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Search Results (6,475)

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Keywords = temporal patterns

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22 pages, 3249 KiB  
Article
LSTM-Autoencoder Based Detection of Time-Series Noise Signals for Water Supply and Sewer Pipe Leakages
by Yungyeong Shin, Kwang Yoon Na, Si Eun Kim, Eun Ji Kyung, Hyun Gyu Choi and Jongpil Jeong
Water 2024, 16(18), 2631; https://doi.org/10.3390/w16182631 - 16 Sep 2024
Viewed by 300
Abstract
The efficient management of urban water distribution networks is crucial for public health and urban development. One of the major challenges is the quick and accurate detection of leaks, which can lead to water loss, infrastructure damage, and environmental hazards. Many existing leak [...] Read more.
The efficient management of urban water distribution networks is crucial for public health and urban development. One of the major challenges is the quick and accurate detection of leaks, which can lead to water loss, infrastructure damage, and environmental hazards. Many existing leak detection methods are ineffective, especially in complex and aging pipeline networks. If these limitations are not overcome, it can result in a chain of infrastructure failures, exacerbating damage, increasing repair costs, and causing water shortages and public health risks. The leak issue is further complicated by increasing urban water demand, climate change, and population growth. Therefore, there is an urgent need for intelligent systems that can overcome the limitations of traditional methodologies and leverage sophisticated data analysis and machine learning technologies. In this study, we propose a reliable and advanced method for detecting leaks in water pipes using a framework based on Long Short-Term Memory (LSTM) networks combined with autoencoders. The framework is designed to manage the temporal dimension of time-series data and is enhanced with ensemble learning techniques, making it sensitive to subtle signals indicating leaks while robustly dealing with noise signals. Through the integration of signal processing and pattern recognition, the machine learning-based model addresses the leak detection problem, providing an intelligent system that enhances environmental protection and resource management. The proposed approach greatly enhances the accuracy and precision of leak detection, making essential contributions in the field and offering promising prospects for the future of sustainable water management strategies. Full article
(This article belongs to the Special Issue Prediction and Assessment of Hydrological Processes)
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<p>Water supply and sewage system.</p>
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<p>LSTM-autoencoder architecture.</p>
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<p>Proposed framework.</p>
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<p>Actual valve installation site.</p>
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<p>Completed sensor installation.</p>
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<p>Sensor installation close to the ground.</p>
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<p>Use case of leak detection.</p>
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<p>Leak data without noise.</p>
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<p>FFT for leak data.</p>
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<p>Actual and predicted values for data without noise.</p>
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<p>Actual and predicted values for data with noise.</p>
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<p>Noise attenuation.</p>
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<p>Accuracy.</p>
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<p>Precision.</p>
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<p>Recall.</p>
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<p>F1 scores.</p>
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<p>AUC scores.</p>
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21 pages, 1298 KiB  
Article
Seasonal Variability and Hydrological Patterns Influence the Long-Term Trends of Nutrient Loads in the River Po
by Edoardo Cavallini, Pierluigi Viaroli, Mariachiara Naldi, Mattia Saccò, Alessandro Scibona, Elena Barbieri, Silvia Franceschini and Daniele Nizzoli
Water 2024, 16(18), 2628; https://doi.org/10.3390/w16182628 - 16 Sep 2024
Viewed by 269
Abstract
This study investigates the long-term trends (1992–2022) of nitrogen and phosphorus loadings exported by the River Po to the Adriatic Sea, to better analyse how changes in hydrology are affecting the timing and magnitude of river nutrient loads. We used 30 years of [...] Read more.
This study investigates the long-term trends (1992–2022) of nitrogen and phosphorus loadings exported by the River Po to the Adriatic Sea, to better analyse how changes in hydrology are affecting the timing and magnitude of river nutrient loads. We used 30 years of monitoring data in order to (a) identify the main temporal patterns and their interactions at a decadal, annual and seasonal scale, (b) estimate precipitation effects on load formation and evaluate whether and to which extent the hydrological regime affects nutrient export across the years and (c) analyse the nutrient export regime at a monthly scale and the main transport dynamic of N and P chemical species (hydrological vs. biogeochemical control). The long-term analysis shows a general decrease of both P and N loadings, but the trends are different between the elements and their chemical species, as well as undergoing different seasonal variations. We found a statistically significant relationships between precipitation and loads, which demonstrates that precipitation patterns drive the exported load at the intra- and interannual time scales considered in this study. Precipitation-induced load trends trigger seasonal changes in nutrient deliveries to the sea, peaking in spring and autumn. The nitrogen decrease is mainly concentrated in the summer dry period, while total phosphorus diminishes mainly in spring and autumn. This mismatch of N and P results in variable molar N:P ratios within the year. The effects of extreme drought and flood events, along with the progressive decrease in the snowmelt contribution to water fluxes, are expected to exacerbate the variability in the N and P loadings, which in turn is expected to perturbate the biodiversity, food webs and trophic state of the Northern Adriatic Sea. Full article
22 pages, 7490 KiB  
Article
Incorporating Ecosystem Service Trade-Offs and Synergies with Ecological Sensitivity to Delineate Ecological Functional Zones: A Case Study in the Sichuan-Yunnan Ecological Buffer Area, China
by Peipei Miao, Cansong Li, Baichuan Xia, Xiaoqing Zhao, Yingmei Wu, Chao Zhang, Junen Wu, Feng Cheng, Junwei Pu, Pei Huang, Xiongfei Zhang and Yi Chai
Land 2024, 13(9), 1503; https://doi.org/10.3390/land13091503 - 16 Sep 2024
Viewed by 195
Abstract
Enhancing regional ecosystem stability and managing land resources effectively requires identifying ecological function zones and understanding the factors that influence them. However, most current studies have primarily focused on ecosystem service bundles, paying less attention to the trade-offs, synergies, and ecological sensitivity, leading [...] Read more.
