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27 pages, 4435 KiB  
Article
Remote Ischemic Post-Conditioning (RIC) Mediates Anti-Inflammatory Signaling via Myeloid AMPKα1 in Murine Traumatic Optic Neuropathy (TON)
by Naseem Akhter, Jessica Contreras, Mairaj A. Ansari, Andrew F. Ducruet, Md Nasrul Hoda, Abdullah S. Ahmad, Laxman D. Gangwani, Kanchan Bhatia and Saif Ahmad
Int. J. Mol. Sci. 2024, 25(24), 13626; https://doi.org/10.3390/ijms252413626 - 19 Dec 2024
Abstract
Traumatic optic neuropathy (TON) has been regarded a vision-threatening condition caused by either ocular or blunt/penetrating head trauma, which is characterized by direct or indirect TON. Injury happens during sports, vehicle accidents and mainly in military war and combat exposure. Earlier, we have [...] Read more.
Traumatic optic neuropathy (TON) has been regarded a vision-threatening condition caused by either ocular or blunt/penetrating head trauma, which is characterized by direct or indirect TON. Injury happens during sports, vehicle accidents and mainly in military war and combat exposure. Earlier, we have demonstrated that remote ischemic post-conditioning (RIC) therapy is protective in TON, and here we report that AMPKα1 activation is crucial. AMPKα1 is the catalytic subunit of the heterotrimeric enzyme AMPK, the master regulator of cellular energetics and metabolism. The α1 isoform predominates in immune cells including macrophages (Mφs). Myeloid-specific AMPKα1 KO mice were generated by crossing AMPKα1Flox/Flox and LysMcre to carry out the study. We induced TON in mice by using a controlled impact system. Mice (mixed sex) were randomized in six experimental groups for Sham (mock); Sham (RIC); AMPKα1F/F (TON); AMPKα1F/F (TON+RIC); AMPKα1F/F LysMCre (TON); AMPKα1F/F LysMCre (TON+RIC). RIC therapy was given every day (5–7 days following TON). Data were generated by using Western blotting (pAMPKα1, ICAM1, Brn3 and GAP43), immunofluorescence (pAMPKα1, cd11b, TMEM119 and ICAM1), flow cytometry (CD11b, F4/80, CD68, CD206, IL-10 and LY6G), ELISA (TNF-α and IL-10) and transmission electron microscopy (TEM, for demyelination and axonal degeneration), and retinal oxygenation was measured by a Unisense sensor system. First, we observed retinal morphology with funduscopic images and found TON has vascular inflammation. H&E staining data suggested that TON increased retinal inflammation and RIC attenuates retinal ganglion cell death. Immunofluorescence and Western blot data showed increased microglial activation and decreased retinal ganglion cell (RGCs) marker Brn3 and axonal regeneration marker GAP43 expression in the TON [AMPKα1F/F] vs. Sham group, but TON+RIC [AMPKα1F/F] attenuated the expression level of these markers. Interestingly, higher microglia activation was observed in the myeloid AMPKα1F/F KO group following TON, and RIC therapy did not attenuate microglial expression. Flow cytometry, ELISA and retinal tissue oxygen data revealed that RIC therapy significantly reduced the pro-inflammatory signaling markers, increased anti-inflammatory macrophage polarization and improved oxygen level in the TON+RIC [AMPKα1F/F] group; however, RIC therapy did not reduce inflammatory signaling activation in the myeloid AMPKα1 KO mice. The transmission electron microscopy (TEM) data of the optic nerve showed increased demyelination and axonal degeneration in the TON [AMPKα1F/F] group, and RIC improved the myelination process in TON [AMPKα1F/F], but RIC had no significant effect in the AMPKα1 KO mice. The myeloid AMPKα1c deletion attenuated RIC induced anti-inflammatory macrophage polarization, and that suggests a molecular link between RIC and immune activation. Overall, these data suggest that RIC therapy provided protection against inflammation and neurodegeneration via myeloid AMPKα1 activation, but the deletion of myeloid AMPKα1 is not protective in TON. Further investigation of RIC and AMPKα1 signaling is warranted in TON. Full article
(This article belongs to the Special Issue New Therapeutic Targets for Neuroinflammation and Neurodegeneration)
Show Figures

Figure 1

Figure 1
<p>(<b>A</b>) Representative in vivo funduscopic fluorescein image from C56BL/6 mice showing inflammation in blood vessels in TON as compared with control eye. Intravenous fluorescein angiography of the mouse retina shows poor perfusion through attenuated vasculature (due to progression of the retinal degeneration) following TON. (<b>B</b>) H&amp;E data showed increased neuronal cell death in ganglion cell layer in TON compared with control. However, the neuronal cell death is prevented with RIC treatment. Fluorescein angiography imaging (<b>A</b>) was captured within 5 mins of fluorescein dye injection through tail vein.</p>
Full article ">Figure 2
<p>(<b>A</b>,<b>B</b>) Immunofluorescence staining showed microglial marker TMEM119 expression in mouse retina. TON (with AMPK) increases microglial activation, and RIC downregulated significantly. Myeloid pAMPKα1 KO group showed heightened microglial activation; notably, RIC demonstrated no significant effects. Florescence color intensity was measured by Image J software (NIH, <a href="https://imagej.net/ij/" target="_blank">https://imagej.net/ij/</a>). White boxes show the TMEM119 expression in inner nuclear layer (INL) and GCL (ganglion cell layer) region of mouse eye. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>. (<b>C</b>–<b>I</b>) Representative pseudocolor and histograms of flow cytometry show the gating strategy for microglia/macrophages (CD11b+_F4/80+) and CD68+ and CD206+ expressing microglia in blood. Bar graph summarizing the cell counts of microglia (M1/M2) in the blood after 5 days of TON. Red, TMEM119 (activated microglial marker); Blue, DAPI. We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysMCre (TON); AMPKα1<sup>F/F</sup> LysMCre (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
Full article ">Figure 2 Cont.
<p>(<b>A</b>,<b>B</b>) Immunofluorescence staining showed microglial marker TMEM119 expression in mouse retina. TON (with AMPK) increases microglial activation, and RIC downregulated significantly. Myeloid pAMPKα1 KO group showed heightened microglial activation; notably, RIC demonstrated no significant effects. Florescence color intensity was measured by Image J software (NIH, <a href="https://imagej.net/ij/" target="_blank">https://imagej.net/ij/</a>). White boxes show the TMEM119 expression in inner nuclear layer (INL) and GCL (ganglion cell layer) region of mouse eye. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>. (<b>C</b>–<b>I</b>) Representative pseudocolor and histograms of flow cytometry show the gating strategy for microglia/macrophages (CD11b+_F4/80+) and CD68+ and CD206+ expressing microglia in blood. Bar graph summarizing the cell counts of microglia (M1/M2) in the blood after 5 days of TON. Red, TMEM119 (activated microglial marker); Blue, DAPI. We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysMCre (TON); AMPKα1<sup>F/F</sup> LysMCre (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
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<p>Effect of RIC on IL10 and neutrophil expression following TON. (<b>A</b>,<b>B</b>,<b>D</b>,<b>F</b>) Representative pseudocolor and histograms of flow cytometry show the gating strategy for microglia/macrophages (CD11b+_IL10+, F4/80+_IL10+ and CD68+_IL10+) and CD68+_LY6G+-expressing neutrophils in blood. (<b>C</b>,<b>E</b>,<b>G</b>,<b>H</b>) Representative bar graph summarizing the cell counts of IL10+ and Ly6G+ in the blood after 5 days of TON. Six experimental groups included Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysMCre (TON); AMPKα1<sup>F/F</sup> LysMCre (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). ** <span class="html-italic">p</span> &lt; 0.01.*** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
Full article ">Figure 3 Cont.
<p>Effect of RIC on IL10 and neutrophil expression following TON. (<b>A</b>,<b>B</b>,<b>D</b>,<b>F</b>) Representative pseudocolor and histograms of flow cytometry show the gating strategy for microglia/macrophages (CD11b+_IL10+, F4/80+_IL10+ and CD68+_IL10+) and CD68+_LY6G+-expressing neutrophils in blood. (<b>C</b>,<b>E</b>,<b>G</b>,<b>H</b>) Representative bar graph summarizing the cell counts of IL10+ and Ly6G+ in the blood after 5 days of TON. Six experimental groups included Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysMCre (TON); AMPKα1<sup>F/F</sup> LysMCre (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). ** <span class="html-italic">p</span> &lt; 0.01.*** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
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<p>The effect of RIC on TON induced pro-inflammatory signaling. (<b>A</b>,<b>B</b>) ELISA results in blood plasma showing TNF and IL10 expression. Fluorescence color intensity was measured by Image J software. We used 6 experimental group, Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
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<p>Effect of RIC on TON induced pro-inflammatory signaling. (<b>A</b>,<b>B</b>) The effect of RIC on ICAM-1 expression assessed by immunofluorescence and (<b>C</b>,<b>D</b>) ICAM1 Protein expression was checked by Western blot. Fluorescence color intensity as well as western blot band intensity was measured by Image J software (NIH, <a href="https://imagej.net/ij/" target="_blank">https://imagej.net/ij/</a>). We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. Scale bar 50 μm. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
Full article ">Figure 5 Cont.
