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PE&RS June 2001VOLUME 67, NUMBER 6PHOTOGRAMMETRIC ENGINEERING & REMOTE SENSING JOURNAL OF THE AMERICAN SOCIETY FOR PHOTOGRAMMETRY AND REMOTE SENSING Highlight Article Introduction In late 2000, the U.S.Geological Survey (USGS) EROS Data Center (EDC) completed the circa 1992 National Land Cover Data set (NLCD). The NLCD, derived from early 1990s Landsat Thematic Mapper (TM) imagery and other sources of digital data, represents an intermediate-scale national land cover data set. The resolution of this data set lends itself to many regional to national scale investigations, including analyses of water quality, ecosystem health, wildlife habitat, land cover assessments and other land management issues. The purpose of this paper is to describe the characteristics and uses of this data set. One of the goals in the development of the NLCD was to generate a reasonably consistent and seamless 30 meter product for the conterminous United States. The methodology employed to develop the NLCD is analogous to the database approach originally envisioned by Lauer (1986). The early developmental stages of the data set have been described elsewhere (Vogelmann et al. 1998a and b). In addition to the spectral information provided by the TM, ancillary spatial data were used to improve classification results, when appropriate. The NLCD may be considered as a replacement/update to the intermediate-scale Land Use and Land Cover data set (USGS, 1990) developed in the 1970s and early 1980s. Materials & Methods Landsat TM data used to develop the NLCD were terrain-corrected using 3-arc-second digital terrain elevation data (DTED; U.S. Geological Survey, 1993). The TM data were geo-registered to the Albers Equal Area projection grid using ground control points, resulting in a root mean square registration error of less than one pixel (30 m). Two or more TM data sets for each path/row, representing different seasons, were used to generate the NLCD product. Two or more TM scenes representing different times of the growing season (e.g. leaf-on and leaf-off) generally improves upon the quality of land cover information that can be derived as compared to analysis of a single scene. Ancillary Spatial Data. In addition to TM data, a variety of other intermediate-scale spatial data were used to help develop the NLCD; these included Digital Terrain Elevation Data (DTED) and derivative DTED products (slope, aspect, shaded relief), population density data at the census block level (Bureau of the Census, 1991 a and b; 1992), Land Use and Land Cover data (USGS 1990), and digital National Wetlands Inventory data (NWI; Fish and Wildlife Service, 1996). Other data sets were used to a lesser extent, and included available water capacity and organic carbon (0-40 cm depth) data derived from the State Soil Geographic (STATSGO) Data Base (U.S. Department of Agriculture, 1994), and land cover information derived from various state or national programs. Land cover data from the USGS Biological Resource Division Gap Analysis Program (Scott et al., 1996) were used when available.
General Classification Methods. Mosaics of leaf-on (i.e. summer) and leaf-off (i.e. spring) imagery were generated for each of 31 regional units (based on political administrative units, contiguity of Landsat scenes and data volume) covering the conterminous United States (Figure 1). Each unit was classified separately using one of several methods. In most cases the general thematic approach was to designate either mosaic (leaf-on or the leaf-off) as the “baseline” data set, and to use that spectral information as the primary source of information from which to derive the classification product. The decision as to which mosaic to use was based on a subjective evaluation of which appeared to be the “best” mosaic in terms of overall data quality and information content. Leaf-off mosaics were chosen as baseline data sets more frequently than leaf-on mosaics. Ancillary spatial information, including spectral data from the image mosaic representing the other season, was used to refine or aid in the labeling process. After development of a first order classification product, a series of recoding operations were performed to fix obvious misclassifications and to further refine the classification.
