33 research outputs found

    A subpixel target detection algorithm for hyperspectral imagery

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    The goal of this research is to develop a new algorithm for the detection of subpixel scale target materials on the hyperspectral imagery. The signal decision theory is typically to decide the existence of a target signal embedded in the random noise. This implies that the detection problem can be mathematically formalized by signal decision theory based on the statistical hypothesis test. In particular, since any target signature provided by airborne/spaceborne sensors is embedded in a structured noise such as background or clutter signatures as well as broad band unstructured noise, the problem becomes more complicated, and particularly much more under the unknown noise structure. The approach is based on the statistical hypothesis method known as Generalized Likelihood Ratio Test (GLRT). The use of GLRT requires estimating the unknown parameters, and assumes the prior information of two subspaces describing target variation and background variation respectively. Therefore, this research consists of two parts, the implementation of GLRT and the characterization of two subspaces through new approaches. Results obtained from computer simulation, HYDICE image and AVI RIS image show that this approach is feasible

    MDAS: a new multimodal benchmark dataset for remote sensing

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    In Earth observation, multimodal data fusion is an intuitive strategy to break the limitation of individual data. Complementary physical contents of data sources allow comprehensive and precise information retrieval. With current satellite missions, such as ESA Copernicus programme, various data will be accessible at an affordable cost. Future applications will have many options for data sources. Such a privilege can be beneficial only if algorithms are ready to work with various data sources. However, current data fusion studies mostly focus on the fusion of two data sources. There are two reasons; first, different combinations of data sources face different scientific challenges. For example, the fusion of synthetic aperture radar (SAR) data and optical images needs to handle the geometric difference, while the fusion of hyperspectral and multispectral images deals with different resolutions on spatial and spectral domains. Second, nowadays, it is still both financially and labour expensive to acquire multiple data sources for the same region at the same time. In this paper, we provide the community with a benchmark multimodal data set, MDAS, for the city of Augsburg, Germany. MDAS includes synthetic aperture radar data, multispectral image, hyperspectral image, digital surface model (DSM), and geographic information system (GIS) data. All these data are collected on the same date, 7ย Mayย 2018. MDAS is a new benchmark data set that provides researchers rich options on data selections. In this paper, we run experiments for three typical remote sensing applications, namely, resolution enhancement, spectral unmixing, and land cover classification, on MDAS data set. Our experiments demonstrate the performance of representative state-of-the-art algorithms whose outcomes can serve as baselines for further studies. The dataset is publicly available at https://doi.org/10.14459/2022mp1657312 (Hu etย al.,ย 2022a) and the code (including the pre-trained models) at https://doi.org/10.5281/zenodo.7428215 (Hu etย al.,ย 2022b)

