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Search Results (573)

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Keywords = FY-4A

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19 pages, 6344 KiB  
Article
Evaluation of Fengyun-4B Satellite Temperature Profile Products Using Radiosonde Observations and ERA5 Reanalysis over Eastern Tibetan Plateau
by Yuhao Wang, Xiaofei Wu, Haoxin Zhang, Hong-Li Ren and Kaiqing Yang
Remote Sens. 2024, 16(22), 4155; https://doi.org/10.3390/rs16224155 - 7 Nov 2024
Viewed by 457
Abstract
The latest-generation geostationary meteorological satellite, Fengyun-4B (FY-4B), equipped with the Geostationary Interferometric Infrared Sounder (GIIRS), offers high-spatiotemporal-resolution three-dimensional temperature structures. Its deployment serves as a critical complement to atmospheric temperature profile (ATP) observation in the Tibetan Plateau (TP). Based on radiosonde observation (RAOB) [...] Read more.
The latest-generation geostationary meteorological satellite, Fengyun-4B (FY-4B), equipped with the Geostationary Interferometric Infrared Sounder (GIIRS), offers high-spatiotemporal-resolution three-dimensional temperature structures. Its deployment serves as a critical complement to atmospheric temperature profile (ATP) observation in the Tibetan Plateau (TP). Based on radiosonde observation (RAOB) and the fifth-generation ECMWF global climate atmospheric reanalysis (ERA5), this study validates the availability and representativeness of FY-4B/GIIRS ATP products in the eastern TP region. Due to the issue of satellite zenith, this study focuses solely on examining the eastern TP region. Under a clear sky, FY-4B/GIIRS ATP exhibits good consistency with RAOB compared to cloudy conditions, with an average root mean square error (RMSE) of 2.57 K. FY-4B/GIIRS tends to underestimate temperatures in the lower layers while overestimating temperatures in the upper layers. The bias varies across seasons. Except for summer, the horizontal and vertical bias distribution patterns are similar, though there are slight differences in values. Despite the presence of bias, FY-4B/GIIRS ATP maintains a good consistency with observations and reanalysis data, indicating commendable product quality. These results demonstrate that it can play a vital role in augmenting the ATP observation network limited by sparse radiosonde stations in the eastern TP, offering crucial data support for numerical weather prediction, weather monitoring, and related meteorological research in this region. Full article
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<p>(<b>a</b>) Distribution map of the nine RAOB stations (red triangles) over the TP. (<b>b</b>) The FY-4B/GIIRS observation pixels (blue dots) for the Garze station in the MW method at 12 UTC on 17 January 2023. The color shading represents the elevation (units, m), and the red line in (<b>a</b>) indicates the border of the TP.</p>
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<p>RMSE (green bars) and the number of effective data (orange bars) for the IDW and the MW method at nine RAOB stations.</p>
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<p>The percentages of the FY-4B/GIIRS ATP products quality flags during clear sky (green bars) and cloudy sky (orange bars).</p>
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<p>The average ATP observed by FY-4B/GIIRS (blue line) and RAOB (orange line) and the average bias of FY-4B/GIIRS referring to RAOB (cyan line with triangles) for (<b>a</b>–<b>i</b>) 00 UTC and (<b>j</b>–<b>r</b>) 12 UTC. The light cyan shading accompanied with the bias line indicates one standard variation of the bias.</p>
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<p>Scatter plot of FY-4B/GIIRS ATP versus the RAOB ATP (black dashed line represents the 1:1 line, red line represents regression line). (<b>a</b>–<b>i</b>) represent nine RAOB stations arranged in order of elevation from lowest to highest.</p>
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<p>Same as <a href="#remotesensing-16-04155-f005" class="html-fig">Figure 5</a>, but for ERA5 ATP versus the RAOB ATP. (<b>a</b>–<b>i</b>) represent nine RAOB stations arranged in order of elevation from lowest to highest.</p>
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<p>(<b>a</b>) Satellite zenith angle (shaded, degree) of FY-4B/GIIRS at 11:00 UTC on 17 January 2024 and the annual mean troposphere temperature (<b>b</b>) before and (<b>c</b>) after filtering based on the satellite zenith angle of 60° as the red line shown in (<b>b</b>). The black line in (<b>a</b>–<b>c</b>) indicates the TP region. Points A and B in (<b>b</b>) are the intersection points of the contour line of 60° and the borderline of the TP region in (<b>a</b>).</p>
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<p>The spatial distribution of annual mean temperature bias between FY-4B/GIIRS and ERA5 ATP: (<b>a</b>) horizontal distribution of troposphere (600–100 hPa) averaged bias and (<b>b</b>) vertical distribution of regional averaged bias for the blue box in (<b>a</b>). The shading in (<b>b</b>) indicates one STD range of the bias.</p>
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<p>Scatter plot of seasonal average FY-4B/GIIRS ATP versus ERA5 ATP for each of the four seasons among the eastern TP, the black dashed line represents the 1:1 line, and the red line represents the regression line. (<b>a</b>–<b>d</b>) correspond to winter, spring, summer, and autumn, respectively.</p>
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<p>The horizontal distribution of annual mean troposphere (600–100 hPa) averaged temperature bias between FY-4B/GIIRS and ERA5 ATP. (<b>a</b>–<b>d</b>) correspond to winter, spring, summer, and autumn, respectively.</p>
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<p>The vertical distribution of annual mean regional averaged temperature bias between FY-4B/GIIRS and ERA5 ATP for the blue box in <a href="#remotesensing-16-04155-f008" class="html-fig">Figure 8</a>a. The shading indicates one STD range of the bias. (<b>a</b>–<b>d</b>) correspond to winter, spring, summer, and autumn, respectively.</p>
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24 pages, 6494 KiB  
Article
Reconstruction of Fine-Spatial-Resolution FY-3D-Based Vegetation Indices to Achieve Farmland-Scale Winter Wheat Yield Estimation via Fusion with Sentinel-2 Data
by Xijia Zhou, Tao Wang, Wei Zheng, Mingwei Zhang and Yuanyuan Wang
Remote Sens. 2024, 16(22), 4143; https://doi.org/10.3390/rs16224143 - 6 Nov 2024
Viewed by 540
Abstract
The spatial resolution (250–1000 m) of the FY-3D MERSI is too coarse for agricultural monitoring at the farmland scale (20–30 m). To achieve the winter wheat yield (WWY) at the farmland scale, based on FY-3D, a method framework is developed in this work. [...] Read more.
The spatial resolution (250–1000 m) of the FY-3D MERSI is too coarse for agricultural monitoring at the farmland scale (20–30 m). To achieve the winter wheat yield (WWY) at the farmland scale, based on FY-3D, a method framework is developed in this work. The enhanced deep convolutional spatiotemporal fusion network (EDCSTFN) was used to perform a spatiotemporal fusion on the 10 day interval FY-3D and Sentinel-2 vegetation indices (VIs), which were compared with the enhanced spatial and temporal adaptive reflectance fusion model (ESTARFM). In addition, a BP neural network was built to calculate the farmland-scale WWY based on the fused VIs, and the Aqua MODIS gross primary productivity product was used as ancillary data for WWY estimation. The results reveal that both the EDCSTFN and ESTARFM achieve satisfactory precision in the fusion of the Sentinel-2 and FY-3D VIs; however, when the period of spatiotemporal data fusion is relatively long, the EDCSTFN can achieve greater precision than ESTARFM. Finally, the WWY estimation results based on the fused VIs show remarkable correlations with the WWY data at the county scale and provide abundant spatial distribution details about the WWY, displaying great potential for accurate farmland-scale WWY estimations based on reconstructed fine-spatial-temporal-resolution FY-3D data. Full article
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<p>Overview of the study region: (<b>a</b>) location of the Weihe Plain; (<b>b</b>) FY-3D false colour composite image for 3 May 2020; and (<b>c</b>) locations of the county-scale WWY data points used in the WWY estimation.</p>
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<p>Flowchart of the 10 day interval VI imagery reconstruction and farmland-scale WWY estimation.</p>
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<p>Flowchart of farmland-scale WWY estimation: (<b>a</b>) Y estimation model based on the cumulative GPP; and (<b>b</b>) farmland-scale Y estimation model based on multiple parameters.</p>
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<p>Results of the consistency analysis of the Sentinel-2 and FY-3D VIs: (<b>a</b>) R<sup>2</sup> values between the aggregated Sentinel-2 VI imagery and the FY-3D VI imagery at an SR of 250 m; and (<b>b</b>) average deviations and RMSE values of the fitting results between the aggregated Sentinel-2 VI imagery and FY-3D VI imagery. The error line in (<b>b</b>) denotes the RMSE of the fitting results.</p>
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<p>EVI at each WW growing stage from 2020 to 2022.</p>
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<p>Y estimation model based on the cumulative GPP for the main WW growing period and the Y estimation precision evaluation results in 2020 and 2021. The dotted lines in the figures denote the fitted linear functions, which are close to the diagonal solid lines, indicating that the systematic deviation in the Y estimation results is small. (<b>a</b>) Linear regression model between the cumulative GPP data for the main WW growing period and the county-scale WWY from 2014 to 2018, (<b>b</b>) linear regression results between the WWY estimation results from 2020 based on the cumulative GPP and county-scale Y statistical data, and (<b>c</b>) linear regression results between the WWY estimation results in 2021 based on the cumulative GPP and county-scale Y statistical data.</p>
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<p>WWY estimation results for 2020 to 2022 based on the MODIS cumulative GPP data.</p>
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<p>Farmland-scale WWY estimation results for the Weihe Plain from 2020 to 2022 based on multiple parameters.</p>
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<p>Linear regression results between the farmland-scale WWY estimation results and the Y statistical data in 2020 and 2021. The dotted lines in the figures denote the fitted linear functions, which are close to the diagonal solid lines, indicating that the systematic deviation of the Y estimation results is small.</p>
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18 pages, 10136 KiB  
Article
The Combination Application of FY-4 Satellite Products on Typhoon Saola Forecast on the Sea
by Chun Yang, Bingying Shi and Jinzhong Min
Remote Sens. 2024, 16(21), 4105; https://doi.org/10.3390/rs16214105 - 2 Nov 2024
Viewed by 604
Abstract
Satellite data play an irreplaceable role in global observation data systems. Effective comprehensive application of satellite products will inevitably improve numerical weather prediction. FengYun-4 (FY-4) series satellites can provide not only radiance data but also retrieval data with high temporal and spatial resolutions. [...] Read more.
