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Keywords = uncertainty measure

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21 pages, 1750 KiB  
Article
Optimal Regulation Strategy of Distribution Network with Photovoltaic-Powered Charging Stations Under Multiple Uncertainties: A Bi-Level Stochastic Optimization Approach
by Nanxing Chen, Zhaobin Du and Wei Du
Electronics 2024, 13(23), 4600; https://doi.org/10.3390/electronics13234600 - 21 Nov 2024
Abstract
In order to consider the impact of multiple uncertainties on the interaction between the distribution network operator (DNO) and photovoltaic powered charging stations (PVCSs), this paper proposes a regulation strategy for a distribution network with a PVCS based on bi-level stochastic optimization. First, [...] Read more.
In order to consider the impact of multiple uncertainties on the interaction between the distribution network operator (DNO) and photovoltaic powered charging stations (PVCSs), this paper proposes a regulation strategy for a distribution network with a PVCS based on bi-level stochastic optimization. First, the interaction framework between the DNO and PVCS is established to address the energy management and trading problems of different subjects in the system. Second, considering the uncertainties in the electricity price and PV output, a bi-level stochastic model is constructed with the DNO and PVCS targeting their respective interests. Furthermore, the conditional value-at-risk (CVaR) is introduced to measure the relationship between the DNO’s operational strategy and the uncertain risks. Next, the Karush–Kuhn–Tucker (KKT) conditions and duality theorem are utilized to tackle the challenging bi-level problem, resulting in a mixed-integer second-order cone programming (MISCOP) model. Finally, the effectiveness of the proposed regulation strategy is validated on the modified IEEE 33-bus system. Full article
(This article belongs to the Special Issue Integration of Distributed Energy Resources in Smart Grids)
18 pages, 1554 KiB  
Article
Mapping Seagrass Distribution and Abundance: Comparing Areal Cover and Biomass Estimates Between Space-Based and Airborne Imagery
by Victoria J. Hill, Richard C. Zimmerman, Dorothy A. Byron and Kenneth L. Heck
Remote Sens. 2024, 16(23), 4351; https://doi.org/10.3390/rs16234351 - 21 Nov 2024
Abstract
This study evaluated the effectiveness of Planet satellite imagery in mapping seagrass coverage in Santa Rosa Sound, Florida. We compared very-high-resolution aerial imagery (0.3 m) collected in September 2022 with high-resolution Planet imagery (~3 m) captured during the same period. Using supervised classification [...] Read more.
This study evaluated the effectiveness of Planet satellite imagery in mapping seagrass coverage in Santa Rosa Sound, Florida. We compared very-high-resolution aerial imagery (0.3 m) collected in September 2022 with high-resolution Planet imagery (~3 m) captured during the same period. Using supervised classification techniques, we accurately identified expansive, continuous seagrass meadows in the satellite images, successfully classifying 95.5% of the 11.18 km2 of seagrass area delineated manually from the aerial imagery. Our analysis utilized an occurrence frequency (OF) product, which was generated by processing ten clear-sky images collected between 8 and 25 September 2022 to determine the frequency with which each pixel was classified as seagrass. Seagrass patches encompassing at least nine pixels (~200 m2) were almost always detected by our classification algorithm. Using an OF threshold equal to or greater than >60% provided a high level of confidence in seagrass presence while effectively reducing the impact of small misclassifications, often of individual pixels, that appeared sporadically in individual images. The image-to-image uncertainty in seagrass retrieval from the satellite images was 0.1 km2 or 2.3%, reflecting the robustness of our classification method and allowing confidence in the accuracy of the seagrass area estimate. The satellite-retrieved leaf area index (LAI) was consistent with previous in situ measurements, leading to the estimate that 2700 tons of carbon per year are produced by the Santa Rosa Sound seagrass ecosystem, equivalent to a drawdown of approximately 10,070 tons of CO2. This satellite-based approach offers a cost-effective, semi-automated, and scalable method of assessing the distribution and abundance of submerged aquatic vegetation that provides numerous ecosystem services. Full article
23 pages, 9176 KiB  
Article
Influence of Boundary Conditions on the Estimation of Thermal Properties in Insulated Building Walls
by Manon Rendu, Jérôme Le Dréau, Patrick Salagnac and Maxime Doya
Buildings 2024, 14(12), 3706; https://doi.org/10.3390/buildings14123706 - 21 Nov 2024
Abstract
The objective of this study is to evaluate the ability of inverse techniques to estimate the resistance and the capacity of a highly insulated multilayer wall under real weather conditions. The wall is equipped with temperature sensors inside and on its inner and [...] Read more.
The objective of this study is to evaluate the ability of inverse techniques to estimate the resistance and the capacity of a highly insulated multilayer wall under real weather conditions. The wall is equipped with temperature sensors inside and on its inner and outer surfaces, and the boundary conditions have been measured over a 14-day period. Uncertainties on various parameters of the model are evaluated, including internal and external convective heat transfer coefficients (±20% and ±7 W.m-².K−1 respectively), external long-wave heat transfer coefficient (±0.15 W.m−2.K−1) and solar absorption coefficient (±0.06). A sensitivity analysis demonstrated the high correlation with some parameters defining the thermal performance of the walls (thermal resistance or capacity). A solution is proposed to limit the number of identified parameters, while allowing the identification of the thermal resistance and the thermal capacity of the walls. There are two cases: either the weather conditions are accurately measured (temperature, short- and long-wave radiation) and the thermal characteristics can be assessed, or intrusive sensors are installed, and the thermal characteristics can be evaluated more accurately. Full article
(This article belongs to the Section Building Energy, Physics, Environment, and Systems)
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Figure 1

Figure 1
<p>Locations of sensors in the wall.</p>
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<p>Photos of the experimental setup: (<b>a</b>) outdoor air temperature sensor; (<b>b</b>) radiometers; (<b>c</b>) sonic anemometer; (<b>d</b>) outdoor surface temperature sensors; (<b>e</b>) indoor air temperature sensors with ventilated shield and indoor surface temperature sensors.</p>
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<p>Boundary conditions for the <span class="html-italic">ROLBS case:</span> temperature and solar radiation (<b>a</b>), the related wind rose (<b>b</b>) and wind speed and direction against time (<b>c</b>).</p>
Full article ">Figure 3 Cont.