    Radiometrically-Accurate Hyperspectral Data Sharpening

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    Improving the spatial resolution of hyperpsectral image (HSI) has traditionally been an important topic in the field of remote sensing. Many approaches have been proposed based on various theories including component substitution, multiresolution analysis, spectral unmixing, Bayesian probability, and tensor representation. However, these methods have some common disadvantages, such as that they are not robust to different up-scale ratios and they have little concern for the per-pixel radiometric accuracy of the sharpened image. Moreover, many learning-based methods have been proposed through decades of innovations, but most of them require a large set of training pairs, which is unpractical for many real problems. To solve these problems, we firstly proposed an unsupervised Laplacian Pyramid Fusion Network (LPFNet) to generate a radiometrically-accurate high-resolution HSI. First, with the low-resolution hyperspectral image (LR-HSI) and the high-resolution multispectral image (HR-MSI), the preliminary high-resolution hyperspectral image (HR-HSI) is calculated via linear regression. Next, the high-frequency details of the preliminary HR-HSI are estimated via the subtraction between it and the CNN-generated-blurry version. By injecting the details to the output of the generative CNN with the low-resolution hyperspectral image (LR-HSI) as input, the final HR-HSI is obtained. LPFNet is designed for fusing the LR-HSI and HR-MSI covers the same Visible-Near-Infrared (VNIR) bands, while the short-wave infrared (SWIR) bands of HSI are ignored. SWIR bands are equally important to VNIR bands, but their spatial details are more challenging to be enhanced because the HR-MSI, used to provide the spatial details in the fusion process, usually has no SWIR coverage or lower-spatial-resolution SWIR. To this end, we designed an unsupervised cascade fusion network (UCFNet) to sharpen the Vis-NIR-SWIR LR-HSI. First, the preliminary high-resolution VNIR hyperspectral image (HR-VNIR-HSI) is obtained with a conventional hyperspectral algorithm. Then, the HR-MSI, the preliminary HR-VNIR-HSI, and the LR-SWIR-HSI are passed to the generative convolutional neural network to produce an HR-HSI. In the training process, the cascade sharpening method is employed to improve stability. Furthermore, the self-supervising loss is introduced based on the cascade strategy to further improve the spectral accuracy. Experiments are conducted on both LPFNet and UCFNet with different datasets and up-scale ratios. Also, state-of-the-art baseline methods are implemented and compared with the proposed methods with different quantitative metrics. Results demonstrate that proposed methods outperform the competitors in all cases in terms of spectral and spatial accuracy

    A multiscale remote sensing assessment of subtropical indigenous forests along the wild coast, South Africa

