U.S. AVHRR MOSAIC The mosaic of the conterminous United States was prepared using 16 images from the Advanced Very High Resolution Radiometer (AVHRR) sensors on the meteorological satellites NOAA-8 and NOAA-9. The images were acquired between May 24, 1984 and May 14, 1986. Standard image processing techniques were used to enhance the detail and the data were resampled to a resolution of 1000 meters (1 km) per picture element (pixel) and cast into an Albers Equal Area projection. The satellite image was then further enhanced by digitally introducing terrain shading based on USGS digital elevation models. The image size for the U.S. AVHRR mosaic is 2874 lines by 4632 samples. The satellites launched by the National Oceanic and Atmospheric Administration (NOAA) in Sun-synchronous polar obits have an orbital period of approximately 102 minutes. The orbital height is 805 km with a swatch width of 3000 km at the nadir. The orbital tracks repeat every 8 days, thereby providing more frequent coverage than the Landsat series of satellites. Two channels of data were used in the false-color infrared mosaic image. Channel 1 (0.58-0.68 um) was used to control the amount of blue and green in the composite, and Channel 2 (0.72-1.1 um) was used to control the amount of red. Channel 1 is in the red portion of the visible spectrum, which is sensitive to daytime clouds and vegetation. Channel 2 is in the reflected infrared (near-infrared) part of the spectrum and is used for shoreline and vegetation discrimination. The image simulates a false-color infrared composite as it would appear using these AVHRR channels to display on an 24-bit color monitor typically found on larger image processing systems. This composite was processed as a single image file and its color palette containing an optimum subset of 255 colors. This subset is from the thousands of colors need to show the original two channel composite as displayed on the 24-bit monitor. This optimum subset allows display of color composite images representing multiple AVHRR sensor channels on PC's having an 8-bit VGA graphics capability. On false-color infrared mosaics, vegetation appears in various tones of red instead of green. The "redness" indicates vegetation density and type and whether growing on dry land or in a swamp (a mixture of reddish vegetation and dark blue surface water produce dark tones). Grasslands appear light red, deciduous trees and croplands appear red, and coniferous forests appear dark red or maroon. Desert areas appear white and urban areas (pavement and buildings) appear bluish green. Lakes, rivers, and oceans appear in various shades of blue, dark blue for deep water and light blue for shallow or turbid water. Exposed bedrock generally appears as a dark bluish-green or other dark tone. Further information on the image enhancement techniques and the identification of the specific images used in the mosaic may be obtained from the U.S. Geological Survey, EROS Data Center, Customer Services, Sioux Falls, SD 57198. A two-sided 19" x 23" color map of the mosaic is available for a nominal fee by requesting the "United States Satellite View" from the U.S.