<p>Boundary conditions for the <span class="html-italic">ROLBS case:</span> temperature and solar radiation (<b>a</b>), the related wind rose (<b>b</b>) and wind speed and direction against time (<b>c</b>).</p>
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<p>Boundary conditions for the <span class="html-italic">typical cloudy day</span> and the <span class="html-italic">typical sunny day</span>.</p>
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<p>Estimation of location of sensor <span class="html-italic">S<sub>2</sub></span> based on the temperature distribution under steady-state conditions.</p>
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<p>Location of boundary conditions and sensors.</p>
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<p>Outdoor convective heat transfer coefficients for different correlations in the <span class="html-italic">ROLBS case</span>.</p>
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<p><span class="html-italic">RC model</span> structure for the <span class="html-italic">6R3C model</span>.</p>
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<p>Validation of the <span class="html-italic">24R21C model</span>.</p>
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<p>Principle of inverse method, adapted from [<a href="#B54-buildings-14-03706" class="html-bibr">54</a>].</p>
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<p>Study of the impact of the variation of heat transfer coefficients during the <span class="html-italic">cloudy day</span> and the <span class="html-italic">sunny day</span>.</p>
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<p>Sensitivity analysis of the parameters estimated during both typical days (<span class="html-italic">BC1</span>).</p>
Full article ">Figure 13
<p>Estimation of <span class="html-italic">R</span>- and <span class="html-italic">C</span>-values—data with and without noise—<span class="html-italic">BC1</span>.</p>
Full article ">Figure 14
<p>Sensitivity analysis of the parameters to be estimated with free floating conditions (<span class="html-italic">sunny day</span>) and with active heating (1 March 2019) with <span class="html-italic">BC2</span>.</p>
Full article ">Figure 15
<p>Estimation of <span class="html-italic">R</span>- and <span class="html-italic">C</span>-values—data with and without noise—<span class="html-italic">BC2</span>.</p>
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<p>Estimation of <span class="html-italic">R</span>- and <span class="html-italic">C</span>-values from measured experimental data and using outside and inside boundary conditions.</p>
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<p>Temperature measured in the wall and estimated by the model and the residuals.</p>
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<p>Procedure for experimental design.</p>
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12 pages, 3514 KiB  
Article
Elevational Effects of Climate Warming on Tree Growth in a Picea schrenkiana Forest in the Eastern Tianshan Mountains
by Jianing He, Zehao Shen, Caiwen Ning, Wentao Zhang and Ümüt Halik
Forests 2024, 15(12), 2052; https://doi.org/10.3390/f15122052 - 21 Nov 2024
Viewed by 176
Abstract
Considerable uncertainty exists regarding the overall effects of future climate change on forests in arid mountains, and the elevational range of drought-induced tree growth decline remains unclear. Tianshan is the largest mountain in arid regions globally. Here, we analyzed tree ring data of [...] Read more.
Considerable uncertainty exists regarding the overall effects of future climate change on forests in arid mountains, and the elevational range of drought-induced tree growth decline remains unclear. Tianshan is the largest mountain in arid regions globally. Here, we analyzed tree ring data of pure stands of Schrenk spruce (Picea schrenkiana Fisch. et Mey.) in the Jiangbulake region in the eastern Tianshan Mountains along an elevational gradient (1800–2600 m a.s.l.). The radial growth of P. schrenkiana trees declined in three of the nine sample strips (1800–2100 m a.s.l.) over the last two decades. P. schrenkiana growth response (measured by the tree ring width index, RWI) to temperature significantly changed at an elevational “inflection point” at 2100–2200 m. RWI was significantly negatively correlated with temperature at low elevations, whereas the opposite was observed at high elevations. Precipitation and minimum temperatures in winter and spring and mean temperatures in spring and summer were the main drivers of P. schrenkiana growth, with the effect of maximum temperatures on tree growth concentrated in the spring. In addition to climate warming in the study area since the 1970s, tree growth (as measured by the basal area increment, BAI) at elevations below 2200 m initially increased and then decreased. Tree growth at higher elevations continues to increase. Since 2000, the average RWI at high elevations exceeded that at low elevations. The average BAI values at high and low elevations have gradually approached each other in recent decades, although lower elevations exhibited higher values in the past. Full article
(This article belongs to the Special Issue Forest Growth Modeling in Different Ecological Conditions)
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Figure 1

Figure 1
<p>Geographic location map of the study area and sampling sites. (<b>a</b>) is China, (<b>b</b>) is the eastern section of the Tianshan, and (<b>c</b>) is Jiangbulake, which is also the sampling area of this study.</p>
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<p>Tree ring width index of <span class="html-italic">P. schrenkiana</span> along the elevation of 1800 m to 2600 m.</p>
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<p>Trends in average annual temperature and precipitation at meteorological stations in the vicinity of the study area since 1960 yr. (<b>a</b>) is the change and trend in precipitation dynamics over the years in the study area, and (<b>b</b>) is the change and trend in temperature dynamics over the years.</p>
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<p>Correlation analysis between tree ring width index at different elevations and precipitation in different seasons and months (* is 0.01 ≤ <span class="html-italic">p</span> ≤ 0.05; ** is 0.001 ≤ <span class="html-italic">p</span> ≤ 0.01; *** is <span class="html-italic">p</span> ≤ 0.001).</p>
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<p>Correlation analysis of tree ring width index at different elevations with temperature in different seasons and months. (<b>a</b>–<b>c</b>) are the correlation analyses of tree ring width index and average, maximum, and minimum temperature, respectively. The number of * represents the significance level of the correlation (* is 0.01 ≤ <span class="html-italic">p</span> ≤ 0.05; ** is 0.001 ≤ <span class="html-italic">p</span> ≤ 0.01; *** is <span class="html-italic">p</span> ≤ 0.001).</p>
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<p>Correlation analysis between tree ring width index and standardized precipitation evapotranspiration index at different elevations (* is 0.01 ≤ <span class="html-italic">p</span> ≤ 0.05; ** is 0.001 ≤ <span class="html-italic">p</span> ≤ 0.01; *** is <span class="html-italic">p</span> ≤ 0.001).</p>
Full article ">Figure 7
<p>Segmentation and linear fitting of BAI at different elevations from 1969 to 2021. a and b represent the growth trend of trees at different times.</p>
Full article ">Figure 8
<p>Average RWI and BAI changes in high- and low-elevation trees. (<b>a</b>) Average RWI; (<b>b</b>) average BAI; (<b>c</b>) low-elevation RWI minus high-elevation RWI; (<b>d</b>) low-elevation BAI minus high-elevation BAI.</p>
Full article ">
24 pages, 7050 KiB  
Article
Quantile Connectedness of Uncertainty Indices, Carbon Emissions, Energy, and Green Assets: Insights from Extreme Market Conditions
by Tiantian Liu, Yulian Zhang, Wenting Zhang and Shigeyuki Hamori
Energies 2024, 17(22), 5806; https://doi.org/10.3390/en17225806 - 20 Nov 2024
Viewed by 234
Abstract
In this study, we investigate the volatility spillover effects across uncertainty indices (Infectious Disease Equity Market Volatility Tracker (IDEMV) and Geopolitical Risk Index (GPR)), carbon emissions, crude oil, natural gas, and green assets (green bonds and green stock) under extreme market conditions based [...] Read more.
In this study, we investigate the volatility spillover effects across uncertainty indices (Infectious Disease Equity Market Volatility Tracker (IDEMV) and Geopolitical Risk Index (GPR)), carbon emissions, crude oil, natural gas, and green assets (green bonds and green stock) under extreme market conditions based on the quantile connectedness approach. The empirical findings reveal that the total and directional connectedness across green assets and other variables in extreme market conditions is much higher than that in the median, and there is obvious asymmetry in the connectedness measured at the extreme lower and upper quantiles. Our findings suggest that the uncertainty caused by COVID-19 has a more significant impact on green assets than the uncertainty related to the Russia–Ukraine war under normal and extreme market conditions. Furthermore, we discover that the uncertainty indices are more important in predicting green asset volatility under extreme market conditions than they are in the normal market. Finally, we observe that the dynamic total spillover effects in the extreme quantiles are significantly higher than those in the median. Full article
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Figure 1

Figure 1
<p>Time variations of variables.</p>
Full article ">Figure 2
<p>Volatility connectedness network plot at the median, lower, and upper quantiles. Note: The color of the nodes indicates whether they are net transmitters (red) or net receivers (green) of the system. The size of a node reflects the magnitude of its net connectedness. The edge arrow direction and edge thickness represent the direction and strength of the net pairwise connectedness between a pair of markets, respectively. GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 3
<p>Total spillover effects at the median, lower, and upper quantiles. Note: The dynamic spillover effects were captured using a 200-day rolling window based on a QVAR model with a lag of 5 (BIC) and a 10-step-ahead forecast horizon.</p>
Full article ">Figure 3 Cont.
