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23 pages, 5693 KiB  
Article
Sea Surface Wind Speed Retrieval Using Gaofen-3-02 Full Polarization Data
by Kuo Zhang, Yuxin Hu, Junxin Yang and Xiaochen Wang
Remote Sens. 2025, 17(4), 591; https://doi.org/10.3390/rs17040591 (registering DOI) - 9 Feb 2025
Viewed by 222
Abstract
The primary payload onboard the Gaofen-3-02 (GF3-02) satellite is a C-band Synthetic Aperture Radar (SAR) capable of achieving a maximum resolution of 1 m. This instrument is critical to monitor the marine environment, particularly for tracking sea surface wind speeds, an important marine [...] Read more.
The primary payload onboard the Gaofen-3-02 (GF3-02) satellite is a C-band Synthetic Aperture Radar (SAR) capable of achieving a maximum resolution of 1 m. This instrument is critical to monitor the marine environment, particularly for tracking sea surface wind speeds, an important marine environmental parameter. In this study, we utilized 192 sets of GF3-02 SAR data, acquired in Quad-Polarization Strip I (QPSI) mode in March 2022, to retrieve sea surface wind speeds. Prior to wind speed retrieval for vertical-vertical (VV) polarization, radiometric calibration accuracy was analyzed, yielding good performance. The results showed a bias and root mean square errors (RMSEs) of 0.02 m/s and 1.36 m/s, respectively, when compared to the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis V5 (ERA5) data. For horizontal–horizontal (HH) polarization, two types of polarization ratio (PR) models were introduced based on the GF3-02 SAR data. Combining these refitted PR models with CMOD5.N, the results for HH polarization exhibited a bias of −0.18 m/s and an RMSE of 1.25 m/s in comparison to the ERA5 data. Regarding vertical–horizontal (VH) polarization, two linear models based on both measured normalized radar cross sections (NRCSs) and denoised NRCSs were developed. The findings indicate that denoising significantly enhances the accuracy of wind speed measurements for VH polarization when dealing with low wind speeds. When compared against buoy data, the wind speed retrieval results demonstrated a bias of 0.23 m/s and an RMSE of 1.77 m/s. Finally, a comparative analysis of the above retrieval results across all three polarizations was conducted to further understand their respective performances. Full article
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<p>The geolocations of the acquired QPSI mode data.</p>
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<p>The flow chart of the comparison process between ERA5 data and SAR data.</p>
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<p>The geolocations of the matched scene–buoy pairs. (<b>a</b>) Station 46002; (<b>b</b>) Station 51000; (<b>c</b>) Station 51004. The buoys are denoted by black dots. The red boxes represent the scenes that match the buoys.</p>
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<p>The flow chart of the comparison process between buoy data and SAR data.</p>
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<p>The relationship between the absolute bias of NRCS at a wind speed bias of 0.5 m/s and wind speed for different incidence angles and relative wind directions.</p>
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<p>The disparity between the simulated NRCSs and the actual measured NRCSs in the subscene. The red horizontal lines indicate the threshold, which is 1.43 dB.</p>
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<p>Evaluating the consistency between the wind speeds derived from VV polarization data and the corresponding ERA5 wind speeds. (<b>a</b>) Scatter diagram; (<b>b</b>) histogram.</p>
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<p>The dependence of the PR in a linear unit on incidence angle and relative wind direction. (<b>a</b>) PR and incidence angle (<b>b</b>) PR and relative wind direction.</p>
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<p>Comparisons of the three refitted models and the GF3-02 SAR data.</p>
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<p>Comparisons of the converted NRCS from HH polarization and the measured NRCS for VV polarization. (<b>a</b>) Refitted Elfouhaily model. (<b>b</b>) Refitted Thompson model. (<b>c</b>) Refitted Mouche model. (<b>d</b>) Refitted Mouche–azimuth model.</p>
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<p>Examinations of the wind speeds obtained from HH polarization against the ERA5 wind speeds. Scatter diagram: (<b>a</b>) Refitted Elfouhaily model. (<b>b</b>) Refitted Thompson model. (<b>c</b>) Refitted Mouche model. (<b>d</b>) Refitted Mouche–azimuth model. Histogram: (<b>e</b>) Refitted Elfouhaily model. (<b>f</b>) Refitted Thompson model. (<b>g</b>) Refitted Mouche model. (<b>h</b>) Refitted Mouche–azimuth model.</p>
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<p>Examinations of the wind speeds obtained from HH polarization against the ERA5 wind speeds. Scatter diagram: (<b>a</b>) Refitted Elfouhaily model. (<b>b</b>) Refitted Thompson model. (<b>c</b>) Refitted Mouche model. (<b>d</b>) Refitted Mouche–azimuth model. Histogram: (<b>e</b>) Refitted Elfouhaily model. (<b>f</b>) Refitted Thompson model. (<b>g</b>) Refitted Mouche model. (<b>h</b>) Refitted Mouche–azimuth model.</p>
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<p>Scatter plots of the NRCS for VH polarization and the matched ERA5 wind speeds. (<b>a</b>) Measured NRCS. (<b>b</b>) Denoised NRCS.</p>
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<p>Examinations of the wind speeds retrieved from VH polarization in comparison with the ERA5 wind speeds. Scatter diagram: (<b>a</b>) Measured NRCS. (<b>b</b>) Denoised NRCS. Histogram: (<b>c</b>) Measured NRCS. (<b>d</b>) Denoised NRCS.</p>
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<p>Examinations of the wind speeds retrieved from VH polarization in comparison with the buoy wind speeds. (<b>a</b>) Measured NRCS. (<b>b</b>) Denoised NRCS.</p>
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<p>The distribution map of retrieved wind speed and wind speed bias compared with ERA5 data for the typhoon Hinnamnor. (<b>a</b>) Retrieved wind speed. (<b>b</b>) Wind speed bias.</p>
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<p>The distribution of wind speed retrieval results of VV polarization, HH polarization and VH polarization.</p>
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<p>The spatial distribution of wind speed retrieval results (<b>a</b>) VV polarization. (<b>b</b>) HH polarization. (<b>c</b>) VH polarization.</p>
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<p>The spatial distribution of retrieved wind speed bias compared with ERA5 wind speed. (<b>a</b>) VV polarization. (<b>b</b>) HH polarization. (<b>c</b>) VH polarization.</p>
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23 pages, 6481 KiB  
Article
Nonlinear Quantization Method of SAR Images with SNR Enhancement and Segmentation Strategy Guidance
by Zijian Yao, Linlin Fang, Junxin Yang and Lihua Zhong
Remote Sens. 2025, 17(3), 557; https://doi.org/10.3390/rs17030557 - 6 Feb 2025
Viewed by 314
Abstract
The quantization process of synthetic aperture radar (SAR) images faces significant challenges due to their high dynamic range, resulting in notable quantization distortion. This not only degrades the visual quality of the quantized images but also severely impacts the accuracy of image interpretation. [...] Read more.
