wind velocity vectors, ice motion vectors, or sample
data with text annotation may be overlayed on raster
images. For example, sparse data such as produced
by the ERS-1 Scatterometer or the DMSP Passive
Microwave Special Sensor Microwave Imager (SSM/I)
may be overlayed on ERS-1 SAR imagery or NOAA
AVHRR imagery to produce an easily read, multisensor
image on screen or hardcopy.
6.3 Sparse Data Interpolation
Sparse data requires special processing to fill in the
points between samples when image fusion with SAR
imagery is required. For example, sample spacing
in an ERS-1 SAR image is normally 12.5m. The
sample spacing of SSM/I data is 25km. Thus with
respect to the SAR image, the SSM/I data is very
sparse and must be interpolated. EV-SAR has several
interpolation functions for sparse data. These are
based on signal models for the sensor. Dispersion-
based techniques use a resolution model for the sensor
to interpolate the data points. Interpolation techniques
use a spatial model of the data to interpolate points on
a surface.
Sparse data interpolation is done in three steps.
First, a blank image (the slave image) is filled with zero
pixel values and is coregistered to the SAR (master)
image. Second, the sparse data points read from a
tabular or vector file are placed in the blank image
using the lat./long. georeferencing to map the data
samples into pixel coordinates. Finally, the third step
is the dispersion or interpolation to fill in all the pixels
in the slave image.
6.4 RGB and IHS Image Fusion
Image-Image fusion may done in EV-SAR using
standard Reg-Green-Blue (RGB) and Intensity-Hue-
Saturation (IHS) multichannel image combination
techniques. One application of IHS image fusion is the
combination of ice concentration data (derived from
the DMSP SSM/I passive microwave data) with a SAR
image showing in detail the ice flows[8]. A total of three
categories of ice concentrations (thin ice, first year ice,
and old ice) are coregistered to the ERS-1 SAR im-
age, sparse data interpolated, and converted to IHS.
The hue and saturation channels then contain the ice
concentration information. The intensity channel is re-
placed by the ERS-1 SAR image, and the IHS data set
is then converted back to RGB for display. The result
is an ERS-1 SAR image coloured to represent green
for thin ice, blue for first year ice, and red for old ice.
The more saturated the colour, the greater the ice con-
centration. Sample point data and coast lines may be
overlayed completing the data product. An example
of an ERS-1 SAR image with sample data overlay and
latitude /longitude grid is given in Figure 15.
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Figure 15: Example ERS-1 SAR image with sample
data overlay (Copyright ESA 1992).
7. CONCLUSIONS
Users have found the EV-SAR application package
to be a powerful low-cost solution for working with
SAR imagery. With the recent availability of the
new satellite SAR imagery (ERS-1 1991, JERS-1 1992,
RADARSAT 1995), interest in SAR will increase. This
package acts as a tutorial in SAR for users who are
new to SAR remote sensing. It serves as a tool to
aid the expert user in SAR image measurement and
interpretation.
ACKNOWLEDGEMENTS
The authors acknowledge the support of the Canada
Centre for Remote Sensing, National Resources
Canada, and the Ice Services Branch, Atmospheric En-
vironment Service, Environment Canada.
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[2] Guindon, B., M. Adair, 1992. Analytic formulation for spaceborne SAR
image geocoding and “value-added” product generation using digital elevation
data, Canadian Journal of Remote Sensing, 18(1):2-12.
[3] He, D.C., Wang, L., 1989. Texture unit, texture spectrum and texture
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[6] Lopes, A., et al., 1990. Maximum a posteriori speckle filtering and first
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