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Temporal variations in the linkage between the net ecosystem exchange of water vapour and CO2 over boreal forests in eastern Siberia
http://hdl.handle.net/2237/24075
http://hdl.handle.net/2237/240750ded1e71-5174-4d14-bbe2-0eafe280f026
名前 / ファイル | ライセンス | アクション |
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10_1002eco_1449.pdf (1.4 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2016-05-02 | |||||
タイトル | ||||||
タイトル | Temporal variations in the linkage between the net ecosystem exchange of water vapour and CO2 over boreal forests in eastern Siberia | |||||
言語 | en | |||||
著者 |
Kotani, Ayumi
× Kotani, Ayumi× Kononov, Alexander V.× Ohta, Takeshi× Maximov, Trofim C. |
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アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
権利 | ||||||
言語 | en | |||||
権利情報 | This is the peer reviewed version of the following article: [Kotani, A., Kononov, A. V., Ohta, T. and Maximov, T. C. (2014), Temporal variations in the linkage between the net ecosystem exchange of water vapour and CO2 over boreal forests in eastern Siberia. Ecohydrol., 7: 209–225. doi:10.1002/eco.1449], which has been published in final form at [http://doi.org/10.1002/eco.1449]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving. | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | boreal forest | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Siberia | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | evapotranspiration | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | CO2 exchange | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | water use efficiency | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | This study investigated evapotranspiration and CO2 exchange, observed by the eddy covariance method, over two larch-dominated forests, in the middle part of the Lena basin, eastern Siberia. Compared with the Spasskaya Pad (SP) forest, the Elgeeii (EG) forest had more plant biomass and a soil texture that allowed for larger water retention. Observations in three growing seasons revealed that the two sites had similar seasonal patterns of meteorological conditions and almost the same total evapotranspiration; however, the net and gross uptakes of CO2 at the EG forest were 1·61 and 1·31 times those at the SP forest, respectively. The difference in aboveground biomass was probably responsible for the higher productivity at EG. Less aboveground biomass would result in less transpiration by trees at SP, which would be compensated for in total evapotranspiration by soil evaporation and transpiration by the forest floor vegetation. It is likely that forest transpiration is commonly optimized to the same level of evapotranspiration under similar meteorological conditions through differences in the contributions of evapotranspiration from the forest floor vegetation and the soil water availability. Water use efficiency (WUE) displayed different patterns, reflecting the seasonal variations in each flux. Seasonal sequences in the WUE at EG indicated a midsummer depletion, which is commonly observed in forest ecosystems under a broad climate. Daily variation corresponding to the vapour pressure deficit and the cloud cover conditions (reduced solar radiation) was also observed. In contrast, WUE was relatively invariable at the seasonal and daily scales at SP. Copyright © 2013 John Wiley & Sons, Ltd. | |||||
言語 | en | |||||
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出版者 | Wiley | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
出版タイプ | ||||||
出版タイプ | AM | |||||
出版タイプResource | http://purl.org/coar/version/c_ab4af688f83e57aa | |||||
DOI | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.1002/eco.1449 | |||||
ISSN | ||||||
収録物識別子タイプ | PISSN | |||||
収録物識別子 | 1936-0592 | |||||
書誌情報 |
en : Ecohydrology 巻 7, 号 2, p. 209-225, 発行日 2014-04 |
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著者版フラグ | ||||||
値 | author | |||||
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識別子 | http://doi.org/10.1002/eco.1449 | |||||
識別子タイプ | DOI | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/24075 | |||||
識別子タイプ | HDL |