The quantization process of synthetic aperture radar (SAR) images faces significant challenges due to their high dynamic range, resulting in notable quantization distortion. This not only degrades the visual quality of the quantized images but also severely impacts the accuracy of image interpretation. To mitigate the distortion caused by uniform quantization and enhance visual quality, this paper introduced a novel nonlinear quantization framework via signal-to-noise ratio (SNR) enhancement and segmentation strategy guidance. This framework introduces guiding information to improve quantization performance in weak scattering regions. A histogram adjustment method is developed to incorporate the spatial information of SAR images into the quantization process to enhance the quantization performance, specifically within weak scattering regions. Additionally, the optimal quantizer is improved by refining the SNR distribution across quantization units, addressing imbalances in their allocation. Experimental results based on Gaofen-3 (GF-3) satellite data demonstrate that the proposed algorithm approaches the global quantization performance of optimal quantizers while achieving superior local quantization performance compared to existing methods. Full article
(This article belongs to the Section Remote Sensing Image Processing)
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<p>Overview of the nonlinear quantization method framework.</p>
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<p>Overall framework of the proposed method.</p>
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<p>Results of the dynamic range of SAR images and histogram proportion. (<b>a</b>) Dynamic range results of SAR images for different land cover types. (<b>b</b>) Histogram proportion of SAR images for different land cover types in the [1:1000] quantization level range.</p>
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<p>Extraction results of sparse strong scattering points. The orange regions indicate the distribution of strong scattering points, while the blue histograms represent the image histogram. (<b>a</b>) Histogram of the land scene. (<b>b</b>) Histogram of the coast scene. (<b>c</b>) Histogram of the ocean scene.</p>
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<p>Segmentation experiment results. (<b>a</b>,<b>d</b>,<b>g</b>) Original quantized images. (<b>b</b>,<b>e</b>,<b>h</b>) Histogram segmentation results. (<b>c</b>,<b>f</b>,<b>i</b>) Morphological transformation processing results.</p>
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<p>Histogram of fine-tuning experimental results. (<b>a</b>–<b>f</b>) Histogram fusion results of six different SAR coast scene images.</p>
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<p>Image quantization experimental results.</p>
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<p>Local effects of nonlinear quantization experiment. (<b>a</b>) Original image, with the selected weak scattering area indicated by a red box. (<b>b</b>) Uniform quantization. (<b>c</b>) Histogram equalization. (<b>d</b>) Logarithmic quantization. (<b>e</b>) Optimal quantization. (<b>f</b>) The algorithm proposed in this paper.</p>
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<p>Quantization distortion experimental results for each quantization levels.</p>
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<p>Q–SNR experimental results for each quantization level.</p>
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<p>Q–SNR experimental results at the quantization levels of [0, 3000].</p>
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<p>Ground truth and clustering results with different methods. (<b>a</b>) Original image. (<b>b</b>) Ground truth label. (<b>c</b>) Histogram equalization clustering. (<b>d</b>) Log quantization clustering. (<b>e</b>) Optimal quantization clustering. (<b>f</b>) Proposed method clustering.</p>
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<p>Comparisons of <math display="inline"><semantics> <msub> <mi>F</mi> <mn>1</mn> </msub> </semantics></math> score in different binary classifications with different methods. (<b>a</b>) <math display="inline"><semantics> <msub> <mi>F</mi> <mn>1</mn> </msub> </semantics></math> score curve of land classification. (<b>b</b>) <math display="inline"><semantics> <msub> <mi>F</mi> <mn>1</mn> </msub> </semantics></math> score curve of ocean classification.</p>
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20 pages, 4669 KiB  
Article
Monitoring Mangrove Phenology Based on Gap Filling and Spatiotemporal Fusion: An Optimized Mangrove Phenology Extraction Approach (OMPEA)
by Yu Hong, Runfa Zhou, Jinfu Liu, Xiang Que, Bo Chen, Ke Chen, Zhongsheng He and Guanmin Huang
Remote Sens. 2025, 17(3), 549; https://doi.org/10.3390/rs17030549 - 6 Feb 2025
Viewed by 348
Abstract
Monitoring mangrove phenology requires frequent, high-resolution remote sensing data, yet satellite imagery often suffers from coarse resolution and cloud interference. Traditional methods, such as denoising and spatiotemporal fusion, faced limitations: denoising algorithms usually enhance temporal resolution without improving spatial quality, while spatiotemporal fusion [...] Read more.
Monitoring mangrove phenology requires frequent, high-resolution remote sensing data, yet satellite imagery often suffers from coarse resolution and cloud interference. Traditional methods, such as denoising and spatiotemporal fusion, faced limitations: denoising algorithms usually enhance temporal resolution without improving spatial quality, while spatiotemporal fusion models struggle with prolonged data gaps and heavy noise. This study proposes an optimized mangrove phenology extraction approach (OMPEA), which integrates Landsat and MODIS data with a denoising algorithm (e.g., Gap Filling and Savitzky–Golay filtering, GF–SG) and a spatiotemporal fusion model (e.g., Enhanced Spatial and Temporal Adaptive Reflectance Fusion Model, ESTARFM). The key of OMPEA is that GF–SG algorithm filled data gaps from cloud cover and satellite transit gaps, providing high-quality input to ESTARFM and improving its accuracy of NDVI imagery reconstruction in mangrove phenology extraction. By conducting experiments on the GEE platform, OMPEA generates 1-day, 30 m NDVI imagery, from which phenological parameters (i.e., the start (SoS), end (EoS), length (LoS), and peak (PoS) of the growing season) are derived using the maximum separation (MS) method. Validation in four mangrove areas along the coastal China shows that OMPEA significantly improves the potential to capture mangrove phenology in the presence of incomplete data. The OMPEA significantly increased usable data, adding 7–33 Landsat images and 318–415 MODIS images per region. The generated NDVI series exhibits strong spatiotemporal consistency with original data (R2: 0.788–0.998, RMSE: 0.007–0.253) and revealed earlier SoS and longer LoS at lower latitudes. Cross-correlation analysis showed a 2–3 month lagged effects of temperature on mangroves’ growth, with precipitation having minimal impact. The proposed OMPEA improves the possibility of capturing mangrove phenology under non-continuous and low-resolution data, providing valuable insights for large-scale and long-term mangrove conservation and management. Full article
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<p>Map of study area: (<b>a</b>) the overall distribution of study area; (<b>b1</b>–<b>b4</b>) Zhangjiangkou National Mangrove Nature Reserve (ZNR) in Fujian Province, Qi’ao Island Provincial Nature Reserve (QPR) in Guangdong Province, Beilun Estuary National Nature Reserve (BNR) in Guangxi Province, and Dongzhaigang National Mangrove Nature Reserve (DNR) in Hainan Province.</p>
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<p>Workflow of mangrove phenology extraction based on OMPEA.</p>
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<p>Landsat 8 NDVI (16-day 30 m) and denoised Landsat NDVI (16-day 30 m) generated by OMPEA. Gray pixel indicates pixel with no data.</p>
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<p>MODIS NDVI (1-day 500 m) and denoised MODIS NDVI (1-day 30 m) generated by OMPEA. Gray pixel indicates pixel with no data.</p>
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<p>The OMPEA-generated fused NDVI imagery. Gray pixel indicates pixel with no data.</p>
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<p>Scatter density plots and marginal histograms of fused NDVI and denoised Landsat NDVI.</p>
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<p>Composite scatter plots and line plots of various NDVI time series.</p>
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<p>Fused NDVI time-series curve and phenological parameters.</p>
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<p>Boxplots of mangrove phenological parameters.</p>
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<p>The time-series curves for fused NDVI, precipitation, temperature, and their lagged time-series curves with corresponding lag days.</p>
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<p>The OMPEA-generated fused NDVI in QPR from 17 January 2020 to 24 March 2021. (<b>a</b>) Description of denoised Landsat 8 NDVI in a full-time range. (<b>b</b>) Description of denoised Landsat 8 NDVI across three different time ranges, (<b>c</b>,<b>d</b>) is fused NDVI that using (<b>a</b>,<b>b</b>) as inputs, respectively. Gray pixel indicates pixel with no data.</p>
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22 pages, 2496 KiB  
Article
Positioning Technology Without Ground Control Points for Spaceborne Synthetic Aperture Radar Images Using Rational Polynomial Coefficient Model Considering Atmospheric Delay
by Doudou Hu, Chunquan Cheng, Shucheng Yang and Chengxi Hu
Appl. Sci. 2025, 15(3), 1615; https://doi.org/10.3390/app15031615 - 5 Feb 2025
Viewed by 333
Abstract
This study addresses the issue of atmospheric delay correction for the rational polynomial coefficient (RPC) model associated with spaceborne synthetic aperture radar (SAR) imagery under conditions lacking ephemeris data, proposing a novel approach to enhance the geometric positioning accuracy of RPC models. A [...] Read more.