Enhancing regional ecosystem stability and managing land resources effectively requires identifying ecological function zones and understanding the factors that influence them. However, most current studies have primarily focused on ecosystem service bundles, paying less attention to the trade-offs, synergies, and ecological sensitivity, leading to a more uniform approach to functional zoning. This study aimed to analyze and describe the spatial and temporal patterns of four essential ecosystem services, including water yield (WY), net primary productivity (NPP), soil conservation (SC), and habitat quality (HQ), in the Sichuan-Yunnan ecological buffer area over the period from 2005 to 2019. Spatial overlay analysis was used to assess ecological sensitivity, trade-offs, synergies, and ecosystem service bundles to define ecological functional zones. Geographic detectors were then applied to identify the primary drivers of spatial variation in these zones. The findings showed a progressive improvement in ecosystem service functions within the Sichuan-Yunnan ecological buffer zone. Between 2005 and 2019, NPP, soil conservation, and water yield all demonstrated positive trends, while HQ displayed a declining trend. There was significant spatial heterogeneity and distinct regional patterns in ecosystem service functions, with a general decrease from southwest to northeast, particularly in NPP and HQ. Trade-offs were evident in most ecosystem services, with the most significant between WY and HQ and most in the northeast and east regions. Ecological sensitivity decreased from southwest to northeast. Regions with a higher ecological sensitivity were primarily situated in the southwestern region, and their spatial distribution pattern was comparable to that of high habitat quality. The spatial overlay analysis categorized areas into various types, including human production and settlement zones, ecologically vulnerable zones, ecological transition zones, and ecological conservation zones, accounting for 17.28%, 22.30%, 7.41%, and 53.01% of the total area, respectively. The primary environmental factor affecting ecological function zoning was identified as precipitation, while the main social variables were human activity and population density. This study enhances the understanding of ecological functions and supports sustainable development in the Sichuan-Yunnan ecological buffer area, offering important guidance for ecological zoning. Full article
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<p>Study area.</p>
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<p>Land cover type.</p>
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<p>Research framework. (AHP: the analytical hierarchy process; R: R language; GDP: gross domestic product).</p>
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<p>The annual average value of four ecosystem services in the ecological conservation area of Sichuan-Yunnan provinces from 2005 to 2019. (HQ: habitat quality).</p>
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<p>Ecosystem service proportion trends over time. (HQ: habitat quality).</p>
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<p>Spatio-temporal distribution and variations of ecosystem services in the ecological conservation area of Sichuan-Yunnan provinces from 2000 to 2019. Note: (<b>a</b>) NPP (net primary productivity), (<b>b</b>) WY (water yield), (<b>c</b>) HQ (habitat quality), (<b>d</b>) SC (soil conservation).</p>
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<p>Trade-offs/synergy analysis of temporal changes in ecosystem services.</p>
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<p>Trade-offs/synergy analysis of spatial changes in ecosystem services. (HQ: habitat quality).</p>
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<p>Comprehensive spatial pattern of ecological sensitivity.</p>
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<p>Classification results of ecosystem service bundles (<b>a</b>) and radar chart of ecosystem services by service cluster (<b>b</b>).</p>
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<p>Spatial distribution and pattern of ecosystem service clusters in the ecological conservation area in Sichuan-Yunnan provinces from 2005 to 2019 (ESB: Ecosystem service bundles).</p>
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<p>Ecosystem service function divisions in ecological conservation areas in Sichuan-Yunnan provinces.</p>
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<p>Results of the interaction between factors in the study area. [X1–X8 for each of the eight impact factors: land use type, normalized difference vegetation index (NDVI), nighttime lighting, population density, human activities, temperature, precipitation, and topographic relief].</p>
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<p>Rainfall and temperature changes in Sichuan-Yunnan provinces from 2005 to 2019.</p>
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15 pages, 2429 KiB  
Article
Current Status of Liverwort Herbaria Specimens and Geographical Distribution in China
by Jiaqi Cui, Xiuhua Yang, Xiaoyu Li, Jitong Li, Siqi Dong, Hongfeng Wang and Chengjun Yang
Plants 2024, 13(18), 2583; https://doi.org/10.3390/plants13182583 - 15 Sep 2024
Viewed by 297
Abstract
Specimen data play a crucial role in geographical distribution research. In this study, the collection information of liverwort specimens in China was compiled and analyzed to investigate the history, current status, and limitations of liverwort research in China. By utilizing the latest systematic [...] Read more.
Specimen data play a crucial role in geographical distribution research. In this study, the collection information of liverwort specimens in China was compiled and analyzed to investigate the history, current status, and limitations of liverwort research in China. By utilizing the latest systematic research findings and corresponding environmental data, a niche model was developed to offer theoretical support for exploring the potential geographical distribution and diversity of liverwort resources. A total of 55,427 liverwort specimens were collected in China, resulting in the recording of 1212 species belonging to 169 genera and 63 families. However, there are imbalances in the distributions of liverwort data among different groups, collection units, and geographical areas, with families such as Lejeuneaceae, Porellaceae, and Plagiochilaceae having the highest number of specimens. Similarly, genera such as Porella, Frullania, and Horikawaella were well represented. Remarkably, 125 species had specimen counts exceeding 100. Unfortunately, approximately 51.77% of the species had fewer than 10 recorded specimens. There were four obvious peaks in the collection years of the bryophyte specimens in China, among which the largest collection occurred from 2010 to 2023. Notably, the number of specimens collected at different stages closely aligned with the history of taxonomic research on liverworts in China. The results of the integrity of the liverwort collection indicate that there is insufficient representation of some families and genera, with a concentration of common and widely distributed large families and genera. Tropical and subtropical humid areas are key regions for liverwort diversity, with water and temperature being the primary environmental factors influencing their geographical distribution. The specific temporal and spatial data of species recorded from plant specimens will enhance the study of species diversity, comprehensive protection, and sustainable utilization. Additionally, these data will contribute to the investigation of large-scale biodiversity distribution patterns and the impact of global change on diversity. Full article
(This article belongs to the Special Issue Mapping Asia Plants)
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<p>Statistical depiction of liverwort specimen data collected in China. (<b>a</b>) The source of collections of liverwort specimens in China. (<b>b</b>) Status of liverwort specimens in China at the species level.</p>
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<p>Collection period of liverwort specimens in China. (<b>a</b>) Year of collection of liverwort specimens in China. (<b>b</b>) Relative proportions of liverwort specimens collected at various periods in China.</p>
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<p>The number of liverwort specimens from provincial regions of China.</p>
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<p>Distribution of liverwort specimens and species in different provinces of China. The white dots indicate sampling points with duplicate sites removed.</p>
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<p>Response curves of dominant environmental variables.</p>
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<p>Simulation results of the MaxEnt model of suitable areas for liverworts in China.</p>
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11 pages, 696 KiB  
Article
The Temporal Change in Ionised Calcium, Parathyroid Hormone and Bone Metabolism Following Ingestion of a Plant-Sourced Marine Mineral + Protein Isolate in Healthy Young Adults
by Marta Kozior, Olusoji Aboyeji Demehin, Michelle Mary Ryan, Sean O’Connell and Philip Michael Jakeman
Nutrients 2024, 16(18), 3110; https://doi.org/10.3390/nu16183110 - 14 Sep 2024
Viewed by 417
Abstract
Abstract: Background: An increase in plant-sourced (PS) nutrient intake is promoted in support of a sustainable diet. PS dietary minerals and proteins have bioactive properties that can affect bone health and the risk of fracture. Methods: In a group randomised, cross-over design, this [...] Read more.
Abstract: Background: An increase in plant-sourced (PS) nutrient intake is promoted in support of a sustainable diet. PS dietary minerals and proteins have bioactive properties that can affect bone health and the risk of fracture. Methods: In a group randomised, cross-over design, this study evaluated the post-ingestion temporal pattern of change in arterialised ionised calcium (iCa), parathyroid hormone (PTH), C-terminal crosslinked telopeptide of type I collagen (CTX) and procollagen type 1 amino-terminal propeptide (P1NP) for 4 h following ingestion of a novel supplement (SUPP) containing a PS marine multi-mineral + PS protein isolate. A diurnally matched intake of mineral water was used as a control (CON). Results: Compared to baseline, the change in iCa concentration was 0.022 (95%CI, 0.006 to 0.038, p = 0.011) mmol/l greater in SUPP than CON, resulting in a −4.214 (95%CI, −8.244 to −0.183, p = 0.042) pg/mL mean reduction in PTH, a −0.64 (95%CI, −0.199 to −0.008, p = 0.029) ng/mL decrease in the biomarker of bone resorption, CTX, and no change in the biomarker of bone formation, P1NP. Conclusions: When used as a dietary supplement, or incorporated into a food matrix, the promotion of PS marine multi-mineral and PS protein isolates may contribute to a more sustainable diet and overall bone health. Full article
(This article belongs to the Special Issue Mineral Nutrition on Human Health and Disease)
12 pages, 3459 KiB  
Article
Retrospective Analysis of Clinicopathological Characteristics of Surgically Treated Basal Cell Carcinomas of the Face: A Single-Centre Maxillofacial Surgery Experience
by Abdullah Saeidi, Aydin Gülses, Maryam Jamil, Albraa Alolayan, Shadia Elsayed, Jörg Wiltfang and Christian Flörke
J. Clin. Med. 2024, 13(18), 5470; https://doi.org/10.3390/jcm13185470 - 14 Sep 2024
Viewed by 329
Abstract
Background: Basal cell carcinoma is the most common nonmelanoma skin cancer, followed by cutaneous squamous cell carcinoma. The objective of the current study was to retrospectively evaluate the epidemiology, characteristic variations, histological aspects, and prognosis of basal cell carcinoma of the facial [...] Read more.
