Ecosystem modeling of methane and carbon dioxide fluxes for boreal forest sites

Predicted daily fluxes from an ecosystem model for water, carbon dioxide, a nd methane were compared with 1994 and 1996 Boreal Ecosystem-Atmosphere Stu dy (BOREAS) field measurements at sites dominated by old black spruce (Pice a mariana (Mill.) BSP) (OBS) and boreal fen vegetation near Thompson, Man. Model settings for simulating daily changes in water table depth (WTD) for both sites were designed to match observed water levels, including predicti ons for two microtopographic positions (hollow and hummock) within the fen study area. Water run-on to the soil profile from neighboring microtopograp hic units was calibrated on the basis of daily snowmelt and rainfall inputs to reproduce BOREAS site measurements for timing and magnitude of maximum daily WTD for the growing season. Model predictions for daily evapotranspir ation rates closely track measured fluxes for stand water loss in patterns consistent with strong controls over latent heat fluxes by soil temperature during nongrowing season months and by variability in relative humidity an d air temperature during the growing season. Predicted annual net primary p roduction (NPP) for the OBS site was 158 g C.m(-2) during 1994 and 135 g C. m(-2) during 1996, with contributions of 75% from overstory canopy producti on and 25% from ground cover production. Annual NPP for the wetter fen site was 250 g C.m(-2) during 1994 and 270 g C.m(-2) during 1996. Predicted sea sonal patterns for soil CO2 fluxes and net ecosystem production of carbon b oth match daily average estimates at the two sites. Model results for metha ne flux, which also closely match average measured flux levels of -0.5 mg C H4.m(-2). day(-1) for OBS and 2.8 mg CH4.m(-2). day(-1) for fen sites, sugg est that spruce areas are net annual sinks of about -0.12 g CH4.m(-2), wher eas fen areas generate net annual emissions on the order of 0.3-0.85 g CH4. m(-2), depending mainly on seasonal WTD and microtopographic position. Fen hollow areas are predicted to emit almost three times more methane during a given year than fen hummock areas. The validated model is structured for e xtrapolation to regional simulations of interannual trace gas fluxes over t he entire North America boreal forest, with integration of satellite data t o characterize properties of the land surface.