The DIAL tool provides digital image processing to display the metadata as text
and the processed data as an image.
Each sample is a subset of the MISR Oblique Forward (CF) GRP data set.
The
sample data are subset from the Oblique Forward (CF) granule (the Oblique Forward (CF) camera)
for 3 blocks (Numbers 54, 55 and 56) from orbit 3734, path 40, on August 30, 2000. The data
file for the red band is larger because the data correspond to the higher
spatial sampling rate of 275 m per pixel while the other bands
have a spatial sampling rate of 1.1 km. Each block is 2048 samples across-track
and 512 lines along-track in 275 m sampling (512 pixels by 128 pixels at 1.1 km),
with four spectral bands as separate Scientific Data Sets (SDSs).
The difference between L1B2 Ellipsoid and Terrain georectified radiances
is in the altitude data used in the resampling algorithm.
In the Ellipsoid product, this altitude is represented by the WGS84 ellipsoid.
In the Terrain product, it is the altitude of the Earth's terrain.
The white dots within the thumbnail images are fill data,
representing areas on the Space Oblique Mercator (SOM) grid that could NOT be
observed by the CF camera, due to its 60-degree forward look angle.
This artifact of the TERRAIN-projected data is minimal in flat areas
and does not appear in ELLIPSOID-projected data.
The data
subset covers the central part of the U.S. state of Idaho (Sawtooth
Mountains and Snake River Plains), with adjacent parts of Montana
(Bitterroot Range), and of Wyoming (under the clouds). Areas of interest
include many national forests (Bitterroot, Boise, Challis, Nez Perce,
Payette, Salmon, Sawtooth, Targhee), national monuments (Craters
of the Moon, Hagerman Fossil Beds), and wilderness areas.
The sample includes
clear sky areas, areas with clouds, and areas with wildfire smoke
and haze. Block #56 has it all: urban area (Boise, ID), lakes, rivers,
sagebrush rangeland and farmland (Snake River Plains), lava flows,
forested mountains, alpine mountains, granite ridges, talus slopes,
alluvial fans, fire-burned areas, burning fires, smoke and haze,
cloud shadows and at least two types of clouds. The user wishing
to read about this area as it was in 1900 is referred to the first
few chapters of the U.S. Geological Survey Bulletin 199 (Russell, 1902,
Geology and Water Resources of the Snake River Plains of Idaho).
Top
of Page