Interannual variation of evapotranspiration in an eastern Siberian larch forest

被引：10
作者：
Xue, Bao-Lin [1 ]
Komatsu, Hikaru [1 ,2 ]
Kumagai, Tomo'omi [1 ,3 ]
Kotani, Ayumi [4 ]
Otsuki, Kyoichi [1 ]
Ohta, Takeshi [4 ]
机构：
[1] Kyushu Univ, Fac Agr, Fukuoka 812, Japan
[2] Natl Taiwan Univ, Sch Forestry & Resource Conservat, Taipei 10764, Taiwan
[3] Duke Univ, Dept Civil & Environm Engn, Durham, NC 27706 USA
[4] Nagoya Univ, Grad Sch Bioagr Sci, Nagoya, Aichi 4648601, Japan
来源：
HYDROLOGICAL PROCESSES | 2012年 / 26卷 / 15期
基金：
日本科学技术振兴机构;
关键词：
boreal deciduous forest; evapotranspiration; interannual variation; leaf expansion; leaf fall; eastern Siberia; JACK PINE FOREST; BOREAL FOREST; CANOPY CONDUCTANCE; SEASONAL-VARIATION; FLUX MEASUREMENTS; PAIRED-CATCHMENT; GROWING-SEASON; ENERGY FLUXES; WATER-BALANCE; EVAPORATION;
D O I：
10.1002/hyp.9195
中图分类号：
TV21 [水资源调查与水利规划];
学科分类号：
081501 ;
摘要：
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 20032006 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. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码：2360 / 2368
页数：9
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