During the initial stages of the project, the primary steps for generating the NLCD classification product were: (1) Cluster the baseline mosaic using unsupervised classification. (2) Interpret and label clusters using aerial photographs. (3) Resolve confused clusters by constructing logical or threshold models that utilize appropriate ancillary data. (4) Develop and incorporate information from onscreen digitizing (e.g. quarries, transitional bare areas). As the project progressed, some classification teams individualized the approach on a case-by-case basis. More in-depth methodology for this process has been described elsewhere (Vogelmann et al., 1998 b). Modifications were based upon data quality issues, characteristics of the region being analyzed, and familiarity with other approaches that would facilitate and/or more readily automate the classification process. In the case of multiscene mosaics, spectral clusters developed from unsupervised clustering can be very complex, and a single cluster may represent many different types of land cover. In these cases, splitting the clusters into meaningful land cover units via modeling based on spectral and ancillary data can be quite difficult. Not only are the thresholds used to make land cover separation important, but the order of threshold implementation can also have substantial effects on the land cover estimates. Determining the optimal set of thresholds and the optimal order of implementation for complex “confused clusters” can be time consuming and difficult. One approach taken was to use decision trees to facilitate the modeling process. Decision trees derive objective, efficient, and ordered thresholds using non-parametric techniques (Friedl and Brodley 1997 and Hansen et al. 1996). Decision trees have been successfully used to derive land cover (Friedl and Brodley 1997) and to identify important data layers or spectral bands (Hansen et al. 1996; Prince and Steininger 1999). For decision tree training, the image clusters were included only as an ancillary data set. Multiple decision trees trained with different data layer set combinations and/or decision tree parameter options produced multiple land cover maps. Majority land cover from the multiple land cover maps for each pixel was used as a preliminary land cover map. Decision trees were also used to help define classification “rules” in an expert system classifier (ERDAS 1998). The expert system allowed quick identification of which rules affected which pixels and quick modification of either rules or rule confidence levels. While it was apparent that the decision trees maintained a high degree of detail in the land cover products, the need for visual inspection and “heads up” on-screen corrections of the preliminary land cover persisted. In all cases, results were scrutinized in order to ensure comparability of land cover data among regions and to correct obvious classification errors. Edge-matching of adjacent mosaics was then performed to yield a reasonably seamless national-scale product. This was a major task due to seasonal and interpretation differences that invariably resulted in thematic seam lines at the boundaries of the mosaics. As the mosaics were finally pieced together, individual states were extracted using boundaries defined by the 1:100,000 scale Digital Line Graph series. The state files were designated “preliminary” and made available to the user community for review and feedback. Initially, the state land cover files were available to users who contacted the USGS/EDC Land Cover Applications Center to gain access to the data. The intent was to ensure that users understood the “preliminary” nature of the data, as well as its limitations, and to register the user and solicit feedback regarding the utility of the data and any problems that were identified. As feedback was received, it was reviewed and a determination made if an update was required. In many cases, updates were made, and the registered users were apprised of the changes. Accuracy Assessment Methods. When all the states comprising a Federal Region were finalized, the accuracy assessment (AA) phase was initiated. At this time, the AA for regions 1-4 (Figure 2) are complete, regions 5,7, and 10 are underway, and the remainder are in the planning stages. The accuracy assessment was based on interpretations of 1990 vintage aerial photographs acquired by the National Aerial Photography Program (NAPP). The accuracy assessment of NLCD was achieved with The sampling design incorporated three levels of stratification and a two-stage cluster sampling protocol (Stehman et al., 2000). Each Federal region constituted a stratum and was sampled independently. Within each mapping region, geographic strata were created using 15 x 15 or 30 x 30 minute grid cells, depending on the size of the region. Primary sampling units (PSU) defined by non-overlapping, interior regions of NAPP were delineated within these strata. A single PSU was randomly selected from each grid cell, with all PSU’s having an equal probability of being selected. All pixels selected within the first-stage PSU’s were stratified by mapped landcover class, and a simple random sample of approximately 80 to 100 pixels was selected for each land-cover class. To obtain reference land cover class labels, each sample (pixel) was identified on a NAPP aerial photograph. A suite of attributes was collected by photointerpreters, including primary and alternate landcover label (an alternate reference label only provided when appropriate), landcover heterogeneity in the vicinity of the sample unit, and a confidence rating of the photointerpreted landcover label. For a more detailed discussion on the reference data collection and evaluation, refer to Yang et al. (2000) and Zhu et al. (2000). For each mapping region, stratified sampling formulas were applied to estimate the error matrix cell proportions (Stehman and Czaplewski, 1998), and subsequently, the estimates of overall and class-specific user and producer’s accuracy (Story and Congalton, 1986). The use of stratified formulas is important because of sampling methods that have been chosen for the project. Accuracy results were computed through weighting the cell proportions by the proportion of each land cover within a given Federal region. Results and Discussion Land cover for larger scale areas located in Colorado (Figure 4) provide information
regard-ing the level of detail typical of the NLCD, with the image to the right
showing full resolution and detail of the data set.
