Annual variation of methane emissions from forested bogs in West Siberia (2005–2009): a case of high CH4 and precipitation rate in the summer of 2007

• Main Authors: Sasakawa, M., Ito, A., Machida, T., Tsuda, N., Niwa, Y., Davydov, D., Fofonov, A., Arshinov, M.
• Format: Text
• Language: English
• Published: 2018
• Subjects: taiga; Siberia
• Online Access: https://doi.org/10.5194/acpd-10-27759-2010; https://www.atmos-chem-phys-discuss.net/acp-2010-777/

We have been conducting continuous measurements of CH 4 and CO 2 on a network of towers (JR-STATION: Japan–Russia Siberian Tall Tower Inland Observation Network) located in taiga, steppe, and wetland biomes of Siberia. Here we describe measurements from two forested bog sites, Karasevoe (KRS; 58°15′ N, 82°25′ E) and Demyanskoe (DEM; 59°47′ N, 70°52′ E), in West Siberia from 2005 to 2009. Although both CH 4 and CO 2 accumulation (ΔCH 4 and ΔCO 2 ) during nighttime (duration of 7 h beginning 21:30 LST) at KRS in July 2007 showed an anomalously high concentration, the higher ratios of ΔCH 4 /ΔCO 2 compared with those in other years indicate that a considerably more CH 4 flux occurred relative to the CO 2 flux in response to large precipitation recorded in 2007 (~2.7 mm d −1 higher than the climatological 1979–1998 base). Estimated seasonal CH 4 fluxes based on the ratio of ΔCH 4 /ΔCO 2 and the CASA 3-hourly CO 2 flux for the 2005–2009 period exhibited a seasonal variation with a maximum in July at both sites. Annual values of the CH 4 emission from the forested bogs around KRS (approx. 7.8×10 4 km 2 ) calculated from a process-based ecosystem model, Vegetation Integrative Simulator for Trace gases (VISIT), showed inter-annual variation of 0.54, 0.31, 0.94, 0.44, and 0.41 Tg CH 4 yr −1 from 2005 to 2009, respectively, with the highest values in 2007. It was assumed in the model that the area flooded with water is proportional to the cumulative anomaly in monthly precipitation rate.