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    The subtropical forests located along South Africaโ€™s Wild Coast region, declared as one of the biodiversity hotspots, provide benefits to the local and national economy. However, there is evidence of increased pressure exerted on the forests by growing population and reduced income from activities not related to forest products. The ability of remote sensing to quantify subtropical forest changes over time, perform species discrimination (using field spectroscopy) and integrating field spectral and multispectral data were all assessed in this study. Investigations were conducted at pixel, leaf and sub-pixel levels. Both per-pixel and sub-pixel classification methods were used for improved forest characterisation. Using SPOT 6 imagery for 2013, the study determined the best classification algorithm for mapping sub-tropical forest and other land cover types to be the maximum likelihood classifier. Maximum likelihood outperformed minimum distance, spectral angle mapper and spectral information divergence algorithms, based on overall accuracy and Kappa coefficient values. Forest change analysis was made based on spectral measurements made at top of the atmosphere (TOC) level. When applied to the 2005 and 2009 SPOT 5 images, subtropical forest changes between 2005-2009 and 2009-2013 were quantified. A temporal analysis of forest cover trends in the periods 2005-2009 and 2009-2013 identified a decreasing trend of -3648.42 and -946.98 ha respectively, which translated to 7.81 percent and 2.20 percent decrease. Although there is evidence of a trend towards decreased rates of forest loss, more conservation efforts are required to protect the Wild Coast ecosystem. Using field spectral measurements data, the hierarchical method (comprising One-way ANOVA with Bonferroni correction, Classification and Regression Trees (CART) and Jeffries Matusita method) successfully selected optimal wavelengths for species discrimination at leaf level. Only 17 out of 2150 wavelengths were identified, thereby reducing the complexities related to data dimensionality. The optimal 17 wavelength bands were noted in the visible (438, 442, 512 and 695 nm), near infrared (724, 729, 750, 758, 856, 936, 1179, 1507 and 1673 nm) and mid-infrared (2220, 2465, 2469 and 2482 nm) portions of the electromagnetic spectrum. The Jeffries-Matusita (JM) distance method confirmed the separability of the selected wavelength bands. Using these 17 wavelengths, linear discriminant analysis (LDA) classified subtropical species at leaf level more accurately than partial least squares discriminant analysis (PLSDA) and random forest (RF). In addition, the study integrated field-collected canopy spectral and multispectral data to discriminate proportions of semi-deciduous and evergreen subtropical forests at sub-pixel level. By using the 2013 land cover (using MLC) to mask non-forested portions before sub-pixel classification (using MTMF), the proportional maps were a product of two classifiers. The proportional maps show higher proportions of evergreen forests along the coast while semi-deciduous subtropical forest species were mainly on inland parts of the Wild Coast. These maps had high accuracy, thereby proving the ability of an integration of