As described in the paper by John Mather and Tom Kelsall, the
COBE (Cosmic Background Explorer) project is designed to
make a substantial improvement in our knowledge of the condition in the universe at large red shifts. The focus of the
mission is to study attributes of the primeval cosmic background radiation and to set limits on the universal radiation
energy density at shorter wavelengths - radiation emanating
from distant sources but at later times than the primeval
fireball. In introducing the accompanying paper, I thought
it might be worthwhile to describe the scientific strategy driving
the COBE mission.
The COBE mission has been under study since 1974 by a
team of scientists consisting of S. Gulkis (Jet Propulsion Laboratory), M. Hauser (NASA Goddard Space Flight Center), J.
Mather (NASA), G. Smoot (University of California, Berkeley),
R. Weiss (MIT), and D. Wilkinson (Princeton). The team
members have been involved in ground based, balloon borne
and airborne experiments to measure the background radiation
and are keenly aware of limitations of these platforms and the
arguments in favor of a space borne experiment. It is worth
repeating these arguments:
(1) Freedom from atmospheric emission and fluctuations
in the emission.
(2) Full sky coverage with a single instrument.
(3) A benign and controlled thermal environment to reduce
systematic errors.
(4) The ability to perform absolute primary calibration in
flight without the necessity of windows to avoid condensation
of the atmosphere on calibrators and instruments.
(5) Sufficient time both to perform tests for systematic
errors and to gain the increase in sensitivity permitted by
extended observation time.
In planning the COBE mission, the team came to know the
peculiar difficulties of carrying out a space mission. Aside from
the ever present problem of maintaining the project within an
assigned budget, the mission had to be designed so that it would
still be the "right thing to do" in the field after the 5 to 10
years it takes between initial planning and execution. One had
to anticipate the progress that could still be made by using
other platforms and blend this with the fact that in the space
mission one would be dealing with technology that was 3 to
5 years behind the state of the art (to allow time for space
quahfication).
In an interim report to NASA in 1977, the conclusion of the
team was that the technology was sufficiently advanced and the
instrument systematic noise sources were well enough
understood or controllable so that the major limitation in a
space mission to perform precision measurements of the background would be the "noise" produced by the local astrophysical environment. The complement of instruments chosen
for the mission, as well as the need for full sky coverage and
extended observation time, are based primarily on the hope
that the local astrophysical "noise" can be discriminated from
the cosmic background by its peculiar set of spectra and anisotropic angular distribution. In the COBE mission, the data
from one instrument truly serves to enhance the value of that
from another. Examples of this are discussed in the
accompanying paper.