MULTI-SOURCE IMAGE CLASSIFICATION

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MULTI-SOURCE IMAGE CLASSIFICATION Hillary Tribby, James Kroll, Daniel Unger, I-Kuai Hung, Hans Williams Corresponding Author: Daniel Unger (unger@sfasu.edu Arthur Temple College of Forestry and Agriculture Stephen F. Austin State University Nacogdoches, Teas 7596 ABSTRACT Since multi-source image classifications have the ability to eceed single source processes, such as traditional unsupervised classification methods, this paper will present the integration of four types of data: Lidar, elevation, multispectral and thermal. Using multi-source data and maimum lielihood classification methodology, as well as all possible permutations of data types, this paper will discuss ways to increase accuracy assessments of forested areas in east Teas and find the best combination of data sources. Key Words: Land Cover, Accuracy, Lidar, Terrain, Canopy Elevation

INTRODUCTION Land cover classification is a method to demarcate the landscape for the purpose of determining the dominant cover and monitoring the changes in land cover over time. Numerous schemes have been developed for use with land cover and land use classifications, but early in satellite remote sensing Anderson and his colleagues (976 developed and published a rubric by which to define dominant cover. Although important information can be etracted from a single satellite image, the inclusion of multiple sources and types of data may be best for analysis. This project assessed the utility of combining terrain and canopy elevation values derived from lidar (light detection and ranging with traditional multispectral and thermal satellite imagery to increase the accuracy of land cover classifications. OBJECTIVES Since remote sensing technologies are constantly changing incorporating data into any given remote sensing project has become more comple. This project evaluated and recommends which data sources should be integrated into image classifications in order to produce the most accurate land cover map. These results will aid decision-maers in determining what data will be included and provide the most accurate information possible. Our primary objective was to evaluate the accuracy of single and multi-source image land cover classifications based on the hypotheses that: ( the addition of lidar derived components will

increase land cover map accuracy; and, ( the addition of thermal data will increase land cover map accuracy. METHODS Using the inherent maimum lielihood (ML algorithm in ENVI (Environment for Visualizing Images, the Principal Components of a Landsat ETM+ scene were classified according to the Anderson Land Use Land Cover System (Table ; Figure. Since lidar data were collected as vector data, it must be transformed into a continuous format. Moving windows that capture the highest elevation point for a given area were used to generate a surface elevation Table. Eigenvalues associated with each of the Landsat ETM+ Principal Component bands. Band Eigenvalue Percent Variability 877.5889 89.78 7.7970 7.34 3 0.604. 4 4.5 0.43 5.8339 0.9 6.4560 0.5

Landsat ETM+ Imagery Image Acquisition Radiometric Correction Geometric Correction Training Site Selection Thermal OR Principal Component Analysis Digital Terrain Model OR Maimum Lielihood Classification Canopy Height Model Accuracy Assessment and Z Statistic Pairwise Comparison of Maps,, 3, 4, and 5 Including multiple sources of data for integration into a classification requires data normalization and stacing. Figure. Schematic of image classification methodology and accuracy assessment.

model (Popescu, Wynne & Nelson 00. The digital terrain model was created using the second lidar return (Woolard & Colby, 00; Lee & Shan, 003; Popescu, 004. The second return represented the laser signal hits that penetrated the canopy and returned from the ground. Using the Geostatistical Analyst etension in ArcGIS 9.0, a digital terrain model was generated using Radial Basis Function. Numerous interpolation techniques were used and the RBF- Multiquadric had the lowest Root Mean Square Error. The terrain model was subtracted from the surface model to generate the Canopy Height Model. The Kˆ statistic is a measure of agreement between the reference data and the classified land cover map and is calculated using the variables in the error matri: Kˆ n i n ii i i i+ i+ + i + i Where is the number of rows, ii is the number of observations in row i and column i, i+ and +i are the marginal totals of row i and column i, and n is the number of observations (Congalton, 99. To determine the Z statistic the variance must be calculated using the Delta method: vâr ( ˆ θ ( θ K ( θ( θ θ θ3 3 ( θ ( θ ( θ 4θ 4 + + 4 n ( θ ( θ

