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15 pages, 1726 KiB  
Article
Forecasting Wind–Photovoltaic Energy Production and Income with Traditional and ML Techniques
by Giovanni Masala and Amelie Schischke
Econometrics 2024, 12(4), 34; https://doi.org/10.3390/econometrics12040034 - 12 Nov 2024
Viewed by 345
Abstract
Hybrid production plants harness diverse climatic sources for electricity generation, playing a crucial role in the transition to renewable energies. This study aims to forecast the profitability of a combined wind–photovoltaic energy system. Here, we develop a model that integrates predicted spot prices [...] Read more.
Hybrid production plants harness diverse climatic sources for electricity generation, playing a crucial role in the transition to renewable energies. This study aims to forecast the profitability of a combined wind–photovoltaic energy system. Here, we develop a model that integrates predicted spot prices and electricity output forecasts, incorporating relevant climatic variables to enhance accuracy. The jointly modeled climatic variables and the spot price constitute one of the innovative aspects of this work. Regarding practical application, we considered a hypothetical wind–photovoltaic plant located in Italy and used the relevant climate series to determine the quantity of energy produced. We forecast the quantity of energy as well as income through machine learning techniques and more traditional statistical and econometric models. We evaluate the results by splitting the dataset into estimation windows and test windows, and using a backtesting technique. In particular, we found evidence that ML regression techniques outperform results obtained with traditional econometric models. Regarding the models used to achieve this goal, the objective is not to propose original models but to verify the effectiveness of the most recent machine learning models for this important application, and to compare them with more classic linear regression techniques. Full article
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Figure 1

Figure 1
<p>Power plant location.</p>
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<p>Power curve of the turbine.</p>
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<p>Backtesting and rolling windows.</p>
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<p>(<b>a</b>) Autocorrelation functions for the main variables. (<b>b</b>) Partial autocorrelation functions for the main variables.</p>
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22 pages, 2149 KiB  
Article
Robust Biometric Verification Using Phonocardiogram Fingerprinting and a Multilayer-Perceptron-Based Classifier
by Roberta Avanzato, Francesco Beritelli and Salvatore Serrano
Electronics 2024, 13(22), 4377; https://doi.org/10.3390/electronics13224377 - 8 Nov 2024
Viewed by 392
Abstract
Recently, a new set of biometric traits, called medical biometrics, have been explored for human identity verification. This study introduces a novel framework for recognizing human identity through heart sound signals, commonly referred to as phonocardiograms (PCGs). The framework is built on extracting [...] Read more.
Recently, a new set of biometric traits, called medical biometrics, have been explored for human identity verification. This study introduces a novel framework for recognizing human identity through heart sound signals, commonly referred to as phonocardiograms (PCGs). The framework is built on extracting and suitably processing Mel-Frequency Cepstral Coefficients (MFCCs) from PCGs and on a classifier based on a Multilayer Perceptron (MLP) network. A large dataset containing heart sounds acquired from 206 people has been used to perform the experiments. The classifier was tuned to obtain the same false positive and false negative misclassification rates (equal error rate: EER = FPR = FNR) on chunks of audio lasting 2 s. This target has been reached, splitting the dataset into 70% and 30% training and testing non-overlapped subsets, respectively. A recurrence filter has been applied to also improve the performance of the system in the presence of noisy recordings. After the application of the filter on chunks of audio signal lasting from 2 to 22 s, the performance of the system has been evaluated in terms of recall, specificity, precision, negative predictive value, accuracy, and F1-score. All the performance metrics are higher than 97.86% with the recurrence filter applied on a window lasting 22 s and in different noise conditions. Full article
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Figure 1

Figure 1
<p>Block diagram of biometric authentication modes: (<b>a</b>) identification mode; (<b>b</b>) verification mode.</p>
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<p>Examples of PCG recordings for 2 subjects: (<b>a</b>) 1st PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, (<b>b</b>) 2nd PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>, (<b>c</b>) 1st PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, and (<b>d</b>) 2nd PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>.</p>
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<p>Examples of PCG recordings for 2 subjects: (<b>a</b>) 1st PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, (<b>b</b>) 2nd PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>, (<b>c</b>) 1st PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, and (<b>d</b>) 2nd PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>.</p>
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<p>Details (extracted at t = 20 s and lasting 2 s) of PCG recordings for 2 subjects: (<b>a</b>) 1st PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, (<b>b</b>) 2nd PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>, (<b>c</b>) 1st PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>1</mn> </mrow> </msub> </semantics></math>, and (<b>d</b>) 2nd PCG recording of a male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mrow> <mi>y</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>.</p>
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<p>Mel-frequency spectrograms and image representation of the related averaged vector <math display="inline"><semantics> <mover accent="true"> <mi>c</mi> <mo>→</mo> </mover> </semantics></math> evaluated for (<b>a</b>) 1st PCG chunk for female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mi>x</mi> </msub> </semantics></math>, (<b>b</b>) 2nd PCG chunk for female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mi>x</mi> </msub> </semantics></math>, (<b>c</b>) 1st PCG chunk for male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mi>y</mi> </msub> </semantics></math>, and (<b>d</b>) 2nd PCG chunk for male subject <math display="inline"><semantics> <msub> <mi>M</mi> <mi>y</mi> </msub> </semantics></math>.</p>
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<p>Architecture of MLP binary classifier implemented to perform human identity verification by means of PCG features extracted from a segment of audio recording lasting 2 s; the output <math display="inline"><semantics> <mrow> <mi>y</mi> <mo>(</mo> <mi>m</mi> <mo>)</mo> </mrow> </semantics></math> is true for identity verified, false for identity not verified.</p>
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<p>Architecture of the recurrence filter.</p>
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<p>Example of chunk affected by noises (2nd PCG recording of a female subject <math display="inline"><semantics> <msub> <mi>F</mi> <mrow> <mi>x</mi> <mo>,</mo> <mn>2</mn> </mrow> </msub> </semantics></math>): (<b>a</b>) signal plus office noise, SNR = 15 dB (in red), (<b>b</b>) signal plus babble noise, SNR = 20 dB (in red), (<b>c</b>) signal plus babble noise, SNR = 30 dB (in red), (<b>d</b>) Mel spectrogram and features for chunk in (<b>a</b>), (<b>e</b>) Mel spectrogram and features for chunk in (<b>b</b>), and (<b>f</b>) Mel spectrogram and features for chunk in (<b>c</b>).</p>
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<p>Output of the loss function during the training phase for each epoch.</p>
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<p>ROC curve for HSCT-11 database without application of the “recurrence filter”.</p>
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<p>DET curve for HSCT-11 database without application of the “recurrence filter”. Red dashed line corresponds to the EER.</p>
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<p>Confusion matrices varying “recurrence filter” length obtained with the testing set portion of the system database: (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>L</mi> <mo>=</mo> <mn>0</mn> </mrow> </semantics></math>: no filtering, response time 2 s; (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>L</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>: response time 6 s; (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>L</mi> <mo>=</mo> <mn>4</mn> </mrow> </semantics></math>: response time 10 s; (<b>d</b>) <math display="inline"><semantics> <mrow> <mi>L</mi> <mo>=</mo> <mn>6</mn> </mrow> </semantics></math>: response time 14 s.</p>
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<p>Performance indexes varying “recurrence filter” length (response time) for the four datasets: (<b>a</b>) recall, (<b>b</b>) specificity, (<b>c</b>) precision, (<b>d</b>) negative predictive value, (<b>e</b>) accuracy, and (<b>f</b>) F1-score.</p>
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23 pages, 32897 KiB  
Article
On the Suitability of Different Satellite Land Surface Temperature Products to Study Surface Urban Heat Islands
by Alexandra Hurduc, Sofia L. Ermida and Carlos C. DaCamara
Remote Sens. 2024, 16(20), 3765; https://doi.org/10.3390/rs16203765 - 10 Oct 2024
Viewed by 964
Abstract
Remote sensing satellite data have been a crucial tool in understanding urban climates. The variety of sensors with different spatiotemporal characteristics and retrieval methodologies gave rise to a multitude of approaches when analyzing the surface urban heat island effect (SUHI). Although there are [...] Read more.