Background: Basal cell carcinoma is the most common nonmelanoma skin cancer, followed by cutaneous squamous cell carcinoma. The objective of the current study was to retrospectively evaluate the epidemiology, characteristic variations, histological aspects, and prognosis of basal cell carcinoma of the facial region based on a single-centre experience. Methods: Data from 125 patients admitted to the Department of Oral and Maxillofacial Surgery, University Medical Center Schleswig-Holstein (UKSH), Kiel, for surgical treatment of basal cell carcinomas of the face between January 2015 and April 2021 were evaluated. Results: The mean patient age was 79.58 years, 60.5% were male and 39.5% were female. Six patients (4.8%) had tumour recurrence with no regional metastasis. Seventy-nine patients (63%) were classified as T1. The nose and the temporal region were the most common areas. The mean tumour thickness was 3.20 mm. Conclusions: Micronodular, sclerosing/morphoeic, nodular, and superficial growth patterns of basal cell carcinoma are highly correlated to recurrence, so an excision safety margin is recommended. There is a strong correlation between tumour thickness and recurrence among basal cell carcinoma cases. When completely excised, the recurrence rate for basal cell carcinoma is relatively low. Full article
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<p>Basal cell carcinoma T-classification distribution, T4 was only 1% and T1 was predominant at 63% of patients.</p>
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<p>(<b>A</b>) Multiple BCC in the scalp and forehead region. (<b>B</b>) Different patient with BCC in the temporal region. (<b>C</b>) The image in (<b>B</b>), magnified.</p>
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<p>(<b>A</b>) BCC in the lateral eye corner. (<b>B</b>) BCC in the medial eye corner. (<b>C</b>) BCC in the lower eyelid. (<b>D</b>) BCC in the upper eyelid.</p>
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<p>(<b>A</b>) BCC of the nose. (<b>B</b>) The same patient as in (<b>A</b>), magnified image.</p>
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<p>The total frequency % of BCC tumour location.</p>
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<p>Growth type of BCC. Nodular growth type was the most common among 64 cases, followed by sclerodermiform and superficial growth types, with 31% and 6%, respectively.</p>
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<p>Tumour thickness distribution across T-classification among patients diagnosed with BCC. Most of these patients had a tumour thickness of 2 mm and were classified as T1.</p>
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<p>Tumour thickness mean and recurrence rate among patients diagnosed with BCC. Only 6 patients (4.8%) had tumour recurrence with a maximum tumour thickness of 8 mm.</p>
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29 pages, 17461 KiB  
Article
An Integrated CEEMDAN to Optimize Deep Long Short-Term Memory Model for Wind Speed Forecasting
by Yingying He, Likai Zhang, Tengda Guan and Zheyu Zhang
Energies 2024, 17(18), 4615; https://doi.org/10.3390/en17184615 - 14 Sep 2024
Viewed by 204
Abstract
Accurate wind speed forecasting is crucial for the efficient operation of renewable energy platforms, such as wind turbines, as it facilitates more effective management of power output and maintains grid reliability and stability. However, the inherent variability and intermittency of wind speed present [...] Read more.
Accurate wind speed forecasting is crucial for the efficient operation of renewable energy platforms, such as wind turbines, as it facilitates more effective management of power output and maintains grid reliability and stability. However, the inherent variability and intermittency of wind speed present significant challenges for achieving precise forecasts. To address these challenges, this study proposes a novel method based on Complete Ensemble Empirical Mode Decomposition with Adaptive Noise (CEEMDAN) and a deep learning-based Long Short-Term Memory (LSTM) network for wind speed forecasting. In the proposed method, CEEMDAN is utilized to decompose the original wind speed signal into different modes to capture the multiscale temporal properties and patterns of wind speeds. Subsequently, LSTM is employed to predict each subseries derived from the CEEMDAN process. These individual subseries predictions are then combined to generate the overall final forecast. The proposed method is validated using real-world wind speed data from Austria and Almeria. Experimental results indicate that the proposed method achieves minimal mean absolute percentage errors of 0.3285 and 0.1455, outperforming other popular models across multiple performance criteria. Full article
(This article belongs to the Special Issue Advances in Wind and Solar Farm Forecasting—3rd Edition)
12 pages, 6075 KiB  
Article
Spatial and Temporal Evolution Characteristics of the Ecosystem Service Value along the Beijing–Hangzhou Grand Canal
by Yuqing Xu, Di Hu, Handong He, Zhuo Zhang and Duo Bian
Appl. Sci. 2024, 14(18), 8295; https://doi.org/10.3390/app14188295 (registering DOI) - 14 Sep 2024
Viewed by 199
Abstract
The study of the spatiotemporal evolution characteristics of ecosystem service values (ESVs) is an important basis for the coordinated development of the regional nature, economy, and society and the optimization of the ecological environment. The ecological zone is an important component of the [...] Read more.
The study of the spatiotemporal evolution characteristics of ecosystem service values (ESVs) is an important basis for the coordinated development of the regional nature, economy, and society and the optimization of the ecological environment. The ecological zone is an important component of the Beijing–Hangzhou Grand Canal cultural belt. Ecosystem services are a concrete manifestation of land use structure and function. A thorough study of the value of ecosystem services in areas along the Beijing–Hangzhou Grand Canal is important for promoting the long-term and stable sustainable development of the regional economy. Based on a revised equivalent factor table, this study selected land use data from 1991, 2006, and 2021 to analyze the temporal and spatial evolution characteristics of ESVs along the Beijing–Hangzhou Grand Canal. The results show that (1) the ESVs along the Grand Canal first increased and then decreased from 1991 to 2021. The reason for this is the change in land use along the Beijing–Hangzhou Grand Canal. Specifically, the conversion of land use types from farmland to water areas contributed to the increase in the value of ecosystem services, while the conversion of farmland and grassland into construction land led to a decrease in the service value of the region. (2) the value of individual ecosystem services along the Beijing–Hangzhou Grand Canal from 1991 to 2021 varied greatly. The ESV provided by hydrological regulation was the largest and the ESV provided by maintenance nutrients was the smallest. (3) the areas along the Beijing–Hangzhou Grand Canal exhibited a specific pattern in terms of the value of ecosystem services, with the regions centered in Beijing and Tianjin showing relatively low values, while the middle section of the Grand Canal demonstrated relatively high ESV. According to the spatial and temporal distribution characteristics and the leading factor for the changes in ESVs, appropriate policies can be formulated in respective regions to implement ecological protection and land use planning, thereby providing a reference for the adaptation and restoration strategies of the ecosystem along the Grand Canal. Full article
(This article belongs to the Section Earth Sciences)
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<p>Location and scope of the study area.</p>
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<p>Changes in individual ESVs.</p>
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<p>ESVs from 1991 to 2021.</p>
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<p>Changes in ESVs from 1991 to 2021.</p>
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16 pages, 13238 KiB  
Article
Transfer of Periodic Phenomena in Multiphase Capillary Flows to a Quasi-Stationary Observation Using U-Net
by Bastian Oldach, Philipp Wintermeyer and Norbert Kockmann
Computers 2024, 13(9), 230; https://doi.org/10.3390/computers13090230 - 13 Sep 2024
Viewed by 216
Abstract
Miniaturization promotes the efficiency and exploration domain in scientific fields such as computer science, engineering, medicine, and biotechnology. In particular, the field of microfluidics is a flourishing technology, which deals with the manipulation of small volumes of liquid. Dispersed droplets or bubbles in [...] Read more.