Satellite data play an irreplaceable role in global observation data systems. Effective comprehensive application of satellite products will inevitably improve numerical weather prediction. FengYun-4 (FY-4) series satellites can provide not only radiance data but also retrieval data with high temporal and spatial resolutions. To evaluate the potential benefits of the combination application of FY-4 Advanced Geostationary Radiance Imager (AGRI) products on Typhoon Saola analysis and forecast, two group of experiments are set up with the Weather Research and Forecasting model (WRF). Compared with the benchmark experiment, whose sea surface temperature (SST) is from the National Centers for Environmental Prediction (NCEP) reanalysis data, the SST replacement experiments with FY-4 A/B SST products significantly improve the track and precipitation forecast, especially with the FY-4B SST product. Based on the above results, AGRI clear-sky and all-sky assimilations with FY-4B SST are implemented with a self-constructed AGRI assimilation module. The results show that the AGRI all-sky assimilation experiment can obtain better analyses and forecasts. Furthermore, it is proven that the combination application of AGRI radiance and SST products is beneficial for typhoon prediction. Full article
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<p>The weighting function of channels 9-14 of FY-4A AGRI with RTTOV and the U.S. standard atmospheric profile.</p>
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<p>(<b>a</b>) The evolution of the best track, (<b>b</b>) the central sea level pressure (units: hPa) and maximum wind (units: knot) for Typhoon Saola from 0000 UTC 22 August to 1200 UTC 3 September 2023.</p>
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<p>Initial SST (units: K) from (<b>a</b>) <span class="html-italic">CON</span>, (<b>b</b>) SSTA, and (<b>c</b>) SSTB.</p>
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<p>The predicted (<b>a</b>) track, (<b>b</b>) track errors (units: km), (<b>c</b>) CSLP errors (units: hPa), and (<b>d</b>) MW errors (units: knot) in <span class="html-italic">CON</span> (light blue lines), SSTA (red lines), and SSTB (light green lines) are compared to the JMA best track estimates (blue lines) from 0600 UTC 30 August to 1200 UTC 2 September 2023.</p>
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<p>Time series of the U and V components of average steering flow (units: m/s) from 0600 UTC 30 August to 1200 UTC 2 September 2023.</p>
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<p>The 24 h accumulated precipitation (units: mm) from 1200 UTC 1 September to 1200 UTC 2 September 2023 of (<b>a</b>) the Micaps observation; (<b>b</b>) the interpolated Micaps observation with a horizontal resolution of 0.5° × 0.5°; (<b>c</b>) <span class="html-italic">CON</span>; (<b>d</b>) SSTA; and (<b>e</b>) SSTB. The dots with different colors in (<b>a</b>) represent different accumulated precipitation, as shown in the color bar.</p>
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<p>Performance diagram for the 24 h accumulated precipitation for the <span class="html-italic">CON</span> (light blue), SSTA (red), and SSTB (light green) with a threshold of (<b>a</b>) 0.01 mm; (<b>b</b>) 10 mm; (<b>c</b>) 25 mm; (<b>d</b>) 50 mm; and (<b>e</b>) 75 mm from 1200 UTC 1 September to 1200 UTC 2 September 2023.</p>
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<p>(<b>a</b>,<b>b</b>) The AGRI observed brightness temperature (units: K) distributions at channel 9 after QC in (<b>a</b>) CLR and (<b>b</b>) ALL valid at 1500 UTC 30 August 2023. (<b>c</b>) The counts of assimilated AGRI observations at channel 9 in ALL and CLR with different cloud mask types every 3 hr from 0900 UTC 30 August to 1500 UTC 30 August 2023.</p>
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<p>The IPs (units: %) over <span class="html-italic">CON</span> of individual experiments every 3 h from 0900 UTC 30 August to 1500 UTC 30 August 2023 in (<b>a</b>) <span class="html-italic">CTTs</span> and (<b>b</b>) agreements on sky conditions.</p>
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<p>The predicted (<b>a</b>) track, (<b>b</b>) track errors (units: km), (<b>c</b>) CSLP errors (units: hPa), and (<b>d</b>) MW errors (units: knot) in <span class="html-italic">CON</span> (light blue lines), SSTB (light green lines), CLR (light yellow lines), ALL (orange lines), CLR + SSTB (light red lines), and ALL + SSTB (brown lines) are compared to the JMA best track estimates (blue lines) from 1800 UTC 30 August to 1200 UTC 2 September 2023.</p>
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<p>The (<b>a</b>) U and (<b>b</b>) V components of steering flows (units: m/s) from 700 to 200 hPa with an interval of 50 hPa in individual experiments at 0600 UTC 1 September 2023.</p>
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<p>The same as <a href="#remotesensing-16-04105-f007" class="html-fig">Figure 7</a> but for (<b>a</b>) the interpolated Micaps observation with a horizontal resolution of 0.5° × 0.5°; (<b>b</b>) <span class="html-italic">CON</span>; (<b>c</b>) CLR; (<b>d</b>) ALL; (<b>e</b>) SSTB; (<b>f</b>) CLR + SSTB; and (<b>g</b>) ALL + SSTB.</p>
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<p>The same as <a href="#remotesensing-16-04105-f006" class="html-fig">Figure 6</a> but for <span class="html-italic">CON</span> (light blue), SSTB (light green), CLR (light yellow), ALL (orange), CLR + SSTB (light red), and ALL + SSTB (brown) with a threshold of (<b>a</b>) 0.01 mm; (<b>b</b>) 10 mm; (<b>c</b>) 25 mm; (<b>d</b>) 50 mm; and (<b>e</b>) 75 mm.</p>
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20 pages, 5140 KiB  
Article
Distribution-Based Approach for Efficient Storage and Indexing of Massive Infrared Hyperspectral Sounding Data
by Han Li, Mingjian Gu, Guang Shi, Yong Hu and Mengzhen Xie
Remote Sens. 2024, 16(21), 4088; https://doi.org/10.3390/rs16214088 - 1 Nov 2024
Viewed by 441
Abstract
Hyperspectral infrared atmospheric sounding data, characterized by their high vertical resolution, play a crucial role in capturing three-dimensional atmospheric spatial information. The hyperspectral infrared atmospheric detectors HIRAS/HIRAS-II, mounted on the FY3D/EF satellite, have established an initial global coverage network for atmospheric sounding. The [...] Read more.