field spectral and multispectral data in mapping semi-deciduous and evergreen forest species. Overall, the study has demonstrated the importance of the MLC and LDA and served to integrate field spectral and multispectral data in subtropical forest characterisation at both leaf and top-of-atmosphere levels. The success of both the MLC and LDA further highlighted how essential parametric classifiers are in remote sensing forestry applications. Main subtropical characteristics highlighted in this study were species discrimination at leaf level, quantifying forest change at pixel level and discriminating semi-deciduous and evergreen forests at sub-pixel level

    Urban Growth and LULC Change Dynamics Using Landsat Record of Region of Waterloo from 1984 to 2013

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    Frequent human activities resulted by rapid urbanization lead to a variety of urban-related environmental and socio-economic issues. Therefore, for effective environmental management and urban planning, monitoring urban growth and detecting its resulting land use and land cover (LULC) change is very important. Most of the previous studies focused on bi-temporal or coarsely multi-temporal change detection to extract stationary change information over a time span. However, higher-order change information, for instance, acceleration or deceleration of urban growth, which would not be observed by bi-temporal method, is more meaningful information for policy makers to understand the urbanization process. With the free access to the USGS Landsat archive and development of remote sensing techniques, detecting urban growth pattern (intensification or sprawl) and LULC change dynamics with temporally high frequent datasets become possible. In this study, bi-temporal, multi-temporal and long-term annual change detection were applied to the Region of Waterloo, Ontario, Canada, to identify the urban growth pattern and LULC change dynamics. Classification was performed for each scene to extract LULC information from 1984 to 2013. This study demonstrates that machine learning classifiers, such as support vector machine (SVM), random forest (RF) and artificial neural network (ANN), perform better than classical maximum likelihood classifier (MLC), among which SVM performs the best. Total urban built-up area of the Region of Water increased from 30% in 1984 to 55% in 2013, replacing large area of vegetated area (agricultural lands and grassland. Outward (sprawl) and inward (intensification) growth patterns were detected both spatially and temporally. Within this time span, built-up area experienced a relatively accelerating growth in 1990s and in early 2000s. In terms of long-term record, Kitchener had the fastest growing rate of low-density built-up (residential) area. The coverage of high-density built-up (commercial and industrial) area in Cambridge increased most dramatically. And the built-up area of Waterloo experienced the lowest growth rate. These important findings indicate that using long-term temporal-dense Landsat datasets enables monitoring of urban growth and LULC change dynamics. Such valuable long-term results can be used for better analysis of urban growth and LULC change patterns for planners and policy makers to comprehensively understand the urbanization process in the past and make better planning in the future