The equal-area projection of the NLCD allows easy area tabulations of the
various land cover classes. Table 2 shows the percentage land cover estimates
derived from raw pixel count for each of the ten U.S. Federal Regions of the
conterminous U.S. This information is also shown graphically for the conterminous
U.S. in Figure 5. At a glance, it can be seen that the four forest classes
(deciduous, evergreen, mixed forest and woody wetlands) make up a significant
proportion of the NLCD, combining for a total of 32.1% of the area of the conterminous
U.S. Agriculture (pasture/hay, row crops, small grains, fallow and orchards/vineyards)
makes up about 26.4% of the surface area of the conterminous U.S. Urban classes
(low and high intensity residential, commercial/industrial/transportation)
account for 2.0 % of the surface area. Land cover area estimates are also available
for each of the 48 conterminous U.S. states, and may be obtained at: http://edcwww.cr.usgs.gov/programs/lccp/natllandcover.html
based on raw pixel counts from the National Land Cover Data set 1992.
Accuracy. Several rules for defining agreement between map and reference data may be applied given the information collected from NAPP photos and land cover maps. Comparing results across a range ofagreement protocols and data sub-sets permits evaluation of the reference data quality and more thorough investigation of thematic map accuracy (Congalton and Green 1993, Khorram et al. 1999). In this paper, accuracy results are briefly reported for the first four regions in the eastern United States combined (see Figure 2) by defining agreement as a match between the primary or alternate reference land-cover label and the mode land-cover label in a 3x3 pixel window surrounding the sample. Detailed region specific accuracy assessment results completed thus far can be obtained at: http://edcwww.usgs.gov/programs/lccp/accuracy and also from Yang et al. (2001a). Overall accuracy for the eastern United States was 81% for Anderson Level I aggregations (i.e. water, urban, barren land, forest, agricultural land, wetland, rangeland; Anderson et al., 1976), and 60% for all classes (analogous to Anderson Level II classes). As expected, a significant source of disagreement between map and reference land-cover labels (approximately 20%) was between classes that aggregate into a single Anderson Level I class. Other sources of disagreement were between the forest and agricultural classes, which accounted for approximately five percent of the error, and between the forested wetland class (91) and the upland forest classes (41, 42, 43). At Anderson Level II, notably high commission errors occurred for mines (class
32), hay/pasture (class 81) and high intensity residential (class 22). Not
surprisingly, high intensity residential was most often confused with the other
urban classes (low intensity residential and commercial/industrial). Meanwhile,
hay/pasture was most often confused with row crops (class 82). Mines were often
confused with transitional, hay/pasture and deciduous forest. Some of these
latter discrepancies undoubtedly were related to changing surface conditions
that occurred between image and photograph acquisitions. NLCD Availability, Users and their Applications. The NLCD is available (FTP download or CDROM) from the USGS EROS Data Center website: edcwww.cr.usgs.gov/programs/lccp/natllandcover.html Since October, 1999 over 8500 state land cover files have been downloaded from the USGS EROS Data Center FTP site. The files on the FTP site are generic binary files (one file for each state) and are available at no charge to data users. A text file is associated with each binary file, and provides information on map projection, coordinates, and other parameters. Additionally, the states in Regions 1-4 are also available on 8 CDROMs. States in Regions 5-10 will ultimately be available on CDROM. Each CD contains as many contiguous state files as will fit (e.g. all six New England states are available on one CD). A total of 31 CDs are required to hold all the NLCD files. As of December 31, 2000, over 200 CDs (600 files) have been purchased from the following web site: http://edcwww.cr.usgs.gov/programs/lccp/nlcd.jsp.
