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1993-05-03
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PUBLIC INFORMATION OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. TELEPHONE (818) 354-5011
FOR IMMEDIATE RELEASE June 23, 1988
When a rocket rose into the sky north of Los
Angeles in a dazzling evening launch 10 years ago this week,
the satellite it carried was destined to usher in a new era
of space research focusing on unsolved questions of the
world's oceans and weather.
The satellite, Seasat, tested a payload of advanced
sensing instruments. During its 3-1/2-month mission, Seasat
collected what scientists have called an explosion of
oceanographic information -- comparable to a century's worth
of observations from a fleet of ships.
Because of the way it showed how space sensors
could be used in oceanography, Seasat also became parent to a
new generation of missions planned by a handful of countries.
Those missions could provide answers to some of the
world's most baffling -- and threatening -- weather
phenomena.
Seasat's influence has reached beyond oceanography
to affect other research work at JPL. Instruments derived
from the 10-year-old mission are due to fly to Venus and Mars
on interplanetary probes in next year's Magellan mission and
1992's Mars Observer.
An international symposium celebrating Seasat's ▄j▄î
launch anniversary will be hosted in London next Tuesday
through Thursday (June 28-30) by the British National Space
Centre. Gene Giberson, JPL's project manager for Seasat,
and Peter Woiceshyn, a JPL scientist who has worked on Seasat
continuously since its inception, will be featured speakers.
"The impacts Seasat has had on both Earth science
studies and even deep-space research at JPL have been
remarkable," said Giberson. "This single mission has produced
offspring that have shaped the future direction of many of
our programs."
Launched on June 26, 1978, on an Atlas-Agena rocket
from Vandenberg Air Force Base, Calif., Seasat carried a
payload of five scientific instruments unlike any package on
any previous remote-sensing satellite.
Previous Earth remote-sensing satellites were
generally equipped with a camera and perhaps one or two other
passive instruments.
Seasat, on the other hand, carried a complex array
of active sensing devices, such as radars and other
microwave instruments, to monitor a broad range of
oceanographic phenomena.
(Passive sensors simply collect natural energy such
as sunlight reflected by the Earth -- similar to a camera
taking pictures in available light. Active sensors such as
radars emit energy of their own to collect data -- somewhat
like a camera equipped with its own flash attachment.)
Among the experimental instruments Seasat pioneered ▄j▄
were a synthetic aperture radar, which provided highly
detailed images of ocean and land surfaces; a radar
scatterometer, to measure near-surface wind speed and
direction; a radar altimeter, to measure the height of the
ocean surface and waves; and a scanning multichannel
microwave radiometer, to measure surface temperature, wind
speeds and sea ice cover. The satellite also carried a
passive visual and infrared radiometer to provide supporting
data for the other four experiments.
With Seasat's proof that the instruments would work
as intended, other projects at JPL and at space centers
around the world have borrowed from the mission's concepts.
Key among them is a host of international projects
scheduled over the next decade to probe the world's oceans
and weather in unprecedented detail. Scientists say those
missions can help solve currently baffling questions that
would provide a variety of benefits with a possibly enormous
cost savings -- and could avert potential disasters.
El Nino, an unusual water warming in the eastern
Pacific Ocean in 1982 and 1983, for example, caused billions
of dollars in damage and considerable loss of life.
Scientists have also been puzzled by an increase of carbon
dioxide in the atmosphere, which could have severe
consequences on plants and animal life. Missions derived from
Seasat are expected to help scientists understand both
phenomena.
In addition, the new generation of oceanographic ▄j▄î
missions is expected to provide important, cost-saving aids
for such industries as fishing, shipping and offshore oil
production, and for agencies such as the National Oceanic and
Atmospheric Administration (NOAA) and the U.S. Navy.
Among the new projects are two NASA efforts managed
by JPL -- TOPEX/Poseidon and the NASA Scatterometer (NSCAT).
TOPEX/Poseidon, a joint satellite mission with the
French space agency, is scheduled for a late 1991 launch on
an Ariane rocket. It will map the circulation of the world's
oceans using a radar altimeter.
NSCAT is a second-generation instrument being
developed to measure wind speed and direction over the
oceans' surfaces. A proposal to fly NSCAT as part of the
payload on Japan's planned Advanced Earth Observation
Satellite (ADEOS) is currently under review.
Both TOPEX/Poseidon and NSCAT are intended to
support oceanographic studies during the 1990s under the
World Ocean Circulation Experiment (WOCE) and the Tropical
Oceans Global Atmospheres Experiment (TOGA). These decade-
long programs, sponsored by the World Climate Research
Program, involve studies at and below the ocean surface in
all parts of the world's seas.
Still another U.S. mission whose heritage can be
traced to Seasat is Geosat, a U.S. Navy satellite launched in
1985 with an altimeter similar to Seasat's.
International projects scheduled for the near
future include the European Space Agency's first remote- ▄j▄î
sensing satellite, Earth Resources Satellite 1 (E-ERS-1), due
for launch in 1990; Japan's Earth Resources Satellite 1
(J-ERS-1), scheduled for a 1992 launch; Japan's ADEOS,
proposed for launch in 1993; and the international Radarsat,
a proposed 1994 mission that would be a cooperative venture
between Canada and the United States.
Seasat's impacts, however, have not been limited to
satellite oceanography. Instruments that are direct
descendants of those in Seasat's payload have found their way
into a variety of other NASA missions at JPL.
One of the most prominent is JPL's Shuttle Imaging
Radar (SIR), a series of synthetic aperture radar experiments
flown on NASA's Space Shuttle. They are direct follow-ons of
Seasat's synthetic aperture radar, which marked the first
time NASA had flown that advanced radar instrument in space.
The first and second experiments in the series --
SIR-A, which flew on a shuttle mission in 1981, and SIR-B, a
shuttle payload in 1984 -- offered scientists several
unexpected discoveries. During airborne tests, for example,
SIR-A pierced cloud-covered rain forests of Guatemala to
reveal previously unknown agricultural canals dug by the
ancient Maya. SIR-B "saw" through the sands of Egypt to
produce a picture of a riverbed buried for many centuries.
JPL is currently working on SIR-C, the third SIR
experiment, slated for a 1991 shuttle mission. Also planned
is an advanced radar system that will be flown on an Earth
Observing System (Eos) platform as part of NASA's Space ▄j▄î
Station program in the late 1990s.
A radar like the one first flown on Seasat is also
set to go into deeper space on the NASA/JPL Magellan mission
to Venus in April 1989. Magellan will use a synthetic
aperture radar to pierce Venus' dense cloud cover to provide
the most complete, highest-resolution images of the planet's
surface ever made.
Another planetary mission benefiting from Seasat is
Mars Observer, scheduled for launch in 1992. That spacecraft
will orbit the red planet to conduct extensive studies of the
Martian surface with instruments including an altimeter
derived from the Seasat payload.
At JPL, Giberson was Seasat project manager; Dr.
James A. Dunne was project scientist. S. W. McCandless Jr.
was Seasat program manager at NASA Headquarters in
Washington, D.C.
Seasat was funded by NASA's Office of Space Science
and Applications.
#####
6-23-88 FOD
# 1203