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    ํ•™์œ„๋…ผ๋ฌธ(๋ฐ•์‚ฌ) -- ์„œ์šธ๋Œ€ํ•™๊ต๋Œ€ํ•™์› : ๊ณต๊ณผ๋Œ€ํ•™ ๊ฑด์„คํ™˜๊ฒฝ๊ณตํ•™๋ถ€, 2022. 8. ์„œ์ผ์›.๊ธฐ์กด์˜ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ ๋†๋„ ๊ณ„์ธก์€ ์ƒ˜ํ”Œ๋ง ๊ธฐ๋ฐ˜ ์ง์ ‘๊ณ„์ธก ๋ฐฉ์‹์— ์˜์กดํ•˜์—ฌ ์‹œ๊ณต๊ฐ„์  ๊ณ ํ•ด์ƒ๋„ ์ž๋ฃŒ ์ทจ๋“์ด ์–ด๋ ค์šด ์‹ค์ •์ด๋‹ค. ์ด๋Ÿฌํ•œ ํ•œ๊ณ„์ ์„ ๊ทน๋ณตํ•˜๊ธฐ ์œ„ํ•ด ์ตœ๊ทผ ์œ„์„ฑ๊ณผ ๋“œ๋ก ์„ ํ™œ์šฉํ•˜์—ฌ ์ดฌ์˜๋œ ๋‹ค๋ถ„๊ด‘ ํ˜น์€ ์ดˆ๋ถ„๊ด‘ ์˜์ƒ์„ ํ†ตํ•ด ๊ณ ํ•ด์ƒ๋„์˜ ๋ถ€์œ ์‚ฌ๋†๋„ ์‹œ๊ณต๊ฐ„๋ถ„ํฌ๋ฅผ ๊ณ„์ธกํ•˜๋Š” ๊ธฐ๋ฒ•์— ๋Œ€ํ•œ ์—ฐ๊ตฌ๊ฐ€ ํ™œ๋ฐœํžˆ ์ง„ํ–‰๋˜๊ณ  ์žˆ๋‹ค. ํ•˜์ง€๋งŒ, ๋‹ค๋ฅธ ํ•˜์ฒœ ๋ฌผ๋ฆฌ๋Ÿ‰ ๊ณ„์ธก์— ๋น„ํ•ด ๋ถ€์œ ์‚ฌ ๊ณ„์ธก ์—ฐ๊ตฌ๋Š” ํ•˜์ฒœ์— ๋”ฐ๋ผ ๋ถ€์œ ์‚ฌ๊ฐ€ ๋‹ค์–‘ํ•˜๊ฒŒ ๋ถ„ํฌํ•˜๊ณ  ๋‹ค๋ฅธ ๋ถ€์œ ๋ฌผ์งˆ ํ˜น์€ ํ•˜์ƒ์— ์˜ํ•œ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ์˜ ์˜ํ–ฅ ๋•Œ๋ฌธ์— ๋ถ„๊ด‘ ์ž๋ฃŒ๋ฅผ ํ†ตํ•ด ์ •ํ™•ํ•œ ๋ถ€์œ ์‚ฌ๋†๋„ ๋ถ„ํฌ๋ฅผ ์žฌํ˜„ํ•˜๊ธฐ ์–ด๋ ค์šด ์‹ค์ •์ด๋‹ค. ํŠนํžˆ, ๋ถ€์œ ์‚ฌ ๋ถ„๊ด‘ ํŠน์„ฑ์— ์˜ํ–ฅ์„ ๋ฏธ์น˜๋Š” ์ž…๋„๋ถ„ํฌ, ๊ด‘๋ฌผํŠน์„ฑ, ์นจ๊ฐ•์„ฑ ๋“ฑ์ด ํ•˜์ฒœ์— ๋”ฐ๋ผ ๊ฐ•ํ•œ ์ง€์—ญ์„ฑ์„ ๋‚˜ํƒ€๋‚ด๊ธฐ์— ์ด๋Ÿฌํ•œ ์š”์ธ์—์„œ ์•ผ๊ธฐ๋˜๋Š” ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์œผ๋กœ ์ธํ•ด ํŠน์ • ์‹œ๊ธฐ์™€ ์ง€์—ญ์—๋งŒ ์ ํ•ฉํ•œ ์›๊ฒฉํƒ์‚ฌ ๊ธฐ๋ฐ˜ ๊ณ„์ธก ๋ชจํ˜•๋“ค์ด ๊ฐœ๋ฐœ๋˜์–ด ์™”๋‹ค. ๋ณธ ์—ฐ๊ตฌ์—์„œ๋Š” ์ด๋Ÿฌํ•œ ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์„ ๋ฐ˜์˜ํ•˜์—ฌ ๋‹ค์–‘ํ•œ ํ•˜์ฒœ ๋ฐ ์œ ์‚ฌ ์กฐ๊ฑด์—์„œ ์ ์šฉ ๊ฐ€๋Šฅํ•œ ๊ณ ํ•ด์ƒ๋„ ์ดˆ๋ถ„๊ด‘์˜์ƒ์„ ํ™œ์šฉํ•œ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ๋†๋„ ๊ณ„์ธก๋ฐฉ๋ฒ•์„ ๊ฐœ๋ฐœํ•˜๊ธฐ ์œ„ํ•ด ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘ํ™” ๊ธฐ๋ฒ•๊ณผ ๋‹ค์–‘ํ•œ ํŒŒ์žฅ๋Œ€์˜ ๋ถ„๊ด‘ ๋ฐด๋“œ๋ฅผ ํ•™์Šตํ•  ์ˆ˜ ์žˆ๋Š” ๊ธฐ๊ณ„ํ•™์Šต ํšŒ๊ท€ ๋ชจํ˜•์„ ๊ฒฐํ•ฉํ•˜์—ฌ CMR-OV๋ผ๋Š” ๋ฐฉ๋ฒ•๋ก ์„ ์ œ์‹œํ•˜์˜€๋‹ค. CMR-OV ๊ฐœ๋ฐœ ๋ฐ ๊ฒ€์ฆ์€ 1) ์‹คํ—˜์  ์—ฐ๊ตฌ๋ฅผ ํ†ตํ•œ ํ•˜์ฒœ ๋ถ€์œ ์‚ฌ ๋ถ„๊ด‘ ํŠน์„ฑ์˜ ์ฃผ์š” ๊ต๋ž€ ์š”์ธ ๋ถ„์„, 2) ์ตœ์  ํšŒ๊ท€๋ชจํ˜• ์„ ์ • ๋ฐ ์ดˆ๋ถ„๊ด‘ ํด๋Ÿฌ์Šคํ„ฐ๋ง๊ณผ์˜ ๊ฒฐํ•ฉ, 3) ํ˜„์žฅ์ ์šฉ์„ฑ ํ‰๊ฐ€์˜ ๊ณผ์ •์„ ๊ฑฐ์ณ ์ˆ˜ํ–‰๋˜์—ˆ๋‹ค. ์‹คํ—˜์  ์—ฐ๊ตฌ์—์„œ๋Š” ์šฐ์„  ์‹ค๋‚ด ์‹คํ—˜์‹ค์—์„œ ํšก๋ฐฉํ–ฅ ํ˜ผํ•ฉ๊ธฐ๋ฅผ ํ™œ์šฉํ•˜์—ฌ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ๋ฅผ ์ œ๊ฑฐํ•˜๊ณ  ์™„์ „ ํ˜ผํ•ฉ๋œ ์ƒํƒœ์—์„œ ๋ถ€์œ ์‚ฌ์˜ ๊ณ ์œ  ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ ์ž๋ฃŒ๋ฅผ ์ˆ˜์ง‘ํ•˜์˜€๋‹ค. ์ด๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ์‹ค์ œ ํ•˜์ฒœ๊ณผ ์œ ์‚ฌํ•œ ์กฐ๊ฑด์˜ ์‹ค๊ทœ๋ชจ ์˜ฅ์™ธ ์ˆ˜๋กœ ์‹คํ—˜์—์„œ ๋‹ค์–‘ํ•œ ์œ ์‚ฌ ํŠน์„ฑ(์ž…๋„ ๋ฐ ๊ด‘๋ฌผ)๊ณผ ํ•˜์ƒ ํŠน์„ฑ(์‹์ƒ ๋ฐ ๋ชจ๋ž˜)์— ๋Œ€ํ•œ ์ดˆ๋ถ„๊ด‘ ์ž๋ฃŒ๋ฅผ ์ˆ˜์ง‘ํ•˜์—ฌ ๊ณ ์œ  ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ๊ณผ ๋น„๊ตํ•˜์˜€๋‹ค. ๊ทธ ๊ฒฐ๊ณผ, ๋ถ€์œ ์‚ฌ์˜ ๋ถ„๊ด‘ ํŠน์„ฑ์€ ์œ ์‚ฌ์˜ ์ข…๋ฅ˜ ๋ฐ ์ž…๋„์— ๋”ฐ๋ผ ๋†๋„ ์ฆ๊ฐ€์— ๋”ฐ๋ฅธ ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ์˜ ๋ฐ˜์‚ฌ์œจ ๋ณ€ํ™”๊ฐ€ ์ƒ์ดํ•˜๊ฒŒ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ๋˜ํ•œ, 1 m ์ดํ•˜์˜ ์–•์€ ์ˆ˜์‹ฌ ์กฐ๊ฑด์—์„œ๋Š” ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ์˜ ์˜ํ–ฅ์œผ๋กœ ํ•˜์ƒ ์ข…๋ฅ˜์— ๋”ฐ๋ผ ์ดˆ๋ถ„๊ด‘ ์ŠคํŽ™ํŠธ๋Ÿผ์˜ ๊ฐœํ˜•์ด ํฌ๊ฒŒ ๋ณ€ํ™”ํ•˜์˜€์œผ๋ฉฐ, ๊ณ ๋†๋„์˜ ๋ถ€์œ ์‚ฌ๊ฐ€ ๋ถ„ํฌํ•  ๋•Œ๋„ ๋ฐ”๋‹ฅ ๋ฐ˜์‚ฌ๊ฐ€ ํฌ๊ฒŒ ์˜ํ–ฅ์„ ๋ฏธ์น˜๋Š” ๊ฒƒ์„ ํ™•์ธํ•˜์˜€๋‹ค. ์ด๋Ÿฌํ•œ ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์ด ๋ฐ˜์˜๋œ ๋ถ€์œ ์‚ฌ๋†๋„์™€ ์ดˆ๋ถ„๊ด‘ ์ž๋ฃŒ์˜ ๊ด€๊ณ„๋ฅผ ๊ตฌ์ถ•ํ•˜๊ธฐ ์œ„ํ•˜์—ฌ ๊ธฐ๊ณ„ํ•™์Šต ๊ธฐ๋ฐ˜ ๋žœ๋คํฌ๋ ˆ์ŠคํŠธ ํšŒ๊ท€ ๋ชจํ˜•๊ณผ ๊ฐ€์šฐ์‹œ์•ˆ ํ˜ผํ•ฉ ๋ชจํ˜• ๊ธฐ๋ฐ˜ ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘ ๊ธฐ๋ฒ•์„ ๊ฒฐํ•ฉํ•œ CMR-OV๋ฅผ ์ ์šฉํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ์—ฐ๊ตฌ๋“ค์—์„œ ์ฃผ๋กœ ํ™œ์šฉ๋œ ๋ฐด๋“œ๋น„ ๊ธฐ๋ฐ˜์˜ ๋ชจํ˜•๊ณผ ๋‹จ์ผ ๊ธฐ๊ณ„ํ•™์Šต๋ชจํ˜•์— ๋น„ํ•ด ์ •ํ™•๋„๊ฐ€ ํฌ๊ฒŒ ํ–ฅ์ƒํ•˜์˜€๋‹ค. ํŠนํžˆ, ๊ธฐ์กด ์ตœ์  ๋ฐด๋“œ๋น„ ๋ถ„์„ (OBRA) ๋ฐฉ๋ฒ•์€ ๋น„์„ ํ˜•์„ฑ์„ ๊ณ ๋ คํ•ด๋„ ์ข์€ ์˜์—ญ์˜ ํŒŒ์žฅ๋Œ€๋งŒ์„ ๊ณ ๋ คํ•˜๋Š” ํ•œ๊ณ„์ ์œผ๋กœ ์ธํ•ด ๋ถ„๊ด‘๋‹ค์–‘์„ฑ์„ ๋ฐ˜์˜ํ•˜์ง€ ๋ชปํ•˜๋Š” ๊ฒƒ์œผ๋กœ ๋ฐํ˜€์กŒ๋‹ค. ํ•˜์ง€๋งŒ, CMR-OV๋Š” ํญ ๋„“์€ ํŒŒ์žฅ๋Œ€ ์˜์—ญ์„ ๊ณ ๋ คํ•จ๊ณผ ๋™์‹œ์— ๋†’์€ ์ •ํ™•๋„๋ฅผ ์‚ฐ์ถœํ•˜์˜€๋‹ค. ์ตœ์ข…์ ์œผ๋กœ CMR-OV๋ฅผ ํ™ฉ๊ฐ•์˜ ์ง์„ ๊ตฌ๊ฐ„ ๋ฐ ์‚ฌํ–‰๊ตฌ๊ฐ„๊ณผ ๋‚™๋™๊ฐ•๊ณผ ํ™ฉ๊ฐ•์˜ ํ•ฉ๋ฅ˜๋ถ€์— ์ ์šฉํ•˜์—ฌ ํ˜„์žฅ๊ฒ€์ฆ์„ ์ˆ˜ํ–‰ํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ๋ชจํ˜• ๋Œ€๋น„ ์ •ํ™•๋„์™€ ๋ถ€์œ ์‚ฌ ๋†๋„ ๋งตํ•‘์˜ ์ •๋ฐ€์„ฑ์—์„œ ํฐ ๊ฐœ์„ ์ด ์žˆ์—ˆ์œผ๋ฉฐ, ๋น„ํ•™์Šต์ง€์—ญ์—์„œ๋„ ๋†’์€ ์ •ํ™•๋„๋ฅผ ์‚ฐ์ถœํ•˜์˜€๋‹ค. ํŠนํžˆ, ํ•˜์ฒœ ํ•ฉ๋ฅ˜๋ถ€์—์„œ๋Š” ์ดˆ๋ถ„๊ด‘ ๊ตฐ์ง‘์„ ํ†ตํ•ด ๋‘ ํ•˜์ฒœ ํ๋ฆ„์˜ ๊ฒฝ๊ณ„์ธต์„ ๋ช…ํ™•ํžˆ ๊ตฌ๋ณ„ํ•˜์˜€์œผ๋ฉฐ, ์ด๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ์ง€๋ฅ˜์™€ ๋ณธ๋ฅ˜์— ๋Œ€ํ•ด ๊ฐ๊ฐ ๋ถ„๋ฆฌ๋œ ํšŒ๊ท€๋ชจํ˜•์„ ๊ตฌ์ถ•ํ•˜์—ฌ ๋ณต์žกํ•œ ํ•ฉ๋ฅ˜๋ถ€ ๊ทผ์—ญ ๊ฒฝ๊ณ„์ธต์—์„œ์˜ ๋ถ€์œ ์‚ฌ ๋ถ„ํฌ๋ฅผ ๋ณด๋‹ค ์ •ํ™•ํ•˜๊ฒŒ ์žฌํ˜„ํ•˜์˜€๋‹ค. ๋˜ํ•œ, ๋‚˜์•„๊ฐ€์„œ ์žฌํ˜„๋œ ๊ณ ํ•ด์ƒ๋„์˜ ๋ถ€์œ ์‚ฌ ๊ณต๊ฐ„๋ถ„ํฌ๋ฅผ ๋ฐ”ํƒ•์œผ๋กœ ํ˜ผํ•ฉ๋„๋ฅผ ์‚ฐ์ •ํ•œ ๊ฒฐ๊ณผ, ๊ธฐ์กด ์ ๊ณ„์ธก ๋Œ€๋น„ ์ƒ์„ธํ•˜๊ฒŒ ๋ถ€์œ ์‚ฌ ํ˜ผํ•ฉ์— ๋Œ€ํ•œ ์ •๋Ÿ‰์  ํ‰๊ฐ€๊ฐ€ ๊ฐ€๋Šฅํ•œ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค. ๋”ฐ๋ผ์„œ, ๋ณธ ์—ฐ๊ตฌ์—์„œ ๊ฐœ๋ฐœํ•œ ์ดˆ๋ถ„๊ด‘์˜์ƒ ๊ธฐ๋ฐ˜ ๋ถ€์œ ์‚ฌ ๊ณ„์ธก ๊ธฐ์ˆ ์„ ํ†ตํ•ด ์ถ”ํ›„ ํ•˜์ฒœ ์กฐ์‚ฌ ๋ฐ ๊ด€๋ฆฌ ์‹ค๋ฌด์˜ ์ •ํ™•์„ฑ ๋ฐ ํšจ์œจ์„ฑ์„ ํฌ๊ฒŒ ์ฆ์ง„ํ•  ์ˆ˜ ์žˆ์„ ๊ฒƒ์œผ๋กœ ๊ธฐ๋Œ€๋œ๋‹ค.The conventional measurement method of suspended sediment concentration (SSC) in the riverine system is labor-intensive and time-consuming since it has been conducted using the sampling-based direct measurement method. For this reason, it is challenging to collect high-resolution datasets of SSC in rivers. In order to overcome this limitation, remote sensing-based techniques using multi- or hyper-spectral images from satellites or UAVs have been recently carried out to obtain high-resolution SSC distributions in water environments. However, suspended sediment in rivers is more dynamic and spatially heterogeneous than those in other fields. Moreover, the sediment and streambed properties have strong regional characteristics depending on the river type; thus, only models suitable for a specific period and region have been developed owing to the increased spectral variability of the water arising from various types of suspended matter in the water and the heterogeneous streambed properties. Therefore, to overcome the limitations of the existing monitoring system, this study proposed a robust hyperspectral imagery-based SSC measurement method, termed cluster-based machine learning regression with optical variability (CMR-OV). This method dealt with the spectral variability problem by combining hyperspectral clustering and machine learning regression with the Gaussian mixture model (GMM) and Random forest (RF) regression. The hyperspectral clustering separated the complex dataset into several homogeneous datasets according to spectral characteristics. Then, the machine learning regressors corresponding to clustered datasets were built to construct the relationship between the hyperspectral spectrum and SSC. The development and validation of the proposed method were carried out through the following processes: 1) analysis of confounding factors in the spectral variability through experimental studies, 2) selection of an optimal regression model and validation of hyperspectral clustering, and 3) evaluation of field applicability. In the experimental studies, the intrinsic hyperspectral spectra of suspended sediment were collected in a completely mixed state after removing the bottom reflection using a horizontal rotating cylinder. Then, hyperspectral data on various sediment properties (particle size and mineral contents) and river bed properties (sand and vegetation) were collected from sediment tracer experiments in field-scale open channels under different hydraulic conditions and compared with intrinsic hyperspectral spectra. Consequently, the change of the hyperspectral spectrum was different according to the sediment type and particle size distribution. In addition, under the shallow water depth condition of 1 m or less, the shape of the hyperspectral spectrum changed significantly depending on the bed type due to the bottom reflectance. The bottom reflectance substantially affected the hyperspectral spectrum even when the high SSC was distributed. As a result of combining the GMM and RF regression with building a relationship between the SSC and hyperspectral data reflecting the spectral variability, the accuracy was substantially improved compared to the other methods. In particular, even when nonlinearity is considered based on the existing optimal band ratio analysis (OBRA) method, spectral variability could not be reflected due to the limitation of considering only a narrow wavelength range. On the other hand, CMR-OV showed high accuracy while considering a wide range of wavelengths with clusters having distinct spectral characteristics. Finally, the CMR-OV was applied to the straight and meandering reaches of the Hwang River and the confluence of the Nakdong and Hwang Rivers in South Korea to assess field applicability. There was a remarkable improvement in the accuracy and precision of SSC mapping under various river conditions compared to the existing models, and CMR-OV showed robust performance even with non-calibrated datasets. At the river confluence, the mixing pattern between the main river and tributary was apparently retrieved from CMR-OV under optically complex conditions. Compared to the non-clustered model, hyperspectral clustering played a primary role in improving the performance by separating the water bodies originating from both rivers. It was also possible to quantitatively evaluate the complicated mixing pattern in detail compared to the existing point measurement. Therefore, it is expected that the accuracy and efficiency of river investigation will be significantly improved through the SSC measurement method presented in this study.Abstract of dissertation i List of figures ix List of tables xvii List of