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Exploring the Unknown - NASA's History Office

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EXPLORING THE UNKNOWN 161<br />

and <strong>the</strong> Wea<strong>the</strong>r Bureau were more free to think about experimental satellites to test out<br />

new instruments that might be incorporated into future generations of operational satellites.<br />

Nimbus 1, launched April 28, 1964, experienced a number of problems and operated<br />

for only a month; Nimbus 2, launched May 15, 1966, was much more successful, testing<br />

out improved cameras. NASA also tested meteorological satellite technology as part of <strong>the</strong><br />

Applications Technology Satellite (ATS) project to orbit experimental geosynchronous<br />

satellites (used for communications experiments as well as meteorological ones). In<br />

December 1966 and November 1967, ATS-1 and -3 explored <strong>the</strong> possibility of observing<br />

wea<strong>the</strong>r with line scan imagers, a possibility conceived by Vernon Soumi, a professor at <strong>the</strong><br />

University of Wisconsin; <strong>the</strong> resulting continuous coverage (images of <strong>the</strong> full Earth disc<br />

every thirty minutes) proved extremely valuable for tracking storms and even showed<br />

short-lived cloud patterns correlated to tornadoes. 31 Continuous coverage from geosynchronous<br />

orbit made it possible to observe <strong>the</strong> motion of clouds and deduce wind speed<br />

at <strong>the</strong> level of <strong>the</strong> clouds—a significant step toward <strong>the</strong> three-dimensional quantitative<br />

data meteorologists wanted. Three o<strong>the</strong>r satellites in <strong>the</strong> series, ATS-2, -4, and -5, also carried<br />

meteorological experiments, but all suffered launch problems. 32 ATS-6, launched in<br />

May 1974, carried a new cloud-imaging radiometer along with a more powerful transmitter<br />

that made it possible for anyone with an easy-to-build ground station to receive <strong>the</strong><br />

images. 33<br />

While <strong>the</strong> ATS program tested ideas for wea<strong>the</strong>r satellites in geosynchronous orbit,<br />

<strong>the</strong> Nimbus program continued to test advanced instruments in low-Earth orbit, with five<br />

launches between 1969 and 1978. Nimbus 3, launched April 1969, carried five new sensors.<br />

These included <strong>the</strong> first sounding instruments using remote sensing to furnish measurements<br />

of temperature and o<strong>the</strong>r variables at different levels of <strong>the</strong> atmosphere for<br />

providing numerical data for climate models. The sounding instruments on Nimbus 3<br />

measured temperature, water vapor, and ozone content of various atmospheric levels;<br />

later Nimbus satellites carried sounding instruments to measure o<strong>the</strong>r variables. The sensors<br />

worked well, but <strong>the</strong> data proved much less useful for wea<strong>the</strong>r prediction than scientists<br />

had expected. Meteorologists had hoped that data on temperature, wind speed, and<br />

o<strong>the</strong>r factors could be plugged into a model of how <strong>the</strong> atmosphere worked to provide<br />

wea<strong>the</strong>r predictions. Satellite sounding instruments provided much of <strong>the</strong> data needed<br />

with reasonable accuracy, but existing climate models were not designed to assimilate<br />

<strong>the</strong>se data easily. Meteorologists discovered that <strong>the</strong>y needed to perform much more<br />

research before <strong>the</strong>y could use data acquired by satellite to improve <strong>the</strong> accuracy of wea<strong>the</strong>r<br />

predictions. 34<br />

In August 1966, <strong>the</strong> Wea<strong>the</strong>r Bureau stated <strong>the</strong> following as its objectives for an operational<br />

satellite system: “(1) [t]he establishment and maintenance of a satellite system to<br />

obtain global observations on a regular basis, (2) meteorological observations from synchronous<br />

altitude, and (3) global observations of atmospheric structure needed for<br />

numerical wea<strong>the</strong>r forecasting.” [II-6] The first objective was met by continuing improvements<br />

in <strong>the</strong> TIROS series of low-altitude satellites, which were flown from 1966 to 1969.<br />

NASA launched an Improved TIROS Operational Satellite (ITOS) in January 1970. 35<br />

31. The ATS cameras provided pictures every thirty minutes, compared to once or twice a day from <strong>the</strong><br />

TIROS Operational System. For a discussion of <strong>the</strong> usefulness of continuous coverage, see W.L. Smith et al., “The<br />

Meteorological Satellite: Overview of 25 Years of Operation,” Science 231 (January 31, 1986): 455–62.<br />

32. Hill, Wea<strong>the</strong>r from Above, pp. 23–26, 29–32.<br />

33. Ibid., pp. 33–35.<br />

34. James C. Fletcher to Stuart Eizenstat, “Possible Initiatives,” February 16, 1977, suggests that NASA<br />

hoped that sounding instruments would lead to a major new research initiative. Pamela E. Mack, “Cloudy Seeing:<br />

Developing New Sensors for Wea<strong>the</strong>r Satellites,” paper presented at <strong>the</strong> Society for <strong>the</strong> <strong>History</strong> of Technology’s<br />

annual meeting, London, England, August 1996.

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