Remote sensing satellite data have been a crucial tool in understanding urban climates. The variety of sensors with different spatiotemporal characteristics and retrieval methodologies gave rise to a multitude of approaches when analyzing the surface urban heat island effect (SUHI). Although there are considerable advantages that arise from these different characteristics (spatiotemporal resolution, time of observation, etc.), it also means that there is a need for understanding the ability of sensors in capturing spatial and temporal SUHI patterns. For this, several land surface temperature products are compared for the cities of Madrid and Paris, retrieved from five sensors: the Spinning Enhanced Visible and InfraRed Imager onboard Meteosat Second Generation, the Advanced Very-High-Resolution Radiometer onboard Metop, the Moderate-resolution Imaging Spectroradiometer onboard both Aqua and Terra, and the Thermal Infrared Sensor onboard Landsat 8 and 9. These products span a wide range of LST algorithms, including split-window, single-channel, and temperature–emissivity separation methods. Results show that the diurnal amplitude of SUHI may not be well represented when considering daytime and nighttime polar orbiting platforms. Also, significant differences arise in SUHI intensity and spatial and temporal variability due to the different methods implemented for LST retrieval. Full article
(This article belongs to the Section AI Remote Sensing)
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Figure 1
<p>Land cover resampled for the three projections of LST products (<b>a</b>–<b>f</b>) along with the percentage of urban pixels (<b>g</b>–<b>l</b>).</p>
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<p>Time of observation of each sensor: (<b>a</b>) for Madrid during daytime and time of minimum SUHI (SUHI<sub>min</sub>), (<b>b</b>) for Madrid during nighttime and time of maximum SUHI (SUHI<sub>max</sub>), (<b>c</b>) for Paris during daytime and SUHI<sub>max</sub>, (<b>d</b>) for Paris during nighttime and SUHI<sub>min</sub>. Colored bins are sampled every 15 min.</p>
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<p>Mean DJF (December, January, February) LST for all products considered. (<b>a1</b>–<b>a9</b>) The spatial pattern during daytime, and in the case of the MLST, the most frequent hour of the LST maximum and SUHI minimum are shown; (<b>b1</b>–<b>b9</b>) histograms of urban and rural LST shown in (<b>a1</b>–<b>a9</b>); (<b>c1</b>–<b>c7</b>) as in the first line but for nighttime and for the LST minimum and SUHI maximum; (<b>d1</b>–<b>d7</b>) as in (<b>b1</b>–<b>b9</b>) but for nighttime. Please note that color bars are different amongst the different products to allow a better visualization of patterns, but value ranges of the histograms are the same.</p>
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<p>As <a href="#remotesensing-16-03765-f003" class="html-fig">Figure 3</a> but for JJA (June, July, and August). (<b>a1</b>–<b>a9</b>) The spatial pattern during daytime, and in the case of the MLST, the most frequent hour of the LST maximum and SUHI minimum are shown; (<b>b1</b>–<b>b9</b>) histograms of urban and rural LST shown in (<b>a1</b>–<b>a9</b>); (<b>c1</b>–<b>c7</b>) as in the first line but for nighttime and for the LST minimum and SUHI maximum; (<b>d1</b>–<b>d7</b>) as in (<b>b1</b>–<b>b9</b>) but for nighttime. Please note that color bars are different amongst the different products to allow a better visualization of patterns, but value ranges of the histograms are the same.</p>
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<p>As <a href="#remotesensing-16-03765-f003" class="html-fig">Figure 3</a> but for Paris. (<b>a1</b>–<b>a9</b>) The spatial pattern during daytime, and in the case of the MLST, the most frequent hour of the LST and SUHI maximum; (<b>b1</b>–<b>b9</b>) histograms of urban and rural LST shown in (<b>a1</b>–<b>a9</b>); (<b>c1</b>–<b>c7</b>) as in the first line but for nighttime and for the LST and SUHI minimum; (<b>d1</b>–<b>d7</b>) as in (<b>b1</b>–<b>b9</b>) but for nighttime. Please note that color bars are different amongst the different products to allow a better visualization of patterns, but value ranges of the histograms are the same.</p>
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<p>As <a href="#remotesensing-16-03765-f003" class="html-fig">Figure 3</a> but for Paris and DJF; (<b>a1</b>–<b>a9</b>) The spatial pattern during daytime, and in the case of the MLST, the most frequent hour of the LST and SUHI maximum; (<b>b1</b>–<b>b9</b>) histograms of urban and rural LST shown in (<b>a1</b>–<b>a9</b>); (<b>c1</b>–<b>c7</b>) as in the first line but for nighttime and for the LST and SUHI minimum; (<b>d1</b>–<b>d7</b>) as in (<b>b1</b>–<b>b9</b>) but for nighttime, an extension of the histogram in (<b>d6</b>) is seen in (<b>d8</b>). Please note that color bars are different amongst the different products to allow a better visualization of patterns, but value ranges of the histograms are the same.</p>
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<p>Diurnal cycle of SUHI for Madrid: (<b>a</b>) DJF, (<b>b</b>) MAM, (<b>c</b>) JJA, (<b>d</b>) SON.</p>
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<p>As <a href="#remotesensing-16-03765-f007" class="html-fig">Figure 7</a> but for Paris.</p>
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<p>Correlation of monthly SUHI anomalies between all products considered: (<b>a</b>) daytime, (<b>b</b>) nighttime. Blank spaces correspond to pairs of products with no significant correlation (<span class="html-italic">p</span>-value &gt; 0.05).</p>
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<p>As <a href="#remotesensing-16-03765-f009" class="html-fig">Figure 9</a> but for Paris. (<b>a</b>) daytime, (<b>b</b>) nighttime. Blank spaces correspond to pairs of products with no significant correlation (<span class="html-italic">p</span>-value &gt; 0.05).</p>
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16 pages, 13318 KiB  
Article
Investigation and Validation of Split-Window Algorithms for Estimating Land Surface Temperature from Landsat 9 TIRS-2 Data
by Qinghua Su, Xiangchen Meng and Lin Sun
Remote Sens. 2024, 16(19), 3633; https://doi.org/10.3390/rs16193633 - 29 Sep 2024
Viewed by 845
Abstract
Land surface temperature (LST) is important in a variety of applications, such as urban thermal environment monitoring and water resource management. In this paper, eleven candidate split-window (SW) algorithms were adapted to Thermal Infrared Sensor-2 (TIRS-2) data of the Landsat 9 satellite for [...] Read more.
Land surface temperature (LST) is important in a variety of applications, such as urban thermal environment monitoring and water resource management. In this paper, eleven candidate split-window (SW) algorithms were adapted to Thermal Infrared Sensor-2 (TIRS-2) data of the Landsat 9 satellite for estimating the LST. The simulated dataset produced by extensive radiative transfer modeling and five global atmospheric profile databases was used to determine the SW algorithm coefficients. Ground measurements gathered at Surface Radiation Budget Network sites were used to confirm the efficiency of the SW algorithms after their performance was initially examined using the independent simulation dataset. Five atmospheric profile databases perform similarly in training accuracy under various subranges of total water vapor. The candidate SW algorithms demonstrate superior performance compared to the radiative transfer equation algorithm, exhibiting a reduction in overall bias and RMSE by 1.30 K and 1.0 K, respectively. It is expected to provide guidance for the generation of the Landsat 9 LST using the SW algorithms. Full article
(This article belongs to the Special Issue Surface Radiative Transfer: Modeling, Inversion, and Applications)
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Graphical abstract

Graphical abstract
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<p>Performance of the eleven candidate SW algorithms under different total water vapor (TWV) subranges: (<b>a</b>) 0 &lt; TWV &lt; 1.5 g/cm<sup>2</sup>, (<b>b</b>) 1.5 &lt; TWV &lt; 3.0 g/cm<sup>2</sup>, (<b>c</b>) 3.0 &lt; TWV &lt; 4.5 g/cm<sup>2</sup>, (<b>d</b>) 4.5 &lt; TWV &lt; 10 g/cm<sup>2</sup>, and (<b>e</b>) 0 &lt; TWV &lt; 10 g/cm<sup>2</sup>.</p>
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<p>Performance of the eleven candidate SW algorithms under different total water vapor (TWV) subranges: (<b>a</b>) 0 &lt; TWV &lt; 1.5 g/cm<sup>2</sup>, (<b>b</b>) 1.5 &lt; TWV &lt; 3.0 g/cm<sup>2</sup>, (<b>c</b>) 3.0 &lt; TWV &lt; 4.5 g/cm<sup>2</sup>, (<b>d</b>) 4.5 &lt; TWV &lt; 10 g/cm<sup>2</sup>, and (<b>e</b>) 0 &lt; TWV &lt; 10 g/cm<sup>2</sup>.</p>
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<p>Performance of the eleven candidate SW algorithms before and after adding random noise under different total water vapor (TWV) subranges: (<b>a</b>–<b>c</b>) 0 &lt; TWV &lt; 1.5 g/cm<sup>2</sup>, (<b>d</b>–<b>f</b>) 4.5 &lt; TWV &lt; 10 g/cm<sup>2</sup>. The random noise is added in the emissivity (<b>a</b>,<b>d</b>), brightness temperature (<b>b</b>,<b>e</b>), and TWV (<b>c</b>,<b>f</b>).</p>
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<p>The bias (<b>a</b>) and RMSE (<b>b</b>) between the retrieved Landsat 9 LST and the in situ LST for all matchups at the SURFRAD sites.</p>
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<p>The bias (<b>a</b>) and RMSE (<b>b</b>) between the retrieved Landsat 9 LST and the MODIS LST.</p>
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<p>Spatial distribution of the difference between the retrieved Landsat 9 LST and the MODIS LST. (<b>a</b>,<b>e</b>) LST retrieved from RTE algorithm, (<b>b</b>,<b>f</b>) LST retrieved from SW1 algorithm, (<b>c</b>,<b>g</b>) LST retrieved from SW3 algorithm, and (<b>d</b>,<b>h</b>) LST retrieved from SW5 algorithm.</p>
Full article ">Figure 5 Cont.
