Net ecosystem exchange (NEE) of carbon dioxide was measured at treeline for
est and fen tundra sites near Churchill, Canada during three consecutive gr
owing seasons (1997-1999). Although both sites demonstrated a net uptake of
CO2 in each of the years, there was considerable variation in the flux bet
ween sites and between years. Mean daily NEE at the forest varied from -1.5
(+/-0.25 SD) g CO2 m(-2) d(-1) in 1997 to -7.3 (+/-0.39) g CO2 m(-2) d(-1)
in 1999. The fen mean daily NEE varied from -1.1 (+/-0.36) g CO2 m(-2) d(-
1) in 1997 to -3.1 (+/-0.50) g CO2 m(-2) d(-1) in 1998. Integrated over the
65-d measurement period the forest was a net sink of -100, -313, and -478
g CO2 m(-2) in 1997, 1998, and 1999, respectively, and the fen net sink was
-73, -202, and -38 g CO2 m(-2), respectively. Interannual variations in th
e fen NEE were closely related to water table draw-down (soil wetness), the
forest NEE was unaffected by water table change. The forest seasonally cum
ulative NEE was closely associated with timing of snowmelt and accumulated
heat content prior to leaf-out. Earlier snowmelt and greater heat accumulat
ion produced a larger growing season sink. It is likely these events also i
nfluenced the fen NEE, but the relationship is complicated by water table e
ffects. These results suggest that carbon dioxide exchange varies considera
bly across the northern treeline, and that there may be an important biosph
eric feedback between climate warming, treeline advance, and carbon cycling
.