Miniaturization promotes the efficiency and exploration domain in scientific fields such as computer science, engineering, medicine, and biotechnology. In particular, the field of microfluidics is a flourishing technology, which deals with the manipulation of small volumes of liquid. Dispersed droplets or bubbles in a second immiscible liquid are of great interest for screening applications or chemical and biochemical reactions. However, since very small dimensions are characterized by phenomena that differ from those at macroscopic scales, a deep understanding of physics is crucial for effective device design. Due to small volumes in miniaturized systems, common measurement techniques are not applicable as they exceed the dimensions of the device by a multitude. Hence, image analysis is commonly chosen as a method to understand ongoing phenomena. Artificial Intelligence is now the state of the art for recognizing patterns in images or analyzing datasets that are too large for humans to handle. X-ray-based Computer Tomography adds a third dimension to images, which results in more information, but ultimately, also in more complex image analysis. In this work, we present the application of the U-Net neural network to extract certain states during droplet formation in a capillary, which forms a constantly repeated process that is captured on tens of thousands of CT images. The experimental setup features a co-flow setup that is based on 3D-printed capillaries with two different cross-sections with an inner diameter, respectively edge length of 1.6 mm. For droplet formation, water was dispersed in silicon oil. The classification into different droplet states allows for 3D reconstruction and a time-resolved 3D analysis of the present phenomena. The original U-Net was modified to process input images of a size of 688 × 432 pixels while the structure of the encoder and decoder path feature 23 convolutional layers. The U-Net consists of four max pooling layers and four upsampling layers. The training was performed on 90% and validated on 10% of a dataset containing 492 images showing different states of droplet formation. A mean Intersection over Union of 0.732 was achieved for a training of 50 epochs, which is considered a good performance. The presented U-Net needs 120 ms per image to process 60,000 images to categorize emerging droplets into 24 states at 905 angles. Once the model is trained sufficiently, it provides accurate segmentation for various flow conditions. The selected images are used for 3D reconstruction enabling the 2D and 3D quantification of emerging droplets in capillaries that feature circular and square cross-sections. By applying this method, a temporal resolution of 25–40 ms was achieved. Droplets that are emerging in capillaries with a square cross-section become bigger under the same flow conditions in comparison to capillaries with a circular cross section. The presented methodology is promising for other periodic phenomena in different scientific disciplines that focus on imaging techniques. Full article
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<p>Principle sketch of how a periodic process like repeated slug formation can be classified according to the state of droplet formation. The left side shows a regular slug flow, which is typical for multiphase flows in capillaries, and the droplet formation mechanism with the steps from <math display="inline"><semantics> <msub> <mi>l</mi> <mn>1</mn> </msub> </semantics></math> to <math display="inline"><semantics> <msub> <mi>l</mi> <mn>5</mn> </msub> </semantics></math>. On the right side, the repeated slug flow formation is temporally resolved for the steps <math display="inline"><semantics> <msub> <mi>l</mi> <mn>1</mn> </msub> </semantics></math> to <math display="inline"><semantics> <msub> <mi>l</mi> <mn>5</mn> </msub> </semantics></math> to obtain a series of stationary states that enable 3D analysis.</p>
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<p>(<b>a</b>) The µ-CT used for the experiments and its surrounding peripherals. (<b>b</b>) A close-up view of the specimen chamber with an installed capillary under investigation.</p>
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<p>(<b>a</b>) The U-Net architecture that was used for this work with an input image and the classification of the image as the output. (<b>b</b>) An example CT image of an emerging droplet, the human-labeled ground truth and the outlet of the U-Net that was trained for 50 epochs. (<b>c</b>) A sketch of the ARM. The datasets are fed to the U-Net and are classified according to the defined states. Projection images are acquired at each angular position from 0 to <math display="inline"><semantics> <msup> <mn>227</mn> <mo>∘</mo> </msup> </semantics></math> in <math display="inline"><semantics> <msup> <mn>0.25</mn> <mo>∘</mo> </msup> </semantics></math> increments. The U-Net is applied to select one image for each angular position that captures a desired droplet state. The selected projection images are then used to reconstruct a 3D volume for image analysis.</p>
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<p>The training <span class="html-italic">accuracy</span> (dotted gray line) and validation <span class="html-italic">accuracy</span> (solid black line) for 50 epochs can be tracked on the left Y-axis. The corresponding <span class="html-italic">IoU</span> (red markers) is given on the left Y-axis for 1, 5, 10, 20, 30, and 50 epochs of training.</p>
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<p>(<b>a</b>) The 2D droplet contours tracked over the 24 steps provided by the U-Net classification by plotting droplet radii over the droplet length. The diagram emphasizes the droplet evolution starting at the filling stage (dotted light-gray lines) and over the necking stage (dashed dark-gray line), until the droplet detaches (solid black line) in the circular capillary (top) with an inner diameter <math display="inline"><semantics> <msub> <mi>d</mi> <mrow> <mi>c</mi> <mo>,</mo> <mi>i</mi> </mrow> </msub> </semantics></math> of 1.6 mm and for the square capillary (bottom) with <math display="inline"><semantics> <msub> <mi>d</mi> <mi>h</mi> </msub> </semantics></math> = 1.6 mm. (<b>b</b>) The reconstructed 3D representation of the different droplet states in the circular (top) and square (bottom) capillary for the filling stage (left), necking stage (middle), and the detached droplet (right) for a constant Weber number <math display="inline"><semantics> <mrow> <mi>W</mi> <mi>e</mi> </mrow> </semantics></math>.</p>
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<p>Comparison of the input image, the ground truth, and the U-Net output for 1, 5, 10, 20, 30, and 50 epochs of training.</p>
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23 pages, 4848 KiB  
Article
Summer Chukchi Sea Near-Surface Salinity Variability in Satellite Observations and Ocean Models
by Semyon A. Grodsky, Nicolas Reul and Douglas Vandemark
Remote Sens. 2024, 16(18), 3397; https://doi.org/10.3390/rs16183397 - 12 Sep 2024
Viewed by 345
Abstract
The Chukchi Sea is an open estuary in the southwestern Arctic. Its near-surface salinities are higher than those of the surrounding open Arctic waters due to the key inflow of saltier and warmer Pacific waters through the Bering Strait. This salinity distribution may [...] Read more.
The Chukchi Sea is an open estuary in the southwestern Arctic. Its near-surface salinities are higher than those of the surrounding open Arctic waters due to the key inflow of saltier and warmer Pacific waters through the Bering Strait. This salinity distribution may suggest that interannual changes in the Bering Strait mass transport are the sole and dominant factor shaping the salinity distribution in the downstream Chukchi Sea. Using satellite sea surface salinity (SSS) retrievals and altimetry-based estimates of the Bering Strait transport, the relationship between the Strait transport and Chukchi Sea SSS distributions is analyzed from 2010 onward, focusing on the ice-free summer to fall period. A comparison of five different satellite SSS products shows that anomalous SSS spatially averaged over the Chukchi Sea during the ice-free period is consistent among them. Observed interannual temporal change in satellite SSS is confirmed by comparison with collocated ship-based thermosalinograph transect datasets. Bering Strait transport variability is known to be driven by the local meridional wind stress and by the Pacific-to-Arctic sea level gradient (pressure head). This pressure head, in turn, is related to an Arctic Oscillation-like atmospheric mean sea level pattern over the high-latitude Arctic, which governs anomalous zonal winds over the Chukchi Sea and affects its sea level through Ekman dynamics. Satellite SSS anomalies averaged over the Chukchi Sea show a positive correlation with preceding months’ Strait transport anomalies. This correlation is confirmed using two longer (>40-year), separate ocean data assimilation models, with either higher- (0.1°) or lower-resolution (0.25°) spatial resolution. The relationship between the Strait transport and Chukchi Sea SSS anomalies is generally stronger in the low-resolution model. The area of SSS response correlated with the Strait transport is located along the northern coast of the Chukotka Peninsula in the Siberian Coastal Current and adjacent zones. The correlation between wind patterns governing Bering Strait variability and Siberian Coastal Current variability is driven by coastal sea level adjustments to changing winds, in turn driving the Strait transport. Due to the Chukotka coastline configuration, both zonal and meridional wind components contribute. Full article