Hyperspectral infrared atmospheric sounding data, characterized by their high vertical resolution, play a crucial role in capturing three-dimensional atmospheric spatial information. The hyperspectral infrared atmospheric detectors HIRAS/HIRAS-II, mounted on the FY3D/EF satellite, have established an initial global coverage network for atmospheric sounding. The collaborative observation approach involving multiple satellites will improve both the coverage and responsiveness of data acquisition, thereby enhancing the overall quality and reliability of the data. In response to the increasing number of channels, the rapid growth of data volume, and the specific requirements of multi-satellite joint observation applications with infrared hyperspectral sounding data, this paper introduces an efficient storage and indexing method for infrared hyperspectral sounding data within a distributed architecture for the first time. The proposed approach, built on the Kubernetes cloud platform, utilizes the Google S2 discrete grid spatial indexing algorithm to establish a grid-based hierarchical model for unified metadata-embedded documents. Additionally, it optimizes the rowkey design using the BPDS model, thereby enabling the distributed storage of data in HBase. The experimental results demonstrate that the query efficiency of the Google S2 grid-based embedded document model is superior to that of the traditional flat model, achieving a query time that is only 35.6% of the latter for a dataset of 5 million records. Additionally, this method exhibits better data distribution characteristics within the global grid compared to the H3 algorithm. Leveraging the BPDS model, the HBase distributed storage system adeptly balances the node load and counteracts the detrimental effects caused by the accumulation of time-series remote sensing images. This architecture significantly enhances both storage and query efficiency, thus laying a robust foundation for forthcoming distributed computing. Full article
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<p>Illustration of ground field-of-view arrangement for the HIRAS series detector [<a href="#B36-remotesensing-16-04088" class="html-bibr">36</a>,<a href="#B37-remotesensing-16-04088" class="html-bibr">37</a>].</p>
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<p>The system architecture for the efficient storage and indexing of hyperspectral infrared sounding data.</p>
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<p>A schematic diagram of the design structure of rowkeys.</p>
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<p>The table structure of infrared hyperspectral sounding data in HBase.</p>
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<p>Collections on MongoDB cluster.</p>
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<p>The relationship between coding level and grid resolution.</p>
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<p>Comparison of loading times by various index methods.</p>
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<p>Comparison of storage structure in MongoDB.</p>
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<p>Grid-based heatmap visualization of different methods: (<b>a</b>) Google S2 algorithm; (<b>b</b>) H3 algorithm.</p>
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<p>The histogram of pixels of grids in different methods: (<b>a</b>) Google S2 algorithm; (<b>b</b>) H3 algorithm.</p>
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<p>Query time and storage time are utilized as comparative metrics to assess performance by different methods: (<b>a</b>) storage time and (<b>b</b>) query time.</p>
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<p>Distribution of regions in different models: (<b>a</b>) DP model, (<b>b</b>) FP model, and (<b>c</b>) BPDS model.</p>
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14 pages, 4553 KiB  
Article
Peptide-Based Rapid and Selective Detection of Mercury in Aqueous Samples with Micro-Volume Glass Capillary Fluorometer
by Marta Sosnowska, Emil Pitula, Monika Janik, Piotr Bruździak, Mateusz Śmietana, Marcin Olszewski, Dawid Nidzworski and Beata Gromadzka
Biosensors 2024, 14(11), 530; https://doi.org/10.3390/bios14110530 - 1 Nov 2024
Viewed by 678
Abstract
Mercury, a toxic heavy metal produced through both natural and anthropogenic processes, is found in all of Earth’s major systems. Mercury’s bioaccumulation characteristics in the human body have a significant impact on the liver, kidneys, brain, and muscles. In order to detect Hg [...] Read more.
Mercury, a toxic heavy metal produced through both natural and anthropogenic processes, is found in all of Earth’s major systems. Mercury’s bioaccumulation characteristics in the human body have a significant impact on the liver, kidneys, brain, and muscles. In order to detect Hg2+ ions, a highly sensitive and specific fluorescent biosensor has been developed using a novel, modified seven amino acid peptide, FY7. The tyrosine ring in the FY7 peptide sequence forms a 2:1 complex with Hg2+ ions that are present in the water-based sample. As a result, the peptide’s fluorescence emission decreases with higher concentrations of Hg2+. The FY7 peptide’s performance was tested in the presence of Hg2+ ions and other metal ions, revealing its sensitivity and stability despite high concentrations. Conformational changes to the FY7 structure were confirmed by FTIR studies. Simultaneously, we designed a miniaturized setup to support an in-house-developed micro-volume capillary container for volume fluorometry measurements. We compared and verified the results from the micro-volume system with those from the commercial setup. The micro-volume capillary system accommodated only 2.9 µL of sample volume, allowing for rapid, sensitive, and selective detection of toxic mercury (II) ions as low as 0.02 µM. Full article
(This article belongs to the Special Issue Micro-nano Optic-Based Biosensing Technology and Strategy)
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<p>The selectivity of FY7 peptide (5 µM) for Hg<sup>2+</sup> ions in MES buffer solutions (50 mM, pH 5.65). Concentrations of all metal ions were at 0.5, 5.0, and 10 µM. F0 and F were the fluorescence intensities of FY7 in the absence and presence of metal ions, respectively. Error bars represent the standard deviation of three independent measurements.</p>
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<p>(<b>A</b>) Fluorescence emission spectra of FY7 (5 µM) upon the addition of Hg<sup>2+</sup> ions (0–10 µM) in MES buffer solutions (50 mM, pH 5.65). (<b>B</b>) Plots of fluorescence intensity of FY7 as a function of Hg<sup>2+</sup> ions concentration (µM). Error bars represent the standard deviation of three independent measurements.</p>
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<p>Fluorescence response of FY7 (5 µM) to Hg<sup>2+</sup> (0.5 equiv.) in the presence of various metal ions (5 equiv.) in MES buffer solutions (50 mM, pH 5.65). Error bars represent the standard deviation of three independent measurements.</p>
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<p>Job’s plot for determining the stoichiometry of FY7 and Hg<sup>2+</sup> in MES buffer solutions (50 mM, pH 5.65), the total concentration of FY7 and Hg<sup>2+</sup> was 5 µM. Error bars represent the standard deviation of three independent measurements.</p>
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<p>(<b>a</b>) Raw spectra of FY7 peptide (blue line) and FY7–Hg<sup>2+</sup> complex (orange line) in the amide bands region of the peptide. (<b>b</b>) Spectra after water vapor correction. (<b>c</b>) Spectra after removing the contribution of D<sub>2</sub>O in the studied range. (<b>d</b>) Second derivatives of FTIR spectra. Please see a description in the text.</p>
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<p>Schematic representation of an experimental setup for micro-volume capillary measurements.</p>
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<p>(<b>A</b>) The selectivity of the FY7 peptide (50 µM) for Hg<sup>2+</sup> ions (2.5 µM) in MES buffer solutions (50 mM, pH 5.65) measured in a low-volume fluorescence setup. Concentrations of all metal ions were at 0.5, 5.0, and 10 µM. F0 and F were the fluorescence intensities of FY7 in the absence and presence of metal ions, respectively. (<b>B</b>) Plot of fluorescence intensity of FY7 as a function of Hg<sup>2+</sup> ion concentration (µM); the dotted line is an approximation used for LOD estimation.</p>
Full article ">Figure 7 Cont.
<p>(<b>A</b>) The selectivity of the FY7 peptide (50 µM) for Hg<sup>2+</sup> ions (2.5 µM) in MES buffer solutions (50 mM, pH 5.65) measured in a low-volume fluorescence setup. Concentrations of all metal ions were at 0.5, 5.0, and 10 µM. F0 and F were the fluorescence intensities of FY7 in the absence and presence of metal ions, respectively. (<b>B</b>) Plot of fluorescence intensity of FY7 as a function of Hg<sup>2+</sup> ion concentration (µM); the dotted line is an approximation used for LOD estimation.</p>
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<p>Fluorescence response of FY7 (50 µM) to Hg<sup>2+</sup> (2.5 µM) in the presence of various metal ions (10 µM) in MES buffer solutions (50 mM, pH 5.65) measured in a low-volume fluorescence setup.</p>
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24 pages, 7524 KiB  
Article
A Study on Typhoon Center Localization Based on an Improved Spatio-Temporally Consistent Scale-Invariant Feature Transform and Brightness Temperature Perturbations
by Chaoyu Yan, Jie Guang, Zhengqiang Li, Gerrit de Leeuw and Zhenting Chen
Remote Sens. 2024, 16(21), 4070; https://doi.org/10.3390/rs16214070 - 31 Oct 2024
Viewed by 608
Abstract
Extreme weather events like typhoons have become more frequent due to global climate change. Current typhoon monitoring methods include manual monitoring, mathematical morphological methods, and artificial intelligence. Manual monitoring is accurate but labor-intensive, while AI offers convenience but requires accuracy improvements. Mathematical morphology [...] Read more.
