reduced available Cd levels in the soil, primarily through enhanced cation exchange rather than changes in pH. Plant responses to Cd stress included increased glutathione reductase activity and elevated cysteine levels, which further contributed to Cd passivation. Microbial diversity in the soil increased, particularly among sulfur- and nitrogen-cycling bacteria such as Deltaproteobacteria and Nitrospira, suggesting their role in mitigating Cd stress. These findings highlight the potential of Cys-BC as an effective agent for the remediation of Cd-contaminated soils. Full article
(This article belongs to the Special Issue Microbial Interaction with Horticulture Plant Growth and Development)
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<p>Effects of different biochar treatments on oxidative stress markers content in lettuce: (<b>a</b>) malondialdehyde, (<b>b</b>) hydrogen peroxide, (<b>c</b>) glutathione, and (<b>d</b>) cysteine. Lowercase (a–d) letters are used to denote differential rankings.</p>
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<p>Effects of different biochar treatments on the activity of antioxidant enzymes of lettuce: (<b>a</b>) superoxide dismutase, (<b>b</b>) peroxidase, (<b>c</b>) catalase, and (<b>d</b>) reductase. Lowercase (a–d) letters are used to denote differential rankings.</p>
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<p>The linear regression models correlating Cd residues in lettuce with DTPA-extractable Cd in soil. (<b>a</b>) shoot Cd and (<b>b</b>) root Cd under raw BC treatments; (<b>c</b>) shoot Cd and (<b>d</b>) root Cd under Cys-BC treatments.</p>
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<p>Effects of different biochar treatments on soil properties: (<b>a</b>) proportion of various Cd fractions, (<b>b</b>) DPTA available Cd content, (<b>c</b>) soil pH, and (<b>d</b>) soil CEC.</p>
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<p>The <span class="html-italic">t</span>-test for the variability in the abundance of soil bacteria and fungi in the different biochar treatments, (<b>a</b>) differences in bacteria of raw BC treatments at the phylum level, (<b>b</b>) differences in bacteria of Cys-BC treatments at the phylum level, (<b>c</b>) differences in fungi at the phylum level, (<b>d</b>) differences in bacteria of raw BC treatments at the program level, (<b>e</b>) differences in bacteria of Cys-BC treatments at the program level, (<b>f</b>) differences in fungi at the program level, (<b>g</b>) differences in bacteria of raw BC treatments at the order level, (<b>h</b>) differences in bacteria in Cys-BC treatments at the order level, (<b>i</b>) differences in fungi at the order level. Analyses of variance levels of significance (LS): * <span class="html-italic">p</span> &lt; 0.1, ** <span class="html-italic">p</span> &lt; 0.01, ns: not significant.</p>
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<p>Canonical correspondence analysis (CCA) of bacteria (<b>a</b>,<b>b</b>) fungi in soil sample groups.</p>
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