<p>Effect of RIC on TON induced pro-inflammatory signaling. (<b>A</b>,<b>B</b>) The effect of RIC on ICAM-1 expression assessed by immunofluorescence and (<b>C</b>,<b>D</b>) ICAM1 Protein expression was checked by Western blot. Fluorescence color intensity as well as western blot band intensity was measured by Image J software (NIH, <a href="https://imagej.net/ij/" target="_blank">https://imagej.net/ij/</a>). We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1<sup>F/F</sup> (TON); AMPKα1<sup>F/F</sup> (TON+RIC); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON); AMPKα1<sup>F/F</sup> LysM<sup>Cre</sup> (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. Scale bar 50 μm. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
Full article ">Figure 6
<p>(<b>A</b>–<b>D</b>) Effect of RIC therapy on retinal oxygenation in TON. Oxygen levels were analyzed with UniSense sensor system (Sweden). We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1F/F (TON); AMPKα1F/F (TON+RIC); AMPKα1F/F LysM<sup>Cre</sup> (TON); AMPKα1F/F LysM<sup>Cre</sup> (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001, **** <span class="html-italic">p</span> &lt; 0.0001. ns, non-significant. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
Full article ">Figure 7
<p>(<b>A</b>–<b>D</b>) Effect of RIC therapy on TON retina. Western blot analysis demonstrated significant changes in protein expression level of Brn3a and GAP43 between TON+RIC and TON group. Densitometry analysis was carried out by Image J software (NIH, <a href="https://imagej.net/ij/" target="_blank">https://imagej.net/ij/</a>). We used 4 experimental groups, AMPKα1F/F (TON); AMPKα1F/F (TON+RIC); AMPKα1F/F LysM<sup>Cre</sup> (TON); AMPKα1F/F LysM<sup>Cre</sup> (TON+RIC). Differences among experimental groups were determined by analysis of variance (one-way ANOVA) followed by Newman–Keuls multiple comparison tests. The results represent the means ± SEM of fold changes (<span class="html-italic">n</span> = 5). * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01. ns, non-significant.</p>
Full article ">Figure 8
<p>Representative ultrastructural features of axonal injury in traumatic optic neuropathy. Electron micrographs are taken across the longitudinal plane through the injury front and show a range of axoplasmic, axolemmal and myelin sheath abnormalities. RIC therapy attenuated this degenerating process in TON. We used 6 experimental groups, Sham (mock); Sham (RIC); AMPKα1F/F (TON); AMPKα1F/F (TON+RIC); AMPKα1F/F LysM<sup>Cre</sup> (TON); AMPKα1F/F LysM<sup>Cre</sup> (TON+RIC). Scale bar 4 μm. For Sham (mock) and Sham (RIC), both groups are regarded as AMPKα1<sup>F/F</sup>.</p>
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<p>Schematic representation demonstrating increased M1-type macrophages causing inflammation and demyelination of optic nerve (ON) in TON. Our hypothesis demonstrates that RIC therapy activates AMPKα1 to modulate macrophage polarization toward M2-type anti-inflammatory macrophages that protect demyelination of downregulated ON.</p>
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23 pages, 6442 KiB  
Article
Integration of Drone and Satellite Imagery Improves Agricultural Management Agility
by Michael Gbenga Ogungbuyi, Caroline Mohammed, Andrew M. Fischer, Darren Turner, Jason Whitehead and Matthew Tom Harrison
Remote Sens. 2024, 16(24), 4688; https://doi.org/10.3390/rs16244688 - 16 Dec 2024
Viewed by 366
Abstract
Effective agricultural management hinges upon timely decision-making. Here, we evaluated whether drone and satellite imagery could improve real-time and remote monitoring of pasture management. Using unmanned aerial systems (UAS), we quantified grassland biomass through changes in sward height pre- and post-grazing by sheep. [...] Read more.
Effective agricultural management hinges upon timely decision-making. Here, we evaluated whether drone and satellite imagery could improve real-time and remote monitoring of pasture management. Using unmanned aerial systems (UAS), we quantified grassland biomass through changes in sward height pre- and post-grazing by sheep. As optical spectral data from Sentinel-2 satellite imagery is often hindered by cloud contamination, we assessed whether machine learning could help improve the accuracy of pasture biomass prognostics. The calibration of UAS biomass using field measurements from sward height change through 3D photogrammetry resulted in an improved regression (R2 = 0.75, RMSE = 1240 kg DM/ha, and MAE = 980 kg DM/ha) compared with using the same field measurements with random forest-machine learning and Sentinel-2 imagery (R2 = 0.56, RMSE = 2140 kg DM/ha, and MAE = 1585 kg DM/ha). The standard error of the mean (SEM) for the field biomass, derived from UAS-measured sward height changes, was 1240 kg DM/ha. When UAS data were integrated with the Sentinel-2-random forest model, SEM reduced from 1642 kg DM/ha to 1473 kg DM/ha, demonstrating that integration of UAS data improved model accuracy. We show that modelled biomass from 3D photogrammetry has significantly higher accuracy than that predicted from Sentinel-2 imagery with random forest modelling (S2-RF). Our study demonstrates that timely, accurate quantification of pasture biomass is conducive to improved decision-making agility, and that coupling of UAS with satellite imagery may improve the accuracy and timeliness of agricultural biomass prognostics. Full article
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Figure 1

Figure 1
<p>Location of commercial sheep farm “Okehampton” (42°30′S, 147°59′E) near Triabunna, southeastern Tasmania, Australia. The yellow panel represents Site 1 (12 subplots of 0.25 ha), while the red panel represents Cottage paddock, and the blue panel represents Old Bougainville (located on the hilltop) is Site 2. Red dots depict sampling points located within each polygon of the imagery. The study site was mapped using 2020/21 global land cover from the European Space Agency (ESA), developed and validated with 10 m resolution of Sentinel–2 and Sentinel–1 imagery (<a href="https://doi.org/10.5281/zenodo.5571936" target="_blank">https://doi.org/10.5281/zenodo.5571936</a>).</p>
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<p>Representative ground cover for the Cottage and Old Bougainville fields at Okehampton, Triabunna, Australia, January 2019. (<b>a</b>) Typical ground cover of Phalaris (<span class="html-italic">Phalaris aquatica</span> L.) shows a high proportion of bare ground and Flatweed (<span class="html-italic">Hypochaeris radicata</span>), (<b>b</b>) sheep track beside the heavily browsed ground from historical management. (<b>c</b>) Flatweed and Phalaris, and (<b>d</b>) healthy Phalaris, (<b>e</b>,<b>f</b>) were taken in November 2022 at the Vault paddock. Panel (<b>e</b>) shows an extremely high volume (&gt;10,000 kg DM/ha) of grassland, while (<b>f</b>) depicts a 0.5 × 0.5 m quadrat, where physical biomass measurements were taken.</p>
Full article ">Figure 3
<p>UAS campaign with survey protocol installations to compare UAS grass height measurements and destructively sampled biomass at the Okehampton farm, Triabunna, Tasmania, Australia. (<b>a</b>) Ground control point at the boundary of Vault paddocks, (<b>b</b>) bricks and pins installation to identify the ground control points, (<b>c</b>,<b>d</b>) diagonal transects along each paddock where sampled biomass data was collected, and (<b>e</b>) example of 3D point cloud photo of one of the processed UAS images captured for a pre-grazing event at Okehampton sheep grazing farm, Triabunna (photo taken in the pre-trial flight on 2 December 2021), and (<b>f</b>) DJI Matrice 300 RTK with Zenmuse P1. Images (<b>b</b>,<b>d</b>,<b>e</b>) were adopted from Harrison et al. [<a href="#B45-remotesensing-16-04688" class="html-bibr">45</a>].</p>
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<p>Workflow showing main components of the method.</p>
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<p>Relationship between mean sward height predicted from UAS and actual sampled biomass. The relationship translates delta pasture height (i.e., pasture height before and after grazing) into biomass.</p>
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<p>Sentinel−2 random forest model outputs compared with UAS−calibrated biomass data using linear regression for Vault and Bougainville.</p>
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<p>Sentinel-2 biomass calibration using UAS-derived biomass change data. Sentinel-2 data was based on the test set-obtained S2-RF–enabled model. Each point represents the average biomass at the paddock level for the drone and satellite. The calibration was conducted to elucidate whether UAS imagery could improve the temporal frequency and accuracy of biomass estimates from Sentinel-2 imagery, addressing challenges posed by frequent cloud cover obscuring satellite images in the high latitudes of southern Australia.</p>
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<p>Comparison of the seasonality of UAS biomass in two representative paddocks against Sentinel-2 model estimates. The UAS model estimates biomass changes based on grass height variations between pre- and post-grazing events, while the Sentinel-2 estimates biomass using the nearest temporal imagery and a random forest algorithm. Each point represents the average biomass (mean) at the paddock level for both the drone and satellite.</p>
Full article ">Figure 9
<p>Pixel-based comparison and spatial resolution between the RGB fitted-UAS and Sentinel-2 instruments deployed for investigating grassland biomass at Okehampton in Triabunna, Australia. The field size is 0.25 ha. (<b>a</b>) RGB (red, green, and blue) image for pre-graze on 25 January 2023 for the Vault paddocks, (<b>b</b>) post-grazing event on 27 January 2023, and (<b>c</b>) Sentinel-2 image available on 24 January 2023. Field biomass was sampled on 25 January 2023. Units of each legend are shown in kg DM/ha. Note: The Sentinel-2 image (<b>c</b>) was enlarged for improved visual clarity.</p>
Full article ">Figure 10
<p>Botanical composition as a contribution toward grassland biomass in each paddock. Note: scaling is unique to each paddock as species distribution differs across plots.</p>
Full article ">Figure 11
<p>NDVI response to weekly rainfall and grazing management in Cottage and Old Bougainville paddocks, highlighting pasture species productivity and grazing patterns. The Cottage paddock (<b>a</b>) was used as business-as-usual by opening its gate to adjoining paddocks. Pasture species show peak heights when sheep move to adjoining paddocks. The Old Bougainville paddock (<b>b</b>) shows non-selective grazing from increased stocking rates (ewes that were lambing).</p>
Full article ">Figure 12
<p>Correlation between weekly rainfall and NDVI response, highlighting the significant relationship in the Cottage and Old Bougainville paddocks during the spring of 2019 in Okehampton, Triabunna, Australia. Each data point represents the average NDVI and cumulative rainfall for that week.</p>
Full article ">Figure 13
<p>Correlation between NDVI and pasture species (Phalaris and Cocksfoot) indicates a varying relationship influenced by grazing intensity and management practices. No statistical correlation was observed between NDVI and botanical composition. The moderate correlation between Phalaris species and NDVI indicates dominance of the said species in the Cottage paddock.</p>
Full article ">
27 pages, 14705 KiB  
Article
Monitoring the Impact of Floods on Water Quality Using Optical Remote Sensing Imagery: The Case of Lake Karla (Greece)
by Triantafyllia-Maria Perivolioti, Konstantinos Zachopoulos, Marianthi Zioga, Maria Tompoulidou, Sotiria Katsavouni, Dimitra Kemitzoglou, Dimitrios Terzopoulos, Antonios Mouratidis and Vasiliki Tsiaoussi
Water 2024, 16(23), 3502; https://doi.org/10.3390/w16233502 - 5 Dec 2024
Viewed by 1243
Abstract
This study investigates the performance of published bio-optical remote sensing indices/algorithms for monitoring water quality changes in Lake Karla, Greece, caused by Storm Daniel after the September 2023 flooding event. Commonly applied indices were utilised to estimate chlorophyll-a (Chl-a) and total suspended solids [...] Read more.
