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solar radiation, like the greenhouse gas increase, is expected
to cause global warming. In the stratosphere, however, the two
effects produce temperature changes of opposite sign. A monitoring
program that would augment long term observations of tropospheric
parameters with similar observations of stratospheric parameters
could separate these diverse climate perturbations and perhaps
isolate a greenhouse footprint of climate change. Monitoring global
change in the troposphere is a key element of all facets of the
United States Global Change Research Program (USGCRP), not just of
the study of solar influences on global change. The need for
monitoring the stratosphere is also important for global change
research in its own right because of the stratospheric ozone
layer.
There are no firm plans at present to implement the primary
recommendation of this report, a program of continuous monitoring
of solar irradiance to provide the data needed to diagnose and
interpret solar influences on climate change. Because current solar
radiometric techniques are insufficiently accurate, ensuring data
continuity over many decades will require a series of space based
observations with sufficient temporal overlap for calibration
transfer and prevention of data loss from instrument failure. This
measurement program may well be precluded by the dearth of access
to space.
Scientific Conclusions
Q: Do solar variations directly force global surface
temperature?
A: Yes.
Inexorable change is predicted for the biosphere, that sphere of
the terrestrial global environment where life exists. It is
imperative to reliably detect, understand, and predict climate
change arising from increasing greenhouse gases and aerosols in the
Earth's atmosphere. This requires that natural climate forcing,
particularly solar variability, also be detected and understood. In
the study of solar influences on global change, determining the
extent to which solar influences modify global surface temperature
is a matter of the highest priority.
Energy from the Sun sustains life on Earth. By far the dominant
energy input is the visible solar radiation that heats the Earth's
land