Feedbacks of Arctic Ecosystems to the Climate System Vegetation Responses of Energy and Greenhouse Gas Exchange to the Climate Change

Researchers:Yoshinobu Harazono and Hiroki Iwata
Funding Source: IARC/NSF
Collaborators: Masahito Ueyama (Osaka Prefecture Univ.), Toru Iwata (Okayama Univ.), Akira Miyata (National Institute for Agro-Environmental Sciences), Walter C. Oechel (San Diego State Univ.), Kazuhito Ichii (Fukushima Univ.), John Kimball (Univ. of Montana)

The project goals are 1) To improve our understanding of the effects of changing permafrost on the regional hydrology and greenhouse gas budget, by continuous energy and trace gas flux observations at arctic and subarctic ecosystems. 2) To reveal the key parameters controlling carbon and energy budget of arctic and subarctic ecosystems, by comparing observed data and tuned process-based models such as BIOME-BGC, resulting in the future contributions of larger-scale climate estimation.

We continue the long-term flux observations of energy, CO2, and water vapor by the eddy correlation method and methane by the gradient method throughout the year in a black spruce forest in interior Alaska. The compiled data are applied to examine the key parameters controlling the energy and carbon exchange in the ecosystem. The ecosystem process model is improved by applying the observation data. Also, the data are provided for scientific purposes and are shared among ecosystem model study groups.

A unique observation site, which is the only tower site operated throughout the year in the high-latitude boreal ecosystem, is kept by IARC to reduce uncertainties in hydrology and carbon cycle in the high-latitude ecosystem. The observed data are complied and shared among model study groups. The compiled data and examined key parameters are applied to improve the tuned process-based ecosystem model, and the future changes in hydrology and carbon cycle are estimated.

The observed data are unique to high-latitude ecosystems. The data are complied and shared among model study groups. Also the key parameters are synthesized with the process-based model, resulting in better estimations of future hydrology and carbon cycles in high-latitude ecosystems.