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  • Session 1
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  • ACRS 1999


    Hyper Spectral Image Processing
    Spectral Mixture Analysis of Hyperspectral Data

    5. Spectral Unmixing Analysis
    The spectral mixture of only two materials can be solved with the data of each band. According to Eq.(1), the ith spectral band is mixed as:

    DNi=(Ri1*F1+Ri2*Ei     (4)

    Combining Eq.(4) with the constraint expressed in Eq.(2), one can solve F1 as following,


    Let F1 be the fraction coefficient of the vegetation foreground, then the solutions of F1 in each band for all the sample data in the data set can be shown graphically in figure 9. Unstable solutions are obtained when the spectral band has almost the same reflectance, i.e., Ri1»Ri2. Removing the unstable solutions, the variation of the solutions can be clearly shown in figure 10. Linearity of spectral mixing can be validated in most of the bands except the absorption bands. One can remark that while most of the spectral bands provide positive effects, there are some spectral bands may contaminate the solution.


    Figure 9: The solution of F1.



    Figure 10: The solution of F1 after removing unstable ones.


    For each sample data, the fraction coefficients were also calculated by using CLS. The results are graphically shown in figure 11. As mentioned above, the spectral bands do not have equal contributions to the solution of spectral unmixing. In addition, as shown in figure 7, the bands do not contain equal noise either. A weighted least squares (WLS) computation is, therefore, proposed to improve the solution. The discrepancy of band reflectance between endmembers and the noise level of measurements can be the reference to adjust the weights. The final results are graphically shown in figure 11.


    Figure 11: CLS solutions.



    Figure 12: WLS solutions.


    Conclusding Remarks
    A pixel-covered area is commonly recognized as a square. However, the shape of the GIFOV is actually not a square. This situation causes a problem that the fraction coefficients derived from spectral unmixing do not correspond with the proportions of the þ endmembers distributed within a square pixel. A variation of a spatial distribution of objects within a pixel would result in a large difference.

    Due to the differences of the discrepancy of band reflectance between endmembers and the noise level of measurements, the spectral bands do not have equal contributions to the solution of spectral unmixing. A weighted least squares (WLS) computation is proved to be effective for improving the solution of spectral unmixing.

    Acknowledgements
    This research project was sponsored by the National Science Council of Republic of China under the grants of NSC88-2211-E006-051.

    References
    • Adams, J.B., M.O. Smith, and P.E. Johnson, 1986. Spectral mixture modeling: A new analysis of rock and soil types at the Viking Lander 1 site. Journal of Geophysical Research, vol. 91(B8), pp. 8090-8112.
    • Boardman, J.W., 1994. Geometric mixture analysis of imaging spectrometry data. In: Geoscience and Remote Sensing Symposium, IGARSS ’94, Surface and atmospheric remote sensing: technologies, data analysis and interpretation, vol. 4, pp. 2369-2371.
    • Goetz, A.F.H., G. Vane, J.E. Solomon and B.N. Rock, 1985. Imaging spectrometry for Earth remote sensing. Science, vol. 228, pp. 1147-1153.
    • Geophysical & Environmental Research Corp., 1999. GER 1500 Spectroradiometer user manual, Release 2.4.
    • Horwitz, H.M., R.F. Nalepka, P.D. Hyde and J.P. Morgenstern, 1971. Estimating the proportions of objects within a single resolution element of a multispectral scanner. In: Proceedings of the 7 th International Symposium on Remote Sensing of Environment, Ann Arbor, Michigan, pp. 1307-1320.
    • Shimabukuro, Y.E. and J.A. Smith, 1991. The least-squares mixing models to generate fraction images derived from remote sensing multispectral data. IEEE Transaction on Geoscience and Remote Sensing, vol. 29(1), pp. 16-20.
    • Wu, H.-H.P. and R.A. Schowengerdt, 1993. Improved fraction image estimation using image restoration. IEEE Transaction on Geoscience and Remote Sensing, vol.31(4), pp. 771-778.
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