<p>Total spillover effects at the median, lower, and upper quantiles. Note: The dynamic spillover effects were captured using a 200-day rolling window based on a QVAR model with a lag of 5 (BIC) and a 10-step-ahead forecast horizon.</p>
Full article ">Figure 4
<p>Net directional spillover effects at the median. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 5
<p>Net directional spillover effects at the lower quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 6
<p>Net directional spillover effects at the upper quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 6 Cont.
<p>Net directional spillover effects at the upper quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 7
<p>Net pairwise directional spillover effects between green assets and other assets at the median. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 8
<p>Net pairwise directional spillover effects between green assets and other assets at the lower quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 8 Cont.
<p>Net pairwise directional spillover effects between green assets and other assets at the lower quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 9
<p>Net pairwise directional spillover effects between green assets and other assets at the upper quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">Figure 9 Cont.
<p>Net pairwise directional spillover effects between green assets and other assets at the upper quantile. Note: GB, Solactive Green Bond Index; GS, Standard &amp; Poor Global Clean Energy Index; Oil, Brent Crude Oil; Gas, Henry Hub Natural Gas; Carbon, Carbon Emissions Futures; IDEMV, Infectious Disease Equity Market Volatility Tracker; GPR, Geopolitical Risk Index.</p>
Full article ">
28 pages, 12380 KiB  
Article
Characterization of CYGNSS Ocean Surface Wind Speed Products
by Christopher Ruf, Mohammad Al-Khaldi, Shakeel Asharaf, Rajeswari Balasubramaniam, Darren McKague, Daniel Pascual, Anthony Russel, Dorina Twigg and April Warnock
Remote Sens. 2024, 16(22), 4341; https://doi.org/10.3390/rs16224341 - 20 Nov 2024
Viewed by 149
Abstract
Since its launch in 2016, a number of wind speed retrieval algorithms have been developed for the NASA CYGNSS satellite observations. We assess their accuracy and precision and characterize the dependence of their performance on environmental factors. The dependence of retrieval uncertainty on [...] Read more.
Since its launch in 2016, a number of wind speed retrieval algorithms have been developed for the NASA CYGNSS satellite observations. We assess their accuracy and precision and characterize the dependence of their performance on environmental factors. The dependence of retrieval uncertainty on the wind speed itself is considered. The triple colocation method of validation is used to correct for the quality of the reference wind speed products with which CYGNSS is compared. The dependence of retrieval performance on sea state is also considered, with particular attention being paid to the long wave portion of the surface roughness spectrum that is less closely coupled to the instantaneous local wind speed than the capillary wave portion of the spectrum. The dependence is found to be significant, and the efficacy of the approaches taken to account for it is examined. The dependence of retrieval accuracy on wind speed persistence (the change in wind speed prior to a measurement) is also characterized and is found to be significant when winds have increased markedly in the ~2 h preceding an observation. Full article
(This article belongs to the Section Ocean Remote Sensing)
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Figure 1

Figure 1
<p>(<b>a</b>) Level 2 wind speed processing flow: FDS (maroon) and YSLF (green). (<b>b</b>) Level 3 FDS and MRG processing flow.</p>
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<p>Locations of the colocated tropical buoys used for intercomparison.</p>
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<p>Histograms of (<b>a</b>) spatial and (<b>b</b>) temporal separation between matchups of CYGNSS and ERA5 wind speed samples. The mean separations are 17.2 km and 30.3 min.</p>
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<p>Distribution of the number (#) of data samples in each wind speed bin for the four data products in the storm matchup dataset.</p>
Full article ">Figure 5
<p>Density scatterplots comparing (<b>a</b>) CYGNSS FDS and (<b>b</b>) NOAA wind speed products with near-coincident buoy reference winds. ‘Slope’ represents the best-fit linear regression value, and ‘Corr.’ denotes its correlation coefficient. Correlation coefficients with a significance level (<span class="html-italic">p</span>-value &lt; 0.05) are marked with an asterisk (*).</p>
Full article ">Figure 6
<p>(<b>a</b>,<b>c</b>) RMSD between CYGNSS and buoys (indicated by bars) at different rain rate (R; in mm/h) conditions, and (<b>b</b>,<b>d</b>) scatterplot of difference between CYGNSS and buoy winds as functions of buoy precipitation rate, with best-fit linear regression lines overlaid in. Panels (<b>a</b>,<b>b</b>) correspond to low wind conditions (≤6 m/s), while panels (<b>c</b>,<b>d</b>) depict conditions with buoy winds &gt;6 m/s. The error bars correspond to the 95% confidence limit estimated via the bootstrap method. Matchup samples are illustrated by the number on each bar. Correlation coefficients with a significance level (<span class="html-italic">p</span>-value &lt; 0.05) are marked with an asterisk (*).</p>
Full article ">Figure 7
<p>(<b>a</b>) Log-density scatterplot between FDS wind speed and ERA5 matchup reference winds. (<b>b</b>) RMSD and bias between the two wind speeds as a function of the reference wind. (<b>c</b>) Log density scatterplot between NOAA wind speed and ERA5 matchup reference winds. (<b>d</b>) RMSD and bias between the two wind speeds as a function of the reference wind. Note the change in scale for (<b>c</b>) needed to include NOAA’s outliers.</p>
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<p>Time series of FDS RMS and mean difference (RMSD and Bias) with respect to ERA5.</p>
Full article ">Figure 9
<p>PDFs of v3.2 FDS winds by (<b>a</b>) CYGNSS satellite Flight Model (FM), (<b>b</b>) port/starboard antenna, and (<b>c</b>) GPS block type, with ERA5 winds as the reference.</p>
Full article ">Figure 10
<p>Geographical distribution of FDS bias with respect to ERA5 (FDS—ERA5). Data are averaged over all of December 2023.</p>
Full article ">Figure 11
<p>Log density scatterplots for each pair of storm-specific matchup datasets. (<b>a</b>) SFMR vs. HWRF, (<b>b</b>) HWRF vs. MRG (<b>c</b>) SFMR vs. MRG, (<b>d</b>) MRG vs. NOAA, (<b>e</b>) HWRF vs. NOAA, and (<b>f</b>) SFMR vs. NOAA.</p>
Full article ">Figure 12
<p>Log density scatterplots after a data-quality filter has been applied which requires coincident HWRF and SFMR values to differ by no more than 10 m/s. (<b>a</b>) SFMR vs. HWRF, (<b>b</b>) HWRF vs. MRG (<b>c</b>) SFMR vs. MRG, (<b>d</b>) MRG vs. NOAA, (<b>e</b>) HWRF vs. NOAA, and (<b>f</b>) SFMR vs. NOAA. These are the samples used for triple colocation analysis.</p>
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<p>RMSD and RMSE performance for MRG and NOAA products.</p>
Full article ">Figure 14
<p>Scatterplot of matchups between the 34-knot wind radius derived from CYGNSS MRG wind fields and those measured by ASCAT. Different storm quadrants are denoted by symbol shapes. Different ranges of storm intensity are denoted by symbol color.</p>
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<p>Mean revisit time of FDS wind speed product as a function of latitude.</p>
Full article ">Figure 16
<p>Dependence of CYGNSS wind speed error on SWH: (<b>a</b>) FDS without SWH correction, (<b>b</b>) FDS with SWH correction, and (<b>c</b>) NOAA with SWH correction.</p>
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<p>Dependence of (<b>a</b>) ASCAT and (<b>b</b>) GMI wind speed bias on SWH.</p>
Full article ">Figure 18
<p>Bias in the CYGNSS FDS wind speed product as a function wind speed persistence for wind speed ranges of (<b>a</b>) 0–5 m/s, (<b>b</b>) 5–10 m/s, (<b>c</b>) 10–15 m/s, (<b>d</b>) 15–20 m/s, (<b>e</b>) &gt;20 m/s. Persistence &lt; 0 implies prior winds were higher. Bias is the average (FDS–ERA5) difference for all of CY2022. Error bars are the standard deviation of all samples averaged in each wind speed and persistence bin.</p>
Full article ">Figure 19
<p>Bias in the CYGNSS NOAA wind speed product as a function wind speed persistence prior to the measurement for wind speed ranges of (<b>a</b>) 0–5 m/s, (<b>b</b>) 5–10 m/s, (<b>c</b>) 10–15 m/s, (<b>d</b>) 15–20 m/s, (<b>e</b>) &gt;20 m/s. Persistence &lt; 0 implies prior winds were higher. Bias is the average (NOAA–ERA5) difference for all of CY2022. Error bars are the standard deviation of all samples averaged in each wind speed and persistence bin.</p>
Full article ">
20 pages, 1947 KiB  
Article
Pressure Control of Multi-Mode Variable Structure Electro–Hydraulic Load Simulation System
by He Hao, Hao Yan, Qi Zhang and Haoyu Li
Sensors 2024, 24(22), 7400; https://doi.org/10.3390/s24227400 - 20 Nov 2024
Viewed by 267
Abstract
During the loading process, significant external position disturbances occur in the electro–hydraulic load simulation system. To address these position disturbances and effectively mitigate the impact of uncertainty on system performance, this paper first treats model parameter uncertainty and external disturbances as lumped disturbances. [...] Read more.
