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were analyzed according to the Coastal Change Analysis Program (C-CAP) protocol
to determine land cover and a subsequent change detection. The data were field
validated to produce a land cover inventory for Great Bay New Hampshire. 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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            <gco:CharacterString>To improve the understanding of coastal uplands and wetlands, and
their linkages with the distribution, abundance, and health of living marine
resources.

SPATIAL DATA ORGANIZATION INFORMATION 
Direct Spatial Reference: Raster

SPATIAL REFERENCE INFORMATION - PLANAR 
Grid Coordinate System Name: Universal Transverse Mercator
UTM Zone Number: 19
Scale Factor at Central Meridian: 1
Longitude of Central Meridian: -69
Latitude of Projection Origin: 0
False Easting: 500000.00000
False Northing: 0.00000
Planar Coordinate Encoding Method: Row and column
Abscissa Resolution: 30
Ordinate Resolution: 30
Planar Distance Units: Meters

SPATIAL REFERENCE INFORMATION - GEODETIC MODEL 
Horizontal Datum Name: North American Datum 1983
Ellipsoid Name: GRS80
Semi-major Axis: 6378206.4
Denominator of Flattening Ratio: 294.98

NATIVE: ERDAS IMAGINE Version 8.2 on a SUN Sparc-10 using SUN Operating System
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                  <gco:CharacterString>EARTH SCIENCE &gt; LAND SURFACE &gt; LAND USE/LAND COVER &gt; LAND COVER</gco:CharacterString>
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                              <gco:Date>2008-02-05</gco:Date>
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                        <gco:CharacterString>Olsen, L.M., G. Major, K. Shein, J. Scialdone, R. Vogel, S. Leicester, H. Weir, S. Ritz, T. Stevens, M. Meaux, C.Solomon, R. Bilodeau, M. Holland, T. Northcutt, R. A. Restrepo, 2007 .   NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version  6.0.0.0.0</gco:CharacterString>
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                           <gmd:date>
                              <gco:Date>2009-06-10</gco:Date>
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                        <gco:CharacterString>Olsen, L.M., G. Major, K. Shein, J. Scialdone, R. Vogel, S. Leicester, H. Weir, S. Ritz, T. Stevens, M. Meaux, C.Solomon, R. Bilodeau, M. Holland, T. Northcutt, R. A. Restrepo, 2007 .   NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version  6.0.0.0.0</gco:CharacterString>
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                        <gco:CharacterString>IDN Nodes</gco:CharacterString>
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                              <gco:Date>2007-04-01</gco:Date>
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                        <gco:CharacterString>Olsen, L.M., G. Major, K. Shein, J. Scialdone, R. Vogel, S. Leicester, H. Weir, S. Ritz, T. Stevens, M. Meaux, C.Solomon, R. Bilodeau, M. Holland, T. Northcutt, R. A. Restrepo, 2007 .   NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version  6.0.0.0.0</gco:CharacterString>
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                              <gco:Date>2009-12-22</gco:Date>
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      ACCESS CONSTRAINTS: None, except for a possible fee at the cost of
      reproduction.
      
      DISTRIBUTION LIABILITY: Users must assume responsibility to determine the
      usability of these data. 
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      Data set is not for use in litigation. While efforts have been made to ensure
      that these data are accurate and reliable within the state of the art, NOAA,
      cannot assume liability for any damages, or misrepresentations, caused by any
      inaccuracies in the data, or as a result of the data to be used on a particular
      system. NOAA makes no warranty, expressed or implied, nor does the fact of
      distribution constitute such a warranty. Additional Use Constraints: None
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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
      NAD 27 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: Reprojected into
      the horizontal datum NAD83 UTM 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 Great Bay, New
      Hampshire- 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 New Hampshire Great Bay 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 to create a land cover for the Great Bay New Hampshire. 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 Great Bay New Hampshire. 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: 20000214
      
      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. Unknown. GEOSPATIAL DATA PRESENTATION FORM: remote-sensing
      image. ONLINE LINKAGE: http://edc.usgs.gov/eros-home.html. 
      TYPE OF SOURCE MEDIA: 8 mm magnetic tape. 
      BEGINNING TIME: 19860609. 
      ENDING TIME: 19930612. 
      SOURCE CURRENTNESS REFERENCE: Date of Landsat Scenes. 
      SOURCE CITATION ABBREVIATION: unknown.
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