This study investigates the performance of published bio-optical remote sensing indices/algorithms for monitoring water quality changes in Lake Karla, Greece, caused by Storm Daniel after the September 2023 flooding event. Commonly applied indices were utilised to estimate chlorophyll-a (Chl-a) and total suspended solids (TSS) using Sentinel-2 high-resolution optical imagery. In situ measurements were undertaken and water samples were collected during the pre-flooding period, post-flooding, and one-year post-flood, providing a basis for validating the remote sensing models. Monitoring results showed that most physicochemical parameters changed considerably. Chl-a and TSS were estimated by testing five and seven indices, respectively. Regarding the Chl-a estimation, the NDCI and 2-BDA indices outperformed other models, having high correlations with in situ Chl-a measurements and effectively following the in situ Chl-a temporal trends. Among the TSS indices, NDWI and TUR-IND demonstrated better performances, effectively capturing the variations in suspended solids. Overall, this study highlights the potential of Sentinel-2 imagery in assessing water quality changes, particularly in response to flooding events. It is an exploratory approach to assess the feasibility of utilising optical satellite data for evaluating the environmental impacts of natural disasters on lake water quality and supports decision-making in environmental management. Additionally, it identifies potential challenges and considerations that must be addressed to ensure effective application. Full article
(This article belongs to the Special Issue Application of Satellite Remote Sensing in Water Quality Monitoring)
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Figure 1

Figure 1
<p>The location of the sampling points: The central sampling point (SP0) is defined according to the Joint Ministerial Decision no. YPEN/DPDYP/107168/1444. Points SP1–SP6 are peripheral points within the lake under investigative monitoring. The sampling points SP2 and SP5 are located at the pumping stations DP1 and DP2, while SP6, SP4, SP3, and SP2 are located at the collectors S3, S4, S6, and S7 accordingly. Peripheral sampling points SP3–6 are grouped using orange colour, indicating that they receive direct inflows from the corresponding collectors. Peripheral sampling points SP1 and SP2 are grouped using green colour, as they do not receive direct inflows from collectors. Despite the absence of direct collector inflows, they are influenced by inflows from the basin.</p>
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<p>A photo captured during the in situ measurements at sampling station SP0 in Lake Karla after the flood event.</p>
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<p>(<b>a</b>) Temperature, (<b>b</b>) pH, (<b>c</b>) oxygen saturation, (<b>d</b>) dissolved oxygen (DO), (<b>e</b>) electrical conductivity (EC), (<b>f</b>) total suspended solids (TSS), (<b>g</b>) total phosphorus (TP), and (<b>h</b>) chlorophyll-a (Chl-a) of water samples collected from sampling points SP0–SP6 at Lake Karla (2023–2024).</p>
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<p>Concentrations of ions (<b>a</b>) Cl<sup>−</sup>, (b) SO<sub>4</sub><sup>−2</sup>, (<b>c</b>) Na<sup>+</sup>, (<b>d</b>) K<sup>+</sup>, (<b>e</b>) Mg<sup>+2</sup>, and (<b>f</b>) Ca<sup>+2</sup>; (<b>g</b>) ammonium ions (NH<sub>4</sub><sup>+</sup>); (<b>h</b>) nitrate ions (NO<sub>3</sub><sup>−</sup>); (<b>i</b>) total alkalinity (TA); and (<b>j</b>) biochemical oxygen demand (BOD<sub>5</sub>) of water samples collected from sampling points SP0–SP6 at Lake Karla (2023–2024). * Values &lt; LOQ.</p>
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<p>Histograms of the Sentinel-2 band values over different dates (pre-flooding period, post-flooding period, and one-year post-flood), with a focus on pixels corresponding to the lake area.</p>
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<p>Spearman correlation heatmaps for reflectance values between different dates (pre-flood, post-flood, and one year post-flood) for each band.</p>
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<p>Temporal variance and statistical significance of Sentinel-2 bands across pre-flood and post-flood periods and one-year post-flood. Each plot illustrates the variance of individual bands over time (pre-flooding period, post-flooding period, and one year after flooding), with a focus on pixels corresponding to the lake area. Red asterisks denote dates where variance changes are statistically significant between consecutive dates (<span class="html-italic">p</span>-values).</p>
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<p>(<b>a</b>,<b>b</b>) Temporal trends of in situ chlorophyll-a (Chl-a) measurements across the different stations during the pre-flood and post-flood periods and one -year post-flood compared with Chl-a indices derived from Sentinel-2 imagery. The plots are presented separately in different images for improved visualisation and clarity.</p>
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<p>(<b>a</b>,<b>b</b>) Temporal trends of in situ chlorophyll-a (Chl-a) measurements across the different stations during the pre-flood and post-flood periods and one -year post-flood compared with Chl-a indices derived from Sentinel-2 imagery. The plots are presented separately in different images for improved visualisation and clarity.</p>
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<p>(<b>a</b>–<b>c</b>) Temporal trends of in situ TSS measurements across the different stations during pre-flood and post-flood periods and one-year post- flood, compared with TSS indices derived from Sentinel-2 imagery. The plots are presented separately in different images for improved visualisation and clarity.</p>
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<p>(<b>a</b>–<b>c</b>) Temporal trends of in situ TSS measurements across the different stations during pre-flood and post-flood periods and one-year post- flood, compared with TSS indices derived from Sentinel-2 imagery. The plots are presented separately in different images for improved visualisation and clarity.</p>
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<p>Spearman correlation coefficients of the studied indices with in situ (<b>A</b>) chlorophyll-a (Chl-a) and (<b>B</b>) total suspended solids (TSS) measurements.</p>
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<p>Linear regression model for NDCI.</p>
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<p>The combined regression model for TSS prediction using TUR-IND, NDWI, and their interaction term.</p>
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<p>Sentinel-2-derived chlorophyll-a concentration (µg/L) maps over Lake Karla showing variations during the pre-flood (June to August 2023) and post-flood (September to December 2023) periods and one-year post-flood (June–July 2024). Warmer colours (red/purple) indicate higher chlorophyll-a concentrations, while cooler colours (blue/green) represent lower concentrations.</p>
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<p>Sentinel-2-derived TSS concentration (mg/L) maps over Lake Karla, showing variations during the pre-flood (June to August 2023) and post-flood periods (September to December 2023) and one-year post-flood (June–July 2024). Warmer colours (red/orange) indicate higher TSS concentrations, while cooler colours (blue/green) represent lower concentrations.</p>
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21 pages, 3528 KiB  
Systematic Review
Assessing Drone-Based Remote Sensing for Monitoring Water Temperature, Suspended Solids and CDOM in Inland Waters: A Global Systematic Review of Challenges and Opportunities
by Shannyn Jade Pillay, Tsitsi Bangira, Mbulisi Sibanda, Seifu Kebede Gurmessa, Alistair Clulow and Tafadzwanashe Mabhaudhi
Drones 2024, 8(12), 733; https://doi.org/10.3390/drones8120733 - 3 Dec 2024
Viewed by 1016
Abstract
Monitoring water quality is crucial for understanding aquatic ecosystem health and changes in physical, chemical, and microbial water quality standards. Water quality critically influences industrial, agricultural, and domestic uses of water. Remote sensing techniques can monitor and measure water quality parameters accurately and [...] Read more.
Monitoring water quality is crucial for understanding aquatic ecosystem health and changes in physical, chemical, and microbial water quality standards. Water quality critically influences industrial, agricultural, and domestic uses of water. Remote sensing techniques can monitor and measure water quality parameters accurately and quantitatively. Earth observation satellites equipped with optical and thermal sensors have proven effective in providing the temporal and spatial data required for monitoring the water quality of inland water bodies. However, using satellite-derived data are associated with coarse spatial resolution and thus are unsuitable for monitoring the water quality of small inland water bodies. With the development of unmanned aerial vehicles (UAVs) and artificial intelligence, there has been significant advancement in remotely sensed water quality retrieval of small water bodies, which provides water for crop irrigation. This article presents the application of remotely sensed data from UAVs to retrieve key water quality parameters such as surface water temperature, total suspended solids (TSS), and Chromophoric dissolved organic matter (CDOM) in inland water bodies. In particular, the review comprehensively analyses the potential advancements in utilising drone technology along with machine learning algorithms, platform type, sensor characteristics, statistical metrics, and validation techniques for monitoring these water quality parameters. The study discusses the strengths, challenges, and limitations of using UAVs in estimating water temperature, TSS, and CDOM in small water bodies. Finally, possible solutions and remarks for retrieving water quality parameters using UAVs are provided. The review is important for future development and research in water quality for agricultural production in small water bodies. Full article
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<p>Selection of the studies considered in this review.</p>
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<p>Spatial distribution of UAV-based remote sensing studies focused on monitoring surface water temperature, TSS and CDOM.</p>
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<p>Topical concepts in monitoring water quality utilising UAV-derived remotely sensed data using information from abstracts, titles and keywords from literature.</p>
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<p>The frequency of studies per year based on both satellite sensors and UAVs.</p>
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<p>Percentage of each water quality parameter from the total number of selected studies.</p>
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<p>Frequency of studies relating to UAV platform types across a temporal scale.</p>
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<p>Frequency of sensor types used onboard drone platforms for detecting water temperature, TSS and CDOM.</p>
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<p>Indices used to delineate water bodies from surrounding vegetation. (NDVI = Normalised Difference Vegetation Index; NDWI = Normalised Difference Water Index; WRI = Water Ratio Index; NDREI = Normalised Difference Red Edge Index; AWEI = Automated Water Extraction Index; MNDWI = Modified Normalised Difference Water Index).</p>
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<p>Machine learning algorithms used to detect and map surface water temperature, TSS, and CDOM. (IMP-MPP = improved matching pixel by pixel; LSTM = Long Short-Term Memory; LASSO = Least Absolute Shrinkage and Selection Operator; GBDT = Gradient Boost Decision Trees; DNN = Deep Neural Networks; ANN = Artificial Neural Networks; SVM = Support Vector Machines; RF = Random Forest; LR = Linear Regression).</p>
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<p>Average error assessment of machine learning algorithms.</p>
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18 pages, 11301 KiB  
Article
Integration of Optical Remote Sensing and Laser Point Cloud for Forest Stock Estimation in Karst Mountainous Areas
by Jiajia Zheng, Zhongfa Zhou, Meng Zhu, Jiale Wang, Jiaxue Wan and Yangyang Long
Forests 2024, 15(12), 2106; https://doi.org/10.3390/f15122106 - 28 Nov 2024
Viewed by 497
Abstract
This study addresses the challenges posed by the complex topography and forest structure in karst mountainous areas, as well as the difficulties in estimating forest stock using traditional methods. We propose a method that integrates optical remote sensing data from Sentinel-2 into airborne [...] Read more.
This study addresses the challenges posed by the complex topography and forest structure in karst mountainous areas, as well as the difficulties in estimating forest stock using traditional methods. We propose a method that integrates optical remote sensing data from Sentinel-2 into airborne LiDAR data to estimate forest stock in karst areas. First, an Allometric Growth Model correlating tree height and diameter at breast height (DBH) in karst areas was developed based on field measurements. Tree height information extracted from LiDAR data was then combined with the binary wood volume model specific to fir trees in Guizhou Province to calculate the individual tree biomass of fir trees. In addition, this study evaluated the robustness of three machine learning methods, the Random Forest Regression Model, K-Nearest Neighbors Regression Model, and Backpropagation Neural Network Model, in estimating forest stock in karst mountainous areas. The results indicate the following: (1) The Allometric Growth Model based on field data showed strong predictive power for DBH and can be used for large-scale estimation. (2) The distribution characteristics of individual tree biomass and plot biomass under different site conditions revealed the distribution pattern of fir trees in the study area, providing important information for understanding the growth status of forest stock in the region. (3) The Random Forest Regression Model demonstrated exceptional accuracy, generalization capability, and robustness in the estimation of forest stock within karst mountainous regions. This study provides an effective technical tool for estimating forest stock in karst areas and under complex terrain conditions and has significant scientific value and practical implications for the monitoring and management of forest ecosystem carbon sinks. Full article
(This article belongs to the Section Forest Inventory, Modeling and Remote Sensing)
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<p>Overview map of the study area. (<b>a</b>) Geographic location of the study area. (<b>b</b>) Map showing the RGB of the four ALS sample plots. (<b>c</b>) Map of tree growth in the sample plots.</p>
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<p>Diagram of the LiDAR data processing process.</p>
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<p>DBH-H nonlinear curve fitting plot.</p>
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<p>Distribution of individual wood volume.</p>
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<p>Distribution of storage volume in sample plots.</p>
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<p>Correlation analysis between accumulation and factors.</p>
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<p>Comparison of the estimated and true values of the 3 models. (<b>a</b>) RF Model. (<b>b</b>) KNN Model. (<b>c</b>) BP Model.</p>
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23 pages, 3752 KiB  
Article
Characterization of Phytoplankton Composition in Lake Maggiore: Integrated Chemotaxonomy for Enhanced Cyanobacteria Detection
by Elisabetta Canuti and Martina Austoni
Microorganisms 2024, 12(11), 2211; https://doi.org/10.3390/microorganisms12112211 - 31 Oct 2024
Viewed by 692
Abstract
Cyanobacterial blooms in lakes have increased in frequency and intensity over the past two decades, negatively affecting ecological and biogeochemical processes. This study focuses on the phytoplankton composition of Lake Maggiore, with a special emphasis on cyanobacteria detection through pigment composition. While microscopy [...] Read more.
Cyanobacterial blooms in lakes have increased in frequency and intensity over the past two decades, negatively affecting ecological and biogeochemical processes. This study focuses on the phytoplankton composition of Lake Maggiore, with a special emphasis on cyanobacteria detection through pigment composition. While microscopy is the standard method for phytoplankton identification, pigment-based methods provide broader spatiotemporal coverage. Between May and September 2023, five measurement campaigns were conducted in Lake Maggiore, collecting bio-geochemical and bio-optical data at 27 stations. The total Chlorophyll-a (TChl a) was measured, with concentrations ranging from 1.13 to 6.9 mg/m3. Phytoplankton pigment composition was analyzed using High-Performance Liquid Chromatography (HPLC) and the CHEMTAX approach was applied for phytoplankton classification. The results were cross-validated using Principal Component Analysis (PCA), Hierarchical Cluster Analysis (HCA), and microscopic counts. Cyanobacteria were identified based on unique pigment markers, such as carotenoids. The HPLC-derived pigment classification results aligned well with both PCA and HCA and microscopic counts verified the accuracy of the pigment-based chemotaxonomy. The study demonstrates that pigment-based classification methods, when combined with statistical analyses, offer a reliable alternative for identifying cyanobacteria and other phytoplankton groups, with potential applications in support of remote sensing algorithm development. Full article
(This article belongs to the Special Issue Phytoplankton and Environment Interactions)
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<p>Spatial distribution of the LM23 collecting stations: the size is proportional to the TChl <span class="html-italic">a</span> content.</p>
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<p>Boxplot of the pigment concentrations log<sub>10</sub>-transformed) of Lake Maggiore 2023 (LM23) campaigns. Each box shows the interquartile range (IQR), with the central line indicating the median concentration. Whiskers extend to 1.5 times the IQR, with outliers represented by dots beyond this range.</p>
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<p>The log–log correlation TAcc/TChl <span class="html-italic">a</span> along the five Lake Maggiore Campaigns; the axis in log scale (mg/m<sup>3</sup>). The green dots are the 27 stations of the five campaigns on Lake Maggiore.</p>
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<p>Ternary plot of functional Indices pPF, nPF, and mPF for LM23 campaigns.</p>
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<p>Hierarchical clustering of phytoplankton pigment ratios to TChl <span class="html-italic">a</span> for the LM23 dataset. The three-seizes major pigment communities (micro-, nano-, and pico-phytoplankton, from left to right) are identified based on a linkage distance cutoff of 0.5 (red dashed line).</p>
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<p>The loadings corresponding to the principal component modes for the pigments ratio to the TChl <span class="html-italic">a</span> are shown in panels (<b>a</b>–<b>d</b>) for the LM23 dataset.</p>
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<p>The algal group composition at various stations in Lake Maggiore is determined by CHEMTAX analysis, with each bar representing a specific station. The height of each bar indicates the TChl <span class="html-italic">a</span> concentration in mg/m<sup>3</sup>, and the stations are organized chronologically from May to October, as indicated by the vertical dashed lines separating each month.</p>
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<p>CHEMTAX distribution (<b>a</b>) and corresponding microscopy determination (<b>b</b>) for matched stations.</p>
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<p>Dominant phytoplankton groups at each station as identified by Network (<b>a</b>) and CHEMTAX (<b>b</b>) analysis. Stations are color-coded to indicate the prevailing algal groups: red for diatoms, green for Chrysophyceae, yellow for Cryptophyceae, and blue for pico-nano mixed fraction (only in Network analysis).</p>
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24 pages, 12756 KiB  
Article
An Empirical Algorithm for Estimating the Absorption of Colored Dissolved Organic Matter from Sentinel-2 (MSI) and Landsat-8 (OLI) Observations of Coastal Waters
by Vu Son Nguyen, Hubert Loisel, Vincent Vantrepotte, Xavier Mériaux and Dinh Lan Tran
Remote Sens. 2024, 16(21), 4061; https://doi.org/10.3390/rs16214061 - 31 Oct 2024
Viewed by 955
Abstract
Sentinel-2/MSI and Landsat-8/OLI sensors enable the mapping of ocean color-related bio-optical parameters of surface coastal and inland waters. While many algorithms have been developed to estimate the Chlorophyll-a concentration, Chl-a, and the suspended particulate matter, SPM, from OLI and MSI data, the absorption [...] Read more.
Sentinel-2/MSI and Landsat-8/OLI sensors enable the mapping of ocean color-related bio-optical parameters of surface coastal and inland waters. While many algorithms have been developed to estimate the Chlorophyll-a concentration, Chl-a, and the suspended particulate matter, SPM, from OLI and MSI data, the absorption by colored dissolved organic matter, acdom, a key parameter to monitor the concentration of dissolved organic matter, has received less attention. Herein we present an inverse model (hereafter referred to as AquaCDOM) for estimating acdom at the wavelength 412 nm (acdom (412)), within the surface layer of coastal waters, from measurements of ocean remote sensing reflectance, Rrs (λ), for these two high spatial resolution (around 20 m) sensors. Combined with a water class-based approach, several empirical algorithms were tested on a mixed dataset of synthetic and in situ data collected from global coastal waters. The selection of the final algorithms was performed with an independent validation dataset, using in situ, synthetic, and satellite Rrs (λ) measurements, but also by testing their respective sensitivity to typical noise introduced by atmospheric correction algorithms. It was found that the proposed algorithms could estimate acdom (412) with a median absolute percentage difference of ~30% and a median bias of 0.002 m−1 from the in situ and synthetic datasets. While similar performances have been shown with two other algorithms based on different methodological developments, we have shown that AquaCDOM is much less sensitive to atmospheric correction uncertainties, mainly due to the use of band ratios in its formulation. After the application of the top-of-atmosphere gains and of the same atmospheric correction algorithm, excellent agreement has been found between the OLI- and MSI-derived acdom (412) values for various coastal areas, enabling the application of these algorithms for time series analysis. An example application of our algorithms for the time series analysis of acdom (412) is provided for a coastal transect in the south of Vietnam. Full article
(This article belongs to the Special Issue Remote Sensing Band Ratios for the Assessment of Water Quality)
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Graphical abstract

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<p>Global distribution of the in situ (red triangles) and match-up dataset for a<sub>cdom</sub> (λ) (green triangles) and for both <span class="html-italic">R</span><sub>rs</sub> (λ) and a<sub>cdom</sub> (λ) (blue triangles) data points. The squares represent the locations of Landsat-8 and Sentinel-2 near-simultaneous nadir-captured image pairs used for the calibration of a<sub>cdom</sub> (412) product (black squares) and the time series analysis (blue squares).</p>
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<p>The RGB of Landsat-8 (dimmed image) and Sentinel-2 (bounded by black box) images used for algorithm sensitivity analysis. The red line is the transect in front of the Ganh Hao River in Vietnam.</p>
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<p>Flowchart of the water classification method proposed in this study.</p>
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<p>Histograms of the a<sub>cdom</sub> (412) values for (<b>a</b>) DSM, (<b>b</b>) DSM-1 (i.e., Class 1), and (<b>c</b>) DSM-2 (i.e., Class 2).</p>
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<p>Comparison of ACOLITE-derived and measured values of <span class="html-italic">R</span><sub>rs</sub> (λ) from the (<b>a</b>) OLI and (<b>b</b>) MSI 10 m spatial resolution (right) match-up dataset. The different statistical indicators calculated for the data of ACOLITE-derived versus measured <span class="html-italic">R</span><sub>rs</sub> (λ) are provided (see text for details). The solid line is the 1:1 line. The different colors stand for a given wavelength.</p>
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<p>Radar plots summarizing the performances of the different a<sub>cdom</sub> (412) algorithms as indicated for (<b>a</b>) MSI and Class 1 water, (<b>b</b>) MSI and Class 2 water, (<b>c</b>) OLI and Class 1 waters, and (<b>d</b>) OLI and Class 2 waters. The number following the algorithm name represents the value of the surface of the polygon (the smaller the value the better the algorithm performs).</p>