abbreviations xix List of symbols xxii 1. Introduction 1 2. Theoretical research 13 2.1.1 Pre-processing of hyperspectral image (HSI) 19 2.1.2 Optical characteristics of suspended sediment in rivers 28 2.1.2.1 Theory of solar radiation transfer in rivers 28 2.1.2.2 Heterogeneity of sediment properties 33 2.1.2.3 Effects of bottom reflectance 38 2.1.2.4 Vertical distribution of suspended sediment 41 2.1.3 Retrieval of suspended sediment from remote sensing data 46 2.1.3.1 Remote sensing-based regression approach 46 2.1.3.2 Clustering of remote sensing data 52 2.2 Mapping of suspended sediment concentration in rivers 56 2.2.1 Traditional method for spatial measurement 56 2.2.2 Spatial measurement at river confluences 57 2.2.2.1 Dynamics of flow and mixing at river confluences 57 2.2.2.2 Field experiments in river confluences 64 3. Experimental studies 68 3.1 Experimental cases 68 3.2 Laboratory experiment 74 3.2.1 Experimental setup 74 3.2.2 Experimental method 78 3.3 Field-scale experiments in River Experiment Center 83 3.3.1 Experiments in the straight channel 83 3.3.2 Experiments in the meandering channel 96 3.4 Field survey 116 3.4.1 Study area and field measurement 116 3.4.2 Hydraulic and sediment data in rivers with simple geometry 122 3.4.3 Hydraulic and sediment data in river confluences 126 3.5 Analysis of hyperspectral data of suspended sediment 141 3.5.1 Hyperspectral data of laboratory experiment 142 3.5.2 Hyperspectral data of field-scale experiments 146 3.5.2.1 Effect of bottom reflectance 146 3.5.2.2 Principal component analysis of the effect of suspended sediment properties 154 4. Development of suspended sediment concentration estimator using UAV-based hyperspectral imagery 164 4.1 Outline of Cluster-based Machine learning Regression with Optical Variability (CMR-OV) 164 4.2 Pre-processing of hyperspectral images 168 4.3 Regression models and clustering technique 173 4.3.1 Index-based regression models 173 4.3.2 Machine learning regression models 175 4.3.3 Relevant band selection 183 4.3.4 Gaussian mixture model for clustering 185 4.3.5 Performance criteria 188 4.4 Model development and evaluation 189 4.4.1 Comparison of regression models 189 4.4.1.1 OBRA-based explicit models 189 4.4.1.2 Machine learning-based implicit models 194 4.4.2 Assessment of hyperspectral clustering 200 4.4.3 Spatio-temporal SSCV mapping using CMR-OV 215 5. Evaluation of field applicability of CMR-OV 225 5.1 Outline of field applicability test 225 5.2 Cross-applicability validation of CMR-OV 227 5.3 Assessment of field applicability in rivers with simple geometry 234 5.4 Assessment of field applicability in river confluences 241 5.4.1 Classification of river regions using hyperspectral clustering 241 5.4.2 Retrievals of SSCV map 258 5.4.3 Mixing pattern extraction from SSCv map 271 6. Conclusions and future study 274 6.1 Conclusions 274 6.2 Future directions 278 Reference 280 Appendix 308 Appendix A. Breakthrough curve (BTC) analysis 308 Appendix B. Experimental data 310 Appendix B. 1. BTCs of in-situ measured SSC from field-scale experiments 310 Appendix B. 2. Dataset of spectra from hyperspectral images and corresponding SSC in rivers 330 Appendix C. CMR-OV code 331 ๊ตญ๋ฌธ์ดˆ๋ก 337๋ฐ•

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