This study addresses the issue of atmospheric delay correction for the rational polynomial coefficient (RPC) model associated with spaceborne synthetic aperture radar (SAR) imagery under conditions lacking ephemeris data, proposing a novel approach to enhance the geometric positioning accuracy of RPC models. A satellite position inversion method based on the vector-autonomous intersection technique was developed, incorporating ionospheric delay and neutral atmospheric delay models to derive atmospheric delay errors. Additionally, an RPC model reconstruction approach, which integrates atmospheric correction, is proposed. Validation experiments using GF-3 satellite imagery demonstrated that the atmospheric delay values obtained by this method differed by only 0.0001 m from those derived using the traditional ephemeris-based approach, a negligible difference. The method also exhibited high robustness in long-strip imagery. The reconstructed RPC parameters improved image-space accuracy by 18–44% and object-space accuracy by 19–32%. The results indicate that this approach can fully replace traditional ephemeris-based methods for atmospheric delay extraction under ephemeris-free conditions, significantly enhancing the geometric positioning accuracy of SAR imagery RPC models, with substantial application value and development potential. Full article
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<p>Radar LOS vector inversion.</p>
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<p>Satellite position inversion.</p>
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<p>Ionospheric single-layer model.</p>
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<p>GF-3 data. (<b>a</b>) area1; (<b>b</b>) area2. The red box indicates the data of rail lift and the blue box indicates the data of rail descent.</p>
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<p>Satellite position inversion accuracy. (<b>a</b>) Satellite position error; (<b>b</b>) slant-range error.</p>
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<p>Electron density and specific humidity in the zenith direction. (<b>a</b>) Electron density in the zenith direction; (<b>b</b>) specific humidity in the zenith direction.</p>
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<p>Atmospheric delamination delay. (<b>a</b>) gf1 ionospheric delay; (<b>b</b>) gf7 ionospheric delay; (<b>c</b>) gf1 neutral atmospheric delay; (<b>d</b>) gf7 neutral atmospheric delay.</p>
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<p>Atmospheric delay.</p>
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<p>SAR image positioning accuracy. (<b>a</b>) Image-space accuracy; (<b>b</b>) object-space accuracy.</p>
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24 pages, 8896 KiB  
Article
A Prediction of Estuary Wetland Vegetation with Satellite Images
by Min Yang, Bin Guo, Ning Gao, Yang Yu, Xiaoli Song and Yanfeng Gu
J. Mar. Sci. Eng. 2025, 13(2), 287; https://doi.org/10.3390/jmse13020287 - 4 Feb 2025
Viewed by 384
Abstract
Estuarine wetlands are the transition zone between marine, freshwater, and terrestrial ecosystems and are more ecologically fragile. In recent years, the spread of exotic vegetation, specifically Spartina alterniflora, in the Yellow River estuary wetlands has significantly encroached upon the habitats of native [...] Read more.
Estuarine wetlands are the transition zone between marine, freshwater, and terrestrial ecosystems and are more ecologically fragile. In recent years, the spread of exotic vegetation, specifically Spartina alterniflora, in the Yellow River estuary wetlands has significantly encroached upon the habitats of native species such as Phragmites australis, Suaeda glauca Bunge, and Tamarix chinensis Lour. With advances in land prediction modeling, predicting wetland vegetation distribution can aid management and decision-making for ecological restoration. We selected the core area as the study object and coupled the hydrological model MIKE 21 with the PLUS model to predict the potential future distribution of invasive and dominant species in the region. (1) Based on the fine classification results from satellite images of GF1/G2/G5, we gained an understanding of the changes in wetland vegetation types in the core area of the reserve in 2018 and 2020. (2) Using public data such as ERA5 and GEO as input for basic environmental data, using MIKE 21 to provide high-spatial-resolution hydrodynamic parameters for the PLUS model as an environmental driver, we modeled the spatial distribution of various wetland vegetation in the Yellow River estuary wetland in Dongying under different artificial restoration measures. (3) We predicted the 2022 distribution of typical vegetation in the region, used the classification results of GF6 as the actual distribution, compared the spatial distribution with the actual distribution, and obtained a kappa coefficient of 0.78; the predicted values of the model are highly consistent with the true values. This study combines the fine classification results of vegetation based on hyperspectral remote sensing, the construction of a coupled model, and the prediction effect of typical species, providing a reference for constructing and optimizing the vegetation prediction model of estuarine wetlands. It also allows scientific and effective decision-making for the management of ecological restoration of delta wetlands. Full article
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<p>Research area-the Yellow River estuary wetlands.</p>
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<p>Schematic diagram of the coupling models.</p>
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<p>Grid range of MIKE 21.</p>
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<p>Schematic diagram of the ecological restoration area of the Yellow River estuary delta.</p>
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<p>The processing flow of MIKE 21-PLUS coupling model in artificial ecological restoration measures.</p>
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<p>Hydrodynamic simulation of MIKE21 model. (<b>a</b>) Hydrodynamic simulation within the restoration area; (<b>b</b>) current velocity without tidal creek; and (<b>c</b>) flow velocity under tidal ditch conditions.</p>
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<p>Changes in the distribution of features in the Yellow River estuary, 2018–2022.</p>
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<p>Model realization process for mowing and replanting.</p>
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<p>Comparison of observed and modeled salinity in Laizhou Bay. (Salinity data from the environmental survey of Laizhou Bay in August 2020 by Beihai Bureau of the Ministry of Natural Resources).</p>
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<p>Comparison of simulation results based on MIKE 21-PLUS with actual results.</p>
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<p>Comparison of simulation results between natural and artificial restoration scenarios in the restoration area.</p>
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<p>Environmental drivers of the evolution of the distribution of <span class="html-italic">Spartina alterniflora</span>, <span class="html-italic">Suaeda glauca Bunge</span>, and <span class="html-italic">Reed</span> (<span class="html-italic">Phragmites australis</span>).</p>
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<p>Comparison of <span class="html-italic">F</span><sub>1</sub>-<span class="html-italic">score</span> for simulating vegetation distribution in the Yellow River estuary wetland in 2022 using MIKE21-PLUS and PLUS.</p>
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24 pages, 7022 KiB  
Article
Evaluation of the Sensitivity of the Weather Research and Forecasting Model to Changes in Physical Parameterizations During a Torrential Precipitation Event of the El Niño Costero 2017 in Peru
by Alejandro Sánchez Oliva, Matilde García-Valdecasas Ojeda and Raúl Arasa Agudo
Water 2025, 17(2), 209; https://doi.org/10.3390/w17020209 - 14 Jan 2025
Viewed by 558
Abstract
This study evaluates the sensitivity of the Weather Research and Forecasting (WRF-ARW) model in its version 4.3.3 during different experiments on a torrential precipitation event associated with the 2017 El Niño Costero in Peru. The results are compared with two reference datasets: precipitation [...] Read more.