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<p>The OLI maps of the standard deviation of modeled a<sub>cdom</sub> (412) for the algorithm combinations listed in <a href="#remotesensing-16-04061-t002" class="html-table">Table 2</a>. The name of the algorithm for each water class in each combination is displayed at the top of each map from (<b>a</b>–<b>e</b>).</p>
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<p>The MSI maps of the standard deviation of modeled a<sub>cdom</sub> (412) at a 60 m spatial resolution for the algorithm combinations listed in <a href="#remotesensing-16-04061-t003" class="html-table">Table 3</a>. The name of the algorithm for each water class in each combination is displayed at the top of each individual map from (<b>a</b>–<b>f</b>).</p>
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<p>Comparison of AquaCDOM-derived and measured values of a<sub>cdom</sub> (412) for OLI (top row) and MSI (bottom row) from the DSM-D (panels (<b>a</b>,<b>d</b>)) and DSM-V (panels (<b>b</b>,<b>e</b>)) datasets. Histograms of the derived and measured a<sub>cdom</sub> (412) values from DSM-V for OLI and MSI are shown in (<b>c</b>,<b>f</b>), respectively. The different statistical indicators calculated for the data of AquaCDOM-derived and measured a<sub>cdom</sub> (412) are provided (see text for details). The percentage of retrieved data points is indicated in brackets. The solid line is the 1:1 line. The different colors stand for different water classes as indicated.</p>
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<p>Comparison of AquaCDOM-derived and measured values of a<sub>cdom</sub> (412) for OLI from the (<b>a</b>) DSM-V and (<b>b</b>) Mu-CDOM datasets. (<b>c</b>) Map of the standard deviation of the AquaCDOM-derived a<sub>cdom</sub> (412) values. Comparison of SAVE-derived and measured values of a<sub>cdom</sub> (412) for OLI from the (<b>d</b>) DSM-V and (<b>e</b>) Mu-CDOM datasets. (<b>f</b>) Map of the standard deviation of the SAVE-derived a<sub>cdom</sub> (412) values. The different statistical indicators calculated for the data of model-derived versus measured a<sub>cdom</sub> (412) values are provided (see text for details). The percentage of retrieved data points is indicated in brackets. The solid line is the 1:1 line. The different colors stand for different water classes as indicated.</p>
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<p>Same as <a href="#remotesensing-16-04061-f010" class="html-fig">Figure 10</a> but for MSI.</p>
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<p>Comparison of AquaCDOM-derived and measured values of a<sub>cdom</sub> (440) for OLI from the (<b>a</b>) DSM-V and (<b>b</b>) Mu-CDOM datasets. (<b>c</b>) Map of the standard deviation of the AquaCDOM-derived a<sub>cdom</sub> (440) values. Comparison of MDN-derived and measured values of a<sub>cdom</sub> (440) for OLI from the (<b>d</b>) DSM-V and (<b>e</b>) Mu-CDOM datasets. (<b>f</b>) Map of the standard deviation of the MDN-derived a<sub>cdom</sub> (440) values. The different statistical indicators calculated for the data of model-derived versus measured a<sub>cdom</sub> (440) are provided (see text for details). The percentage of retrieved data points is indicated in brackets. The solid line is the 1:1 line. The different colors stand for different water classes as indicated.</p>
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<p>Same as <a href="#remotesensing-16-04061-f012" class="html-fig">Figure 12</a> but for MSI.</p>
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<p>Comparison of OLI-derived and MSI-derived a<sub>cdom</sub> (412) values over the 11 near-simultaneous acquisition scenes. The different statistical indicators calculated for the data of OLI-derived versus MSI-derived a<sub>cdom</sub> (412) are provided.</p>
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<p>(<b>a</b>) Temporal variability of a<sub>cdom</sub> (412) in Ganh Hao transect (<a href="#remotesensing-16-04061-f002" class="html-fig">Figure 2</a>) in relation to the (<b>b</b>) monthly accumulated rainfall (in mm) and (<b>c</b>) the monthly mean intraday high and low tide height difference (in m).</p>
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<p>Location of the a<sub>cdom</sub> (412) match-up data points (purple triangles) for OLCI on Sentinel-3. In situ a<sub>cdom</sub> (412) measurements were extracted from SeaBASS.</p>
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<p>Comparison of AquaCDOM-derived and measured values of a<sub>cdom</sub> (412) for the OLCI match-up dataset presented in <a href="#remotesensing-16-04061-f0A1" class="html-fig">Figure A1</a>.</p>
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<p>(<b>a</b>) An RGB composite of an OLI image over a Vietnam coastal area. The black line represents the transect along which the a<sub>cdom</sub> (412) value estimated from AquaCDOM is extracted. The location of the boundary between the two water classes is shown by a white dot. (<b>b</b>) The spatial distribution of the two water classes used in this study. (<b>c</b>) The a<sub>cdom</sub> (412) spatial distribution estimated from the AquaCDOM algorithm. (<b>d</b>) The a<sub>cdom</sub> (412) values along the cross-shore transect. The red line shows the spatial delimitation between the two water classes along the cross-shore transect.</p>
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38 pages, 18360 KiB  
Review
A Review of Rotational Seismology Area of Interest from a Recording and Rotational Sensors Point of View
by Anna T. Kurzych and Leszek R. Jaroszewicz
Sensors 2024, 24(21), 7003; https://doi.org/10.3390/s24217003 - 31 Oct 2024
Viewed by 2298
Abstract
This article reviews rotational seismology, considering different areas of interest, as well as measuring devices used for rotational events investigations. After a short theoretical description defining the fundamental parameters, the authors summarized data published in the literature in areas such as the indirect [...] Read more.
This article reviews rotational seismology, considering different areas of interest, as well as measuring devices used for rotational events investigations. After a short theoretical description defining the fundamental parameters, the authors summarized data published in the literature in areas such as the indirect numerical investigation of rotational effects, rotation measured during earthquakes, teleseismic wave investigation, rotation induced by artificial explosions, and mining activity. The fundamental data on the measured rotation parameters and devices used for the recording are summarized and compared for the above areas. In the section on recording the rotational effects associated with artificial explosions and mining activities, the authors included results recorded by a rotational seismograph of their construction—FOSREM (fibre-optic system for rotational events and phenomena monitoring). FOSREM has a broad range of capabilities to measure rotation rates, from several dozen nrad/s to 10 rad/. It can be controlled remotely and operated autonomously for a long time. It is a useful tool for systematic seismological investigations in various places. The report concludes with a short discussion of the importance of rotational seismology and the great need to obtain experimental data in this field. Full article
(This article belongs to the Section Remote Sensors)
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Figure 1
<p>Observation of structural damages after earthquakes: (<b>a</b>) pictures of rotated objects in downtown L’Aquila with non-coherent directions of rotation (both clockwise and counter-clockwise) caused by the 2009 L’Aquila (central Italy) earthquake [<a href="#B12-sensors-24-07003" class="html-bibr">12</a>]; (<b>b</b>) damages in buildings after 21 September 1999, a strong earthquake of 7.3 in the central part of Taiwan, presented in the 921 Earthquake Museum of Taiwan; and (<b>c</b>) example of an overall rotation of the base of the structure with an overturning motion [<a href="#B14-sensors-24-07003" class="html-bibr">14</a>] during 1999 Kocaeli earthquake, Turkey.</p>
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<p>The Cartesian coordinate system for translational (<span class="html-italic">V<sub>x</sub></span>, <span class="html-italic">V<sub>y</sub></span>, <span class="html-italic">V<sub>z</sub></span>) and rotational (<span class="html-italic">ω<sub>x</sub></span>, <span class="html-italic">ω<sub>y</sub></span>, <span class="html-italic">ω<sub>z</sub></span>) velocity components.</p>
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<p>The rotational rate peak amplitude versus epicentral distance (<b>a</b>), and magnitude (<b>b</b>) based on data presented in [<a href="#B102-sensors-24-07003" class="html-bibr">102</a>].</p>
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<p>The peak rotational velocity recorded by the R-1 based on [<a href="#B64-sensors-24-07003" class="html-bibr">64</a>] for 52 local earthquakes at the HGSD station in eastern Taiwan as a function of (<b>a</b>) sensor’s distance and (<b>b</b>) earthquake magnitude.</p>
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<p>The rotational rate peak amplitude versus epicentral distance (<b>a</b>) and magnitude (<b>b</b>) based on data presented in [<a href="#B111-sensors-24-07003" class="html-bibr">111</a>].</p>
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<p>Recording of rotational component around the vertical axis (solid line) and transverse acceleration (dashed), measured by C-II and EARSS/40T, respectively, during the New Ireland earthquake, 19 January 1999 03:35:33.8 (magnitude 7.0) [<a href="#B88-sensors-24-07003" class="html-bibr">88</a>].</p>
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<p>The rotational rate peak amplitude versus epicentral distance (<b>a</b>) and magnitude (<b>b</b>) based on data presented in [<a href="#B90-sensors-24-07003" class="html-bibr">90</a>].</p>
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<p>ROMY at the Geophysical Observatory, Fürstenfeldbruck, Germany: (<b>a</b>) top view from the ground, (<b>b</b>) the schema of the ROMY [<a href="#B124-sensors-24-07003" class="html-bibr">124</a>].</p>
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<p>Rotational seismometer METR-03 [<a href="#B148-sensors-24-07003" class="html-bibr">148</a>] used in the experiment presented in [<a href="#B142-sensors-24-07003" class="html-bibr">142</a>].</p>
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<p>Examples of data recorded during microshocks by FOSREM-1 and -2 in Książ, Poland with an absolute maximum signal amplitude equal to: (<b>a</b>) 3.41 mrad/s (FOSREM-1), 3.13 mrad/s (FOSREM-2); (<b>b</b>) 0.0081 mrad/s (FOSREM-1), 0.0075 mrad/s (FOSREM-2); (<b>c</b>) 0.022 marad/s (FOSREM-1), 0.021 mrad/s (FOSREM-2); (<b>d</b>) 0.02 mrad/s (FOSREM-1), 0.017 mrad/s (FOSREM-2).</p>
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<p>“Rotation and strain in Seismology: A comparative Sensor Test“, which took place in Geophysical Observatory Fürstenfeldbruck, Germany: (<b>a</b>) the gathered rotational sensors in the bunker, (<b>b</b>) view of the test field during sensors installation, and (<b>c</b>) the data recorded by FOSREMs (type FOS5-01,-02) on the 19 November 2019.</p>
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<p>The examples of the torsion (<b>a</b>,<b>b</b>) and tilt (<b>c</b>,<b>d</b>) recordings in the frequency range from DC to 10.25 Hz detected by FOSREM-1/-2 from 12/01/2017 to 18/01/2018 at Książ observatory, Poland.</p>
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30 pages, 11775 KiB  
Article
Predictive Modelling of Land Cover Changes in the Greater Amanzule Peatlands Using Multi-Source Remote Sensing and Machine Learning Techniques
by Alex Owusu Amoakoh, Paul Aplin, Pedro Rodríguez-Veiga, Cherith Moses, Carolina Peña Alonso, Joaquín A. Cortés, Irene Delgado-Fernandez, Stephen Kankam, Justice Camillus Mensah and Daniel Doku Nii Nortey
Remote Sens. 2024, 16(21), 4013; https://doi.org/10.3390/rs16214013 - 29 Oct 2024
Viewed by 1246
Abstract
The Greater Amanzule Peatlands (GAP) in Ghana is an important biodiversity hotspot facing increasing pressure from anthropogenic land-use activities driven by rapid agricultural plantation expansion, urbanisation, and the burgeoning oil and gas industry. Accurate measurement of how these pressures alter land cover over [...] Read more.