<p>Spatial distribution of the difference between the retrieved Landsat 9 LST and the MODIS LST. (<b>a</b>,<b>e</b>) LST retrieved from RTE algorithm, (<b>b</b>,<b>f</b>) LST retrieved from SW1 algorithm, (<b>c</b>,<b>g</b>) LST retrieved from SW3 algorithm, and (<b>d</b>,<b>h</b>) LST retrieved from SW5 algorithm.</p>
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<p>Scatterplots between the air temperature at the first layer and the total water vapor of the six atmospheric profile databases. (<b>a</b>) CLAR, (<b>b</b>) ERA5, (<b>c</b>) GAPRI (<b>d</b>) SeeBor, (<b>e</b>) TIGR and (<b>f</b>) WYO.</p>
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<p>Scatterplots between the air temperature at the first layer and the total water vapor of the six atmospheric profile databases. (<b>a</b>) CLAR, (<b>b</b>) ERA5, (<b>c</b>) GAPRI (<b>d</b>) SeeBor, (<b>e</b>) TIGR and (<b>f</b>) WYO.</p>
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17 pages, 6764 KiB  
Article
Fault Diagnosis Method for Vacuum Contactor Based on Time-Frequency Graph Optimization Technique and ShuffleNetV2
by Haiying Li, Qinyang Wang and Jiancheng Song
Sensors 2024, 24(19), 6274; https://doi.org/10.3390/s24196274 - 27 Sep 2024
Viewed by 447
Abstract
This paper presents a fault diagnosis method for a vacuum contactor using the generalized Stockwell transform (GST) of vibration signals. The objective is to solve the problem of low diagnostic performance efficiency caused by the inadequate feature extraction capability and the redundant pixels [...] Read more.
This paper presents a fault diagnosis method for a vacuum contactor using the generalized Stockwell transform (GST) of vibration signals. The objective is to solve the problem of low diagnostic performance efficiency caused by the inadequate feature extraction capability and the redundant pixels in the graph background. The proposed method is based on the time-frequency graph optimization technique and ShuffleNetV2 network. Firstly, vibration signals in different states are collected and converted into GST time-frequency graphs. Secondly, multi-resolution GST time-frequency graphs are generated to cover signal characteristics in all frequency bands by adjusting the GST Gaussian window width factor λ. The OTSU algorithm is then combined to crop the energy concentration area, and the size of these time-frequency graphs is optimized by 68.86%. Finally, considering the advantages of the channel split and channel shuffle methods, the ShuffleNetV2 network is adopted to improve the feature learning ability and identify fault categories. In this paper, the CKJ5-400/1140 vacuum contactor is taken as the test object. The fault recognition accuracy reaches 99.74%, and the single iteration time of model training is reduced by 19.42%. Full article
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Figure 1
<p>Acceleration sensor mounting position diagram.</p>
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<p>Closing vibration signal waveforms in different states.</p>
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<p>GST time-frequency graphs of vibration signals in different states: (<b>a</b>) normal; (<b>b</b>) iron core rusting; (<b>c</b>) closing spring fatigue; (<b>d</b>) base screw loosening.</p>
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<p>Vibration signal GST time-frequency graph data augmentation.</p>
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<p>Cropping optimization of the GST time-frequency graph.</p>
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<p>ShuffleNetV2 network architecture.</p>
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<p>Two basic modules for ShuffleNetV2: (<b>a</b>) basic unit; (<b>b</b>) down-sampling unit.</p>
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<p>The framework of vacuum contactor fault diagnosis.</p>
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<p>Multi-resolution GST time-frequency graphs.</p>
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<p>The values of SSIM between time-frequency graph augmented data and original data.</p>
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<p>Optimization results of cropped GST time-frequency graphs: (<b>a</b>) normal; (<b>b</b>) iron core rusting; (<b>c</b>) closing spring fatigue; (<b>d</b>) base screw loosening.</p>
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<p>State recognition confusion matrices for GST time-frequency graphs: (<b>a</b>) without cropping optimization; (<b>b</b>) with cropping optimization.</p>
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<p>The accuracy of the test set for GST time-frequency graphs in four networks. AlexNet [<a href="#B28-sensors-24-06274" class="html-bibr">28</a>], ResNet50 [<a href="#B29-sensors-24-06274" class="html-bibr">29</a>], ResNeXt50 [<a href="#B30-sensors-24-06274" class="html-bibr">30</a>], ShuffleNetV2 [<a href="#B33-sensors-24-06274" class="html-bibr">33</a>].</p>
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16 pages, 8514 KiB  
Article
Sinus Floor Augmentation with Synthetic Hydroxyapatite (NanoBone®) in Combination with Platelet-Rich Fibrin: A Case Series
by Luís Francisco, Manuel Francisco, Rosana Costa, Miguel Nunes Vasques, Marta Relvas, António Rajão, Luís Monteiro, Paulo Rompante, Fernando Guerra and Marco Infante da Câmara
Biomedicines 2024, 12(8), 1661; https://doi.org/10.3390/biomedicines12081661 - 25 Jul 2024
Viewed by 953
Abstract
Several techniques have been described for maxillary sinus graft augmentation, including the lateral window technique and crestal approach with osteotomes or osseodensification. Platelet-rich fibrin has been used in maxillary sinus lift procedures due to its ability to accelerate soft and hard tissue healing. [...] Read more.
Several techniques have been described for maxillary sinus graft augmentation, including the lateral window technique and crestal approach with osteotomes or osseodensification. Platelet-rich fibrin has been used in maxillary sinus lift procedures due to its ability to accelerate soft and hard tissue healing. The aim of this study was to evaluate the potential of PRF in combination with the synthetic hydroxyapatite NanoBone® to enhance bone regeneration in sinus floor elevation with the lateral window technique. Out of the 50 individuals screened in a preoperative assessment visit from the CESPU—Famalicão clinical unit and intervened upon between January 2023 and December 2023, only 6 patients who met the study’s inclusion criteria consented to participate. In a split-mouth study, twelve sinus graft surgeries were carried out. Our observations reveal that for the test group (NanoBone®/PRF), there is a 27.5 ± 4.9% increase new vital bone, 23.0 ± 3.7% increase in inert bone particles, and 49.4 ± 2.8% increase in connective tissue. Meanwhile, for the control group (NanoBone®), there is a 19.5 ± 3.0% increase in new vital bone, 23.4 ± 5.7% increase in inert bone particles, and 57.0 ± 3.5% increase in connective tissue. The results strongly indicate that mixing liquid PRF with NanoBone® does not have a negative influence on the amount of viable bone formation, and it seems to slightly increase the amount of new bone formation and revascularization in sinus bone graft procedures with the lateral window technique compared to the single use of NanoBone®. Full article
(This article belongs to the Section Nanomedicine and Nanobiology)
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<p>A visual representation of the surgery. (<b>a</b>) Bony window with Acteon Satelec<sup>®</sup> piezoelectric device; (<b>b</b>) Schneiderian membrane elevated; (<b>c</b>) Aggregation of NanoBone<sup>®</sup> with liquid fibrin; (<b>d</b>) Biomaterial insertion in the sinus cavity; (<b>e</b>) Straumann<sup>®</sup> Fex collagen membrane over the bony window.</p>
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<p>Harvesting of the bone specimen with a 2.5 mm diameter trephine bur. (<b>a</b>) Surgical site; (<b>b</b>) Trephine drill with collected bone; (<b>c</b>) Trephine drill with bone specimen in a 10% formaldehyde sterile vial.</p>
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<p>CONSORT flowchart.</p>
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<p>Newly formed bone, residual bone graft material, and connective tissue for both control (NanoBone<sup>®</sup> alone) and test groups (NanoBone<sup>®</sup>/liquid fibrin). Bars represent the mean and standard deviation of individuals results. (A) New vital bone, (B) particles, (C) new vital bone + particles, and (D) connective tissue. (*** <span class="html-italic">p</span> &lt; 0.0005).</p>
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<p>Histologic results in both groups: (<b>a</b>) test group; (<b>b</b>) control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in both groups: (<b>a</b>) test group; (<b>b</b>) control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in both groups: (<b>a</b>) test group; (<b>b</b>) control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in both groups: (<b>a</b>) test group; (<b>b</b>) control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in the test group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in both groups: (<b>a</b>,<b>b</b>) test group; (<b>c</b>) control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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<p>Histologic results in the control group. 10 × 0.5 magnification and toluidine blue staining.</p>
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10 pages, 959 KiB  
Communication
One Algorithm to Rule Them All? Defining Best Strategy for Land Surface Temperature Retrieval from NOAA-AVHRR Afternoon Satellites
by Yves Julien, José A. Sobrino and Juan-Carlos Jiménez-Muñoz
Remote Sens. 2024, 16(15), 2720; https://doi.org/10.3390/rs16152720 - 25 Jul 2024
Viewed by 582
Abstract
The NOAA-AVHRR (National Oceanographic and Atmospheric Administration–Advanced Very High-Resolution Radiometer) archive includes data from 1981 onwards, which allow for estimating land surface temperature (LST), a key parameter for the study of global warming as well as surface characterization. However, algorithms for LST retrieval [...] Read more.