This study evaluates the sensitivity of the Weather Research and Forecasting (WRF-ARW) model in its version 4.3.3 during different experiments on a torrential precipitation event associated with the 2017 El Niño Costero in Peru. The results are compared with two reference datasets: precipitation estimations from CHIRPS satellite data and SENAMHI meteorological station values. The event, which had significant economic and social impacts, is simulated using two nested domains with resolutions of 9 km (d01) and 3 km (d02). A total of 22 experiments are conducted, resulting from the combination of two planetary boundary layer (PBL) schemes: Yonsei University (YSU) and Mellor–Yamada–Janjic (MYJ), with five cumulus parameterization schemes: Betts–Miller–Janjic (BMJ), Grell–Devenyi (GD), Grell–Freitas (GF), Kain–Fritsch (KF), and New Tiedtke (NT). Additionally, the effect of turning off cumulus parameterization in the inner domain (d02) or in both (d01 and d02) is explored. The results show that the YSU scheme generally provides better results than the MYJ scheme in detecting the precipitation patterns observed during the event. Furthermore, it is concluded that turning off cumulus parameterization in both domains produces satisfactory results for certain regions when it is combined with the YSU PBL scheme. However, the KF cumulus parameterization is considered the most effective for intense precipitation events in this region, although it tends to overestimate precipitation in high mountain areas. In contrast, for lighter rains, combinations of the YSU PBL scheme with the GD or NT parameterization show a superior performance. It is worth nothing that for all experiments here used, there is a clear underestimation in terms of precipitation, except in high mountain regions, where the model tends to overestimate rainfall. Full article
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<p>The WRF model domains: the outer domain (d01) with a 9 km spatial resolution and the inner domain (d02) with a 3 km spatial resolution. The locations of the 20 selected meteorological stations are shown as purple dots.</p>
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<p>Accumulated precipitation of the event for simulations under the YSU PBL. The first row shows the accumulated precipitation in CHIRPS (reference data), and from the second row onward, each row corresponds to a cumulus parameterization. The left column shows the results for d01. The center column shows parameterization in both domains. The right column shows parameterization in d01 and the explicit resolution in d02.</p>
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<p>As <a href="#water-17-00209-f002" class="html-fig">Figure 2</a>, but for MYJ PBL.</p>
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<p>The 3-day accumulated precipitation for simulations with an explicitly resolved CU in both domains and for the two PBLs evaluated.</p>
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<p>Relative bias (%) of experiments completed with YSU PBL when compared to CHIRPS.</p>
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<p>Comparison of the relative bias (%) of the experiments for the d02 domain with respect to CHIRPS using the MYJ PBL.</p>
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<p>Relative bias (%) for both PBLs with the explicit resolution of the model in both domains.</p>
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17 pages, 7144 KiB  
Article
Fine-Grained Building Classification in Rural Areas Based on GF-7 Data
by Mingbo Liu, Ping Wang, Peng Han, Longfei Liu and Baotian Li
Sensors 2025, 25(2), 392; https://doi.org/10.3390/s25020392 - 10 Jan 2025
Viewed by 391
Abstract
Building type information is widely used in various fields, such as disaster management, urbanization studies, and population modelling. Few studies have been conducted on fine-grained building classification in rural areas using China’s Gaofen-7 (GF-7) high-resolution stereo mapping satellite data. In this study, we [...] Read more.
Building type information is widely used in various fields, such as disaster management, urbanization studies, and population modelling. Few studies have been conducted on fine-grained building classification in rural areas using China’s Gaofen-7 (GF-7) high-resolution stereo mapping satellite data. In this study, we employed a two-stage method combining supervised classification and unsupervised clustering to classify buildings in the rural area of Pingquan, northern China, based on building footprints, building heights, and multispectral information extracted from GF-7 data. In the supervised classification stage, we compared different classification models, including Extreme Gradient Boosting (XGBoost) and Random Forest classifiers. The best-performing XGBoost model achieved an overall roof type classification accuracy of 88.89%. Additionally, we proposed a template-based building height correction method for pitched roof buildings, which combined geometric features of the building footprint, street view photos, and height information extracted from the GF-7 stereo image. This method reduced the RMSE of the pitched roof building heights from 2.28 m to 1.20 m. In the cluster analysis stage, buildings with different roof types were further classified in the color and shape feature spaces and combined with the building height information to produce fine-grained building type codes. The results of the roof type classification and fine-grained building classification reveal the physical and geometric characteristics of buildings and the spatial distribution of different building types in the study area. The building classification method proposed in this study has broad application prospects for disaster management in rural areas. Full article
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<p>The study area: (<b>a</b>) location of the study area; (<b>b</b>) GF-7 MUX multispectral image of the study area.</p>
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<p>Workflow of the fine-grained building classification. The process of extracting building height from GF-7 data is also demonstrated.</p>
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<p>Template-based height correction for pitched roof buildings: (<b>a</b>) image of the pitched roof building; (<b>b</b>) minimum bounding rectangle and the eave zone; (<b>c</b>) street view photo of pitched roof buildings; and (<b>d</b>) template used for height correction.</p>
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<p>Samples of different roof types: (<b>a</b>) pitched; (<b>b</b>) greenhouse; (<b>c</b>) color steel; (<b>d</b>) flat; (<b>e</b>) complex.</p>
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<p>Roof types in the study area. Aggregated to 50 m ground sampling distance (GSD) for visualization.</p>
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<p>Height validation of pitched roof buildings: (<b>a</b>) before correction; (<b>b</b>) after correction.</p>
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<p>Fine-grained building types in the study area. Aggregated to 50 m GSD for visualization.</p>
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<p>Samples of several representative building types.</p>
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<p>Confusion matrices of different supervised classification models.</p>
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<p>Height validation scatterplot of: (<b>a</b>) greenhouses; (<b>b</b>) color steel roof buildings; (<b>c</b>) flat roof buildings; and (<b>d</b>) complex roof buildings.</p>
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<p>Distribution of buildings with different roof types in color and shape dimensions and statistical indicators in cluster analysis. Cluster 1 to cluster 4 are represented by blue, red, green, and yellow colors, respectively.</p>
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15 pages, 2654 KiB  
Technical Note
Analysis of Roadside Land Use Changes and Landscape Ecological Risk Assessment Based on GF-1: A Case Study of the Linghua Expressway
by Mengdi Wen, Liangliang Zhang, Huawei Wan, Peirong Shi, Longhui Lu, Zixin Zhao, Zhiru Zhang and Jinhui Wu
Remote Sens. 2025, 17(2), 211; https://doi.org/10.3390/rs17020211 - 8 Jan 2025
Viewed by 700
Abstract
The rapid construction of expressways in China has brought significant economic and social benefits, but it has also imposed substantial ecological pressures, particularly in sensitive regions. Landscape ecological risk assessment, as an important means to predict and measure the adverse effects of human [...] Read more.
The rapid construction of expressways in China has brought significant economic and social benefits, but it has also imposed substantial ecological pressures, particularly in sensitive regions. Landscape ecological risk assessment, as an important means to predict and measure the adverse effects of human activities on the ecological environment, is being paid more and more attention. However, most studies focus on the static landscape mosaic pattern and lack dynamic analysis. Moreover, they mainly focus on the ecological effect of the road operation stage, ignoring the monitoring and analysis of the whole construction process. Based on this, the current study examines the landscape ecological risk and land use changes along the Linghua Expressway in Gansu Province using high-resolution GF-1 remote sensing imagery. A landscape ecological risk assessment (LERA) model was employed to quantify the land use changes and assess the ecological risks before and after the expressway construction between 2018 and 2022. The results revealed a decrease in cropland and forest land, accompanied by an increase in the grassland and road areas. The landscape ecological risk index decreased from 0.318 in 2018 to 0.174 in 2022, indicating an improvement in ecological resilience. However, high-risk zones remain near the expressway, emphasizing the need for continuous monitoring and proactive ecological management strategies. These findings contribute to sustainable infrastructure planning, particularly in ecologically sensitive regions. Full article
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<p>The flow chart of this study.</p>
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<p>Linghua Expressway main line and research area.</p>
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<p>Remote sensing images of the study area in 2018 (<b>a</b>) and 2022 (<b>b</b>).</p>
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<p>Landscape ecological risk sample grid of the study area.</p>
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<p>Land use classification maps of the study area in 2018 (<b>a</b>) and 2022 (<b>b</b>).</p>
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<p>Spatial distribution of landscape ecological risk of the study area in 2018 (<b>a</b>) and 2022 (<b>b</b>).</p>
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<p>Landscape ecological risk classification area proportion.</p>
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27 pages, 17432 KiB  
Article
Retrieval and Analysis of Sea Surface Salinity in Coastal Waters Using Satellite Data Based on IGWO–BPNN: A Case Study of Qinzhou Bay, Guangxi, China
by Maoyuan Zhong, Huanmei Yao, Yin Liu, Junchao Qiao, Meijun Chen and Weiping Zhong
Water 2025, 17(1), 94; https://doi.org/10.3390/w17010094 - 1 Jan 2025
Viewed by 588
Abstract
This study proposes a high-precision method for retrieving sea surface salinity (SSS) using GF-1 satellite imagery, focusing on Qinzhou Bay along the Guangxi coast. The analysis identified the spectral index B3×B4/(B1×B2) as having the strongest correlation with SSS (R = 0.929). To enhance [...] Read more.