Extreme weather events like typhoons have become more frequent due to global climate change. Current typhoon monitoring methods include manual monitoring, mathematical morphological methods, and artificial intelligence. Manual monitoring is accurate but labor-intensive, while AI offers convenience but requires accuracy improvements. Mathematical morphology methods, such as brightness temperature perturbation (BTP) and a spatio-temporally consistent (STC) Scale-Invariant Feature Transform (SIFT), remain mainstream for typhoon positioning. This paper enhances BTP and STC SIFT methods for application to Fengyun 4A (FY-4A) Advanced Geosynchronous Radiation Imager (AGRI) L1 data, incorporating parallax correction for more accurate surface longitude and latitude positioning. The applicability of these methods for different typhoon intensities and monitoring time resolutions is analyzed. Automated monitoring with one-hour observation intervals in the northwest Pacific region demonstrates high positioning accuracy, reaching 25 km or better when compared to best path data from the China Meteorological Administration (CMA). For 1 h remote sensing observations, BTP is more accurate for typhoons at or above typhoon intensity, while STC SIFT is more accurate for weaker typhoons. In the current era of a high temporal resolution of typhoon monitoring using geostationary satellites, the method presented in this paper can serve the national meteorological industry for typhoon monitoring, which is beneficial to national pre-disaster prevention work as well as global meteorological research. Full article
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<p>The yellow rectangular box represents the study area.</p>
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<p>Typhoon automatic center positioning process.</p>
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<p>Parallax correction geometry relationship model [<a href="#B32-remotesensing-16-04070" class="html-bibr">32</a>].</p>
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<p>The application of the typhoon detection algorithm to identify the typhoon cloud system over the northwest Pacific using FY-4A AGRI level 1 data on 6 November 2019, at 02:00 Beijing time (typhoon HL). (<b>a</b>) The initial data after projection conversion pre-processing, (<b>b</b>) the spatial distribution of the BT over the study area (unit: K), (<b>c</b>) the binarized image of the BT spatial distribution, and (<b>d</b>) further processing that shows the locations of candidate target cloud systems.</p>
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<p>The application of the typhoon detection algorithm to identify the typhoon cloud system over the northwest Pacific using FY-4A AGRI level 1 data on 6 November 2019, at 02:00 Beijing time (typhoon HL). (<b>a</b>) The initial data after projection conversion pre-processing, (<b>b</b>) the spatial distribution of the BT over the study area (unit: K), (<b>c</b>) the binarized image of the BT spatial distribution, and (<b>d</b>) further processing that shows the locations of candidate target cloud systems.</p>
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<p>The BT distribution of the typhoon cloud system using FY-4A AGRI level 1 data on 6 November 2019, at 02:00 Beijing time: the BT distribution of the target cloud system before (<b>a</b>) and after (<b>b</b>) parallax correction. (<b>c</b>) and (<b>d</b>) show details of the typhoon eye area before and after parallax correction, respectively.</p>
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<p>Results from the BTP typhoon localization algorithm applied to FY-4A AGRI level 1 data over the northwest Pacific on 6 November 2019, at 02:00 Beijing time (typhoon HL): (<b>a</b>) the longitudinal BT gradient near the typhoon eye area (unit: km); (<b>b</b>) latitudinal BT gradient near the typhoon eye area; (<b>c</b>) spatial distribution of BT divergence (unit: <math display="inline"><semantics> <mrow> <mi mathvariant="normal">N</mi> <mo>·</mo> <msup> <mrow> <mi mathvariant="normal">m</mi> </mrow> <mrow> <mo>−</mo> <mn>3</mn> </mrow> </msup> <mo>×</mo> <msup> <mrow> <mn>10</mn> </mrow> <mrow> <mn>7</mn> </mrow> </msup> </mrow> </semantics></math>); (<b>d</b>) spatial distribution of the BT curl (unit: <math display="inline"><semantics> <mrow> <mi mathvariant="normal">N</mi> <mo>·</mo> <msup> <mrow> <mi mathvariant="normal">m</mi> </mrow> <mrow> <mo>−</mo> <mn>3</mn> </mrow> </msup> <mo>×</mo> <msup> <mrow> <mn>10</mn> </mrow> <mrow> <mn>7</mn> </mrow> </msup> </mrow> </semantics></math>); (<b>e</b>) spatial distribution of BTP. The location of the typhoon as determined from the BTP distribution is indicated with a red + and the location of the typhoon center provided by CMA is indicated with a blue star.</p>
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<p>Results from the BTP typhoon localization algorithm applied to FY-4A AGRI level 1 data over the northwest Pacific on 6 November 2019, at 02:00 Beijing time (typhoon HL): (<b>a</b>) the longitudinal BT gradient near the typhoon eye area (unit: km); (<b>b</b>) latitudinal BT gradient near the typhoon eye area; (<b>c</b>) spatial distribution of BT divergence (unit: <math display="inline"><semantics> <mrow> <mi mathvariant="normal">N</mi> <mo>·</mo> <msup> <mrow> <mi mathvariant="normal">m</mi> </mrow> <mrow> <mo>−</mo> <mn>3</mn> </mrow> </msup> <mo>×</mo> <msup> <mrow> <mn>10</mn> </mrow> <mrow> <mn>7</mn> </mrow> </msup> </mrow> </semantics></math>); (<b>d</b>) spatial distribution of the BT curl (unit: <math display="inline"><semantics> <mrow> <mi mathvariant="normal">N</mi> <mo>·</mo> <msup> <mrow> <mi mathvariant="normal">m</mi> </mrow> <mrow> <mo>−</mo> <mn>3</mn> </mrow> </msup> <mo>×</mo> <msup> <mrow> <mn>10</mn> </mrow> <mrow> <mn>7</mn> </mrow> </msup> </mrow> </semantics></math>); (<b>e</b>) spatial distribution of BTP. The location of the typhoon as determined from the BTP distribution is indicated with a red + and the location of the typhoon center provided by CMA is indicated with a blue star.</p>
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<p>Typhoon center localization with the STC SIFT feature method using FY-4A AGRI level 1 data on 6 November 2019, at 02:00 Beijing time (typhoon HL): (<b>a</b>) feature point distributions in the extracted historical image (<b>left</b>) and the current image (<b>right</b>); (<b>b</b>) results of matching the remaining feature points after STC filtering and rotation uniform distribution filtering; (<b>c</b>) the comparison of the final positioning result (red +) with the typhoon center location provided by CMA (blue star).</p>
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<p>The comparison of the optimal paths of SD, HMN, HL, and HK determined using two typhoon localization methods, with the best path provided by CMA. The left column shows results from the BTP typhoon localization method and the right column shows results from the STC SIFT feature typhoon localization method for typhoons SD (<b>a</b>,<b>b</b>), HNM (<b>c</b>,<b>d</b>), HL (<b>e</b>,<b>f</b>), and HK (<b>g</b>,<b>h</b>). The average accuracy, from comparison with the CMA path, is indicated in each figure. The region outlined by blue lines delineates the portion of the typhoon characterized by lower intensity (before developing into typhoon intensity, TY). <a href="#remotesensing-16-04070-t004" class="html-table">Table 4</a> presents the typhoon localization accuracy for the blue-outlined area.</p>
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<p>The error analysis of different typhoon localization methods under various typhoon intensities. Panel (<b>a</b>) illustrates the error analysis for STC SIFT at different typhoon intensities; panel (<b>b</b>) shows the error analysis for BTP typhoon localization under varying intensities; and panel (<b>c</b>) depicts the error analysis for BTP localization without parallax correction across different typhoon intensities. The orange line represents the median error, while the green dashed line indicates the mean error. The top and bottom edges of each box correspond to the upper and lower quartiles of the error distribution, and the whiskers denote the maximum and minimum error values.</p>
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18 pages, 5420 KiB  
Article
Artificial Intelligence-Based Precipitation Estimation Method Using Fengyun-4B Satellite Data
by Nianqing Liu, Jianying Jiang, Dongyan Mao, Meng Fang, Yun Li, Bowei Han and Suling Ren
Remote Sens. 2024, 16(21), 4076; https://doi.org/10.3390/rs16214076 - 31 Oct 2024
Viewed by 492
Abstract
This paper proposes a novel precipitation estimation method based on FY-4B meteorological satellite data (FY-4B_AI). This method facilitates the spatiotemporal matching of 125 features derived from the multi-temporal and multi-channel data of the FY-4B satellite with precipitation data at stations. Subsequently, a precipitation [...] Read more.
