| Literature DB >> 22291550 |
Elia Quirós1, Angel M Felicísimo, Aurora Cuartero.
Abstract
This work proposes a new method to classify multi-spectral satellite images based on multivariate adaptive regression splines (MARS) and compares this classification system with the more common parallelepiped and maximum likelihood (ML) methods. We apply the classification methods to the land cover classification of a test zone located in southwestern Spain. The basis of the MARS method and its associated procedures are explained in detail, and the area under the ROC curve (AUC) is compared for the three methods. The results show that the MARS method provides better results than the parallelepiped method in all cases, and it provides better results than the maximum likelihood method in 13 cases out of 17. These results demonstrate that the MARS method can be used in isolation or in combination with other methods to improve the accuracy of soil cover classification. The improvement is statistically significant according to the Wilcoxon signed rank test.Entities:
Keywords: TERRA-ASTER image; area under the ROC curve (AUC); multi-spectral classification; multivariate adaptive regression splines (MARS)
Year: 2009 PMID: 22291550 PMCID: PMC3260627 DOI: 10.3390/s91109011
Source DB: PubMed Journal: Sensors (Basel) ISSN: 1424-8220 Impact factor: 3.576
Figure 1.Location of the Extremadura test area in southeastern Spain.
Main characteristics of the ASTER sensor systems.
| 1 | 0.52–0.60 | 15 | 8 bits | |
| 2 | 0.63–0.69 | |||
| 3N | 0.78–0.86 | |||
| 3B | 0.78–0.86 | |||
| 4 | 1.60–1.70 | 30 | 8 bits | |
| 5 | 2.145–2.185 | |||
| 6 | 2.185–2.225 | |||
| 7 | 2.235–2.285 | |||
| 8 | 2.295–2.365 | |||
| 9 | 2.360–2.430 | |||
| 10 | 8.125–8.475 | 90 | 12 bits | |
| 11 | 8.475–8.825 | |||
| 12 | 8.925–9.275 | |||
| 13 | 10.25–10.95 | |||
| 14 | 10.95–11.65 | |||
Figure 2.Extremadura forest map (EFM).
Forest categories of area under study.
| Water | 49.6 | 1.3% | |
| Mixed silicicolous scrubland | 47.5 | 1.2% | |
| Agricultural land | 2,422.9 | 61.4% | |
| Mixed riparian forest | 23.5 | 0.6% | |
| Dense seasonal pasture | 135.6 | 3.4% | |
| Open formation | 8.7 | 0.2% | |
| Dense formation | 8.6 | 0.2% | |
| Boulders | 2.1 | 0.1% | |
| Rocky desert | 42.2 | 1.1% | |
| 109.2 | 2.8% | ||
| 22.0 | 0.6% | ||
| 10.4 | 0.3% | ||
| 194.7 | 4.9% | ||
| 10.1 | 0.3% | ||
| 53.5 | 1.4% | ||
| 786.0 | 19.9% | ||
| 1.4 | 0.0% | ||
| 17.8 | 0.5% |
Figure 3.Re-sampling example for TIR bands.
Regions of interest (ROI) used in the classifications.
| Water | 49.6 | 33.3 | 67.19% | |
| Mixed silicicolous scrubland | 47.5 | 28.4 | 59.73% | |
| Mixed riparian forest | 23.5 | 11.6 | 49.18% | |
| Dense seasonal pasture | 135.6 | 52.2 | 38.47% | |
| Open formation | 8.7 | 2.8 | 31.89% | |
| Dense formation | 8.6 | 5.6 | 64.68% | |
| Boulders | 2.1 | 0.8 | 36.22% | |
| Rocky desert | 42.2 | 23.5 | 55.82% | |
| 109.2 | 69.6 | 63.69% | ||
| 22.0 | 10.6 | 48.33% | ||
| 10.4 | 8.1 | 78.18% | ||
| 194.7 | 140.6 | 72.25% | ||
| 10.1 | 5.7 | 55.93% | ||
| 53.5 | 26.0 | 48.48% | ||
| 786.0 | 544.2 | 69.23% | ||
| 1.4 | 0.7 | 52.24% | ||
| 17.8 | 12.1 | 67.92% |
Figure 4.Work flow for the MARS process classification.
Figure 5.Fragment of the ROI ASCII export file.
Figure 6.(a) ML classification map, (b) Parallelepiped classification map, (c) MARS classification map.
Area under the ROC curve (AUC) statistics.
| AUC | AUC | AUC | |||
|---|---|---|---|---|---|
| 999 | Water | 33.3 | 0.945 | 0.793 | |
| 547 | Mixed silicicolous scrubland | 28.4 | 0.813 | 0.754 | |
| 507 | Mixed riparian forest | 11.6 | 0.814 | ||
| 458 | Dense seasonal pasture | 52.2 | 0.714 | 0.687 | |
| 454 | Open formation | 2.8 | 0.929 | 0.954 | |
| 453 | Dense formation | 5.6 | 0.961 | 0.971 | |
| 337 | Boulders | 0.8 | 0.963 | 0.791 | |
| 329 | Rocky desert | 23.5 | 0.884 | 0.701 | |
| 309 | 69.6 | 0.699 | 0.670 | ||
| 303 | 10.6 | 0.826 | 0.728 | ||
| 221 | 8.1 | 0.898 | 0.657 | ||
| 62 | 140.6 | 0.856 | 0.834 | ||
| 61 | 5.7 | 0.939 | 0.870 | ||
| 46 | 26.0 | 0.841 | 0.766 | ||
| 45 | 544.2 | 0.577 | 0.600 | ||
| 26 | 0.7 | 0.957 | 0.903 | ||
| 23 | 12.1 | 0.952 | 0.924 | ||