(This article belongs to the Special Issue Application of Remote Sensing in Coastline Monitoring)
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Figure 1

Figure 1
<p>September climatological SSS and standard deviation of monthly SSS from (<b>a</b>,<b>b</b>) satellite SMAP data (2015–2024), (<b>c</b>,<b>d</b>) high-resolution RARE1 (1980–2021) ocean reanalysis, and (<b>e</b>,<b>f</b>) low-resolution SODA (1980–2015) ocean reanalysis. Anadyr Current (1), Alaska Coastal Current (2), and Siberian Coastal Current (3) are sketched in (<b>e</b>). Chukchi Sea (180–200°E, 66–73°N) and Bering Strait (190–192.5°E, 65–66.5°N) box areas are shown in (<b>c</b>).</p>
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<p>September–October SSS anomaly (SSSA) from (<b>a</b>) four different satellite salinity products averaged over the Chukchi Sea box and (<b>b</b>) TSG transects averaged over (65.5°–70°N, 170°–167°W) domain. Bars for different satellite products are shifted in (<b>a</b>) to avoid overlapping. X-ticks correspond to Jan. See <a href="#sec2-remotesensing-16-03397" class="html-sec">Section 2</a> for description of satellite datasets. For each satellite dataset, the seasonal cycle of SSS is calculated based on the SMAP period since 2015.</p>
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<p>September (<b>a</b>–<b>i</b>) SMAP SSS, (<b>j</b>–<b>r</b>) ancillary SST from the Canada Meteorological Center (CMC) included in SMAP version 6.0. (<b>s</b>–<b>zz</b>) May–August de-trended multi-satellite sea level anomaly (SSHA).</p>
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<p>September SSS anomaly (SSSA) averaged over the Chukchi Sea box versus May–August along channel geostrophic velocity component (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>A</mi> </mrow> </semantics></math>) averaged over the Bering Strait box from the AVISO all-satellite altimeter analysis. Each symbol represents the mean of up to five satellite datasets shown in <a href="#remotesensing-16-03397-f002" class="html-fig">Figure 2</a>a, while vertical bars represent their STD. See <a href="#remotesensing-16-03397-f001" class="html-fig">Figure 1</a>c for the locations of the two boxes. Symbol colors correspond to years. Linear regression (solid), <math display="inline"><semantics> <mrow> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">A</mi> <mo>=</mo> <msubsup> <mrow> <mn>0.11</mn> </mrow> <mrow> <mn>0.03</mn> </mrow> <mrow> <mn>0.19</mn> </mrow> </msubsup> <mo>⋅</mo> <mo> </mo> <mi>v</mi> <mi>A</mi> </mrow> </semantics></math> explains ~40% of SSSA variance, where subscripts are the 95% confidence interval of the regression coefficient.</p>
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<p>(<b>a</b>) Spatial and (<b>b</b>) temporal parts of the leading EOF of May–August monthly de-trended SSH anomalies (SSHA) from satellite altimetry (1993–2023, ~53% of explained variance). EOF is computed for grid points with at least half of ice-free data. (<b>c</b>) SSHA averaged over the Chukchi Sea box (black in a, the same as in <a href="#remotesensing-16-03397-f001" class="html-fig">Figure 1</a>c).</p>
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<p>Time regression of May–August anomalies of (<b>a</b>) Chukchi Sea SSHA, (<b>b</b>) Bering Strait northward wind (<math display="inline"><semantics> <mrow> <mi>V</mi> <mn>10</mn> <mi>A</mi> </mrow> </semantics></math>) with atmospheric mean sea level pressure anomaly (MSLPA) elsewhere. (<b>c</b>,<b>d</b>) Time series of May–August mean SSHA and <math display="inline"><semantics> <mrow> <mi>V</mi> <mn>10</mn> <mi>A</mi> </mrow> </semantics></math>. Values in (<b>a</b>,<b>b</b>) show MSLPA (mbar) corresponding to one STD of SSHA and <math display="inline"><semantics> <mrow> <mi>V</mi> <mn>10</mn> <mi>A</mi> </mrow> </semantics></math>, respectively. Panel (<b>c</b>) is the same as in <a href="#remotesensing-16-03397-f005" class="html-fig">Figure 5</a>c.</p>
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<p>Monthly (May–August) Bering Strait geostrophic velocity anomaly (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>A</mi> </mrow> </semantics></math>) from satellite altimetry vs. (<b>a</b>) Bering Strait meridional wind anomaly (<math display="inline"><semantics> <mrow> <mi>V</mi> <mn>10</mn> <mi>A</mi> </mrow> </semantics></math>) and (<b>c</b>) Chukchi Sea surface height anomaly (SSHA). Velocity anomaly components (<b>b</b>) due to wind (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>A</mi> <mi>w</mi> </mrow> </semantics></math>), and (<b>d</b>) Chukchi Sea SSHA (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>A</mi> <mi>h</mi> </mrow> </semantics></math>), which are calculated by subtracting signals linearly correlated with SSHA and <math display="inline"><semantics> <mrow> <mi>V</mi> <mn>10</mn> <mi>A</mi> </mrow> </semantics></math>, respectively.</p>
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<p>Chukchi Sea SSS anomaly temporally regressed on BS salinity transport anomaly components due to (<b>a</b>) pressure head (<math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>v</mi> </mrow> <mrow> <mi>h</mi> </mrow> <mrow> <mo>′</mo> </mrow> </msubsup> <mo>⋅</mo> <mo>Δ</mo> <mi>S</mi> </mrow> </semantics></math>), (<b>b</b>) meridional winds over the Strait (<math display="inline"><semantics> <mrow> <mi>v</mi> <msub> <mrow> <mo>′</mo> </mrow> <mrow> <mi>w</mi> </mrow> </msub> <mo>⋅</mo> <mo>Δ</mo> <mi>S</mi> </mrow> </semantics></math>), and (<b>c</b>) salinity variations in the Strait (<math display="inline"><semantics> <mrow> <mi>v</mi> <mo>⋅</mo> <mi>S</mi> <mo>′</mo> </mrow> </semantics></math>). Magnitudes correspond to one standard deviation of the respective Bering Strait forcing factor. Inlays show vertical profiles of salinity response in red (Chukotka) and blue (eastern Chukchi Sea) boxes shown in (<b>c</b>). Eastern box vertical profiles are not shown in (<b>a</b>,<b>b</b>) due to negligible response magnitudes. Data are from 1980–2021 RARE1 ocean reanalysis. Points with fewer than 20 examples of September ice-free data are blanked. The geographic grid is drawn with 10° and 5° intervals in longitude and latitude, respectively, starting from 170°E, 60°N.</p>
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<p>The same as in <a href="#remotesensing-16-03397-f008" class="html-fig">Figure 8</a> but for lower-resolution SODA3 reanalysis.</p>
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<p>(<b>a</b>) Seasonal cycle of total (<math display="inline"><semantics> <mrow> <mi>v</mi> </mrow> </semantics></math>) and geostrophic (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>g</mi> </mrow> </semantics></math>) at the surface averaged across Bering Strait along 65.75N. (<b>b</b>) Scatter diagram of Bering Strait volume transport anomaly with total (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>A</mi> </mrow> </semantics></math>) and geostrophic (<math display="inline"><semantics> <mrow> <mi>v</mi> <mi>g</mi> <mi>A</mi> </mrow> </semantics></math>) monthly anomalies. Because both velocity anomalies are linearly correlated with Bering Strait (BS) transport anomalies, they also are mutually correlated, <math display="inline"><semantics> <mrow> <mi>v</mi> <mi>g</mi> <mi>A</mi> <mo>=</mo> <mn>0.63</mn> <mo>⋅</mo> <mi>v</mi> <mi>A</mi> </mrow> </semantics></math>.</p>
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<p>Regression of (<b>a</b>) winter (November–February) and (<b>b</b>) summer (May–August) AO index with ERA5 monthly MSLPA. MSLP values correspond to one standard deviation of AO index during winter and summer months. Note the difference in color scale limits between (<b>a</b>,<b>b</b>). (<b>c</b>) Scatter diagram of summer sea level anomaly averaged over the Chukchi Sea box (<a href="#remotesensing-16-03397-f001" class="html-fig">Figure 1</a>c) and AO index.</p>
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<p>Time regression of May–August Bering Strait salinity flux anomaly components, (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>v</mi> <mo>′</mo> <mo>Δ</mo> <mi>S</mi> </mrow> </semantics></math> and (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>v</mi> <msup> <mrow> <mi>S</mi> </mrow> <mrow> <mo>′</mo> </mrow> </msup> </mrow> </semantics></math>, on concurrent de-trended SSH anomalies. Magnitudes correspond to one standard deviation of the respective salinity flux component.</p>
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<p>The same as in <a href="#remotesensing-16-03397-f008" class="html-fig">Figure 8</a> but for ORA5S reanalysis based on the NEMO ocean model.</p>
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<p>Time regression of May–August Bering Strait salinity flux anomaly component, <math display="inline"><semantics> <mrow> <mi>v</mi> <mi>S</mi> <mo>′</mo> </mrow> </semantics></math>, on concurrent atmospheric mean sea level pressure anomaly. Magnitude corresponds to one STD of <math display="inline"><semantics> <mrow> <mi>v</mi> <mi>S</mi> <mo>′</mo> </mrow> </semantics></math>.</p>
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28 pages, 8636 KiB  
Article
Karst Hydrological Connections of Lakes and Neoproterozoic Hydrogeological System between the Years 1985–2020, Lagoa Santa—Minas Gerais, Brazil
by Wallace Pacheco Neto, Rodrigo de Paula and Paulo Galvão
Water 2024, 16(18), 2591; https://doi.org/10.3390/w16182591 - 12 Sep 2024
Viewed by 394
Abstract
This study focuses on a complex Brazilian Neoproterozoic karst (hydro)geological and geomorphological area, consisting of metapelitic–carbonate sedimentary rocks of ~740–590 Ma, forming the largest carbonate sequence in the country. At the center of the area lies the Lagoa Santa Karst Environmental Protection Area [...] Read more.
