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to determine land cover and a subsequent change detection. The data were field
validated and mosaicked to produce a land cover inventory for Southern Maine.
If you wish to create an attribute table to identify the different land cover
classifications, an easy reference table is available under the PROCESS
DESCRIPTION section.</gco:CharacterString>
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SPATIAL DATA ORGANIZATION INFORMATION 
Direct Spatial Reference: Raster

SPATIAL REFERENCE INFORMATION - PLANAR 
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UTM Zone Number: 19
Scale Factor at Central Meridian: 1
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Ellipsoid Name: GRS80
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      ATTRIBUTE ACCURACY REPORT: A team of field investigators participated in data
      verification exercises on December 9-13, 1996. Data validation teams consisted
      of personnel from the NOAA Coastal Services Center and Oak Ridge National
      Laboratory. Each team was equipped with a portable color laptop computer linked
      to a Global Positioning System (GPS). The field station runs software that
      supports the classified data as a raster background with the road network as a
      vector overlay with a simultaneous display of live GPS coordinates. Accuracy
      assessment points were generated with ERDAS Imagine software using a stratified
      random sample in 3x3 pixel homogeneous windows. To make the acquisition of the
      field reference data more practical, a twenty pixel buffer area around roads
      (i.e. 10 pixels on each side of the road) was created. 7,000 random points were
      generated within this area for the accuracy assessment. Collection of ground
      reference information for areas that have experienced a change in land cover
      type is a troublesome task. Pre-Processing Steps: The scene was georectified to
      UTM Zone 19 coordinates. Ancillary data sets: Subsequent field work and the use
      of collateral data such as USGS maps county marsh inventories, and National
      Wetland Inventory data led to further refinements in the image classification.
      Shoreline features can be extracted from Landsat images by detecting the
      land/water interface. However, care must be used to avoid misinterpreting tidal
      differences as changes in shorelines, since the satellite images from which
      these land cover images are derived and acquired at different tidal stages,
      depending on when the satellite is overhead. The land cover classifications
      represent the instantaneous state of the shoreline at the moment of image
      acquisition. C-CAP data are mapped at 1:100,000 scale with 22 standard classes
      constituting major landscape components. They are not jurisdictional (can't be
      used for permitting) and will not identify individual species. However, they
      are useful for identifying regional landscape patterns, major functional
      niches, environmental impact assessment, urban planning, and zoning
      applications. If you need change analysis data at this scale, C-CAP may be your
      only option. C-CAP is designed around a 1 to 5 year revisit cycle. Land Cover
      is the complete human and natural landscape recorded as surface components -
      forest, water, wetlands, concrete, asphalt, etc. Land cover can be documented
      by analyzing spectral signatures of satellite and aerial imagery. Land Use is
      the documentation of human uses of the landscape - residential, commercial,
      agricultural, etc. Land use can be inferred but, not explicitly derived from
      satellite and aerial imagery. There is no spectral basis for land use
      determination in satellite imagery. C-CAP data can be used to identify concrete
      and asphalt as land cover, but we can only infer that these materials denote a
      residential or commercial use. Post-Processing Steps: The data were clipped to
      Maine's southern state boundaries and put through a datum conversion from NAD27
      to UTM NAD83 zone 19. Known Problems: In addition, a very small portion of the
      June 1993 scene was obscured by numerous small cumulus clouds and shadows. The
      areas affected by clouds and shadows were mapped using an algorithm developed
      by ORNL. The corresponding areas were classified using an August 31, 1993
      Landsat scene. Accuracy Results: This data set was found to be 86.4% accurate
      with a Kappa coefficient of 0.842. 
      
      LOGICAL CONSISTENCY REPORT: Tests for logical consistency indicate that all row
      and column positions in the selected latitude/longitude window contain data.
      Conversion and integration with vector files indicates that all positions are
      consistent with earth coordinates covering the same area. Attribute files
      appear to be logically consistent. Examining the change matrix for logical
      fallacies, we find, for example, that a very small number of pixels changed
      from developed land to any other category. 
      
      COMPLETENESS REPORT: The classification scheme comprehensively includes all
      anticipated land covers, and all pixels have been classified. The NOAA Coastal
      Change Analysis Program (C-CAP): Guidance for Regional Implementation, NOAA
      National Marine Fisheries Service Report 123, discusses the interagency effort
      to develop the land cover classification scheme and defines all categories. 
      
      HORIZONTAL POSITIONAL ACCURACY REPORT: Precision corrected images were
      purchased from the EROS Data Center in UTM NAD27 meters to an RMSE +/- 0.5
      pixels. 
      
      VERTICAL POSITIONAL ACCURACY REPORT: There was no terrain correction in the
      georeferencing procedure. 
      