The NOAA-AVHRR (National Oceanographic and Atmospheric Administration–Advanced Very High-Resolution Radiometer) archive includes data from 1981 onwards, which allow for estimating land surface temperature (LST), a key parameter for the study of global warming as well as surface characterization. However, algorithms for LST retrieval were developed before the latest sensors and were based on more reduced atmospheric datasets. Here, we present 50 novel sets of coefficients for an LST retrieval algorithm from NOAA-AVHRR sensors, to which we added one historical methodology, which we validate against historical in situ as well as independent satellite data. This validation shows that the historical algorithm performs surprisingly well, with an in situ RMSE below 1.5 K and a quasi-null bias when compared with independent satellite data. A couple of the novel algorithms also perform within expectations (errors below 1.5 K), so any of these could be used for the complete processing of the AVHRR dataset. In our case, considering consistency with previous works, we opt for the use of the historical algorithm, now also tested for more recent periods. Full article
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<p>Distribution of the satellite validation data through 1981–2022. The number of validation data points for each satellite are in parentheses.</p>
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9 pages, 2884 KiB  
Comment
Comment on Yu et al. Land Surface Temperature Retrieval from Landsat 8 TIRS—Comparison between Radiative Transfer Equation-Based Method, Split Window Algorithm and Single Channel Method. Remote Sens. 2014, 6, 9829–9852
by Almustafa Abd Elkader Ayek and Bilel Zerouali
Remote Sens. 2024, 16(14), 2514; https://doi.org/10.3390/rs16142514 - 9 Jul 2024
Viewed by 887
Abstract
Accurate land surface temperature (LST) retrieval from satellite data is pivotal in environmental monitoring and scientific research. This study addresses the impact of variability in the effective wavelengths used for LST retrieval from the Thermal Infrared Sensor (TIRS) data of Landsat 8. We [...] Read more.
Accurate land surface temperature (LST) retrieval from satellite data is pivotal in environmental monitoring and scientific research. This study addresses the impact of variability in the effective wavelengths used for LST retrieval from the Thermal Infrared Sensor (TIRS) data of Landsat 8. We conduct a detailed analysis comparing the effective wavelengths reported by Yu et al. (2014) and those derived from data provided by the USGS. Our analysis reveals significant variability in the effective wavelengths for bands 10 and 11 of Landsat 8. By applying Planck’s Law and utilizing the K1 and K2 coefficients available in the metadata of Landsat 8 products, we derive the effective wavelengths for bands 10 and 11. We also rederive the effective wavelength by integrating the spectral response function of the TIRS1 sensor. Our findings indicate that the effective wavelength for band 10 is 10.814 μm, aligning with the USGS data, while the effective wavelength for band 11 is 12.013 μm. We discuss the implications of these corrected effective wavelengths on the accuracy of LST retrieval algorithms, particularly the single channel algorithm (SC) and the radiative transfer equation (RT) employed by Yu et al. The importance of using precise effective wavelengths in satellite-based temperature retrieval is emphasized, to ensure the reliability and consistency of results. This analysis underscores the critical role of accurate spectral calibration parameters in remote sensing studies and provides valuable insights in the field of land surface temperature retrieval from Landsat 8 TIRS data. Full article
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<p>TIRS relative spectral response.</p>
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<p>Spectral response function for Landsat 8 product (B10).</p>
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<p>Standard deviation for Landsat 8 product (B10).</p>
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<p>Spectral response function for Landsat 8 product (B11).</p>
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<p>Standard deviation for Landsat 8 product (B11).</p>
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<p>The relative spectral response function for band 10 using cubic interpolation.</p>
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<p>The relative spectral response function for band 11 using cubic interpolation.</p>
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24 pages, 8649 KiB  
Article
Assessing the Impact of Land Use and Land Cover Changes on Surface Temperature Dynamics Using Google Earth Engine: A Case Study of Tlemcen Municipality, Northwestern Algeria (1989–2019)
by Imene Selka, Abderahemane Medjdoub Mokhtari, Kheira Anissa Tabet Aoul, Djamal Bengusmia, Kacemi Malika and Khadidja El-Bahdja Djebbar
ISPRS Int. J. Geo-Inf. 2024, 13(7), 237; https://doi.org/10.3390/ijgi13070237 - 2 Jul 2024
Cited by 2 | Viewed by 2485
Abstract
Changes in land use and land cover (LULC) have a significant impact on urban planning and environmental dynamics, especially in regions experiencing rapid urbanization. In this context, by leveraging the Google Earth Engine (GEE), this study evaluates the effects of land use and [...] Read more.
Changes in land use and land cover (LULC) have a significant impact on urban planning and environmental dynamics, especially in regions experiencing rapid urbanization. In this context, by leveraging the Google Earth Engine (GEE), this study evaluates the effects of land use and land cover modifications on surface temperature in a semi-arid zone of northwestern Algeria between 1989 and 2019. Through the analysis of Landsat images on GEE, indices such as normalized difference vegetation index (NDVI), normalized difference built-up index (NDBI), and normalized difference latent heat index (NDLI) were extracted, and the random forest and split window algorithms were used for supervised classification and surface temperature estimation. The multi-index approach combining the Normalized Difference Tillage Index (NDTI), NDBI, and NDVI resulted in kappa coefficients ranging from 0.96 to 0.98. The spatial and temporal analysis of surface temperature revealed an increase of 4 to 6 degrees across the four classes (urban, barren land, vegetation, and forest). The Google Earth Engine approach facilitated detailed spatial and temporal analysis, aiding in understanding surface temperature evolution at various scales. This ability to conduct large-scale and long-term analysis is essential for understanding trends and impacts of land use changes at regional and global levels. Full article
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<p>Location map of Tlemcen, Algeria.</p>
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<p>Conceptual framework of the study.</p>
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<p>Classified LULC maps of Tlemcen: (<b>a</b>) 2019, (<b>b</b>) 2009, (<b>c</b>) 1999, and (<b>d</b>) 1989.</p>
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<p>Description of LULC statistics of Tlemcen from 1989 to 2019.</p>
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<p>LST distribution for Tlemcen in (<b>a</b>) 2019, (<b>b</b>) 2009, (<b>c</b>) 1999, and (<b>d</b>) 1989.</p>
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<p>Spatial normal difference vegetation index (NDVI) in Tlemcen. NDVI maps are shown for (<b>a</b>) 2019, (<b>b</b>) 2009, (<b>c</b>) 1999, and (<b>d</b>) 1989.</p>
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<p>Spatial NDBI in Tlemcen. NDBI maps are shown for (<b>a</b>) 2019, (<b>b</b>) 2009, (<b>c</b>) 1999, and (<b>d</b>) 1989.</p>
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<p>Spatial NDLI in Tlemcen. NDLI maps are shown for (<b>a</b>) 2019, (<b>b</b>) 2009, (<b>c</b>) 1999, and (<b>d</b>) 1989.</p>
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22 pages, 6217 KiB  
Article
A Mathematical Model for Integrated Disaster Relief Operations in Early-Stage Flood Scenarios
by Nur Insani, Sona Taheri and Mali Abdollahian
Mathematics 2024, 12(13), 1978; https://doi.org/10.3390/math12131978 - 26 Jun 2024
Viewed by 1595
Abstract
When a flood strikes, the two most critical tasks are evacuation and relief distribution. It is essential to integrate these tasks, particularly before the floodwater reaches the vulnerable area, to minimize loss and damage. This paper presents a mathematical model of vehicle routing [...] Read more.
