Ds. Lemmen et al., IMPACTS OF FUTURE CLIMATE-CHANGE ON THE SOUTHERN CANADIAN PRAIRIES - A PALEOENVIRONMENTAL PERSPECTIVE, Geoscience Canada, 24(3), 1997, pp. 121-133
Water and soil are critical to the prosperity of the southern Canadian
prairies. Both have been strongly influenced by historic climate vari
ability, and by even more significant climate changes that have occurr
ed during the Holocene.These observations, together with general circu
lation model projections of increasing aridity in this region, raise c
oncerns about the potential impacts of future climate change. Collabor
ative, multidisciplinary research conducted over the past five years a
s part of the Palliser Triangle Global Change Project has focussed on
geoscientific aspects of climate change in the driest portion of the C
anadian prairie provinces. Reconstruction of past climates, based on m
ultiple paleolimnological indicators (plant macrofossils, diatoms, ost
racodes, algal pigments, sedimentology, mineralogy, and stable isotope
geochemistry), demonstrates that the historic record of roughly 100 y
ears does not adequately capture the range of climatic variability obs
erved during even the last 2000 years. The response of hydrologic and
geomorphic systems to past changes in climate documents a surprisingly
dynamic landscape. The best analogues for projected future climates f
eature a regional water table more than 4 m below its present level an
d enhanced wind erosion. The paleoenvironmental record highlights the
susceptibility of water and soil resources to climate-induced impacts
that are likely to adversely affect human activities in the region ove
r the next century.