Our knowledge of global climate change has many uncertainties. Whether
global air temperature will increase, by how much, and when, are subj
ect to debate, but there is little doubt that tropospheric concentrati
ons of several trace gases are increasing. While possible increases in
the average air temperature is a product of these changes, the increa
ses in the trace gases alone will have an effect on agriculture. Incre
ases in the ambient concentrations of carbon dioxide are expected to h
ave a positive net effect on crop production. In contrast, any increas
es in the penetration of surface-level ultraviolet-B (280-320 nm) radi
ation, and known increases in surface ozone concentrations, are consid
ered to have adverse effects on certain crops. Our present knowledge o
f the joint effects on crops of elevated levels of carbon dioxide, ult
raviolet-B radiation and ozone, and possible alterations in air temper
ature and precipitation patterns, is virtually zero. Therefore, any pr
edictions of the effects of global climate change on agriculture are s
ubject to significant uncertainties. In contrast, coupling of climate
change (only temperature and precipitation) models to crop production
has led to a number of future scenarios. In spite of their present lim
itations, results from these efforts can be useful in planning for fut
ure agriculture.