When a flood strikes, the two most critical tasks are evacuation and relief distribution. It is essential to integrate these tasks, particularly before the floodwater reaches the vulnerable area, to minimize loss and damage. This paper presents a mathematical model of vehicle routing problems to optimize an integrated disaster relief operation. The model addresses routing for both the evacuation and relief distribution tasks in the early stages of a flood, aiming to identify a minimal number of vehicles required with their corresponding routes to transport vulnerable individuals and simultaneously distribute emergency relief. The new model incorporates several features, including vehicle reuse, multi-trip and split delivery scenarios for evacuees and emergency relief items, uncertainty in evacuation demands, and closing time windows at evacuation points. Due to the complexity of vehicle routing problems, particularly in large-scale scenarios, the exact approach for obtaining optimal solutions is time-consuming. Therefore, we propose the use of a metaheuristic algorithm, specifically a modified genetic algorithm, to find an approximate solution for the proposed model. We apply the developed model and modified algorithm to various simulated flood scenarios and a real-life case study from Indonesia. The experimental results demonstrate that our approach requires fewer vehicles compared to standard models for similar scenarios. Moreover, while the exact approach fails to find optimal solutions within a reasonable timeframe for large-scale scenarios, our new approach provides near-optimal solutions in a much shorter time. In smaller simulated scenarios, the modified genetic algorithm obtains optimal or near-optimal solutions approximately 92.5% faster than the exact approach. Full article
(This article belongs to the Section Computational and Applied Mathematics)
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<p>Relief disaster operations with evacuation and relief distribution tasks.</p>
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<p>The proposed modified genetic algorithm (MGA) utilising a modified best cost route as the crossover operator, a modified local search as the mutation operator and a constructive heuristic for generating an initial population and repairing it.</p>
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<p>Network traveling times.</p>
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<p>Evacuation and relief distribution plans of the integrated (<b>left</b>) and hierarchical (<b>right</b>) models.</p>
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<p>Bontoala district in Gowa regency, South Sulawesi, Indonesia.</p>
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<p>Distribution of temporary shelters in Bontoala, South Sulawesi, Indonesia.</p>
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25 pages, 2095 KiB  
Article
Operational Angular Track Reconstruction in Space Surveillance Radars through an Adaptive Beamforming Approach
by Marco Felice Montaruli, Maria Alessandra De Luca, Mauro Massari, Germano Bianchi and Alessio Magro
Aerospace 2024, 11(6), 451; https://doi.org/10.3390/aerospace11060451 - 1 Jun 2024
Viewed by 1199
Abstract
In the last few years, many space surveillance initiatives have started to consider the problem represented by resident space object overpopulation. In particular, the European Space Surveillance and Tracking (EUSST) consortium is in charge of providing services like collision avoidance, fragmentation analysis, and [...] Read more.
In the last few years, many space surveillance initiatives have started to consider the problem represented by resident space object overpopulation. In particular, the European Space Surveillance and Tracking (EUSST) consortium is in charge of providing services like collision avoidance, fragmentation analysis, and re-entry, which rely on measurements obtained through ground-based sensors. BIRALES is an Italian survey radar belonging to the EUSST framework and is capable of providing measurements including Doppler shift, slant range, and angular profile. In recent years, the Music Approach for Track Estimate and Refinement (MATER) algorithm has been developed to retrieve angular tracks through an adaptive beamforming technique, guaranteeing the generation of more accurate and robust measurements with respect to the previous static beamforming approach. This work presents the design of a new data processing chain to be used by BIRALES to compute the angular track. The signal acquired by the BIRALES receiver array is down-converted and the receiver bandwidth is split into multiple channels, in order to maximize the signal-to-noise ratio of the measurements. Then, the signal passes through a detection block, where an isolation procedure creates, for each epoch, signal correlation matrices (CMs) related to the channels involved in the detection and then processes them to isolate the data stream related to a single detected source. Consequently, for each epoch and for each detected source, just the CM featuring the largest signal contribution is kept, allowing deriving the Doppler shift measurement from the channel illumination sequence. The MATER algorithm is applied to each CM stream, first estimating the signal directions of arrival, then grouping them in the observation time window, and eventually returning the target angular track. Ambiguous estimates may be present due to the configuration of the receiver array, which cause spatial aliasing phenomena. This problem can be addressed by either exploiting transit prediction (in the case of cataloged objects), or by applying tailored criteria (for uncatalogued objects). The performance of the new architecture was assessed in real operational scenarios, demonstrating the enhancement represented by the implementation of the channelization strategy, as well as the angular measurement accuracy returned by MATER, in both nominal and off-nominal scenarios. Full article
(This article belongs to the Section Astronautics & Space Science)
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<p>BIRALES receivers (red dots) installed along the antenna focal line of the eight cylindrical parabolic concentrators called <span class="html-italic">1N-section</span>. Each receiver contains 16 dipoles.</p>
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<p>MUSIC array responses, generated through simulated data based on BIRALES characteristics, for a single (<b>a</b>) and two sources (<b>b</b>) simultaneously detected.</p>
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<p>Track estimate (<b>a</b>) and track refinement (<b>b</b>) results in the cataloged case.</p>
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<p>Track estimate (<b>a</b>) and track refinement (<b>b</b>) results in the catalogued case.</p>
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<p>Track estimate (<b>a</b>) and track refinement (<b>b</b>) results in the cataloged case for a multiple source scenario.</p>
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<p>Track estimate result (<b>a</b>) and the DOA estimation selection based on <span class="html-italic">delta-k</span> technique-based criterion (<b>b</b>) in the uncatalogued case for the multiple sources scenario.</p>
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<p>Flow diagram of the BIRALES processing chain for the MATER algorithm.</p>
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<p>CM eigenvalues related to the acquisition on 18 April, by function of the observation time window and illuminated channels, before and after removing noise. Two detection trends can be noticed: the largest CM eigenvalue trend represents the satellite Sentinel-3B, for which the observation was scheduled, while the smaller one concerns the satellite Starlink-4114, which was also detected during the acquisition.</p>
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<p>Time evolution of the detected signal, in terms of illuminated channels and Doppler shift. Two detection trends can be noticed: the longer one (Detection A) is related to the detection of the satellite Sentinel-3B, while the shorter one is related (Detection B) to the satellite Starlink-4114.</p>
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<p>Clustered CM eigenvalues related to the acquisition on 18 April. Two detection trends can be noticed: the larger eigenvalue one (Detection A) is related to the detection of the satellite Sentinel-3B, while the smaller eigenvalue is related (Detection B) to the satellite Starlink-4114.</p>
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<p>Doppler shift time profile returned by the pipeline. Detection A refers to the satellite Sentinel-3B, while Detection B refers to the satellite Starlink-4114.</p>
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<p>DOA estimations and angular tracks returned by the MATER algorithm. Detection A refers to the satellite Sentinel-3B, while Detection B refers to the satellite Starlink-4114. The angular track (continuous black line) is longer than the path covered by the estimated signal DOAs, as the former is related to all detection epochs, while the latter is related to a reduced time window, guaranteeing a more accurate DOA estimation in the track estimate phase of the MATER algorithm.</p>
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<p>SARAL satellite observation: eigenvalue time trend. By processing the data with the original architecture (<b>a</b>), that is without the channelization strategy, the two largest CM eigenvalue trends could be identified, related to a Cassiopea-A radio-astronomical source (the larger) and to the target satellite (the smaller). With the new architecture pipeline (<b>b</b>), just the latter trend remained.</p>
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<p>SARAL satellite observation: array response at a generic acquisition epoch. By processing the data with the original architecture (<b>a</b>), that is, without the channelization strategy, both the DOA estimation of the Cassiopea-A radio-astronomical source and that of the target satellite can be noticed, together with the related ambiguities. With the new architecture pipeline (<b>b</b>), at the same generic epoch, only the DOA estimation of the target satellite remains, together with the ambiguous solutions.</p>
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<p>SARAL satellite observation: MATER angular track. By processing the data with the original architecture (<b>a</b>), that is, without the channelization strategy, the DOA estimations of both the Cassiopea-A radio-astronomical source (circle clusters) and that of the target satellite (which constitutes angular sequences) can be noticed. With the new architecture pipeline (<b>b</b>), only the DOA estimations related to the target satellite remain. It can be also noticed that the DOA estimations in the new architecture are denser than in the original one, because of the shorter integration time, and the angular track returned by MATER is longer.</p>
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<p>Observation of the Aeolus satellite on 27 July 2023, during its assisted re-entry: DOA estimations and angular track returned by the MATER algorithm in the uncatalogued case. The ambiguity was solved thanks to the geometrical filters.</p>
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<p>Observation of the Aeolus satellite on 27 July 2023, during its assisted re-entry: transit prediction delay with respect to the MATER estimation represented through the angular coordinate evolution throughout the entire acquisition (<b>a</b>) and using the BIRALES array response at a generic acquisition epoch (<b>b</b>).</p>
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<p>Calibrator data set: cumulative distribution functions describing the orbits of the observed objects at the detection epoch. The orbits are represented in terms of the semi-major axis, eccentricity, inclination, and right ascension of the ascending node.</p>
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<p>Calibrator data set: cumulative distribution functions of the angular RMSE, for both cataloged and uncatalogued cases, for the two angular coordinates separately. Overall, the cataloged and uncatalogued cases showed similar results, and the angular track turned out to be generally more accurate along the <math display="inline"><semantics> <mrow> <mo>Δ</mo> <msub> <mi>γ</mi> <mn>1</mn> </msub> </mrow> </semantics></math> direction than along the <math display="inline"><semantics> <mrow> <mo>Δ</mo> <msub> <mi>γ</mi> <mn>2</mn> </msub> </mrow> </semantics></math> one, because of the length of the angular path traveled during the integration time.</p>
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<p>Calibrators data set: angular track and DOA estimations returned by the MATER algorithm for the observation of the satellite COSMOS 2517 (norad ID 41579) conducted on 7 April 2022. An incorrect angular track was returned by the exploited ambiguity solving criterion, as the assumption that the source spent a remarkable portion of the transit in the central region of the receiver FoV was not matched.</p>
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30 pages, 1637 KiB  
Article
Enhancing Monthly Streamflow Prediction Using Meteorological Factors and Machine Learning Models in the Upper Colorado River Basin
by Saichand Thota, Ayman Nassar, Soukaina Filali Boubrahimi, Shah Muhammad Hamdi and Pouya Hosseinzadeh
Hydrology 2024, 11(5), 66; https://doi.org/10.3390/hydrology11050066 - 1 May 2024
Cited by 1 | Viewed by 3122
Abstract
Streamflow prediction is crucial for planning future developments and safety measures along river basins, especially in the face of changing climate patterns. In this study, we utilized monthly streamflow data from the United States Bureau of Reclamation and meteorological data (snow water equivalent, [...] Read more.
