Estimating methane emissions using vegetation mapping in the taiga–tundra boundary of a north-eastern Siberian lowland

作者：Tomoki Morozumi, Ryo Shingubara, Rikie Suzuki, Hideki Kobayashi, Shunsuke Tei, Shinya Takano, Rong Fan, Maochang Liang, T. C. Maximov, Atsuko Sugimoto · 发表于：Tellus B · 年份：2019 · DOI：10.1080/16000889.2019.1581004 · 被引用次数：24 · 研究领域：Climate change and permafrost、Peatlands and Wetlands Ecology、Cryospheric studies and observations

Taiga–tundra boundary ecosystems are affected by climate change. Methane (CH 4 ) emissions in taiga–tundra boundary ecosystems have sparsely been evaluated from local to regional scales. We linked in situ CH 4 fluxes (2009–2016) with vegetation cover, and scaled these findings to estimate CH 4 emissions at a local scale (10 × 10 km) using high-resolution satellite images in an ecosystem on permafrost (Indigirka lowland, north-eastern Siberia). We defined nine vegetation classes, containing 71 species, of which 16 were dominant. Distribution patterns were affected by microtopographic height, thaw depth and soil moisture. The Indigirka lowland was covered by willow-dominated dense shrubland and cotton-sedge-dominated wetlands with sparse larch forests. In situ CH 4 emissions were high in wetlands. Lakes and rivers were CH 4 sources, while forest floors were mostly neutral in terms of CH 4 emission. Estimated local CH 4 emissions (37 mg m −2 d −1 ) were higher than those reported in similar studies. Our results indicate that: (i) sedge and emergent wetland ecosystems act as hot spots for CH 4 emissions, and (ii) sparse tree coverage does not regulate local CH 4 emissions and balance. Thus, larch growth and distribution, which are expected to change with climate, do not contribute to decreasing local CH 4 emissions.