Measurements of landscape-scale methane emission were made over an aapa mir
e near Kaamanen in Finnish Lapland (69 degrees 8' N, 27 degrees 16' E, 155
m ASL. Emissions were measured during the spring thaw, in summer and in aut
umn. No effect of water table position on CH4 emission was found as the wat
er table remained at or above the surface of the peat. Methane emission flu
xes increased with surface temperature from which an activation energy of -
99 kJ mol(-1) was obtained. Annual emission from the site, modelled from te
mperature regression and short-term flux measurements made in three separat
e years, was calculated to be 5.5 +/- 0.4 g CH4 m(-2) y(-1) of which 0.6 +/
-0.1 g CH4 m(-2) y(-1) (11%) was released during the spring thaw which last
ed 20 to 30 days.
The effect of global warming on the CH4 budget of the site was estimated us
ing the central scenario of the SILMU (Finnish Research Programme on Climat
e Change) model which predicts annual mean temperature increases of 1.2, 2.
4 and 4.4 degreesC in 2020, 2050 and 2100, respectively. Maximum enhancemen
ts in CH4 emission due to warming were calculated to be 18, 40 and 84% for
2020, 2050 and 2100, respectively. Actual increases may be smaller because
prediction of changes in water table are highly uncertain.