This paper proposes a novel precipitation estimation method based on FY-4B meteorological satellite data (FY-4B_AI). This method facilitates the spatiotemporal matching of 125 features derived from the multi-temporal and multi-channel data of the FY-4B satellite with precipitation data at stations. Subsequently, a precipitation model was constructed using the light gradient boosting machine (LGBM) algorithm. A comparative analysis of FY-4B_AI and GPM/IMERG-L products for over 450 million station cases throughout 2023 revealed the following: (1) The results demonstrate that FY-4B_AI is more accurate than GPM/IMERG-L. Six of the eight evaluation indices exhibit superior performance for FY-4B_AI in comparison to GPM/IMERG-L. These indices include the mean absolute error (MAE), root mean square error (RMSE), relative error (RE), correlation coefficient (CC), probability of detection (POD), and critical success index (CSI). As for the MAE, the results are 1.67 (FY-4B_AI) and 1.92 (GPM/IMERG-L), respectively. The RMSEs are 3.68 and 4.07, respectively. The REs are 17.72% and 26.28%, respectively. The CCs are 0.44 and 0.36, respectively. The PODs are 61.84% and 47.31%, respectively. The CSIs are 0.30 and 0.27, respectively. However, with regard to the mean errors (MEs) and false alarm rates (FARs), FY-4B_AI (−0.88 and 62.85%, respectively) displays a slight degree of inferiority in comparison to GPM/IMERG-L (−0.80 and 62.21%, respectively). (2) An evaluation of two strong weather events to represent the spatial distribution of precipitation in different climatic zones revealed that both FY-4B_AI and GPM/IMERG-L are equally capable of accurately representing these phenomena, irrespective of whether the region in question is humid, as is the case in the southeast, or dry, as is the case in the northwest. Full article
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<p>Distribution of ground-based precipitation observation stations in mainland China (red dots) [<a href="#B21-remotesensing-16-04076" class="html-bibr">21</a>].</p>
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<p>Data processing flow and algorithm model for multi-temporal FY-4B meteorological satellite precipitation estimation product based on artificial intelligence.</p>
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<p>Monthly distribution of satellite−derived precipitation accuracy evaluation indices from January to December 2023.</p>
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<p>Monthly distribution of satellite−derived precipitation accuracy evaluation indices from January to December 2023.</p>
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<p>Yearly precipitation distribution map of China in 2023 (unit: mm) (cited from Figure 1.15 of the ‘China Climate Bulletin (2023)’).</p>
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<p>Overlay of FY-4B_AI, GPM/IMERG-L, ground station truth values, and infrared cloud images from 13:00 to 14:00 (UTC) on 18 June 2023.</p>
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<p>Overlay of FY-4B_AI, ground station truth values, and GPM/IMERG-L with infrared cloud images from 09:00 to 13:00 on 20 July 2023.</p>
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18 pages, 6070 KiB  
Article
Diurnal Cycles of Cloud Properties and Precipitation Patterns over the Northeastern Tibetan Plateau During Summer
by Bangjun Cao, Xianyu Yang, Yaqiong Lu, Jun Wen and Shixin Wang
Remote Sens. 2024, 16(21), 4059; https://doi.org/10.3390/rs16214059 - 31 Oct 2024
Viewed by 386
Abstract
In the context of rising temperatures and increasing humidity in Northwest China, substantial gaps remain in understanding the mechanisms of land–atmosphere cloud–precipitation coupling across the northeastern Tibetan Plateau (TP), Loess Plateau (LP), and Huangshui Valley (HV). This study addresses these gaps by investigating [...] Read more.
In the context of rising temperatures and increasing humidity in Northwest China, substantial gaps remain in understanding the mechanisms of land–atmosphere cloud–precipitation coupling across the northeastern Tibetan Plateau (TP), Loess Plateau (LP), and Huangshui Valley (HV). This study addresses these gaps by investigating cloud properties and precipitation patterns utilizing the Fengyun-4 Satellite Quantitative Precipitation Estimation Product (FY4A-QPE) and ERA5 datasets. We specifically focus on Lanzhou, a pivotal city within the LP, and Xining, which epitomizes the HV. Our findings reveal that diurnal variations in precipitation are significantly less pronounced in the eastern regions compared to northeastern TP. This discrepancy is attributed to marked diurnal fluctuations in convective available potential energy (CAPE) and wind shear between 200 and 500 hPa. While both cities share similar wind shear patterns and moisture transport directions, Xining benefits from enhanced snowmelt and effective water retention in surrounding mountains, resulting in higher precipitation levels. Conversely, Lanzhou suffers from moisture deficits, with dry, hot winds exacerbating the situation. Notably, precipitation in Xining is strongly correlated with CAPE, influenced by diurnal variability, and intensified by valley and lake–land breezes, which drive afternoon convection. In contrast, Lanzhou’s precipitation exhibits a weak relationship with CAPE, as even elevated values fail to generate significant cloud formation due to insufficient moisture. The ongoing trends of warming and humidification may lead to improved precipitation patterns, especially in the HV, with potential ecological benefits. However, concentrated rainfall during summer afternoons and midnights raises concerns regarding extreme weather events, highlighting the susceptibility of the HV to geological hazards. This research underscores the need to further explore the uncertainties inherent in precipitation dynamics in these regions. Full article
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Graphical abstract

Graphical abstract
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<p>Topographic features of the eastern Tibetan Plateau, highlighting Section A as the northern region and Section B as the southern region. The stars indicate the locations of Yushu, Xining, Haidong, and Lanzhou city from west to east. Annotations include the Loess Plateau, Huangshui Valley, and northeastern Tibetan Plateau (TP).</p>
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<p>Diurnal variation in precipitation during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B), based on quantitative precipitation estimates from the Fengyun 4A Satellite (FY4A QPE).</p>
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<p>Diurnal variations in cloud base height (CBH) during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B) derived from ERA5 data.</p>
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<p>Pressure-level profiles showing cloud liquid water content (shaded color), cloud base (green line), zero-degree level (orange line), and topography (red line) along longitude for (<b>a</b>,<b>b</b>) daytime ((<b>a</b>) during the mei-yu, (<b>b</b>) during midsummer periods) and nighttime ((<b>c</b>) during the mei-yu, (<b>d</b>) during midsummer periods) in Section A, and daytime ((<b>e</b>) during the mei-yu, (<b>f</b>) during midsummer periods) and nighttime ((<b>g</b>) during the mei-yu, (<b>h</b>) during midsummer periods) in Section B.</p>
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<p>Similar with <a href="#remotesensing-16-04059-f004" class="html-fig">Figure 4</a>, but for cloud ice water content. Pressure-level profiles showing cloud ice water content (shaded color), cloud base (green line), zero-degree level (orange line), and topography (red line) along longitude for (<b>a</b>,<b>b</b>) daytime ((<b>a</b>) during the mei-yu, (<b>b</b>) during midsummer periods) and nighttime ((<b>c</b>) during the mei-yu, (<b>d</b>) during midsummer periods) in Section A, and daytime ((<b>e</b>) during the mei-yu, (<b>f</b>) during midsummer periods) and nighttime ((<b>g</b>) during the mei-yu, (<b>h</b>) during midsummer periods) in Section B.</p>
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<p>Correlation of CAPE, cloud LWC, and IWC with precipitation rate during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B), derived from ERA5.</p>
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<p>Integral of water vapor flux in Section A and B at 1400 LT (<b>a</b>) and 0200 LT (<b>b</b>) during the mei-yu period and at 1400 LT (<b>c</b>) and 0200 LT (<b>d</b>) during midsummer periods from the ERA5 dataset.</p>
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<p>Diurnal variation in convective available potential energy (CAPE) during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B) from ERA5.</p>
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<p>Diurnal variation in dewpoint spread during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B).</p>
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<p>Diurnal variation in <math display="inline"><semantics> <mrow> <mo>∆</mo> <mi mathvariant="normal">V</mi> </mrow> </semantics></math> during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B).</p>
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<p>Correlation of <math display="inline"><semantics> <mrow> <mo>∆</mo> <mi mathvariant="normal">V</mi> </mrow> </semantics></math> and water vapor and precipitation during the mei-yu ((<b>a</b>) for Section A, (<b>c</b>) for Section B) and midsummer periods ((<b>b</b>) for Section A, (<b>d</b>) for Section B).</p>
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15 pages, 1649 KiB  
Article
Exploring the Plastic Surgery Related Experiences, Needs, Confidence and Knowledge Gaps of Foundation Year Doctors
by Natalia Gili
Int. Med. Educ. 2024, 3(4), 434-448; https://doi.org/10.3390/ime3040033 - 28 Oct 2024
Viewed by 381
Abstract
Plastic surgery is a diverse speciality relevant to non-plastic doctors, as plastic surgeons frequently collaborate with other specialities and its basic principles are transferable across multiple specialities. Foundation-year (FY) doctors are the most junior doctors in the workforce and may need to apply [...] Read more.
