201. Year-to-year differences in evapotranspiration from understory vegetation and whole ecosystem in an eastern Siberian larch forest
- Author
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Iida, Shinichi, Ohta, Takeshi, Matsumoto, Kazuho, Nakai, Taro, Kononov, Alexander V., Maximov, Trofim C., van der Molen, Michiel K., Dolman, Albertus J., Yabuki, Hironori, Iida, Shinichi, Ohta, Takeshi, Matsumoto, Kazuho, Nakai, Taro, Kononov, Alexander V., Maximov, Trofim C., van der Molen, Michiel K., Dolman, Albertus J., and Yabuki, Hironori
- Abstract
We measured the evapotranspiration from the understory vegetation and the whole ecosystem of a Siberian larch forest on the forest floor and above the forest canopy, respectively, using the eddy-covariance method, and obtained the year-to-year difference in evapotranspiration during the early (from 1st to 10th), middle(11th to 20th) and late (21th to the end) periods of month. The year-to-year differences in evapotranspiration from whole ecosystem and understory vegetation were in the range from -11.0 mm to 9.5 mm and from -2.4 mm to 4.7 mm, respectively. These values explained from 20% to 30% of monthly mean evapotranspiration, and thus significant differences were found in this site. To clarify the factor controlling the year-to-year difference in evapotranspiration, we analyzed the relationships among the year-to-year differences in evapotranspiration, radiative and advective terms of Penman–Monteith equation. As a result, due to the small value of decoupling factor of this forest, the most important factor was the year-to-year difference in the advective term. We found that the difference in vapor pressure deficit resulting in the change of the surface conductance was important for year-to-year difference in the advective term in this site.
- Published
- 2016