Skip past header information
USGS - science for a changing world

U.S. Geological Survey Open-File Report 2010-1332

GLORIA Sidescan-Sonar Imagery for Parts of the U.S. Exclusive Economic Zone and Adjacent Areas


Methods: Digital Processing and Mosaicking of GLORIA

Skip past contents information
Title Page
Introduction
Methods
  • Remote Sensing
  • Digital Processing
  • Aleutian Arc
    Atlantic Coast
    Bering Sea
    Cayman Trough
    Gulf of Alaska
    Gulf of Mexico
    Hawaii I
    Hawaii II
    Hawaii III
    Johnston Atoll
    Kingman-Palmyra
    Pacific Coast
    Puerto Rico
    Data Catalog
    Acknowledgments
    References
    List of Figures
    Contacts

    Digital Processing

    Gulf of Mexico GLORIA mosaic #13.
    Figure 6. Completed GLORIA digital mosaic number 13 from the Gulf of Mexico. Click to enlarge figure.

    The imagery contained in the GLORIA mosaics are assembled from digitally collected, computer processed sidescan sonographs. The sonographs, or swaths, were recorded digitally on 9-track magnetic tapes in 6-hour-long files (considered the raw data) and generally referred to as "passes" (fig. 8). The passes were processed individually through a standard set of processing programs to correct for geometric and radiometric distortions that exist in the raw data. The software, written specifically to correct both the geometric and radiometric distortions were part of an operational software package referred to as the U.S. Geological Survey's Mini Image Processing System (MIPS) (Chavez, 1984).

    During the several years of data collection and processing, the computer programs and processing steps were refined though the processing remained essentially standardized, thus keeping the data quality consistent despite the large number of personnel working on the program over the years. The computer programs focused on GLORIA-specific algorithms that included corrections for slant-range geometry, water-column offset, aspect ratio distortion, ship's velocity changes, speckle noise, and shading due to signal drop off as a function of range.

    Classification of the computer programs used in the initial processing of the raw data are grouped in two categories. The first set of programs were used to correct for geometric distortions in the dataset that are a result of the way the data are collected. The result of these programs were to move the pixels and put them in their proper across- and along-track location. The second group of programs were to apply radiometric corrections to improve the quality of the collected data. The result of these programs were to modify the pixel values. (Condit, 1979)

    A brief description of the major processing steps follows. The descriptions have been grouped within the two categories (geometric or radiometric corrections) for simplicity of the discussion. In actuality, the processing sequence for a 6-hour-long pass mixes the sequence of the geometric and radiometric corrections. A typical processing sequence may be examined with this flowchart (fig. 7).

    Geometric distortions and their correction may be summarized as:

    1. Slant-range correction - This processing step corrects slant-range to ground-range and removes the water-column gap in the image. The water-column offset is the distance the sonar vehicle is above the seafloor. Slant-range error is mislocation of pixels in the across-track direction compared to their proper location on a map because the sensor is measuring range distance from a point above the seafloor rather than horizontal distances to the seafloor. After the slant-range correction has been made, the across-track location of targets is accurate (fig. 9).
    2. Aspect ratio distortion correction - The image aspect ratio distortion occurs from the higher density of data points collected across-track than along-track. The distance traveled by the ship between each consecutive scan is computed from the navigation data, and the number of pixels (each representing 50 m) required along the particular segment was calculated. The original along-track scan is duplicated the appropriate number of times to fill the space with 50 m pixels in order to achieve a 1:1 ratio between along-track and across-track distances. The practice of duplication to create a square 50 m pixel size was followed so that information in the across-track direction would not have to be omitted (fig. 12).

    Radiometric corrections applied may be summarized as:

    1. Across-track shading correction - This enhancement was used to correct for horizontal shading problems that result from attenuation and transmitter power build-up (fig. 10). Result of this correction is normalization of the data in the near and far range so they can be compared directly with each other.
    2. Striped noise removal - During data acquisition some sonar lines have lower backscatter values than the adjacent lines due to vehicle instability or noise in the water-column. This results in a striped appearance in the across-track direction of the image. This enhancement is applied to remove the striping noise that occurs in the image and is completed in a three part process. The correction involves combining two filtered components of the image. One image contains the high-frequency (high-pass filter) component of every line without the noise. The other image contains the low-frequency background brightness (low-pass filter) of a broader swath image without the noise. The high-pass and low-pass images are then combined to recreate an image very similar to the original but without the noise (fig. 11).
    3. Speckle-noise removal - A small, 2-by-2 pixel, low-pass smoothing filter was used to suppress the speckle noise present in the sonar imagery. The filter, computed as a moving average across the image, was chosen because it produces a minimal amount of blurring and helps reduce the blocky appearance of the image due to the 2.5 times image stretching done in the along-track direction as a result of the aspect ratio correction (fig. 12).

    Digital Mosaicking

    After the sidescan-sonar swaths were processed to correct them geometrically and radiometrically, they were ready for digital mosaicking. Initially the final results of the digital mosaicking steps were to create mosaics of a 2-degree by 2-degree area. However in some areas, such as the Alaska regions, mosaics of a 3-degree by 2-degree area were created.

    Digital mosaicking of the GLORIA data is more difficult than that of other image data because geometric control is available only at nadir (Chavez and others, 1996). The mosaicking procedure involves several steps. To begin, the swaths needed to create a straight line segment for a given map area must be identified. This was done by referencing the survey track map and the processed GLORIA data to match the dates and times of the necessary segments. Multiple 6-hour-long passes were spliced end-to-end to make a continuous line segment that passed through the intended mosaic area and where the portions of the ship's heading remained generally constant. If necessary, the swaths were tone matched by applying a contrast stretch to minimize the seam where they were joined.

    Four control points were then selected as nadir references from the newly created strips. The first and fourth control points reflected the start and end of the line segment while the second and third control points were selected to be spaced evenly within the swath. From these four points a trigometric computation was made to produce an additional eight control points that would tie the edge of the image to the map space. With these twelve control points, the strip was georeferenced within the map area. This step was repeated for each strip of sonar data for each specific area (fig. 13).

    After all the swaths for a given map area were georeferenced, the adjacent lines segments were stenciled together to create a continuous mosaic. In cases where further registration of the strips was required to align seafloor features, additional ground control points and rubber sheeting was done prior to the stenciling. When the swaths were aligned, interactive stenciling of the swaths was done by drawing a polygon around the area of the swath to be retained (fig. 14).

    The final step is the digital mosaicking procedure. This process of combining several arbitrarily shaped images to form one large, radiometrically-balanced image can be very user intensive. In the case of sidescan-sonar, the images are the adjacent swaths collected during the survey. The mapped swaths are combined together along user-specified cut lines defining the polygon and image precedence (which part of the image to keep; which part of the image to remove). Ideally, the cut-line boundaries can be blended together to reduce the boundary between images so they are not easily seen. The stenciled line segments were then combined sequentially to build the composite map (fig. 15).

    A more detailed description of the GLORIA digital processing and program details is available from Chavez (1986) and Chavez and others (1996).

    Skip USGS links group

    Accessibility FOIA Privacy Policies and Notices

    Take Pride in America logo USAGov logo U.S. Department of the Interior | U.S. Geological Survey
    End of USGS links group