Since the data have been available, the USGS/EDC Land Cover Applications Center has compiled a database of users and their applications. The goal is to gather user information to better understand the need for land cover data. To date, over 500 people have registered as users of the NLCD. The following information was derived from that database. Users and Applications of NLCD. As expected, Federal and State agencies along with Universities are the major users of the NLCD, but many, non-governmental organizations (NGOs), commercial and local agencies are also showing interest in the NLCD (see Figure 5). The reported size of study areas to which NLCD data are being applied (Figure 5) indicates that most, but not all users are using NLCD for large area assessments. Approximately 8% of the users are using the data for relatively small areas (county size or smaller). The NLCD is being used for a wide range of applications (Table 3). While some users appear to push the limits of the data, we have not ascertained whether this group scrutinized the data as recommended and were satisfied with what they found. Many of these users report there is no other source of data. Limitations and Reflections Accuracy. While the 80% accuracy level achieved for the NLCD at Anderson Level 1 is a reasonable value considering the scope of the project, the level of accuracy for the Anderson Level 2 type classes (60%) is lower than anticipated. There are a number of variables that affect accuracy levels, and discussion of some of these as they pertain to NLCD is warranted. One source of Anderson level 2-type error relates to the level of class distinctness. Some groups of classes fall on a continuum, grading from one class to another (both in the field as well as spectrally). The forest classes and residential classes are good examples of this as they grade from one class to another with no definite demarcation between them (e.g. deciduous to mixed to evergreen; low intensity to high intensity residential). While the definitions of these classes include percentage thresholds as cutoff values (e.g. low intensity residential is characterized by having 0-75% built-up material, and high intensity residential has 75-100% built-up material), the classes are not particularly well-defined, especially near the threshold value. Yet unless the accuracy values are thoroughly scrutinized, a point that is labeled as “high-intensity residential” that has 72% built-up material will simply be a misclassification contributing to error. Another source of error relates to interpretability and quality of reference material used in the accuracy assessment. In this investigation, AA was accomplished using NAPP photography. It is noteworthy that the forested wetland class had a relatively high error based upon the AA, yet the original source for much of the forested wetlands information was NWI. Wetlands for NWI were originally delineated by interpretation of air photos. The NWI data in turn were relied upon heavily to delineate wetlands for NLCD. Yet the air photo validation of forested wetlands of NLCD indicated high levels of “error.” The discrepancies resulted from (1) differences in photointerpreters, and/or (2) the fact that the photographic materials used for NLCD were not ideal for discriminating forested wetlands (whereas the photos used for NWI were better). In either case, it is apparent that there is error associated with the photointer-pretation phase of the accuracy assessment that adds to classification “error.” Quality of air photos, which includes year and season of photo acquisition, may be a major factor influencing the accuracy assessment error for other classes as well, especially those that have a propensity to change intra- and inter-annually (e.g. agricultural crops). It is important that users of the NLCD carefully evaluate the accuracy values in the context of their particular applications. Those users who do not need Anderson Level 2 type class information may wish to combine classes into an Anderson Level 1-type of a product, and thus work with land cover data with higher accuracies that will enhance the integrity of their results. Conversely, users working with the NLCD data in spatial modeling capacities may wish to keep the data in the 21-class form. These users may recognize that while there is error associated with the classification product, there may also be high levels of uncertainly associated with the models that they are running, and that some information for given classes is better than none. It should also be kept in mind that scaling issues affect classification accuracies, with a general trend of increasing accuracies with coarser levels of spatial aggregations of pixels. For instance, higher levels of error are associated with these error assessments conducted at the single pixel level than at the 3x3 pixel level. Many users do not need the NLCD at the level of spatial detail provided, and will find it beneficial to spatially aggregate to the scale appropriate for their application. While we do not know the levels of accuracy associated with the 1 km NLCD products, we are reasonably certain that the accuracy levels of these data sets will be high enough for many national-scale applications. Flexibility. Users often desire more land cover classes than NLCD, but they need to recognize that increasing the number of classes tends to exponentially increase the