Plastic surgery is a diverse speciality relevant to non-plastic doctors, as plastic surgeons frequently collaborate with other specialities and its basic principles are transferable across multiple specialities. Foundation-year (FY) doctors are the most junior doctors in the workforce and may need to apply plastic surgery knowledge and principles during their clinical duties. Despite this, formal plastic surgery education for junior doctors is limited, resulting in an educational gap. This study gains insight into the perceived confidence, knowledge gaps, skills, educational activities and needs related to plastic surgery. This qualitative study uses phenomenology through semi-structured individual interviews with eight FY doctors. Data was analysed using reflexive thematic analysis. This study revealed that plastic surgery features diversely in the work life of FYs, who often manage patients with a lack of knowledge and confidence, influencing patient care and FY wellbeing. FYs primarily acquire knowledge and confidence through experiential learning and individual initiative. A need for curriculum improvements was expressed. FYs are an essential part of the workforce who exhibited educational gaps and a lack of confidence in plastic surgery knowledge. We suggest improved integration of plastic surgery into the FY curriculum for improved FY knowledge and patient care. Full article
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<p>Identified themes and subthemes.</p>
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<p>Clinical encounters managed directly by FY doctors.</p>
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<p>Identified barriers to learning and fulfilling needs.</p>
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<p>Novel insights into the specific plastic surgery aspects and skills relevant to the educational needs of FY doctors.</p>
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20 pages, 6032 KiB  
Article
Feasibility Analysis for Predicting Indian Ocean Bigeye Tuna (Thunnus obesus) Fishing Grounds Based on Temporal Characteristics of FY-3 Microwave Radiation Imager Data
by Yun Zhang, Jinglan Ye, Shuhu Yang, Yanling Han, Zhonghua Hong and Wanting Meng
J. Mar. Sci. Eng. 2024, 12(11), 1917; https://doi.org/10.3390/jmse12111917 - 27 Oct 2024
Viewed by 462
Abstract
Efficient and accurate fishery forecasting is of great significance in ensuring the efficiency of fishery operations. This paper proposes a fishery forecasting method using a brightness temperature (TB) time series spatial feature extraction and fusion model. Using Indian Ocean bigeye tuna fishery data [...] Read more.
Efficient and accurate fishery forecasting is of great significance in ensuring the efficiency of fishery operations. This paper proposes a fishery forecasting method using a brightness temperature (TB) time series spatial feature extraction and fusion model. Using Indian Ocean bigeye tuna fishery data from 2009 to 2021 as a reference, this paper discusses the feasibility of fishery forecasting using FY-3 Microwave Radiation Imager (MWRI) Level 1 TB data. For this paper, we designed a deep learning network model for radiometer TB time series feature extraction (TimeTB-FishNet) based on the Convolutional Neural Network (CNN), Gated Recurrent Unit (GRU), and Attention mechanism. After expanding the dimensions of TB features, the model uses them together with spatiotemporal feature factors (year, month, longitude, and latitude) as features. By adding the GRU and Attention to the CNN, the CNN-GRU-Attention model architecture is established and can extract deep time series spatial features from the data to achieve the best results. In the model validation experiments, the TimeTB-FishNet model performed optimally, with a coefficient of determination (R2) of 0.6643. In the generalization experiments, the R2 also reached 0.6261, with a root mean square error (RMSE) of 46.6031 kg/1000 hook. When the sea surface height (SSH) was introduced, the R2 further reached 0.6463, with a lower RMSE of 45.1318 kg/1000 hook. The experimental results show that the proposed method and model are feasible and effective. The proposed model can directly use enhanced radiometer TB data without relying on lagging ocean environmental product data, performing deep temporal and spatial feature extraction for fishery forecasting. This method can provide a reference for the fishing of bigeye tuna in the Indian Ocean. Full article
(This article belongs to the Section Marine Aquaculture)
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<p>Thermodynamic diagram of the CPUE (kg/1000 hook) value and bright temperature value of 18V in bigeye tuna January, 2009. (<b>a</b>) CPUE (kg/1000 hook) value thermodynamic diagram; (<b>b</b>) 18V TB (K) value thermodynamic diagram.</p>
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<p>Bigeye tuna CPUE (kg/1000 hook) grid expansion before and after comparison for January, 2009, (<b>a</b>) before grid expansion (gray means a missing CPUE value) and (<b>b</b>) after grid expansion.</p>
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<p>Bigeye tuna CPUE (kg/1000 hook) grid expansion before and after comparison for January, 2009, (<b>a</b>) before grid expansion (gray means a missing CPUE value) and (<b>b</b>) after grid expansion.</p>
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<p>Time series data construction.</p>
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<p>Prediction model frame diagram.</p>
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<p>TB temporal space feature extraction fusion model structure.</p>
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<p>Distribution of TimeFS_Fish Dataset. (<b>a</b>) Distribution of TimeFS_Fish training set data. (<b>b</b>) Distribution of TimeFS_Fish validation set data. (<b>c</b>) Distribution of TimeFS_Fish validation set data.</p>
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<p>Distribution of TimeFS_Fish Dataset. (<b>a</b>) Distribution of TimeFS_Fish training set data. (<b>b</b>) Distribution of TimeFS_Fish validation set data. (<b>c</b>) Distribution of TimeFS_Fish validation set data.</p>
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<p>RF results (<b>left</b>) and CNN results (<b>right</b>) in 2019.</p>
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<p>CNN-GRU results (<b>left</b>) and TimeTB-FishNet results (<b>right</b>) in 2019.</p>
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<p>Scatter plot of TimeTB-FishNet predicted results and actual CPUE in 2020-2021.</p>
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<p>Introduction to the SSH model structure.</p>
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<p>TimeFH_Fish results in 2020–2021.</p>
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18 pages, 10792 KiB  
Article
Precipitation Retrieval from FY-3G/MWRI-RM Based on SMOTE-LGBM
by Yanfang Lv, Lanjie Zhang, Wen Fan and Yibo Zhang
Atmosphere 2024, 15(11), 1268; https://doi.org/10.3390/atmos15111268 - 23 Oct 2024
Viewed by 359
Abstract
Using the FY-3G/MWRI-RM observations, this paper proposes a precipitation retrieval method that combines the Synthetic Minority Over-sampling Technique with Light Gradient Boosting Machine (SMOTE-LGBM) and analyzes the impact of MWRI-RM channel settings on precipitation retrieval. The SMOTE-LGBM-based model consists of two LGBM models [...] Read more.
