Abstract
In a deciduous larch forest in eastern Siberia, the mean and standard deviation of the total evapotranspiration (E) during May to September (day of year (DOY)=121-274) for 2003-2006 were 181.5 and 26.4mm, respectively. The interannual variation (IAV) in the total E was caused by the IAV in E for the canopy-foliated period (DOY=164-253), not by the IAV in the dates of leaf expansion and leaf fall. For the years with higher total E, E in the canopy-foliated period was consistently higher, which corresponded to the higher soil water content in these years.
| Original language | English |
|---|---|
| Pages (from-to) | 2360-2368 |
| Number of pages | 9 |
| Journal | Hydrological Processes |
| Volume | 26 |
| Issue number | 15 |
| DOIs | |
| Publication status | Published - Jul 15 2012 |
All Science Journal Classification (ASJC) codes
- Water Science and Technology
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Xue, B. L., Komatsu, H., Kumagai, T., Kotani, A., Otsuki, K., & Ohta, T. (2012). Interannual variation of evapotranspiration in an eastern Siberian larch forest. Hydrological Processes, 26(15), 2360-2368. https://doi.org/10.1002/hyp.9195