This study focuses on a complex Brazilian Neoproterozoic karst (hydro)geological and geomorphological area, consisting of metapelitic–carbonate sedimentary rocks of ~740–590 Ma, forming the largest carbonate sequence in the country. At the center of the area lies the Lagoa Santa Karst Environmental Protection Area (LSKEPA), located near the Minas Gerais’ state capital, Belo Horizonte, and presents a series of lakes associated with the large fluvial system of the Velhas river under the influence, locally, of carbonate rocks. The hydrodynamics of carbonate lakes remain enigmatic, and various factors can influence the behavior of these water bodies. This work analyzed the hydrological behavior of 129 lakes within the LSKEPA to understand potential connections with the main karst aquifer, karst-fissure aquifer, and porous aquifer, as well as their evolution patterns in the physical environment. Pluviometric surveys and satellite image analysis were conducted from 1984 to 2020 to observe how the lakes’ shorelines behaved in response to meteorological variations. The temporal assessment for understanding landscape evolution proves to be an effective tool and provides important information about the interaction between groundwater and surface water. The 129 lakes were grouped into eight classes representing the hydrological connection patterns with the aquifers in the region, with classes defined for perennial lakes: (1) constantly connected, (2) seasonally disconnected, and (3) disconnected; for intermittent lakes: (4) disconnected during the analyzed time interval, (5) seasonally connected, (6) disconnected, (7) extremely disconnected, and (8) intermittent lakes that connected and stopped drying up. The patterns observed in the variation of lakes’ shorelines under the influence of different pluviometric moments showed a positive correlation, especially in dry periods, where these water bodies may be functioning as recharge or discharge zones of the karst aquifer. These inputs and outputs are conditioned to the well-developed karst tertiary porosity, where water flow in the epikarst moves according to the direction of enlarged karstified fractures, rock foliation planes, and lithological contacts. Other factors may condition the hydrological behavior of the lakes, such as rates of evapotranspiration, intensity of rainfall during rainy periods, and excessive exploitation of water. Full article
(This article belongs to the Special Issue Recent Advances in Karstic Hydrogeology, 2nd Edition)
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Figure 1
<p>Geological and location map of the study area highlighting the Lagoa Santa Karst Environmental Protection Area, Minas Gerais, Brazil, and the lakes analyzed in this work. Geology modified from “Projeto Vida” [<a href="#B21-water-16-02591" class="html-bibr">21</a>] and profile modified from [<a href="#B22-water-16-02591" class="html-bibr">22</a>].</p>
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<p>Example of Landsat satellite images used in this study, representing the rainy season of 1999 and the dry season of the same year.</p>
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<p>Graphical representation of perimeter variation over the years for the studied lakes (example Lake 28).</p>
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<p>Flowchart summarizing the steps taken to identify the expansion or contraction behavior of each lake over the analyzed years.</p>
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<p>Bar chart representing the annual average precipitation between the hydrological years 1984–1985 and 2019–2020. The orange bars indicate precipitation during the dry months (April to September), while the blue bars show precipitation during the wet months (October to March). The red line marks the average precipitation for the 36 years analyzed in this study, with confidence intervals represented by the dashed blue line (positive confidence interval) and the dashed yellow line (negative confidence interval).</p>
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<p>Bar chart representing rainfall and drought cycles. Values above the historical average (black dashed line) during dry precipitation cycles were defined as atypical dry hydrological years, while values below the historical average (black dashed line) during wet cycles were defined as atypical wet hydrological years.</p>
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<p>Graph of the precipitation cycles, showing their averages, and trend lines representing the precipitation variation within each cycle. Below is a table summarizing the averages and equations of the trend lines for each cycle, with angular coefficients in blue (positive) and red (negative).</p>
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<p>Identification and distribution of perennial lakes (in blue) and intermittent lakes (in orange) in the study area. (<b>A</b>) and (<b>B</b>): Highlights of some lakes.</p>
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<p>Graphical representation of the perimeter variation of perennial lake 23 over the time interval used. The precipitation cycles and the trend lines of perimeter variation in each cycle can be observed. The table below provides the trend line equations within each cycle, along with their positive and negative angular coefficients.</p>
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<p>Graphical representation with examples of the behavior of perennial lakes that are constantly connected (<b>a</b>), seasonally disconnected perennial lakes (<b>b</b>), and disconnected perennial lakes (<b>c</b>).</p>
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<p>Illustration of the proposed classes of hydrological connection for the analyzed perennial lakes.</p>
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<p>Graphical representation, with examples of the behavior of intermittent lakes that disconnected from the aquifer at some point (<b>a</b>), intermittently connected lakes (<b>b</b>), disconnected intermittent lakes (<b>c</b>), extremely disconnected intermittent lakes (<b>d</b>), and fully connected intermittent lakes (<b>e</b>).</p>
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24 pages, 10739 KiB  
Article
Daily Brain Metabolic Rhythms of Wild Nocturnal Bats
by Tianhui Wang, Hui Wang, Yujia Chu, Mingyue Bao, Xintong Li, Guoting Zhang and Jiang Feng
Int. J. Mol. Sci. 2024, 25(18), 9850; https://doi.org/10.3390/ijms25189850 - 12 Sep 2024
Viewed by 227
Abstract
Circadian rhythms are found in a wide range of organisms and have garnered significant research interest in the field of chronobiology. Under normal circadian function, metabolic regulation is temporally coordinated across tissues and behaviors within a 24 h period. Metabolites, as the closest [...] Read more.