      PROCESS DESCRIPTION: The processing steps for each C-CAP Southern Maine Land
      Cover 1986 Analysis product are intricately associated. Each database is the
      result of many processing steps with numerous iterations for each step. The
      output of one processing step or database is often the input data for another
      processing step. A brief description of the processing steps used in the land
      cover classification of the this project follows. Further description of the
      processing steps can be found in the NOAA Coastal Change Analysis Program
      (C-CAP): Guidance for Regional Implementation, NOAA National Marine Fisheries
      Service Report 123 (Dobson et al, 1995). Baseline Classification Process: The
      Southern Maine land cover/change classification product was processed using an
      iterative classification approach. Landsat Thematic Mapper data for
      path/row/date(s): 12/30 19860609 were analyzed and mosaicked to create land
      cover for Southern Maine. The scene was classified, focusing first on
      separating major categories (e.g. water, forest, marsh, herbaceous upland, and
      developed) using standard supervised classification techniques. Numerous
      individual areas were chosen as training sites for the land cover
      classification. The mean and covariance statistics for these areas are passed
      to an isodata classification algorithm which assigns an unknown pixel to the
      class in which it has the highest probability of being a member. Then iterative
      unsupervised classifications were performed on each major category individually
      by masking out all other major categories. With this type of unsupervised
      classification, the computer is allowed to query the multispectral properties
      of the masked scene using user specified criteria and to identify X mutually
      exclusive clusters in N-dimensional feature space. By masking out all data but
      a single major category, the spectral variance is greatly reduced thus
      decreasing classification errors. After several classification iterations of
      the masked data, final classification labels were assigned to the spectral
      clusters. Changes among major categories were permitted to occur even at this
      stage of processing. Subsequent field work and the use of collateral data such
      as USGS maps, TIGER road data, and National Wetland Inventory data led to
      further refinements in the image classification. In small areas where landcover
      class confusion could not be separated spectrally, human pattern recognition
      was used to recode the data. A spatial filter was applied to the final
      classification data file. Change Classification Process: Landsat Thematic
      Mapper data for path/row(s) 12/30 19860609 were analyzed to arrive at a land
      cover for Southern Maine. The change date land cover classification was in part
      derived from the baseline classification. Only the pixels in the June 12, 1993
      image that changed spectrally from the change date image were classified for
      the June 9, 1986 data file. All other pixels were simply replaced with the
      baseline image classification. It is possible to simply identify the amount of
      change between two images by image differencing the same band in two images
      which have previously been rectified to a common basemap. Image differencing
      involves subtracting the imagery of one date from that of another. The
      subtraction results in positive and negative values in areas of radiance change
      and zero values in areas of no-change in a new 'change image'. The images are
      subtracted resulting in an signed 16-bit analysis with pixel values ranging
      from -255 to 255. The results were transformed into positive unsigned 16-bit
      values by adding a constant, c. The operation is expressed mathematically as:
      Dijk = BVijk(1) - BVijk(2) + c where Dijk = change pixel value BVijk(1) =
      brightness value at time 1 BVijk(2) = brightness value at time 2 c = a constant
      (e.g., 255). i = line number j = column number k = a single band (e.g. TM band
      4). The 'change image' produced using image differencing usually yields a BV
      distribution approximately gaussian in nature, where pixels of no BV change are
      distributed around the mean and pixels of change are found in the tails of the
      distribution. A threshold value was carefully chosen to identify spectral
      'change' and 'no-change' pixels in the 'change image.' A 'change/no-change'
      mask was derived by performing image differencing on band 4, and Normalized
      Difference Vegetation Index (NDVI) of the two date dataset and recoded into a
      binary mask file. The 'change/no-change' mask was then overlaid onto the
      earlier date of imagery and only those pixels which were detected as having
      spectrally changed were viewed as candidate pixels for categorical change.
      Change Detection Database The change date and baseline land cover
      classifications were compared on a pixel by pixel basis using a change
      detection matrix. This traditional post-classification comparison yields 'from
      land cover class - to land cover class' change information. Many pixels with
      sufficient change to be included in the mask of candidate pixels in the
      spectral change process did not qualify as categorical land cover change. This
      method may reduce change detection errors (omission and commission) and
      provides detailed 'from-to' change class information. The technique reduces
      effort by allowing analysts to focus on the small amount of area that has
      changed between dates. PROCESS DATE: 19960930
      
      PROCESS DESCRIPTION: This data was projected to Universal Transverse Mercator
      zone 19 with a horizontal datum of NAD83. PROCESS DATE: Unknown
      
      SOURCE INFORMATION - CITATION: Earth Observation Satellite Company. Landsat
      Thematic Mapper Source_Geospatial_Data_Presentation_Form: remote-sensing image.
      1986-06-09. OTHER CITATION DETAILS: Landsat Thematic Mapper scenes processed:
      Path = 12 Row = 30 Date 06-09-1986
      TYPE OF SOURCE MEDIA: 8 mm magnetic tape. 
      SOURCE CURRENTNESS REFERENCE: ground condition. 
      SOURCE CITATION ABBREVIATION: south_86. 
      SOURCE CONTRIBUTION: Source used in land cover classification.
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