This study proposes a high-precision method for retrieving sea surface salinity (SSS) using GF-1 satellite imagery, focusing on Qinzhou Bay along the Guangxi coast. The analysis identified the spectral index B3×B4/(B1×B2) as having the strongest correlation with SSS (R = 0.929). To enhance the performance of the Back Propagation Neural Network (BPNN) model, optimization algorithms including Improved Grey Wolf Optimization (IGWO), Particle Swarm Optimization (PSO), and White Shark Optimization (WSO) were applied. Comparative results show that IGWO significantly optimized network weights and thresholds, yielding superior test performance metrics (MAE = 0.906 psu, MAPE = 4.124%, RMSE = 1.067 psu, and R2 = 0.953), demonstrating strong generalization ability. Validation using third-party data indicated accuracy reductions of 10.9% and 8.6% in Qinzhou Bay and Tieshan Port, respectively, highlighting the model’s robustness and broad applicability. SSS retrieval results for Qinzhou Bay in 2023 revealed significant spatial and seasonal variations: the Inner Bay exhibited lower salinity (average 14 psu) from April to September due to freshwater inflows, while salinity increased (average 22 psu) from November to February. The Outer Bay, influenced by its connection to the South China Sea, maintained consistently high salinity levels (25–30 psu) year-round. Additionally, different models showed varying levels of effectiveness in Qinzhou Bay’s complex salinity environment; the IGWO–BPNN model, with its dynamic weight adjustment mechanism, demonstrated superior adaptability in areas with high salinity variability, outperforming other models. These findings suggest that the IGWO–BPNN model provides high accuracy and stability, supporting real-time, precise monitoring in Qinzhou Bay and similar coastal waters, thereby offering robust support for water quality management and marine conservation. Full article
(This article belongs to the Special Issue Remote Sensing in Coastal Water Environment Monitoring)
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<p>Study area and sampling points distribution.</p>
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<p>Measurement and recording of ship’s progress.</p>
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<p>Three-dimensional SSS distribution: (<b>a</b>) aerial survey data from September 2015 to January 2016; (<b>b</b>) aerial survey data from 20 May 2023; (<b>c</b>) aerial survey data from 20 to 21 November 2023.</p>
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<p>Observational perspective.</p>
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<p>Experimental spectrum and spectrum preprocess.</p>
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<p>Technical road chart.</p>
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<p>Structure of BPNN with a hidden layer.</p>
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<p>IGWO–BPNN optimisation process.</p>
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<p>Comparative analysis of water reflectance curves from GF-1 satellite imagery and empirical spectra measurements.</p>
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<p>Performance evaluation of the SSS retrieval model with optimization algorithms on the validation set.</p>
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<p>Distribution map of monitoring points in Tieshan Port on 4 November 2021.</p>
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<p>Temporal generalization validation results of the IGWO–BPNN model: (<b>a</b>) retrieval result; (<b>b</b>) fitting result.</p>
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<p>Spatial generalization validation results of the IGWO–BPNN model: (<b>a</b>) retrieval result; (<b>b</b>) fitting result.</p>
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<p>Model error comparison by region: (<b>a</b>) BPNN; (<b>b</b>) PSO–BPNN; (<b>c</b>) WSO–BPNN; (<b>d</b>) IGWO–BPNN.</p>
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<p>Spatiotemporal distribution characteristics of monthly SSS in 2023.</p>
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<p>Seasonal salinity variations in the Inner Bay, 2023: (<b>a</b>) March; (<b>b</b>) November; and (<b>c</b>) December (Dry Season); (<b>d</b>) April; and (<b>e</b>) May (Wet Season).</p>
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<p>Seasonal salinity interactions between Bay Neck and Outer Bay, 2023: (<b>a</b>) January and (<b>b</b>) December (Winter); (<b>c</b>) April and (<b>d</b>) May (Summer).</p>
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<p>Monthly variation of average SSS concentration in different regions of Qinzhou Bay.</p>
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17 pages, 4838 KiB  
Article
XCO2 Data Full-Coverage Mapping in China Based on Random Forest Models
by Ruizhi Chen, Zhongting Wang, Chunyan Zhou, Ruijie Zhang, Huizhen Xie and Huayou Li
Remote Sens. 2025, 17(1), 48; https://doi.org/10.3390/rs17010048 - 27 Dec 2024
Viewed by 569
Abstract
Carbon dioxide (CO2) is a key driver of global climate change. Since the Industrial Revolution, the rapid rise in atmospheric CO2 levels has significantly intensified global warming and climate-related issues. To accurately and promptly monitor changes in CO2 concentrations [...] Read more.
Carbon dioxide (CO2) is a key driver of global climate change. Since the Industrial Revolution, the rapid rise in atmospheric CO2 levels has significantly intensified global warming and climate-related issues. To accurately and promptly monitor changes in CO2 concentrations and to support the development of climate policies, this study proposes a method based on random forest models to generate a continuous monthly dataset of CO2 column concentration (XCO2) across the entire Chinese region from 2004 to 2023. The study integrates XCO2 satellite observations from SCIAMACHY, GOSAT, OCO-2, and GF-5B, alongside nighttime light remote sensing data, meteorological parameters, vegetation indices, and CO2 profile data. Using the random forest algorithm, a complex relationship model was established between XCO2 concentrations and various environmental variables. The goal of this model is to provide XCO2 estimates with enhanced spatial coverage and accuracy. The XCO2 concentrations predicted by the model show a high level of consistency with satellite observations, achieving a correlation coefficient (R-value) of 0.9959 and a root mean square error (RMSE) of 1.1631 ppm. This indicates that the model offers strong predictive accuracy and generalization ability. Additionally, ground-based validation further confirmed the model’s effectiveness, with a correlation coefficient (R-value) of 0.956 when compared with TCCON site observation data. Full article
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<p>Display of original XCO<sub>2</sub> data from multi-source carbon satellites.</p>
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<p>The workflow of XCO<sub>2</sub> full-coverage mapping.</p>
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<p>Test set overall results in China from 2004 to 2020.</p>
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<p>Representative regions used in this study.</p>
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<p>Test set overall results from 2004 to 2020 in the representative regions.</p>
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<p>(<b>a</b>) Data pairs compared with TCCON for RF; (<b>b</b>) data pairs compared with TCCON for CT; (<b>c</b>) data pairs compared with TCCON for SAT; (<b>d</b>) monthly TCCON XCO<sub>2</sub> compared with RF, The shaded areas show the comparison results for 2016.</p>
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<p>Spatial distribution pattern of XCO<sub>2</sub>: (<b>a</b>) average from 2015 to 2020; (<b>b</b>) result for 2015; (<b>c</b>) result for 2017; (<b>d</b>) result for 2019.</p>
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<p>Interannual variation in XCO<sub>2</sub> from 2015 to 2020.</p>
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<p>Interannual variation distribution of XCO<sub>2</sub>: (<b>a</b>) average from 2015 to 2020; (<b>b</b>) variation from 2019 to 2020; (<b>c</b>) variation from 2018 to 2019; (<b>d</b>) variation from 2017 to 2018; (<b>e</b>) variation from 2016 to 2017; (<b>f</b>) variation from 2015 to 2016.</p>
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18 pages, 12334 KiB  
Article
Canopy Height Integration for Precise Forest Aboveground Biomass Estimation in Natural Secondary Forests of Northeast China Using Gaofen-7 Stereo Satellite Data
by Caixia Liu, Huabing Huang, Zhiyu Zhang, Wenyi Fan and Di Wu
Remote Sens. 2025, 17(1), 47; https://doi.org/10.3390/rs17010047 - 27 Dec 2024
Cited by 1 | Viewed by 606
Abstract
Accurate estimates of forest aboveground biomass (AGB) are necessary for the accurate tracking of forest carbon stock. Gaofen-7 (GF-7) is the first civilian sub-meter three-dimensional (3D) mapping satellite from China. It is equipped with a laser altimeter system and a dual-line array stereoscopic [...] Read more.
