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Volcanic ash cloud detection from MODIS image based on CPIWS method

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Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Volcanic ash cloud detection has been a difficult problem in moderate-resolution imaging spectroradiometer (MODIS) multispectral remote sensing application. Principal component analysis (PCA) and independent component analysis (ICA) are effective feature extraction methods based on second-order and higher order statistical analysis, and the support vector machine (SVM) can realize the nonlinear classification in low-dimensional space. Based on the characteristics of MODIS multispectral remote sensing image, via presenting a new volcanic ash cloud detection method, named combined PCA-ICA-weighted and SVM (CPIWS), the current study tested the real volcanic ash cloud detection cases, i.e., Sangeang Api volcanic ash cloud of 30 May 2014. Our experiments suggest that the overall accuracy and Kappa coefficient of the proposed CPIWS method reach 87.20 and 0.7958%, respectively, under certain conditions with the suitable weighted values; this has certain feasibility and practical significance.
Czasopismo
Rocznik
Strony
151--163
Opis fizyczny
Bibliogr. 36 poz.
Twórcy
autor
  • School of Computer Engineering and Science, Shanghai University, Shanghai, China
autor
  • School of Computer Engineering and Science, Shanghai University, Shanghai, China
autor
  • School of Computer Engineering and Science, Shanghai University, Shanghai, China
autor
  • Earthquake Administration of Shanghai Municipality, Shanghai, China
autor
  • School of Computer Engineering and Science, Shanghai University, Shanghai, China
Bibliografia
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  • 7. Ellrod GP (2004) Impact on volcanic ash detection caused by the loss of the 12.0 µm “Split Window” band on GOES imagers. J Volcanol Geotherm Res 135(1–2):91–103. doi:10.1016/j.jvolgeores.2003.12.009
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  • 10. Hillger DW, Clark J (2002a) Principal component image analysis of MODIS for volcanic ash. Part I: most important bands and implications for future GOES imagers. J Appl Meteorol 41(1):985–1001. doi:10.1175/1520-0450(2002)041<0985:PCIAOM>2.0.CO;2
  • 11. Hillger DW, Clark J (2002b) Principal component image analysis of MODIS for volcanic ash. Part II: simulation of current GOES and GOES-M imagers. J Appl Meteorol 41(10):1003–1010. doi:10.1175/1520-0450(2002)041<1003:PCIAOM>2.0.CO;2
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  • 15. Li CF, Yin JY (2013) Variational Bayesian independent component analysis-support vector machine for remote sensing classification. Comput Electr Eng 39(3):717–726. doi:10.1016/j.compeleceng.2012.10.004
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  • 23. Prata AJ, Prata AT (2012) Eyjafjallajökull volcanic ash concentrations determined using spin enhanced visible and infrared imager measurements. J Geophys Res 117(D20):2156–2202. doi:10.1029/2011JD016800
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  • 28. Spinetti C, Barsotti S, Neri A, Buongiorno MF, Doumaz F, Nannipieri L (2013) Investigation of the complex dynamics and structure of the 2010 Eyjafjallajökull volcanic ash cloud using multispectral images and numerical simulations. J Geophys Res 118(10):4729–4747. doi:10.1002/jgrd.50328
  • 29. Wang XM, Zeng SG, Xia DS (2006) Remote sensing image classification based on a loose modified fast ICA algorithm. J. Comput Res Dev 43(4):708–715 (in Chinese)
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  • 33. Western LM, Watson MI, Francis PN (2015) Uncertainty in two-channel infrared remote sensing retrievals of a well-characterised volcanic ash cloud. Bull Volcanol 77(8):1–12. doi:10.1007/s00445-015-0950-y
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  • 36. Zhao Y, Liang Y, Ma BJ, Li YS, Wu XJ (2014) Identification of Icelandic volcanic ash cloud based on FY-3A remote sensing data. Acta Petrol Sin 30(12):3693–3700
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-3a18b8ce-01b8-4dbd-a89b-ed2faae6d615
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