Streamflow prediction is crucial for planning future developments and safety measures along river basins, especially in the face of changing climate patterns. In this study, we utilized monthly streamflow data from the United States Bureau of Reclamation and meteorological data (snow water equivalent, temperature, and precipitation) from the various weather monitoring stations of the Snow Telemetry Network within the Upper Colorado River Basin to forecast monthly streamflow at Lees Ferry, a specific location along the Colorado River in the basin. Four machine learning models—Random Forest Regression, Long short-term memory, Gated Recurrent Unit, and Seasonal AutoRegresive Integrated Moving Average—were trained using 30 years of monthly data (1991–2020), split into 80% for training (1991–2014) and 20% for testing (2015–2020). Initially, only historical streamflow data were used for predictions, followed by including meteorological factors to assess their impact on streamflow. Subsequently, sequence analysis was conducted to explore various input-output sequence window combinations. We then evaluated the influence of each factor on streamflow by testing all possible combinations to identify the optimal feature combination for prediction. Our results indicate that the Random Forest Regression model consistently outperformed others, especially after integrating all meteorological factors with historical streamflow data. The best performance was achieved with a 24-month look-back period to predict 12 months of streamflow, yielding a Root Mean Square Error of 2.25 and R-squared (R2) of 0.80. Finally, to assess model generalizability, we tested the best model at other locations—Greenwood Springs (Colorado River), Maybell (Yampa River), and Archuleta (San Juan) in the basin. Full article
(This article belongs to the Section Hydrology–Climate Interactions)
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<p>Visual Representation of Analyzed Factors (Temperature, Snow Water Equivalent, Precipitation, and Streamflow) in Streamflow Prediction.</p>
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<p>Colorado River Basin by United States Geological Survey (USGS) (<a href="https://www.usgs.gov/media/images/colorado-river-basin-map" target="_blank">https://www.usgs.gov/media/images/colorado-river-basin-map</a> (accessed on 10 February 2024)).</p>
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<p>Spatial Distribution of SNOTEL Weather Stations and USGS Gauges within the Upper Colorado River Basin.</p>
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<p>Time Series Plots of SNOTEL Data - Snow Water Equivalent (SWE) in inches, Precipitation Accumulation (Prcp_Acc) in inches, and Average Temperature (Avg_Temp) in degrees Fahrenheit.</p>
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<p>Time Series Plot of Streamflow Data from the US Bureau of Reclamation.</p>
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<p>Temporal Variation of Streamflow in Relation to Meteorological Variables.</p>
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<p>Correlation Analysis between Streamflow and Meteorological Variables.</p>
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<p>A Simplified Structure of RFR.</p>
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<p>The Structure of LSTM Memory Unit.</p>
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<p>Comparison of RMSE Distribution between Univariate and Multivariate Models.</p>
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<p>Comparison of Median <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math> between Univariate and Multivariate Time-Series Models.</p>
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<p>MAE, RMSE, SMAPE, MAPE, and <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math> Results of Univariate Time-Series ML Models.</p>
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<p>RMSE Distribution of Univariate Time-Series Models.</p>
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<p>RMSE Distribution of Multivariate Time-Series Models.</p>
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<p>RMSE, SMAPE, MAPE, and <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math> Results of Multivariate Time-Series ML Models.</p>
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<p>Comparison of Predicted and Observed USBR Streamflow Using Multivariate Time-Series Models (RFR, LSTM, GRU) with Input-Output Combinations of 12-12 and 24-12, for the Period from May 2015 to April 2016 over the Test Set.</p>
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<p>Comparison of Predicted vs. Observed Streamflow from Multivariate Time-Series Models (RFR, LSTM, GRU) over the Test Set (May 2015–April 2016).</p>
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<p>Heatmap Visualization of Evaluation Metrics (MAPE, SMAPE, <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math>, MAE, and RMSE) for Univariant RFR Model.</p>
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<p>Predictions of Univariate Time-Series RFR Models with Different Look-back Span Windows against Ground Truth (May 2018–April 2019).</p>
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<p>Heatmap Visualization of Evaluation Metrics (MAPE, SMAPE, <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math>, MAE, and RMSE) for Multivariate RFR Model.</p>
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<p>Predictions of Multivariate Time-Series RFR Models with Different Look-back Span Windows against Ground Truth (May 2018–April 2019).</p>
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<p>Top Features’ Combinations Count.</p>
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<p>Feature Importance of Meteorological Factors.</p>
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<p>Boxplot of <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math> for RFR Model Across Different Streamflows.</p>
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10 pages, 1056 KiB  
Article
Analysis of Interference Effect in Double Optomechanically Induced Transparency System
by Shengyan Liu, Zhengkai Han, Deen Li and Chaohua Tan
Photonics 2024, 11(4), 289; https://doi.org/10.3390/photonics11040289 - 22 Mar 2024
Cited by 2 | Viewed by 952
Abstract
We propose a scheme to investigate the interference properties of a double optomechanically induced transparency system, which involves two charged nanomechanical resonators, coupled via Coulomb interaction. The results show that the opening of transparency windows is caused by a destructive interference effect only [...] Read more.