level of effort in creating the land cover classification product. In addition, higher numbers of classes generally result in higher levels of error. In spite of these observations, we recognize that there is a need within the user community for products that provide more thematic information than is currently provided by NLCD. Certainly there is more land cover information that can be gleaned from the Landsat data and ancillary data sets than provided by NLCD. Standard classifications such as those done to generate NLCD tend to generalize and simplify the landscape into a set number of discrete units, and much potentially useful information tends to be lost in the process. One of the goals with future work will be to generate a land characteristics database at 30 m resolution that provides users with more capabilities towards tailoring products that will fit with their applications. Techniques are currently being developed for this, and will be implemented during “MRLC 2000” when a new National Land Cover Database will be generated for the entire United States using 2000 vintage Landsat data. One of the goals of this research will be to provide more quantitative information for selected continuous variables (e.g. canopy closure, impermeable surfaces). In addition, it is anticipated that users will have access to more intermediate data layers (i.e. pre-classification derivative products) that will be useful for deriving specific land cover variables appropriate for their applications that are not included in the final NLCD data sets. Quality of Source Data. High quality land cover products can be derived only when input data are also of high quality. Generally, the Landsat 5 TM data acquired by the MRLC were of high quality from the standpoint of cloud and haze coverage. However, many of the data sets were sub-optimal in terms of seasonality. Many land cover features are much easier to map accurately using remotely sensed data sets from the appropriate time of year. For instance, hay/pasture is easier to discriminate from other types of land cover in early spring rather than mid-summer. While early spring and midsummer TM data sets were targeted for developing the NLCD, the data sets from the optimal time periods were often not available due to cloud contamination. In addition, it was often difficult to ascertain what “optimal” time periods were for each scene. Thus, during the scene-selection phase of the project, there were two confounding issues: (1) lack of data from the appropriate time(s) of year and (2) lack of knowledge as to the time frames of optimal land cover separability for each scene. Determination of the date to be used was generally subjective, and was based on our somewhat limited understanding of phenological patterns and opinion as to what time periods would give us the best land cover separability. With the potential of using both Landsat 5 and 7 data for the next national mapping effort, the issue of clouds adversely affecting data availability may not be as great a problem as during the first effort. The two satellites are offset by eight days, and thus there will be twice as many opportunities to acquire cloud-free data throughout the growing season as during the first mapping effort. While the primary source of data for land cover mapping will be from Landsat 7 ETM+ data, it should be possible to augment the database with Landsat 5 TM data when necessary. Both TM and ETM+ data have been shown to provide similar information from an applications standpoint (Vogelmann et al., 2001), and with some exceptions and modifications, it should be possible to use the two sources of data interchangeably. The other issue, lack of knowledge as to the time frames of optimal land cover separability, has been the focus of research since the completion of NLCD. In brief, it has been determined that use of the high temporal resolution data provided by AVHRR in conjunction with NLCD-derived land cover information provides useful information regarding optimal time periods for Landsat data acquisitions. Briefly, seasonal AVHRR-derived Normalized Difference Vegetation Index (NVDI) data were obtained for the dominant NLCD-derived land cover types for each path and row or mapping zone. Plots of AVHRR-derived NDVI versus date were developed for each major type of land cover for each path/row or mapping zone. Comparisons of the plots were then done to determine the three best dates for separating as many of the dominant types of land cover for each path/row as possible. Further details are provided in Yang et al. (2001b). This information is being used to target dates for scene acquisition for the next mapping effort. It is anticipated that three scenes, representing different seasons, will be acquired for each scene for MRLC 2000. Conclusions Acknowledgments. This work was performed in part by the Raytheon Corporation under U.S. Geological Survey Contract 1434-CR-97-40274. Authors References Brown, J.F., T.R. Loveland, J.W. Merchant, B.C. Reed, and D.O. Ohlen, 1993. Using multisource data in global land cover characterization: concepts, requirements and methods. Photogrammetric Engineering and Remote Sensing, 59:977—987. Bureau of the Census, 1991a. Census of population and housing, 1990, public law 94-171 data (United States) (machine readable data files), The U.S. Bureau of the Census (producer and distributor), Washington, D.C. Bureau of the Census, 