Studying Earth as a system including the hydrological, biological, geochemical,
cryospheric and solid earth components requires routine acquisition of
high-resolution, synoptic-scale observations that can be composited into snapshots
of Earth in a sequence of moments. Only space-borne imaging instruments can
provide this sort of data, and synthetic aperture radar (SAR) data are particularly
well-suited for this task (see story, this issue).
As an active microwave sensor, SAR in general can image in day or night and through most weather conditions. The SAR onboard Canadas RADARSAT-1 satellite has additional important attributes, including selectable resolutions from 10 to 100 meters and swath widths from 50 to 500 kilometers. The resulting images can be mosaicked together to generate near-instantaneous views of continental proportions.
In 1998, we reported in Eos on global remote sensing data campaigns using RADARSAT-1 and including the Canadian Space Agencys Background Mission. The following are some of the products from those campaigns in the form of image mosaics. We created these mosaics from RADARSAT-1s ensemble of beams. They render single-season views of entire continents and could serve as benchmarks for monitoring global change.
Canada: A Winter View This winter view of the entire Canadian landmass and its coastal zones was compiled with images acquired mainly during the week of Jan. 25, 1999. The 276 images mosaicked together were acquired in roughly 80 ScanSAR Narrow beam swaths, the first received on January 25 and the last on February 2. Each of the images in the mosaic has a pixel spacing of 50 meters. The full-resolution mosaic is provided at 150-meter pixel spacing. This unique image product is a true picture of Canada at a given point in time. It shows the Hudson Bay sea ice and its coastal contact, the shape of land features in the winter of 1999, and, presumably, even a transient weather-related element in the form of a white band in the lower right corner of the mosaic, which runs across southern Ontario and west-central Quebec. Such temporal views created on a seasonal and multi-annual basis can help us understand the impact of environmental changes and human actions on a regions ecosystems and natural resources.
A Closer Look At Craters These wide-area digital radar image mosaics can be used for a variety of applications. For example, the preserved record of terrestrial impact craters is several factors smaller than the integrated impact flux estimates and erosional rates for such landforms would suggest. This means that there is a vast missing record lurking in those parts of Earths continental geologic record for which the wide-area surveys are either nonexistent or hampered by difficulties associated with access, weather and land cover. A clear advantage with radar images in comparison with the optical images is the tonal and textural properties of the radar images that suppress superficial effects and enhance the structural and morphological contrasts, as seen here on the crater site from Canada (see white box, above; for a close-up view of a crater in Africa, see below). As one of the many applications of SAR data, these mosaics therefore have good potential use in inventorying Earths impact craters.
Mapping Africa This RADARSAT-1 image mosaic (left) of Africa is split along the vegetation line that coincides roughly with 10 degrees north, separating the African sub-Sahara from the Sahara. The northern and the Saharan parts of Africa were imaged at a coarser resolution of 50 meters with the satellites ScanSAR Narrow beam and the remainder of the continent with the 25-meter-resolution ScanSAR Wide beam. The structural and vegetation contrast of the SAR images manifests itself in several regions, including the rainforest of the Congo basin, the east-African rift structures and the west-African dykes that extend offshore, along which a number of volcanic peaks are aligned. The full-resolution digital mosaic should aid African ecological studies and resource management.The crater shown here (below) is at the center of the white box on the African continent (to the left).
Antarctica Revealed [see print issue for image] This first high-resolution (25-meter pixel spacing) radar mosaic of Antarctica was compiled from RADARSAT-1 Standard and Extended Low beam data acquired during an 18-day period in September and October of 1997. The image is a remarkable depiction of the southern continent. The boundary separating seasonal sea ice from the ice sheet and the few rocky areas of the coastline is clearly evident. Short-term summer melting results in morphologic changes to the near-surface snow, which then appears in the mosaic as bright regions around the perimeter of the continent. The large-scale bright and dark patterns across the continental interior are mainly caused by spatial changes in surface accumulation rate. The thousands of kilometers of sinuous bands that wind across east Antarctica are associated with ice flow divides. Preliminary comparisons between the 1997 and 2000 data sets reveal complex changes in the ice sheet margin and document the continued retreat of Antarctic Peninsula ice shelves.