Robinson, J. A. and C. A. Evans. 2002.
Space Station Allows Remote Sensing of Earth to within Six Meters. Eos,
Transactions, American Geophysical Union 83(17):185, 188. |
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Budgetary challenges and research limitations of the International Space Station during its construction are routinely discussed in the media (e.g. Lawler, 2001). In spite of these challenges, the Earth remote sensing experiment, Crew Earth Observations (Robinson and Evans, 2001), is already yielding significant data returns by adopting the successful photographic methods used in earlier Earth imaging programs from the Space Shuttle and Mir Space Station (Lulla and Dessinov, 2000). Early results have revolutionized our understanding of the ability of humans to compensate for the relative motion of the Earth and achieve high remote sensing spatial resolution in handheld images. Images captured for Crew Earth Observations have spatial resolutions of less than 6 m, approaching the highest spatial resolution of color images now available from commercial remote sensing satellites. A total of 4385 images of Earth were captured
by the first resident Space Station crew, using digital still cameras,
35-mm film cameras, and 70-mm film cameras. Image acquisition by the second
crew is ongoing. Similar cameras have been used successfully on the Space
Shuttle and Mir to photograph Earth, with a >30-year database of nearly
400,000 photographs collected to date (Lulla et al, 1996). The photographs
are in the public domain, cataloged in a database maintained by the Earth
Sciences and Image Analysis Laboratory at the NASA Johnson Space Center.
The database is searchable on the World Wide Web (The Gateway to Astronaut
Photography of Earth, http://eol.jsc.nasa.gov/sseop). The photographs
are routinely digitized for use in scientific analysis, and can be used
as 3-band (red, green, blue) digital data ( e.g., Webb et al, 2000; Robinson
et al, in press).
In order to achieve the maximum potential spatial resolution determined by the geometries, the camera system must capture information at a sufficient speed to eliminate effects of relative ground motion. The speed of the Space Station relative to the ground is approximately 7.3 km s-1. At a normal shutter speed of 1/500 second, the expected blur due to motion relative to the ground would be 14.6 m. From previous experience, we knew that apparent ground motion was not limiting spatial resolution in handheld photographs. Photographs taken by astronauts from lower orbits using 250 – 300 mm lenses with 6.2 million megapixel digital still cameras or 70mm film cameras with film digitized at 2400 pixels per inch have had calculated spatial resolutions of approximately 10-15 m, without adding the 14.6 m smear due to ground motion. These resolutions were confirmed by validation of actual ground resolved distances (Webb et al, 2000; Robinson, et al, in press), and showed no evidence of ground smear, even when calculated spatial resolutions were < 15 m. Because of the success of astronauts in tracking and eliminating ground motion in their hand-held photography of Earth, new 350-mm and 400-mm lenses were recommended for use in photographing the Earth from the International Space Station and Space Shuttle flights. These lenses would give a best-case spatial resolution of about 8-11 m from Space Station altitudes. Although never envisioned to be used for photographing the Earth, a 2´ extender was also available for the 35-mm and digital still cameras. With time to adapt to the microgravity environment, special training in motion tracking (Glazovskiy and Dessinov, 2000), and extensive experience on orbit, Space Station crewmembers decided to test the use of the new 400-mm lens in combination with the 2´ extender in photographing the Earth. The sharpness of images acquired using doubled magnification have surprised both crewmembers and scientists on the ground, and have changed our view of the level of detail that can be recorded by humans from orbit. An example of the high spatial resolution achieved is shown in the figure. Digitized at 2075 ppi, this 35-mm film image of the Aswan High Dam, Egypt was taken using the Nikon F5 camera from a 379 km altitude while the Space Shuttle and Space Station were docked together in orbit. If the shot was a perfect nadir view, the calculated spatial resolution without ground motion would be 5.75 m/pixel. By measuring the known distances between airport marking aids on the Aswan Airport runway, the observed spatial resolution of the image is 5.98 m/pixel. This image is typical of the detail obtained for areas around the world by the ISS crewmembers. Engineers are currently developing electronic and mechanical motion compensation strategies for use on remote sensing instruments to be mounted in the U.S. Laboratory Window Observational Research Facility (WORF). Motion compensation technologies will be used for a variety of remote sensing instruments that will be mounted in the window so that they can achieve spatial resolution of 10 m or less on the ground. The engineering of these instruments is different than that for satellite-mounted instruments because there is less control over the movement of the platform (in this case the International Space Station) but there are also few requirements for the instruments to be “space hardened,” as they can be operated and maintained inside the cabin. The ability of crewmembers to compensate for motion represents a challenge to engineers to match their performance, while also validating the potential high resolution that can be obtained from the Space Station. The ISS provides great potential as a remote-sensing platform capable of providing high-resolution imagery of the Earth’s surface. The optical-quality window in the U.S. Destiny Laboratory (described in an earlier EOS article, Eppler et al, 1996) became part of the orbiting station in February 2001, with the WORF support system scheduled for installation in 2002. With several remote sensing instruments at different stages in the planning process, and advancing imaging technologies for handheld use, high-resolution images of the Earth from the International Space Station should soon be commonplace. References
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