Using the FY-3G/MWRI-RM observations, this paper proposes a precipitation retrieval method that combines the Synthetic Minority Over-sampling Technique with Light Gradient Boosting Machine (SMOTE-LGBM) and analyzes the impact of MWRI-RM channel settings on precipitation retrieval. The SMOTE-LGBM-based model consists of two LGBM models for precipitation identification and estimation, respectively. The SMOTE method is used to address the imbalance between precipitation and non-precipitation samples. Using the Integrated Multi-Satellite Retrievals for the Global Precipitation Measurement (IMERG) product as a reference, we validate the retrieved precipitation by the SMOTE-LGBM-based model with an independent testing dataset. The critical success indexes are 0.483 and 0.526, and the Pearson correlation coefficients are 0.611 and 0.645 for the ocean and land regions, respectively. The spatial distributions of the retrieved and IMERG accumulated precipitation in the testing dataset are similar. In addition, we visualize and analyze the cases of Meiyu and two typhoons. The results indicate that the SMOTE-LGBM-based model effectively represents the spatial distribution characteristics of precipitation and achieves high agreement with IMERG precipitation products. Overall, the SMOTE-LGBM-based model successfully retrieves precipitation from MWRI-RM and provides accurate precipitation products for FY-3G/MWRI-RM for the first time. Full article
(This article belongs to the Special Issue Precipitation Monitoring and Databases)
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<p>The number and distribution of samples in the ocean and land region. (<b>a</b>) The number of precipitation and non-precipitation samples; (<b>b</b>) histogram distributions of precipitation rates for precipitation samples.</p>
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<p>The overall framework of the SMOTE-LGBM-based precipitation retrieval model.</p>
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<p>The steps of SMOTE for resampling the precipitation identification dataset.</p>
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<p>Fisher measures of the MWRI-RM channel features at different precipitation rates in the ocean region.</p>
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<p>Similar to <a href="#atmosphere-15-01268-f004" class="html-fig">Figure 4</a>, but for land regions.</p>
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<p>Brightness temperature maps from 26 channels of MWRI-RM and the IMERG precipitation map on 30 May 2024, during Typhoon Maliksi.</p>
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<p>Number of precipitation samples for the IMERG precipitation product (<b>a</b>) and the retrieved precipitation (<b>b</b>) on a 0.1 × 0.1 degree grid in the testing dataset.</p>
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<p>Accumulated precipitation for the IMERG precipitation product (<b>a</b>) and the retrieved precipitation (<b>b</b>) on a 0.1 × 0.1 degree grid in the testing dataset.</p>
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<p>The scatter density map of IMERG and retrieved accumulate precipitation for the ocean region (<b>a</b>) and the land region (<b>b</b>) in the testing dataset.</p>
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<p>The IMERG precipitation product and the precipitation retrievals of SMOTE-LGBM-based model under Meiyu at 6:07 UTC on 25 June 2024.</p>
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<p>The IMERG precipitation product and the precipitation retrievals of SMOTE-LGBM-based model under tropical cyclone Ewiniar at 2:45 UTC on 28 May 2024.</p>
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<p>The IMERG precipitation product and the precipitation retrievals of SMOTE-LGBM-based model under tropical cyclone Maliksi at 4:10 UTC on 30 May 2024.</p>
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22 pages, 6149 KiB  
Article
ER-MACG: An Extreme Precipitation Forecasting Model Integrating Self-Attention Based on FY4A Satellite Data
by Mingyue Lu, Jingke Zhang, Manzhu Yu, Hui Liu, Caifen He, Tongtong Dong and Yongwei Mao
Remote Sens. 2024, 16(20), 3911; https://doi.org/10.3390/rs16203911 - 21 Oct 2024
Viewed by 505
Abstract
Extreme precipitation events often present significant risks to human life and property, making their accurate prediction an essential focus of current research. Recent studies have primarily concentrated on exploring the formation mechanisms of extreme precipitation. Existing prediction methods do not adequately account for [...] Read more.
Extreme precipitation events often present significant risks to human life and property, making their accurate prediction an essential focus of current research. Recent studies have primarily concentrated on exploring the formation mechanisms of extreme precipitation. Existing prediction methods do not adequately account for the combined terrain and atmospheric effects, resulting in shortcomings in extreme precipitation forecasting accuracy. Additionally, the satellite data resolution used in prior studies fails to precisely capture nuanced details of abrupt changes in extreme precipitation. To address these shortcomings, this study introduces an innovative approach for accurately predicting extreme precipitation: the multimodal attention ConvLSTM-GAN for extreme rainfall nowcasting (ER-MACG). This model employs high-resolution Fengyun-4A(FY4A) satellite precipitation products, as well as terrain and atmospheric datasets as inputs. The ER-MACG model enhances the ConvLSTM-GAN framework by optimizing the generator structure with an attention module to improve the focus on critical areas and time steps. This model can alleviate the problem of information loss in the spatial–temporal convolutional long short-term memory network (ConvLSTM) and, compared with the standard ConvLSTM-GAN model, can better handle the detailed changes in time and space in extreme precipitation events to achieve more refined predictions. The main findings include the following: (a) The ER-MACG model demonstrated significantly greater predictive accuracy and overall performance than other existing approaches. (b) The exclusive consideration of DEM and LPW data did not significantly enhance the ability to predict extreme precipitation events in Zhejiang Province. (c) The ER-MACG model significantly improved in identifying and predicting extreme precipitation events of different intensity levels. Full article
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<p>The location and terrain of Zhejiang, China.</p>
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<p>Distribution of precipitation values.</p>
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<p>Identification of independent extreme precipitation events.</p>
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<p>The structure of Att-ConvLSTM.</p>
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<p>The structure of the Att module.</p>
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<p>The structure and data flow of ER-MACG. t – m + 1, where t represents the past m frames of images at time t and t + 1:t + 1 + m represents the future m frames of images at time t.</p>
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<p>Evaluation curves of the POD (<b>a</b>), FAR (<b>b</b>), CSI (<b>c</b>), R (<b>d</b>), RMSE (<b>e</b>), and MAE (<b>f</b>) performance metrics for different forecasting methods over 50 min.</p>
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<p>Cumulative precipitation distribution map for rainfall exceeding 18 mm/5 min from May to October 2018–2023.</p>
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<p>Comparison of Three Precipitation Intensities During Extreme Precipitation Events. (<b>a</b>) Case 1 moderate precipitation. (<b>b</b>) Case 2 heavy precipitation. (<b>c</b>) Case 3 light precipitation.</p>
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<p>Comparison of Three Precipitation Intensities During Extreme Precipitation Events. (<b>a</b>) Case 1 moderate precipitation. (<b>b</b>) Case 2 heavy precipitation. (<b>c</b>) Case 3 light precipitation.</p>
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12 pages, 454 KiB  
Article
Evaluation of Ability of Inactivated Biomasses of Lacticaseibacillus rhamnosus and Saccharomyces cerevisiae to Adsorb Aflatoxin B1 In Vitro
by Rogério Cury Pires, Julia da Costa Calumby, Roice Eliana Rosim, Rogério D’Antonio Pires, Aline Moreira Borowsky, Sher Ali, Esther Lima de Paiva, Ramon Silva, Tatiana Colombo Pimentel, Adriano Gomes da Cruz, Carlos Augusto Fernandes de Oliveira and Carlos Humberto Corassin
Foods 2024, 13(20), 3299; https://doi.org/10.3390/foods13203299 - 17 Oct 2024
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Abstract
Biological decontamination strategies using microorganisms to adsorb aflatoxins have shown promising results for reducing the dietary exposure to these contaminants. In this study, the ability of inactivated biomasses of Lacticaseibacillus rhamnosus (LRB) and Saccharomyces cerevisiae (SCB) incorporated alone or in combination into functional [...] Read more.
Biological decontamination strategies using microorganisms to adsorb aflatoxins have shown promising results for reducing the dietary exposure to these contaminants. In this study, the ability of inactivated biomasses of Lacticaseibacillus rhamnosus (LRB) and Saccharomyces cerevisiae (SCB) incorporated alone or in combination into functional yogurts (FY) at 0.5–4.0% (w/w) to adsorb aflatoxin B1 (AFB1) was evaluated in vitro. Higher adsorption percentages (86.9–91.2%) were observed in FY containing 1.0% LR + SC or 2.0% SC (w/w). The survival of mouse embryonic fibroblasts increased after exposure to yogurts containing LC + SC at 1.0–4.0% (w/w). No significant differences were noted in the physicochemical and sensory characteristics between aflatoxin-free FY and control yogurts (no biomass) after 30 days of storage. The incorporation of combined LRB and SCB into yogurts as vehicles for these inactivated biomasses is a promising alternative for reducing the exposure to dietary AFB1. The results of this trial support further studies to develop practical applications aiming at the scalability of using the biomasses evaluated in functional foods to mitigate aflatoxin exposure. Full article
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<p>Survival of mouse embryonic fibroblasts (MEF-1) analyzed by the MTT assay, after exposure to 1.0 µg/mL of aflatoxin B<sub>1</sub> (AFB<sub>1</sub>) and functional yogurts (FY) containing 0, 1.0, 2.0, or 4.0% (<span class="html-italic">w</span>/<span class="html-italic">w</span>) of cell inactivated biomasses (BM) of <span class="html-italic">Lacticaseibacillus rhamnosus</span> (1.0 × 10<sup>10</sup> cells/g) and <span class="html-italic">Saccharomyces cerevisiae</span> (1.0 × 10<sup>10</sup> cells/g). BM was inactivated by autoclaving at 121 °C for 10 min. Values are expressed as mean ± standard deviation of percentages relative to control (C, no exposure to AFB<sub>1</sub> or FY containing BM) of 3 independent experiments with 3 replicates each. <sup>a–f</sup> Bars with different letters differ significantly (<span class="html-italic">p</span> &lt; 0.05).</p>
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22 pages, 5856 KiB  
Article
Assessment of FY-3E GNOS II Radio Occultation Data Using an Improved Three-Cornered Hat Method
by Jiahui Liang, Congliang Liu, Xi Wang, Xiangguang Meng, Yueqiang Sun, Mi Liao, Xiuqing Hu, Wenqiang Lu, Jinsong Wang, Peng Zhang, Guanglin Yang, Na Xu, Weihua Bai, Qifei Du, Peng Hu, Guangyuan Tan, Xianyi Wang, Junming Xia, Feixiong Huang, Cong Yin, Yuerong Cai and Peixian Liadd Show full author list remove Hide full author list
Remote Sens. 2024, 16(20), 3808; https://doi.org/10.3390/rs16203808 - 13 Oct 2024
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Abstract
The spatial–temporal sampling errors arising from the differences in geographical locations and measurement times between co-located Global Navigation Satellite System (GNSS) radio occultation (RO) and radiosonde (RS) data represent systematic errors in the three-cornered hat (3CH) method. In this study, we propose a [...] Read more.
