Earth observation guideKinds of data

Hyperspectral imaging

Hundreds of narrow bands give every pixel a full spectrum, enough to tell crops, pigments and minerals apart.

The basics

Where a multispectral sensor reports a few broad colours, a hyperspectral one reports hundreds of narrow ones, so every pixel carries a complete spectrum, much as every fingerprint carries a complete pattern. A multispectral image can say that a field is green. A hyperspectral image can often say which crop it is, whether it is short of nitrogen, or which mineral is in an exposed rock, because many materials differ only in thin absorption features that broad bands average away. The price is data volume and signal. Narrow bands gather less light, so the pixels are normally larger and each image covers less ground.

Why it matters

Hyperspectral data answers questions that broad colours cannot, such as which crop is in a field, whether it is short of nitrogen, or which mineral is exposed in a rock. The data are large and the pixels are usually coarser, so it pays when the question depends on fine detail in the spectrum rather than fine detail in the picture.

Wavelengtha narrow dipBlack: the true spectrumOrange: four broad bands average the dip awayBlue: many narrow bands catch it
A narrow dip in a spectrum is the fingerprint of a material. Four broad bands average it away, and many narrow bands catch it.

In depth

The data are an image cube with two spatial axes and one spectral axis, drawn in Figure 1. Imaging spectrometry, described in an influential 1985 paper, records images in many contiguous bands so that a spectrum can be read for every pixel [1]. Narrow absorption features, which are diagnostic of molecular bonds in minerals, pigments and water, are resolved only when the resolving power of equation 2 on the four resolutions page is high enough, in practice with bands of the order of 10 nanometres wide [1, 2].

Image cube

Across trackAlong trackWavelength

Spectrum of the outlined pixel

WavelengthReflectancenarrowabsorptionnarrowabsorption
Figure 1. A hyperspectral image cube. Two axes are position on the ground and the third is wavelength. Reading along the third axis at one pixel gives that pixel's spectrum.

A pixel often covers more than one material, so its spectrum is a blend. The common model treats the measured spectrum r\mathbf{r} as a linear mixture of KK pure spectra, the endmembers mk\mathbf{m}_k, weighted by their fractional abundances aka_k, plus noise ε\boldsymbol{\varepsilon} [3, 4].

r=∑k=1Kak mk+ε,ak≥0,∑k=1Kak=1\mathbf{r} = \sum_{k=1}^{K} a_k\,\mathbf{m}_k + \boldsymbol{\varepsilon},\qquad a_k \ge 0,\quad \sum_{k=1}^{K} a_k = 1
(1)

where r\mathbf{r} is the measured spectrum of the pixel, a vector of reflectances with one entry per band and no unit; KK is the number of endmembers; mk\mathbf{m}_k is the spectrum of endmember kk, in the same form as r\mathbf{r}; aka_k is its fractional abundance, the share of the pixel it covers, between 0 and 1; and ε\boldsymbol{\varepsilon} is the residual noise, one entry per band. The two conditions on the right keep every abundance non-negative and make the abundances sum to one.

Unmixing estimates the endmembers and the abundances from the image itself or from a library of laboratory spectra, and returns maps of how much of each material every pixel contains. The model is a first approximation, because light that bounces between different materials mixes non-linearly, and the review literature treats those cases separately [4]. The data volume grows with the product of rows, columns, bands and bit depth, so a hyperspectral scene is far larger than a multispectral scene of the same size, and analysing it usually starts by reducing the number of dimensions [2].

References

  1. Goetz, A. F. H., Vane, G., Solomon, J. E. and Rock, B. N. (1985) Imaging Spectrometry for Earth Remote Sensing. Science, 228(4704), 1147-1153. https://doi.org/10.1126/science.228.4704.1147
  2. Bioucas-Dias, J. M., Plaza, A., Camps-Valls, G. et al. (2013) Hyperspectral Remote Sensing Data Analysis and Future Challenges. IEEE Geoscience and Remote Sensing Magazine, 1(2), 6-36. https://doi.org/10.1109/MGRS.2013.2244672
  3. Keshava, N. and Mustard, J. (2002) Spectral unmixing. IEEE Signal Processing Magazine, 19(1), 44-57. https://doi.org/10.1109/79.974727
  4. Bioucas-Dias, J. M., Plaza, A., Dobigeon, N. et al. (2012) Hyperspectral Unmixing Overview: Geometrical, Statistical, and Sparse Regression-Based Approaches. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 5(2), 354-379. https://doi.org/10.1109/JSTARS.2012.2194696