1991b. Census of population and housing, 1990, public law 94-171 data, on-line documentation (United States), The U.S. Bureau of the Census, Washington, D.C. Bureau of the Census, 1992. TIGER/Line Files, (machine readable data files), The Bureau of the Census (producer and distributor), Washington, D.C. Congalton, R. and K. Green, 1993. A practical look at sources of confusion in error matrix generation. Photogrammetric Engineering and Remote Sensing, 59:641-644. Dobson, J.E., E.A. Bright, R.L. Ferguson, D.W. Field, L.L. Wood, K.D. Haddad, H. Iredale, J.R. Jensen, V.V. Klemas, R.J. Orth, and J.P. Thomas, 1995. NOAA Coastal Change Analysis Program (C-CAP): guidance for regional implementation, NOAA Technical Report NMFS 123, U.S. Department of Commerce, Seattle, Washington. ERDAS, 1998. ERDAS Imagine Expert Classifier. ERDAS, Atlanta, GA. Friedl, M.A. and C.E. Brodley, 1997. Decision tree classification of land cover from remotely sensed data. Remote Sensing of Environment, 61:399-409. Hansen, M., R. Dubayah and R. Defries, 1996. Classification trees: an alternative to traditional land cover classifiers. International Journal of Remote Sensing, 17:1075-1081. Khorram, S., G. Biging, D. Colby, R. Congalton, J. Dobson, R. Ferguson, M. Goodchild, J. Jensen, and T. Mace, 1999. Accuracy Assessment of Remote Sensing-derived Change Detection. Monograph. American Society of Photogrammetry and Remote Sensing, Bethesda, MD, 64 pp. Lauer, D.T, 1986. Applications of Landsat data and the data base approach. Photogrammetric Engineering and Remote Sensing, 52: 1193-1199. Loveland, T.L., J.W. Merchant, D.O. Ohlen, and J.F. Brown, 1991. Development of a landcover characteristics database for the conterminous U.S. Photogrammetric Engineeering and Remote Sensing, 57:1,453-1,463. Loveland, T.L. and D. M. Shaw, 1996. Multiresolution land chracterization: building collaborative partnerships, In Gap Analysis: A Landscape Approach to Biodiversity Planning (eds. J.M. Scott, T. Tear, and F. Davis), Proceedings of the ASPRS/GAP Symposium, Charlotte, NC, (National Biological Service, Moscow, ID), pp. 83-89. Prince, S.D. and M.K. Steininger, 1999. Biophysical stratification of the Amazon basin. Global Change Biology, 5:1-22. Scott, J.M., T.H. Tear, and F.W. Davis (eds.), 1996. Gap Analysis. A Landscape Approach to Biodiversity Planning, American Society for Photogrammetry and Remote Sensing, Bethesda, MD, 320 pp. Stehman, S.V. and R.L. Czaplewski, 1998. Design and analysis for thematic map accuracy assessment: Fundamental principles. Remote Sensing of Environment, 64:331-344. Stehman, S.V., J.D. Wickham, L. Yang, and J.H. Smith, 2000. Assessing the accuracy of large-area land cover maps: Experiences from the Multi-resolution Land-cover Characteristics (MRLC) Project. Proceedings of the 4th International Symposium on Spatial Accuracy Assessment in Natural Resources and Environmental Sciences, Delft University Press, The Netherlands, 601-608. Story, M. and R.G. Congalton, 1986. Accuracy assessment: A user’s perspective, Photogrammetric Engineering and Remote Sensing, 52:397-399. U.S. Department of Agriculture, 1994. State Soil Geographic (STATSGO) Data Base, Data Use Information, United States Department of Agriculture Miscellaneous Publication Number 1492. U.S. Fish and Wildlife Service, 1996. National Wetlands Inventory (NWI) Metadata, U.S. Fish and Wildlife Service, National Wetlands Inventory, St. Petersburg, Florida. U.S. Geological Survey, 1990. Land use and land cover digital data from 1:250,000- and 1:1,000,000-scale maps, Data User’s Guide 4, Reston, Virginia, Department of the Interior, U.S. Geological Survey, 33 pp. U.S. Geological Survey, 1993. U.S. GeoData digital elevation models, Data User’s Guide 5, Reston, Virginia, Department of the Interior, U.S. Geological Survey, 51 pp. Vogelmann, J.E., D. Helder, R.A. Morfitt, M.J. Choate, J.W. Merchant, and H. Bulley, 2001. Effects of Landsat 5 TM and Landsat 7 ETM+ radiometric and geometric calibrations and corrections for landscape characterization, Remote Sensing of Environment, in press. Vogelmann, J.E., T.L. Sohl, and S.M. Howard, 1998. Regional characterization of land cover using multiple sources of data, Photogrammetric Engineering and Remote Sensing, 64:45-57. Vogelmann, J.E., T.L. Sohl, P. V. Campbell, and D.M. Shaw, 1998. Regional land cover characterization using Landsat Thematic Mapper data and ancillary data sources. Environmental Monitoring and Assessment, 451:415-428. Yang, L., S.V. Stehman, J.D. Wickham, J.H. Smith, and N.J. Van Driel, 2000. Thematic validation of land cover data of the eastern United States using aerial photography: feasibility and challenges. Proceedings of the 4th International Symposium on Spatial Accuracy Assessment in Natural Resources and Environmental Sciences, pp. 747-754. Yang, L., S. Stehman, J. Smith, and J. Wickman, 2001a. Thematic Accuracy of MRLC Land Cover for the Eastern United States, Remote Sensing of Environment, in press. Yang, L., C. Homer, K. Hegge, B. Wylie, and B. Reed, 2001b. A Landsat 7 scene selection strategy for national land cover and land use characterization. In prep. Zhu, Z, L. Yang, S.V. Stehman, and R.L. Czaplewski, 2000. Accuracy assessment for the U.S. Geological Survey regional land cover mapping program: New York and New Jersey Region, Photogrammetric Engineering and Remote Sensing, 66:1425-1435.
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