Accurate estimates of forest aboveground biomass (AGB) are necessary for the accurate tracking of forest carbon stock. Gaofen-7 (GF-7) is the first civilian sub-meter three-dimensional (3D) mapping satellite from China. It is equipped with a laser altimeter system and a dual-line array stereoscopic mapping camera, which enables it to synchronously generate full-waveform LiDAR data and stereoscopic images. The bulk of existing research has examined how accurate GF-7 is for topographic measurements of bare land or canopy height. The measurement of forest aboveground biomass has not received as much attention as it deserves. This study aimed to assess the GF-7 stereo imaging capability, displayed as topographic features for aboveground biomass estimation in forests. The aboveground biomass model was constructed using the random forest machine learning technique, which was accomplished by combining the use of in situ field measurements, pairs of GF-7 stereo images, and the corresponding generated canopy height model (CHM). Findings showed that the biomass estimation model had an accuracy of R2 = 0.76, RMSE = 7.94 t/ha, which was better than the inclusion of forest canopy height (R2 = 0.30, RMSE = 21.02 t/ha). These results show that GF-7 has considerable application potential in gathering large-scale high-precision forest aboveground biomass using a restricted amount of field data. Full article
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<p>Location map of the study area (Shangzhi, Heilongjiang, China). (<b>a</b>) The location of the study area; (<b>b</b>) field plots over the GF-7 multispectral image on 20 August 2020 (R—red, G—green, B—blue).</p>
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<p>The procedure for calculating forest canopy height and biomass from GF-7 stereoscopic imagery.</p>
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<p>The August and November DSM and CHM. This figure shows only the DSM and CHM for the common regions between August and November, highlighted by the read box. (<b>a</b>,<b>b</b>) DSMs for August and November, respectively, and (<b>e</b>,<b>f</b>) show the larger detail plots in the red boxes. (<b>c</b>,<b>d</b>) CHMs for August and November, respectively, and (<b>g</b>,<b>h</b>) show the larger detail plots in the red boxes.</p>
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<p>The scatter plot illustrates the relationship between canopy heights predicted using a canopy height model and field-measured heights for two different time points: August and November. The light green points and corresponding regression line represent the August data, while the light blue points and their regression line represent the November data. The 1:1 line (grey dashed) indicates perfect concordance between predicted and measured heights.</p>
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<p>Feature importance scores for predicting AGB using random forest models under two scenarios: S1 and S2. Features are ranked in decreasing order of importance based on the mean decrease in mean squared error (MSE). The feature “class” refers to land cover classification data, distinguishing between forested and non-forested areas, derived from geographic national condition data.</p>
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<p>Predicted biomass maps in different scenarios: (<b>a</b>) for S1 scenario and (<b>b</b>) for S2 scenario. Detailed drawings of the red-framed area are shown in <a href="#remotesensing-17-00047-f008" class="html-fig">Figure 8</a>.</p>
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<p>Scatter plots depicting the relationship between predicted biomass (t/ha) and field-measured biomass (t/ha) for four different scenarios (S1, S2, S3, and S4) in 2020. Detailed scenario descriptions are provided in <a href="#remotesensing-17-00047-t002" class="html-table">Table 2</a>. (<b>a</b>) Scatter plot includes a regression line, with annotations displaying the regression equation, coefficient of determination (R<sup>2</sup>), and root mean square error (RMSE) to quantitatively assess model performance. (<b>b</b>) Residuals for each model’s prediction compared with field biomass. The results demonstrate incremental improvements in biomass prediction accuracy from S1 to S4, highlighting the significant impact of incorporating CHM and DSM data. Scenarios S2 and S3 show enhanced prediction accuracy due to the inclusion of detailed canopy height information.</p>
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<p>Biomass, spectrum, and canopy height spatial features at the same location. The biomass detail map on the far left shows the result of the S1 scenario, while the one on the right shows the result of the S2 scenario. The biomass ramp is consistent with that shown in <a href="#remotesensing-17-00047-f006" class="html-fig">Figure 6</a>, and the RGB channel denotes the real color channel display of GF-7. The CHM ramp is similar to those shown in <a href="#remotesensing-17-00047-f003" class="html-fig">Figure 3</a>. The last column shows land cover, with black indicating forested area and white representing non-forest land. Figure (<b>a</b>): the disturbance of water bodies and soil moisture on the river valley delta causes the forest vegetation spectra to be mistaken for bare soil and water bodies, which leads to an underestimating of biomass forecast based solely on spectral properties. The regional variability of forest species and height under various topographic circumstances is depicted in Figure (<b>b</b>). Because of the region’s eastern side’s relative flatness, low forest heights, and predominance of coniferous tree species, biomass estimations that consider CHM factors are more accurate in reflecting the real distribution. Figure (<b>c</b>): due to the overestimation of the height of the farmland vegetation caused by spectral features alone (August during the growing season), the farmland’s spectrum is viewed as being spectral like the forest. In agriculture, the average biomass is less than 5 t/ha, although biomass is more precisely anticipated because of the constraint that CHM is approximately 0 t/ha. A logging site is in the region of figure (<b>d</b>), with low biomass. A more accurate prediction of the biomass distribution is made by taking canopy height features into account.</p>
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20 pages, 5308 KiB  
Article
Atmospheric Modulation Transfer Function Calculation and Error Evaluation for the Panchromatic Band of the Gaofen-2 Satellite
by Zhengqiang Li, Mingjun Liang, Yan Ma, Yang Zheng, Zhaozhou Li and Zhenting Chen
Remote Sens. 2024, 16(24), 4676; https://doi.org/10.3390/rs16244676 - 14 Dec 2024
Viewed by 879
Abstract
In the optical satellite on-orbit imaging quality estimation system, the calculation of Modulation Transfer Function (MTF) is not fully standardized, and the influence of atmosphere is often simplified, making it difficult to obtain completely consistent on-orbit MTF measurements and comparisons. This study investigates [...] Read more.