During the loading process, significant external position disturbances occur in the electro–hydraulic load simulation system. To address these position disturbances and effectively mitigate the impact of uncertainty on system performance, this paper first treats model parameter uncertainty and external disturbances as lumped disturbances. The various states of the servo valve and the pressures within the hydraulic cylinder chambers are then examined. Building on this foundation, the paper proposes a nonlinear multi-mode variable structure independent load port electro–hydraulic load simulation system that is tailored for specific loading conditions. Secondly, in light of the significant motion disturbances present, this paper proposes an integral sliding mode active disturbance rejection composite control strategy that is based on fixed-time convergence. Based on the structure of the active disturbance rejection control framework, the fixed-time integral sliding mode and active disturbance rejection control algorithms are integrated. An extended state observer is designed to accurately estimate the lumped disturbance, effectively compensating for it to achieve precise loading of the independent load port electro–hydraulic load simulation system. The stability of the designed controller is also demonstrated. The results of the simulation research indicate that when the command input is a step signal, the pressure control accuracy under the composite control strategy is 99.94%, 99.86%, and 99.76% for disturbance frequencies of 1 Hz, 3 Hz, and 5 Hz, respectively. Conversely, when the command input is a sinusoidal signal, the pressure control accuracy remains high, measuring 99.94%, 99.8%, and 99.6% under the same disturbance frequencies. Furthermore, the simulation demonstrates that the influence of sensor random noise on the system remains within acceptable limits, highlighting the effective filtering capabilities of the extended state observer. This research establishes a solid foundation for the collaborative control of load ports and the engineering application of the independent load port electro–hydraulic load simulation system. Full article
(This article belongs to the Section Electronic Sensors)
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<p>Schematic view of independent load port electro–hydraulic load simulation system model (1—tank, 2—hydraulic pump, 3—relief valve, 4—electro–hydraulic servo valve, 5—independent load port electro–hydraulic load simulation system controller, 6—pressure sensor, 7—hydraulic cylinder, 8—displacement sensor, 9—linear actuator, 10—linear actuator controller).</p>
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<p>Block diagram of fixed-time integral sliding mode active disturbance rejection composite control.</p>
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<p>Closed-loop pressure with a disturbance frequency of 1 Hz.</p>
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<p>Closed-loop pressure error with a disturbance frequency of 1 Hz.</p>
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<p>Controller output with a disturbance frequency of 1 Hz.</p>
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<p>Closed-loop pressure with a disturbance frequency of 3 Hz.</p>
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<p>Closed-loop pressure error with a disturbance frequency of 3 Hz.</p>
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<p>Controller output with a disturbance frequency of 3 Hz.</p>
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<p>Closed-loop pressure with a disturbance frequency of 5 Hz.</p>
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<p>Closed-loop pressure error with a disturbance frequency of 5 Hz.</p>
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<p>Controller output with a disturbance frequency of 5Hz.</p>
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<p>Closed-loop pressure with a disturbance frequency of 1 Hz.</p>
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<p>Closed-loop pressure error with a disturbance frequency of 1 Hz.</p>
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<p>Controller output with a disturbance frequency of 1 Hz.</p>
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<p>Closed-loop pressure with a disturbance frequency of 3 Hz.</p>
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<p>Closed-loop pressure error with disturbance frequency of 3 Hz.</p>
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<p>Controller output with a disturbance frequency of 3 Hz.</p>
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<p>Closed-loop pressure with a disturbance frequency of 5 Hz.</p>
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<p>Closed-loop pressure error with a disturbance frequency of 5 Hz.</p>
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<p>Controller output with a disturbance frequency of 5 Hz.</p>
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<p>Pressure curve under random noise of 50 mV.</p>
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<p>Pressure curve under random noise of 100 mV.</p>
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16 pages, 5881 KiB  
Article
Projection of Changes in Stream Water Use Due to Climate Change
by Young-Ho Seo, Junehyeong Park, Byung-Sik Kim and Jang Hyun Sung
Sustainability 2024, 16(22), 10120; https://doi.org/10.3390/su162210120 - 20 Nov 2024
Viewed by 258
Abstract
This study investigates the impact of rising temperatures on residential water use (RWU) in Seoul from 2015 to 2021, addressing the challenges of urban water sustainability under climate change. Using advanced models—convolutional neural networks (CNNs), long short-term memory (LSTM) Networks, eXtreme Gradient Boosting [...] Read more.
