Micrometeorological measurements of methane flux at a boreal forest in central Alaska
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概要
- 論文の詳細を見る
Methane (CH_4) flux at a black spruce forest in central Alaska was determined by applying the three types of modified gradient method. One type used the eddy diffusivity obtained by CO_2 flux and CO_2 gradient. Others established the flux gradient relationship assuming Monin-Obukhov similarity. The wind speed and temperature profile functions were corrected for the influence of the roughness sublayer, and then applied to the modified gradient methods. More than 70% of the data were rejected by the strict quality control and a continental climate, such as calm wind. Although the diurnal variations of CH_4 flux by the three methods were different, the seasonal variation showed similar tendency; a weak emission on snowpack, an obvious emission around spring thaw, and CH_4 uptake in the late growing season. As calculated CH_4 flux was in the same range as with previous studies conducted by the chamber measurement.
- 国立極地研究所の論文
著者
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Ohtaki Eiji
Graduate School Of Natural Science And Technology Okayama University
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Ueyama Masahito
International Arctic Research Center, University of Alaska
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Harazono Yoshinobu
International Arctic Research Center, University of Alaska
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Okada Ryo
Institution of Geosciences, University of Tsukuba
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Nojiri Atsushi
Graduate School of Natural Science and Technology, Okayama University
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Miyata Akira
National Institute of Agro-Environmental Sciences
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Okada Ryo
Institution Of Geosciences University Of Tsukuba
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Nojiri Atsushi
Graduate School Of Natural Science And Technology Okayama University
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Harazono Yoshinobu
International Arctic Research Center University Of Alaska
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Ueyama Masahito
International Arctic Research Center University Of Alaska
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Miyata Akira
National Institute For Agro-environmental Sciences
関連論文
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