Since 1996 a broad range of publications has been produced by Canadian geom
orphologists and hydrologists. These publications have been distributed in
journals with national and international circulations. Although there remai
ns a major focus on the study of observable processes in pluvial, aeolian,
coastal and slope environments there is also a strong, historical component
to explanations of landforms, landform assemblages and sedimentary sequenc
es. Some of these histories have incorporated the effects of high-magnitude
(catastrophic) events, some of which may have no modern analogues. Perspec
tives on the interactions among microclimatic variables, including changes
induced by human actions, continue to evolve. Forest clearance and its effe
cts on evaporation rates, water-table levels and timing of snowmelt, the hu
man use of wetlands and release of methane and carbon dioxide, will continu
e to demand the attention of scholars interested in explaining future clima
tic scenarios.