This study investigates the impact of rising temperatures on residential water use (RWU) in Seoul from 2015 to 2021, addressing the challenges of urban water sustainability under climate change. Using advanced models—convolutional neural networks (CNNs), long short-term memory (LSTM) Networks, eXtreme Gradient Boosting (XGBoost), and Bayesian Neural Networks (BNNs)—we examined RWU prediction accuracy and incorporated a method to quantify prediction uncertainties. As a result, the BNN model emerged as a robust alternative, demonstrating competitive predictive accuracy and the capability to account for uncertainties in predictions. Recent studies highlight a strong correlation between rising temperatures and increased RWU, especially during summer, with tropical nights (with temperatures above 25 °C) becoming more common; Seoul experienced a record 26 consecutive tropical nights in July 2024, underscoring a trend toward higher RWU. To capture these dynamics, we employed Shared Socioeconomic Pathway (SSP) scenarios and downscaled the KACE-1-0-G Global Climate Model (GCM) for Seoul, projecting a progressive increase in RWU: 0.49% in the F1 period (2011–2040), 1.53% in F2 (2041–2070), and 2.95% in F3 (2071–2100), with significant rises in maximum RWU across these intervals. Our findings highlight an urgent need for proactive measures to secure water resources in response to the anticipated increase in urban water demand driven by climate change. Full article
(This article belongs to the Section Sustainable Water Management)
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<p>Pungnap water intake Facility and Paldang Dam.</p>
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<p>RWU and temperatures in Seoul.</p>
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<p>The structures of the deep learning models.</p>
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<p>Training and validation histories of the artificial neural networks: (<b>a</b>) CNN, (<b>b</b>) LSTM, and (<b>c</b>) BNN.</p>
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<p>RWU Predictions with the regression models: (<b>a</b>) CNN, (<b>b</b>) LSTM, (<b>c</b>) XGBoost, and (<b>d</b>) BNN.</p>
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<p>The regression models’ predictions with observations across temperature Ranges.</p>
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<p>BNN ensemble of RWU: (<b>a</b>) monthly and (<b>b</b>) seasonal predictions.</p>
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<p>Projection of RWU changes during the future period.</p>
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10 pages, 3558 KiB  
Article
The New Deep-Underground Direct Measurement of 22Ne(α, γ)26Mg with EASγ: A Feasibility Study
by Daniela Mercogliano, Andreas Best and David Rapagnani
Galaxies 2024, 12(6), 79; https://doi.org/10.3390/galaxies12060079 - 20 Nov 2024
Viewed by 196
Abstract
22Ne(α, γ)26Mg is pivotal in the understanding of several open astrophysical questions, as the nucleosynthesis beyond Fe through the s-process, but its stellar reaction rate is still subject to large uncertainties. These mainly arise from its extremely low rate in [...] Read more.
22Ne(α, γ)26Mg is pivotal in the understanding of several open astrophysical questions, as the nucleosynthesis beyond Fe through the s-process, but its stellar reaction rate is still subject to large uncertainties. These mainly arise from its extremely low rate in the Gamow energy region, whose measurement is hampered by the unavoidable presence of the cosmic ray background noise. A possibility to overcome this issue is to perform the measurement in a quasi background-free environment, such as that offered by the underground Bellotti Ion Beam Facility at LNGS. This is the key idea of EASγ experiment. In this study, the signal from the de-excitation of the compound nucleus 26Mg has been simulated and its detection has been investigated both on surface and deep-underground laboratories. The simulation results show the enhancement in sensitivity achieved by performing the measurement deep underground and with an additional shielding, yielding to unprecedented sensitivity. Full article
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<p>The final configuration on the NaI(Tl) simulated using GEANT4. Six parallelepiped-shaped NaI(Tl) surround the target chamber at a fixed distance of 15 cm. In cyan, the enriched <sup>22</sup>Ne gas target.</p>
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<p>NaI background-acquisition spectra in three different experimental scenarios: The black line is the background acquired on surface laboratory leaving the detector unshielded. The peaks corresponding to the <sup>40</sup>K and <sup>208</sup>Tl are clearly visible. The blue spectrum is the background registered by the same detector but located deep-underground at the Bellotti IBF. The red line is the spectrum acquired deep-underground and with an additional lead shielding.</p>
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<p>(<b>a</b>) Comparison of the simulated signal (in red) with the experimental background acquired on surface and with the detector unshielded (light blue). (<b>b</b>) A black line for the sum of signal and background is added. The location of the two primary transitions <math display="inline"><semantics> <mrow> <mn>11,319.5</mn> <mo> </mo> <mi>keV</mi> <mspace width="0.166667em"/> <mo>→</mo> <mspace width="0.166667em"/> <mn>7061</mn> <mspace width="0.166667em"/> <mi>keV</mi> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <mn>11,319.5</mn> <mo> </mo> <mi>keV</mi> <mspace width="0.166667em"/> <mo>→</mo> <mspace width="0.166667em"/> <mn>1808.74</mn> <mspace width="0.166667em"/> <mi>keV</mi> </mrow> </semantics></math> is marked by the two green arrows.</p>
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<p>(<b>a</b>) Comparison of the simulated signal (in red) with the experimental background acquired deep-underground and without shielding (light blue). In black, the signal + background spectrum. (<b>b</b>) In the zoomed spectrum, the two bumps corresponding to the two primary transitions <math display="inline"><semantics> <mrow> <mn>11,319.5</mn> <mo> </mo> <mi>keV</mi> <mspace width="0.166667em"/> <mo>→</mo> <mspace width="0.166667em"/> <mn>7061</mn> <mspace width="0.166667em"/> <mi>keV</mi> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <mn>11,319.5</mn> <mo> </mo> <mi>keV</mi> <mspace width="0.166667em"/> <mo>→</mo> <mspace width="0.166667em"/> <mn>1808.74</mn> <mspace width="0.166667em"/> <mi>keV</mi> </mrow> </semantics></math> are now visible.</p>
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<p>(<b>a</b>) Simulated signal (in red) compared with the background acquired underground and with the array shielded (light blue). In black, the signal+background spectrum. (<b>b</b>) A secondary transition is now visible (marked with the yellow arrow), partially overlapped with the peak corresponding to the de-excitation from the first excited state to the ground state <math display="inline"><semantics> <mrow> <mn>1808.74</mn> <mspace width="0.166667em"/> <mi>keV</mi> <mspace width="0.166667em"/> <mo>→</mo> <mn>0</mn> </mrow> </semantics></math>.</p>
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<p>Simulated signal (in red) compared with the background acquired underground and with the array shielded (light blue). The shape of the spectrum for 10,949 keV for <math display="inline"><semantics> <msup> <mn>10</mn> <mn>6</mn> </msup> </semantics></math> events of events is shown as reference by using the gray dotted line. The peaks corresponding to the primary transitions and the <math display="inline"><semantics> <mrow> <mn>1808.74</mn> <mspace width="0.166667em"/> <mi>keV</mi> <mo>→</mo> <mspace width="0.166667em"/> <mn>0</mn> </mrow> </semantics></math> are highlighted.</p>
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15 pages, 5207 KiB  
Article
Threshold Ranges of Multiphase Components from Natural Ice CT Images Based on Watershed Algorithm
by Shengbo Hu, Qingkai Wang, Chunjiang Li and Zhijun Li
Water 2024, 16(22), 3330; https://doi.org/10.3390/w16223330 - 19 Nov 2024
Viewed by 308
Abstract
The multiphase components of natural ice contain gas, ice, unfrozen water, sediment and brine. X-ray computed tomography (CT) analysis of ice multiphase components has the advantage of high precision, non-destructiveness and visualization; however, it is limited by the segmentation thresholds. Due to the [...] Read more.
