N. Vanbreemen et al., IMPACTS OF ELEVATED CARBON-DIOXIDE AND TEMPERATURE ON A BOREAL FORESTECOSYSTEM (CLIMEX PROJECT), ECOSYSTEMS, 1(4), 1998, pp. 345-351
To evaluate the effects of climate change on boreal forest ecosystems,
both atmospheric CO2 (to 560 ppmv) and air temperature (by 3 degrees-
5 degrees C above ambient) were increased at a forested headwater catc
hment in southern Norway. The entire catchment (860 m(2)) is enclosed
within a transparent greenhouse, and the upper 20% of the catchment ar
ea is partitioned such that it receives no climate treatment and serve
s as an untreated control. Both the control and treatment areas inside
the greenhouse receive deacidified rain. Within 3 years, soil nitroge
n (N) mineralization has increased and the growing season has been pro
longed relative to the control area. This has helped to sustain an inc
rease in plant growth relative to the control and has also promoted in
creased N export in stream water. Photosynthetic capacity and carbon-n
itrogen ratio of new leaves of most plant species did not change. Whil
e the ecosystem now loses N, the long-term fate of soil N is a key unc
ertainty in predicting the future response of boreal ecosystems to cli
mate change.