We propose a scheme to investigate the interference properties of a double optomechanically induced transparency system, which involves two charged nanomechanical resonators, coupled via Coulomb interaction. The results show that the opening of transparency windows is caused by a destructive interference effect only in the weak optical coupling region. For strong optical coupling, normal mode splitting dominates the transparency phenomenon. In the intermediate region, both destructive interference and normal mode splitting contribute to the transparency windows. When the Coulomb coupling is much weaker than the optical coupling, the Coulomb interaction strength linearly determines the distance between the two transparency windows, and has nearly no influence on the destructive interference effect. Otherwise, the system will work in a nonlinear region. Full article
(This article belongs to the Section Quantum Photonics and Technologies)
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Figure 1

Figure 1
<p>(Color online) Schematic diagram of the optomechanical system which consists of a fixed mirror and two nanomechanical resonators (NR<sub>1</sub> and NR<sub>2</sub>). NR<sub>1</sub> and NR<sub>2</sub> are charged by the bias gate voltage with <math display="inline"><semantics> <msub> <mi>q</mi> <mn>1</mn> </msub> </semantics></math> and <math display="inline"><semantics> <msub> <mi>q</mi> <mn>2</mn> </msub> </semantics></math>, respectively. NR<sub>1</sub> and NR<sub>2</sub> are separated by a distance <math display="inline"><semantics> <msub> <mi>r</mi> <mn>0</mn> </msub> </semantics></math>, and the small displacements of which respect to their equilibrium positions are denoted by <math display="inline"><semantics> <msub> <mi>x</mi> <mn>1</mn> </msub> </semantics></math> and <math display="inline"><semantics> <msub> <mi>x</mi> <mn>2</mn> </msub> </semantics></math>, respectively. The optomechanical cavity with length <span class="html-italic">L</span> is driven by a strong coupling field <math display="inline"><semantics> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> </semantics></math> with frequency <math display="inline"><semantics> <msub> <mi>ω</mi> <mi>l</mi> </msub> </semantics></math> and a weak probe field <math display="inline"><semantics> <msub> <mi mathvariant="script">E</mi> <mi>p</mi> </msub> </semantics></math> with a frequency of <math display="inline"><semantics> <msub> <mi>ω</mi> <mi>p</mi> </msub> </semantics></math>. The output field due to the interacting process is denoted by <math display="inline"><semantics> <msub> <mi mathvariant="script">E</mi> <mi>out</mi> </msub> </semantics></math>.</p>
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<p>(Color online) Absorption <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>t</mi> <mi>a</mi> </msub> <msup> <mrow> <mo>|</mo> </mrow> <mn>2</mn> </msup> </mrow> </semantics></math> as a function of <math display="inline"><semantics> <mrow> <mi>δ</mi> <mo>−</mo> <msub> <mi>ω</mi> <mn>1</mn> </msub> </mrow> </semantics></math> and coupling power <math display="inline"><semantics> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> </semantics></math> for (<b>a</b>) without the Coulomb interaction characterized by <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>=</mo> <mn>0</mn> </mrow> </semantics></math>, (<b>b</b>) with the Coulomb coupling strength <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>=</mo> <mn>8</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>36 </mn> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mrow> <mi>Hz</mi> <mo>/</mo> <msup> <mi mathvariant="normal">m</mi> <mn>2</mn> </msup> </mrow> </semantics></math>.</p>
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<p>(Color online) (<b>a</b>) Energy-level diagram of the optomechanical system, where <span class="html-italic">N</span>, <math display="inline"><semantics> <msub> <mi>n</mi> <mn>1</mn> </msub> </semantics></math>, <math display="inline"><semantics> <msub> <mi>n</mi> <mn>2</mn> </msub> </semantics></math> are quantum number of the cavity photon and NR<sub>1</sub> and NR<sub>2</sub> phonons, respectively. (<b>b</b>) Energy-level diagram of the optomechanical system in the dressed state picture.</p>
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<p>(Color online) (<b>a</b>–<b>c</b>) Fitting results of the absorption <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>t</mi> <mi>a</mi> </msub> <msup> <mrow> <mo>|</mo> </mrow> <mn>2</mn> </msup> </mrow> </semantics></math> for Coulomb interaction strength <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>=</mo> <mn>8</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>36</mn> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mrow> <mi>Hz</mi> <mo>/</mo> <msup> <mi mathvariant="normal">m</mi> <mn>2</mn> </msup> </mrow> </semantics></math> via fitting models <math display="inline"><semantics> <msub> <mi>A</mi> <mi>ATS</mi> </msub> </semantics></math> and <math display="inline"><semantics> <msub> <mi>A</mi> <mi>EIT</mi> </msub> </semantics></math> in different regions, and only the best fitting results are kept. (<b>a</b>) <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> <mo>=</mo> <mn>2</mn> <mo>×</mo> <msup> <mn>10</mn> <mrow> <mo>−</mo> <mn>4</mn> </mrow> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mi mathvariant="normal">W</mi> </semantics></math>, with a good fit to <math display="inline"><semantics> <mrow> <msub> <mi>A</mi> <mi>EIT</mi> </msub> <mrow> <mo>(</mo> <mn>0.0001</mn> <mo>,</mo> <mo>−</mo> <mn>0.0860</mn> <mo>,</mo> <mn>0.0002</mn> <mo>,</mo> <mn>0.1252</mn> <mo>,</mo> <mn>0.1262</mn> <mo>)</mo> </mrow> </mrow> </semantics></math>. (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> <mo>=</mo> <mn>2</mn> <mo>×</mo> <msup> <mn>10</mn> <mrow> <mo>−</mo> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mi mathvariant="normal">W</mi> </semantics></math>, with a good fit to <math display="inline"><semantics> <mrow> <msub> <mi>A</mi> <mi>ATS</mi> </msub> <mrow> <mo>(</mo> <mn>0.0355</mn> <mo>,</mo> <mo>−</mo> <mn>0.1655</mn> <mo>,</mo> <mn>0.0337</mn> <mo>,</mo> <mn>0.0192</mn> <mo>,</mo> <mn>0.0191</mn> <mo>)</mo> </mrow> </mrow> </semantics></math>. (<b>c</b>) <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> <mo>=</mo> <mn>1</mn> <mo>×</mo> <msup> <mn>10</mn> <mrow> <mo>−</mo> <mn>1</mn> </mrow> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mi mathvariant="normal">W</mi> </semantics></math>, with a good fit to <math display="inline"><semantics> <mrow> <msub> <mi>A</mi> <mi>ATS</mi> </msub> <mrow> <mo>(</mo> <mn>0.0439</mn> <mo>,</mo> <mo>−</mo> <mn>0.3251</mn> <mo>,</mo> <mn>0.0457</mn> <mo>,</mo> <mn>0.0068</mn> <mo>,</mo> <mn>0.0069</mn> <mo>)</mo> </mrow> </mrow> </semantics></math>. (<b>d</b>) Per-point weights <math display="inline"><semantics> <msub> <mi>ω</mi> <mi>i</mi> </msub> </semantics></math> as a function of coupling field power <math display="inline"><semantics> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> </semantics></math>.</p>
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<p>(Color online) (<b>a</b>) Absorption <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>t</mi> <mi>a</mi> </msub> <msup> <mrow> <mo>|</mo> </mrow> <mn>2</mn> </msup> </mrow> </semantics></math> as a function of <math display="inline"><semantics> <msub> <mi>δ</mi> <mi>ω</mi> </msub> </semantics></math> and Coulomb interaction strength <math display="inline"><semantics> <mi>λ</mi> </semantics></math> with <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="script">E</mi> <mi>l</mi> </msub> <mo>=</mo> <mn>2</mn> <mo>×</mo> <msup> <mn>10</mn> <mrow> <mo>−</mo> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mi mathvariant="normal">W</mi> </semantics></math>, the other system parameters are the same as those given above, and two solid lines are the typical absorption profiles with different <math display="inline"><semantics> <mi>λ</mi> </semantics></math> fitted in the following. (<b>b</b>) The distance <span class="html-italic">D</span> between the two transparency windows as a function of <math display="inline"><semantics> <mi>λ</mi> </semantics></math>.</p>
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<p>(Color online) Fitting results of the absorption <math display="inline"><semantics> <mrow> <mrow> <mo>|</mo> </mrow> <msub> <mi>t</mi> <mi>a</mi> </msub> <msup> <mrow> <mo>|</mo> </mrow> <mn>2</mn> </msup> </mrow> </semantics></math> via fitting models <math display="inline"><semantics> <msub> <mi>A</mi> <mi>ATS</mi> </msub> </semantics></math> and <math display="inline"><semantics> <msub> <mi>A</mi> <mi>EIT</mi> </msub> </semantics></math> with different Coulomb interaction strength <math display="inline"><semantics> <mi>λ</mi> </semantics></math>. (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>=</mo> <mn>6</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>36</mn> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mrow> <mi>Hz</mi> <mo>/</mo> <msup> <mi mathvariant="normal">m</mi> <mn>2</mn> </msup> </mrow> </semantics></math>, with a good fit to <math display="inline"><semantics> <mrow> <msub> <mi>A</mi> <mi>ATS</mi> </msub> <mrow> <mo>(</mo> <mn>0.0337</mn> <mo>,</mo> <mo>−</mo> <mn>0.1526</mn> <mo>,</mo> <mn>0.0331</mn> <mo>,</mo> <mn>0.0140</mn> <mo>,</mo> <mn>0.0143</mn> <mo>)</mo> </mrow> </mrow> </semantics></math>. (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>λ</mi> <mo>=</mo> <mn>1.2</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>37</mn> </msup> </mrow> </semantics></math><math display="inline"><semantics> <mrow> <mi>Hz</mi> <mo>/</mo> <msup> <mi mathvariant="normal">m</mi> <mn>2</mn> </msup> </mrow> </semantics></math>, with a good fit to <math display="inline"><semantics> <mrow> <msub> <mi>A</mi> <mi>ATS</mi> </msub> <mrow> <mo>(</mo> <mn>0.0264</mn> <mo>,</mo> <mo>−</mo> <mn>0.1944</mn> <mo>,</mo> <mn>0.0268</mn> <mo>,</mo> <mn>0.0358</mn> <mo>,</mo> <mn>0.0349</mn> <mo>)</mo> </mrow> </mrow> </semantics></math>.</p>
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29 pages, 8599 KiB  
Article
Remote Sensing and Field Measurements for the Analysis of the Thermal Environment in the “Bosco Verticale” Area in Milan City
by Georgios Kalogeropoulos, Julia Tzortzi and Argiro Dimoudi
Land 2024, 13(2), 182; https://doi.org/10.3390/land13020182 - 3 Feb 2024
Cited by 1 | Viewed by 1475
Abstract
The trend of urbanization nowadays has caused serious issues related to climate. One of the most important ones is that of the ‘Urban Heat Island (UHI)’ and it occurs in major cities throughout the world. The most important categories, and therefore the most [...] Read more.