where θ n i ii θ n i i + + i θ 3 n i ii ( i+ + + i and θ n 4 3 i j ij ( +. j+ + i Once variance has been calculated the Z statistic can be calculated: Z Kˆ vâr ( Kˆ The Z statistic informs the researcher whether or not the agreement between the reference data and the land cover map was greater than random chance. Since the Z statistic is standardized and normally distributed, with the null hypothesis that Kˆ is equal to zero and the alternative hypothesis that Kˆ is not equal to zero, if Z Z α/ then the null hypothesis is rejected. Z scores

with a value greater than one standard deviation from the mean or.960 is deemed significant. The Z statistic was also used to determine significant differences between two map accuracies: Z vâr Kˆ ( Kˆ + vâr( Kˆ Kˆ By calculating the Kˆ, variance, and Z statistics for two error matrices, significant differences can be identified (Congalton & Green, 999. RESULTS Of the five land cover maps, all map Z scores were deemed significant, indicating that the classifications were better than random chance (Table. Differences between the maps were not deemed to be significantly different, indicating that the addition of multiple sources of data did not effect the supervised classification of Landsat ETM+ data (Table 3. Although the incorporation of multiple sources did not significantly effect the accuracy assessment, the inclusion of multiple data sources did produced the highest appa statistic. Future studies should assess the accuracy of higher spatial resolution image classifications that include similar data.

Table. Land cover map results showing significant Z scores. Land Cover Map Overall Kappa Variance Z Score Accuracy % Coefficient Principal Component Analysis 65.63 0.586 0.009 6.84 (PCA PCA and Canopy Height Model 64.3 0.5664 0.00363 9.400 (CHM PCA and Digital Terrain Model 69.30 0.683 0.003.6 (DTM PCA and Thermal Data 67.6 0.6050 0.00074 8.456 PCA, CHM, DTM, and Thermal 70.4 0.6384 0.00430 9.73

Table 3. Kappa analysis results describing the pairwise comparisons of error matrices. Map Map Z Score PCA PCA and CHM 0.67 PCA PCA and DTM 0.705 PCA PCA and Thermal 0.4793 PCA PCA, CHM, DTM, and Thermal 0.7577 PCA and CHM PCA and DTM 0.759 PCA and CHM PCA and Thermal 0.565 PCA and CHM PCA, CHM, DTM, and Thermal 0.8070 PCA and DTM PCA and Thermal 0.360 PCA and DTM PCA, CHM, DTM, and Thermal 0.76 PCA and Thermal PCA, CHM, DTM, and Thermal 0.4554

REFERENCES Anderson, J. R., Hardy, E. E., Roach, J. T. & Witmer, R. E. (976. A land use and land cover classification system for use with remote sensor data (Geological survey professional paper 964. Washington, DC: U.S. Government Printing Office. Congalton, R. G. (99. A review of assessing the accuracy of classifications of remotely sensed data. Rem. Sens. Env., 37, 35-46. Congalton, R.G. & Green, K. (999. Assessing the accuracy of remotely sensed data: Principles and practices. Boca Raton, FL: Lewis Pubs. Lee, D. S. & Shan, J. (003. Combining lidar elevation data and IKONOS multispectral imagery for coastal classification mapping. Marine Geodesy, 6, 7-7. Popescu, S. C., Wynne, R. H. & Nelson, R. F. (00. Estimating plot-level tree heights with lidar: local filtering with a canopy-height based variable window size. Comp. & Electron. Ag., 37, 7-95. Popescu, S. C. (004. Seeing the trees in the forest: Using small-footprint airborne lidar measurements. PhD. dissertation, Virginia Polytechnic Institute and State University, Blacsburg, VA. 55 p.

Woolard, J. W. & Colby, J. D. (00. Spatial characterization, resolution, and volumetric change of coastal dunes using airborne LIDAR: Cape Hatteras, North Carolina. Geomorphology, 48, 69-87.