The spatial–temporal sampling errors arising from the differences in geographical locations and measurement times between co-located Global Navigation Satellite System (GNSS) radio occultation (RO) and radiosonde (RS) data represent systematic errors in the three-cornered hat (3CH) method. In this study, we propose a novel spatial–temporal sampling correction method to mitigate the sampling errors associated with both RO–RS and RS–model pairs. We analyze the 3CH processing chain with this new correction method in comparison to traditional approaches, utilizing Fengyun-3E (FY-3E) GNSS Occultation Sounder II (GNOS II) RO data, atmospheric models, and RS datasets from the Hailar and Xisha stations. Overall, the results demonstrate that the improved 3CH method performs better in terms of spatial–temporal sampling errors and the variances of atmospheric parameters, including refractivity, temperature, and specific humidity. Subsequently, we assess the error variances of the FY-3E GNOS II RO, RS and model atmospheric parameters in China, in particular the northern China and southern China regions, based on large ensemble datasets using the improved 3CH data processing chain. The results indicate that the FY-3E GNOS II BeiDou navigation satellite system (BDS) RO and Global Positioning System (GPS) RO show good consistency, with the average error variances of refractivity, temperature, and specific humidity being less than 1.12%2, 0.13%2, and 700%2, respectively. A comparison of the datasets from northern and southern China reveals that the error variances for refractivity are smaller in northern China, while temperature and specific humidity exhibit smaller error variances in southern China, which is attributable to the differing climatic conditions. Full article
(This article belongs to the Special Issue International GNSS Service Validation, Application and Calibration)
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<p>The spatial distribution of radiosonde stations. Diamond symbols represent radiosonde stations, and the color of the symbols indicates the number of occultations co-located with each station. The two square symbols represent the northernmost Hailar station (49.25°N, 119.70°E) and the southernmost Xisha station (16.83°N, 112.33°E), respectively, and the solid blue line is the north–south dividing line.</p>
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<p>The number of FY-3E GNOS II BDS and GPS occultations co-located with each radiosonde station: blue bars indicate BDS data, and green bars represent GPS data. The dataset spans from 1 September 2022 to 31 August 2023.</p>
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<p>Statistical comparison of refractivity, temperature, and specific humidity profiles of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 located at the Xisha and Hailar radiosonde stations. The ensemble of data span from 1 September 2022 to 31 August 2023 and the statistics include the mean (solid line) and the standard deviation (“std”; dashed line), respectively.</p>
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<p>Refractivity error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Hailar station for different sampling correction schemes.</p>
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<p>Refractivity error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Xisha station for different sampling correction schemes.</p>
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<p>Temperature error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Hailar station for different sampling correction schemes.</p>
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<p>Temperature error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Xisha station for different sampling correction schemes.</p>
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<p>Specific humidity error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Hailar station for different sampling correction schemes.</p>
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<p>Specific humidity error variances (percentage square) of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets at the Xisha station for different sampling correction schemes.</p>
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<p>Estimated error variances of refractivity, temperature, and specific humidity of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets in China (percentage squared).</p>
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<p>Estimated error variances of refractivity, temperature, and specific humidity of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets in southern China (percentage squared).</p>
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<p>Estimated error variances of refractivity, temperature, and specific humidity of (<b>a</b>–<b>c</b>) RO, (<b>d</b>–<b>f</b>) RS, and (<b>g</b>–<b>i</b>) ERA5 datasets in northern China (percentage squared).</p>
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18 pages, 12939 KiB  
Article
Dust Monitoring and Three-Dimensional Transport Characteristics of Dust Aerosol in Beijing, Tianjin, and Hebei
by Siqin Zhang, Jianjun Wu, Jiaqi Yao, Xuefeng Quan, Haoran Zhai, Qingkai Lu, Haobin Xia, Mengran Wang and Jinquan Guo
Atmosphere 2024, 15(10), 1212; https://doi.org/10.3390/atmos15101212 - 10 Oct 2024
Viewed by 520
Abstract
Global dust events have become more frequent due to climate change and increased human activity, significantly impacting air quality and human health. Previous studies have mainly focused on determining atmospheric dust pollution levels through atmospheric parameter simulations or AOD values obtained from satellite [...] Read more.
Global dust events have become more frequent due to climate change and increased human activity, significantly impacting air quality and human health. Previous studies have mainly focused on determining atmospheric dust pollution levels through atmospheric parameter simulations or AOD values obtained from satellite remote sensing. However, research on the quantitative description of dust intensity and its cross-regional transport characteristics still faces numerous challenges. Therefore, this study utilized Fengyun-4A (FY-4A) satellite Advanced Geostationary Radiation Imager (AGRI) imagery, Cloud-Aerosol Lidar, and Infrared Pathfinder Satellite Observation (CALIPSO) lidar, and other auxiliary data, to conduct three-dimensional spatiotemporal monitoring and a cross-regional transport analysis of two typical dust events in the Beijing–Tianjin–Hebei (BTH) region of China using four dust intensity indices Infrared Channel Shortwave Dust (Icsd), Dust Detection Index (DDI), dust value (DV), and Dust Strength Index (DSI)) and the HYSPLIT model. We found that among the four indices, DDI was the most suitable for studying dust in the BTH region, with a detection accuracy (POCD) of >88% at all times and reaching a maximum of 96.14%. Both the 2021 and 2023 dust events originated from large-scale deforestation in southern Mongolia and the border area of Inner Mongolia, with dust plumes distributed between 2 and 12 km being transported across regions to the BTH area. Further, when dust aerosols are primarily concentrated below 4 km and PM10 concentrations consistently exceed 600 µg/m3, large dust storms are more likely to occur in the BTH region. The findings of this study provide valuable insights into the sources, transport pathways, and environmental impacts of dust aerosols. Full article
(This article belongs to the Section Aerosols)
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<p>Administrative map. (<b>a</b>) National 1 km DEM elevation map. (<b>b</b>) PM<sub>10</sub> monitoring station distribution in Beijing-Tianjin-Hebei Region. (<b>c</b>) Bar chart of dust source management project construction in Beijing-Tianjin-Hebei Region (2015–2019).</p>
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<p>Technical flowchart.</p>
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<p>Histogram of frequency distribution for thin clouds, thick clouds, and dust under four dust intensity indices.</p>
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<p>Dust identification results in the Beijing–Tianjin–Hebei Region. AGRI true-color images for 15 March 2021, UTC 03:00–06:00 (<b>a<sub>1</sub></b>–<b>a<sub>4</sub></b>), and DDI distribution maps (<b>b<sub>1</sub></b>–<b>b<sub>4</sub></b>); AGRI true-color images for 22 March 2023, UTC 03:00–06:00 (<b>c<sub>1</sub></b>–<b>c<sub>4</sub></b>), and DDI distribution maps (<b>d<sub>1</sub></b>–<b>d<sub>4</sub></b>); DDI violin and boxplot statistics for 15 March 2021, and 22 March 2023, UTC 03:00–06:00 (<b>e</b>).</p>
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<p>HYSPLIT backward trajectory simulations and FY-4A true-color images for the two dust events: (<b>a</b>,<b>b</b>) Beijing backward trajectory simulation for 15 March 2021; (<b>d</b>,<b>e</b>) Beijing backward trajectory simulation for 22 March 2023; (<b>c</b>) an FY-4A true-color image for 15 March 2021, at UTC 04:00; (<b>f</b>) an FY-4A true-color image for 22 March 2023, at UTC 04:00.</p>
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<p>Vertical distribution characteristics of aerosols and hourly changes in PM<sub>10</sub> concentration in the BTH and Inner Mongolia regions: 15 March 2021, BTH and Inner Mongolia regions (<b>a<sub>1</sub></b>–<b>a<sub>3</sub></b>, <b>b<sub>1</sub></b>–<b>b<sub>3</sub></b>); 21 March 2023, BTH and Inner Mongolia regions (<b>c<sub>1</sub></b>–<b>c<sub>3</sub></b>, <b>d<sub>1</sub></b>–<b>d<sub>3</sub></b>).</p>
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