The trend of urbanization nowadays has caused serious issues related to climate. One of the most important ones is that of the ‘Urban Heat Island (UHI)’ and it occurs in major cities throughout the world. The most important categories, and therefore the most studied ones, are the canopy urban heat island (CUHI) and surface heat island (SUHI). The aim and the novelty of the current study was to assess different remote sensing approaches to detect the thermal environment of an open area inside a large city. The study was undertaken in an urban area with green spaces, in the Bosco Verticale area in the city of Milan, during the spring and summer period of 2021. The area is characterized by different types of cover materials, which were investigated in terms of surface temperature under shaded and non-shaded conditions. Both field measurements and remote sensing techniques were applied. Remote sensing techniques included downscaling techniques and the usage of different split-window algorithms applied on the Landsat8 satellite sensor data. The land surface temperature (LST) extracted from remote sensing methods was compared with the surface temperature derived from in situ measurements. For the needs of the study, both in situ measurements and the collection of meteorological data from different fixed meteorological stations throughout the city of Milan were carried out. The results revealed the significance of greenery presence inside the urban environment, as a comparison of the meteorological data across the urban area of Milan showed that the areas with a low presence of greenery were found to be warmer than those with a higher presence of green elements. Concerning the field measurements in the study area, the results showed a significant reduction in both surface and air temperature in shaded places. On the other hand, the presence of conventional artificial materials in sunny areas led to relatively high values of both surface and air temperature. The downscaling method showed satisfying results in terms of average LST values; however, some discrepancies appeared in terms of the RMSE index. The application of split-window algorithms has shown that some forms of the ‘Generalized split-window algorithm’ and some forms of the ‘Jimenez-Munoz algorithm’ presented better performance among the studied algorithms. Comparing the LST values derived from the most representative algorithm, the ‘Du, Wan algorithm’, with those derived from downscaling methods, it was found to be quite close. However, under shaded conditions, the results derived from the ‘Split-window algorithm’ were found to be more precise. The application of remote sensing techniques in microscale in urban regions should be further studied in future, as they could be an essential tool for observing microclimatic conditions in urban areas and on building scale. Full article
(This article belongs to the Section Land – Observation and Monitoring)
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<p>(<b>a</b>) Satellite view of the study area (QGIS). (<b>b</b>) Pavement concrete tiles (personal photo). (<b>c</b>) Narrow sand roads (personal photo). (<b>d</b>) Paved road (personal photo). (<b>e</b>) Grass (personal photo). (<b>f</b>) Narrow concrete roads (personal photo). (<b>g</b>) Rubber (personal photo).</p>
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<p>(<b>a</b>) Satellite view of the study area (QGIS). (<b>b</b>) Pavement concrete tiles (personal photo). (<b>c</b>) Narrow sand roads (personal photo). (<b>d</b>) Paved road (personal photo). (<b>e</b>) Grass (personal photo). (<b>f</b>) Narrow concrete roads (personal photo). (<b>g</b>) Rubber (personal photo).</p>
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<p>(<b>a</b>) The cover-type materials in the study area. (<b>b</b>) The measurement points (1–14) in the study area. (<b>c</b>) Weather stations’ locations in the city (QGIS).</p>
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<p>(<b>a</b>) The cover-type materials in the study area. (<b>b</b>) The measurement points (1–14) in the study area. (<b>c</b>) Weather stations’ locations in the city (QGIS).</p>
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<p>Flowchart of the downscaling technique of the LST images from 1000 m spatial resolution (MODIS) to 10 m (Sentinel-2).</p>
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<p>Flowchart for the downscaling technique of the LST images from 1000 m spatial resolution (MODIS) to 30 m (Landsat8).</p>
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<p>Average hourly temperature values in both shaded and exposed-to-the-sun areas: (<b>a</b>) surface temperature with IR instrument; (<b>b</b>) surface temperature with TC instrument; (<b>c</b>) air temperature with IR instrument.</p>
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<p>Average hourly temperature values in both shaded and exposed-to-the-sun areas: (<b>a</b>) surface temperature with IR instrument; (<b>b</b>) surface temperature with TC instrument; (<b>c</b>) air temperature with IR instrument.</p>
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<p>(<b>a</b>) Air temperature and (<b>b</b>) Relative humidity distribution in relation to the NVDI index of meteorological stations’ location areas.</p>
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<p>Linear correlation between: (<b>a</b>) downscaled and IR-measured surface temperature values; (<b>b</b>) downscaled and TC-measured surface temperature values.</p>
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<p>Investigation of the downscaled LST values in different material surface areas: (<b>a</b>) pavement tile; (<b>b</b>) sand; (<b>c</b>) grass; (<b>d</b>) rubber; (<b>e</b>) concrete.</p>
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<p>Investigation of the downscaled LST values in relation to (<b>a</b>) sun exposure; (<b>b</b>) albedo coefficient.</p>
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<p>Correlation between land surface temperature derived from the ‘Du, Wan algorithm’ and surface temperature acquired from: (<b>a</b>) IR instrument; (<b>b</b>) TC instrument.</p>
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<p>Investigation of the LST values with different materials: (<b>a</b>) pavement tiles; (<b>b</b>) sand; (<b>c</b>) grass; (<b>d</b>) rubber; (<b>e</b>) concrete.</p>
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<p>Investigation of the LST values in relation to (<b>a</b>) sun exposure; (<b>b</b>) albedo coefficient.</p>
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<p>Root mean square error index (RMSE) for the applied split-window algorithms concerning (<b>a</b>) pavement tile areas; (<b>b</b>) sand areas; (<b>c</b>) grass areas; (<b>d</b>) rubber areas; (<b>e</b>) concrete areas.</p>
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<p>Root mean square error index (RMSE) for the applied split-window algorithms concerning (<b>a</b>) pavement tile areas; (<b>b</b>) sand areas; (<b>c</b>) grass areas; (<b>d</b>) rubber areas; (<b>e</b>) concrete areas.</p>
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<p>Root mean square error index (RMSE) for the applied split-window algorithms concerning (<b>a</b>) pavement tile areas; (<b>b</b>) sand areas; (<b>c</b>) grass areas; (<b>d</b>) rubber areas; (<b>e</b>) concrete areas.</p>
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<p>(<b>a</b>) Correlation between land surface temperature derived from the combined split-window algorithms and surface temperature acquired from: (<b>a</b>) IR instrument (<b>b</b>) TC instrument.</p>
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<p>Spatial distribution of surface temperature as derived from combined split-window algorithms in: (<b>a</b>) grass areas; (<b>b</b>) sand areas; (<b>c</b>) pavement areas; (<b>d</b>) concrete areas; (<b>e</b>) rubber areas.</p>
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17 pages, 2311 KiB  
Article
A Novel Respiratory Rate Estimation Algorithm from Photoplethysmogram Using Deep Learning Model
by Wee Jian Chin, Ban-Hoe Kwan, Wei Yin Lim, Yee Kai Tee, Shalini Darmaraju, Haipeng Liu and Choon-Hian Goh
Diagnostics 2024, 14(3), 284; https://doi.org/10.3390/diagnostics14030284 - 28 Jan 2024
Cited by 2 | Viewed by 1987
Abstract
Respiratory rate (RR) is a critical vital sign that can provide valuable insights into various medical conditions, including pneumonia. Unfortunately, manual RR counting is often unreliable and discontinuous. Current RR estimation algorithms either lack the necessary accuracy or demand extensive window sizes. In [...] Read more.
Respiratory rate (RR) is a critical vital sign that can provide valuable insights into various medical conditions, including pneumonia. Unfortunately, manual RR counting is often unreliable and discontinuous. Current RR estimation algorithms either lack the necessary accuracy or demand extensive window sizes. In response to these challenges, this study introduces a novel method for continuously estimating RR from photoplethysmogram (PPG) with a reduced window size and lower processing requirements. To evaluate and compare classical and deep learning algorithms, this study leverages the BIDMC and CapnoBase datasets, employing the Respiratory Rate Estimation (RRest) toolbox. The optimal classical techniques combination on the BIDMC datasets achieves a mean absolute error (MAE) of 1.9 breaths/min. Additionally, the developed neural network model utilises convolutional and long short-term memory layers to estimate RR effectively. The best-performing model, with a 50% train–test split and a window size of 7 s, achieves an MAE of 2 breaths/min. Furthermore, compared to other deep learning algorithms with window sizes of 16, 32, and 64 s, this study’s model demonstrates superior performance with a smaller window size. The study suggests that further research into more precise signal processing techniques may enhance RR estimation from PPG signals. Full article
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<p>The process of classical algorithm and deep learning algorithm.</p>
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<p>Respiratory signal extraction.</p>
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<p>Deep learning algorithm flow chart.</p>
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<p>CNN-LSTM neural network architecture.</p>
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<p>Prediction loss versus epoch train with a 210 window size.</p>
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<p>Normal signal (<b>Left</b>); fluctuation signal (<b>Right</b>).</p>
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