In the optical satellite on-orbit imaging quality estimation system, the calculation of Modulation Transfer Function (MTF) is not fully standardized, and the influence of atmosphere is often simplified, making it difficult to obtain completely consistent on-orbit MTF measurements and comparisons. This study investigates the effects of various factors—such as edge angle, edge detection methods, oversampling rate, and interpolation techniques—on the accuracy of MTF calculations in the commonly used slanted-edge method for on-orbit MTF assessment, informed by simulation experiments. A relatively optimal MTF calculation process is proposed, which employs the Gaussian fitting method for edge detection, the adaptive oversampling rate, and the Lanczos (a = 3) interpolation method, minimizing the absolute deviation in the MTF results. A method to quantitatively analyze the atmospheric scattering and absorption MTF is proposed that employs a radiative transfer model. Based on the edge images of GF-2 satellite, images with various atmospheric conditions and imaging parameters are simulated, and their atmospheric scattering and absorption MTF is obtained through comparing the MTFs of the ground and top atmosphere radiance. The findings reveal that aerosol optical depth (AOD), viewing zenith angle (VZA), and altitude (ALT) are the primary factors influencing the accuracy of GF-2 satellite on-orbit MTF measurements in complex scenarios. The on-orbit MTF decreases with the increase in AOD and VZA and increases with the increase in ALT. Furthermore, a collaborative analysis of the main influencing factors of atmospheric scattering and absorption MTF indicates that, taking the PAN band of the GF-2 satellite as an example, the atmospheric MTF values are consistently below 0.7905. Among these, 90% of the data are less than 0.7520, with corresponding AOD conditions ranging from 0 to 0.08, a VZA ranging from 0 to 50°, and an ALT ranging from 0 to 5 km. The results can provide directional guidance for the selection of meteorological conditions, satellite attitude, and geographical location during satellite on-orbit testing, thereby enhancing the ability to accurately measure satellite MTF. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>The PAN band image of the GF-2 satellite on 24 October 2021 at the Baotou site.</p>
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<p>Overall flowchart of this study.</p>
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<p>Flow chart of the quantitative calculation of atmospheric effects based on the atmospheric radiation transfer model.</p>
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<p>Frequency variations in (<b>a</b>) system MTF, (<b>b</b>) detector MTF, (<b>c</b>) aberration ATF, and (<b>d</b>) diffraction-limited optics OTF in the PAN band of the GF2 satellite for edge tilt angles of 0.5–44.5°.</p>
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<p>Variation in MTF in polar coordinates at edge inclination angles of 0.5–44.5°, with angular intervals of 0.2°, where (<b>a</b>) is the case of the adaptive oversampling rate under the Gaussian fitting method, (<b>b</b>) is the adaptive oversampling rate under the error fitting method, and (<b>c</b>) is the adaptive oversampling rate under the centroid detection method.</p>
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<p>Group diagram of the effect of doubling rate on MTF, where (<b>a</b>–<b>d</b>) are the Gaussian fitting method, (<b>e</b>–<b>h</b>) are the error fitting method, and (<b>i</b>–<b>l</b>) are the centroid detection fitting method. The first column of each row of images represents the case of no oversampling, the second column represents the case of 2× oversampling, the third column represents the case of 4× oversampling, and the fourth column represents the case of 8×oversampling.</p>
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<p>Group diagram of the effect of interpolation methods on MTF, where (<b>a</b>) is the Lanczos (a = 3) interpolation method, (<b>b</b>) is the continuum magic interpolation method, (<b>c</b>) is the Lanczos (a = 2) interpolation method, (<b>d</b>) is the f Lanczos (a = 1) interpolation method, (<b>e</b>) is the Bin average interpolation method, and (<b>f</b>) is the Mitchell kernel interpolation method.</p>
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<p>Group diagram of the results of atmospheric scattering and absorption MTF variations in various bands calculated based on satellite images, where (<b>a</b>) AOD, (<b>b</b>) CWV, (<b>c</b>) SZA, (<b>d</b>) ALT, (<b>e</b>) RAZ, and (<b>f</b>) SZA.</p>
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<p>(<b>a</b>) The distribution of MTF values of different edge detection methods, (<b>b</b>) the distribution of MTF values of different interpolation methods, and (<b>c</b>) the distribution of MTF values for different oversampling rates. (<b>d</b>) The distribution of ΔMTF values of different edge detection methods, (<b>e</b>) the distribution of ΔMTF values of different interpolation methods, and (<b>f</b>) the distribution of ΔMTF values for different oversampling rates. For (<b>b</b>) and (<b>e</b>), Lanczos (a = 3), Continuum magic, Lanczos (a = 2), Lanczos (a = 1), Bin average, and Mitchell kernel are abbreviated, respectively, as L (a = 3), CM, L (a = 2), L (a = 1), BA, MK; for (<b>c</b>) and (<b>f</b>), adaptive oversampling, no oversampling, 2× oversampling, 4× oversampling, and 8× oversampling is abbreviated, respectively, as AO, NO, 2×O, 4×O, 8×O. The red solid line in the middle of the box plot represents the median MTF value, the blue lines at the top and bottom respectively indicate the first and third quartiles of the MTF value, and the red dashed line at 0.1283 indicates the theoretical value of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>T</mi> <mi>F</mi> </mrow> <mrow> <mi>s</mi> <mi>y</mi> <mi>s</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
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<p>(<b>a</b>) The distribution of MTF values of different edge detection methods, (<b>b</b>) the distribution of MTF values of different interpolation methods, and (<b>c</b>) the distribution of MTF values for different oversampling rates. (<b>d</b>) The distribution of ΔMTF values of different edge detection methods, (<b>e</b>) the distribution of ΔMTF values of different interpolation methods, and (<b>f</b>) the distribution of ΔMTF values for different oversampling rates. For (<b>b</b>) and (<b>e</b>), Lanczos (a = 3), Continuum magic, Lanczos (a = 2), Lanczos (a = 1), Bin average, and Mitchell kernel are abbreviated, respectively, as L (a = 3), CM, L (a = 2), L (a = 1), BA, MK; for (<b>c</b>) and (<b>f</b>), adaptive oversampling, no oversampling, 2× oversampling, 4× oversampling, and 8× oversampling is abbreviated, respectively, as AO, NO, 2×O, 4×O, 8×O. The red solid line in the middle of the box plot represents the median MTF value, the blue lines at the top and bottom respectively indicate the first and third quartiles of the MTF value, and the red dashed line at 0.1283 indicates the theoretical value of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>T</mi> <mi>F</mi> </mrow> <mrow> <mi>s</mi> <mi>y</mi> <mi>s</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
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<p>Histogram of the atmospheric scattering and absorption MTF for the PAN band, accompanied by a cumulative data curve. Three vertical black dashed lines indicate the positions at which the cumulative percentages reach 50%, 80%, and 90%, respectively.</p>
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<p>Group diagram illustrating ranges of atmospheric conditions that satisfy the different requirements for atmospheric impact, including (<b>a</b>) an atmospheric scattering and absorption MTF above 0.75, (<b>b</b>) an atmospheric scattering and absorption MTF above 0.78, and (<b>c</b>) an atmospheric scattering and absorption MTF above 0.79, depicted in three-dimensional positions.</p>
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15 pages, 16510 KiB  
Article
Mosaicking and Correction Method of Gaofen-3 ScanSAR Images in Coastal Areas with Subswath Overlap Range Constraints
by Jiajun Wang, Guowang Jin, Xin Xiong, Jiahao Li, Hao Ye and He Yang
J. Mar. Sci. Eng. 2024, 12(12), 2277; https://doi.org/10.3390/jmse12122277 - 11 Dec 2024
Viewed by 499
Abstract
The ScanSAR mode image obtained by the Gaofen-3 (GF-3) satellite has an imaging width of up to 130–500 km, which is of great significance in monitoring oceanography, meteorology, water conservancy, and transportation. To address the issues of subswath misalignment and the inability to [...] Read more.