The multiphase components of natural ice contain gas, ice, unfrozen water, sediment and brine. X-ray computed tomography (CT) analysis of ice multiphase components has the advantage of high precision, non-destructiveness and visualization; however, it is limited by the segmentation thresholds. Due to the proximity of the CT value ranges of gas, ice, unfrozen water, sediment and brine within the samples, there is uncertainty in the artificial determination of the CT image segmentation thresholds, as well as unsuitability of the global threshold segmentation methods. In order to improve the accuracy of multi-threshold segmentation in CT images, a CT system was used to scan the Yellow River ice, the Wuliangsuhai lake ice and the Arctic sea ice. The threshold ranges of multiphase components within the ice were determined by watershed algorithm to construct a high-precision three-dimensional ice model. The results indicated that CT combined with watershed algorithm was an efficient and non-destructive method for obtaining microscopic information within ice, which accurately segmented the ice into multiphase components such as gas, ice, unfrozen water, sediment, and brine. The gas CT values of the Yellow River ice, the Wuliangsuhai lake ice and the Arctic sea ice ranged from −1024 Hu~−107 Hu, −1024 Hu~−103 Hu, and −1024 Hu~−160 Hu, respectively. The ice CT values of the Yellow River ice, the Wuliangsuhai lake ice and the Arctic sea ice ranged from −103 Hu~−50 Hu, −100 Hu~−38 Hu, −153 Hu~−51 Hu. The unfrozen water CT values of the Yellow River ice and the Wuliangsuhai lake ice ranged from −8 Hu~18 Hu, −8 Hu~13 Hu. The sediment CT values of the Yellow River ice and the Wuliangsuhai lake ice ranged from 20 Hu~3071 Hu, 20 Hu~3071 Hu, and the brine CT values of the Arctic sea ice ranged from −6 Hu~3071 Hu. The errors between the three-dimensional ice model divided by threshold ranges and measured sediment content were less than 0.003 g/cm3, which verified the high accuracy of the established microscopic model. It provided a scientific basis for ice engineering, ice remote sensing, and ice disaster prevention. Full article
(This article belongs to the Special Issue Ice and Snow Properties and Their Applications)
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<p>Flow chart of the experimental processing.</p>
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<p>CT original image and research area frame.</p>
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<p>Histogram of ice sample CT values. There are no peaks and valleys in the CT value histograms, which proves that the CT values range of gas, unfrozen water, ice, and sediment within the samples are similar without significant intervals.</p>
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<p>Schematic diagram of watershed algorithm model.</p>
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<p>Schematic of sample collection and two-dimensional image threshold segmentation. (<b>a</b>) The Yellow River ice sample. Original two-dimensional CT images of (<b>b</b>) top layer, (<b>c</b>) 25 cm from the bottom layer, (<b>d</b>) bottom layer. Histograms of CT values for (<b>e</b>) top layer, (<b>f</b>) 25 cm from the bottom layer, (<b>g</b>) bottom layer. Two-dimensional image multi-threshold segmentation results of (<b>h</b>) top layer, (<b>i</b>) 25 cm from the bottom layer, (<b>j</b>) bottom layer.</p>
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<p>Three-dimensional reconstructed images of the Yellow River ice samples. Global three-dimensional image of (<b>a</b>) the Yellow River No. 3 ice sample, and (<b>c</b>) the Yellow River No. 4 ice sample. Local three-dimensional images of (<b>b</b>) the Yellow River No. 3 ice sample, and (<b>d</b>) the Yellow River No. 4 ice sample.</p>
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<p>Study area and local three-dimensional reconstructed images of the Wuliangsuhai lake ice. (<b>a</b>) the Wuliangsuhai No. 1 and No. 2 ice samples collection areas. Global three-dimensional images of (<b>b</b>) the Wuliangsuhai No. 1 ice sample, and (<b>d</b>) the Wuliangsuhai No. 2 ice sample. Local three-dimensional images of (<b>c</b>) the Wuliangsuhai No. 1 ice sample, and (<b>e</b>) the Wuliangsuhai No. 2 ice sample.</p>
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<p>Global three-dimensional image of (<b>a</b>) the Arctic No. 1 ice sample. Local three-dimensional image of (<b>b</b>) the Arctic No. 1 ice sample.</p>
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<p>Distribution of sediment content in the Yellow River ice along the depth direction.</p>
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15 pages, 1102 KiB  
Article
Optimal Paradigms for Quantitative Modeling in Systems Biology Demonstrated for Spinal Motor Neuron Synthesis
by Gülbahar Akgün and Rza Bashirov
Appl. Sci. 2024, 14(22), 10696; https://doi.org/10.3390/app142210696 - 19 Nov 2024
Viewed by 303
Abstract
Since the 1990s, Petri nets have been used in systems biology for quantitative modeling. Despite the increasing number of models developed during this period, doubts remain about their biological relevance. Although biological systems predominantly exhibit intracellular or cellular structures, the models rely largely [...] Read more.
Since the 1990s, Petri nets have been used in systems biology for quantitative modeling. Despite the increasing number of models developed during this period, doubts remain about their biological relevance. Although biological systems predominantly exhibit intracellular or cellular structures, the models rely largely on deterministic predictions, failing to capture the inherent randomness and uncertainties of such systems. The question arises whether these models accurately describe the dynamic behavior of biological systems. This paper introduces a methodology for selecting the appropriate modeling paradigms in systems biology. Initially, we construct a Petri net model and perform deterministic, stochastic, and fuzzy stochastic simulations. Then we perform various statistical tests to measure the discrepancies between the simulation results. Based on scale-density analysis, we determine the modeling approach that best approximates the biological system. Finally, we compare the results of the statistical tests and the scale-density analysis to identify the optimal modeling approach. We applied the proposed methodology to the synthesis of spinal motor neuron protein from the spinal motor neuron-2 gene. Analysis revealed significant discrepancies between the simulation results of different modeling paradigms. Due to the sparse nature of the underlying drug-disease network, we conclude that the fuzzy stochastic paradigm provides the most biologically relevant results. We predict drug combinations that could lead to an up to 149-fold increase in spinal motor neuron protein levels, indicating a promising treatment for the disease. This methodology has the potential for application to other gene-drug-disease networks and broader biological systems. Full article
(This article belongs to the Special Issue Bioinformatics & Computational Biology)
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<p>Illustration of how spatial scale and density analysis of biological systems influence the choice of modeling methods.</p>
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<p>An illustration of how the similarities and differences between results from deterministic, purely stochastic, and fuzzy stochastic simulations affect the selection of a modeling paradigm.</p>
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<p>(<b>a</b>) The definition of a triangular fuzzy number, and (<b>b</b>) its adaptation to the rate of transcription.</p>
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<p>Petri net model of drug-disease network of SMN synthesis from <span class="html-italic">SMN2</span>.</p>
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<p>Impact of effective combinations of drugs on the SMN protein folding (expressed in folds).</p>
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<p>Impact of effective combinations of two drugs on the SMN protein folding (expressed in folds).</p>
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<p>Impact of effective combinations of three drugs on the SMN protein folding (expressed in folds).</p>
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<p>Impact of effective combinations of four drugs on the SMN protein folding (expressed in folds).</p>
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<p>Impact of effective combinations of five drugs on the SMN protein folding (expressed in folds).</p>
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<p>Impact of effective combinations of six drugs on the SMN protein folding (expressed in folds).</p>
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<p>Test statistics collected from Friedman and Dun–Bonferroni tests for the best effective combinations of drugs.</p>
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26 pages, 3838 KiB  
Article
High-Order Disturbance Observer-Based Fuzzy Fixed-Time Safe Tracking Control for Uncertain Unmanned Helicopter with Partial State Constraints and Multisource Disturbances
by Ruonan Ren, Zhikai Wang, Haoxiang Ma, Baofeng Ji and Fazhan Tao
Drones 2024, 8(11), 679; https://doi.org/10.3390/drones8110679 - 18 Nov 2024
Viewed by 236
Abstract
In the real-world operation of unmanned helicopters, various state constraints, system uncertainties and multisource disturbances pose considerable risks to their safe fight. This paper focuses on anti-disturbance adaptive safety fixed-time control design for the uncertain unmanned helicopter subject to partial state constraints and [...] Read more.
