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 |
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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