Climate is one of the conditions which permits, inhibits, retards or e
nhances certain responses in the geomorphic environment. Components of
climate important to geomorphic processes include (1) the duration an
d character of climate episodes, i.e., the variation of the various cl
imate parameters during any such period, and (2) the nature of discont
inuities at both a climate episode's beginning and end, i.e., the magn
itude of change and the rate of change occurring at the time of discon
tinuity. We will evaluate changes in the climate character over the Ho
locene, compare that to that observed during the instrumental period a
nd, in turn, compare to predicted changes for an atmosphere with twice
today's carbon dioxide concentration.