Circadian rhythms are found in a wide range of organisms and have garnered significant research interest in the field of chronobiology. Under normal circadian function, metabolic regulation is temporally coordinated across tissues and behaviors within a 24 h period. Metabolites, as the closest molecular regulation to physiological phenotype, have dynamic patterns and their relationship with circadian regulation remains to be fully elucidated. In this study, untargeted brain metabolomics was employed to investigate the daily rhythms of metabolites at four time points corresponding to four typical physiological states in Vespertilio sinensis. Key brain metabolites and associated physiological processes active at different time points were detected, with 154 metabolites identified as rhythmic. Analyses of both metabolomics and transcriptomics revealed that several important physiological processes, including the pentose phosphate pathway and oxidative phosphorylation, play key roles in regulating rhythmic physiology, particularly in hunting and flying behaviors. This study represents the first exploration of daily metabolic dynamics in the bat brain, providing insights into the complex regulatory network of circadian rhythms in mammals at a metabolic level. These findings serve as a valuable reference for future studies on circadian rhythms in nocturnal mammals. Full article
(This article belongs to the Section Molecular Endocrinology and Metabolism)
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Graphical abstract

Graphical abstract
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<p>Annotated metabolites in the bat brain were detected for (<b>A</b>) super-classification, (<b>B</b>) classification, and (<b>C</b>) sub-classification, respectively.</p>
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<p>Results of inter-sample relationships. (<b>A</b>) Metabolite principal component analysis (PCA) among samples of the brain at different states. (<b>B</b>) The heat map of sample correlation analysis.</p>
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<p>Heatmaps of 293 DAMs from six pairwise comparisons across four time points corresponding to four physiological states. The four columns represent the amount of each DAM detected in the rest, sleep, wake, and activity state, respectively.</p>
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<p>(<b>A</b>) Venn diagram of DAMs from four pairwise comparisons involved every two adjacent time points. (<b>B</b>) The change patterns of eight common metabolites from four pairwise comparisons detected. Raw data normalization was conducted using MetaboAnalystR 4.0 [<a href="#B24-ijms-25-09850" class="html-bibr">24</a>], which was integrated within the R software version 4.2.3 by utilizing the sum of features for each sample.</p>
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<p>KEGG pathways were significantly enriched by DAMs detected from six pairwise comparisons. Pathways enriched by higher abundant metabolites detected in the former state than in the latter of one comparison are shown in red, and pathways enriched by higher abundant metabolites detected in the latter state are shown in blue. Significant pathways were obtained by KEGG enrichment analysis of DAMs in six pairwise comparison groups. Pathways significantly enriched in DAMs that were more abundant in the previous state in the comparison group are shown in red. Pathways significantly enriched in DAMs that were richer in the latter state in the comparison group are shown in blue.</p>
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<p>Summary of the more active physiological processes for each time point in the bat brain.</p>
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<p>Clusters of 293 DAMs according to their change patterns across four time points. (<b>A</b>) Ten clusters of DAMs. The number under the cluster indicates the DAMs clustered in it. (<b>B</b>) KEGG pathways were significantly enriched by DAMs from cluster 1, cluster 6, and cluster 9 (DAMs from other clusters were not significantly enriched in any pathway).</p>
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<p>(<b>A</b>)The KEGG pathways were significantly enriched by rhythmic DAMs. (<b>B</b>) The KEGG pathway–metabolite interaction network analysis. Diamonds represent pathways, circles represent metabolites.</p>
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<p>Clusters of 154 rhythmic DAMs according to their change patterns across four time points. Six clusters of rhythmic DAMs (<b>up</b>) and related heatmaps (<b>down</b>). The number under the cluster indicates the rhythmic metabolites clustered in it.</p>
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<p>The pathway–metabolite interaction network of significantly enriched pathways from six pairwise comparisons and associated involved metabolites. The rhythmic and differential characteristics of metabolites were labeled with different colors.</p>
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<p>Illustration of the main process of the pentose phosphate pathway. The simple heatmap showed the content of corresponding metabolites across four time points from 4:00 to 22:00. The deeper the red color, the higher the content; the deeper the green color, the lower the content. The blue pathways showed the rhythmic metabolites detected in the brain of a bat.</p>
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<p>Correlation of brain metabolites with four states based on WGCNA. (<b>A</b>) Module–state relationship. (<b>B</b>) Yellow module metabolite network for the metabolites from the yellow module. The top 10 metabolites with the highest connectivity are shown with highlighted colors.</p>
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<p>(<b>A</b>) A network of DEGs correlated with tryptophan. The red connecting line indicates a positive correlation and the blue connecting line indicates a negative correlation. (<b>B</b>) The expressed trends of tryptophan and <span class="html-italic">Per1</span>/<span class="html-italic">2</span> across four states.</p>
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<p>Melatonin synthesis process. The simple heatmap showed the content of corresponding metabolites across four time points from 4:00 to 22:00. The deeper the red color, the higher the content; the deeper the green color, the lower the content.</p>
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26 pages, 29764 KiB  
Article
Mapping Fruit-Tree Plantation Using Sentinel-1/2 Time Series Images with Multi-Index Entropy Weighting Dynamic Time Warping Method
by Weimeng Xu, Zhenhong Li, Hate Lin, Guowen Shao, Fa Zhao, Han Wang, Jinpeng Cheng, Lei Lei, Riqiang Chen, Shaoyu Han and Hao Yang
Remote Sens. 2024, 16(18), 3390; https://doi.org/10.3390/rs16183390 - 12 Sep 2024
Viewed by 367
Abstract
Plantation distribution information is of great significance to the government’s macro-control, optimization of planting layout, and realization of efficient agricultural production. Existing studies primarily relied on high spatiotemporal resolution remote sensing data to address same-spectrum, different-object classification by extracting phenological information from temporal [...] Read more.
Plantation distribution information is of great significance to the government’s macro-control, optimization of planting layout, and realization of efficient agricultural production. Existing studies primarily relied on high spatiotemporal resolution remote sensing data to address same-spectrum, different-object classification by extracting phenological information from temporal imagery. However, the classification problem of orchard or artificial forest, where the spectral and textural features are similar and their phenological characteristics are alike, still presents a substantial challenge. To address this challenge, we innovatively proposed a multi-index entropy weighting DTW method (ETW-DTW), building upon the traditional DTW method with single-feature inputs. In contrast to previous DTW classification approaches, this method introduces multi-band information and utilizes entropy weighting to increase the inter-class distances. This allowed for accurate classification of orchard categories, even in scenarios where the spectral textures were similar and the phenology was alike. We also investigated the impact of fusing optical and Synthetic Aperture Radar (SAR) data on the classification accuracy. By combining Sentinel-1 and Sentinel-2 time series imagery, we validated the enhanced classification effectiveness with the inclusion of SAR data. The experimental results demonstrated a noticeable improvement in orchard classification accuracy under conditions of similar spectral characteristics and phenological patterns, providing comprehensive information for orchard mapping. Additionally, we further explored the improvement in results based on two different parcel-based classification strategies compared to pixel-based classification methods. By comparing the classification results, we found that the parcel-based averaging method has advantages in clearly defining orchard boundaries and reducing noise interference. In conclusion, the introduction of the ETW-DTW method is of significant practical importance in addressing the challenge of same-spectrum, different-object classification. The obtained orchard distribution can provide valuable information for the government to optimize the planting structure and layout and regulate the macroeconomic benefits of the fruit industry. Full article
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Figure 1
<p>(<b>a</b>) Topography of the study area; (<b>b</b>) the location of the study area in Shanxi Province and the position highlighted by a black triangle; (<b>c</b>) a typical fruit plantation landscape in Miaoshang county via Google Earth (Google Earth, Image © 2020 DigitalGlobe).</p>
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<p>Cropping calendars of major crops in the study area.</p>
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<p>Temporal coverage of the Sentinel-1 and Sentinel-2 time series data used in this study. (<b>a</b>) The cloud cover of Sentinel-2 time series scenes of 2019 and 2020; (<b>b</b>) The data collection of Sentinel-1 and Sentinel-2; (<b>c</b>) The number of high quality observations of Sentinel-2.</p>
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<p>The workflow of the ETW-DTW approach for orchards classification.</p>
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<p>The Workflow of Minimum intra-class Distance for Classification. The symbol * denotes the element-wise multiplication of corresponding elements in each matrix.</p>