The Greater Amanzule Peatlands (GAP) in Ghana is an important biodiversity hotspot facing increasing pressure from anthropogenic land-use activities driven by rapid agricultural plantation expansion, urbanisation, and the burgeoning oil and gas industry. Accurate measurement of how these pressures alter land cover over time, along with the projection of future changes, is crucial for sustainable management. This study aims to analyse these changes from 2010 to 2020 and predict future scenarios up to 2040 using multi-source remote sensing and machine learning techniques. Optical, radar, and topographical remote sensing data from Landsat-7, Landsat-8, ALOS/PALSAR, and Shuttle Radar Topography Mission derived digital elevation models (DEMs) were integrated to perform land cover change analysis using Random Forest (RF), while Cellular Automata Artificial Neural Networks (CA-ANNs) were employed for predictive modelling. The classification model achieved overall accuracies of 93% in 2010 and 94% in both 2015 and 2020, with weighted F1 scores of 80.0%, 75.8%, and 75.7%, respectively. Validation of the predictive model yielded a Kappa value of 0.70, with an overall accuracy rate of 80%, ensuring reliable spatial predictions of future land cover dynamics. Findings reveal a 12% expansion in peatland cover, equivalent to approximately 6570 ± 308.59 hectares, despite declines in specific peatland types. Concurrently, anthropogenic land uses have increased, evidenced by an 85% rise in rubber plantations (from 30,530 ± 110.96 hectares to 56,617 ± 220.90 hectares) and a 6% reduction in natural forest cover (5965 ± 353.72 hectares). Sparse vegetation, including smallholder farms, decreased by 35% from 45,064 ± 163.79 hectares to 29,424 ± 114.81 hectares. Projections for 2030 and 2040 indicate minimal changes based on current trends; however, they do not consider potential impacts from climate change, large-scale development projects, and demographic shifts, necessitating cautious interpretation. The results highlight areas of stability and vulnerability within the understudied GAP region, offering critical insights for developing targeted conservation strategies. Additionally, the methodological framework, which combines optical, radar, and topographical data with machine learning, provides a robust approach for accurate and detailed landscape-scale monitoring of tropical peatlands that is applicable to other regions facing similar environmental challenges. Full article
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<p>Study area map: (<b>a</b>) agro-ecological zones and the regional administrative boundaries of Ghana; (<b>b</b>) identified patchy peatlands and communities fringing them, as well as the district administrative boundaries in the GAP. Peatland information was obtained from Hen Mpoano’s data repository and is based on participatory GIS and ground truthing approach. Basemap: Google Hybrid, Map data (© 2023 Google).</p>
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<p>Digital elevation model (DEM) of the study area showing the Amanzule, Tano, and Ankobra rivers. The colour gradients represent variations in terrain elevation, with the scale indicating relative heights in meters above sea level (Source: authors’ own creation using SRTM-derived DEM data accessed via Google Earth Engine).</p>
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<p>Workflow for land cover change analysis using multi-sensor data, featuring model building with Random Forest (RF) classification, feature optimisation through Recursive Feature Elimination (RFE), and GIS-based land cover projection.</p>
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<p>Plot of accuracy vs. number of image features.</p>
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<p>Feature importance scores of selected image features following RFE. Original bands, texture, spectral indices, and terrain features were chosen based on the number of features that retained optimal accuracy.</p>
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<p>Land cover changes in the GAP between 2010, 2015, and 2020.</p>
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<p>Land cover maps for GAP from (<b>a</b>) 2010, (<b>b</b>) 2015, and (<b>c</b>) 2020.</p>
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<p>Sankey diagram showing dynamic land cover transitions in the GAP: (<b>a</b>) represents transitions from 2010 to 2015 and (<b>b</b>) depicts changes from 2015 to 2020.</p>
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<p>Early growth stages of replanted mangroves in GAP (Source: Hen Mpoano, [<a href="#B20-remotesensing-16-04013" class="html-bibr">20</a>]).</p>
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18 pages, 5084 KiB  
Article
Activation of Ms 6.9 Milin Earthquake on Sedongpu Disaster Chain, China with Multi-Temporal Optical Images
by Yubin Xin, Chaoying Zhao, Bin Li, Xiaojie Liu, Yang Gao and Jianqi Lou
Remote Sens. 2024, 16(21), 4003; https://doi.org/10.3390/rs16214003 - 28 Oct 2024
Viewed by 619
Abstract
In recent years, disaster chains caused by glacier movements have occurred frequently in the lower Yarlung Tsangpo River in southwest China. However, it is still unclear whether earthquakes significantly contribute to glacier movements and disaster chains. In addition, it is difficult to measure [...] Read more.
In recent years, disaster chains caused by glacier movements have occurred frequently in the lower Yarlung Tsangpo River in southwest China. However, it is still unclear whether earthquakes significantly contribute to glacier movements and disaster chains. In addition, it is difficult to measure the high-frequency and large gradient displacement time series with optical remote sensing images due to cloud coverage. To this end, we take the Sedongpu disaster chain as an example, where the Milin earthquake, with an epicenter 11 km away, occurred on 18 November 2017. Firstly, to deal with the cloud coverage problem for single optical remote sensing analysis, we employed multiple platform optical images and conducted a cross-platform correlation technique to invert the two-dimensional displacement rate and the cumulative displacement time series of the Sedongpu glacier. To reveal the correlation between earthquakes and disaster chains, we divided the optical images into three classes according to the Milin earthquake event. Lastly, to increase the accuracy and reliability, we propose two strategies for displacement monitoring, that is, a four-quadrant block registration strategy and a multi-window fusion strategy. Results show that the RMSE reduction percentage of the proposed registration method reaches 80%, and the fusion method can retrieve the large magnitude displacements and complete displacement field. Secondly, the Milin earthquake accelerated the Sedongpu glacier movement, where the pre-seismic velocities were less than 0.5 m/day, the co-seismic velocities increased to 1 to 6 m/day, and the post-seismic velocities decreased to 0.5 to 3 m/day. Lastly, the earthquake had a triggering effect around 33 days on the Sedongpu disaster chain event on 21 December 2017. The failure pattern can be summarized as ice and rock collapse in the source area, large magnitude glacier displacement in the moraine area, and a large volume of sediment in the deposition area, causing a river blockage. Full article
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<p>Overview of the study area. (<b>a</b>) Image footprints of the Sentinel-2 (S2), Beijing-2 (BJ-2), and SuperView-1 (SV-1) used in this study with a shaded 30 m Shuttle Radar Topography Mission (SRTM) digital elevation model (DEM) as the background. Fault data and seismicity activities with a magnitude above four were downloaded from the Chinese Earthquake Network Center (<a href="http://www.ceic.ac.cn/" target="_blank">http://www.ceic.ac.cn/</a>, accessed on 20 December 2023). (<b>b</b>) Enlarged topography of the Sedongpu Basin. The black line defines the extent of the Sedongpu basin, the yellow and green rectangles represent two representative stable areas, and the red line represents the profile A-B-C-D along the glacier flow direction.</p>
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<p>Flowchart of pre-, co-, and post-seismic glacier displacement monitoring and accuracy evaluation with multi-temporal optical image correlation.</p>
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<p>Technical flowchart of the four-quadrant block image registration method.</p>
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<p>Optical image correlation results for image pair acquired on 7 November 2017 and 21 December 2017 with different registration strategies. The first row (<b>a</b>–<b>d</b>) is block diagrams, the second row (<b>e</b>–<b>h</b>) is the north–south results, and the third row (<b>i</b>–<b>l</b>) is the east–west results. (<b>e</b>,<b>i</b>) are the results without registration, (<b>f</b>,<b>j</b>) are the results after overall registration, (<b>g</b>,<b>k</b>) are the results after top and bottom block registration, and (<b>h</b>,<b>l</b>) are the results after four-quadrant block registration.</p>
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<p>The accuracy evaluation of four registration methods was conducted over two stable areas indicated in <a href="#remotesensing-16-04003-f001" class="html-fig">Figure 1</a>. (<b>a</b>,<b>b</b>) are the Mean Value (MEV) and Standard Deviation (STD) of the N–S and E–W displacement in the green and yellow regions, respectively. (<b>c</b>,<b>d</b>) are the reduction percentage of Root Mean Square Error (RMSE) in the green and yellow areas, respectively.</p>
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<p>Optical image correlation results with different window sizes. (<b>a</b>–<b>d</b>) are north–south results, (<b>e</b>–<b>h</b>) are east–west results, (<b>i</b>–<b>l</b>) are fusion results from different window sizes shown in 2D and 3D DEM.</p>
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<p>Accuracy evaluation for different window sizes was conducted over two stable areas indicated in <a href="#remotesensing-16-04003-f001" class="html-fig">Figure 1</a>. (<b>a</b>,<b>b</b>) the MEV and STD of the N–S and E–W displacement; (<b>c</b>,<b>d</b>) the RMSE reduction percentage in the green and yellow areas, respectively.</p>
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<p>Displacement magnitudes and directions for three stages during the pre-, co-, and post-seismic periods. (<b>a</b>) Show the gully distribution with I–V and the direction of the glacial displacement. (<b>b</b>–<b>d</b>) are the pre-seismic displacement field from Sentinel-2 images, (<b>e</b>) the co-seismic high-resolution displacement field, (<b>f</b>) the post-seismic displacement field from Sentinel-2 images.</p>
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<p>Displacement rate maps and the profile of Sedongpu Glacier at three stages. (<b>a</b>–<b>c</b>) the daily displacement during the pre-, co-, and post-seismic periods, respectively. (<b>d</b>) The profile of daily displacement rate during three stages. The three sections are separated by dashed lines, with section I corresponding to AB, section II to BC, and section III to CD.</p>
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<p>(<b>a</b>,<b>b</b>) are Planet satellite images from 21 December and 26 December 2017, respectively, used to observe changes before and after the disaster chain. (<b>c</b>) The schematic diagram of longitudinal section in Sedongpu. (<b>d</b>) The failure pattern of the Sedongpu disaster chain.</p>
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20 pages, 17607 KiB  
Article
Remote Sensing Evaluation of Trophic Status in the Daihai Lake Based on Fuzzy Classification
by Fang Wang, Song Qing, Chula Sa, Quan Lai and An Chang
Water 2024, 16(21), 3032; https://doi.org/10.3390/w16213032 - 23 Oct 2024
Viewed by 596
Abstract
Trophic state index (TSI) is a critical ecological and environmental issue in water resource management that has garnered significant attention. Given the complexity of optical characteristics in aquatic environments, this study employs fuzzy classification methods (FCM) and composite nutrient status indices to meticulously [...] Read more.