In the real-world operation of unmanned helicopters, various state constraints, system uncertainties and multisource disturbances pose considerable risks to their safe fight. This paper focuses on anti-disturbance adaptive safety fixed-time control design for the uncertain unmanned helicopter subject to partial state constraints and multiple disturbances. Firstly, a developed safety protection algorithm is integrated with the fixed-time stability theory, which assures the tracking performance and guarantees that the partial states are always constrained within the time-varying safe range. Then, the compensation mechanism is developed to weaken the adverse impact induced by the filter errors. Simultaneously, the influence of the multisource disturbances on the system stability are weakened through the Ito^ differential equation and high-order disturbance observer. Further, the fuzzy logic system is constructed to approximate the system uncertainties caused by the sensor measurement errors and complex aerodynamic characteristics. Stability analysis proves that the controlled unmanned helicopter is semi-globally fixed-time stable in probability, and the state errors converge to a desired region of the origin. Finally, simulations are provided to illustrate the performance of the proposed scheme. Full article
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<p>Schematic diagram of the UAH system.</p>
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<p>Control diagram of this paper.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mrow> <mi>X</mi> </mrow> </semantics></math>-axis.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mrow> <mi>Y</mi> </mrow> </semantics></math>-axis.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mrow> <mi>Z</mi> </mrow> </semantics></math>-axis.</p>
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<p>Tracking performance of velocity.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mi>ϕ</mi> </semantics></math>.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mi>θ</mi> </semantics></math>.</p>
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<p>Tracking performance of <math display="inline"><semantics> <mi>ψ</mi> </semantics></math>.</p>
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<p>Tracking performance of angular velocity.</p>
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<p>Control inputs of the designed scheme.</p>
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<p>Tracking performance of position subsystem.</p>
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<p>Tracking performance of attitude subsystem.</p>
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<p>Tracking performance of <math display="inline"><semantics> <msub> <mi>d</mi> <mn>1</mn> </msub> </semantics></math>.</p>
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<p>Tracking performance of <math display="inline"><semantics> <msub> <mi>d</mi> <mn>2</mn> </msub> </semantics></math>.</p>
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<p>Three-dimensional trajectory diagram.</p>
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<p>Tracking performance of <span class="html-italic">X</span> under different control schemes.</p>
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35 pages, 14662 KiB  
Article
A Statistical Approach for Characterizing the Behaviour of Roughness Parameters Measured by a Multi-Physics Instrument on Ground Surface Topographies: Four Novel Indicators
by Clément Moreau, Julie Lemesle, David Páez Margarit, François Blateyron and Maxence Bigerelle
Metrology 2024, 4(4), 640-672; https://doi.org/10.3390/metrology4040039 - 18 Nov 2024
Viewed by 216
Abstract
With a view to improve measurements, this paper presents a statistical approach for characterizing the behaviour of roughness parameters based on measurements performed on ground surface topographies (grit #080/#120). A S neoxTM (Sensofar®, Terrassa, Spain), equipped with three optical instrument [...] Read more.
With a view to improve measurements, this paper presents a statistical approach for characterizing the behaviour of roughness parameters based on measurements performed on ground surface topographies (grit #080/#120). A S neoxTM (Sensofar®, Terrassa, Spain), equipped with three optical instrument modes (Focus Variation (FV), Coherence Scanning Interferometry (CSI), and Confocal Microscopy (CM)), is used according to a specific measurement plan, called Morphomeca Monitoring, including topography representativeness and several time-based measurements. Previously applied to the Sa parameter, the statistical approach based here solely on the Quality Index (QI) has now been extended to a multi-parameter approach. Firstly, the study focuses on detecting and explaining parameter disturbances in raw data by identifying and quantifying outliers of the parameter’s values, as a new first indicator. This allows us to draw parallels between these outliers and the surface topography, providing reflection tracks. Secondly, the statistical approach is applied to highlight disturbed parameters concerning the instrument mode used and the concerned grit level with two other indicators computed from QI, named homogeneity and number of modes. The applied method shows that a cleaning of the data containing the parameters values is necessary to remove outlier values, and a set of roughness parameters could be determined according to the assessment of the indicators. The final aim is to provide a set of parameters which best describe the measurement conditions based on monitoring data, statistical indexes, and surface topographies. It is shown that the parameters Sal, Sz and Sci are the most reliable roughness parameters, unlike Sdq and S5p, which appear as the most unstable parameters. More globally, the volume roughness parameters appear as the most stable, differing from the form parameters. This investigated point of view offers thus a complementary framework for improving measurement processes. In addition, this method aims to provide a global and more generalizable alternative than traditional methods of uncertainty calculation, based on a thorough analysis of multi-parameter and statistical indexes. Full article
(This article belongs to the Special Issue Advances in Optical 3D Metrology)
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<p>Morphomeca Monitoring showing the measurement strategy according to the paper grit levels, the measurement modes, the iterations, and the repetitions [<a href="#B54-metrology-04-00039" class="html-bibr">54</a>].</p>
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<p>Scheme of measurement process steps [<a href="#B54-metrology-04-00039" class="html-bibr">54</a>].</p>
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<p>Example of a ground surface with and without a second-order form removal, and calculation of some roughness parameters.</p>
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<p>Flow chart representing the adopted methodology to find the reliable parameter.</p>
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<p>Quality Index computed for the Sa roughness parameter (<b>a</b>), raw Sa values versus timestamp (<b>b</b>) and calculation of the new indicators <span class="html-italic">(%-Out</span>, <span class="html-italic">NBmode</span>, <span class="html-italic">Homo_Q</span>, <span class="html-italic">Mean_Q</span>) (<b>c</b>) for each instrument mode and grit.</p>
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<p>Raw values of the Sp roughness parameter versus acquisition time, as presented in Morphomeca Monitoring: with outliers for grit #080 (<b>a</b>) and grit #120 (<b>c</b>), without outliers for grit #80 (<b>b</b>) and grit #120 (<b>d</b>).</p>
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<p><span class="html-italic">QI</span> PDF (<b>i</b>) and timestamp graph (<b>ii</b>) with outliers for different cases of indicator performance: the best <span class="html-italic">Mean_Q</span> and worst <span class="html-italic">Homo_Q</span> (<b>a</b>), the worst <span class="html-italic">Mean_Q</span> (<b>b</b>), the highest <span class="html-italic">NBmode</span> (<b>c</b>), the best <span class="html-italic">Homo_Q</span> (<b>d</b>), the lowest <span class="html-italic">%-Out</span> (<b>e</b>) and the highest <span class="html-italic">%-Out</span> (<b>f</b>).</p>
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<p><span class="html-italic">QI</span> PDF (<b>i</b>) and timestamp graph (<b>ii</b>) without outliers for the same cases of indicator performance presented in <a href="#metrology-04-00039-f007" class="html-fig">Figure 7</a>: initially the best <span class="html-italic">Mean_Q</span> and worst <span class="html-italic">Homo_Q</span> (<b>a</b>), initially the worst <span class="html-italic">Mean_Q</span> (<b>b</b>), initially the highest <span class="html-italic">NBmode</span> (<b>c</b>), initially the best <span class="html-italic">Homo_Q</span> (<b>d</b>), initially the lowest <span class="html-italic">%-Out</span> (<b>e</b>) and initially the highest <span class="html-italic">%-Out</span> (<b>f</b>).</p>
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<p>Example of roughness parameter ranking, depending on the severity rate.</p>
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<p>Occurrence of the parameters having a severity rate below 5% for each grit level and instrument mode presented in <a href="#app5-metrology-04-00039" class="html-app">Appendix E</a>.</p>
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<p>Surface features obtained by grinding process on TA6V.</p>
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<p>Focus variation (FV), grit #080.</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the FV mode and the grit #080: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the FV mode and the grit #120: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the CM mode and the grit #080: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the CM mode and the grit #120: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the CSI mode and the grit #080: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of the roughness parameters for the indicators (<span class="html-italic">NBmode</span>, <span class="html-italic">Mean_Q</span>, <span class="html-italic">Homo_Q</span>), for the CSI mode and the grit #120: with outliers (<b>a</b>) and without outliers (<b>b</b>).</p>
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<p>Ranking of roughness parameters from the severity rate for each measurement/grit couple.</p>
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39 pages, 8691 KiB  
Review
Comprehensive Review of Lithium-Ion Battery State of Charge Estimation by Sliding Mode Observers
by Vahid Behnamgol, Mohammad Asadi, Mohamed A. A. Mohamed, Sumeet S. Aphale and Mona Faraji Niri
Energies 2024, 17(22), 5754; https://doi.org/10.3390/en17225754 - 18 Nov 2024
Viewed by 452
Abstract
The state of charge (SoC) is a critical parameter in lithium-ion batteries and their alternatives. It determines the battery’s remaining energy capacity and influences its performance longevity. Accurate SoC estimation is essential for making informed charging and discharging decisions, mitigating the risks of [...] Read more.