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<p>Example of the HANTS-fitted and the original NDVI time series in 2020. The red points represent the original values of the NDVI temporal profile, and the HANTS fitted curve is illustrated by the bule line.</p>
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<p>The order and change law of index materiality. (<b>a</b>) The correlation of each index in jujube samples; (<b>b</b>) the correlation of each index in persimmon samples; (<b>c</b>) the correlation of each index in apple samples; (<b>d</b>) the correlation of each index in peach samples; (<b>e</b>) the correlation of each index in corn samples; (<b>f</b>) the importance of each index in each period.</p>
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<p>Differences in timing curves of each index or band from November 2019 to April 2020. (<b>a</b>) NDVI timing reference curve for each category; (<b>b</b>) MNDWI timing reference curve for each category; (<b>c</b>) NIR timing reference curve for each category; (<b>d</b>) SWIR timing reference curve for each category; (<b>e</b>) VV/VH timing reference curve for each category; the buffer band is the standard deviation of each timing curve.</p>
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<p>Entropy weight matrix. The horizontal axis represents various indices used in the classification, while the vertical axis represents the categories to be classified. Colors range from purple to yellow, indicating the magnitude of weights—darker colors correspond to larger weights, and lighter colors to smaller weights. For instance, when classifying with the apple category as the standard curve, the pixels/plots to be classified need to calculate TW-DTW distances with the respective NDVI, NIR, SWIR, MNDWI, and VV/VH temporal curves of apples. The obtained distances were then multiplied by the corresponding weights of each index to derive the final ETW-DTW distance.</p>
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<p>Spatial distribution map of various crops at plot scale: (<b>a</b>) distribution map of ETW-DTW method; (<b>b</b>) distribution map of results with NDVI timing curve as input; (<b>c</b>) distribution map of results with SWIR timing curve as input; (<b>d</b>) distribution map of results with VV/VH timing curve as input; (<b>e</b>) distribution map of results with MNDWI timing curve as input; (<b>f</b>) distribution map of results with NIR timing curve as input.</p>
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<p>Distribution extraction results of pixel scale and plot scale in ETW-DTW. (<b>a</b>) classification results of pixel scale ETW-DTW; (<b>b</b>) classification results of P1-based ETW-DTW; (<b>c</b>) classification results of P2-based ETW-DTW.</p>
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<p>Comparison of local magnification results of pixel scale and plot scale: the first row (<b>a1</b>–<b>d1</b>) displays the Google image of these four areas, the second row (<b>a2</b>–<b>d2</b>) displays the P1-based classification results, the third row (<b>a3</b>–<b>d3</b>) displays the pixel scale-based classification results, and the 4th row (<b>a4</b>–<b>d4</b>) displays the P2-based classification results.</p>
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<p>Entropy weight matrix of optical indices. The horizontal axis represents various indices (NDVI, NIR, SWIR, and MNDWI) of optical imagery. The vertical axis represents the categories to be classified (apples, peaches, persimmons, and jujubes). Colors range from purple to yellow, indicating the magnitude of weights—darker colors corresponded to larger weights, and lighter colors to smaller weights.</p>
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22 pages, 6472 KiB  
Article
Identifying Determinants of Spatiotemporal Disparities in Ecological Quality of Mongolian Plateau
by Zhengtong Wang, Yongze Song, Zehua Zhang, Gang Lin, Peng Luo, Xueyuan Zhang and Zhengyuan Chai
Remote Sens. 2024, 16(18), 3385; https://doi.org/10.3390/rs16183385 - 12 Sep 2024
Viewed by 325
Abstract
Vegetation quality is crucial for maintaining ecological health, and remote sensing techniques offer precise assessments of vegetation’s environmental quality. Although existing indicators and remote sensing approaches provide extensive spatial coverage, challenges remain in effectively integrating diverse indicators for a comprehensive evaluation. This study [...] Read more.
Vegetation quality is crucial for maintaining ecological health, and remote sensing techniques offer precise assessments of vegetation’s environmental quality. Although existing indicators and remote sensing approaches provide extensive spatial coverage, challenges remain in effectively integrating diverse indicators for a comprehensive evaluation. This study introduces a comprehensive ecological quality index (EQI) to assess vegetation quality on the Mongolian Plateau from 2001 to 2020 and to identify the determinants of EQI variations over space and time. We developed the EQI using remotely sensed normalized difference vegetation index (NDVI) data and the net primary productivity (NPP). Our analysis revealed distinct spatial patterns, with high ecological quality concentrated in northern Mongolia and eastern Inner Mongolia. Temporal fluctuations, indicative of ecological shifts, were primarily observed in eastern Mongolia and specific zones of Inner Mongolia. We employed a Geographically Optimal Zones-based Heterogeneity (GOZH) model to analyze the spatial scales and interactions influencing EQI patterns. This study found that precipitation, with an Omega value of 0.770, was the dominant factor affecting the EQI, particularly at spatial scales of 40–50 km. The GOZH model provided deeper insights into the spatial determinants of the EQI compared with previous models, highlighting the importance of climatic variables and their interactions in driving ecological quality. This research enhanced our understanding of vegetation quality dynamics and established a foundation for ecosystem conservation and informed management strategies, emphasizing the critical role of climate, especially precipitation, in shaping ecological landscapes. Full article
(This article belongs to the Section Earth Observation Data)
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<p>The location and geographical condition of the study area, the Mongolian Plateau, for the analysis of spatiotemporal disparities in ecological quality.</p>
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<p>The spatial distribution of potential variables influencing the EQI includes soil, climate, geographical, and human activity variables.</p>
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<p>Spatiotemporal distributions and analysis of ecological quality metrics over the Mongolian Plateau from 2001 to 2020, with spatial distribution of the annual mean NDVI (<b>A</b>) and NDVI trend derived from linear regression (<b>B</b>), statistical summary of NDVI trends (<b>C</b>), annual NDVI trend for the entire region (<b>D</b>), spatial distribution of the annual mean NPP (<b>E</b>) and NPP trend derived from linear regression (<b>F</b>), statistical summary of NPP trends (<b>G</b>), and annual NPP trend for the entire region (<b>H</b>). The blue lines in (<b>D</b>,<b>H</b>) are the fitted linear trends.</p>
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<p>Spatial distribution of the estimated EQI of the Mongolian Plateau. (<b>A</b>) Annual mean EQI from 2001 to 2020. (<b>B</b>) Standard deviation (SD) of the EQI during the time period. (<b>C</b>) The relationship between the mean and SD of the EQI index. (The gradient from blue to yellow represents the observation density, increasing from low to high, and the red line illustrates the fitted nonlinear trend.).</p>
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<p>Distribution and analysis of the temporal trends in the EQI from 2001 to 2020 over the Mongolian Plateau: (<b>A</b>) spatial distribution of EQI trends; (<b>B</b>) spatial distribution of the significance levels of the EQI trends; (<b>C</b>) EQI trend for the entire study area (the blue line is the fitted linear trend); and (<b>D</b>) statistical summary of EQI trends.</p>
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<p>Spatial clusters of EQI trends across the Mongolian Plateau.</p>
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<p>Spatial scale effects of determinants for EQI (<b>A</b>) and EQI trends (<b>B</b>).</p>
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<p>The power of determinants of individual variables associated with the EQI (<b>A</b>) and EQI trends (<b>B</b>).</p>
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<p>The power of determinants of variable interactions associated with the EQI and EQI trends.</p>
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<p>Model performance comparison between GOZH and OPGD models for exploring determinants of EQI (<b>A</b>) and EQI trends (<b>B</b>).</p>
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4 pages, 170 KiB  
Proceeding Paper
Enhancing Water Demand Forecasting: Leveraging LSTM Networks for Accurate Predictions
by Fatemeh Boloukasli ahmadgourabi, Melica Khashei Varnamkhasti, Morad Nosrati Habibi, Niuosha Hedaiaty Marzouny and Rebecca Dziedzic
Eng. Proc. 2024, 69(1), 120; https://doi.org/10.3390/engproc2024069120 - 12 Sep 2024
Viewed by 124
Abstract
This study aims to create a reliable water-demand forecasting system using Long Short-Term Memory networks. The model integrates hourly water demands from 10 District Metered Areas of a Water Distribution Network in northeast Italy and weather data, handling missing values with LSTM-based data [...] Read more.
This study aims to create a reliable water-demand forecasting system using Long Short-Term Memory networks. The model integrates hourly water demands from 10 District Metered Areas of a Water Distribution Network in northeast Italy and weather data, handling missing values with LSTM-based data imputation. It considers temporal aspects like time, weekdays, holidays, and weekend patterns, employing sine and cosine transformations to capture daily cycles. To ensure the model’s robustness, the testing was conducted during the last week of the dataset, specifically week 81, with iterative adjustments to the LSTM’s hyperparameters to optimize prediction accuracy. These tuning efforts focused on learning rate, number of layers, and batch size, tailored to maximize the system’s performance. This method is essential for smart decision-making in water utility management and demonstrates significant potential for improving operational efficiencies. Full article
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