Trophic state index (TSI) is a critical ecological and environmental issue in water resource management that has garnered significant attention. Given the complexity of optical characteristics in aquatic environments, this study employs fuzzy classification methods (FCM) and composite nutrient status indices to meticulously classify in-situ remote sensing reflectance data, aiming to develop evaluation models for different nutrient status categories to facilitate the assessment of the Daihai River in Inner Mongolia, China. Subsequently, we applied this model to MSI data to analyze the nutrient status of Daihai Lake from 2016 to 2021. Furthermore, a structural equation model (SEM) was utilized to explore the primary driving factors influencing nutrient status. The results indicated that the water bodies in Daihai Lake can be broadly classified into three categories, with the nutrient status models demonstrating robust performance for each category (R2 = 0.80, R2 = 0.83, and R2 = 0.74). Comparisons were made between nutrient status accuracies obtained through the NCM and FCM based on measured data, yielding R2 values of 0.74 and 0.85, respectively. Furthermore, the TSI results derived from MSI inversion were validated, with NCM achieving an R2 of 0.49, RMSE of 6.88, and MAPE of 10.36%, while FCM exhibited an R2 of 0.55, RMSE of 8.89, and MAPE of 13.18%. An SEM–based analysis revealed that over the long term, human activities exerted a more substantial impact on eutrophication in Daihai Lake, while climatic factors played an accelerating and reinforcing role. These results are consistent with prior research in the Daihai area, indicating a state of mild eutrophication and the potential of the fuzzy classification method and comprehensive trophic status index method in eutrophication assessment. Full article
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<p>Locations of the Daihai Lake and sampling sites.</p>
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<p>Flow chart of the study process.</p>
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<p>Classification of measured remote sensing reflectance classification. (<b>a</b>) The distribution of all spectral data. (<b>b</b>) The central spectrum of each of the three classes after performing fuzzy classification on all spectral data. (<b>c</b>–<b>e</b>): The distribution of spectral data for the three groups, with sample sizes of 9, 54, and 93, respectively.</p>
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<p>Accuracy test of the NCM method.</p>
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<p>Accuracy test of the FCM method.</p>
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<p>Atmospheric correction.Comparison of in-situ measured reflectance and satellite-derived reflectance for different dates at the site.</p>
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<p>Comparison of in situ TSI and remote sensing retrieval.</p>
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<p>Optical classification and model application of remote sensing image water bodies. The black circles highlights the regions where differences exist between the two images.</p>
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<p>TSI monthly spatial variation.</p>
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<p>TSI annual spatial variation.</p>
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<p>Trend analysis of factors influencing trophic status (<b>a</b>) and structural equation models (<b>b</b>).</p>
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<p>Distribution of membership degree from fuzzy clustering algorithms.The horizontal axis represents the water body types.</p>
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18 pages, 12989 KiB  
Article
Design of Exterior Orientation Parameters Variation Real-Time Monitoring System in Remote Sensing Cameras
by Hongxin Liu, Chunyu Liu, Peng Xie and Shuai Liu
Remote Sens. 2024, 16(21), 3936; https://doi.org/10.3390/rs16213936 - 23 Oct 2024
Viewed by 713
Abstract
The positional accuracy of satellite imagery is essential for remote sensing cameras. However, vibrations and temperature changes during launch and operation can alter the exterior orientation parameters of remote sensing cameras, significantly reducing image positional accuracy. To address this issue, this article proposes [...] Read more.
The positional accuracy of satellite imagery is essential for remote sensing cameras. However, vibrations and temperature changes during launch and operation can alter the exterior orientation parameters of remote sensing cameras, significantly reducing image positional accuracy. To address this issue, this article proposes an exterior orientation parameter variation real-time monitoring system (EOPV-RTMS). This system employs lasers to establish a full-link active optical monitoring path, which is free from time and space constraints. By simultaneously receiving star and laser signals with the star tracker, the system monitors changes in the exterior orientation parameters of the remote sensing camera in real time. Based on the in-orbit calibration geometric model, a new theoretical model and process for the calibration of exterior orientation parameters are proposed, and the accuracy and effectiveness of the system design are verified by ground experiments. The results indicate that, under the condition of a centroid extraction error of 0.1 pixel for the star tracker, the EOPV-RTMS achieves a measurement accuracy of up to 0.6″(3σ) for a single image. Displacement variation experiments validate that the measurement error of the system deviates by at most 0.05″ from the theoretical calculation results. The proposed EOPV-RTMS provides a new design solution for improving in-orbit calibration technology and image positional accuracy. Full article
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<p>Exterior orientation parameters variation real-time monitoring system layout.</p>
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<p>Laser propagation path in the EOPV-RTMS.</p>
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<p>Laser relay system layout.</p>
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<p>Transmission and reflectivity curves of the narrow band-pass filter and dichroic mirror.</p>
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<p>EOPV-RTMS calibration process.</p>
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<p>Simplification of the exterior orientation parameters variation real-time monitoring system model.</p>
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<p>Impact of star tracker centroid extraction errors on the measurement accuracy of the EOPV-RTMS.</p>
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<p>Measurement accuracy of the EOPV-RTMS (centroid extraction error of star tracker ≤ 0.1 pixel).</p>
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<p>Verification platform for the EOPV-RTMS.</p>
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<p>Laser image points from four lasers in the star tracker.</p>
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<p>Measurement accuracy of the EOPV-RTMS.</p>
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<p>Measurement results of exterior orientation parameters changes during focal plane movement along the X/Y axis.</p>
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22 pages, 19266 KiB  
Article
High-Resolution Infrared Reflectance Distribution Measurement Under Variable Temperature Conditions
by Yujian Yang, Yao Li, Ang Huang, Fanshan Meng, Jinghui Wang, Wei Dong and Yiwen Li
Sensors 2024, 24(21), 6780; https://doi.org/10.3390/s24216780 - 22 Oct 2024
Viewed by 485
Abstract
The bidirectional reflectance distribution function (BRDF) can effectively characterize the reflectance properties of a target, which can be used to correct infrared remote sensing data and improve the accuracy of remote sensing measurements. When the surface temperature changes, the reflectance characteristics of the [...] Read more.
The bidirectional reflectance distribution function (BRDF) can effectively characterize the reflectance properties of a target, which can be used to correct infrared remote sensing data and improve the accuracy of remote sensing measurements. When the surface temperature changes, the reflectance characteristics of the target usually change, and it is necessary to carry out BRDF measurements under variable temperature conditions. In this paper, a variable-temperature infrared BRDF measurement system based on a robotic arm is developed to realize high-resolution wide-temperature region measurement of BRDF. To improve the measurement accuracy, the shaping optical path was used to expand the laser beam, combined with the laser level to accurately adjust the three-dimensional coordinates of the robotic arm, and the dichotomy method is used to calibrate the detector nonlinearly. A portable heater suitable for the mechanical arm corner mechanism is developed, and fast and high-precision temperature control is realized by proportional integral derivative (PID) control. The specular and diffuse BRDF distributions were measured at room temperature to verify the effectiveness of the system. The BRDF distribution of SUS314 stainless steel samples with different roughness is measured during two temperature increases from 20 °C to 1000 °C, and the changing rule of BRDF under variable temperature environment is summarized, which provides technical support for evaluating the optical properties of high-temperature materials and improving the measurement accuracy of remote sensing data. Full article
(This article belongs to the Section Optical Sensors)
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<p>Schematic of infrared BRDF measurement system with variable temperature.</p>
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<p>Photo of laser source module.</p>
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<p>World coordinates of point where sample is illuminated: (<b>a</b>) Front view; (<b>b</b>) Side view; (<b>c</b>) Vertical view.</p>
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<p>(<b>a</b>) Photo of sample vertical projection onto the center of a circular guideway; (<b>b</b>,<b>c</b>) light path adjustment process.</p>
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<p>Adjustment process of the <math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <msup> <mrow> <mi>z</mi> </mrow> <mrow> <mo>′</mo> </mrow> </msup> </mrow> <mo>→</mo> </mover> </mrow> </semantics></math> axis in the world coordinate system: (<b>a</b>) Stereogram; (<b>b</b>) Vertical view; (<b>c</b>) Front view.</p>
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<p>Schematic of beam-expanding optical path.</p>
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<p>Infrared imaging with beam widening and spot illumination.</p>
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<p>Interface of the controlling program.</p>
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<p>(<b>a</b>) Detector assembly; (<b>b</b>) interior of the darkroom.</p>
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<p>Diagram of light path for converging lenses.</p>
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<p>Non-linear effect of the detector. Dichotomous correction of the optical path.</p>
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<p>(<b>a</b>) Fitting curve of the non-linear coefficients of the detector; (<b>b</b>) detector non-linearity correction curve.</p>
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<p>(<b>a</b>) Exploded view of the heater. 1 Heater top cover, 2 Heating tank, 3 Thermocouple, 4–6 heating plate, 7 Insulation shell, 8–11 Insulation layer. (<b>b</b>) Physical view of the heater.</p>
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<p>Schematic of measured sample.</p>
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<p>(<b>a</b>) Temperature profile during commissioning stage of PID parameters. (<b>b</b>) Temperature curve of the temperature control stage.</p>
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<p>(<b>a</b>) Plated sample and its BRDF distribution. (<b>b</b>) Gold plate and its BRDF distribution.</p>
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<p>Appearance and microstructure of samples with different roughness: (<b>a</b>) unheated; (<b>b</b>) after initial heating; (<b>c</b>) after secondary heating.</p>
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<p>Surface change of 800 mesh samples when heated to 1000 °C for the first and second time.</p>
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<p>BRDF distributions of samples with various roughness at initial heating to 20 °C and 1000 °C.</p>
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<p>Variation in BRDF peak values with temperature at initial heating of samples with different roughness: (<b>a</b>) 80-mesh sample; (<b>b</b>) 180-mesh sample; (<b>c</b>) 400-mesh sample; (<b>d</b>) 800-mesh sample.</p>
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<p>BRDF distributions of samples with various roughnesses at secondarily heated to 20 °C and 1000 °C.</p>
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<p>BRDF peak versus temperature during second heating of samples with different roughness: (<b>a</b>) 80-mesh sample; (<b>b</b>) 180-mesh sample; (<b>c</b>) 400-mesh sample; (<b>d</b>) 800-mesh sample.</p>
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13 pages, 3215 KiB  
Article
A Metal-Organic Framework-Based Colorimetric Sensor Array for Transcutaneous CO2 Monitoring via Lensless Imaging
by Syed Saad Ahmed, Jingjing Yu, Wei Ding, Sabyasachi Ghosh, David Brumels, Songxin Tan, Laxmi Raj Jaishi, Amirhossein Amjad and Xiaojun Xian
Biosensors 2024, 14(11), 516; https://doi.org/10.3390/bios14110516 - 22 Oct 2024
Viewed by 1304
Abstract
Transcutaneous carbon dioxide (TcPCO2) monitoring provides a non-invasive alternative to measuring arterial carbon dioxide (PaCO2), making it valuable for various applications, such as sleep diagnostics and neonatal care. However, traditional transcutaneous monitors are bulky, expensive, and pose risks such as skin burns. To [...] Read more.