The state of charge (SoC) is a critical parameter in lithium-ion batteries and their alternatives. It determines the battery’s remaining energy capacity and influences its performance longevity. Accurate SoC estimation is essential for making informed charging and discharging decisions, mitigating the risks of overcharging or deep discharge, and ensuring safety. Battery management systems rely on SoC estimation, utilising both hardware and software components to maintain safe and efficient battery operation. Existing SoC estimation methods are broadly classified into direct and indirect approaches. Direct methods (e.g., Coulumb counting) rely on current measurements. In contrast, indirect methods (often based on a filter or observer) utilise a model of a battery to incorporate voltage measurements besides the current. While the latter is more accurate, it faces challenges related to sensor drift, computational complexity, and model inaccuracies. The need for more precise and robust SoC estimation without increasing complexity is critical, particularly for real-time applications. Recently, sliding mode observers (SMOs) have gained prominence in this field for their robustness against model uncertainties and external disturbances, offering fast convergence and superior accuracy. Due to increased interest, this review focuses on various SMO approaches for SoC estimation, including first-order, adaptive, high-order, terminal, fractional-order, and advanced SMOs, along with hybrid methods integrating intelligent techniques. By evaluating these methodologies, their strengths, weaknesses, and modelling frameworks in the literature, this paper highlights the ongoing challenges and future directions in SoC estimation research. Unlike common review papers, this work also compares the performance of various existing methods via a comprehensive simulation study in MATLAB 2024b to quantify the difference and guide the users in selecting a suitable version for the applications. Full article
(This article belongs to the Section D: Energy Storage and Application)
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<p>Classification of SoC estimation methods.</p>
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<p>Classification of battery models for SoC estimation.</p>
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<p>First order resistor-capacitor electrical modelling of a LIB.</p>
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<p>Open circuit voltage vs. SoC of LIB for different temperatures [<a href="#B101-energies-17-05754" class="html-bibr">101</a>].</p>
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<p>First order battery equivalent circuit model with hysteresis.</p>
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<p>Hysteresis loop in battery charging/discharging OCV curves [<a href="#B103-energies-17-05754" class="html-bibr">103</a>].</p>
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<p>Simplified first-order ECM of the LIB.</p>
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<p>Second Order RC ECM.</p>
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<p>Second order battery ECM with the hysteresis.</p>
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<p>Nth-order Randle battery ECM.</p>
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<p>Fractional order RC ECM.</p>
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<p>Classification of SMO-based SoC estimation methods.</p>
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<p>Considered second-order battery ECM for the simulation test.</p>
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<p>Estimation results using the conventional first-order sliding mode observer.</p>
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<p>Estimation results using the approximated first-order sliding mode observer.</p>
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<p>Estimation results using the conventional adaptive sliding mode observer.</p>
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<p>Estimation results using the approximated adaptive sliding mode observer.</p>
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<p>Estimation results using the second-order super-twisting sliding mode observer.</p>
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<p>Estimation results using the conventional terminal sliding mode observer.</p>
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<p>Estimation results using the approximated terminal sliding mode observer.</p>
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<p>Comparison of the V<sub>oc</sub> estimation by the conventional first-order, adaptive, and terminal SMOs and the super-twisting method at the beginning of simulation.</p>
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<p>Comparison of the SoC estimation by the conventional first-order, adaptive, and terminal SMOs and super-twisting method.</p>
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<p>Comparison of the SoC estimation by the approximated first-order, adaptive, and terminal SMOs and super-twisting method.</p>
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27 pages, 9234 KiB  
Article
Big Data in Leadership Studies: Automated Machine Learning Model to Predict Preferred Leader Behavior Across Cultures
by Erik Lankut, Gillian Warner-Søderholm, Ilan Alon and Inga Minelgaité
Businesses 2024, 4(4), 696-722; https://doi.org/10.3390/businesses4040039 - 18 Nov 2024
Viewed by 531
Abstract
With global leadership as the new norm, discussion about followers’ preferred leader behaviors across cultures is growing in significance. This study proposes a comprehensive predictive model to explore significant preferred leadership factors, drawn from the Leader Behavior Description Questionnaire (LBDQXII), across cultures using [...] Read more.
With global leadership as the new norm, discussion about followers’ preferred leader behaviors across cultures is growing in significance. This study proposes a comprehensive predictive model to explore significant preferred leadership factors, drawn from the Leader Behavior Description Questionnaire (LBDQXII), across cultures using automated machine learning (AML). We offer a robust empirical measurement of culturally contingent leader behavior and entrepreneurship behaviors and provide a tool for assessing the cultural predictors of preferred leader behavior to minimize predictive errors, explore patterns in the data and make predictions in an empirically robust way. Hence, our approach fills a gap in the literature relating to applications of AML in leadership studies and contributes a novel empirical method to better predict leadership preferences. Cultural indicators from Global Leadership and Organizational Behavior (GLOBE) predict the likelihood of the preferred leader behaviors of “Role Assumption”, “Production Emphasis” and “Initiation of Structure”. Hofstede’s Long-Term/Short-Term Orientation is the most critical predictor of preferences for “Tolerance of Uncertainty” and “Initiation of Structure”, whereas the value of restraint impacts the likelihood of preferring leaders with skills in “Integration” and “Consideration”. Significant entrepreneurial values indicators have a significant impact on preferences for leaders focused on “Initiation of Structure”, “Production Emphasis” and “Predictive Accuracy”. Findings also support earlier studies that reveal age and gender significantly impact our preferences for specific leader behaviors. We discuss and offer conclusions to support our findings that foster development of global business managers and practitioners. Full article
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<p>Conceptual model.</p>
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<p>Overview of model blueprints.</p>
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<p>DataRobot feature association heatmap (ChatGPT 4o prompt—12 September 2024).</p>
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<p>(<b>a</b>–<b>l</b>) Relationships between selected features and LBDQ dimensions.</p>
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<p>(<b>a</b>–<b>l</b>) Relationships between selected features and LBDQ dimensions.</p>
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<p>(<b>a</b>–<b>l</b>) Relationships between selected features and LBDQ dimensions.</p>
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<p>(<b>a</b>–<b>l</b>) Relationships between selected features and LBDQ dimensions.</p>
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<p>Blueprints.</p>
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<p>Blueprints.</p>
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<p>Blueprints.</p>
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<p>Blueprints.</p>
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<p>Blueprints.</p>
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<p>Feature impacts for target variables.</p>
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<p>Feature impacts for target variables.</p>
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<p>Feature impacts for target variables.</p>
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<p>Feature impacts for target variables.</p>
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<p>Feature impacts for target variables.</p>
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