The ScanSAR mode image obtained by the Gaofen-3 (GF-3) satellite has an imaging width of up to 130–500 km, which is of great significance in monitoring oceanography, meteorology, water conservancy, and transportation. To address the issues of subswath misalignment and the inability to correct in the processing of GF-3 ScanSAR images in coastal areas using software such as PIE, ENVI, and SNAP, a method for mosaicking and correcting GF-3 ScanSAR images with subswaths that overlap within specified range constraints is proposed. This method involves correlating the coefficients of each subswath thumbnail image in order to determine the extent of the overlap range. Given that the matching points are constrained to the overlap between subswaths, the normalized cross-correlation (NCC) matching algorithm is utilized to calculate the matching points between subswaths. Subsequently, the random sampling consistency (RANSAC) algorithm is employed to eliminate the mismatching points. Subsequently, the subswaths should be mosaicked together with the stitching translation of subswaths, based on the coordinates of the matching points. The image brightness correction coefficient is calculated based on the average grayscale value of pixels in the overlapping region. This is performed in order to correct the grayscale values of adjacent subswaths and thereby reducing the brightness difference at the junction of subswaths. The entire ScanSAR slant range image is produced. By employing the Range–Doppler model for indirect orthorectification, corrected images with geographic information are generated. The experiment utilized three coastal GF-3 ScanSAR images for mosaicking and correction, and the results were contrasted with those attained through PIE software V7.0 processing. This was conducted to substantiate the efficacy and precision of the methodology for mosaicking and correcting coastal GF-3 ScanSAR images. Full article
(This article belongs to the Special Issue Ocean Observations)
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<p>Workflow of this study.</p>
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<p>Mapping relationship between image-matching windows.</p>
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<p>Mosaic relationship between subswaths.</p>
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<p>Distribution diagrams of image connection points obtained by the method presented in this paper: (<b>a</b>) the distribution diagram of image connection points in image 1; (<b>b</b>) the distribution diagram of image connection points in image 2; (<b>c</b>) the distribution diagram of image connection points in image 3.</p>
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<p>Distribution diagrams of wrong image connection points obtained by the method presented in study [<a href="#B17-jmse-12-02277" class="html-bibr">17</a>]: (<b>a</b>) the distribution diagram of image connection points in image 1; (<b>b</b>) the distribution diagram of image connection points in image 2; (<b>c</b>) the distribution diagram of image connection points in image 3.</p>
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<p>The result of PIE software processing of the mosaicking dislocation: (<b>a</b>) mosaic misalignment in image 1; (<b>b</b>) mosaic misalignment in image 1; (<b>c</b>) mosaic misalignment in image 2; (<b>d</b>) mosaic misalignment in image 2; (<b>e</b>) mosaic misalignment in image 2; (<b>f</b>) mosaic misalignment in image 3.</p>
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<p>Area 1 image-mosaicking results: (<b>a</b>) the results of the method presented in this paper before brightness correction; (<b>b</b>) the results of the method presented in this paper after brightness correction; (<b>c</b>) the results of PIE software, and the differences in image widths are caused by its mosaicking errors; (<b>d</b>) the results of the method presented in study [<a href="#B17-jmse-12-02277" class="html-bibr">17</a>], and the differences in image widths are caused by its mosaicking errors.</p>
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<p>Area 2 image-mosaicking results: (<b>a</b>) the results of the method presented in this paper before brightness correction; (<b>b</b>) the results of the method presented in this paper after brightness correction; (<b>c</b>) the results of PIE software, and the differences in image widths are caused by its mosaicking errors; (<b>d</b>) the results of the method presented in study [<a href="#B17-jmse-12-02277" class="html-bibr">17</a>], and the differences in image widths are caused by its mosaicking errors.</p>
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<p>Area 3 image-mosaicking results: (<b>a</b>) the results of the method presented in this paper before brightness correction; (<b>b</b>) the results of the method presented in this paper after brightness correction; (<b>c</b>) the results of PIE software, and the differences in image widths are caused by its mosaicking errors; (<b>d</b>) the results of the method presented in study [<a href="#B17-jmse-12-02277" class="html-bibr">17</a>], and the differences in image widths are caused by its mosaicking errors.</p>
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<p>Image correction results of the method presented in this paper: (<b>a</b>) image 1 correction result; (<b>b</b>) image 2 correction result; (<b>c</b>) image 3 correction result.</p>
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<p>The corrected subswath image obtained by the RPC correcting.</p>
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<p>Result with incorrect rotations.</p>
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7 pages, 11708 KiB  
Proceeding Paper
Urban Functional Zone Mapping by Integrating Multi-Source Data and Spatial Relationship Characteristics
by Daoyou Zhu, Xu Dang, Wenjia Shi, Yixiang Chen and Wenmei Li
Proceedings 2024, 110(1), 17; https://doi.org/10.3390/proceedings2024110017 - 4 Dec 2024
Viewed by 607
Abstract
Timely and precise acquisition of urban functional zone (UFZ) information is crucial for effective urban planning, management, and resource allocation. However, current UFZ mapping approaches primarily focus on individual functional units’ visual and semantic characteristics, often overlooking the crucial spatial relationships between them, [...] Read more.
Timely and precise acquisition of urban functional zone (UFZ) information is crucial for effective urban planning, management, and resource allocation. However, current UFZ mapping approaches primarily focus on individual functional units’ visual and semantic characteristics, often overlooking the crucial spatial relationships between them, resulting in classification inaccuracies. To address this limitation, our study presents a novel framework for UFZ classification that seamlessly integrates visual image features, Points of Interest (POI) semantic attributes, and spatial relationship information. This framework leverages the OpenStreetMap (OSM) road network to partition the study area into functional units, employs a graph model to represent urban functional nodes and their intricate spatial topological relationships, and harnesses the capabilities of Graph Convolutional Network (GCN) to fuse these multi-dimensional features through end-to-end learning for accurate urban function discrimination. Experimental evaluations utilizing Gaofen-2 (GF-2) satellite imagery, POI data, and OSM road network information from Shenzhen, China have yielded remarkable results. Our method has achieved significant improvements in classification accuracy across all functional categories, surpassing approaches that rely solely on visual or semantic features. Notably, the overall classification accuracy reached an impressive 87.92%, marking a significant 2.08% increase over methods that disregard spatial relationship features. Furthermore, our method has demonstrated superior performance when compared to similar techniques, underscoring its effectiveness and potential for widespread application in UFZ classification. Full article
(This article belongs to the Proceedings of The 31st International Conference on Geoinformatics)
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<p>GF-2 satellite imagery of Shenzhen.</p>
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<p>The proposed framework for UFZ classification.</p>
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<p>Confusion matrices for different features. (<b>a</b>) Visual features; (<b>b</b>) semantic features; (<b>c</b>) visual and semantic features; (<b>d</b>) visual, semantic, and spatial relationship features.</p>
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<p>UFZ mapping results that integrate visual, semantic, and spatial relationship features.</p>
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8 pages, 4795 KiB  
Proceeding Paper
Unsupervised Domain Adaptive Transfer Learning for Urban Built-Up Area Extraction
by Feifei Peng, Shuai Yao, Yixiang Chen and Wenmei Li
Proceedings 2024, 110(1), 10; https://doi.org/10.3390/proceedings2024110010 - 3 Dec 2024
Viewed by 473
Abstract
Built-up areas are the main gathering place for human activities. The widespread availability of various satellite sensors provides a rich data source for mapping built-up areas. Deep learning can automatically learn multi-level features of targets from sample data in an end-to-end manner, overcoming [...] Read more.
Built-up areas are the main gathering place for human activities. The widespread availability of various satellite sensors provides a rich data source for mapping built-up areas. Deep learning can automatically learn multi-level features of targets from sample data in an end-to-end manner, overcoming the limitations of traditional methods based on handcrafted features. However, existing deep-learning-based methods rely on the quantity and distribution of sample data, and the trained models often exhibit limited generalization ability when faced with image data from novel scenarios. To effectively tackle this issue, this study proposes an unsupervised domain adaptive transfer learning method based on adversarial machine learning. This method aims to utilize the feature information of the source domain to train a classifier suitable for target domain feature discrimination without requiring a target domain label, and achieve built-up area extraction of different sensor images. The model comprises a feature extraction module, a label classification module, and a domain discrimination module. Through adversarial training, the feature knowledge from the source domain is transferred to the target domain, achieving feature alignment and efficient discrimination of built-up areas. The Gaofen-2 (GF-2) and Sentinel-2 datasets were employed for experimental evaluation. The results show that the proposed method, trained on the GF-2 image dataset (source domain), can be transferred unsupervised to the Sentinel-2 image dataset (target domain), demonstrating robust detection performance. Further comparative experiments have also demonstrated the superiority of our method in extracting built-up areas through transfer learning. Full article
(This article belongs to the Proceedings of The 31st International Conference on Geoinformatics)
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<p>Proposed framework.</p>
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<p>Extraction results of different methods: (<b>a</b>) The test images from left to right are Fu’an, Fuqing, Shenzhen1, and Shenzhen2; (<b>b</b>) Ground truths; (<b>c</b>) Baseline1; (<b>d</b>) Baseline2; (<b>e</b>) Baseline3; (<b>f</b>) Baseline4; (<b>g</b>) Proposed method.</p>
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<p>Sentinel-2 image and extraction results in Shenzhen City.</p>
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<p>Sentinel-2 image and extraction results in Zhuhai City.</p>
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<p>Sentinel-2 image and extraction results in Xiamen City.</p>
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