Transcutaneous carbon dioxide (TcPCO2) monitoring provides a non-invasive alternative to measuring arterial carbon dioxide (PaCO2), making it valuable for various applications, such as sleep diagnostics and neonatal care. However, traditional transcutaneous monitors are bulky, expensive, and pose risks such as skin burns. To address these limitations, we have introduced a compact, cost-effective CMOS imager-based sensor for TcPCO2 detection by utilizing colorimetric reactions with metal–organic framework (MOF)-based nano-hybrid materials. The sensor, with a colorimetric sensing array fabricated on an ultrathin PDMS membrane and then adhered to the CMOS imager surface, can record real-time sensing data through image processing without the need for additional optical components, which significantly reduces the sensor’s size. Our system shows impressive sensitivity and selectivity, with a low detection limit of 26 ppm, a broad detection range of 0–2% CO2, and strong resistance to interference from common skin gases. Feasibility tests on human subjects demonstrate the potential of this MOF-CMOS imager-based colorimetric sensor for clinical applications. Additionally, its compact design and responsiveness make it suitable for sports and exercise settings, offering valuable insights into respiratory function and performance. The sensing system’s compact size, low cost, and reversible and highly sensitive TcPCO2 monitoring capability make it ideal for integration into wearable devices for remote health tracking. Full article
(This article belongs to the Special Issue Recent Advances in Wearable Biosensors for Human Health Monitoring)
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<p>Principle of the colorimetric gas sensor for transcutaneous gas monitoring. (<b>A</b>) Schematic of the diffusion of blood gas through the skin. (<b>B</b>) Images showing the typical color change in the sensing spot in the array when exposed to CO<sub>2</sub>. (<b>C</b>) The chemical reactions that lead to the colorimetric detection of CO<sub>2</sub>. (<b>D</b>) The structure of Co-MOF-71. The light blue octahedrons, the red balls, the dark blue balls, and the green balls represent Co(II) centers, oxygen atoms, carbon atoms, and hydrogen atoms, respectively. (<b>E</b>) The photo shows the PDMS membrane with the sensor array attached to the CMOS imager, captured using a phone camera. (<b>F</b>) Lensless image of the CO<sub>2</sub> sensor array captured by the CMOS imager with its pixels. (<b>G</b>) Schematic of the lensless colorimetric CO<sub>2</sub> sensing system.</p>
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<p>Characteristics of MOF-71 with and without colorimetric CO<sub>2</sub> indicator. (<b>A</b>) SEM images of MOF-71. (<b>B</b>) SEM images of MOF-71 with CO<sub>2</sub> indicator. (<b>C</b>) FTIR spectra of MOF-71 with and without CO<sub>2</sub> indicator. (<b>D</b>) XRD patterns of MOF-71 with and without CO<sub>2</sub> indicator.</p>
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<p>Sensing performance of the MOF-based colorimetric sensor array for CO<sub>2</sub> detection. (<b>A</b>) Real-time absorbance changes in each sensing spot in the sensor array when exposed to clean air (blank area) and 1000 ppm CO<sub>2</sub> (gray shade area) gas alternately for six cycles. Absorbance was calculated with intensity from the CMOS imager. R, G, and B represent the red, green, and blue channels of the CMOS imager, respectively. (<b>B</b>) Comparison of the absorbance (R channel) of each sensing spot in the sensor array and their average absorbance. (<b>C</b>) Response of the sensor arrays with and without MOF-71 to different concentrations of CO<sub>2</sub> (R channel). Absorbance change was calculated from absorbance difference before and after the CO<sub>2</sub> exposure. (<b>D</b>) Calibration plot of the sensor array for CO<sub>2</sub> detection in the range of 0 to 20,000 ppm. (<b>E</b>) Calibration plot of the sensor with the CO<sub>2</sub> concentration in log scale.</p>
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<p>Cross-sensitivity of the MOF-based colorimetric CO<sub>2</sub> sensor array.</p>
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<p>Transcutaneous CO<sub>2</sub> measurement with human subjects. (<b>A</b>) Real-time absorbance change curve of the MOF-based colorimetric CO<sub>2</sub> sensor array exposed to air and skin gas alternately. The blank areas indicate the air purging, and the gray shades indicate the exposure of skin gas. The skin gas was collected from a human subject while resting or doing exercise. The collection time of skin gas is 30 min. (<b>B</b>) The colorimetric sensor response to skin gas collected from different human subjects at resting and doing exercise. (<b>C</b>) Correlation between the readings from the MOF-based colorimetric CO<sub>2</sub> sensor array and commercial CO<sub>2</sub> sensor.</p>
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Article
Estimation of Glacier Outline and Volume Changes in the Vilcanota Range Snow-Capped Mountains, Peru, Using Temporal Series of Landsat and a Combination of Satellite Radar and Aerial LIDAR Images
by Nilton Montoya-Jara, Hildo Loayza, Raymundo Oscar Gutiérrez-Rosales, Marcelo Bueno and Roberto Quiroz
Remote Sens. 2024, 16(20), 3901; https://doi.org/10.3390/rs16203901 - 20 Oct 2024
Viewed by 846
Abstract
The Vilcanota is the second-largest snow-capped mountain range in Peru, featuring 380 individual glaciers, each with its own unique characteristics that must be studied independently. However, few studies have been conducted in the Vilcanota range to monitor and track the area and volume [...] Read more.
The Vilcanota is the second-largest snow-capped mountain range in Peru, featuring 380 individual glaciers, each with its own unique characteristics that must be studied independently. However, few studies have been conducted in the Vilcanota range to monitor and track the area and volume changes of the Suyuparina and Quisoquipina glaciers. Notably, there are only a few studies that have approached this issue using LIDAR technology. Our methodology is based on a combination of optical, radar and LIDAR data sources, which allowed for constructing coherent temporal series for the both the perimeter and volume changes of the Suyuparina and Quisoquipina glaciers while accounting for the uncertainty in the perimeter detection procedure. Our results indicated that, from 1990 to 2013, there was a reduction in snow cover of 12,694.35 m2 per year for Quisoquipina and 16,599.2 m2 per year for Suyuparina. This represents a loss of 12.18% for Quisoquipina and 22.45% for Suyuparina. From 2006 to 2013, the volume of the Quisoquipina glacier decreased from 11.73 km3 in 2006 to 11.04 km3 in 2010, while the Suyuparina glacier decreased from 6.26 km3 to 5.93 km3. Likewise, when analyzing the correlation between glacier area and precipitation, a moderate inverse correlation (R = −0.52, p < 0.05) was found for Quisoquipina. In contrast, the correlation for Suyuparina was low and nonsignificant, showing inconsistency in the effect of precipitation. Additionally, the correlation between the snow cover area and the annual mean air temperature (R = −0.34, p > 0.05) and annual minimum air temperature (R = −0.36, p > 0.05) was low, inverse, and not significant for Quisoquipina. Meanwhile, snow cover on Suyuparina had a low nonsignificant correlation (R = −0.31, p > 0.05) with the annual maximum air temperature, indicating a minimal influence of the measured climatic variables near this glacier on its retreat. In general, it was possible to establish a reduction in both the area and volume of the Suyuparina and Quisoquipina glaciers based on freely accessible remote sensing data. Full article
(This article belongs to the Section Remote Sensing for Geospatial Science)
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Figure 1
<p>An Airborne LIDAR point cloud of 3.2 m spatial resolution was acquired on the Suyuparina and Quisoquipina glaciers in the province of Canchis, Cusco.</p>
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<p>Binarized NDSI images recovered from Landsat 5 images from May 1990 (<b>A</b>) and Landsat 7 from April 2013 (<b>B</b>) for the Suyuparina and Quisoquipina glaciers. In orange and red, the shapefiles of the Suyuparina and Quisoquipina glaciers are delimited by expert criteria.</p>
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<p>Processing scheme. Blue represents inputs, green represents processing, yellow represents intermedium processing, and purple represents outputs.</p>
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<p>(<b>A</b>) Glacierized area of Quisoquipina, and (<b>B</b>) Suyuparina glaciers. In gray is the uncertainty band of the estimated glacier area.</p>
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<p>(<b>Up</b>) Glaciated area of Quisoquipina, and Suyuparina glaciers (<b>Down</b>) analyzed from 1990 to 1999 and from 2000 to 2013.</p>
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<p>(<b>A</b>) Volume changes of the Quisoquipina and (<b>B</b>) Suyuparina glaciers. Confidence intervales to the linear fitted model, shown in gray.</p>
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<p>(<b>A</b>) Glacierized outlines of Suyuparina and Quisoquipina glaciers. (<b>B</b>) Elevation change based on ALOS and LIDAR DEM analysis. Snow glaciological stakes installed between 2014 to 2016 are shown as reference. The background image corresponds to Google Earth 2019.</p>
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<p>Scatterplots of climatic and glacier surface changes. MeanAPE: Mean annual potential evapotranspiration (mm/day), MeanAP: Annual mean precipitation (mm/day), MaxAAT: Max. annual air temperature (°C), MinAAT: Min. annual air temperature (°C), MeanAMAT: Mean annual mean air temperature (°C).</p>
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